A GAZETTEER OF THE STATE OF NEW JERSEY. COMPREHENDING A GENERAL VIEW OF ITS PHYSICAL AND MORAL CONDITION, TOGETHER WITH A TOPOGRAPHICAL AND STATISTICAL ACCOUNT OF ITS COUNTIES, TOWNS, VILLAGES, CANALS, RAIL ROADS, &c. ACCOMPANIED BY A MAP. 8 BY THOMAS F. QORDON. rtnton: PUBLISHED BY DANIEL FENTON. John C. Clark, Printer, Philadelphia. 1834. Entered by THOMAS F. GORDON, according to Act of Congress, in the year 1834, in the Clerk's Office of the District Court for the Eastern District of Pennsylvania. ADVERTISEMENT. THE author of the following work has sought to present to the public, a full and correct portraiture of the State in the year 1833. To this end, he has, personally, visited almost every portion of it; communed with' many of its most distinguished and enlightened citizens, and collected, from numerous but scattered sources, a mass of usefiul and curious information, which must prove alike grateful to the present and succeeding generations. Errors will undoubtedly be discovered in the work; for such a work is peculiarly liable to them; being exposed, not only to the misconceptions of the author, but, to those of his thousand informants. Distance of places from each other, and the area of the townships and counties are, specially, subject to misstatement. The first has been given from the returns of the General Post-Office, measures upon the map, and verbal information of residents; the only and best sources, save actual admeasurement. The area of the townships has been obtained from calculation of their contents, as delineated on Mr. Gordon's map, by means of a reticulated scale of square miles. The result corresponds, so nearly, with the returns of the assessors of such townships, as contain no unimproved lands, as to give considerable confidence in its approximation to the truth. It must be observed, however, that this area comprises roads, lakes, ponds, marshes and, in a word, every thing within the lines. The abstract which has been given of the laws relating to the administration of the government, generally, and of the counties and townships, specially, will appear, to many, trite and familiar; but to the great mass of the people, particularly, to the rising generation, it will not prove the least acceptable portion of the work. To those about to enter on the duties of the citizen, it will commu iv ADVERTISEMENT. nicate much valuable knowledge; and will be useful to all, for occasional reference; comprising, in a small compass, matter of daily interest, which must, elsewhere, be sought, in many volumes. More of this species of information might have been usefully given; but, the volume collected, exceeds, by one-third, the quantity originally proposed; and to get it within the size of a convenient manual, resort has been had to a small type for the prefatory chapters. To the many gentlemen to whom the author is indebted for communications, he tenders his unfeigned thanks; and solicits from them, and others, such corrections and additions as may render the next edition of his work, still more valuable. Philadelphia, January 1, 1834. GAZETTEER OF NEW JERSEY. PREFATORY CHAPTER. PART I. Containing a Physical View of the State. I. General Boundary.-II. Principal Divisions.-III. Southern and Alluvial Division.Bounds-Surface-Nevisink Hills-Sandy Hook-Sea Beach-Bays or LagunesSoil: Forest-Pine Lands-Oak-Cedar Swamp-Marl-Ferruginous Sand-Proportions of Marl used in Agriculture.-Cultivation of the Alluvial District.-Bog Ore-Streams.-IV. Middle and Secondary District: Bounds-A.rea-FormationTrap Ridges-Bergen Ridge-First and Second Mountains-Bituminous CoalMountains from Springfield to Pluckemin.-Pompton Plain: Abundance of Minerals there-Ridges extending to the Delaware-Character of the surrounding Country-Quarries of Freestone near Princeton-Sandy Hill-Primitive Rocks near Trenton.-Copper Mines: at Belleville, Brunswick, Somerville, Greenbrook.V. Mountainous District: Extent-Blended Geological Formation-Limits-Primitive Ridges, Minerals of-Tongue of Transition Formation, Minerals of-Primitive resumed-Valley of the Wallkill, or of Sparta-Singular Geology and Mineralogy-Valley of Paulin's Kill-31ternation of Slate and Limestone-Blue or Kittatinney Mountains-Transition Limestone on Delaware River-Precious Marbles-Manganese-Rivers and Lakes of the Third Section-Timber of the Middle and Northern Sections.-VI. Turnpike Roads.-VII. Rail Roads: Camden and Amboy, West Jersey, Patterson and Hudson, Patterson Junction, Patterson and Fort Lee, Elizabethtown and Somerville, New Jersey, New Jersey, Hudson and Delaware, Delaware and Jobstown.-VIII. Canals Morris, Delaware and Raritan, Manasquan, Salem.-IX. Population-Increase-Tables-Slavery.-X. Statistical Table. XI..griculture, Manufactures and Commerce.--XII. Climate. I. The State of New Jersey is bounded on the N. E. by Orange and Rockland counties, of the State of New York; on the E. by Hudson River and Bay, Staten Island Sound, Raritan Bay and the Atlantic Ocean; on S. E. and S. by the Atlantic; on S. W. by the Delaware Bay, dividing it from the State of Delaware; and on the W., and N. W. by the Delaware River, separating it from Pennsylvania. The N. E. line from Carpenter's Point, at the mouth of the Nevisink, or Mackackomack River, in north lat. 410 21', to a point on the Hudson River, in 41~ north latitude; is in length 45 miles; the E. 60; the S. E. from Sandy Hook to Cape May, 120; and the S. W., W. and N. W. from Cape May to Carpenter's Point, 220 milesmaking the extent of its exterior limit 445 miles. The extreme length of the State, by a line almost due north from Cape May, to the northern angle on the Delaware, is 164 miles; its greatest breadth due E. and W. through Salem, Gloucester, Burlington and Monmouth counties, about 75 miles; and through Warren, Sussex, Morris and Bergen counties, to the extreme N. E. point, on the Hudson River, about 60 miles. It may be crossed, however, by a direct line from S. W. to N. E., from Bordentown to South Amboy, in about 30 miles. The nearest approximation we can make to its area, measuring the map by a reticulated scale of square miles, is about 7,276 square miles, or 4,656,330 acres, contained between 380 58' and 410 21' northern latitude.* II. This area is distributed into three strongly marked divisions; the alluvial and southern; the secondary, hilly and middle; and the mountainous and northern, comprising primitive and transition formations. III. The triangular peninsula, or southern division, bordered on the S. and E. by Delaware Bay and the Ocean, on the N. and W. by the Delaware River, about 110 miles in length, and 75 in breadth, is entirely alluvial. South of the Nevisink Hills, the surface seldom rises 60 feet above the sea. Those hills, adjacent to the Ocean, are 310 feet above its level; and stand where the waves formerly rolled, resting in some places on banks of oyster shells and other marine relics, blended with clay and * Morse gives 8,320 square miles, or 5,324,800 acres; Smith's Hist. N. J. 4,800,000 acres and Darby 6,851, square miles, or 4,384,000 acres. A 2 GENERAL DESCRIPTION. sea mud. A sandy earth, highly coloured by oxide of iron, and imbedding reddish brown sand and puddingstone, cemented by iron, composes the higher strata; and large rocks and beds of ferruginous sandstone, apparently in place, of a more recent formation than the alluvial below, containing sufficient metal to be called an ore of iron, are of frequent occurrence. Particles of iron are blended with the sands of the beach; and some of the streams which descend from the top of the clay strata, are red with iron oxide. Efflorescences of the sulphates of iron and alumine, are often observed; and flame, proceeding from the spontaneous combustion of gases, generated, probably, in beds of sulphuret of iron, has been noticed here. The strata of the steep eastern declivity are exposed by frequent land slips. A small portion, only, of these hills is cultivated. They are rough, broken, and covered with wood, in which deer still find covert. From their summit, a view is disclosed of the ocean, unrivalled in grandeur upon the seaboard of this State; and the coast on the N. E. and S. may be seen as far as the eye can reach. The land prospect, though not so extensive, is scarce less interesting. In this hill, on the side of a branch of the Nevisink River, is a remarkable cave, 30 feet long by 15 broad, divided into three apartments. The entrance and roof are low, the latter arched, and of soft rock, through which the water percolates; the bottom is of loose sand. Sandy Hook, east of, and divided from, the Nevisink Hills by a narrow bay, is six miles in length. It was formerly, and is now, isolated by a channel running from Shrewsbury River, which was first opened in 1778, closed in 1810, but reopened in 1830. The beach running northward several miles from Long Branch, invites to a promenade on the hard sand when the tide is low; but the wrecks of vessels, visible at short intervals, oppress the spectators with recollections of the perils of the sea. From the Hook, this beach extends 125 miles to Cape May, varying in width from half a mile to two miles, but broken in several places by channels communicating with the sea. South of Manasquan it covers a number of bays or salt water lakes, of which Barnegat, Little Egg Harbour, and Great Egg Harbour, are the chief. West of these runs a belt of marsh, in some places from four to five miles wide, intersected by small rivers, with broad and shallow estuaries. The soil of this alluvial district consists of sand and clay, sometimes one overlaying the other; but frequently intimately blended, forming a tolerably fertile loam, which prevails on its northern and western border with a variable breadth. Above Salem, this breadth is from five to twelve miles, but below that town it is sometimes contracted to a mile. East of this strip of loam, and west of the marsh which girds the sea shore, lies an immense sandy plain, scarce broken by any inequality, and originally covered by a pine and shrub-oak forest-a great portion of which has been once, and some of it twice, cut over. There are many square miles on which there is not a human inhabitant, and where the deer, foxes and rabbits are abundant, and the wolf and the bear find a lair to protect their race from extirpation. But in many places the echo is awakened by the woodman's axe, and the louder din of the forge hammer, and the forest glares with the light of the furnace or glass house. In this sandy desert there are found veins of generous soil, which yield a compensatory crop of corn and rye to the labours of the husbandman. This immense forest covers probably four-fifths of the alluvial district; and forty years ago a large portion of it was not worth more than from six to ten cents the acre. There was little demand for the timber, oak being preferred for architectural and economical uses, nor was the land worth clearing for agricultural purposes. The establishment of furnaces and glass manufactories first gave additional value to the woodland near their locations; but for a while they made little apparent reduction of the vast wilderness. Then came the steamboats, which for some years traversed our waters, propelled by timber from New.Jersey, without sensibly diminishing the density of the forest. In a few years more, however, their number was doubled, trebled, quadrupled. Their huge maws, though fed with thousands of shallop loads of pine wood, were insatiable. The demand for fuel became immense; the almost worthless pine) lands rose rapidly in value, and the hitherto almost idle population of the sea-board, found abundant and profitable employment in supplying the growing markets. The introduction of anthracite coal diminished the consumption of oak wood as fuel, but increased that of pine, vast quantities of charcoal being required to ignite the fossil. Yet the invention of the simple portable culinary furnace increased the demand still more, thousands of these convenient utensils being constantly, during the summer months, fed by charcoal. These circumstances have produced an entire revolution in the value of pine lands. They have risen from ten SOUTHERN DIVISION. 3 cents, to an average price of six dollars the acre; and, where very well timbered, and convenient to market, bring from fifteen to twenty-five dollars. Indeed, the soil, denuded of the timber, is worth from four to sixteen dollars the acre, the purchaser looking to the growth of wood for profit on his investment. Where the forest has been felled, an extraordinary change takes place in the subsequent product. The oak springs up where the pine has flourished, and pine where the oak has grown. The second growth becomes fit for the axe, in a space varying from 25 to 40 years. Upon the clay and loam soils, oak grows abundantly; frequently of great size, and of quality much valued in the construction of ships. It is the common timber of the western border, and covers almost exclusively the central portion of the county of Cape May. In the sandy region, are extensive swamps which bear the beautiful and valuable white cedar, much sought for fencing, and which sells readily at from one to three hundred dollars the acre. Throughout a great portion of the alluvial district, from four to twenty feet beneath the surface, is a species of greenish blue earth, mixed with shells, and generally known as marl. As this substance is of great importance to the agricultural interest of the section, some remarks on its physical properties and use will not be out of place here. The essential ingredient of marl, as a manure, is lime; and its value depends upon the proportion of calcareous matter which it contains. When this abounds in connexion with sand only, it produces indurated marl, classed with the limestones, and frequently forming marble of great variety and beauty. We have discovered none of this precious character; but shell limestone, similar to that of the alluvion of North Carolina, Georgia, and Mississippi Territory, has been discovered in several places, and is burned for lime on the banks of the Rancocus, between Eayrstown and Vincent-town. The Jersey marls, at present, are chiefly known as the shell, clay and stone marls. The first is composed of testaceous matter, in various quantities and degrees of combination; and sometimes imbeds bones of marine and land animals.* The quantity of clay in union with calcareous substances, gives name to the second sort. This absorbs and retains moisture better than other kinds, and varies greatly in colour---being brown, blue, red and yellowish. In the third species, sand is combined with calcareous and argillaceous matter, giving hardness proportionate to its quantity; when of thin and laminar structure, this is termed slate marl. From the clay they contain, all these: species are softened by water, and, when exposed to the atmosphere,'gradually fall into powder. By reason of their calcareous principle, all marls effervesce with acids; but as water, alone, frequently produces the same effect when poured on dry clay, it may be necessary, in order to guard against mistake, in making trials upon substances supposed to be marl, to let them remain a short time in mixture with water, previous to the test of acids. The best marls containing the largest proportion of calcareous earth, it is important to know how to ascertain the quantity. Some are so poor as to have only a thirtieth part of their weight of lime. A simple method has been suggested, founded on the fact, that marl commonly contains about forty per cent. of its weight of fixed air or carbonic acid. It is merely by saturating the marl with muriatic or some other acid, and marking correctly the loss of weight which it sustains by the extrication of the fixed air. So, also, if the substance supposed to be marl falls readily to powder when exposed to the air; if the powder, when dry and thrown on hot coals, crackles like salt; and if, when dry, and mixed with water, it have a soapy feel and effervesces much, its quality may be pronounced good. Some marls in England, and probably here, have eighty-four per cent. of carbonate of lime, which is more than limestone generally possesses; and the refuse being often of peaty substances, is more useful as manure than' that of limestone, which is mostly sand or clay. Such marl may be converted into quicklime by burning; and its solution changes vegetable colours to green, possessing all the other properties of caustic lime. Marl is further distinguished by its feeling fat and unctuous, and appearing when dry, after exposure to the weather, as if covered with hoar frost, or sprinkled with fine salt; and even when mixed with the land, giving to the whole surface a whitish appearance. The farmers in Staffordshire, England, consider the soft blue marl, commonly * Among the latter, it is said, are bones of the rhinoceros and other animals of the eastern continent, some of them of extinct species; elephant's teeth, deer's horns, bones of the whale, shark's teeth, and entire skeletons of fish, together with graphytes, belemnites, cardites, and various shell-fish. 4 GENERAL DESCRIPTION. found under clay, or low black ground, at the depth of seven or eight feet, the best for arable land, and the grey sort for pasture. But that which is of a brownish colour, with blue veins, and small.lumps of chalk or limestone lying under stiff clays and very hard to dig, is most esteemed in Cheshire. The marl having a light sand in its composition, usually found at the depth of two or three feet, on the sides of hills, and in wet, boggy grounds, is fat and close, and reckoned the strongest and most beneficial on sandy lands. It is usually called peat or delving marl. What is sometimes called paper marl, frequently lies near coals, and flakes like leaves or pieces of brown paper, being of somewhat lighter colour. That which some call clay marl is very fat, and is sometimes mixed with chalk stones. There is another sort of marl, which breaks of itself into square cubical bits. The two last kinds generally lie under sand and clay; sometimes about a yard deep under the former, but often much deeper under the latter. The stone, slate or flag marl, which is a kind of soft stone, or rather slate, of a bluish colour, is generally allowed very good. It easily breaks down, and dissolves with frost or rain; is found near rivers and on the sides of hills, and is very lasting when used as manure. In many places marl discovers itself to the most negligent eye, particularly on the sides of broken hills or deep hollow roads. Many rivers are bordered with a vast treasure of this sort, which is plundered by every flood. Boggy lands frequently cover it, and in them it seldom lies above three feet deep. It is somewhat lower under stiff clays and marshy levels. The lowest parts of most sandy lands abound with it, at the depth of three, seven, nine or more feet. The depth of the marl itself can seldom be found; for when the upper crust is removed, all that can be seen or dug is marl, to so great a depth that there are few if any instances of a pit having been exhausted. Much of the preceding description of the English marls is applicable to those of New Jersey. The marl region of this State, is classed by some authors with the ferruginous sand formation of the United States. It may be located, so far as it has yet been explored, between two lines; one drawn from Amboy Bay to Trenton, the other from Deal, on the Atlantic, to the mouth of Stow Creek, in Cumberland county, upon the Delaware Rivet: but there is much reason to believe that this formation occupies a great portion of the triangular peninsula south of the Raritan River. Much of the ferruginous sand region, however, is overlaid by deposites of clay containing lignite. Above these is an almost uniform covering of grey sand; yet in many places the marl, with its peculiar fossil, is found immediately beneath the soil. This formation has been traced southward in many places, and most probably extends nearly the whole length of the Atlantic frontier of the United States. In all its localities, it has been identified by similar genera and species of organic remains, though all the genera do not exist in every locality. Thus, at the Deep Cut of the Delaware and Chesapeake Canal, the strata are characterized by great numbers of ammonites, baculites, and other multilocular univalves. These remarks apply to various parts of Burlington and Monmouth counties, in New Jersey. Near New Egypt, are ten or twelve beds, one above the other, with the genera terebratula and gryphma. (Ostrea, Say.) Near Homer's Town, the marl is extremely indurated; and contains terebratula exclusively. Near Walnford, the fossils are chiefly exogyre and belemnites; while at Mullica Hill, in Gloucester county, the beds contain bivalves, and quantities of belemnites; and the calcareous beds of this county contain gryphaea, teredo, alcyonium? sparangus, and several species of Linmean madrepores. The mineralogical characters vary considerably. Of the species of marl in minute grains, loose and friable, and of an uniform dull bluish or greenish colour, often with a shade of grey, and called gunpowder marl, Mr. Seybert has given the following constituents: silex 49.83, alumine 6.00, magnesia 1.83, potash 10.12, water 9.80, protoxide of iron 51.53, loss 89=100 grains. A less cautious analysis by Mr. J. P. Wetherill and Dr. S. G. Morton, of a specimen, apparently similar, from another locality, gave silex 49.00, protoxide of iron 50.00, alumine 5.50, lime 4.70; the remainder being chiefly water and carbonic acid. Hence the predominant constituents of these marls are silex and iron. They often contain beds of a dark bluish tenacious clay, sometimes mixed with the marl, forming marley clay; at others, the marl and clay alternate. Again, marl is seen of a yellowish brown colour, friable or compact, and filled with green specks of the silicate of iron. Some of the greenish varieties are also very compact, rendering it extremely difficult to separate the fossils from their SOUTHERN DIVISION. 5 matrix. The friable blue marls often contain a large proportion of mica, in minute scales. Other localities present beds of.silicious gravel, the pebbles varying from the size of coarse sand, to one and two inches in diameter, cemented together by oxide and phosphate of iron, and containing fossils, similar to those above described. The most striking instance of this kind is at Mullica Hill. Some of the blue marls, which effervesce strongly with acids, contain but five per cent. of lime. But we find large beds of calcareous marl, containing atleast thirty-seven per cent.; the remainder being silex, iron, &c. Also a hard, well characterized, subcrystalline limestone, filled with zeophytes. All these diversified appearances pass, by insensible degrees, into each other, exhibiting an almost endless variety of mineralogical character. The mineral substances found in these beds, are iron pyrites in profusion; chert in the calcareous beds, amber, retinasphalt, lignite and small spherical masses of a dark green colour, and compact texture, apparently analogous to those found in the green sand of France. Their structure does not appear to be organic, although they have, often, a shark's tooth, or a small shell for a nucleus. Larger spherical bodies also occur, resembling the nodules of clay in ironstone, common in some parts of England. As the quality of the marl varies greatly, so does the quantity used in manuring lands. In Monmouth county, south of the Shrewsbury River, there is marl so strong, that five cart-loads the acre are as much as the land will bear advantageously: in other places, from twenty to one hundred and forty loads to the acre are profitably used. It is asserted, that a good dressing will last from twelve to twenty years. It would be difficult to calculate the advantages which the state has gained, and will yet derive from the use of marl. It has already saved some districts from depopulation, and increased the inhabitants of others; and may, one day, contribute to convert the sandy and pine deserts into regions of agricultural wealth. Pine lands, in the counties of Columbia, Albany, and Saratoga, and other parts of the state of New York, of a character similar to those of New Jersey, have been rendered very valuable by gypsum, and rotation of crops, often producing from twenty to twenty-five bushels of wheat to the acre. The sandy soil is in time changed to a rich vegetable mould-and gypsum, therefore, may probably be used with marl to render the pine lands of this State productive. The occupation of a vast proportion of the inhabitants of this section is agricultural. Upon the loam soils large quantities of grass and grain, particularly rye, corn and oats, are produced; and the sandy lands, treated with marl, also give abundant crops of grain and grass. In convenient situations for supplying the markets of New York and Philadelphia, the farmers give much attention to the more profitable culture of garden vegetables, potatoes, melons, fruit, &c. The peach orchards of E. and W. Jersey, give abundance of that delicious fruit to both cities; so low, at times, as fifty cents the bushel. At a distance from the navigable waters, and from market, the grain is commonly fed to stock, and few portions of the United States, of equal area, produce more, or better, pork, than the counties of Monmouth, Burlington and Gloucester; scarce less famed for the quality of their horses. In the counties of Gloucester, Cumberland and Salem, upon the, fresh waters of their streams whose shores are subject to.overflow by the tides, many thousand acres have, by embankment, been converted into productive meadows, which maintain large herds of cattle, and furnish adequate means for enriching the upland. Adjacent to the Delaware Bay and sea coast, are wide tracts of salt meadow, some of which have also been reclaimed by embankment; and the rest afford abundance of coarse hay, free in many places to all who seek it, and valuable in the maintenance of stock and making manure. The. climate is so mild, near the coast, that herds of cattle subsist, through the winter, upon these meadows, and in the neighbouring thickets, without expense to the proprietors. The sea coast is said also to be favourable to the production of good mutton and wool. The great inducements to enterprise and industry constantly operating in the markets upon the borders of this section, have already produced wonderful effects, and cannot fail to excite the inhabitants to still greater efforts to improve the advantages they possess. Extensive beds of the variety of argillaceous oxide of iron, called bog ore, are common throughout this district, which when mixed with mountain ore, in the furnace, makes good iron for castings and the forge. From these furnaces, and those of the glass-houses, fed by the wood of the forest, a considerable portion of the an 6 GENERAL DESCRIPTION. nually growing wealth of the district is derived; and if we add to these, the cord wood, and lumber, and vessels built upon its southern waters, we shall have enumerated the chief sources of the prosperity of the peninsula. In this part of the state, 14 furnaces, including cupolas, and 14 forges, one extensive rolling and slitting mill and nail factory, and 11 glass manufactories, engaged in the manufacture of window-glass and hollow ware, provide a valuable and steady market for large portions of the agricultural product. The whole of this district is tolerably well watered; but the streams are neither large nor rapid, and are- remarkable for the depth of their beds, which cause, indeed, almost the only inequalities of its surface. Those of the northern part of the peninsula interlock their sources in various ways; some flow N. and N. E. as the Millstone and the South Rivers, with their many tributaries; some E. to the Atlantic, as the Swimming, Shark, Manasquan, Metetecunk and Tom's Rivers; whilst others seek the Delaware, as the Assunpink, the Crosswicks, the Rancocus, Cooper's, Big Timber, Mantua and Oldman's Creeks. Those on the south either flow S. E. to the ocean, as the Mullica, Great Egg Harbour and Tuckahoe rivers, or run S. W. into the bay, as Salem, Stow and Cohansey creeks and Maurice River. Most of the streams have a crooked course, and flowing through a flat country, are commonly navigable some miles from their mouth. Unlike the rivers of hilly countries, they are steady in their volumes, and uniform supplies of water can be more confidently relied upon. IV. The second of our divisions of the State is included by a line drawn from Hoboken, running S. of New Brunswick to Trenton, and another from the Ramapo Mountains, on the boundary of New York, curving by the Pompton Mountain or Highlands, Morristown, Baskingridge arid Plemington, to the Delaware, between Alexandria and Milford. This section, from N. E. to S. W. has about 70 miles in length, and an average breadth of about twenty miles. It possesses considerable variety of surface and soil, but is strikingly distinguished by its geological formation, which is chiefly secondary or old red sandstone, upon which rest hills of greater or less elevation, crowned with trap or greenstone rock. Its area includes four-fifths of Bergen county, the whole of Essex, a small portion of Morris, nearly all of Somerset, one-half of Middlesex, and one-half of Hunterdon counties. The sandstone base is found in various states of induration and aggregation. Generally, on the eastern portion of the section, from the Palisades, on the North River, westerly to Hunterdon county, it is compact, hard, and well adapted for building, frequently assuming the form of puddingstone and wacke, and occasionally affording considerable organic remains. Between the south branch of the Raritan and Delaware, still underlaying mountain and valley, the red rock assumes a slaty, shaly form, has more clay in its composition, and, taken from whatever depth, readily disintegrates into loam more fertile than that formed from the harder stone. But for the trap hills which have been thrown upon it, the whole of this section would be a vast plain, whose only inequalities would be formed by the excavations made by the streams in their tbrtuous and generally sluggish passage to the Ocean. From this general formation, however, we must admit the following exceptions. The alluvial borders the first south-eastern trap ridge, known as the first Newark Mountain, from Boundbrook to Springfield, and westward it approaches the Raritan within two miles, forming the bed of that river a little below Brunswick. Wherever excavations have been made in this alluvial tract, strata of sand, gravel, and clay are disclosed, but no rocks in place. Ochres of good quality have been found in many parts of it, and at Uniontown, near Springfield, compact peat of superior quality, resting on marl, supposed to extend through a morass of five hundred acres. Bones of the mastodon were discovered a few years since in this swamp. Extensive beds of white pipe clay, composed principally of alumine, and infusible, have been observed 'between Woodbridge and Amboy, and marine shells in various parts of the district. The alluvial section we have just described, is connected with another five miles in breadth bytwenty in length, formed of the deposits of the Hackensack and Passaic Rivers, between the secondary valley and the Bergen ridge. In this tract, the depth of the deposit is from 12 to 20 feet, its basis sand and shells like the shore of the sea. The whole was formerly covered with wood, of which some groves of cedar still remain, and bodies of trees but little decayed are frequently found at various depths. Indeed, so abundant and sound are the logs on these marshes, that they are used for the foundation of the New Jersey Rail-road, now being constructed MIDDLE DIVISION. 7 here. In this bog, N. of the turnpike road, between Newark and Jersey City, rises an island (Secaucus) about four miles long by one wide, composed, like the adjacent shores, of red and grey sandstone, and having a promontory at either end. That on the south known as Snake Hill, has a conical form, is of trap rock on sandstone rising into mural precipices, and having cubical masses of the trap piled at its southern base. From its wood clad, rocky and precipitous summit, the spectator may behold the Hackensack and Passaic Rivers almost at his feet1 and for several miles dragging their slow length through a sea of verdure; on the west, populous villages and ranges of mountains; on the east the great city of New York, and on the south the wide expanded ocean. Through the grey sandstone of this island, micaceous iron ore is abundantly dispersed; and pectenites and other marine shells are found on its elevated parts. The trap ridges which traverse this division excite much interest. Trapstone is known in many cases to have an igneous origin. Whether it may be ascribed to the same cause in all, is still a vexed question. That it has been found here subsequently to the sandstone on which it reposes, is most obvious; but when or how it has been poured over its base, throughout such great extent 6f country, in Connecticut, New York, and Pennsylvania, will probably never be discovered. We.observe the first mountainous range of this district, on the eastern border adjacent to the Hudson River. It rises gradually from Bergen Point, bounds the State for about 28 miles, and runs a greater distance into the State of New York'. In this State this ridge has an average width of two and a half miles, with a summit of table land. From its western brow there is a gradual descent into the valley of the Hackensack and Passaic. On its eastern side it is uniformly precipitous. At Weehawk, four miles N. of the City of Jersey, the mountain presents a perpendicular wall, elevated 200 feet above the Hudson, commanding a fine view of the surrounding country. From Weehawk to Fort Lee, a distance of about 7 miles, there is an alternation of precipitous ledges and steep declivities, mostly clothed with various.verdure. The hills, retiring at intervals from the shore, give room for narrow but fertile and well cultivated strips of ground, adorned with neat dwellings, environed by fruit trees and diversified crops. From Fort Lee to the state line, the mountain has a uniform appearance. The eastern front rises perpendicularly from 200 to 550 feet; numerous vertical fissures cross-each other at various angles, forming basaltic columns, from which the name of Palisades has been derived. The face of the ledge is bare, but vegetation is occasionally seen in the crevices. From the base of the precipice to the edge of the water, a distance of 3 or 400 feet, there is',a steep declivity covered with angular blocks of stone fallen from the heights, and shaded with trees. The summit of the mountain is slightly undulating table land, gradually rising to the north, with an average width of about two miles, generally covered with wood in all the wildness of nature. The western side of the mountain has a very gradual descent, is cleared and well cultivated, and neat farm houses of freestone line its base, like a village street, for near 20 miles. The prospect is one of the most delightful; numerous farms, rich in luxuriant vegetation, and extensive alluvial meadows through which the Hackensack and its tributaries flow, are bounded by the mountain ranges of the west. The greenstone of this mountain, resting on sandstone, is not so dark as that of New Haven, and is an aggregate of hornblende, feldspar, and epidote, with which prehnite compact and radiated is sometimes associated: At the base of the mountain bordering the river, in many places, secondary argillaceous shist, conglomerate, red, white, yellow and purple sandstone, and indurated clay, alternate, exhibiting a stratification nearly horizontal, the underlaying inclination being from 8 to 10 degrees. These layers are sometimes visible on the mountain's side, at considerable elevations above the river. The sandstone is generally a coarse aggregate of quartz and feldspar, often friable, but sometimes very firmly combined; exhibiting winding vertical fissures. In this base may be observed, in some few places, a compact white sandstone, resembling the Portland stone of England. A metallic vein was worked, at Fort Lee, at the commencement of the revolutionary war, under the impression that it contained gold; but Dr. Torrey has determined, that the ore is pyritous and green carbonate of copper; and the matrix quartz, dipping under the greenstone. Two other prominent mountain ranges intersect the country now under view. They rise near the primitive highlands, two miles north of Pompton, and run about sixty miles in an almost semicircular course. The first ridge, at its commencement, is about twenty miles E. from the Palisades; but at, and south of Patterson, it is not 8 GENERAL DESCRIPTION. more than twelve, from the North River. The most elevated point of these mountains is six miles N. W. from Patterson, where a sugar-loaf peak rises near 1000 feet above the level of the ocean. Its trap rock is generally covered with a thin mould and verdant surface; and a walnut grove, without underwood, occupies, exclusively, about forty acres upon the summit, from which there is a very extensive view, towards the E. N. E. and N. over a tolerably level country. On the N. W,. the waving tops of the Preakness ridge are observed, extending for several miles, indented by ponds of considerable magnitude and depth. North of this ridge is another high and detached hill, sweeping in a semicircle, rising and terminating near the Highlands. Many of the summits are under cultivation, and afford fine views of the great secondary valley, bounded by the Highlands, the Hudson and the Preakness ridge. On the east of the last chain is another section of the trap ranges, called the Totoway mountain. It rises near the Preakness mountain, six miles from Patterson, and unites with the Newark chain, at the Great Falls. It is in many places free from rocks, but on the east side are precipices of considerable height and extent, with waving or denticulated mural faces, presenting columns of basaltic regularity. An insulated semicircular wall of greenstone, with projecting columns, bearing some resemblance to a castle or fort in ruins, occupies a summit of the Totoway ridge. Sandstone quarries are opened in several places at the base of the greenstone; and one, three miles from Patterson, on the Preakness mountain, affords the best freestone of New Jersey. Fine red and grey sandstone sprinkled with mica, alternates with argillaceous strata, dipping under the greenstone, with a western inclination of about 120. Bituminous coal, in layers two inches thick, has frequently been found in this and other parts of the Preakness ridge, in connexion with sandstone and shale, and the neighbourhood is supposed to exhibit indications of more valuable beds of this combustible. Gneiss, granite, pudding and sandstone, in rolled masses, abundantly cover the surface, in many parts of this region. The greenstone of the Preakness range rarely offers interesting imbedded minerals; but prehnite, agate, chalcedony, and a mineral resembling cachelong, have been discovered in it. At the falls of the Passaic, in Patterson, perpendicular mural precipices of greenstone, with wide vertical fissures and amorphous masses at their base, may be observed. The lower strata of this rock contain much argillaceous matter, which partially takes the place of hornblende. The ledges rest on porous rocks, horizontally posited, resembling the toadstone of Derbyshire. Carbonate of lime and other minerals, subject to decay, are imbedded in it; and by their decomposition give a cellular and volcanic appearance. A friable amygdaloid, with an argillaceous base, enclosing nodules of carbonate of lime of a spheroidal oval or almond shape, from the size of a pea to that of a walnut, may also be noticed. The nodules, easily disengaged from the base, exhibit a smooth dark green surface of chlorite. The layers beneath the amygdaloid, are red and grey conglomerate, connected with red sandstone, too porous for use, absorbing much moisture and breaking by the expansive power of frost. Good freestone in nearly a horizontal position, is the basis layer, and forms the bed of the Passaic. In many places the greenstone occupying the summit appears but a few feet in thickness; and it is not arranged in columns of basaltiform regularity. Prehnite, calcareous spar and carbonate of copper, zeolite, stilbite, analcime and datholite, have been found here. Mural precipices of dark fine grained fissile greenstone, are observed at the Little Falls of the Passaic, five miles above Patterson. Vertical seams cross each other here, at various angles, in the ledges, giving to detached pieces a regular prismatic form, with three or four sides, often truncated on one or more of the lateral edges-the tabular form is common. Rock of similar character is observable in other parts of the Preakness ridge. Marine organic remains, such as orthocerites, madrepores, tubipores, pectenites, terebratulas, encrinites, bilabites, serpulites, and other species, generally in an argillaceous base, in mountain and valley, have been observed here, as in other parts of this region. From Patterson to Springfield, the trap ridges are called first and second Newark mountains, and, Caldwell mountain. Their direction is nearly south, with great uniformity of altitude; their eastern declivity steep, their western descent gradual, as is common with mountains of North America. Mural precipices are rarely seen, except at Patterson and Springfield. Wherever ledges appear, the mountain side is covered with small amorphous stones. The red sandstone appears in place, both upon the sides and base. Much of the eastern side is under cultiva MIDDLE DIVISION. 9 tion; the summit and western declivity are generally covered by coppice of small oak, chesnut, walnut, butternut and cedar. The second Newark mountain runs a parallel course with, and is distant from, the first, about a mile. It is less elevated and rocky, and has a more gradual ascent than the other. The view from the first embraces the thickly settled and highly cultivated valley, whose surface appears like a plain, painted with meadows, grain fields and orchards, and studded with the villages of Bloomfield, North and South Orange, and the large towns of Newark and Elizabeth;-beyond which we have in sight the salt meadows, the city and harbour of New York, parts of Long and Staten Islands and the distant ocean. In this valley, fine red and grey freestone alternates with shale. Bituminous coal, in thin layers, is associated with argillaceous shale, in freestone quarries, adjacent to the Passaic. At the termination of the Newark Mountain, at Springfield, and in many parts of the trap ranges, smoke, and in some instances, flame issuing from the crevices of the rock, have been observed by the inhabitants; proceeding probably from carbonated hydrogen gas indicating coal below. Animal and vegetable organic remains have been observed in this freestone. Near Belleville a tooth, almost two inches in length, was discovered, some years since, fifteen feet below the surface. The Newark Mountains terminate at Springfield, where the continuity of the trap range is broken. From this place the greenstone ridges take a S. W. direction of seventeen miles to the vicinity of Boundbrook, and thence, N. W. about ten more to Pluckemin: the second mountain following the curvature of the first. Secondary greenstone is, exclusively, the'rock, in place, of the summits and sides of both ridges, but it seldom appears in ledges of magnitude. Sandstone is as usual the base, and has been observed under the greenstone:, in nearly a horizontal posi tion, with a small dip, sometimes alternating with secondary compact limestone, in layers, from two inches to two feet in thickness. Prehnite is found in considerable quantities, near the foot of the mountain, in amygdaleid with a greenstone base, much of it partly decomposed. It is sometimes imbedded in the rock, in long parallel columns in various directions, its fibres radiating from the centre. Zeolite, stilbite, crystals of quartz, and carbonate of lime, are frequently seen in the valley between the mountains. North of Scotch Plains, sulphat of barytes appears associated with carbonate of lime. A small portion only of these ranges is cleared and cultivated. The mountain, running a S. W. course from Springfield, has been termed, by some geologists, the Granite Ridge. It is described as passing through the State, bordering the oceanic alluvial, and having its highest point near Hoboken-alluding, doubtless, to the height near Weehawk. The Greenstone Ridge would be the more appropriate name. For excepting the serpentine, at Hoboken, there are no primitive rocks in place, between the Hudson and Highland chains; the summit rock of all the ranges being, uniformly, secondary greenstone. The Highland chain runs from S. E. to N. W., the general direction of theprimitive strata; but none of the secondary ranges of New Jersey pursues a course parallel with the primitive. The latter, in many places, preserve for miles an even summit of table-land, whilst the Highland ridges display sugar loaf eminences, and a waving profile, characteristic of the primitive. The extensive secondary range commencing near Pompton, within half a mile of the Highlands, and extending in a semi-circular course until it again approaches them, corroborates, by its direction and the character of its summit, the correctness of these positions. The broad valley, encircled by the Greenstone ridge and the Highlands, contains much fresh water alluvial. Many of its small hills have no rock in place. The plain bordering the Passaic is generally extensive-in some places four miles wide. Peat is observed in several places between the source of the river and Little Falls; and a considerable quantity has been cut, adjacent to the Newark and Morristown turnpike, and the bed discovered to be more than six feet deep. Pompton Plain, near twenty miles in circumference, and environed by mountains, presents a decided fresh water alluvion--strata of gravel, sand, and clay, without rocks in place, have uniformly been found wherever wells have been dug; and it was, probably, at a remote period, the bed of a lake. The waters of the Pequannock Long Pond and Ramapo Rivers pass through it. The southern and much of the western part of the plain is marshy, and embraces about 1500 acres of peat ground, apparently of good quality, judging by a ditch of four miles in length which has been dug through it. In the southern part of the plain, good granular argillaceous oxide B 10 GENERAL DESCRIPTION. of iron, or pea ore, is found over a space of about 200 acres. The Highlands form the west and north-west boundary of the plain, which in other directions is skirted by the Pacganack Mountain, pursuing a serpentine course from North Pompton, to the vicinity of Morristown, separating the wide alluvial plains watered by the Pompton and Passaic Rivers. Upon this range, the summit rock, in place, is, uniformly, a fine grained dark secondary greenstone, often in a state of partial decomposition, exhibiting mural precipices of considerable height and extent, with sandstone at the sides and base. The first contains prehnite, zeolite, analcime, chalcedony, agate, amethyst, jasper, crystals of quartz, and narrow veins of satin spar, in jasper. The part of this range adjacent to Pompton Plains, may, perhaps, from the abundance of these minerals, be useful to the lapidary, as well as to the mineralogist. The agates are from the size of a pin's head to three pounds weight, mostly chalcedony-The eyed and fortification agate has been observed here in a few instances. A mineral specimen was found in this mountain by Judge Kinsey, of near 16 pounds weight, containing agate, amethyst, and white quartz. Another greenstone range, of minor extent, called Long Hill, is situate in the great valley, under review, rising near Chatham, and running westerly about ten miles. The trap of this ridge is in such state of decay, that rocks seldom appear in place. The Passaic pursues a winding course along the base of the mountain, sometimes concealed in groves, at others glancing sheen in the verdant meadows. About the centre of Long Hill are mural precipices, composed of what the farmers call shell rock, resembling the stone on the banks of the Raritan. This secondary formation accompanies the Highlands to the Delaware, and is pierced in several places by broken ridges of the same trap character we have described. Such is the Rocky or Nashanic Mountain, the heights near Rocktown, Lambertville, Belmont, Herberttown, and Woodville, and Rocky Hill, immediately north of Princeton. The sandstone, generally, in this portion of the section, differs materially from that of the Passaic. It extends northerly to the first primitive ridge, north of Flemington, and forms the soil of the broad red shale valley, spreading from that ridge to the Rocky Hills, underlays the last, and extends south of Penington. Its colour is of a darker red than the Newark stone-it appears to be without grain, yields a strong argillaceous odour when breathed upon, and is readily decomposed by exposure to air and moisture. It is, probably, composed of iron, alumine, and silex, with a small portion of sulphur, and may be termed ferruginous shist. The rock is stratified, splitting readily into thin brittle lamine, and is said to rest in some places on good freestone. But on the S. E. near Princeton, are quarries of excellent red and white freestone, similar to that of the Preakness ridge. Sandy Hill, an elevation of the secondary region, situate between Kingston and Brunswick, is alluvial, like the Nevisink Hills, composed of sand, white and coloured clay, containing beds of ferruginous sand and puddingstone. Upon the south-western angle of this district, and particularly at and around Trenton, there is a small portion of primitive, rising through the secondary, into abrupt rocks of granitic character, varying from loose micaceous shale to massive granite, but composed chiefly of hard and compact gneiss. This rock forms the Falls of the Delaware at the head of tide, and stretches away in a S. W. direction through Pennsylvania. From a mass in the bed of the river, large and beautiful specimens of zircon have been taken. The portion of New Jersey which we have now described, is the most populous, and perhaps the most wealthy of the State. Its soil is not so productive as the limestone of the primitive and transition regions; but there is less of it waste, than in those regions, and it is divided into smaller farms, and more assiduously laboured, under the excitement of proximity to the markets of New York and Philadelphia, and that created in the eastern portion by its own manufacturing towns; as Patterson, Little Falls, Godwinsville, New Prospect, Bloomfield, Belleville, North and South Orange' Springfield, Plainfield, Newark, Elizabethtown, Rahway, Woodbridge, New Brunswick, Princeton, Trenton, &c. Besides the minerals already mentioned, large deposits of copper ore have been discovered in this section, at Belleville, at Griggstown, near Brunswick, Woodbridge, Greenbrook, Somerville, and Pluckemin; and it would seem probable that a vein of this metal extends S. W. across the secondary region from Fort Lee. The following account of the mine near New Brunswick is extracted from Morse's Gazetteer:"About the years 1748, 1749, 1750, several lumps of virgin copper, from 5 to 30 MIDDLE DIVISION. 11 lbs. weight, (in the whole upwards of 200 lbs.) were ploughed up in a field belonging to Philip French, Esq., within a quarter of a mile of the town. This circumstance induced Mr. Elias Boudinot to take a lease of the land of Mr. French, for 99 years, with a view to search for copper ore. A company was formed, and about the year 1751, a shaft was commenced in the low ground 300 yards from the river. The spot selected had been marked by a'neighbour, who, passing it in the dark, had observed a flame rising from the ground, nearly as large as the body of a man. At about 15 feet, the miners struck a vein of blue stone, about two feet thick, between loose walls of red sand stone, covered with a sheet of pure copper, somewhat thicker than gold leaf. The stone was filled with grains of virgin copper, much like copper filings, and occasionally lumps of virgin copper of from 5 to 30 pounds were found in it. This vein was followed about thirty feet, when the accumulation of water exceeded the means of the company to remove it. A stamping mill was erected, where, by reducing the ore to powder, and washing it, many tons of pure copper were obtained and exported to England. Sheets of copper of the thickness of two pennies, and three feet square, have been taken from between the rocks, within four feet of the surface, in several parts of the hill. At about fifty or sixty feet deep, a body of fine solid ore was struck in the same vein, but between rocks of white flinty spar, which was soon worked out." Some efforts were made to renew the mining operations here, at various periods, but never with encouraging success. The excavations have been extensive. A shaft of great depth is yet visible; an adit, it is said, was driven several hundred yards beneath the bed of the river, and hydraulic pumps were worked by Lyell's Brook to free the mine from water. The stones around the vicinage are every where coloured by the oxide of copper, and beautiful copper pyrites are obtained from the neighbouring quarries. The Schuyler copper mine, near Belleville, on the left bank of the Passaic, seven miles from Jersey City and Hoboken, was discovered about the year 1719, by Arent Schuyler. The ore cropping out on the side of a hill was easily raised; and as the policy of Great Britain prohibited every species of manufacture in the colonies, it was exported in the crude state to, England. From the books of the discoverer, it appears that before the year 1731, he had shipped 1,386 tons to the Bristol copper and brass works. His son, Col. John Schuyler 'prosecuted the work with more numerous and skilful hands; but the quantity of ore raised by him is unknown, his books having been lost during the war. In 1761, the mine was leased to a company, who erected a steam engine, of the imperfect construction then in use, and worked the mine profitably for four years. In 1765, however, a workman, who had been dismissed, having set fire to the enginehouse, the works were discontinued. Several gentlemen in England, acquainted with the superior quality of the ore of this mine, obtained permission from the crown to erect works for smelting and refining copper in America, and offered to purchase the estate of Mr. Schuyler, containing the mine, at ~100,000 sterling. This offer he refused, but agreed to join them in rebuilding the engine and working the mine. But the revolutionary war, and the deranged state of the country subsequent thereto, and other circumstances, caused the mine to be neglected until 1793, when a new company undertook the work with much vigour, but it would seenm with little prudence. They collected miners from England and Germany, purchased a freehold estate, convenient for the erection of furnaces and manufactories, with an excellent stream of water, rebuilt the engine, and commenced and partly completed other works. Their labours were interrupted by the death of the principal shareholder in the company, the whole interest of which soon after was vested in Mr. Nicholas I. Roosevelt, whose many engagements debarred him from prosecuting this enterprise. Another company, organized in 1825, procured some Cornish miners, and cleared out two adit levels, three old shafts, and sunk one new one about 60 feet deep; erected a new steam engine, and prepared most of the necessaries for working the mine in the deep levels. But, when they were ready to break out ore, some inefficient machinery designed to pump the water from the vein to the great shaft, gave way, and the funds or patience of the company were insufficient to prosecute the enterprise further. Their lease, conformable to its terms, was forfeited. We understand that during the present year (1833), a new association has been formed for working this mine. There are many veins well worth working, particularly those near the surface, containing what is termed stamp ore. The principal vein,'which has proved very 12 GENERAL DESCRIPTION. profitable, is imbedded in a stratum of freestone, from 20 to 30 feet thick, and is called a pipe vein. It dips about 12 degrees from the horizon, rather by steps than a straight line, and increases in richness with its depth. It has been followed 212 feet below the surface, and about 112 feet beneath the adit cut for draining; hence, the water must be pumped to that level. A large shaft has been sunk 140 feet below the adit, 30 feet of which have been filled with mud and rubbish. The engine at the mine has a cylinder 31J inches in diameter, and eight feet stroke, and has ample power to free the mine from water. Excellent cast iron pumps are fixed from the level of the vein to the adit, and from the adit to the surface, for supplying the engine. The vein has been worked about 150 feet, horizontally, from the shaft, declining from the entrance a few feet:, hence, though the leakage is inconsiderable, some method is required to carry it into the shaft, which may be readily done if the shaft be cleared to the bottom. The ore of the principal vein, it is said, yields from 60 to 70 per cent. of copper; and the vein will produce, it is supposed, from 100 to 120 tons of ore annually, which yields from four to seven ounces of silver to the hundred pounds; and, like most copper ores, a small portion of gold. When pure copper was sold in England at ~75 sterling the ton, the ore of this mine was shipped from New York for that market at ~70 the ton. The quality of the ore, and condition of the mine, are attested by several respectable persons, who have skill and proper means to judge of them. If the statement respecting the proportion of silver in this ore be correct, it is more productive than many of the much-worked and highly valued mines of Mexico. The mines of Biscayna, of Royas, of Tehuilotepec, and of Gautla, do not yield more'than three ounces of pure silver to one quintal of the ore; whilst the remarkable rich mines of the Count de la Valenciana, at Guanaxuato, gave only 5.1-10 ounces the quintal. The mean product of the whole Mexican mines, when in their best condition, did not exceed 2J ounces the qtiintal; and that of the ores of Peru was still less; giving at most at Potosi, 53-100, and at Pasco, 1.3-50 ounces, the quintal. If the ores of the Schuyler mine give from four to seven ounces of silver the quintal, and are abundant, they must be better worth working for the silver alone than most of the silver mines of the world; and the copper product must add enormously to their value. The copper 'mine in the trap ridge, two miles north of Somerville, commonly known as Cammam's, has been wrought at intervals for many years, but without profit; more, it is said, because of the want of capital, and public confidence in the operators, than from the poverty of the ores. The following, according to Dr. Torrey, are the principal minerals found here, viz: native copper in irregular masses, weighing from one ounce to eight pounds, and one block has been obtained of 23 pounds; phosphate of copper, massive, and of a verdigris colour, generally accompanying native copper; carbonate of copper, green, in connexion with the phosphate; red oxide of copper; the massive variety of which is the common ore of the mine, found crystallized in octahedra, whose surfaces are extremely brilliant and beautiful; native silver, in small masses, disseminated through the phosphate and crystallized oxide; green quartz, in tabular, partly noded masses, a beautiful mineral, resembling chrysoprase; prehnite, in cavities in the greenstone, very fine; and mountain leather, in thin plates, very tenacious when moistened. Drifts have been made in various directions in this mine, and the ore is said to be abundant, yielding from 25 to 75 per cent. of pure metal. North of the village of Greenbrook, in the same ridge, a vein of copper, many years since, was wrought to a considerable extent; but it, too, has been long abandoned. To these locations of copper, we are now to add another, lately discovered, near Flemington, in a vein remarkably, but not yet extensively, explored. V. The third section, into which we have divided the State, and which we have called the mountainous, is in breadth from 10 to 40 miles, measured at right angles with the direction of the mountains. This district is the most interesting, as it is the most varied, in its geological formation, surface, soil, mineral and vegetable productions. The geological formations here are much blended and confounded; and the most we can attempt is to designate and describe the strongly marked divisions. The secondary section we have above noticed, is bounded on the N. W. throughout its range by a broad district of primitive; containing, however, a large proportion of transition. The southern limits of this district are marked by the chain of highlands running S. W. from the Ramapo and Pompton Mountains, on the line of New York, NORTHERN DIVISION. 18 by Morristown, Baskingridge and Flemington to, and across, the Delaware, near Saxtonville. The extension, northward, is limited to a line running west of the Wallkill Mountains, and thence crossing the Delaware in the neighbourhood of Belvidere. A belt of transition, having an average breadth of about six miles, including Long Pond, Raffenberg and Greenpond Mountains, continues, we believe, along the eastern foot of Musconetcong and Schooley's Mountains, across the State. The continuity of the eastern ridges of the primitive, with its belt-of transition, is interrupted in many places by the streams; yet the hills form few valleys of considerable extent, and are generally less elevated in this State than in the vicinity of the Hudson River, where they rise to 1600 feet. They are usually crowned by sugarloaf eminences, forming a waving profile, characteristic of primitive regions. The summits are commonly covered with masses of rock, which render them unfit for culture. The primitive ridges contain rocks of pretty uniform character; in general coarse, well crystallized aggregates of quartz and feldspar; often enclosing shorl, garnets, hornblende and epidote, with little mica; and in many places, for a considerable extent, none. These simple materials, variously combined, form granite, gneiss and sienite. Primitive greenstone is observable also in some cases. In the transition section, grauwacke and grauwacke slate, are the most common rocks. The extensive ranges in Bergen and Morris counties, of Long Pond, Raffenberg, and Green Pond Mountains, for miles present stupendous mural precipices, facing the east, of a reddish brown grauwacke, composed of red and white quartz, red and grey jasper, and indurated clay. The rocks are stratified, inclining to the north-west at an angle of about 400. They are scattered in abundance on the banks of the Pequannock, from Newfoundland to Pompton. Grauwacke, in place, is sometimes observed, resting on sienite adjacent to the Pequannock. Extensive beds of magnetic iron ore are found on these ranges at Ringwood and Mount Pleasant, and at Suckasunny, at the mines of General Dickenson, being on the strata which extends 300 miles from the White Hills of Newhampshire, to the end of the primitive ridge near Black River. These beds are from 8 to 12 feet thick; and the ore from the mine of General Dickenson produces the best iron manufactured from highland' ore. Calcareous spar and asbestos are frequent, and sulphuret of iron abounds in various parts of the Highlands. Probably, the most extensive bed of the last is in Morris county, near the eastern base of Copperas Mountain, and opposite to Green Pond. Copperas was manufactured here extensively during the late war with Great Britain. Many rich beds of iron ore in this region, are rendered useless for the forge by sulphur. Graphite or black lead, in various stages of purity, is common. At Monro Iron Works, (N. Y.) on the River Ramapo, large plates of black mica, crystallized in hexaedral form, are seen sometimes a foot in diameter. Compact feldspar and epidote, are in the elevated primitive ranges west of the transition district, and compact limestone at various parts of the transition range; and in the vicinity of New Germantown, and on a line running N. E. and S. W. from that point, pudding limestone, not inferior in beauty'to that employed in the capitol of Washington, is abundant, and frequently converted into lime. In the primitive range of Morris county, west of Pompton Plains, called Stony Brook Mountains, chlorite slate is common, and granular limestone has recently been found in the same mountain. The latter is in colour clear white, admits of good polish, and is often associated with beautiful amianthus and talc, alternating in narrow veins. In the same vicinity there is a greyish white marble, rendered porphyritic by grains of noble serpentine disseminated through it. It is hard and receives a fine polish. In the talc, metallic crystals supposed to be chromate of iron, have been observed. From the last mentioned mineral an acid is extracted, which, united with lead, forms chromate of lead, a valuable pigment. Galena has been observed in the grauwacke ranges adjacent to Green Pond, and beautiful tremolite is connected with the white granular limestone of Stoneybrook. North-west of the transition, the primitive resumes its empire, and includes the Wallkill and Hamburg Mountains, which are continued in Schooley's and the Musconetcong Mountains, from the line of New York to the line of Pennsylvania, undivided by any stream. In this ridge and the portion of the primitive sections west of it, the primitive, the transition, and the secondary formations seem combined. This region also includes Marble Mountain, Scott's Mountain, Jenny Jump, Furnace Mountain, Pimple Hill, Pochuck Mountain, and other innominate hills. This, also, is a remarkable mineral district. Schooley's Mountain and the Musconetcong, abound with highly magnetic iron ore, blended however with foreign substances, 14 GENERAL DESCRIPTION. which render liquefaction difficult. Along the valleys and hill sides of this mountain there is an abundance of excellent flints suitable for guns. West of the Hamburg Mountain lies the valley of the Wallkill, or, as it is sometimes called, the Valley of Sparta; running east of north twenty miles to the State of New York, much noted for the number and variety of its minerals. A white crystalline limestone and marble occupies the bottom of the valley, and rises on the west into a low subsidiary ridge following the course of the stream eight or nine miles. The m6talliferous deposits, however, claim the greatest interest. The first or eastern bed, which at Franklin appears like a black mountain mass, contains an ore of iron commonly little magnetic, and, as a new metalliferous combination, has received the name of Franklinite, and is composed of 66 per cent. of iron, 16 of zinc, and 17 of the red oxide of manganese. On its supposed richness the great furnace of Franklin was built, but it was soon discovered that this ore was not only irreducible to metallic iron, but that it obstructed the fusion of other ores. If employed in quantity exceeding one-tenth of the magnetic oxide of iron with which it was economically mixed, there resulted what the smelters term a salamander; an alloy of iron with manganese, which resisted fusion and crystallized even under the blast, so that all the metal was lost, the hearth demolished, and 10 or 12 yoke of oxen required to drag away the useless mass. At Franklin, it is but sparingly intermixed with the red oxide of zinc. About two miles north, the bed ceases to be apparent at the surface, but may be traced seven miles to the south-east. Three miles from the furnace, at Stirling, is another huge mass of this mineral, but so combined with the red oxide of zinc, that the crystals of Franklinite are imbedded in the zinc, forming a metalliferous porphyry. This ore, merely pounded and mixed with copper, was profitably employed during the late war for forming brass. Often, within a few feet west of the Franklinite, appear beds of well characterized magnetic oxide of iron, but always accompanied by hornblende rock. A species of this last ore, found near the furnace, is intimately blended with plumbago. Here, also, are curious beds of yellow garnet, imperfect sienitic granite, in which are beautiful opaque blackish brown masses of garnet of a high resinous lustre, and crystallized on the surface, accompanied with laminated epidote; white and compact massive or minutely laminated augite, in some parts intimately blended with specks of violet, granular feldspat, resembling petrosilex; sphene, brown garnet, dark green granular augite, like the cocolite of Lake Champlain; phosphate of lime; spinelle and black spinelle or fowlerite, from Dr. Fowler, of Franklin, its discoverer; specular iron ore; brucite, bronzite, pargazite and idocras, zircon, tremolite, imbedded in crystals of white augite; actynolite, short crystals of augite almost black, like those of volcanic rocks; apatite, a beautiful apple green feldspar, in crystalline carbo4ate of lime, accompanied with perfect crystals of mica, and hexagonal plates of plumbago, soft and almost as fusible as hornblende; a very brilliant pale green hornblende, passing into sactynolite, which has been denominated maclureite, in honour of him who has done so much for American geology, and natural science in general;-blue and white sapphire, enormous green crystals of augite, at least an inch and a half in diameter, presenting hexaedral or octahedral prisms, with almost equal faces, and termimated by oblique tetrahedral pyrami4s, accompanied, near the junction of granite and crystallized carbonate of lime, with large crystals of feldspar; scapolite, or wernerite; arsenical pyrites, mixed with others resembling the sulphuret of cobalt, or nickel, with a substance like blende, accompanied by dendrodite, and argillaceous iluate of lime. The crystalline calcareous rock which here alternates with granitines of feldspar and quartz, or with beds of sienitic granite, at other places, disappears, and a confluent grauwacke, almost porphyritic, and contemporaneous, apparently, with the other formations, is observed, directly overlaid by a bed of leaden, minutely granular, secondary limestone, containing organic remains of the usual shells and corallines, and layers of blackish hornstone or petrosilex. This rock, as well as the grauwacke beneath has disseminated crystals of blue fluate of lime. In the limestone the cavities are sometimes very numerous, and lined both with pseudomorphous masses and cubes, and white fluate and quartz crystals. Thus we have here before us, as at Lake Champlain, the rare and interesting spectacle of an union of every class of rocks, but passing decidedly into each other, as if almost contemporaneous. This singular formation, to which slate should be added, extends into Orange county, State of r 0 0 "0 0 ad 0 0 C) "0 X0 "0 FREE WHITE FEMALES. 4) 9 ar. a0 P1.1 0; 0 0 o "0 " "0 " "0 0 ad c~S ~.' a) a) "0 "0 0 0 0 0 "0 "0 0 0 ad ad ~a "0 - oa T.'. T.. 00 MALE SLAVES. - ----- "0 ad 0 a) "0d 0d 0 10 FEMALE SLAVES. ad al 10 S.. "0 "0 - 0 ad a) "0 0 ~ 0 "0 0 0 "0 0 ad "0 0 FE RSONS-MALES. PERSONS-FEMALES., "0 ra ad 0n ad "0 0 0 "0 0 ad 0 a) "0 0 "0 0 ad "0 0 "0 ad 0. 0 "0 0 ad 0 I I I P" 1 110, 1 I I I ---I- *I - I-I I- I- I 4175! 1907 2547 2040 '2024 I--I -*-~*I--~lI-..' 55 a Z4 Hunterdon, Sussex, - Burlington, Essex, -- Monmouth, Morris, - Middlesex, Gloucester, Bergen,Somerset, Salem,Cumberland, Cape May, 4194 5901 4334 4337 3777 3218 2999 3779 2416 2140 2193 2065 702ý 1940 24 35) 2176) 2185 1758 16391 1430 1829 1154 1091 1047 960 326 586, 2539 723 3053 661 2554 2 720 31 00i 543 2189 5361 1855 431 1791 4501 2161 302 1330 308 1342 350 1340 266 1026 79 371 5956 24639 20515 3034 2459 280'2 2030 1857 1938 2051 1489 1319 1289 1201 4341 1.967 1931 2022 1999 17701 1522 1517 1531 1435 1096 738 747 262 54158 4082 4162 3645 3110 2877 3384 2306 2044 2025 1999 654j 2371 2201 2244 1747 1556 1491' 1704 1148 985 963 880 3081 3174 2854 2930 21501 2096 1882 2194 1406 1403 1368 1231 402 2776 2759 2934 2076 1917 1941 1979 1465 1395 1289 1156 360 1768, 20501 2051ý 1666 1484 1559 1356 124? 1083 754 780 213 37.14 328 126 134 11 152 23 2 5 4 1351 81 75 40.12 10 181 99 233109 1221!46 168111 41 376218 269200 31 113 4 I I --I 201 41 64 65' 50 8(o 3,167 112 2 A 21 148 42 77, 10 24' 1261 129 179 81 1031, 111 1781, 6 6, 157 2411 27 192 3, 5' 2 1 3 5 I Ifi ~ q A 117 I IAOI'RTinn 1I qTIQ!qGAl 60 2 117 134 85 130 6 217 190 2 27 6 72 71. ý44 100 3 1551 109 4 5 139 241 391 2950 139 257 203 389 511 222 138 52 55 173 90 68 38 86 107 59 92 133 64 17 35K30 146 100 118 68 82ý 7S 37 39 77 85 138 104 44 56 99 57 107 91 65t-' 4 25 24 10901389 119! 39 252! 139 397 115 2231 86 1131 49 273 108 187 1 20 346 73 5021 99 166~ 129 1251 80 34ý 15 1091198 30~ 26 128, 89 131 80 77 73 34 24 80 67 119 86 5 0 4 Q 61 66 74 7 9 48 37 24 14 9 87.76( 3079 25038 21368 21470 18 23089 40 18178 16506 14022 12668 4265 '149 277575 z 0 z I -1--l -I-, -- 1--j. 142055 19970 i 1I2 441J81185 371 059 1285 10361656133241116 21 1 a 1399 ý1950425637124693ý18035V6Ol5839.1762 ý11 CENSUS, 1830. Showing the Aggregate Amount of each description of Persons within the District of JVew Jersey, by Counties. FREE WHITES. MALES. FEMALES. 0 0_ 00 0l 00 0 0 I0 Names of r o o C z 0 o < < < oo oo,o o o o o, b o Bergen 1558 1401 1268 1082 1778 1270 779 509 415 173 61 5 1 1519 1374 1154 983 1656 1102 750 494 402 140 49-11 Essex 3024 2572 2482 2571 4062 522 1449 818 477 211 48 3735 2331 1503 923 606 Morris 1900 1603 1459 1200 2025 1387 906 565 347 170 53 4 1837 1525 1332 1187 1856 1304 827 609 370 170 58 5 Sussex 1898 1590 1342 1140 752 1045 665 445 228 103 28 1624 977 626 375 232 Warren 1614 1363 1205 1090 1773 062 670 341 234 95 14 00 1467 959 566 387 246 0 Somerset 140 1074 1000 921 1255 809 585 434 269 129 46 3 1152 1029 938 854 1259 887 619 438 319 164 56 2 Middlesex 155861 1411 1378 1227 1886 1190 8 13 487 371 183 35 1 1519 1374 1154 983 16561 1203 812 569 401 140 4911 Hunterdon 2345 2572 2482 257123762 15220 141 68185 2211 48 6 2867 2506 2316 2367 3735 2331 15031 231 606 2891635 1 Burlington 2389 2053s 19001603 1926 1580 2638 1 1041 733 44 196 503 4 837 152 1338 1187 1856 1683 1105 789 75270 58 Monmouth 2491 1893 1776 1419 2290 15204 950 731 435 221 284 2 21840 1950 118 1146 212 1454 951 640 437 32 79 3 4 Warren 1614 1363 1205 1090 1773 1062 670 341 234 95 14 2 1507 1268 1128 1042 1467 959 566 387 246 100 23 2 Somerset 1140 1074 1000 921 1255 809 585 434 269 129 46 3 1152 1029 938 854 1259 887 619 438 319 164' 561 2 Middlesex 1561 1411 1378 1227 1886 1190 813 487 371 183 35 1 1507 1398 1285 1239 1831 1203 812 569 401 186 51 5 Hunterdon 2345 2079 1.899 1592 2376 1550 1121 685 500 232 78 8 2191 1931 1797 1736 2509 1612 1216 821 473 274 8111 1 Burlington 2389 2053j 1926 1580 2638 1660 1041 733 441 196 50 3 2283 2037 1848 1665 2780 1683 1105 789 520 235 66 8 Monmouth 2491 1893 1776 1419 2290 1528 950 731 435 221 64 2 2296 1904 1603 1363 2212 1454 951 640 437 208 58 8 Gloucester 2513 1928 1856 1551 2546 1452 907 629 354 151 26 3 2331 1844 1618 1513 2324 1374 871 592 315 148 30 2 Cape May 411 359 341 227 418 284 178 93 63 22 4 405 353 321 264 373 260 175 85 43 25 4 Salem 1067 874 892 785 1090 761 500,253 143 66 11 1 1065 822 836 707 1100 765 498 277 156 67 7 Cumberland 1160 1004 921 738 1112 711 479 330 181 69 16 2 1137 986 873 718 1091 712 488 308 185 75 9 -25071 21204119745 17123 27001 17231111043 7053 4458 202153444 1 2393704791826716784 25817 16623 11007 7307 4705 216058663 2 c. ur CENSUS, 1830 (continued). SLAVES. FREE COLOURED PERSONS. MALES. FEMALES. MALES. FEMALES. -oo~.0 10 4 1.. Names of.. o 0 Counties. ~CCC~~CC,.~0 Ct t-ship, Hunterdon co., and in Montgomery t-ship, Somerset co., about 2 miles N. of Princeton. The surface of this hill is rugged; soil, deep clay, covered with heavy timber. It extends E. and W. about 6 miles, to the Millstone river, which seems to have forced a passage through it. Rocky Hill, p-t., Montgomery t-ship, Somerset co., at the N. E. base of Rocky hill, on the Millstone river, and turnpike road from New Brunswick to Lambertsville, 12 miles S. W. of Somerville, 185 N. E. from W. C., and 14 from Trenton; contains a grist and saw mill, a woollen manufactory, 2 stores, 2 taverns, and 12 or 15 dwellings. Rockaway Creek, Hunterdon co., rises by two branches; one from the northern part of Tewkesbury t-ship, and the other from the western border ROU 228 RYE of Readington t-ship, uniting in the latter t-ship, and thence flowing into Lamington river, or the north branch of the Raritan. By its longest arm the stream has a course of 12 miles. It is a fine, rapid mill stream. Rock Brook, tributary of Beden's Brook, rises in the Nashanic mountain, Amwell t-ship, Hunterdon co., and by a S. E. course of about 6 miles, unites with its recipient near the centre of Montgomery t-ship, Somerset co. Rock Mountain, fills the S. E. angle of Amwell t-ship, and the N. E. angle of Hopewell t-ship, Hunterdon co., and extends N. E. into Somerset co., having a length of about 10 miles, with a very irregular breadth. On the north it sends forth tributaries to the south branch of the Raritan river, and on the south to the Millstone river. The hill is of trap rock, imposed on old, red sandstone. Rocksbury, village of Oxford t-sp, Warren co., 5 miles S. of Belvidere, upon the road leading to Philipsburg; contains a tavern, store, 2 grist and 1 oil mill, an air furnace for small castings, and from 15 to 20 dwellings. Rocktown, small hamlet, of Amwell t-ship, Hunterdon co., 7 miles S. ofFlemington; contains 1 tavern, 1 store, and some 2 or 3 dwellings. It lies in the pass through the Rock mountain, and is named from the abundance of large rocks around it. Rocky Brook, a tributary of Millstone river, rises in Upper Freehold t-ship, Monmouth co., above Imlay's mill, and flows by a N. W. course through East Windsor t-ship, Middlesex co., about 9 miles to its recipient, on the boundary of South Brunswick t-ship, passing through Hightstown, and turning several mills. Rotten Pond, covering about 150 acres, on the boundary between Franklin and Pompton t-ships, Bergen co., and on the Ramapo mountain. Round Valley, in the S. E. angle of Lebanon t-ship, Hunterdon co., nearly surrounded by mountains; drained by Piscot Brook, a tributary of the south branch of the Raritan river. Rowandtown, small village of Newton t-ship, Gloucester co., on the road from Camden to Haddonfield, about 4 miles from the former, and 2 from the latter; contains some 6 or 8 dwellings, and several mechanics; surrounded by a country of sandy loam. Roxbury t-ship, Morris co., bounded N. and W. by the Hopatcong lake and Musconetcong river, which separates it from Warren and Sussex counties; N. E. by Jefferson t-ship; E. by Randolph; S. E. by Chester; and S. W. by Washington t-ships. Centrally distant from Morristown N. W. 14 miles; greatest length N. and S. 12, breadth E. and W. 10 miles; area, 35,840 acres; surface, generally mountainous; but the Suckasunny Plains extend some miles in length, by two or three in breadth. Schooley's mountain fills the greater portion of its area. On its summit lies Budd's Pond, two miles in length by one in breadth, whence flows a tributary of the south branch of the Raritan river; the main stream of which has its source in a small pond, two miles north of Drakesville, in this t-ship. Black river forms, in part, its eastern boundary. On the moun. tain the soil is clay and loam, but limestone is even there mixed with the granitic rock, and is found in the valley on the S. W. Flanders, Suckasunny, Drakestown, and Drakesville, are villages of the t-ship; at the two first of which are post-offices. Population in 1830, 2262. In 1832 the t-ship contained 410 taxables, 92 householders, whose ratables did not exceed $30 in value; 44 single men, 4 stores, 9 saw, 10 grist, and 2 fulling mills, 16 tan vats, 8 distilleries, 15 chairs and sulkies; and it paid state tax, $261 07; county tax, $584 51; poor tax, $300; and road tax, $800. Roxbury. (See Rocksbury.) Ryersons, a village at and near the junction of Ringwood and Pequannock rivers, in the S. E. angle of Pompton t-ship. There are here SAD 229 SAL 1 tavern, 3 grist mills, a carding machine, a furnace, and store, a Dutch Reformed church, an academy, and from 15 to 20 dwellings; surrounded by a rich and productive country. The post-office is at Pompton, on the right side of the river, in Morris co. Roy's Brook, a tributary of the Millstone river, rising at the S. E. foot of Nashanic mountain, and flowing by a devious, but generally, N. E. course of about 7 or 8 miles, to its recipient, below Rogers' mill. Saddle River, rises in the state of New York, 3 or 4 miles beyond the northern boundary of this state, and flows thence, southwardly, about 18 miles, through Bergen co., forming the boundary between Franklin and Harrington t-ships, Saddle River, and New Barbadoes, and Lodi t-ships, to its recipient, the Passaic river, about a mile above Acquackanonck. It has a rapid course, and considerable volume, and mills are strung thickly along its banks. The valley through which it flows is broad, and shows evidence in the gravel, and boulders, and water-worn hills, that at some day, a much larger volume of water ran through it. Saddle River t-ship. The t-ship and river both have their name from the shape of the former, which receives from the Passaic river the shape of a saddle. It is bounded N. by Franklin t-ship; E. by Saddle river, separating it from Harrington, New Barbadoes, and Lodi t-ships; S. by the Passaic river; and W. by Pompton river, which divides it from Morris co., and by Pompton t-ship. Centrally distant N. W. from Hackensacktown 8 miles: greatest length E. and W. 10 miles; breadth N. and S. 8 miles; area, 41,000 acres, of which, about 17,000 are improved: the surface is generally hilly, the First and Second mountains of Essex co., crossing the Passaic and continuing through it. On the east, however, between the Passaic and Saddle rivers, there is a neck of low and level land; soil, red shale and loam; the valleys fertile and well cultivated, and the hills well wooded. Through the valleys flow several small brooks, such as Singack, Preakness, Krokaevall, Goffle, and Ackerman's Brooks. Goffle, and New Manchester, a part of Paterson City, are the chief villages of the t-ship. Popula. tion in 1830, 3397. In 1832 there were 741 taxables, 496 householders, whose ratables did not exceed $30 in value; 80 single men, 7 stores, 8 grist mills, 1 cotton manufactory, 1 furnace, 10 saw mills, 13 tan vats, 2 distilleries, 1 wool factory, 506 horses and mules, and 1324 neat cattle over 3 years of age; and it paid state tax, $364 10; and county tax, $690 26. Salem County has its name from its chief town and seat of justice, Salem, founded by John Fenwicke, in the year 1675. By the act for ascertaining the bounds of all the counties in the province, passed 21st January, 1710, the following were the boundaries given to it: " Beginning at the mouth of a creek on the west side of Stipson's island, called Jecak's creek, now West creek; thence by said creek as high as the tide floweth; thence by a direct line to the mouth of a small creek at Tuckahoe, where it comes into the southernmost main branch of the fork of the Great Egg Harbour river; thence up the said branch to the head thereof; thence along the bounds of Gloucester county to the river Delaware, and thence by the river and bay to the place of beginning; and thus it included the whole of Cumberland county. The latter county was taken from it by the act of 19th Jan. 1748; and the boundaries then established, confirmed by the act of 7th Dec. 1763, by which the southern boundary of Salem county was then fixed as follows: Commencing at the middle of the mouth of Stow creek; thence by the same, opposite to the mills formerly of John Brick; thence up the middle of Stow creek branch opposite the house of Hugh Dunn; thence by a direct line to said house, leaving it in Cumberland county; and thence by a straight line N. 510 15' E. 94 chains, SAL 230, SAL to the house of Aziel Pierson, leaving that also in Cumberland county; thence N. E. by a line intersecting the line of Pilesgrove t-ship, 305 chains; thence by Pilesgrove line S. 470 E. to the middle of Maurice river, below the mouth of Muddy run; thence up the middle of said river to the foot of Scotland branch; thence up the middle of said branch to Gloucester line." The county is, therefore, now bounded by the Delaware bay and river on the S. W., W., and N. W.; by Gloucester co. on the N. E; and Cumberland co, on the S. E. Greatest length N. and S. about 30 miles; breadth E. and W. 26 miles; area, 320 square miles, or 204,936 acres; central lat. 390 33'; long. from W. C. 10 50' E. The surface of the county is geneIally flat. Its soil, in the northern and western parts, clay and loam, mixed more or less with sand, and generally productive, in wheat, grass, oats, &c. In the south-eastern parts, the soil is sandy and gravelly, and less fertile, but yielding much timber and cord wood of oak and pine, which succeed alternately when a clearing is made. This is particularly the case with a strip of about 20 miles long, extending across Lower and Upper Alloways Creek and Pittsgrove t-ships, denominated the Barrens. The county is well watered, having Oldman's creek on its northern boundary, Salem and Alloways creeks running through it centrally, and Stow creek on the southern limits. The county consists of alluvial and diluvial formation, the washings of the ocean and the primitive strata, being very irregularly mingled, and beds of stiff clay, loam, and gravel, are interspersed with white sea sand. From two to twenty feet below the surface, in several places, there is found a species of greenish blue marl, as at Pedricktown and Woodstown, which is used as manure. In it there are shells, as the ammonite, belemnite, ovulite, ostrea, terebratula, &c. similar to those found in the limestone and grauwacke of the transition; and in the horizontal limestone and sandstone. We have not heard of any bog iron ore in the county, though it probably exists; but sandstone and puddingstone, cemented with iron ore, are not uncommon. Salem, Woodstown, Sharptown, Sculltown, Pedricktown, Daretown, Pittstown, Allowaystown, Friesburg, Canton, Hancock's Bridge, and Quinton's Bridge, are villages of the co. The county was originally settled by Dutch and Swedes; and subsequently by the English, companions of John Fenwicke, who landed here in 1675; and it derived its principal inhabitants from the same source. Some Dutch fixed themselves at, and gave name to, Friesburg, in Upper Alloways Creek t-ship. The population by the census of 1830, amounted to 14,155, of whom, 6443 were white males; 6300 white females; 1 slave; 673 free coloured males, and 638 free coloured females. There were also in the county, 6 whites, deaf and dumb; 7 blind, and 27 aliens; and in 1832, taxables, 3092; 1103 householders, whose ratables did not exceed $30; 47 storekeepers, 6 fisheries, 13 grist mills, 19 saw mills, 2 carding machines with spinning machines for wool, 6 fulling mills, 7 tanneries, 15 distilleries, 19 stud horses, 3103 horses and mules, 7300 neat cattle, over 3 years of age; and the county paid for t-ship purposes, $5076; for county purposes, $7000; and state tax, $2156 60. There were in the county 7 Friends' meeting houses, 6 Methodist, 5 Baptist, 1 Seven-day Baptist, 2 Episcopalian, 2 Presbyterian, and 2 African Methodist churches; 1 academy at Salemtown, and sufficient other schools there, and in every t-ship, to teach the rudiments of an English education. The other public buildings of the county consist of a large court-bouse, with fire proof offices detached, of brick; a stone prison, a large poorhouse, with a farm annexed, and two buildings erected for masonic halls. SAL 231 SAL The trade of the county consists of wheat, rye, Indian corn, oats, and garden vegetables for market, lumber, and cord wood. Considerable quantities of grain are annually exported from Salem to the Eastern states. The courts of common pleas and general quarter sessions of the peace, for the county, are annually holden at Salem, on the first Tuesdays of March and December, the second Tuesday of June, and the third Tuesday of September; and the circuit court, on the second Tuesday of June and the first Tuesday of September. The county, by virtue of the constitution, elects one member of council, and three members of the Assembly. STATISTICAL TABLE OF SALEM COUNTY. S Population. Townships. g C Area. Surface. - S1810. 1820. 1830. Upper Alloways Creek, 10~ 9 34,000 p't level, rolling. 1921 2194 2136 Lower Alloways Creek, 12 9 30,000 level. 1182 1217 1222 Elsinborough, 6 4 8000 do. 517 505 503 Mannington, 9 8 20,000 do. 1664 1732 1726 Upper Penn's Neck, 9 7j 21,053 do. 1638 1861 1638 Lower Penn's Neck, 9 6 12,645 do. 1163 1158 994 Pilesgrove, 9 63 24,000 do. 1756 2012 2150 Pittsgrove, 15 7 44,000 p't level, p't roll. 1991 2040 2216 Salem, 2 2 1238 level. 929 1303 1570 ______ I 1 204,9361 12,7611 14,022 14,155 Salem t-ship and post-town, and seat of justice of Salem county, situate 171 miles N. E. of W. C., 65 S. of Trenton, and 34 S. E. from Philadelphia; lat. 390 32'; long. from W. C. 10 35'. The t-ship is of circular form, and is nearly surrounded by water, having on the N. W. the Salem creek, on the N. E. and E. Fenwicke's creek, a tributary of that stream, and on the W. another small tributary of the same stream. The town is distant from the Delaware, by the creek, 31 miles. The t-ship is about 2 miles in diameter, and contains 1238 acres of well improved land, of a rich sandy loam, divided into town lots and 12 farms. The town contains about 250 dwellings; a fine court-house, about 60 by 40 feet, of brick, with brick fire proof offices adjacent; 1 Episcopalian, 1 Methodist, 1 Presbyterian, 1 Baptist, 1 African Methodist, and 2 Quaker (one being orthodox and the other Hicksite) churches; 1 building of brick, of gothic architecture, designed for a masonic hall, but which is now appropriated to other purposes, the lodge being extinct; a bank with capital paid in of $75,000; a stone jail with yard, surrounded by a high stone wall, both of small dimensions; 1 market house, 2 fire engines, 2 public libraries, 1 academy, and 5 daily schools for teaching the rudiments of an English education; 5 Sunday schools, 2 printing offices, at each of which is printed a weekly newspaper, called, respectively, "The Salem Messenger," and "The American Statesman;" 21 stores, 2 hotels, 7 physicians, 5 lawyers, 3 lumber yards, 1 steam mill which grinds much grain, 1 horse mill, 5 apothecaries' stores, 1 livery stable. A steamboat leaves the town daily, for Delaware City and Newcastle, to meet the morning steam-boat from Philadelphia; 1 four horse stage runs daily to Philadelphia, another to Pennsgrove, on the Delaware, to meet the Wilmington steam-boat for Philadelphia; a two horse daily line to Bridgetown, and a two horse line to Centerville, once a week. The creek at the SAL 232 SAN town, is 152 yards wide, over which is a wooden bridge, resting on wooden piers, with a draw for the passage of vessels. Over Fenwicke creek, a short distance above its junction with Salem creek, is another wooden bridge, a neat structure, roofed. Vessels of 50 tons may approach the town safely, bIut the bar at the mouth of the creek prevents the entry of vessels drawing more than eight feet water. Large quantities of wheat, rye, oats, and corn, are exported from this place to the eastern states. The streets of the town are wide--footways paved, and bordered with trees; the houses of frame and brick, the former painted white, are surrounded with gardens and grass lots, and adorned with flowers, giving to the place, a cheerful and healthy appearance, surpassed by few villages in the United States. The t-ship contained in 1830, 1570 inhabitants: in 1832, 267 householders, whose ratables did not exceed $30 in value; and 397 taxables, 2 tan yards, 1 distillery; and it paid taxes for t-ship purposes, $426; county use, $78 25; and state use, $233 35. The site of the town of Salem was the first spot visited, and we believe, the first settled, by the English emigrants to West Jersey. Soon after the sale by Lord Berkeley of one moiety of the province, to Edward Byllinge, John Fenwicke, the agent of the latter set sail, (in 1675) to visit the new purchase in a ship from London, called the Griffith. After a short passage, he landed at this pleasant spot, which, from its aspect of peace, he called Salem. He brought with him two daughters, and several servants, two of which, Samuel Hedge and John Adams, afterwards married his daughters. Other passengers were, Edward Champness, Edward and Samuel Wade, John Smith, Samuel Nichols, Richard Guy, Richard Noble, Richard Hancock, John Pledger, Hypolite Lefever, and John Matlock, and others, who were masters of families. Salem Creek, Salem co., rises in Pittsgrove t-ship, and flows N. W. through that and Pilesgrove t-ship, by Woodstown and Sharptown, about 17 miles to the S. W. angle of Upper Penn's Neck t-ship; thence turning S. and S. W., it divides Mannington and Lower Penn's Neck t-ships, and passing by Salem, empties into the Delaware river, 31 miles below that town. There is a bar at the mouth, on which at high tide there are eight feet water. Vessels of 50 tons approach the town safely; but within the bar, there is water, it is said, for vessels of 300 tons burden. The whole length of the creek may be about 30 miles, and it is navigable for shallops nearly half that distance. A short canal of 3 or 4 miles, through Upper and Lower Penn's Neck t-ships, unites the creek with the Delaware, saving a distance to the craft which navigate the creek, of about 20 miles. Samptown, Piscataway t-ship, Middlesex co., about 8 miles N. from New Brunswick, on the left bank of Cedar creek; contains a Baptist church, 10 or 12 houses, tavern and store, in a tolerably fertile country of red shale. Sand Hills, small hamlet of Nottingham t.ship, Burlington co. There is a tavern, and 12 or 15 dwellings here; the turnpike road, and the Camden and Amboy rail-road, run near it. The carriages from and for Trenton meet the rail-road cars here. Distance from Trenton, about 5, and from Bordentown, 3 miles. Sand Hills, noted hills in the N. W. part of South Brunswick t-ship, Middlesex co., covering an area of about 4 miles by 2; about 7 'miles W. from Brunswick. Sandy Hook, Sandy Hook bay: the first is a sandy beach, extending northward, from Old Shrewsbury inlet, and the S. point of the highlands of Nevisink, 6 miles, of an irregular width, varying from half a mile to a mile, forming the eastern boundary of the bay. The bay sets in from the Raritan bay, southwards, and is about 7 miles wide, between Point SAN 233 SCH Comfort, the western cape, and the p6nt of the Hook. Its depth to the S. point of the Nevisink hills, which form the coast for about 6 miles, is about 6 miles. The western shore encroaches, eastwardly, upon the water until it is narrowed to threequarters of a mile. Sand Pond, a small sheet of water, in Wallkill mountains, Vernon t-ship, Sussex co., which sends forth a small tributary to the Wallkill river. Sand Pond, the source of Stout's brook, on the N. line of Hardwick t-ship. Sandtown, or Berkely, village of Greenwich t-ship, Gloucester co., on Mantua creek, 4, miles S. W. from Woodbury; contains a store, tavern, 12 or 15 dwellings, and an Episcopal church. Sandtown, Nottingham t-ship, Burlington co., on the road from Trenton to Cranberry, about 5 miles E. of the former, on a sandy plain; contains a tavern, smithery, and some half-dozen dwellings. Sandistone t-ship, Sussex co., bounded on the N. E. by Montague t-ship; S. E. by the Blue mountain, which divides it from Newton, Frankford, and Wantage t-ships; S. W. by Walpack t-ship; and W. by the Delaware river; centrally distant, N. W. from Newton, 12 miles; greatest length, -8~, breadth, 7 miles; area, 19,320 acres; surface on the E. mountainous, and on the W. river alluvion. Population in 1830, 1097. There were in the t-ship in 1832, 65 householders, whose ratables did not exceed $30; taxable inhabitants, 240; 4 merchants or traders, 5 pair of stones for grinding grain, 1 carding machine, 4 saw mills, 204 horses and mules, and 841 neat cattle over 3 years; 13 tan vats, 1 distillery. The t-ship paid state and county tax, $426 77; poor tax, $100; road tax, $500. It is watered by the Big and Little Flat Kill creeks, and their tributaries, and by the river Delaware. The Morristown and Milford turn. pike road crosses it north-westward ty, on which lies the post-office, dis 2G tant 241 miles from W. C., 83 from Trenton, and 13 from Newton. Be. tween. the Blue mountain and 'the Delaware, there is a rich flat, increasing from two to six miles in width, through which runs a bed of transition limestone, girded by an alluvial belt. This flat pro4uces excellent crops of wheat. The t-ship was originally settled by Dutch, whilst that people held possession of New York. Sandy New, small hamlet of Middletown t-ship, Monmouth co., 9 miles N. E. of Freehold; contains a tavern, and some 3 or 4 dwellings, in a fine fertile country. Sargeantsville, p-t. of Amwell t-ship, Hunterdon co., 6 miles S. W. from Flemington, 23 N. from Trenton, and 177 N. E. from W. C.; contains a tavern, store, and some 6 or 8 dwellings. Surrounding country hilly and poor; lands rated at $20 per acre. Near this village, on a farm of 150 acres, Mr. R. Rittenhouse has established the Mantua Manual Labour Institute, with accommodations for about 30 students, and the purpose to increase them as they may be required. At this institute are taught the Greek and Latin languages, and all other branches of learning, taught at similar institutions. About three hours every day, Saturday and Sunday excepted, are employed in manual labour, by the students, for which they receive reasonable compensation. The charge for tuition, board, washing, lodging, candles, and fuel, is $25 per quarter. Saw Mill Creek, a marsh stream. about 2 miles in length, in Lodi t-sp, Bergen co. Saxtonville, small hamlet of Amwell t-ship, Hunterdon co., on the river Delaware, 12 miles S. W. from Flemington; contains some 3 or 4 dwellings; named from the proprieStor. Schooley's Mountain, Schugl's Hills, form part of the central gra- nitic chain, which extends in a N. E. - and S. W. direction, across the state Sof New Jersey, from the Delaware to SCH 234 SCH the Hudson river. The name, Schooley's Mountain, derived from a family formerly owning a considerable portion of its soil, is applied chiefly, to that portion of the chain which crosses the N. W. part of Morris county. The height of the mountain above its base, has been determined by geometrical measurement, to be more than 600 feet; and a calculation, made by approximation, on the falls of water, on the different mill dams along the rapid channel of the Musconetcong river, to its junction with the Delaware, and on the descent, thence to Trenton, gives to that base an elevation of 500 feet above tide; making the height of the mountain, above the level of the ocean, somewhat more than 1100 feet. From the top of the mountain a turnpike road runs northward to Sussex, another westward to Easton, a third eastward to New York, and a fourth southward towards Trenton. The mineral spring near the top has given much celebrity to this region. It is said to have been known to the aborigines, and to have been employed by them as a remedy, which, with characteristic selfishness, they would have concealed from the whites. The latter, however, have resorted to it, since the settlement of the country. 'Remarkable cures have been ascribed to it, and some persons have habitually frequented it, season after season, on account of the benefit they have derived from the use of its waters. It is situated in Washington t-ship, Morris co., 19 miles N. W. of Morristown, 50 from New York, 70 N. E. from Philadelphia, 56 from Trenton, and 213 from W. C. The spring is, in strictness, a rill which issues from a perpendicular rock, having an eastern exposure, between 40 and 50 feet above the level of a brook, which gurgles over the stones, and foams down the rocks in 'the channels beneath. A small wooden trough is adapted to the fissure, so as to convey the water to a platform where the visiters assemble, and to the structure containing the baths. The temperature of the water is 560 F. being 60 warmer than the spring water nearer the summit. The fountain emits about 30 gallons per hour; which quantity does not vary with any change of season or weather. The water, like other chalybeates, leaves a deposit of oxidized iron, as it flows, which discolours the troughs, baths, and even the drinking vessels. The bare taste and appearance shows that it is a chalybeate; and it is strongly characterized by the peculiar astringency and savour of ferruginous impregnations. Though remarkably clear when first taken, the water becomes turbid upon standing for some time in the open air, and after a long interval, an irridescent pellicle forms on its surface. Ochre and other indications of iron are dispersed extensively through the surrounding rocks and soil. Iron ore is so plentiful in the vicinity that furnaces are worked, both in the eastern and western district of the chain, and much of the ore is magnetic. Grey limestone is found at the base of the hills and along the valleys. The analysis of the water, by Dr. M'Nevin of New York, has given the following result: Vegetable extract 92, muriate of soda 43, muriate of lime 2.40, muriate of magnesia 50, carbonate of lime 7.99, sulphate of lime 65, carbonate of magnesia 40, silex 80, carbonated oxide of iron 2, loss 41-total 16.50. The iron from the mineral water is very easily separated. Exposure to the atmosphere induces metallic precipitation; and transportation to a distance, even in corked bottles, produces a like effect; and when thus freed from its iron, the water may be used in making tea. The heat of ebullition, also, seems to separate the ferruginous ingredient, and to prevent any dusky or black tint; for if an infusion of green tea be mixed with water fresh from the spring, a dark and disagreeable hue is instantly produced, The carbonic acid which this water contains, is altogether in a state of combination, and hence it never oc SCH 235 SCO casions flatulence or spasm in the weakest stomach, whilst it gradually strengthens the digestive powers.This chalybeate is considered by medical men, as one of the purest of this, or any other country, and as beneficial, in most cases of chronic disease, and general debility, and especially in cases of calculus in the bladder or kidneys. To those in pursuit of health or pleasure, this region presents equal attraction. A short journey brings the patient from the level of tide water to a very desirable elevation, which tempers the summer's heat, and braces the relaxed frame. The plain on the top of the mountain, affords very pleasant rides amid ever changing and delightful scenery, in which cheering views of improved and profitable agriculture are blended with the velvet plain, the craggy hill, and shadowy vale. Thus the invalid has every incentive to exercise, by the highest gratification from his exertions. To him who seeks relaxation from the cares of business, or to change sedentary occupation and feebleness for activity and vigour, the excellent society which assembles here during the summer months, the abundant sport in fowling and fishing, and the delightful scenery, hold forth strong inducements; to which, we would be unjust not to add the excellent fare, cheerful attention, and comfortable accommodation given to visiters at the three hotels, and several farm houses in the vicinity of the spring. Belmont Hall, kept by Mr. G. Bowne, situate on the highest part of the mountain, shadowed and embowered by various fruit, forest, and ornamental trees, is a fine building, 50 feet square and three stories high, with very extensive wings; and the Heath House of Mr. E. Marsh, less showy, but not less commodious or pleasant, afford the visiter all the means of enjoyment usual at wateringplaces; whilst their distance from the fountain, (about I of a mile) by adding the benefits of exercise, does not diminish the salubrious effects of the water. There is, however, a third house, immediately at the spring, where such visiters as desire to be near it, can be accommodated. The season commences here on the 1st of June, and continues during the hot weather. For the man of science, the mineral region, and geological formation of the country, possesses much interest. It abounds with iron and other minerals. The first, in a mine opened within gun-shot of the Heath House, is highly magnetic; so much so, indeed, as to render the use of iron tools about it very inconvenient. The following extraordinary circumstances we give on the authority of Mr. Marsh. The tools, by continued use, become so strongly magnetized, that in boring the rock, the workman is unable, after striking the auger with his hammer, to separate them in the usual mode of wielding the hammer, and is compelled to resort to a lateral or rotatory motion for this purpose; and the crowbar has been known to sustain, in suspension, all. the other tools of the mine, in weight equal to a hundred pounds. These facts are supported by the assurance of General Dickenson, that the magnetic attraction of the tools, used in his mine, adds much to the fatigue of the workmen; and that it is of ordinary occurrence for the hammer to lift the auger from the hole during the process of boring. Besides the houses for public entertainment, at and near the springs, there are several others, which, with a church and school house built by Mr. Marsh, with the aid of the visiters, and a post-office, give the neighbourhood a village-like appearance. And, among the attractions of the mountain, we must not forbear to mention the fishing and boating on Budd's Pond, a beautiful sheet of water, two miles in length by one in breadth, at seven miles distance from the spring. This little mountain lake of great depth and clear as crystal, abounds with perch, sun, pike, and other fish, Scotch Plains, p.t. of Westfield SEC 236 SHI t.ship, Essex county, 14 miles from 4 miles long by half a mile wide; Newark, Somerville, New Bruns- terminating in a very distinguished wick, Morristown, Elizabethtown elevation, called Snake-hill. The Point, and Amboy; 214 miles N. E. island is crossed by the turnpike and from W. C., and 48 from Trenton, rail-road from Hoboken to Paterson. on the road from Springfield to So- Serepta, a post-office, Warren co. merville; contains, within the diame- Seven Causeways, noted union of ter of a mile, 1 Baptist church, an 7 roads, near the junction of 4 mile academy, 1 tavern, 2 stores, 3 grist branch, with Inskeep's branch of the mills, 2 saw mills, 1 oil mill, 1 straw Great Egg Harbour river, 25 miles' paper mill, and about 70 dwellings. S. E. from Camden, on the line of The surface of the adjacent country Deptford and Gloucester t-sps, Glouis level, except on the W. and N. W. cester co. which is mountainous; soil, clay loam, Shabacung Island, formed by the well cultivated, and productive, and Delaware river, and part of the t-ship valued, in farms, at $40 the acre. of Montague, Sussex co., near the Within 2 miles of the village, a bed remote N. end of the state. of carbonate of lime has been lately Shark River, mill stream, rises in discovered, in which are metallic ap- Shrewsbury t-ship, Monmouth co., pearances supposed to be gold and and flows along the boundary, besilver, but which are, probably, only tween that and Howell t-ship, about deceptive pyrites. 6 miles, into a broad estuary, and Scott's Mountain, lying in Green- thence about 3 miles through Shark wich, Oxford, and Mansfield t-ships, inlet, into the Atlantic ocean. Warren co., forms part of the chain Sharptown, p-t. and village of of the South mountain, of which this Pilesgrove t-ship, Salem co., on Saportion covers much of the area of lem creek, between 3 and 4 miles the three t-ships above named. The below Woodstown, and 8 or 9 miles height of the mountain here may be N. E. from Salem, 162 from W. C., from 700 to 800 feet above tide, and and 56 S. from Trenton; contains it is composed of granitic rock, based between 40 and 50 dwellings, 1 taon, or breaking through limestone. vern, 2 stores, 1 grist mill, and one It abounds with iron' of several varie- school house, used occasionally as a ties, which, for near a century, has church. The surrounding country is been extensively worked, near Oxford level and fertile. furnace; where Messrs. Henry and Shawpocussing Creek, small triJordqn are, now, extensively engaged butary of the Delaware river, which in the iron manufacture. The moun- rises in Knowlton t-ship, Warren co., tain is generally well wooded, and at the foot of the Blue mountain, and the valleys fruitful. flows S. W. to its recipient, having a Scrabbletown, hamlet of Hanover course of five miles. t-ship, Burlington co., 10 miles E. Shelltown, on the line between from Mount Holly, and 12 S. E. from Hanover t-ship, Burlington co., and Bordentown; contains a tavern, and Upper Freehold t-ship, Monmouth 6 or 8 cottages, in a poor, sandy, pine co., on a small branch of the Crosscountry. wicks creek; contains some halfSeulltown, a village of Upper dozen dwellings. There is a Friends' Penn's Neck t-ship, Salem co., on meeting house near it, in Monmouth Oldman's Creek, at the head of navi- county. gation; containing from 20 to 30 Shiloh, p-t. in the S. W. angle of dwellings, a tavern, and 2 or 3 stores, Hardwick t-ship, Warren co., 12 It is about 12 miles N. E. of Salem. miles N. E. of Belvidere, and 60 miles Secaucas,. island in the Cedar from Trenton. swamp, of the Hackensack river, in Shiloh, hamlet of Cumberland co., Bergen t-ship, Bergen co. It is near on the line dividing Hopewell from SHR 237 SIX Stow Creek t-ship, about 5 miles N. by the Nevisink and Shrewsbury W. of Bridgeton; contains 8 or 10 rivers, and their tributaries; E. by dwellings, and a Seventh-day Baptist White Pond, and Deal creeks, and church. The country around it is of S. E. by Shark river; surface level; light loam, but in an improving con- soil, clay and sandy loam, on marl, dition. of good quality on Swimming river, Shipetaukin, small branch of the and its tributaries; on the S. of these, Assunpink creek, rising in Lawrence sandy, poor, and covered with pine. t-ship, Hunterdon co., and flowing S. On the E., along the shore near and by a course of 5 or 6 miles to its re- below the Long Branch boardingcipient, through an extensive body of houses, is a very fertile black sand. meadow land. The sea shore in this t-ship, is geneShoal Harbour Creek, small rally high and bold, and without stream at the N. W. foot of the Ne- marsh. The celebrated Long Branch visink hills; runs about a mile and boarding houses, so named from their a half N. E. into Sandy Hook bay. vicinity to a long branch of ShrewsShrewsbury Inlet, Old, was open- bury river, are in this township. ed in 1778, from the ocean into the Population in 1830, 4700. In 1832 estuary formed by the Nevisink and the t-ship contained about 900 taxaShrewsbury rivers, Monmouth co.; bles; 265 householders, whose ratawas closed by the moving of the bles did not exceed $30; and 150 sands in 1810, but was reopened in single men; 21 stores, 5 saw mills,, 1830. Vessels now pass through it. 12 run of stones, for grinding grain, Shrewsbury River, so called, is a 1 carding machine, 60 tan vats, 730 continuation of Sandy Hook bay, horses and mules, 1650 neat cattle, Shrewsbury t-ship, Monmouth co., 3 years old and upwards; and paid which receives from the t-ship, state and county tax, $2144 69. Shrewsbury river proper, a small Shrewsbury, Eatontown, Colts Neck, stream of 6 or 7 miles long, Long Long Branch, and Tinton's Falls, Branch, and several other tributaries, are villages and post-towns of the This arm of the bay, from the mouth t-ship. of the Nevisink river, is about 5 miles Several thousand acres in this long, with an average breadth of a t-ship were settled in 1682, anid the mile'ahd a half, and has a considera- inhabitants were then computed at ble quantity of salt marsh on its bor- 400. Lewis Morris of Barbadoes, ders. It is separated from the Nevi- the brother of Richard Morris, the sink by a high neck of land, 2 miles first settler at Morrisania, New York, wide. and uncle of Lewis Morris, subseShrewsbury, p-t. of Shrewsbury quently governor of New Jersey, had t-sp., Monmouth co., betweenrShrews, iron works and other considerable bury and Nevisink rivers, 12 miles improvements here. E. from Freehold, 50 S. E. from Singack, small tributary of PreakTrenton, and 215 N. E. from W. C.; ness brook, Saddle River t-ship, Bercontains 12 or 15 dwellings, an Epis- gen co. copalian and Presbyterian church, 1 Six Mile Run, village and stream. tavern, and 2 stores. Soil, sandy The first, a post-town on the Princeand light, ton and Brunswick turnpike, (and on Shrewsbury t-ship, Monmouth co., the line between New Brunswick bounded N. by Middletown t-ship; t-ship, Middlesex co., and Franklin E. by, the Atlantic ocean; S. by t-ship, Somerset co.,) 12 miles from Howell t-ship, and W. by Freehold. the one, and 4 from the other, 189 Centrally distant 7 miles E. from from W. C., and 23 from Trenton; Freehold; length N. and S. 13, contains a Dutch Reformedchurch, breadth E. and W. 13 miles; area, 2 taverns, 1 store, and from 10 to.12 64,000 acres; drained on the N. N. dwellings. Soil, red shale, level, and SNU 238 SOM well cultivated.-The stream flows distone t-ship, Sussex co., at the east from North Brunswick, through foot of the Wallkill mountain, and in Franklin t-ship, by a W. course of the valley of the Pacake creek, on about 6 miles, to the Raritan river, the Paterson and Hamburg turnpike Slabtown, hamlet of Springfield road, about 15 miles N. E. of Newt-ship, Burlington co., on the road ton; contains a Methodist meeting from Mount Holly to Bordentown, 4 house, a store, tavern, and tannery, miles N. of the former; contains a and 6 or 8 dwellings. Friends' meeting house, and 10 or 12 Sodom, p-t. of Knowlton t-ship, dwellings, 1 store, and 2 taverns. Warren co., on Paulinskill, 12 miles * Slab Cabin Branch, of the Ran- N. of Belvidere, 4 E. from Columbia; cocus creek, rises in Monmouth co., contains a grist and saw mill, tavern, and flows a S. W. course of 10 miles, store, and some half-dozen dwellings. to its recipient, the North Branch of Some smelting works have lately that creek, on the south boundary of been erected here, said to be for preHanover t-ship, Burlington co. Ha- cious metals, discovered in the Jenny nover furnace lies upon it, and it turns Jump mountain. several mills. Sodom, Lebanon t-ship, HunterSlab Cabin Brook, Dover t-ship, don co. (See Clarkesville.) Monmouth co., a small stream about Somerset County, was taken from 3 miles in length, which flows into Middlesex, by an act of the propriethe south side of Toms' Bay. taries in 1688. Its bounds were subSleepy Creek, a tributary of Atsion sequently modified by the legislative river, rises in Hereford t-ship, and acts of 1709, 1713, and 1741. It is flows by a S. E. course of about 6 now bounded on the N. and N. E. miles, to its recipient, in Galloway by Morris co.; on the E. by Essex t-ship, Gloucester co. and Middlesex; on the S. E. by Mid. Smith's Creek, a small mill stream, dlesex; and on the S. W. and N. W. which rises near Herbertstown, in by Hunterdon co.: greatest length Hopewell t-ship, Hunterdon co., and N. and S. 28 miles; breadth E. and flows S. W. by a course of 6 miles, W. 20 miles; area, 189,800 acres, or to the river Delaware, at the foot of about 297 square miles: central lat. Belle Mount. 400 34'; long. 20 15' from W. C. Smithrille, village of Galloway The whole county lies within the t-ship,, Gloucester co., 42 miles S. E. transition formation, if the old red of Woodbury, and 2 miles E. from sandstone be included within it. Hills Leed's'Point; contains a tavern, store, of trap rock, upon the sandstone base, Methodist meeting house, and 10 or are scattered over it, as at Rock Hill, 12 dwellings; surrounded by pines, near the southern boundary, Rocky, and near the salt marsh. or Nashanic mountain on the S. W., Snake Hill, a noted eminence of and Stony Hill N. of Somerville. Secaucas Island, in the marsh on The ridges N. of the last, contain Hackensack river, and a very pro- grauwacke, and the valleys transiminent object from the road, between tion limestone, generally of a grey Jersey City and Newark. Its for- colour. The surface of the county mation is of trap rock, on sandstone is various: the N. W. section being base. mountainous; the S. and S. W. hilly, Snover's Brook, rises in Sucker whilst the centre and S. E., the valPond, Stillwater t-ship, Sussex co., ley of the Raritan, is either level, or and flows by a S. W. course of about gently undulating. The soil varies 8 or 9 miles through the north part with the surface: that of the hills is of Hardwicke t-ship, into Paulinskill, generally of clay and stiff loam, whilst on the northern part of Hamilton t-sp, that of the plains is a sandy loam, Warren co. formed of the red shale; and the Snufletown, a small village of San- mountain vales, as we have already SOM 289 SOM observed, are of limestone. All are, thence to Philipsburg, opposite to however, fertile under proper culture, Easton. From North Branch a turnand the county may vie with her pike road runs northward over Schooneighbours of Hunterdon, Essex, and ley's mountain to Hacketstown, in Middlesex, in the variety and quanti- Warren co.; and a rail-road is in ty of agricultural products. contemplation, through Somerville to The county is well watered. It is Belvidere. cut into two, almost equal parts, by The post-towns of the county are the main stem and south branch of Baskingridge, Bound Brook, Flagg, the Raritan river, which receives the town, Harlingen, Kline's Mills, Lesnorth branch, flowing southward and ser Cross-Roads, Liberty Corner, centrally through the northern sec- Martinsville, Millington, Millstone, tion, and the Millstone river, flowing North Branch, Peapack, Pluckemin, northward and centrally through the Princeton, Rocky Hill, Somerville, southern section; and it is thus by the county town, and Warren. these three streams, divided into four The county was early settled by parts, intersected by smaller brooks the Dutch, whose industrious habits and creeks, in almost every direction. soon rendered it remarkable for its The Delaware and Raritan canal fruitfulness, and it became soon one enters the county at Kingston, with of the most thickly settled of the prothe Millstone river, and follows that vince. By the census of 1830, the stream to its junction with the Rari- population amounted to 17,689 souls, tan, 3 miles S. E. of Somerville, of whom 7665 were white males, whence it pursues the valley of the 7717 white females; 945 free colourlast stream to Brunswick. ed males, 914 free coloured females; Copper ore has been discovered in considerable veins in the first range of hills, N. E. from Somerville; and mines have been opened in at least two places; the first within 2, and the second within 6 miles of the town. Attempts have been made to work both, but every effort has hitherto been unsuccessful: and yet the ore is said to contain not only a very valuable proportion of copper, but to be worth working on account of the gold which it yields. Public opinion attributes these failures more to the want of adequate capital to sustain the expense of the first steps in mining, than to the want of skill, or poverty of ore. It is said, also, that particles of gold and silver have been discovered in a gangue of carbonate of lime, on Green Brook, N. of the Scotch Plains. -A turnpike road from Brunswick, enters the county by a bridge over Bound Brook, and passes through Somerville, to North Branch, and 214 male slaves, 234 female slaves. Among these there were 118 aliens; deaf and dumb, 14 whites-blind, whites, 17, coloured, 3. In 1832, there were in the co., 3500 taxables; 668 householders, whose ratables did not exceed $30; 391 single men, 68 merchants; 44 saw mills, 64 grist mills, or run of stones for grinding grain, 8 fulling mills, 211 tan vats, 28 distilleries, 11 carding machines, 4621 horses and mules, and 8634 neat cattle, above the age of 3; years; and it paid in state tax, $2642 86, and in county tax, $6000. The courts for the county are holden at Somerville; the common pleas, orphan's court, and general quarter sessions, on the following Tuesdays: viz. last in January, 3d in April, 3d in June, and 1st in October; and the circuit courts on the 3d Tuesday in April, and the 1st in October. SOM 240 SOU STATISTICAL TABLE OF SOMERSET COUNTY. Population. Townships. c Area. Surface. 1810 1820 1830 Bedminster, 8 4j 19,300 hilly, 1312 1393 1453 Bernard, 9 7 25,000 mountainous, 1879 2063 2062 Bridgewater, 13 11 35,000 level, 2906 3147 3549 Franklin, 13 8 30,000 do. [level, 2539 3071 3352 Hillsborough, 10 7 36,000 part hilly, part 2456 2885 2878 Montgomery, 8 8 26,500 hilly, 2282 2495 2834 Warren, 8 4 18,000 mountainous, 1354 1452 1561 1189,800 1 14,728 16,506 17,689 Somers' Point, p-t. and port of entry for Great Egg Harbour district, upon the Great Egg Harbour bay, about 43 miles S. E. from Woodbury, 88 from Trenton, and by postroute 196 from W. C. There is a tavern and boarding house here, and several farm houses. It is much resorted to for sea bathing in summer, and gunning in the fall season. Somerville, p-t. and seat of justice, of Somerset co., situate about a mile N. of the Raritan river, on the turnpike road from New Brunswick to Philipsburg, 14 miles N. W. from: the former, 33 S. E. from the latter, or.from Easton, 28 N. E. from Trenton, and 199 from W. C. It lies upon a high well cultivated plain of red shale, about 2 miles south of a ridge of the South mountains; in which are some noted copper mines. It contains a Dutch Reformed church, a Methodist meeting, an academy where the classics and mathematics are taught, a boarding school for young ladies, 3 taverns well kept, and 7 stores, 1 large grist mill, 5 practising attorneys, 4 physicians, and 1 resident clergyrtan, 600 inhabitants, and about 100 diellings. The court-house and other public buildings, are large and commodious, and many of the private dwellings are very neat; and the town is a healthy, pleasant, and desirable place of residence. The proposed rail road from Elizabethtown to the Delaware, at Belvidere, is designed to pass through it. South Amboy, p-t. of South Amboy t-ship, Middlesex co., at the head of the Raritan bay and mouth of the Raritan river, 15 miles below New Brunswick, and 35 N6 E. from Trenton; contains a hotel and some 15 or 0, dwellings, and an extensive manufactory of stone ware, made from clay obtained in the vicinity. This clay is of excellent quality, and much of it is exported to various parts of the country. It is used in the manufacture of delf ware at Jersey City, and in the fabrication of china at Philadelphia. The beds extend in the hills for several miles around the point. The turnpike road from Bordentown, and the Camden and Amboy rail road terminate here. There is a safe harbour here for vessels, and deep water at the landing. South Amboy t-ship, Middlesex co., bounded N. by the Raritan river; N. E. by the Raritan bay; S. E. by Middletown and Upper Freehold t-ships, of Monmouth c6.; S. W. by Millstone river; and N. W. by North Brunswick and South Brunswick t-ships. Centrally distant S. E. from New Brunswick 9 miles: greatest length N. E. and S. W. 18, and breadth 6 miles; area, 64,000 acres; surface, flat; soil, sandy; drained on the S. W. by the Millstone, and on the N. E. by South river and its tributaries, Tenant's run, Deep run, Matchaponix brook, and Manalapan creek. The turnpike and rail road from Bordentown to Amboy run SPR 241 SPR through the t-ship. Upon the former lie the post-towns of Cranberry and Spotswood, and South Amboy. Population in 1830, 3782. South River. (See Manalapan Brook.) South Brunswick. (See Brunswick, South.) Sparta, p-t. of Hardistone t-ship, Sussex co., at the west foot of the Wallkill mountain, 236 miles N. E. of W. C., 78 from Trenton, and 8 from Newton, on the Union turnpike road, in the valley, and near the source of the Wallkill river. This is a pleasant village, having some very good houses, a neat Presbyterian church with cupola, a school house, 2 grist mills, 2 saw mills, 4 forges for making iron, in which there are, together, 6 fires; 1 tavern, 3 stores, and from 35 to 40 dwellings. Iron and zinc ores are abundant in the neighbourhood; but only a small portion of the first is used in making iron here; the chief part being carted from the mines in Morris co., at the cost of $2 50 the ton. The zinc ore is not worked. The soil in the valley is limestone, and tolerably well cultivated. Speertown, agricultural village of Bloomfield t-ship, Sussex co., 7 miles N. of Newark, near the foot of the First mountain; contains from 20 to 30 dwellings, 1 tavern, 1 store, a Dutch Reformed church, and school; surrounded by a country of red shale, carefully cultivated. Spottswood, thriving p-t. of South Amboy t-ship, Middlesex co., on the turnpike road and rail road from Bordentown to South Amboy, about 25 miles from the former, 202 from W. C., arid 26 from Trenton, and on the South river; contains a large gristmill, a fine Presbyterian church of wood, a Dutch Reformed church, 1 tavern, 2 stores, 2 tobacco manufactories, and about 30 dwellings. Spruce Run, Lebanon t-ship, Hunterdon co., flows S. W. through the north part of the t-ship, and along the west boundary, and is a branch of the Raritan river. 2H Springfield t-ship, Essex county, bounded N. by Livingston t-ship; E. by Orange and Union t-ships; S. by Westfield and New Providence t-ships; and W. by the Passaic river, which divides it from Chatham t-ship, Morris co. Centrally distant W. from Newark 8 miles: greatest length N. and S. 6, breadth E. and W. 5 miles; area, 13,500 acres; surface, generally hilly; soil, clay loam and red shale. It is washed on the eastern boundary by the Rahway river, which receives several tributaries from the t-ship. Springfield the posttown; Vauxhall and part of Chatham are villages of the t-ship. The pretensions of Springfield, as an agricultural t-ship, are not high, but it claims consideration for its paper manufactories. Population in 1830, 1653. In 1832 there were 365 taxables, 97 householders, whose ratables did not exceed $30; 93 single men, 7 merchants, 1 grist mill, 3 carding machines, 12 paper mills, 6 tan vats, 1 woollen mgnufactory, 1 distillery, 220 horses and mules, and 818 neat cattle, above the age of 3 years. It paid state tax, 198 96; county, $520 56; poor, $500; road, $8. Springfield p-t. of the preceding t-ship, on the turnpike road from Elizabethtown to Morristown, 7 miles W. from the one, and 10 E. from the other, 216 N. E. from W. C., and 50 from Trenton, and upon the Rahway river, at the foot of the First mountain; contains about 200 dwellings, some of which are neat structures; 1 Presbyterian church, with cupola and bell; 1 Methodist church, 3-taverns, 5 stores, 2 grist mills, 1 saw mill, and 10 paper mills. The surface of the country around it, is rugged, and the soil, a stiff cold clay, unproductive; and farms are not averaged at more than 20 dollars the acre. Springfield, t-ship, Burlington co., bounded N. by Chesterfield, and Mansfield t-ships; S. E. by Hanover St-ship; S.W. by Northampton t-ship, and W. and N. W. by Burlington SQU 242 STA t-ship; centrally distant N. E. from Mount Holly, 5 miles; greatest length, E. and W. 10 miles; breadth, N. and S. 6 miles; area, 18,000 acres; surface level; soil, sand and sandy loam, well cultivated, and productive; drained, N. by the Assiscunk creek, which forms the northern boundary, and its branches, and S. by the tributaries of the north branch of the Rancocus creek. Slabtown, Jobstown, and Juliustown, are villages of the t-ship, at the two last of which, are post-offices. The population, a great portion of which are Friends, was, in 1830, 1531. In 1832, the t-ship contained, 3 Friends' meeting houses, 147 householders, whose ratables did not exceed $30, in value; 61 single men, 330 taxables; 3 stores, 14 tan vats, 1 distillery for cider, 31 dearborns, 100 covered wagons, 17 chairs, 11 gigs and curricles, 1975 neat cattle, and 507 horses and mules, over 3 years of age; and paid state tax, $388 85; county tax, $1358 29; and township tax, $500. Spring Garden, or North Belleville, Bloomfield t-ship, Essex co., upon the Third river, and about a mile W. of the Passaic river; contains from 50 to 70 dwellings, a cotton manufactory, a school, and a Methodist church. (See Belleville.) Spring Mills, village of Alexandria t-ship, Hunterdon co., 13 miles N. W. from Flemington, on a small stream, which empties into the Delaware; contains a grist mill, and several dwellings. Springtown, small village ofSchooley's mountain, on the Somerville and Easton turnpike road, 18 miles W. of Morristown, and 3 miles E. of the mineral spring; contains some 6 or 8 dwellings. Spring Valley, hamlet of Morris t-ship, Morris co., 4 miles S. E. of Morristown; contains a tavern, and some half-dozen dwellings. Squan Beach, extends from Old Cranberry inlet, N. 10 miles to Manasquan inlet, dividing for part of that distance, Barnegat bay, from the At lantic ocean. It no where exceeds half a mile in width. Squan, a vicinage in the S. E. part of Howell t-ship, Monmouth co., between Manasquan and Metetecunk rivers. It is much frequented for sea-bathing; and comfortable accommodations are found at the farmhouses, of which there are several where boarders are received. Squankum, p-t. of Howell t-ship, Monmouth co., 10 miles S. E. from Freehold, 44 from Trenton, and 209 N. E. from W. C.; contains a Friends' meeting house, a grist mill, and fulling mill, 2 taverns, 1 store, and 12 or 15 dwellings, surrounded by pine forest, and sandy soil. Squankum, tavern, and creek; the creek is a tributary of Inskeep's branch of the Great Egg Harbour river, Deptford t-ship, Gloucester county. Staford t-ship, Monmouth co., bounded on the N. by Dover t-ship; E. and S. E. by the Atlantic ocean; S. W. by Little Egg Harbour t-ship; and W. by Northampton t-ship, Burlington co. Centrally distant S. from Freehold, 38 miles; greatest length, N. and S. 18 miles, breadth 12 miles; area, 87,000 acres; surface level; soil, sand, gravel, and marsh. On the E. front of the t-ship, Long Beach extends upon the ocean, about 11 miles, with an average breadth of about 1 mile, separating Little Egg Harbour bay from the sea. The bay varies from 2 to 3 miles in width, and between it and the fast land, there is a body of salt marsh of like width, through which flow several creeks; the principal are Manahocking, Gunning, Cedar, and Westecunk. Barnegat, Manahocking, Cedar Bridge, and Westecunk, are villages; the two first post-towns of the t-ship. Population in 1830, 2059. In 1832 the county contained about 400 taxables; 64 householders, whose ratables did not exceed $30; 30 single men; 4 stores, 2 saw mills, 1 grist mill, 1 furnace, 210 horses and mules, and 802 neat cattle, above 3 years of age. STE 243 STI Stanhope, forge, and post-town, on the Musconetcong river, and on the Morris canal, on the S. boundary of Byram t-ship, Sussex co., by the post route, 222 miles from W. C., 59 from Trenton, 11 S. of Newton, and 16 N. W. of Morristown; contains a grist mill, 3 forges, 2 taverns, 2 stores, and from 20 to 30 dwellings, and one large school house. The creek has here been led from its bed, by which means a fine waterfall of 30 feet, available for mill purposes, has been obtained; an inclined plane of the canal at this place, surmounts an elevation of 76 feet. This thriving little town was founded by Mr. Silas Dickenson; and is surrounded by an excellent soil of limestone. Staten Island Sound, or ArthurKill, the strait which divides Staten Island from New Jersey. It has a devious, but general N. E. course, from the head of Raritan bay, and including the Kill-van-Kuhl, extends to New York bay, a distance of about 18 miles, having a breadth, commonly much under, and no where exceeding half a mile. It is the ordinary passage of the steamboats which ply between Brunswick, Amboy, and New York. As the tide flows from, and into both bays, from and into this strait, the navigator never has a current with him through its whole length. The channel is skirted on both sides by an agreeable country. That of New Jersey is the more level, and that of Staten Island the more variegated and picturesque. For several miles from New York bay, the shore of the island is so closely covered with houses, as to have the appearance of a continued street. Steddam's Neck, a strip of land lying in the N. W. angle of Greenwich t-ship, formed by the junction of Newport and Stow creeks. Steelman's Creek, small tributary, flowing eastwardly into the Great Egg Harbour river, Weymouth t-ship, Gloucester co. Stephen's Creek, Weymouth t-ship, Gloucester co., tributary of Great Egg Harbour river, having an easterly course of 8 or 9 miles. Two miles from its mouth, is a village and post-town which bears its name; 39 miles S. E. from Woodbury, 78 from Trenton, and 106 N. E. from W. C. It contains a grist and saw mill, tavern, store, and 6 or 8 dwellings. Stewartsville, p-t. of Greenwich t-ship, Warren co., centrally situate in the t-ship, on Merritt's branch of Pohatcong creek, 10 miles S. E. of Belvidere; contains a tavern, a store, and 10 or 12 dwellings; surrounded by a fertile limestone country, and lying about a mile south of the Morris canal, and about 5 miles east from Easton, Pennsylvania. Still Valley, of Greenwich t-ship, Warren co., lying between Lopatcong and Pohatcong creeks, and extending N. E. from the river Delaware. This is a rich valley of limestone land, thickly settled, and highly productive in wheat. There is a post-office here named after the valley, on the turnpike road, between 4 and 5 miles from Easton, Pennsylvania. Stillwater t-ship, Sussex co., bounded N. E. by Newton t-ship; S. E. by Greene t-ship; S. W. by Hardwick t-ship, Warren co.; and N. W. by Walpack t-ship. Centrally distant from Newton, E. 7 miles; greatest length N. and S. 10 miles; breadth E. and W. 7 miles; area, 28,160 acres; surface hilly, on the N. W. mountainous. It is drained by Paulinskill, which crosses it centrally, and receives a tributary from Swartwout's pond in the t-ship. Population in 1830, 1381. Taxables in 1832, 230. Stillwater and Coursenville are post-offices of the t-ship, which contained, in 1832, 40 householders, whose ratables did not exceed $30, 4 run of stones for grinding grain, 4 stores, 6 saw mills, 277 horses and mules, and 692 neat cattle above three years of age, 1 distillery, 64 tan vats. It paid state and county tax, $378 85; poor tax, $200; road tax, $600. S. E. of the Paulinskill, the soil is slate; N. W. STO 244 STR of the creek, lime, slate, andgrey rock, and is generally fertile. Stillwater, p-t. of the above t-ship, by the post-route, 236 miles from W. C., 78 from Trenton, and 7 S. W. from Newton; contains a tavern, store, a grist and oil mill, a Presbyterian church, formerly Dutch Reformed, and 8 or 10 dwellings. The soil around it is limestone, well cultivated. Stipson's Island, a neck of fast land, near the west boundary of Dennis t-ship, Cape May co., projecting into the marshes, having a length of about 3 miles. Stockholm, post-office and forge of Jefferson t-ship, Morris co., upon the Pequannock creek, at the N. E. end of the Greenpond mountain, 18 miles N. W. of Morristown, 249 N. E. from W. C., and 83 from Trenton. Stockingtown, a small hamlet of 6 or 8 dwellings, of Upper Alloways Creek t-ship, Salem co., about 9 miles E. of Salem t-ship, and 3 from Allowaystown. Stone House Brook, branch of the Pompton river, rising in Pequannock t-ship, and flowing by a course of 6 miles N. W. to its recipient, giving motion to some forges. Stony Brook, Pequannock t-ship, Morris co., small tributary of the Rockaway river, which flows by several branches, in length from 4 to 5 miles, through Rockaway valley. Stony Hill, extends from the north branch of the river Raritan, in Bernard and Bridgewater t-ships, through Warren t-ship, in Somerset co., into Essex co., in the form of a crescent; formed of trap rock, on old red sandstone base. Under this name the mountain, following its curve, is about 12 miles long. Stop-the-Jade Creek, tributary of the S. branch of the Rancocus creek, Northampton t-ship, Burlington co.; unites with the latter at Vincenttown, after a westerly course of 9 miles.A mill stream. Stout's Branch, of Paulin's creek, rises in Sand Pond, Hardwick t-ship, Warren co., at the foot of the Blue mountain, and flows by a southerly course of 7 or 8 miles, to its recipient. Stoutsville, on the line dividing Montgomery t-ship, Somerset co., from Hopewell t-ship, Hunterdon co., and on the turnpike road from Brunswick to Lambertsville, 13 miles S. W. from Somerville; contains a tavern, and 6 or 8 dwellings, in a fertile, pleasant valley. Stow Creek t-ship, Cumberland co., bounded N. and W. by Stow creek, which divides it from Salem co.; E. by Hopewell t-ship, and S. by Greenwich t-ship. Centrally distant, N. W. from Bridgeton, 7 miles; greatest length, E. and W. 7; breadth, N. and S. 6 miles; area, 10,240 acres; surface, partly level, partly rolling; soil, clay, loam, sand, and gravel. Population in 1830, 791. In 1832, the t-ship contained 170 taxables, 21 householders, whose ratables did not exceed $30; 4 grist mills, 1 saw mill, 198 horses and 557 cattle, above the age of 3 years, 1 store; and paid road tax, $200; state and county, $437 81. Newport creek forms the boundary between this and Greenwich t-ship. Stow Creek, rises on the confines of Salem and Cumberland cos., and Hopewell and Upper Alloways Creek t-ships, and by a S. W. and S. course, forms the line between these counties, by the meanders of the creek; 25 miles to the Delaware bay. It is navigable for sloops, about 18 miles, and has some good banked meadow on its borders, for the distance of 9 miles, commencing 9 miles from its mouth. Straw, hamlet of Greenwich t-ship, Warren co., about 5 miles S. E. of Philipsburg, and 12 miles' S. of Belvidere; contains 3 or 4 dwellings only. Stralenberg, hamlet, Hackensack t-ship, Bergen co., about 5 miles N. E. of Hackensacktown; contains 1 Dutch Reformed, and 1 Seceder's church, some 8 or 10 dwellings, a store and tavern; surrounded by a pleasant, level country, of fertile loam, well cultivated. SUS 245 SUS Stretch's Point, on Stow creek, Lower Alloways Creek t-ship, Salem co., about 7 miles from the mouth of the creek. Suckasunny, the name of a village and plain; the latter extending in width from 2i to 3 miles, and in length about 6 miles; is sandy and not very fertile, and is drained by Black, or Lamington river. On the N. E. of this plain, terminates the great vein of iron which has continued a S. W. course from the White Hills in New Hampshire. The village and post-town is situate on the Morristown and Easton turnpike road, 11 miles N. W. from the former, 63 N. E. from Trenton, and 226 from W. C.; contains a Presbyterian church, a store and tavern, and some 12 or 15 dwellings. Sucker Pond, a small basin of water, at the east foot of the Blue mountain, in Stillwater t-ship, Sussex co. Sussex County, was taken from Morris, by act of Assembly, 8th June, 1753, with bounds which included the present county of Warren. Warren was erected by act of 20th Nov. 1824; and Sussex is now bounded S. by the Musconetcong river and Hopatcong pond; thence by a line running N. E. dividing it from Morris and Bergen counties, to the line of the state of New York; thence along that line N. W., to the Delaware river, at the mouth of the Nevisink, or Macacomac river; thence by the river, to the mouth of the Flatkill; and thence by a line S. E., separating it from Warren co., to the Musconetcong river, somewhat more than a mile below Andover furnace. Its form approaches an oblong, with a mean length of 26, and breadth of 22 miles; area, about 572 square miles, or 366,000 acres: central lat. 41O 8' N.; long. 20 15' from W. C. The county is divided geologically by the primitive and transition formations. The former passing N. E. by Sparta, and including within its limits, the Hamburg or Wallkill, and the Wawayanda mountains. These mountains abound with a variety of minerals, of which iron and zinc are the most considerable. The country between these hills and the Blue mountain is rolling; nay, hilly; in which, ridges of slate, alternate with valleys of limestone; and is highly fertile, and every where well cultivated. The Blue, or Kitiatinny mountain, is skirted on the east by grey rock, which bears great resemblance to the primitive, and Certainly contains little evidence of recombination. The mountain itself appears to be composed partly of similar rock, of a bluish green and red sandstone, the colours of which are singularly and intimately blended. Upon the N. W. the mountain is bounded by a broad strip of grey limestone. A dividing ridge running from Blue mountain, in Frankford t-ship, north of Culver's Pond, through the S. E. angle of that t-ship, on towards Sparta, gives a determination to the waters of the county, sending part N. E. towards the Hudson, and part towards the Delaware river. Thus all the waters of the eastern portion pourfrom the hills north and south, into the valley of the Wallkill,- where the flatness of the surface causes them to spread over a considerable space, and occasions an extensive marsh along the borders of that stream, greatly enlarged within the bounds of the state of New York. The western portion of the county is drained chiefly by the Paulinskill, flowing by a deep and rapid course, through this and Warren county, to its recipient near Columbia. The face of the country is dotted with large ponds, or small lakes, some of which are on the highest hills. Swartwout's and Culver's ponds are the largest-the first being 3 miles in length, by 1 in breadth, and the other 2 miles in length, by the same breadth. But the most remarkable are the White Ponds, which have been so called, from the appearance of their shores and bottoms, covered with shells of the snail, in very extensive masses. Two of these lie on SUS 246 SUS the line between Newton and Hardiston townships. The agriculture of the 'county is in a state of progressive improvement, and is now very productive. The limestone lands yield large crops of wheat, and the slate, where the rock does not come too near to the surface, is scarce less fertile. Lime is not yet much employed as manure, but its use is growing, and will doubtlessly be extensive, when its benefits shall be generally known. Wheat, rye, oats, corn, and iron, are staple products. The principal towns and post offices, are Newton, the county town, Deckertown, Hamburg, Ogdensburg, Sparta, Andover, Greenville, Stillwater, Branchville, Augusta, and Lafayette. Benville, Coursenville, Flatbrookville, Fredon, Gratitude, Harmony, Hamburg, Lafayette, Libertyville, Lockwood, Monroe, Montague, Sandystone, Stanhope, Vernon, Walpack, and Wantage.' By returns of the assessors, for the year 1832, there were 1075 householders, 58 merchants, shopkeepers, and traders, 87 run of stones for grinding grain, 18 carding machines, 3 iron furnaces, 55 saw mills, 28 forge fires, 7 fulling mills, 3875 horses and mules, 13,070 neat cattle 3 years old and upwards, 6 ferries and toll bridges, 227 tan vats, 36 distilleries, and 101,887 acres of im proved land. The amount of state and county tax, was $7500 95; poor tax, $3300; road tax, $8600. By the census of 1830, the popu. lation of the county amounted to 20,346 souls, of whom 10,240 were white males; 9654 white females; 206 free coloured males; 195 free coloured females; 21 male, and 30 female slaves. Of these inhabitants, 89 were aliens; 6 deaf and dumb; 14 blind. The provision for moral improvement in the county, consist of 2 classical seminaries at Newton, 6 common schools in that town, and others in sufficient numbers for the wants of the people throughout the county; a Lyceum for the cultivation of letters and science, and a public library at Newton; a county Bible society, a county Sunday school union, and district Sunday schools and temperance societies. The county elects 1 member to the legislative council, and 2 to the Assembly. The courts of common pleas, orphans', and quarter sessions, are holden at Newton, on the last Tuesday of January, the 4th Tuesday of May, the 3d of August1 and the 4th of November; and the circuit courts, and sessions of oyer and terminer and general jail delivery, are holden on the 4th Tuesdays of May, and November. STATISTICAL TABLE OF SUSSEX COUNTY. . Population. Townships. Area. Surface. S( 1810. 1820. 1830. Byram, 10 8 21,760 mountainous. 591 672 958 Frankfort, 11 8j 28,800 valley. 1637 2008 1996 'Green, 9 4 14,080 p't hilly, p't level. 801 Hardiston, 13 9 41,960 mountainous. 170Z 2160 2588 Montague, 8I 77 21,620 moun. & riv. flat. 661 964 990 Newton, 12 10 65,926f hilly, p't level. 2082 2743 3464 Sandistone, 8j 7 19,320 moun. & riv. flat. 703 1945 1097 Stillwater, 10 7 28,160 moun. level. 1381 Walpack, 10 4 15,360 moun. &riv. flat. 591 822 660 Wantage, 11 88 42,880 do. do. 2969 3307 4034 Vernon, 11 10 52,480 mountainous. 1708 2096 2377 352,300 12,644 16,617 20,346 SUS 247 SUS We have already, in our introduc- ing iron ore in a blast furnace with antory chapter, noted generally the thracite coal; as the Franklinite requires S. a greater degree of heat to cause it to regeological and mineralogical charac- tain its liquid state, than can be obtained ter of this county. But the reader by the use of charcoal. It occurs in grains will be gratified with the following imbedded in the white carbonate of lime, special notice from Dr. Samuel Fow- and detached in concretions of various ler, whose intimate knowledge of the sizes, from that of a pin's head to a hickory ler, whose intimate knowledge of the nut; also, in regular octahedral crystals, subject, renders the account highly emarginated on the angles, small at Frankvaluable. lin, but very perfect, with brilliant faces. At Sterling, the crystals are large and Perhaps in no quarter of the globe is perfect. I have one from that place that there so much found to interest the mine- measures sixteen inches around the comralogist, as in the white crystalline cal- mon base. careous valley, commencing at Mounts Red Oxide of Zinc.-At Sterling, three Adam and Eve, in the county of Orange, miles from Franklin, a mountain mass of and state of New York, about three miles this formation presents itself about 200 from the line of the state of New Jersey, feet high. Here, as Mr. Nuttall truly oband continuing thence, through Vernon, serves, the red oxide of zinc forms as it Hamburg, Franklin, Sterling, Sparta and were a paste, in which the crystals of Byram, a distance of about twenty-five Franklinite are thickly imbedded; in fact miles, in the county of Sussex, and state a metalliferous porphyry. This appears to of New Jersey. This limestone is highly be the best adapted for manufacturing crystalline, containing no organic re- purposes. The Franklinite imbedded in mains, and is the great imbedding matrix the zinc ore here, is highly magnetic, and of all the curious and interesting minerals may be all separated by magnetic cylinfound in this valley. When burned, it ders, recently brought into use to separate produces lime of a superior quality. A the earthy portion of magnetic iron ore. considerable quantity of 'this stone is It was long since observed, that this ore burned into lime near Hamburg, and when is well adapted for the manufacture of the carted to the towns below, as Patterson, best brass, and may be employed without Newark, &c. is sold for one dollar per any previous preparation. It is reduced bushel. It is principally used in masonry, without any difficulty to a metallic state, for whitewashing, cornice work, and wall and may be made to furnish the sulphate of a fine hard finish, and is considered su- of zinc (white vitriol). perior to the best Rhode Island lime. It is remarked by Professor Bull," that Some varieties, particularly the granular, this ore, from its abundance, and the many furnish a beautiful marble; it is often uses to which it may be applied, promises white, with a slight tinge of yellow, re- to be a valuable acquisition to the manusembling the Parian marble from the facturing interest of the United States." island of Paros; at other times clouded, Berthier found it to contain oxide of zinc black, sometimes veined, black, and at 88, red oxide of manganese 12. other times arborescent..Magnetic Iron Ore. On the west side Franklinite; a new metalliferous combi- of the Franklinite, and often within a few nation, containing, according to Berthier, feet of it, appears an abundance of magof oxide of zinc 17, of iron 66, and man- netic iron ore, usually accompanied by ganese 16, is very abundant; indeed it hornblende rock. In some places it soon appears inexhaustible. It commences runs into the Franklinite, which destroys about half a mile north-east of Franklin its usefulness; and the largest beds are furnace, and extends two miles south- combined with plumbago, which renders west of Sparta, a distance of nine miles. it unprofitable to work in a blooming It is accompanied in this whole distance forge, but valuable in a blast furnace. by the red oxide of zinc, mutually enve- On the Franklin or Warwick mountain, loping each other. The greatest quantity about four miles east of the furnace, are appears to be at Franklin furnace. The numerous beds of iron ore, from which bed here, is about 100 feet high above the many thousand tons have been taken; adjoining land, on the west side of it, and and which still contain a large quantity from ten to forty feet wide. Various at- of-the best quality of ore, either for a tempts have been made to work this ore in blooming forge or blast furnace. Iron a blast furnace, but without success. It pyrites occur here, both in the valley and frequently congeals in the hearth, before on the mountain, of a proper quality to time is allowed to get it out in a liquid manufacture sulphate of iron-(copperas.) state, in consequence of a combination of It also occurs crystallized, in cubes, in the iron with manganese. All this dif- octahedrons, and dodecahedrons, freficulty I apprehend might be overcome, quently perfect, and highly splendid. if a method could be discovered of smelt- The other minerals found in this dis SUS 248 SUS trict are numerous, rare, interesting, and several of them new, and not found in any other place, but better calculated to instruct the naturalist and adorn his cabinet, than for any particular uses to which they have as yet been applied. A catalogue of which I have subjoined, designating the minerals as they occur in each township. In Byram t-ship, considered the south western extremity of the white carbonate of lime. 1. Spinelle, colour reddish brown, green, and black, in octahedral crystals, associated with orange coloured brucite. 2. Brucite of various shades, from that of a straw colour, to a dark orange, and nearly black. 3. Grey hornblende in six-sided prisms, with diedral summits. In the Township of Hardiston. At Sparta: 1. Bracite of a beautiful honey colourthe finest we have is found here. 2. Augite in six-sided prisms, colour brownish green. At Sterling: 1. Spinelle, black, green, and grey, in octahedral crystals. 2. Brucite of various shades. 3. Brutile, colour steel grey; lustre metallic, in acicular prisms, with longitudinal striad. 4. Blendej black and white; the white sometimes in octahedral crystals, the lustre brilliant. 5. Dysluite, in octahedral crystals, colour brown externally, internally yellowish brown; lustre metallic-(a new mineral.) 6. Ferruginous silicate of manganese, in six-sided prisms, colour pale yellow, associated with Franklinite. 7. Tourmaline, imbedded in white feldspar, in six-sided prisms, longitudinally striated; colour reddish brown. 8. Green and blue carbonate of copper. A number of large excavations were made at the Sterling mine for copper, during the revolutionary war, under an erroneous impression, that the red oxide of zinc, was the red copper ore. It was the property of Lord Sterling; hence the name of the Sterling mine. Of copper, we only find there a trace of the green and blue carbonate. At Franklin: 1. Spinelle, black and red crystallized. 2. Ceylonite, green and bluish green, in perfect octahedrons truncated on the angles; lustre of the brilliance of polished steel. 5. Garnets, black, brown, yellow, red, and green-crystallized in dodecahedrons. 6. Silicate of Manganese, light brownish red. 7. Ferro Silicate of Manganese, of Professor Thomson, and the Fowlerite, of Nuttall, light red or. pink, foliated and splendent, has much the appearance of Feldspar, is also in rectangular prisms. 8. Lesqui-Silicate of Manganese, lamellar in scales or small plates; colour, brownish black. 9. Hornblende, crystallized. 10. Actynolite, do. 11. Tremolite, do. 12. Augite, common variety, do. 13. Jeffersonite, do. do. 14. Plumbago, foliated and crystallized in six-sided balls. 15. Brucite of various shades. 16. Scapolite, white, crystallized. 17. Wernerite, yellowv, do. 18. Tourmaline, black, do. 19. Fluate of Lime, earthy and do. 20. Galena. 21. Oolite, in small grains about the size of a mustard seed, disseminated in blue secondary carbonate of lime. 22. Asbestos, connected with Hornblende rock. 23. Green Beryl. 24. Feldspar, green and white, crystallized. 25. Epidote and Pink Carbonate of Lime. 26. Arsenical Pyrites. 27. Serpentine. 28. Sahlite. 29. Cocolite, green and black. 30. Sphene, honey colour, crystallized. 31. Quartz. 32. Jasper, 33. Chalcedony. 34. Amethyst, crystallized. 35. Agate. 36. Mica, black and orange coloured, crystallized. 37. Zircon, crystallized. 38. Sulphate of Molybdena. 39. Phosphate of Iron. 40. Carbonate of Iron. 41. Steatite, foliated with yellow Garnet. 42. Phosphate of Lime, crystallized. 43. Pale Yellow-blende, of a foliated structure-lustre, vitreous. Near Hamburgh. 1. An pre of Manganese, and iron of a light reddish brown, very compact and heavy. 2. Augite and Brucite. In the Township of Vernon. 1. Green Spinelle and Brucite, in octahedral crystals. In Newton Township. 1. Sulphate of Barytes in lamellar masses, and tabular crystals, in a vein traversing secondary limestone. 2. Sapphire, blue and white, in rhombs and six-sided prisms. 3. Red Oxide of Titanium. TAN 249 TIM 4. Grey Spinelle in large octahedral crystals. 5. Mica, copper coloured, in hexahedrfl crystals. 6. Idocrase, crystallized, yellowish brown. 7. Steatite, presenting the pseudomorphous form of quartz, scapolite, and spinelle. 8. Scapolite, in four-sided prisms. For a more particular account of the Newton minerals, see Silliman's Journal, vol. XXI. page 319. In Frankford Township. Serpentine, of a light yellowish green, bears a fine polish, has a glistening lustre, and is quite abundant. Swartwout's Pond, a large sheet of water, of Stillwater t-ship, Sussex co., which sends forth a tributary to Paulinskill. Swedesboro', p-t. of Woolwich t-ship, Gloucester co., 13 miles S. W. from Woodbury, 49 miles from Trenton, and 155 from W. C., at the head of sloop navigation, on Raccoon creek, about 5 miles from its mouth; contains about 100 dwellings, an Episcopal and a Methodist church, an academy, 2 taverns, 4 stores, a merchant grist mill, and an extensive woollen factory, belonging to C. C. Stratton, Esq. The country around it is level; soil, sandy loam, fertile, and well cultivated. Battentown, a mile distant from it, contains 1 tavern, and a few dwellings. Swede's Branch, mill stream of Chester t-ship, Burlington co., flows by a N. W. course of more than 3 miles, to the Delaware river. Swimming River. (See Shrewsbury river.) Tabernacle, village of Northampton t-ship, Burlington co., 12 miles S. W. of Mount Holly; contains a Methodist church, a tavern, and 10 or 12 houses. Talman's Creek, small tributary of the Rancocus creek, rising in Evesham t-ship, Burlington co., near Evesham village, and flows six miles to its recipient. Tansboro', village of Gloucester t-ship, of Gloucester co., on the road from Long-a-coming, to Great Egg Harbour river, 15 miles S. E. from 21 Woodbury, 18 from Camden; contains a tavern, and some half dozen dwellings. Surrounded by a sandy soil, and pine forest. Tarkiln Creek, mill stream of Maurice River t-ship, Cumberland co., rising in the t-ship, and flowing by a southerly course, of 10 miles into the Delaware bay. Taunton Furnace, on Haines' creek, Evesham t-ship, Burlington co., 11 miles S. W. from Mount HolP ly, and 14 S. E. from Camden. Tenants' Run, a tributary of South river, South Amboy t-ship, Middlesex co., flowing N. W., between 3 and 4 miles to its recipient. Tewkesbury, t-ship, Hunterdon co., bounded N. by Washington t-ship, Morris co.; E. by Bedminster t-ship, Somerset co.; S. by Readington t-ship, and W. and S. W. by Lebanon t-ship; centrally distant N. E. from Flemington, 14 miles; greatest length, N. and S., 8; breadth, E. and W. 61 miles; area, 23,000 acres; surface hilly; soil, on the mountain, clay and loam, and in the valley, at its foot, grey limestone, rich and well cultivated; drained by Rockaway creek, and its tributaries, flowing S. E. through the township, and by Lamington river, which runs on the eastern boundary. New Germantown, and Pottersville, are post-towns of the t-ship. Population in 1830, 1659. In 1832 the t-ship contained 8 stores, 6 saw mills, 3 grist mills, 28 tanner's vats, 2 carding machines, 2 fulling mills, 9 distilleries, 417 horses and mules, 696 neat cattle, above 3 years of age; and paid poor tax, $350; road tax, $600; state and county tax, $706 68. Tice's Pond, at the foot of the Ramapo mountain, Pompton t-ship, Bergen co.; covers about 200 acres of ground, and is the source of a tributary of Ringwood river. Timber Creek, Big, Gloucester co., rises by two branches, the lesser in Gloucester, and the greater in Deptford t-ship, uniting about 6 miles above the mouth. The north branch is navigable for sloops from the De TOM 250 TRE laware to Chew's landing, a distance of 8 or 9 miles, and the south, nearly to Blaikwoodtown, a distance of about 10 miles. The whole length of the stream, by its meanders, may be 13 or 14 miles. It receives several small tributaries in its course, and drives some valuable mills. Timber Creek, Little, of Woolwich t-ship, Gloucester co., rises in the t-ship, and flows N. W. 7 or 8 miles, to the Delaware river, below Chester Island. There is a mill upon it, near its head. Tinton Falls, village, and mill site of Shrewsbury t-ship, Monmouth co., upon a branch of the Nevisink river, 9 miles E. from Freehold; contains from 15 to 20 dwellings, a grist and saw mill, 1 tavern, and 2 stores. The water of the S. E. branch of Swimming river, falls over a sand rock, filled with animal remains, and forming a cascade of about 30 feet high. From this rock flows a copious chalybeate spring, which is frequently visited by those who seek health or amusement at the boarding houses near the coast. Titusville, post-office, Hunterdon county. Toms' River, p-t., of Dover t-ship, Monmouth co., upon the head of Toms' River bay, and tide water, 25 miles S. E. from Freehold, 221 from W. City, and 69 from Trenton, and 6 from the confluence of the river with Barnegat bay; a flourishing village, lying on both sides of the creek, united by a wooden bridge, of near 200 feet in length; contains from 50 to 60 frame dwellings, some of which are very neat and commodious; 2 taverns, 5 or 6 stores, and a Methodist meeting. Many sloops and schooners are built here, and more than $200,000 worth of timber and cord-wood, annually exported. Toms' River, mill stream of Monmouth co.; its main branch rises on the line dividing Freehold and Upper Freehold t-ships, and near Paint Island spring; and flows thence by a S. E. and E. course of 30 miles, into Barnegat bay. Above the village of Toms' river, about 4 miles, it receives the south branch, which is formed by many streams from Dover and Upper Fieehold t-ships; and about a mile above the village, Wrangle Brook also unites with it. It drains a wide expanse of forest land, and by the main stream and branches turns many mills and iron works. Townsbury, post-office, Warren county. Tranquility, small tributary of the west branch of Wading river, rises and flows about 4 miles in the neck of land, between the east and west branches of the river. Trap, hamlet of Shrewsbury t-ship, Monmouth co., near Shark river, 11 miles S. E. from Freehold; containing 6 or 8 dwellings, surrounded by a sandy soil and pine forest. Trenton t-ship, Hunterdon co., bounded N. by Hopewell, E. by Lawrence t-ships; S. E. by Nottingham t-ship, of Burlington co.; and S. W. and W. by the river Delaware. Greatest length N. W. and S. E. 8 miles; breadth E. and W. 6 miles; area, 10,609 acres; surface, level; soil, clay and red shale, generally well cultivated, and productive. It is drained by Jacob's creek on the north, and by the Assunpink and its tributaries, on the south. The town of Birmingham, and the city of Trenton, are within its boundary. Population in 1830, 3925. In 1832, there were in the t-ship 11 merchants, 3 fisheries, 2 saw mills, 3 grist mills, 2 ferries and bridges, 220 tan vats, 2 grain distilleries, 469 horses and mules, and 590 neat cattle, above 3 years old; and it paid poor tax, $900; road tax, $400; and county tax, $1264 98. (See Trenton City.) Trenton, city, and seat of government of the state, on the left bank of the Delaware river, three-fourths of a mile above the tide, opposite the lower falls of the river, and* on the north side of the Assunpink creek, Trenton t-ship, Hunterdon co., 30 miles from Philadelphia, 58 from New York; lat. 40~ 13' 41" N.; long. 0~ 21' 15" E. of Philadelphia, TRE 251 TRE and' 20 8' 15" of Washington City. Incorporated by the act of 13th November, 1792, which established its government under a mayor, recorder, 3 aldermen, and 13 assistants, with the usual city privileges, and power to license taverns within the city; and by the act of 3d January, 1817, the mayor, recorder, and aldermen, or any three of them, of whom the mayor and recorder must be one, are empowered to hold a court of general quarter sessions. There are here, a state house, 100 by 60 feet, with bow at either end, cupola, and bell; the building is of stone, stuccoed in imitation of dark granite, and beautifully situated on the bank of the river, commanding a fine view of the stream, the airy bridge which has been thrown over it, and of the undulating shore of Pennsylvania: a house for the residence of the governor of the state; 3 fire-proof offices, a bank incorporated in 1804, with an authorized capital of $600,000, of which $214,740 only have been paid in; an academy in which the languages are taught, 3 boarding and day schools for females, and several common schools. These are, however, in the city proper; but Trenton, as known in common parlance, including the villages of Mill Hill, Bloomsbury, and Lamberton, extending li1 miles down the river bank, has an Episcopal, Presbyterian, Friends', Baptist, Reformed Baptist, Roman Catholic, Methodist, and African Methodist churches. Trenton proper contains 425 dwellings, 13 taverns, about 30 stores, among which are 3 bookstores, and 3 silversmith shops; 3 printing offices, each of which issues a weekly paper, viz. the Union, the True American, and the New Jersey Gazetteer; a public library, established about the year 1750, and a lyceum or literary association. Mill Hill has 78 dwellings, 4 stores, and 4 taverns. Bloomsbury, 145 dwellings, 2 stores, and 5 taverns; and Lamberton, 64 dwellings, 2 stores, and 2 taverns. The Philadelphia steam-boats ply daily, and sometimes several times a day,,one from Lamberton, and others from Bloomsbury; and stages run 3 times a day by the rail-road to New York and Philadelphia. Stages also run hence by Princeton to Brunswick, and to various other parts of the country The Delaware and Raritan canal re ceives its feeder here, on which is an extensive basin for vessels and boats, and the main canal crosses the Assunpink east of the town, over a noble stone aqueduct. The state prison is at Lamberton, where a new prison is also being erected, adapted to the confinement of 150 convicts. The famed bridge over the Delaware, is thrown from Bloomsbury to Morrisville, a span of 1100 feet, having a double carriage-way and foot-paths resting on the chords of, and suspended from, a series of five arches, sup. ported on stone piers. This structure has been much admired for its lightness, grace, and strength. There are on the Assunpink, within the town, two cotton mills, having 5400 spindles, and one mill for power looms, and on the Delaware, two mills for looms; the whole number of looms exceed 200. For some years past Trenton has not been in a very thriving state, but the late improvements have given new life to business and enterprise, and much prosperity is anticipated from the completion of the canal, and particularly from the construction of the mill race, now being made by the Trenton Falls Company. This company was incorporated by an act of the legislature, 16th Feb. 1831, with power to purchase, lease, or sell lands, mills, and water privileges useful in the creation of water power; to cut a wing dam in the Delaware river, between the mouth of the Assunpink and the head of Wells' Falls, and a race-way along the bank, not extending more than one and a half miles below the Trenton Falls; to make lateral race-ways and other works; to sell lots, sites, and privileges under the charter; and with a general power of taking lands neces. TRE 252 TRE sary for their purposes, at the appraisement of the commissioners; and with the customary powers granted to other corporations. Their charter is perpetual, protecting the company from any tax exceeding the half of one per cent. on the actual amount of capital expended in the construction of the work, with the privilege of extending its capital to $200,000. Each share, in the election of managers, is entitled to one vote. The capital subscribed is $90,000; the cost of constructing the work is estimated at $140,000 exclusive of the lands purchased by the company for mill sites and building lots. The canal and race-way commences at the head of Scudder's Falls, directly opposite the upper end of Slack's Island, and continues down the margin of the river, to a point opposite the centre of White's Island, where, leaving the bank, it enters upon the meadows bordering the river, through which it passes to the Assunpink, in Trenton; thence, it is designed to cross this creek by an aqueduct, and to pass through Bloomsbury, to the precincts of Lamberton, where it debouches into the river. The fall in the river Delaware, between the head and foot of the raceway is 20 feet, of which, one foot and a half descent is given to the raceway, leaving a head and fall at the Assunpink of 14 feet, and below the foot of the Trenton Falls 18~ feet. The entire column of the water descending the race-way is estimated at 23,868 cubic feet per minute, at the lowest known state of the water.This at the Assunpink, will afford a power equal to 335 horses; or if all be expended below the Assunpink, equal to 575 horses: or should one-third of the water be used above, and twothirds below the creek, the power above will be equal.to 145 horses, and that below, to 384 horses. This calculation is based on a depth of six feet water only, in the race-way; the minimum supply, after all deductions for leakage and evaporation at the lowest water. This, however, is the view of the power, in what is deemed its first stage. The work commences at the upper end of Slack's Island, which is of considerable extent, situate near the middle of the river. The main channel of the stream was formerly on the right, or Pennsylvania side of the island, but a loose stone wall having, some years since, been thrown across this channel to improve the navigation of the river, the larger portion of the water was thrown into the Jersey channel. This wall remains, but it is overflowed at the lowest water. By raising this dam and throwing the whole current of the river into this channel, or by entirely removing it, and erecting a dam from the head of the company's works to Slack's Island, and reopening the channel on the other side, the water in the raceway would be raised two feet beyond its present elevation; and in constructing their work, the company have adapted it to the reception of that body of water. A column of eight feet instead of six, would thus be gained in the race; the velocity of its current increased to 122 feet per minute, and the quantity of water to 52,704 cubic feet in the same time. The power of the water would then be equal to 960 horses at the Assunpink, or 1260 below it: or should one-third of the power be employed above, and two-thirds below the creek, it would afford the company a power above, equal to 330 horses, below, 840, in the whole 1170. The company propose to let their lands for the erection of mills, above the Assunpink, at 30 cents, and below the creek, at from 40 to 50 cents the foot, perpetual rent, according to situation; with the right of the free use of the company's wharf, rail-road, &c.: and their lands for dwellings, in lots 20 by 75 feet, at $6 per annum. The buildings, in all cases, to be fire proof. And they propose to let the water from the main race-way for mill power, at a perpetual rent of three dollars above, and four dollars below the Assunpink creek, for TRE 253 TRE every square inch area of the aperture, through which it shall be drawn off by a flume, the plan of which is in the office of the company. The aperture to be measured and made according to the standard measure, also kept by the company, and similar to that in the office of the Secretary of State, at Washington, and according to other regulations published by the company. The advantages of this site for manufacturing purposes are perhaps unsurpassed by any in the country. Intermediately situated between the great markets of Philadelphia and New York, 30 miles from the former, and 60 from the latter--surrounded by a rich agricultural country, producing a large surplus quantity of grain of every description, and capable of quadrupling its productions-upon a river, navigable to the ocean,and for near 250 miles above the falls, flowing through a wide and fertile country, whose products may find a ready market here; having also the feeder of the Delaware and Raritan canal, connecting with the main canal in the heart of the city plot, whilst the canal itself unites with the Delaware, below the bar at Bordentown, and passing through Trenton, along the Millstone and Raritan rivers, to New Brunswick, affords a fine sloop navigation, and all the advantages of cheap and rapid water transportation from and to Philadelphia and New York:-the facility of obtaining an abundant and cheap supply of anthracite coal by the river and the Pennsylvania canal, on the opposite bank:-the rail-roads made, and in progress towards New York and Philadelphia, of which, there are two leading to the latter, one on each side of the river; that on the west running directly from the city, and that on the east from Bordentown, combine all that the manufacturer can require:-a healthy country, abundant and cheap provisions, an adequate supply of labourers, convenience in obtaining raw materials, unfailing power for its manipulation, and a chance of, and rea dy access to, the best markets of the country. The following is a description of Trenton, in 1748, as given by the Swedish traveller Kalm-which the citizen will delight to compare with its present condition: " Trenton is a long, narrow town, situate at some distance from the river Delaware, on a sandy plain. It is reckoned 30 miles from Philadelphia. It has two small churches, one for the people belonging to the Church of England, the other for the Presbyterians. The houses are partly built of stone, though most of them are made of wood or planks, commonly two stories high, together with a cellar below the building, and a kitchen under ground, close to the cellar. The houses stand at a moderate distance from one another. They are commonly built so that the street passes along one side of the houses, while gardens of different dimensions bound the other side; in each garden is a draw-well; the place is reckoned very healthy. Our landlord told us that 22 years ago, when he first settled here, (1726) there was hardly more than one house: but from that time, Trenton has increased so much, that there are at present near an hundred houses. The houses were within, divided into several rooms by their partitions of boards. The inhabitants of the place carried on a small trade with the goods which they got from Philadelphia; but their chief gain consisted in the arrival of the numerous travellers between that city and New York; for they are commonly brought by the Trenton yachts from Philadelphia to Trenton, or from thence to Philadelphia. But from Trenton, further to New Brunswick, the travellers go in wagons, which set out every day for that place. Several of the inhabitants also subsist on the carriage of all sorts of goods, which are sent in great quantities, either from Philadelphia to New York, or from thence to the former place-- for between Philadelphia and Trenton, all goods go by water; but be TUC 254 TUR tween Trenton and New Brunswick, Cape May co. Its course, for about they are all carried by land, and both 11 miles, is S., thence due E. for these conveniences belong to people about 12 miles; emptying into Great of this town. For the yachts which Egg Harbour bay. It is a fine mill go between this place and the capital stream, driving several mills, at Marof Pennsylvania, they usually pay a shallville, Etna, and other higher shilling and sixpence, Pennsylvania points, and is navigable for sloops, currency, per person, and every one above the village of Tuckahoe, more pays beside for his baggage. Every than 10 miles from the ocean. passenger must provide meat and Tuckahoe, p-t. on both sides of the drink for himself, and pay some set- Tuckahoe river, over which there is tied fare. Between Trenton and New a bridge, 10 miles above the sea, 46 Brunswick, a person pays 2s. 6d., and miles S. E. from Woodbury, and by the baggage is likewise paid for sepa- post-route 192 from Washington; rately." contains some 20 dwellings, 3 taThe town was founded a few years verns, several stores. It is a place prior to 1720, by William Trent, an of considerable trade in wood, lumenterprising trader, who was distin. ber, and ship building. The land guished for public spirit, and private immediately on the river is good, but character, in the provinces of Penn- a short distance from it, is swampy sylvania and New Jersey. He was and low. at one time, Speaker of the Assembly Tuckerton, p-t, and port of entry, of the former, and at another, Speak- for Little Egg Harbour district, about er of the Assembly of the latter, pro- 35 miles S. E. of Mount Holly, 65 vince. The site of Trenton, before from Trenton, and 189 N. E. from it bore his name, was significantly W. C.; situate on a narrow tongue called Littleworth. Mr. Trent died of land, projecting into the marsh on on the 29th December, 1724. Little Egg Harbour bay, Little Egg Trowbridge Mountain, a long and Harbour t-ship, Burlington co.; conirregularly shaped hill, of Morris co., tains between 30 and 40 dwellings, extending from the N. branch of the 4 taverns, 5' stores, 2 Methodist Raritan, through;Mendham, Ran- churches, a Quaker meeting house. dolph, and Hanover t-ships, to the It lies upon a navigable stream, callRockaway river, ranging S. W. and ed Shord's Mill Branch, 6 miles from N,. E. It is of granitic formation; the bay, whence wood scows and many parts of it in cultivation, but flats ascend to the town. There is a generally sterile, large business done here in timber Troy, hamlet of Hanover t-ship, and cord-wood; and salt is, or was Morris co., on the Parcipany river, manufactured in the vicinity. The about 7 miles N. E. of Morristown; town is frequented during the sumcontains a forge, 1 grist mill, a saw mer season, by many persons for the mill, and 12 or 15 dwellings. Soil, benefits of sea-bathing, &c. A stage sandy loam. plies regularly between it and PhilaTubmill, branch of Wading river, delphia. rises in the west plains of Little Egg Tulipehaukin Creek, tributary of Harbour t-ship, Burlington co., and the west branch of Wading river, flows S. W. 7 miles to its recipient, rises in, and has its whole course of about a mile below Bridgeport. about 8 miles, through Washington Tuckahoe Creek, rises on the line t-ship, Burlington co. between Weymouth t-ship, Glouces- Turpentine, hamlet of Northampter co., and Maurice river t-ship, ton t-ship, Burlington co., on the road Cumberlarid co., and forms, in part, from Mount Holly to Freehold, about the western boundary of the former a mile east from the former; contains co., and also, its southern boundary, a tavern, a store, and some 8 or 10 separating it in the latter case, from dwellings. UPP 255& VAU Turtle Gut Inlet, Lower t-ship, Cape May co., between Five Mile and Two Mile Beach. Tuscomusco Creek, a small tributary of the Atsion river, Evesham t-ship, Burlington co. Two Mile Beach, on the Atlantic ocean, Lower t-ship, Cape May co., between Turtle Gut and Cold Spring Inlet. Union Cross Roads, hamlet of Deptford t-ship, Gloucester co., 4 miles S. E. of Woodbury; contains 3 or 4 dwellings. Union t-ship, Essex co., bounded N. by Orange and Newark t-ships; E. by Elizabethtown t-ship; S. by Rahway, and W. by Westfield and Springfield t-ships. Centrally distant from Newark S. W. 6 miles: greatest length N. and S. 5~, breadth E. and W. 5 miles; area, 12,000 acres; surface, rolling; soil, red shale, well cultivated; watered by Elizabeth river on the east, and Rahway river on the west. Population in 1830, 1405.In 1832 the t-ship contained 350 taxables, 56 householders, whose ratables did not exceed $30 in value; 40 single men, 2 stores, 7 saw mills, 1 woollen factory, 21 tan vats; and paid state tax, $179 65; county, 470 04; poor, $300. There is a fine body of turf here, upon the south branch of Elizabeth river. Union or " Connecticut Farms," is the post-town of the preceding t-ship, situated on the road from Eli. zabethtown to Morristown, 4 miles N. W. of the former, 5 miles S. E. from Newark, 213 N. E. from W. C., and 47 from Trenton; contains a Presbyterian church, and within a half a mile of it, 3 taverns, a store, and about 30 dwellings. Up-Clearing Creek, a small tributary of Cohansey creek, which flows westerly into it, from Hopewell t-sp, Cumberland co. Upper t-ship, Cape May co., bounded N. by Tuckahoe creek, which divides it from Weymouth t-ship, Gloucester co.; E. and S. E. by the Atlantic ocean; S. W. by.Dennis t-sp; and N. W. by Maurice river t-ship, Cumberland co. Centrally distant from Cape May court-house N. E. 13 miles: greatest length N. E. and S. W. 12 miles; breadth S. E. and N. W. 111 miles; area, 37,000 acres; surface, flat; soil, sand and clay; timber, generally oak and cedar. Population in 1830, 1067. In 1832 there were in the t-ship about 200 taxables, 173 householders, whose ratables did not exceed $30; 1 grist mill, 6 saw mills, 6 stores, 140 horses, and 560 cattle above the age of three years. There are 1 Baptist and 1 Episcopalian church, here. The t-ship paid for t-ship expenses, $77 38; county, $466 65; state tax, $150 73. It is drained by Tuckahoe river and Cedar Swamp creek. The last flows N. E. from the S. W. boundary of the t-ship, through an extensive cedar swamp into the river. On the Atlantic front is Ludlam's and Peck's Beaches, having a width of near half a mile, between which the tide flows into several marsh canals and small lagunes. The marsh may have an average width of about two miles. Tuckahoe village lies on the Tuckahoe river, partly in this, and partly in Gloucester co., having a post-office in the latter. Marshallville lies on the line between Cumberland and Cape May counties, but in the former. Vancamp Brook, rises from two ponds at the west foot of the Blue mountain, Walpack t-ship, Sussex co., and by a S. W. course of about 8 miles empties into the Delaware river, in Pahaquarry t-ship. Vansickles, tavern, store, and postoffice, of Bethlehem t-ship, Hunterdon co., on the S. E. foot of the Musconetcong mountain, 10 miles N. W. from Flemington, 36 from Trenton, and 195 from W. C. Varmintown, hamlet of Upper Freehold t-ship, Monmouth co., 6 miles S. E. of Allentown, and 16 S. W. of Freehold; contains a wheelwright and smith shop, and 2 or 3 cottages, in a fertile country of sandy loam. Vauxhall, small hamlet of Spring VIE 256 WAL field t-ship, Essex co., 7 miles W. from Newark, and 21 N. from Springfield. Vealtown, in a vale of Mine mountain, on Mine Brook, Bernard t-ship, Somerset co., 11 miles N. of Somerville; contains a mill and some half dozen dwellings. Vernon t-ship, Sussex co., bounded N. by the state of New York; E. by Pompton t-ship, Bergen co.; S. by Hardiston t-ship; and W. by Wantage t-ship, from which it is separated by the Wallkill river. Greatest length 11, breadth 10 miles; area, 52,480 acres. The whole surface of the t-ship is covered by mountains; the Wallkill and Wawayanda mountains being on the south and east, and the Pochuck mountain on the west. It is drained north by Warwick creek and its tributaries, Black creek and Double Pond creek; south by Pacak creek, a tributary of the Pequannock, and by some small tributaries of the Wallkill river. Population in 1830, 2377; taxables in 1832, 382. There were in the t-ship in 1832, 158 householders, whose ratables did not exceed $30; 2 storekeepers, 5 pairs stones for grinding grain, 1 carding machine, 1 furnace, 3 forges, 8 mill saws, 1 fulling mill, 311 horses and mules, and 1650 neat cattle, 3 years old and upwards, and 6 distilleries. The t-ship paid for school tax, $116; state and county tax, $921 10; poor tax, $300; and road tax, $1200. Hamburg and Vernon are villages and post-towns of this t-ship. The mountains, which on the east, rise to the height of 1000 feet, are composed of primitive rock, in which hornblende is a principal constituent; the valleys are uniformly of' primitive limestone. The mountains yield iron abundantly. Vernon, p-t. of the above named t-ship, lying in the valley between the Wawayanda and Pochuck mountains, 246 miles N. E. from W. C., 88 from Trenton, and 18 from Newton. It contains a tavern, store, and from 10 to 12 dellings. Vienna, p-t. of Independence t-ship, Warren co., on the Pequest creek, near the S. W. boundary of the t-sp, by the post-road 220 miles from W. C., 54 from Trenton, and 12 from Belvidere, upon the verge of the Great Meadows; contains a Presbyterian church, a store, tavern, and 6 or 8 dwellings. Vincenttown, p-t. of Northampton t-ship, Burlington co., at the junction of Stop-the-Jade creek with the south branch of the Rancocus creek,'5 miles S. of Mount Holly, 12 miles S. E. from Burlington, 32 from Trenton, and 159 N. E. from W. C.; contains a grist mill, saw mill, 2 taverns, 4 stores, from 30 to 40 dwellings, a Quaker meeting house, and a house of public worship, free to all denominations; surrounded by a fine fertile country. Wading River, a considerable arm of Little Egg Harbour river, which rises by two branches; the east in Dover t-ship, Monmouth co., and flows S. W. 15 miles, into Washington township; the west in Northampton t-ship, and flows S. W. about 15 miles, td unite with the east, near Bodine's tavern. The main stem flows by a south course, thence of 8 miles to the Little Egg Harbour river, below Swan's Bay. Waertown, hamlet of Stafford t-sp, Monmouth co., upon Barnegat bay, near the mouth of Waertown creek, a small mill stream, of about 3 miles long, 35 miles S. E. from Freehold, and opposite to Barnegat Inlet; contains 10 or 12 dwellings, a tavern and store; in a sandy soil, covered with pine forest. Wallkill Mountains. (See Hamburg.) Wallkill River, rises in Byram t-ship, Sussex co., and flows by a N. E. course of 23 or 24 miles, through Hardiston t-ship, dividing Wantage from Vernon t-ship, into the state of New York, and thence by a like course of 35 or 40 miles, through Orange and Ulster counties, falls into the Hudson river, 3 miles S. E. from the village of Esopus or Kingston. This stream is remarkable for being WAN 257 WAR the drain of a large and valuable tract of marsh meadow land, exceeding 50,000 acres, elevated more than 325 feet above tide water. The waters which descend from the surrounding hills, being slowly discharged from the river, cover these vast meadows every winter, and would render them extremely fertile, could they be effectually drained. Walnut Valley, post-office, Warren co..I Walpack it-ship, of Sussex co., bounded N. E. by Sandistone t-ship; S. E. by the Blue mountain, which separates it from Stillwater t-ship; S. W. by Pahaquarry t-ship; and W. by the river- Delaware. Greatest length 10 miles; breadth 4 miles; area, 15,360 acres; surface on the east, mountainous; on the west, river alluvion. Population in 1830, 660; taxables 137. There were in the t-ship in 1832, 24 householders whose ratables did not exceed $30; 1 storekeeper, 2 saw mills, 146 horses and mules, 3 years old and upwards; 354 neat cattle of like age; 14 tan vats. It paid state and county tax, $293 80; and road tax, $350. It is drained by the Flatkill, which runs centrally through the t-ship, and empties into the Delaware at the Walpack Bend; and by Vancamp Brook, which rises in Long Pond, in the Blue mountain. There is a postoffice here, called after the t-ship, distant from Washington 240, from Trenton 82, and from Newton 12 miles. The Blue mountain covers nearly half the t-ship; between its base and the river is a margin, of an average width of two miles, of limestone, bordered and partly covered by alluvion, rich and highly productive of wheat, corn, &c. There is a German Reformed church in the t-ship. Walpack Bend, a remarkable bind of the river Delaware, at the S. W. angle of Walpack t-ship, about 85 miles above the city of Trenton. Wantage t-ship, of Sussex co., bounded N. by the state of New York; E. by Vernon t-ship; S. by 2K Frankford and Hardiston t-ships; and W. by the Blue mountain, which separates this from Sandistone and Montague t-ships. Greatest length 11 miles; breadth 8' miles; area, 42,880 acres; surface on the west, mountainous and hilly; on the east, rolling. Population in 1830, 4034; taxables 643.,There were in the t-ship in 1832, 208 householders, 11 storekeepers or traders, 18 pairs of stones for grinding grain, 6 saw mills, 1 fulling mill, 5 carding machines, 939 horses and mules, and 3481 neat cattle, over 3 years of age; 18 tan vats, and 3 distilleries. The t-ship paid a school tax of $500; state and county tax, $1706 27; poor tax, $300; and road tax, $1500. It is drained.by Deep Clove river and Papakating creek, uniting south of Deckertown, and thence flowing into the Wallkill river, which forms the whole eastern boundary of the t-ship. The Paterson and Hamburg turnpike road runs N. E., and the Newton and Bolton N. W., through the t-ship; and at their intersection, is the small village of Deckertown. There is a post-office at Deckertown, 444 miles from W. C., 86 from Trenton, and 16 from Newton; and another called Libertyville, 241 miles from W. C., 83 from Trenton, and 10 from Newton. Wantage is a rich t-ship, consisting of limestone and slate soils; the one on the east, and the other on its western side, highly cultivated. Along the Wallkill river, there is a margin of swamp, known as the Drowned Lands, caused by the collection of the waters from the high ground, in a deep and flat valley, through which the river moves sluggishly. These lands are, in places, heavily timbered. Wardle's Beach, on the Atlantic ocean, Shrewsbury t-ship, Monmouth co., extending south from Old Shrewsbury Inlet. Warren County, was taken from Sussex, by Act, 20th Nov., 1824, which directed, That all the lower part of the latter, southwesterly of a line, beginning on the river Dela WAR 258 WAR ware, at the mouth of Flat Brook, in the t-ship of Walpack, and running thence a straight course to the N. E. corner of Hardwicke church, and thence in the same course to the middle of the Musconetcong creek, thence down the middle of the said creek, to the Delaware, should be a new county. Warren is bounded N. E. by Sussex co.; S. E. by the Musconetcong creek, which divides it from Morris and Hunterdon, and W. and N. W. by the river Delaware. Its greatest length, N. E. and S. W. is 35 miles; greatest breadth, E. and W. 17 miles; area, about 350 square miles; central lat. 40' 50' N.; long. 1' 58' E., from W. C. The county is divided between the primitive and transition formations. A strip of the former crosses it, in the neighbourhood of Beattystown, towards Philipsburg, and the other fills the portion N. of a line running N. W. and S. E. by Sparta, towards Belvidere, including the Blue mountain; leaving an intervening strip of primitive, of a wedge-like form, having its broader part resting on New York. From these formations we may expect a great variety of soils; and indeed all the rocks which belong to them, are singularly blended. The valley of the Musconetcong, on the N. W. side, abounds with transition limestone, bordered by a vein of dark slate; and all the valleys, whether of the primitive or transition, are fertilized by the decomposition of the limestone rock, mingling with the sand, loam and clay, washing from the mountains, making a compound, various as the rocks from which it is derived. The metals found within the county, are magnetic iron, brown hematite, and bog ore, in several places, but principally in Scott's mountain, Jenny Jump, and on the Delaware river, near Foul Rift. A mine of magnetic iron ore is wrought in Scott's mountain, Oxford t-ship, where a furnace was established nearly a century since, and has lately been repaired and put into operation. Zinc, or lead, appears in the hills which bound the Musconetcong valley, on the N. W.; but most probably zinc, inasmuch as these hills are in the range of the Wallkill mountain, where that metal lies in large masses. Gold and silver are said to have been discovered in the Jenny Jump mountain, but which, though possibly true, may in all likelihood, be iron or copper pyrites, which have so often been mistaken for the precious metals. Marble, steatite, or soapstone, roofing slate, and manganese, may also be obtained in the county, sufficiently near to navigation, to render them valuable in commerce. The state quarries, near the Blue mountain, are already extensively worked. The county is marked by several prominent mountain ridges, which determine its water courses, and the surface is every where uneven. Entering it from the south, we cross the natural boundary, the Musconetcong creek, which is confined to a narrow valley, by hills, forming a continua. tion of the Wallkill mountain, whose north-western base is washed by the Pohatcong creek, for nearly the whole breadth of the county; and the valley of that stream is divided from that of the Pequest, by Scott's mountain, which breaks into small and diminished knolls, near the eastern extremity of the county. North of the main branch of the Pequest, but embraced by it and its chief tributary, Beaver brook, lies the Jenny Jump mountain, a narrow and isolated ridge. Beaver brook drains a valley of several miles in width, and covered with knolls of slate, and beds of limestone, and circumscribed northward by a long, unbroken, slaty ridge, which bounds the valley of the Paulinskill. Between that stream, and the Blue mountain, the mean distance may be about five miles. The Blue mountain covers the remaining portion of the county, with the exception of a small strip of alluvial, which borders the Delaware river. WAR 259 WAR As in most parts of the primitive and transition formations, the streams are rapid and precipitous, affording advantageous use of their volumes for hydraulic purposes, but are in no instance navigable. The waters of the county, without exception, seek the Delaware; and whilst that river boldly cuts its way through the mountains, these tributaries are compelled to pursue the course of the ridges whose bases they lave. The,only artificial road of the county, is that from Morristown to Philipsburg, opposite to Easton. A rail-road has been authorized by the Legislature, which is designed to unite with a similar road, opposite to Belvidere, on the Delaware, and to proceed thence to the Susquehanna river. The business of the county is chiefly agricultural, and its staples are wheat, corn, rye, oats, and flax; and in the northern part buckwheat. Within a few years, husbandry has made great advances, and yet continues to improve. The use of lime as a manure is becoming general; and the rich valley lands yield very large crops of wheat, which find a ready market at Easton. Flax-seed is also grown in great quantities; of which 12,000 bushels are annually purchased in Belvidere, alone. In 1830, the county contained, 18,627 inhabitants, of whom 9463 were white males, 8695 white females; 214 free coloured males, 208 free coloured females; 21 male, and 26 female slaves. Of this population, 286 were aliens, 10 were deaf and dumb, and 14 were blind. The inhabitants are chiefly of English extraction, and a considerable portion from New England parents. By the abstract of the assessors, reported to the Legislature, in 1832, there were 102,377 acres of improved land, making nearly one-half the area of the county; 1062 householders, whose ratables did not exceed $30; 411 single men; 3489 taxables; 56 merchants, 45 grist mills, 41 saw mills, 16 carding machines, 7 furnaces for casting iron, 2 cotton and woollen factories, 2 fulling mills, 3 oil mills, and 1 plaster mill, 235 tan vats, 1 glass factory, 3 distilleries of grain, and 25 of cider; 14 carriages, with steel springs; 177 riding chairs, gigs and sulkies; 4324 horses, and 7772 neat cattle, over 3 years of age; and it paid for t-ship purposes, $5700; and for state and county purposes, $8999 20. The t-ship of Greenwich alone honourably distinguished itself, by appropriating money to school use, and paid for this object, $500. The religious sects of the county are Presbyterian, Methodist, Episcopalian, Baptists, and Chris-ti-ans. The last has, we believe, two churches, and admits women to officiate in the ministry. These sects rank in number in the order we have placed them. The towns and post-offices of the county are, Belvidere, the seat of justice; Finesville, Hughesville, Bloomsbury, Asbury, Imlaydale, Pleasant Valley, Mansfield, Anderson, Beattystown, Hackettstown, Alamuche, Long Bridge, Johnsonburg, Lawrenceville, Marksborough, Philipsburg, Stewartsville, New Village, Broadway, Concord, Rocksbury, Oxford, Hope, Shiloh, Columbia, Knowlton Mills, Centreville, Sodom, Gravel Hill, &c. The courts of common pleas, orphaA's courts, and quarter sessions, are holden at Belvidere, on the 2d Tuesday of February, 1st Tuesday of June, 4th Tuesday of August, and the 1st Tuesday after the 4th in November. The circuit court and sessions of oyer and terminer, and general jail delivery, are holden on the 1st Tuesday in June, and the 1st Tuesday after the 4th in November. The county elects one member to the council, and two to the general Assembly. WA~ 260 WAS STATISTICAL TABLE OF WARREN COUNTY. - I Population. Townships. " Area. Surface. S1830. Greenwich, 13 11 38,000 hilly. 4486 Hardwick, 11 8 24,320 do. 1962 Independence, 9 8) 29,440 hills and vales. 2126 Knowlton, 10 10 44,800 do. 2827 Mansfield, 15 62 33,000 mountainous. 3303 Oxford, 16 51 42,000 do. 3665 Pahaquarry, 13 21 12,800 do. 258 _224,360 __18,627 Warren t-ship, Somerset co., bounded N. by Bernard t-ship and by Morris t-ship, Morris co., from which it is separated by the Passaic river; N. E. by New Providence; S. E. by Westfield t-ship, of Essex co.; S. by Piscataway t-ship, Middlesex co.; and S, W. by Bridgewater t-ship, Somerset co. Greatest length N. E. and S. W. 8 miles; breadth N. and S. 4 miles: centrally distant N. E. from Somerville 6 miles; area, 18,000 acres; surface, mountainous, the whole t-ship being covered with hills; bent into elliptic form, with a single narrow valley drained by Middle Brook. These hills are low, well wooded, and composed of trap rock, upon old red sandstone, whose disintegration gives a soil of stiff clay and sandy loam. They contain veins of copper ore, apparently, very rich, and said to be valuable not only for the copper they contain, but also for their gold. Several efforts have been made to work them, but none have been successfully prosecuted. Mvines have been opened within 2 miles N. E. of Somerville, which were lately wrought by Mr. Cammams and Dr. Stryker, who have suspended their operations; others, within a mile of the village of Green Brook, and six of Somerville, were worked some 40 years ago. The southern base of these mineral hills is washed by Green Brook. Mount Bethel is a small hamlet at which we believe the post office of the t-ship is kept, called " Warren." Population in 1830, 1501. In 1832 the t-ship contained about 300 taxables, 56 householders, whose ratables did not exceed $30; 42 single men, 4 stores, 8 saw mills, 4 grist fmills, 2 fulling mills, 4 tan vats, 5 distilleries, 3 carding machines, 259 horses and mules, and 873 neat cattle, over 3 years of age. Warwick Creek, rises in Orange co., in the state of New York, from Wickham's Pond, and flows thence by the town of Warwick S. W. into Vernon t-ship, Sussex co., and into the valley between Wawayanda and Pochuck mountains; thence by a N. W. course re-enters the state of New York, and unites with the Wallkill river, in the Great Marsh. This stream gives motion to several mills. Washington t-ship, Morris co., bounded N. by Roxbury t-ship; E. by that t-ship and Chester; S. by Tewkesbury and Lebanon t-ships, Hunterdon co.; and W. by Mansfield and Independence t-ships, Warren co., from which it is separated by Musconetcong creek. Centrally distant W. from Morristown 18 miles: greatest length E. and W. 8, breadth N. and S. 71 miles; area, 27,500 acres; surface, mountainous, Schooley's mountain covering the western portion; on the east of which, lies the German valley, drained by the south branch of the Raritan river: the intervening country between that and the Black river, near the south WAS 261 WAT eastern boundary, is hilly. The soil of the highlands is generally clay and loam, with grey limestone in the valleys. Much of the mountain is cultivated, and with lime, brings abundant crops. The German valley is very rich, and settled by the industrious descendants of Germans. The celebrated mineral spring and houses of public entertainment, are on the mountain. (See Schooley's Mountain.) Springtown and Pleasant Grove are villages of the t-ship.Population in 1830, 2188. In 1832 the t-ship contained 397 taxables, 124 householders, whose ratables did not exceed $30 in value; 8 stores, 11 saw, 6 grist mills, 3 forges, 20 tan vats, 10 distilleries, 532 horses, and 1015 neat cattle, above 3 years of age; and paid the following taxes: state, $314; county, $703 74; poor, $300; road, $500. Washington, village of North Brunswick t-ship, Middlesex co., on the left bank of the South river, 5 miles S. E. from New Brunswick, and about 3 miles from the confluence of that river with the Raritan. There are here 2 taverns, 3 stores, and from 30 to 40 dwellings. An unsuccessful attempt has been made to cut a canal, a mile long, between the South river and the Raritan, in order to save several miles in the navigation from the town to Perth Amboy. Washington t-ship, Burlington co., bounded N. and N. E. by Northampton t-ship; S. E. by Little Egg Harbour t-ship; S. W. and W. by Galloway and Waterford t-ships, Gloucester co.; and N. W. by Evesham t-ship. Centrally distant S. from Woodbury, 22 miles. Greatest breadth, N. and S. 19 miles; greatest length, E. and W. 20 miles; area, 112,000 acres. Surface, level; soil, generally sandy, and covered with forest. Drained S. by the Little Egg Harbour river, and its several branches; Atsion, the main branch, being on the W. boundary, and Wading river running centrally through the t-ship. Shamong, Washington, and Greenbank, are villages of the t-ship. Population in 1830, 1315. In 1832 the t-ship contained 141 householders, whose ratables did not exceed $30; 59 single men; 287 taxables; 6 stores, 3 fisheries, 7 saw mills, 4 grist mills, 2 furnaces, 1 forge, 6 dearborns, 19 covered wagons, 4 gigs and sulkies, 333 neat cattle, 265 horses and mules; and paid state tax, $117 12; county tax, $371 10; township tax, $450. Washington, p-t. of Washington t-ship, Morris co., in the German valley, Schooley's mountain, on the turnpike road from Morristown to Easton, and on the south branch of the Raritan river, 18 miles W. of Morristown, 54 N. E. from Trenton, and 220 by post route from W. C.; contains 1 Presbyterian, and 1 Lutheran church, a school, 1 store, 2 taverns, and about 20 dwellings. It is surrounded by a fertile, well improved, limestone country. (See German Valley.) Washington, village of Mansfield t-ship, Warren county. (See Mansfield.) Waterford t-ship, Gloucester co., bounded N. E. by Chester t-ship; E. by Evesham t-ship, Burlington co.; S. E. by Galloway t-ship; W. by Gloucester and Newton t-ships; and N. W. by the river Delaware. Centrally distant W. from Woodbury 12 miles. Greatest length, N. W. and S. E., 25; breadth, 8 miles. Its form is very irregular, being deeply indented by the adjacent county of Burlington, and being near the middle of its length, scarce more than a mile in width. Its surface is level, broken only by the streams which run through it; soil, sandy, mixed in the northern part, more or less with loam, but generally light, producing tolerable grass, when manured with marl, ashes or lime, and is cultivated in fruit and vegetables for market. The southern part of the t-ship, has a sandy soil, covered with a pine forest, and is valuable chiefly on account of its timber. It is drained, N. E. by Pensauken creek; N. W. WEA 262 WES by Cooper's creek, which, respective. ly, are boundaries; and on the S. E. by several branches of the Atsion river, of which Atquatqua creek runs along the S. E. boundary. Shell marl is found in the t-ship, in the neighbourhood of Long-a-coming, and other places. Waterfordville, and Ellisville, are villages of the t-ship, and Long-a-coming is on the western t-ship line. Population in 1830, 3088. In 1832 the t-ship contained an Episcopal church, 404 householders, whose ratables did not exceed $30, in value; 7 stores, 5 fisheries, 5 grist mills, 4 saw mills, 7 distilleries, 2 glass factories; and paid poor tax, $660 52; county tax, $1321 06; township tax, $1200. BWaterfordville, village of Waterford t-ship, Gloucester co., on the road from Camden to Moorestown, about 5 miles from either; contains,a tavern, store, and 8 or 10 dwellings. Water Street, village of Mendham t-ship, Morris co., on the line between that and Morris t-ship, and on the head waters of Whippany river, 3 miles W. of Morristown; contains a grist mill, store, and half a dozen of dwellings. Watson's Creek, Middletown t-sp., Monmouth co., runs N. E. 2 miles, into Sandy Hook bay. Wawayanda Mountain, Vernon t-ship, Sussex co., extends northerly, across the eastern part of the t-ship, about 9 miles. It interlocks on the S. with the Wallkill mountain. Waycake Creek, Middletown t-sp., Monmouth co., flows N. ahout 5 miles, into the Raritan bay, W. of Point Comfort. Weasel; the name of a dense settlement, of Acquackanonck t-ship, Essex co., extending for near 4 miles, along the right bank of the Passaic, between Acquackanonck village, and Paterson. There may be in the settlement, about 40 dwellings, many of which are very neat. The country is fertile, and extremely well cultivated;-land, in farms, valued at $100 the acre. West or Jecak Creek, forms the S. E. boundary of Cumberland co., between that and Cape May co. It is a mill stream between 6 and 7 miles in length, upon which are Hughes' grist and saw mills. Westfield, small village of Chester t-ship, Burlington co., on the road from Camden to Burlington, 7 miles N. of the former, and 11 S. W. from Mount Holly; contains a Friends' meeting house, and some half dozen farm houses, in a very fertile well cultivated country. Soil, sandy loam. Westfield t-ship, Essex co., bounded N. by Springfield; E. by Union; S. E. by Rahway t-ships; S. by Middlesex co.; W. by Warren t-ship, Somerset co., and by New Providence t-ship. Centrally distant S. W.rfrom Newark 13 miles: greatest length 7, breadth 6 miles; area, 18,000 acres; surface on the N. W. hilly, but subsiding to a plain on the south; soil, clay loam northward, and red shale southward: the latter rich and carefully cultivated. Rahway river courses the eastern, and Green Brook the western, boundary. A more abundant and delightful country is scarce any where to be found, than that along from the foot of the mountain, north of Scotch Plains through the -t-ship. West. field, Plainfield, and Scotch Plains are villages and post-towns of the precinct. Population in 1830, 2492. In 1832 the t-ship contained 475 taxables, 124 householders, whose ratables did not exceed $30; 64 single men, 5 merchants, 5 grist mills, 2 saw mills, 1 paper mill, 423 horses and mules, and 1111 neat cattle, above 3 years old; and paid state tax, $264 78; county, $692 77; poor, $420; road, $800..Westfield, p-t. of the above t-ship, 11 miles S. W. from Newark, 218 N. E. from W. C., 52 from Trenton, and 3- from Scotch Plains, on the road leading thence to Elizabethtown; contains a Presbyterian church, a tavern, store, and smithery, and 25 dwellings. The vicinage is level, with a stiff clay cold soil. Lands WEY 263 WHI valued at an average of 25 dollars per acre. Westecunk Creek, rises by several i branches in Little Egg Harbour t-sp, l Burlington co., and flows S. E. about 8 miles, through Stafford t-ship, Monmouth co., into Little Egg Harbour bay. There was formerly a forge upon the stream. There are now a grist and saw mill, and in the vicinity, some 15 or 20 dwellings. The Palma Christi, or castor bean, is extensively cultivated here. West Milford, post-office of Bergen co., 248 miles from W. C., and 82 N. E. from Trenton. Weston, p-t., on the Millstone river, and on the Delaware and Raritan canal, formerly called Rogers' Mill, about a mile and a half from its confluence with the Raritan river, and 2 miles below the village of Millstone, 3 miles in a direct line S. E. of Somerville, Somerset co., and about 30 from Trentoni contains a saw mill, grist mill, store, and some 10 or 12 dwellings. Weymouth, blast furnace, forge, and village, in Hamilton t-ship, Gloucester co., upon the Great Egg Harbour river, about 5 miles above the head of navigation. The furnace makes about 900 tons of castings annually: the forge having four fires and two hammers, makes about 200 tons bar iron, immediately from the ore. There are also a grist and a saw mill, and buildings for the workmen, of whom 100 are constantly employed about the works, and the persons depending upon them for subsistence, average 600 annually. There are 85,000 acres of land pertaining to this establishment, within which May's Landing is included. The works have a superabundant supply of water, during all seasons of the year. Weymouth t-ship, Gloucester co., bounded N. by Hamilton; E. by Great Egg Harbour river; S. and W. by Tuckahoe river. Centrally distant from Woodbury 41 miles: greatest length N. and S. 12 miles; breadth E. and W. 10 miles; area, 50,000 acres; surface, level; soil, sandy: eastern boundary on the river, and the portion on the S. E. lying between the two rivers is salt marsh. Stephens' Creek and Tuckahoe are villages and post-towns of the t-ship. Population in 1830, 3333. In 1832 the t-ship contained 90 householders, whose ratables did not exceed $30; 4 stores, 2 grist mills, 1 carding machine, 1 blast furnace, and 2 forges called Etna, 4 saw mills, 315 neat cattle, and 90 horses and mules, above 3 years old; and paid county tax, $157 69; poor tax, $78 82; and road tax, $600. Whale Pond Creek, Shrewsbury t-ship, Monmouth co., flows easterly about 5 miles to the ocean, about a mile below the Long Branch boarding houses. It gives motion to a mill. Wheat Sheaf, small village on the line separating Rahway from Elizabethtown t-ship, 8 miles S. W. from Newark, and half-way between Bridgetown and Elizabethtown, 3 miles from either; contains a tavern, from whose sign it has its name; a store, and 8 or 10 dwellings. Whippany, manufacturing village, of Hanover t-ship, Morris co., on the Whippany river, 5 miles N. E. of Morristown; contains a Methodist church, an academy, 3 stores, 1 tavern, 5 cotton manufactories, 2000 spindles, 3 paper mills, and 56 dwellings. Soil, loam, valued at 25 and 30 dollars per acre. Whippany River, Morris co., a considerable tributary of the Rockaway, rises in Mendham t-ship, at the foot of Trowbridge mountain, and flows by a N. E. course of 17 or 18 miles, by Morristown, to its recipient about 2 miles above the junction of that stream with the Passaic. This is a fine mill stream, drives many mills in its course, and is well employed at the village of Whippany. White Hall, hamlet on Schooley's mountain, Lebanon t-ship, Hunterdon co., 18 miles N. E. of Flemington; contains a store, tavern, smith shop, and 4 or 5 dwellings. WIL 264 WIN White Hill, landing and small vil- W. by the Rancocus creek, which lage, on the Delaware river, Mans- separates it from Chester t-ship; and field t-ship, Burlington co.; contains N. W. by the river Delaware. Cen2 taverns, 10 or 12 dwellings, and trally distant N. W. from Mount an air furnace. There is also a ferry Holly, 7 miles. Greatest length, 6, here. breadth, 4 miles; area, 7500 acres. White House, p-t. of Readington Surface, generally level; soil, sand t-ship, Hunterdon co., 10 miles N. E. and sandy loam, well cultivated, and of Flemington, 33 from Trenton, and productive in grass, grain, vegetables 196 from W. C., upon Rockaway and fruit. A small branch of the creek; contains a grist mill, some Rancocus creek, crosses the t-ship. 12 or 15 dwellings, 3 stores, 3 ta- Dunks' ferry, over the Delaware, is verns, and a Presbyterian or Dutch within it, 4 miles below Burlington. Reformed church. The surface of Cooperstown is the only village. Pothe country around it is hilly; soil, pulation in 1830, 782. In 1832 the loam, clay, and red shale. t-ship contained 160 taxables; 50 White Marsh Run, tributary of householders, whose ratables did not Maurice river, rises in Fairfield t-ship, exceed $30; 28 single men; 1 grist Cumberland co., and flows eastward- mill, 2 distilleries, 2 coaches, 6 dearly to its recipient, about 6 miles. borns, 36 covered wagons, 4 chairs White Ponds, two small lakes, and curricles, 5 gigs and sulkies, 269 connected by a brook, lying at the neat cattle, and 176 horses and mules, west foot of Pimple Hill, in Hardis- above 3 years old; and paid state ton t-ship, Sussex co., on the western tax, $109 38; county tax, $381 93; line of the t-ship, distant, in a direct township tax, $400. line N. E. from Newton, 8 miles. Windsor, West, t-ship, Middlesex Wickhechecoke Creek, rises by co., bounded N. E. by South Brunstwo branches in the hills, on the N. wick; S. E. by East Windsor; S. W. of Amwell t-ship, Hunterdon co., W. by Nottingham t-ship, of Burand flows by a southerly course of lington co., and by Lawrence t-ship, 10 miles, into the Delaware, giving Hunterdon co.; and on the N. W. motion to several mills. by Montgomery t-ship, Hunterdon Williamsville, Orange t-ship, Es- co. Centrally distant S. W. from sex co,, 5 miles N. W. of Newark, Brunswick, 17 miles. Greatest length, near the foot of the first mountain; 7, breadth, 5 miles; area, 19,000 contains 8 or 10 houses, acres. Surface, level; soil, sandy Williamsburg, or Penn's Neck, loam and clay, generally well cultiWest Windsor t-ship, Middlesex co., vated, and producing, abundantly, on the straight turnpike, from Tren- grain and grass. Drained on the E. ton toNew Brunswick, 10 miles from by Millstone river; on the S. W. by the first, 15 from the second, 2 miles the Assunpink creek; and on the N. from Princeton, and half a mile W. W. by Stony Brook. The road from Millstone river, and Stony through Princeton divides this from brook; contains a Baptist church, of Somerset co. Princeton, Williamswood; an Episcopalian church; 2 burg, Clarksville, Dutch Neck, and taverns, 1 store, and 12 dwellings. Edinburg, are towns of the t-ship. Sdil, kind, sandy loam, extremely Population in 1830, 2129. In 1832 well cultivated, and productive. There the t-ship contained 448 taxables; are two large quarries of freestone, 226 householders, whose ratables did of excellent building stone upon the not exceed $30; 64 single men; 6 river, merchants; 1 large grist mill, with Williamsburg. (See Cedar Creek.) 3 run of stones; 1 woollen factory, Willingboro' t-ship, Burlington 3 distilleries, and 496 horses and co., bounded N. E. by Burlington mules, and 848 neat cattle, over 3 t-ship; S. E. by Northampton; S. years of age; and paid state tax, WOO 265 WOO $320 49; county, $394 04; road, $200; poor, $450. Excellent freestone, for building, is abundant in the t-ship. Windsor, East, t-ship of Middlesex co., bounded N. by South Brunswick t-ship; N. E. by South Amboy; S. E. by Freehold t-ship, Monmouth co.; S. W. by Nottingham t-ship, Burlington co.; and N. W. by West Windsor t-ship. Centrally distant S. W. from New Brunswick, 20 miles. Greatest length, 12: greatest breadth, 6 miles; area, 24,000 acres. Surface level; soil, sandy and gravelly loam, light, and not generally productive. Drained by Millstone river, and Rocky brook, on the N. E., and by the Assunpink and Miry run, upon the S. W. Hightstown, Millford, Centreville, and Cattail, are villages, the first a post-town, of the t-ship. The turnpike road from Bordentown, to New Brunswick, crosses the t'ship. Population in 1830, 1930. In 188t the t-ship contained 487 taxables; 52 householders, whose ratables did not exceed $30; and 41 single men, 3 merchants, 3 saw mills, 4 grist mills, 1 woollen factory, 2 carding machines, and fulling mills, 32 tan vats, 13 distilleries for cider, and 484 horses and mules, and 897 neat cattle, above 3 years of age; and paid state tax, $286 77; county, $352 53; road tax, $400; poor tax, $700. Woodbridge t-ship, Middlesex co., bounded N, by Westfield, and Rahway t-ships, Essex co.; E. by Staten Island Souud; S. E. by Perth Amboy t-ship; S. by Raritan river; and W. by Piscataway t-ship. Centrally distant from New Brunswick, N. E. 8 miles. Length, E. and W. 9, breadth, N. and S. 9 miles; area, 244000 acres. Surface, level; soil, red shale, universally well cultivated. Drained on the N. E. by a branch of Rahway river, upon which are some mills. Rahway and Woodbridge, are post-towns, Matouchin and Bonhamtown, villages of the t.ship. Two turnpike roads from New Brunswick, run N. E. through the t-ship, which 2L are crossed by an other,, from Perth Amboy to New Durham. Population in 1830, 3969. In 1832 the t-ship contained 700 taxables; 180 householders, whose ratables did not exceed $30 in value; 99 single men; 13 stores, 5 saw mills, 3 grist mills, 40 tan vats, 1 distillery, 585 horses and mules, 1555 neat cattle, 3 years old and upwards; and paid state tax, $594 53; county, $731 03; road, 1800; poor, $1000. This t-ship contains a portion of the thriving town of Rahway. It was incorporated by Governor Philip Carteret, prior to 1680, by one of the most liberal charters which had ever been given in America. (See Records of East Jersey Proprietaries, at Amboy.) In 1682, it was estimated that there were in the t-ship, one hundred and twenty families. They had then erected a court-house and prison, and had many thousand acres surveyed for plantations. Delaplaine, the surveyor-general, was one of the settlers here. Woodbury Creek, Deptford t-ship, Gloucester co., rises by two branches; the southern called Matthew's branch, each about 3 miles above Woodbury, and unite below the town. The north branch is navigable from the town to the river Delaware, 3 miles. Woodbury, p-t., and seat of justice of Gloucester co., on Woodbury creek, at the head of navigation, 8 miles S. of Camden, 39 from Trenton, and 145 from W. C.; contains a spacious court-house of brick, and county offices, fire proof; and of the same material, detached, and a prison, in the rear of the court-house, of stone; 1 Friends' meeting house, large, and of brick; 1 Presbyterian church, frame, with cupola and bell, the upper part of which is used as an academy; and 1 brick Methodist church; 2 common schools; 2 pub-. lie libraries, one of which was founded by the ladies of the town; 2 sunday schools; a county bible society; and temperance society, which has been productive of very beneficial effects; several *store-keepers refusing wOO 266 YAR to sell spirituous liquors; 10 stores, 3 taverns, 4 lawyers, 3 physicians, 1 clergyman, 100 dwelling houses, and 735 inhabitants. The town, for a mile in length, and half a mile in breadth, is incorporated, for the maintenance of a fire engine and fire apparatus, for which eight public wells have been sunk; andthe provisions for defence, against this devastating element, are very efficient. The creek was, 70 years since, stopped out; but the obstruction was removed in 1830, much to the convenience and health of the inhabitants. Vessels now load at the landing, in the town. Woodruff's Gap, through Bear Fort mountain, Pompton t-ship, Bergen co. The Ringwood and Long Pond turnpike road passes through it. Woodstown, p-t., and village, of Pilesgrove t-ship, Salem co., upon' the Salem creek, 10 miles E. of the town of Salem, 161 N. E. from W. CO, and 55 S. of Trenton. The tqwn contains about 150 dwellings, 2 taverns, and 6 stores, 3 schools, 1 Friends' meeting, 1 Baptist, and 1 African Methodist church. In the neighbourhood of the town, there are some valuable marl beds-and the use of marl has much improved the agriculture of the t-ship. Woodsville, p-t. of Hopewell t-sp., Hunterdon co., 10 miles S. from Flemington, 13 N. from Trenton, 179 from W. C., on the turnpike road fromi N. Brunswick, to Lambertsville; contains a store, tavern, and half a dozen dwellings, mostly new. It lies upon the slope of a gently rising ground, from which there is a delightful prospect of the surrounding country; the soil of which is of red shale, and well cultivated. Woolwich t-ship, Gloucester co., bounded on the N. E. by Greenwich; on the S. E. by Franklin, t-ships; S. W. by Pittsgrove, Pilesgrove, and Uipper Penn's Neck, t-ships, Salem co; and N. W. by the river Delaware. Centrally distant S. W, from Woodbury, 11 miles. Greatest length, 16; breadth, 7 miles; area, about 40,000 acres. Surface, level; soil, sandy, and on the S. E. covered witir pine forest. Drained, westerly, by Repaupo, Little Timber, Raccoon, and Oldman's, creeks-the last of which forms the S. W. boundary. Swedesboro' and Battentown, are villages-the first a post-town of the t-ship. Population in 1830, 3033. In 1832 the t-ship contained 333 householders, whose ratables did not exceed $30; 8 stores, 9 grist mills, 4 saw mills, 3 fulling mills, 1 tannery, 8 distilleries, 1433 neat cattle, arid 699 horses and mules above the age of 3 years. Wrangleboro' or Clark's Mill, village, on Nacote creek, of Galloway t-ship, Gloucester co., about 37 miles S. E. from Woodbury; contains a store, one or more taverns, and one mill, and 15 or 20 dwellings. Wrangle Brook, considerable tributary of the south branch of Toms' river, Dover t-ship, Monmouth co., uniting with the main branch, about two miles above Toms' River village. Wrightsville, on the road from Allentown to Freehold, Upper Freehold t-ship, Monmouth co., 5 miles from the former, and 14 from the latter; contains 8 or 10 dwellings and a Quaker meeting house; soil, sandy. In the rear of the village, upon Cattail creek, are some bog meadows, which, in hot weather, are covered, in places, with an efflorescence of sulphate of iron (copperas). Wrightstown, Hanover t-ship, Burlington co., 10 miles N. E. from Mount Holly, and 10 S. E. of Bordenton; contains 2 taverns, 2 stores, a Methodist church, and some 15 or 20 dwellings; surrounded by a very fertile country. Yard's Branch, of Paulinskill, rises in the Blue mountains, in Pahaquarry t-ship, and flows S. W. through Knowlton t-ship to its recipient, near the village of Sodom, having a course of about 8 miles. THE HISTORY OF NEW JERSEY, FROM3 ITIS DISCOVERY BY EUROPEANS, THE ADOPTION OtF ''111 FEDE RAL CONSTITUTION* BY THOMAS F. GORDON. Ermuton: PUBLISHED BY DANIEL FENTON. John C. Clark, Printer, Philadelphia. 1834. Entered by THOMAS F. GORDON, according to the Act of Congress, in the Clerk's Office of the District Court for the Eastern District of Pennsylvania. PREFACE. AN attempt has been made in the following pages to narrate, succinctly, but fully, the history of New Jersey, from the time of its discovery by Europeans, to that of the adoption of the constitution of the United States. By the latter event, the individuality of the State, as a historical subject, is merged in the history of the nation; and the subsequent period of unvaried political prosperity, within her borders, presents few matters for the historian. The story we have told, has, for the inhabitants of the State, the interest of their peculiar and proper affairs; but, like such. affairs, may not prove attractive to strangers. Like Pennsylvania, this State was founded by deeds of peace; and no community, in any country, can have undergone less vicissitude. Her prudence and justice preserved her from Indian hostility, and her distance from the frontier protected her from the inroads of the French. She has known, therefore, no wars, save those commanded by the king, or undertaken in defence of her own civil liberty. To pourtray the part, which, as a colony, she took in the one, and as an independent State, in the other, it has been necessary to treat of the general colonial and revolutionary history; yet no further than was indispensable to exhibit the action of New Jersey. In the compilation of the work, resort has been had to all the known histories of the Anglo-American colonies, to the best writers on the American revolution, and to the minutes of the legislature and the statutes, for a period of more than one hundred and twenty years. From these sources, it is believed, that a faithful and ample narrative has been obtained. More particulars of the horrors which attended the revolutionary war, especially of those which were inflicted by furious tory partisans, might, perhaps, have been added, if full reliance were due to the partial newspaper accounts, frequently written under excitement unfavourable to truth. Yet, enough of these scenes has been described to display the nature and extent of the sufferings of the inhabitants; more would have served rather to disgust, than to entertain, the reader. iv PREFACE. The author submits the result of his labours to the many subscribers by whom they have been encouraged, with an assurance of his readiness, in another edition, to supply such omissions, and to correct such errors, as may be discovered in the present. March, 1834. CONTENTS. CHAPTER I. Comprising Events from the Discovery by Europeans, to the Grant from Charles I. to James Duke of York. I. Ancient and Modern Principles of Colonization. II. Voyages of the Spaniards and Portuguese upon the East Coast of North America. III. Voyages of the Italians, Verrazano, and the Cabots. IV. First English Attempts at Discovery. V. Efforts of Raleigh to establish a Colony. VI. Gosnold opens a new Road-London and Plymouth Companies created. VII. Voyages and Discoveries of Hudson. VIII. Intercourse of the Dutch East India Company with America, and Formation of the Amsterdam Licensed Trading West India Company. IX. Settlement of the Puritans at Plymouth. X. Formation of the Great West India Company in Holland. XI. Voyage and Proceedings of Cornelius Jacobse Mey. XII. Measures of the Company to promote Emigra tion; Purchases of large Tracts of Land from the Indians. XIII. Voyages of De Vries; Colony planted-The Delaware abandoned by the Dutch. XIV. Minisink Settlements on the Delaware. XV. Settlements of the Swedes on the Delaware-first Project of a Colony-first Colony-increase of Settlers. XVI. Colonial Government established-Colonel Printz first Governor. XVII. English Settlements upon the Delaware-prostrated by a united Force of Dutch and Swedes. XVIII. Swedish Government under Printz and his Successors. XIX. Swedish Colony subjected by the Dutch. XX. Dutch Colonial Government on the Delaware-Possessions on the East of New Jersey. XXI. Account of the English Settlements upon the Delaware previous to 1664-under Patent from Lord Baltimoreunder Grant to Sir Edward Ploeyden-by Traders from New Haven. XXII. Plans of New England Settlers for Conquest of the Dutch Colonies. XXIII. Duke of York's Charter from the Crown and Grant to Berkeley and Carteret. XXIV. Conquest of New Netherlands, by Colonel Nicholls. XXV. English Government established on the Delaware. XXVI. Condition of New Netherlands at the time of the Surrender page 1 CHAPTER II. Comprising Events from the Grant to the Duke of York, to the Division of the Colony, into East and West Jersey. I. Nature of the Estate acquired by the Duke of York, by the Grant from Charles I. II. Motives and Nature of the Grant from the Duke of York, to Berkeley and Carteret. 111. Bounds of the Country ceded. IV. Proceedings of the Proprietaries, to settle their Province of New Jersey, &c.-their " Concessions." V. Remarks on the Constitution. VI. Assumption of Government by Colonel Nicholls-Indian Grants. VII. Philip Carteret appointed Governor-His Efforts for Colonization-Advantages enjoyed by the New Colonists. VIII. Unhappy Effects of the Demand of Proprietary Quit Rents. IX. Recapture of New Netherlands by Holland-and Restoration to the English. X. Re-grant of the Province to the Duke-Re-grant to Berkeley and Carteret. XI. Return of Philip Carteret to the Government-Modification of the Constitution. XII. Oppressive Conduct of Andross, Governor of New York. XIII. Division of the Province into East and West Jersey. 23 CHAPTER II. From the Division of the Province, into East and West Jersey, to the Purchase of East Jersey, by Quakers. I. Motives of the Quakers for Emigration. II. Sale of Lord Berkeley, to Byllinge and Fenwicke. III. Assignment of West Jersey to William Penn, and others in Trust, for the Creditors of Byllinge. IV. "Concessions," or Constitution of West Jersey. V. Measures of the Proprietaries to promote Colonization. VI. Commissioners a vi CONTENTS. appointed to Administer the Government of West Jersey-their Proceedings. VII. Increase of Emigrants-Success of their Efforts. VIII. Death of Sir George Carteret-Successful Efforts of the Colonists, to procure Relief from the Jurisdiction of New York. IX. Extraordinary Pretensions of Byllinge. X. Resisted by the Proprietaries, in General AssemblySamuel Jennings elected Governor-Proceeds to England, as Deputy of the Assembly-The Right of Government, purchased by Doctor Daniel Coxe, and subsequently transferred to the West Jersey Society. XII. Meeting of the First Assembly-Proceedings. XIII. Modification of the Law, relating to Religious Faith. XIV. Death of Carteret-his Disposition of East Jersey. XV. Troubles at the Close of the Administration of Philip Carteret. XVI. Review of the Policy of the Proprietary Governments. XVI1. Comparison between the Laws of East and West Jersey 32 CHAPTER IV. From the Purchase of East Jersey, by the Quakers, to the Surrender of the two Provinces to the Crown, 1682-1702. I. Purchase of East Jersey by Penn and his Associates-They admit others, not Quakers, to participate in the Purchase. II. Robert Barclay appointed Governor for Life-Scotch Emigrants-Deputy Governors-Foundation of Amboy-Vain Efforts at Commerce. III. Efforts of James II. to destroy Colonial Charter-Defeated by the Revolution. IV. Andrew Hamilton, Deputy Governor-Death of Robert Barclay-Interregnum-Andrew Hamilton, Governor-in-ChiefSuperseded by Jeremiah Basse-Reappointed-Discontent of the Colonists. V. Attempt of New York to tax the Colony. VI. Proposition from the English Ministers for the Surrender of the Proprietary GovernmentsNegotiations relating thereto. VII. Final and Unconditional SurrenderLord Cornbury appointed Governor-Outline of the New Government. VIII. Stationary Condition of New Jersey-Causes thereof. IX. Condition of the Aborigines--Purchases of their Lands-Traditions of their Origin-Tribes most noted in New Jersey-Treaty at Crosswicks-at Burlington and Easton-Final Extinction of Indian Title to the Soil of New Jersey. X. Review of the Title under the Proprietaries of East Jersey. XI. Review of Title of Proprietaries of West Jersey. XII. Of the Partition Line between East and West Jersey.... 50 CHAPTER V. Comprising the Administration of Lord Cornbury. I. Arrival of Lord Cornbury-Demands a large&nd permanent Salary-being refused, dissolves the House. II. A new Assembly chosen-Part of its Members arbitrarily excluded-Measures of the Governor. III. Third Assembly convenedDetermines to Petition the Queen, and to remonstrate with the Governor -Public Grievances-Delivery of the Remonstrance, by Samuel Jennings. IV. Reply of the Governor. V. Dispute on the Treasurer's Accounts. VI. The Governor refuses the Message of the Assembly, which they enter upon their Minutes. VII. The West Jersey Proprietors, in England, address a Memorial to the Commissioners of Trade and Plantations, against Cornbury-Address of the Lieutenant-Governor, and Provincial Council, to the Queen. VIII. The Governor unable to obtain the gratification of his wishes, by the Assembly, first prorogues, and then dissolves them. IX. Offensive Conduct of Lord Cornbury, in his Government of New York-His Character. X. Is reluctantly removed by Queen Anne-Imprisoned by his Creditors.. 76 CHAPTER VI. Comprising Events from the Removal of Lord Cornbury to the Close of the Administration of Governor Hunter, 1709-1719. I. Lord Cornbury succeeded by Lord Lovelace-His Conciliatory Address to the Assembly. II. Ready disposition of the House to provide for the Support of Government -Change in the Constitution of the Assembly-Assembly obtain a Copy of the Address of the Lieutenant Governor and Council, to the Queen, in favour of Lord Cornbury-Demand a hearing for their Defence before the Governor. III. Death of Lord Lovelace and Accession of Lieutenant Governor Ingoldsby. IV. Promptitude of the Province to aid in reducing the French Possessions in North America. V. Failure of the Expedition, CONTENTS. Vii and renewed Efforts of the Colonists to revive it-Visit of the Chiefs of the Five Nations to England. VI. Capture of Port Royal, &c. by Colonel Nicholson and the American Forces. VII. Governor Ingoldsby removed -Government administered by William Pinhorne as President of Council -succeeded by Governor Hunter. VIII. Biographical Notice of Governor Hunter. IX. Meets the Assembly, which prefers Charges against Members of Council. X. Expulsion of a Member of the House for his Conduct in Council-Address to the Queen. XI. Bills proposed for the Relief of the Quakers defeated by the Council. XII. New Efforts for the Conquest of the French Provinces-Unfortunate Result. XIII. Continued Quiet of the Province. XIV. Division of the Assembly. XV. Governor Hunter returns to Europe-Testimonials in his favour by New Jersey and New York-Exchanges his Commission with William Burnet 84 CHAPTER VII. Containing Events from the arrival of Governor Burnet, to the Death of Governor Morris, 1719-1746. 1. Governor Burnet-Notice of his Character. II. Meets the Assembly-Proceedings. III. Paper Currency-an Account of its Rise and Progress. IV. Bill proposed against denying the Trinity, &c. V. Governor Bernard removed to Massachusetts. VI. Is succeeded by John Montgomery-His Administration. VII. Death of Colonel Montgomery, and Presidency of Colonel Lewis Morris-Arrival of Governor Cosby-Harmony of the Province during his Administration-His Death. VIII. Presidencies of John Anderson and John Hamilton, Esquires. IX. Lewis Morris, Governor of the Province of New Jersey, it being separated from New York-Gratification of the Province. X. He ceases to meet the Council in Legislation. XI. Salaries of Officers. XII. Unpopular Conduct of Governor Morris. XIII. War with Spain-Aid required by Great Britain, from the Colonies-promptly afforded by New Jersey-Further disputes between the Governor and Assembly. XIV. Disingenuous Conduct of the Governor, relative to the Fee Bill. XV. Opposes the Views of the House, on the Bill relative to the Paper Currency-on that, circumscribing the Jurisdiction of the Supreme Court. XVI. Assembly refuse to provide for the Salaries of the Public Officers. XVII: Efforts at accommodation-defeated by the discovery of the duplicity of the GovernorDeath of Governor Morris-John Hamilton, Esq., President. XVIII. Biographical Notice of Governor Morris. XIX. Application made by his Widow, for arrears of Salary-refused... 93 CHAPTER VIII. Comprehending Events from the Death of Governor Morris to the Death of Governor Belcher-from 1746 to 1757. I. War with France-Proposal of Governor Shirley to attack the French Settlements at Cape Breton-New Jersey votes two thousand Pounds for the Service-Favourable result of the Expedition. II. Proposed attack on Canada-New Jersey Regiment raised and placed under the command of Colonel Philip Schuyler-March for Albany-Threatened Mutiny. III. Plan of the proposed Campaign. IV. Treaty of Peace. V. Death of President Harpilton-Devolvement of the Government on President Reading-Arrival of Governor BelcherHis Character. VI. Vexations arising from the Elizabethtown Claims under Indian Grants-the Assembly disposed to palliate the Conduct of the Rioters-Representation of the Council of Proprietors-their grievous Charge against the Members of Assembly, in a Petition to the King-the House transmits a counter Petition-Disingenuous Conduct of the House. VII. Disputes relative to the " Quota Bill." VIII. Hostile proceedings of the French in America. IX. Difference between the French and English, in their mode of cultivating Indian favour. X. Efforts of the French to occupy the English Lands. XI. Expedition of George Washington to Fort Venango. XII. Measures of the English Government to resist French encroachments. XIII. Convention of the Colonies-Plan of Union proposed by Dr. Franklin-Condemned by New Jersey-Military Expedition of Lieutenant Colonel Washington-is captured by the French under De Villiers. XIV. Extensive Military Preparations of Great Britain. XV. Measures of New Jersey. XVI. Arrival of Major General Braddock. XVII. Convention of Governors to determine the Plan of the Campaign. XVIII. Acquisitions in Nova Scotia-Cruel Treatment of the Neutrals. V111 CONTENTS. XIX. New Jersey raises a Regiment for the Northern Expedition-Mr. Philip Schuyler named Colonel. XX. March of General Braddock on the Western Expedition-Fastidiousness and Presumption of the General-is attacked and defeated. XXI. Universal Consternation on this DefeatGovernor Belcher summons the Legislature-Inroads and Cruelties of the Indians-the Inhabitants of New Jersey give aid to those of Pennsylvania. XXII. Success of the Northern Expedition. XXIII. Provision against the Attack of the French and Indians. XXIV. Plans proposed for the Campaign of 1756-Exertions of the Colonies. XXV. War formally declared between Great Britain and France. XXVI. General Shirley removed from the supreme command-General Abercrombie, and, subsequently, Lord Loudon appointed. XXVII. Suspension of Indian Hostilities. XXVIII. Sluggish Military Efforts of the English-Success of the French in the North-Capture of part of the Jersey Regiment, with Colonel Schuyler, at Oswego-Disastrous termination of the Campaign. XXIX. Renewal of Indian Barbarities. XXX. Military Requisitions of Lord Loudon-New Jersey refuses to raise more than five hundred Men. XXXI. Unsuccessful Attempt of Lord Loudon on Louisburg. XXXII. Success of Montcalm-New Jersey prepares to raise four thousand Men-the remainder of the Jersey Regiment captured by the Enemy. XXXIII. Death of Governor Belcher-Biographical Notice of. XXXIV. John Reading, President....... 106 CHAPTER IX. Containing Events from the Presidency of Mr. Reading to the Repeal of the Stamp Act-from the year 1746 to the year 1766. I. Influence of Mr. Pitt and his Policy upon Colonial Affairs-New hopes infused into the Colonists. II. Successful Attack of the English upon the Northern Forts. III. Capture of Fort Du Quesne by General Forbes. IV. Cheerful and ready aid of the Colonies. V. New Jersey supplies one thousand Men, and builds Barracks'for the King's Troops. VI. President Reading superseded by the arrival of Governor Bernard-His Treaty with the IndiansSucceeded by Thomas Boone-He, by Josiah Hardy-He, by William Franklin, the last of the Royal Governors. VII. Efficient Preparations for the Campaign of 1759. VIII. Conquest of the French Colonies in North America. IX. Honourable share of the Provincialists in this Result. X. Treaty of Peace with France and Spain. XI. New Confederacy and Hostilities of the Indians-Six hundred Troops raised by New Jersey. XII. Impressions on the English Ministry, by the Wealth and Power displayed in America. XIII. Proposition of Mr. Grenville to tax the Colonies. XIV. Consideration of the Principles relating to Colonial Taxation. XV. Mr. Grenville communicates his purpose to the Clolonial Agents in London. XVI. Views taken by Colonies of this Proposition. XVII. Propositions by several of the Colonies to raise Money, rejected by Mr. Grenville. XVIII. Act of Parliament for Tax on Colonial Imports and Exports. XIX. Effect of the Measures in America-Proceedings of Massachusetts and Rhode Island. XX. Stamp Actpassed-Its reception in the Colonies. XXI. Temporary Suspension of Legal Proceedings and of the publication of Newspapers. XXII. Anti-Importation Associations. XXIII. Organization of the "Sons of Liberty." XXIV. Proposition of Massachusetts for assembling a Congress of Deputies from the Colonies-Action of New Jersey on this Proposition. XXV. Proceedings of the Congress-Messrs. Ruggles of Massachusetts, and Ogden of New Jersey, refuse to join in a general Petition. XXVI. The Assembly of New Jersey approve the Proceedings of Congress-adopts Resolutions condemnatory of the Stamp Act. XXVI1. Efforts in England for Repeal of the Stamp Act. XXIX. Inquiry before the House of Commons-Repeal of the Stamp Act... 129 CHAPTER X. Comprising Events from 1766 to 1769. I. Remaining Discontents in the Colonies, after the Repeal of the Stamp Act. II. Dissatisfaction in Great Britain on account of the Repeal-American Taxation again proposed in Parliament, by Mr. Townsend-Bill imposing Duties on Goods imported into America, passed. IV. Circular Letter of Massachusetts to the other Colonies. V. Promptitude and Unanimity of the Colonies produced by the Farmers' Letters. VI. Resort to Non-importation Agreements. VII. CONTENTS. ix The Ministry condemn the Circular Letter. VIII. Menacing Resolutions of Parliament against Massachusetts-The other Colonies approve her Conduct. IX. Modified Repeal of the Imposts--Consequent Modification of the Non-importation Agreements. X. Numerous Law Suits-The People complain of the Fees of the Courts. XI. Disputes between the Governor and the Assembly. XII. Robbery of the Treasury of East JerseyThe Assembly require the removal of the Treasurer-He is protected by the Governor. XIII. Efforts of Governor Franklin to encourage the Culture of Hemp, Flax, and Silk. XIV. New apportionment of Members in the Province. XV. Testimonial of the Northern Indians to the Justice of the Colony...... 144 CHAPTER XI. Comprising Events from the year 1773 to 1776. I. Committees of Correspondence established in the several Colonies. II. The British Ministry encourage the shipment of Teas to America, by the East India Company. III. Alarm of the Colonists-Consignees of the India Company compelled to forego their appointments. IV. Measures pursued in New Jersey. V. Reception of the Tea in America. VI. Indignation of the King and Parliament. VII. Violent measures adopted against Boston. VIII. Alarming Act of Parliament, relative to the Provincial Government of Canada. IX. Proceedings of the Inhabitants of Boston-General Commiseration of their Fate. X. New Jersey appoints Members to Congress. XI. Congress assemble at Philadelphia-Their proceedings. XII. The Assembly of New Jersey approve the proceedings of Congress, and appoint Delegates to the next Convention-Instructions. XIII. The Provincial Governors instructed to impede the Union of the Colonies-Efforts of Governor Franklin. XIV. Reply of the House. XV. Rejoinder of the Governor-Address of the Council. XVI. The Assembly petition the King. XVII. Reception of the proceedings of Congress in London. XVIII. Proceedings of Parliament-Conciliatory Propositions of Lord North. XIX. Sense of New Jersey upon this Proposition. XX. State of the Dispute with England. XXI. Second New Jersey Convention called-Encourages Political Associations-Organizes the Militia, and provides Funds. XXII. Meeting of Congress at Philadelphia-Its Measures., XXIII. Appointment of Commander-in-Chief and subordinate Generals. XXIV. Congress again petition the King-Ungracious reception of the petition. XXV. Address their fellow-subjects of Ireland, &c. XXVI. New Jersey Convention re-assembles-Proceedings-Provision for the continuance of a Provincial Congress-Committee of Safety appointed. XXVII. Meeting of the Assembly-Address of Governor Franklin-He claims assurance of protection for himself and others, the King's Officers. XXVIII. Reply of the Assembly. XXIX. Act authorizing the issue of Bills of Credit, for ~100,000, approved by the King..... 153 CHAPTER XII. Comprising Civil Events of the year 1776. I. State of the Public Opinion at the commencement of the year 1776-Gradual growth of the desire of Independence. II. Resolution of Congress for the establishment of Independent Colonial Governments. III. Provincial Congress re-assembles -Proceeds to the Formation of a Colonial Constitution. IV. Review of the Constitution. V. Oath of Abjuration and Allegiance established. VI. Tories-their motives. VII. Law relative to Treason. VIII. Imprisonment and Relegation of Governor Franklin. IX. Measures adopted against the Disaffected. X. Adoption of the Declaration of Independence........ 178 CHAPTER XIII. I. Military Proceedings in Canada. II. Measures adopted in Great Britain. III. Objects proposed for the Campaign of 1776. IV. Operations against New York, and the surrounding Country. V. Proposals for accommodation, by the British Commissioners. VI. Condition of the American Forces, at New York-Landing of Lord Howe, on Long Island. VII. Battle of Brooklyn. VIII. Retreat of the American Army from Long X CONTENTS. Island. IX. Unhappy Effect of the Defeat of the American Army. X. Lord Howe renews his Attempts for accommodation of the Quarrel-Proceedings of Congress. XI. Military Movement of the Armies, after the Battle of Brooklyn. XII. American Army, by advice of General Lee, quit York Island. XIII. Battle of White Plains. XIV. Capture of Fort Washington. XV. Abandonment of Fort Lee, and retreat of the American Army--ts condition-Inhabitants join the British. XVI. Washington crosses the Delaware-The enemy possess themselves of the left bank. XVII. Capture of General Lee. XVIII. New efforts of the Commander-in-Chief-The enemy retire into Winter Quarters. XIX. Battle of Trenton. XX. The British re-open the Campaign. XXI. The American Army re-enters Jersey. XXII. Battle of Princeton. XXIII. The American Army retreat to Morristown-Beneficial results of the late actions. XXIV. Firmness of Congress. XXV. Condition of New Jersey. XXVI. The American Army inoculated for the Small Pox. XXVII. Measures for reclaiming the disaffected of New Jersey. XXVIII. License of American Troops-restrained.... 203 CHAPTER XIV. I. Organization of the New Jersey State Government. II. First Address of the Governor-Other principal Officers. III. Condition of the State at this period. IV. State of the Northern Department-Operations on the Lakes. V. The British seize Rhode Island. VI. Demonstration of General Heath, on Long Island-Condition of the American Army, in New Jersey-Skirmishing. VII. Early efforts of Sir William Howe, to destroy the American Magazines-Stores burned at Peck's-kill-at Danbury. VIII. Successful enterprise of Colonel Meigs, against Sagg Harbour. IX. Movements of General Washington, on opening the Campaign-Removal of the Army to Middlebrook-Disposition of the Troops. X. Operations of the Army under General Howe-Feint to cross the DelawareRetreat from New Jersey-Returns, and attacks the American Army. XI. Perplexity of Washington, caused by the Movements of the British Forces. XII. Capture of Major-general Prescott, by Major Barton. XlII. General Howe embarks for the southward-Measures of Washington thereon. XIV. Attempt of General Sullivan, with Colonel Ogden, upon the Tories on Staten Island. XV. Arrival of the British Army at Elk River-its Progress-Operations of the American Army-Battle of Brandywine. XVI. Subsequent movement of the Armies. XVII. Second encounter of the hostile Armies-they are separated by rain. XVIII. Affairs of Paoli. XIX. The British enter Philadelphia. XX. Congress remove to Lancaster, thence to York. XXI. Attack and defence of the Fortifications on the Delaware. XXII. Battle of Germantown. XXIII. Operations in New Jersey. XXIV. Further proceedings on the Delaware. XXV. Repulse of Count Donop, from Fort Mercer. XXVI. General Greene despatched to New Jersey. XXVII. Capture of Fort Mifflin, and abandonment of Fort Mercer. XXVIII. Attempt of General Dickenson on Staten Island. XXIX. American Army reinforced. XXX. Attacked at White Marsh, by the British. XXXI. The American Army retires into Winter Quarters. XXXII. English plans for the Northern Campaign. XXXIII. Condition of the American Northern Department. XXXIV. Burgoyne captures the Forts on the Lakes, and disperses the American Army. XXXV. Recuperative measures of General Schuyler. XXXVI. Repulse of St. Leger, from Fort Schuyler. XXXVII. Defeat of Colonel Baum, at Bennington. XXXVIII. Beneficial result of these fortunate Events. XXX1X. Battles on the Hudson, and Capture of Burgoyne. XL. Movements of Sir Henry Clinton, in the Highlands. XLI. Effect of the Capture of Burgoyne-at home and abroad. XLII. Congress refuse to execute the Articles-of Capitulation-their reasons. 235 CHAPTER XV. Campaign of 1778. I. Condition of the Army at the Valley Forge and at the commencement of the Campaign. II. British foraging excursions in New Jersey. III. Fortunate escape of an advance party under La Fayette. IV. Effect of the American successes abroad-Efforts of American Agents. V. Measures for Foreign Alliances-Duplicity of France-Treaties with CONTENTS. Xi her. VI. War between Great Britain and France. VII. Opinions in Great Britain-Ministerial measures. VIII. Reception of those measures in America. IX. Arrival of a French Minister Plenipotentiary. X. The British Army evacuates Philadelphia-March through Jersey. XI. Battle of Monmouth-British Army regains New York. XII. Arrival of the French Fleet-proceeds to Rhode Island. XIII. Attempt on NewportAppearance of the English Fleet-French and English Fleets put to Sea -dispersed by Storm. XIV. British Incursions in Connecticut. XV. Disposition of the American Army. XVI. British Incursions into New Jersey. XVII. Movements of the adverse Fleets-Detachment against the Southern States. XVIII. American Army retires to winter quarters -Its improved condition. XIX. Indian devastations-Massacre at Wyoming. XX. Operations against the Indians. XXI. Discontent in the Jersey line. XXII. March of General Sullivan to the Indian countryEvents there. XXIII. Expedition under Colonel Broadhead by the Allegheny River. XXIV. Expedition against the Cherokees under General Pickens. XXV. Unprovoked Slaughter of the Indians at Muskingum. 262 CHAPTER XVI. Comprising a View of the War in the South. I. Inert state of the Country in 1779. II. The British Government adopts views of partial Conquest. III. Georgia overrun--and Charleston threatened-Unsuccessful Siege of Savannah. IV. Sir Henry Clinton subdues South Carolina. V. His measures induce Revolt. VI. General Gates assumes command of the Southern Army-Battle of Camden. VII. Battle of King's Mountain. VIII. Cornwallis reinforced. IX. General Greene appointed to the Southern Department-Battle of the Cowpens-Retreat to Virginia. X. Cornwallis retires, is pursued-Battle of Guilford Court House. X1. Cornwallis marches for Petersburg--Greene for South Carolina-Expedition of Arnold against Virginia-Preparations against him-Defence of Virginia entrusted to La Fayette--Cornwallis takes command of the British Forces in Virginia. XII. Progress of Greene in recovering the Southern States. XIII. Sufferings of the Inhabitants.... 285 CHAPTER XVII. I. Condition of the Armies in the North. II. British Expedition against the Forts on the North River. III. Expedition under Tryon, against Connecticut. IV. Capture of Stony Point, by Wayne. V. Attack of the British Post, on Penobscot river.-VI. Major Lee assaults Paules Hook. VII. Effects of the System of Paper Currency. VIII. Spain declares War against England. IX. Prospects of the Campaign of 1780. X. The American Army retires into winter quarters. XI. Marauding Parties of the Enemy in New Jersey. XII. The Army at Morristown supplied by forced levies of Provisions. XIII. Washington attempts the British Post at Staten Island XIV. Difficulties arising from the want of political power in Congress. XV. Discontents of the Army-Mutiny of the Connecticut troops. XVI. Knyphausen invades New Jersey-Murder of Mrs. Caldwell, and of her Husband. XVII. Battle of Springfield.XVIII. La Fayette returns to the United States. XIX. Renewed efforts for the Defence of the Country. XX. Arrival of the French Fleet and Army-Plans consequent thereon. XXI. Treason of Arnold. XXII. American Army retires into winter quarters. XXIII. European combinations against Great Britain. XXIV. Revolt of the Pennsylvania line-of the Jersey line-Discontent of the Inhabitants of New Jersey. XXV. Gloomy Prospect for the year 1781. XXVI. Combined Operations of the French Fleet and Allied Armies, against Cornwallis-His Capture.XXVII. New London taken and burned by Arnold. XXVIII. Condition of the Country for the Campaign of 1782-Resolutions of the British Parliament in favour of Peace. XXIX. Malignity of the Tories-Murder of Captain Huddy. XXX. Cessation of Hostilities-Treaty of Peace. XXXI. Disbanding of the Army. XXXII. Public Entry of Washington to New York-takes leave of his Officers-Surrenders his Commission to Congress....... 294 Xii CONTENTS. CHAPTER XVIII. I. Peculiar sufferings of the State of New Jersey from the War. II. Laws in New Jersey relative to the Militia. III. Council of Safety. IV. Military efforts of New Jersey. V. State Representatives in Congress. VI. Establishment of the New Jersey Gazette. VII. Unhappy Condition of the States after the return of Peace. VIII. Inefficiency of the Articles of Confederation-Part of New Jersey in their Adoption. IX. Measures proposed in Congress for maintaining Public Credit-Efforts of New. Jersey upon this subject. X. She resorts to Paper Currency and Loan Office for Relief. XI. Difficulties with Great Britain relative to the Execution of the Treaty. XII. Measures for regulating the Trade of the Union-Result in a Proposition for Revision of the Articles of Confederation. XIII. Adoption of the New Constitution-Ratified by New Jersey 320 THE HISTORY OF NEW JERSEY. CHAPTER I. Comprising Events from the Discovery by Europeans, to the Grant from Charles I. to James Duke of York.-I Ancient and Modern Principles of Colonization.HI. Voyages of the Spaniards and Portuguese upon the East Coast of North America.-III. Voyages of the Italians, Verrazano and the Cabots.-IV. First English Attempts at Discovery.-V. Efforts of Raleigh to establish a Colony.-VI. Gosnold opens a new Road-London and Plymouth Companies created.-VII. Voyages and Discoveries of Hudson.-VIII. Intercourse of the Dutch East India Company with America, and Formation of the Amsterdam Licensed Trading West India Company.-IX. Settlemeiit of the Puritans at iPlymouth.- X. Formation of the Great West India Company in Holland.--X1. Voyage and Proceedings of Cornelius Jacobse Mey.-XII. Measures of' the Company to promote Emigration; Purchases of large Tracts of Land from the Indiains.--XIII. Voyages of De Vries; Colony plapted-The Delaware abandoned by the Dutch.XIV. Minisink Settlements onthe Delaware.-XV. Settlements of the Swedes on the Delaware-first Project of a Colony-first Colony-increase of Settlers.XVI; Colonial Government' established-Colonel Printz first Governor.-XVII. English Settlements upon the Delaware-prostrated by a united Fofce of Dutch and Swedes.-XVIII. Swedish Government under Printz and his Successors.XIX. Swedish Colony subjected by the Dutch.-XX. Dutch Colonial Government on the Delaware-Possessions on the East of New Jersey.-XXI. Account of the English Settlements upon the Delaware previous to 1664-under Patent from Lord Baltimore-under Grant to Sir Edward Ploeyden-by Traders from New Haven. -XXI1. Plans of New England Settlers for Conquest of the Dutch Colonies.-XXIH. Duke of York's Charter from the Crown and Grant to Berkeley and Carteret.-XXItV. Conquest of New Netherlands, by Colonel 'Nicholls.XXV. English Government established on the Delaware.-XXVI. Condition of New Netherlandts at the time of the. Surrender. I. A distinction has frequently been taken between ancient and modern colonization; ascribing the former to military, and the latter to commercial principles. But this classification does not embrace the various species of colonies, in present or past time. A more happy division of the subject would seem t6o be,,into colonies founded by individuals, in their search of happiness; and colonies planted by states, with a view to military or commercial purposes. By the first, our race was originally spread over the face of the globe. It has prevailed at all times, as well among the Egyptians, Athenians, and other ancient people, as among the moderns, who instituted the communities of the North American confederacy. The early Greek colonies, generally, sprung from the desire of the citizens to ameliorate their condition; and the immediate impulse was, excess of population, the ambition of chiefs, the love of liberty, or contagious and frequent maladies. The bonds of filiatiot connected the colony with the parent state; and the endearing names of daughter, sister and mother, sanctioned and preserved the alliances between them. But in the Grecian colonies of latter date, we trace commercial and political views. The Carthaginians, also, seem to have established colonies upon commercial principles; and two treaties, recorded A 2 HISTORY OF NEW JERSEY. by Polybius,* between them and the Romans, are in the true spirit of modern colonial policy. On the other hand, the Roman colonies were military establishments, designed to maintain or extend their conquests; and their agrarian allotments, to disbanded veterans and discontented and clamorous citizens, partook of the same character. Commercial motives seem rarely to have blended with the policy of these haughty conquerors. Such, also, in more recent days were the colonies of the Normans, in England, France, and the south of Europe; of the English, in Ireland and Indostan; of the Portuguese and Dutch in either India; and of a portion of the Spanish settlements in the New, World. In general, the civil colonies of the ancients were independent of the authority of the parent state; though, necessarily, influenced by the ties of charity which connected them with her. But, modern history, we believe, furnishes no instance of a colony independent in its inception; unless the short-lived religious communities of the Jesuits, in America, and of the Moravians in the northern parts of both continents, be so considered. The colonies of the western hemisphere were, generally, commenced under the sanction of, and in dependence upon, some European state. Even the ascetic Brownists, in their torpid settlement of New Plymouth, began their labours under the auspices of James I. of England: and though for some years, they were unnoticed by the crown, they claimed and enjoyed the protection due to English subjects. The colonization of America was prompted and directed by various passions. The Spaniards and Portuguese were inspired by visions of sudden wealth, by the love of that fame which chivalric adventure gave, and by an apostolic desire of spreading their religious faith among the heathen. The founders of states in the northern cqntinent, were actuated by more sober, but not dissimilar views. Raleigh and his associates sought wealth and reputation, by extending the power and fame of their mistress and their country; and the provincial proprietaries, holders of large grants from the crown, were excited by ambition and avarice; which in Calvert and Penn, at least, were blended with a noble philanthropy, delighting to assure religious and civil liberty to their associates and their successors. The subgrantees and settlers who subdued the wilderness, came with great diversity of purpose. Many fled from religious, some, from political persecution; but, the larger portion was induced by that well founded hope of ameliorating the condition of themselves and their posterity, which flowed from the unrestrictr.ed possession of a rich and virgin soil, in whose fruits they were protected, against lawful and lawless violence. The religious instruction of the savage is a condition of every royal grant; and afforded to the grantor, doubtless, a full extenuation of the injustice of invasion. The extensive grant of Charles II. to his brother, of York, was moved by political causes, and designed, probably, also, to reward the services of others, which he could not, in a different manner, acknowledge. The immediate grantees of the Duke, were wise enough to see, that their interest lay in the adoption of the most liberal principles of political association, which circumstances would permit; and these circumstances were most favorable, to civil and religious liberty. The period in which the foundations of the Anglo-American colonies were laid, was rife with events, which, sowed the indestructible seeds, and reared into strength the scions of human liberty. The integrity and infallibility of clerical power, had been shaken to pieces by Luther and Calvin; and the divinity of kings had expired with the unhappy Charles. The religious contests, and the transition of power from one religious sect to another, * Lib. iii. c. 22. HISTORY OF NEW JERSEY. 8 had taught to Catholic and Protestant, the advantages, if not the necessity, of religious toleration. Letters, the cause and power of religious freedom, had been equally serviceable to civil liberty; and the great truth which, for ages, had laid buried in the ruins of civilization, beneath sacerdotal palaces and prisons, and the gothic gorgeousness of the feudal system,-the great truth, that political power belonged to, and was made for, the people, had been rediscovered-was proclaimed abroad, and had become generally understood among men-among Englishmen. That truthl had wrenched the sceptre from the grasp of an obstinate and bigoted despot, and borne him to the block-had overthrown a monarchy and created a republic; and because of the abuse of republican forms, had again established a throne. Religious and political freedom were in England terms as familiar as household words, and enforced, even from the hate of her princes, the most profound respect. It was vain, therefore, to think of the formation of new political societies, without adverting to, and securing these great essentials. Kings and proprietaries, who would establish colonies, were compelled to stipulate for religious toleration, and legislative power in the people. Hence, the first Charles, who abominated a parliament, required the proprietary, Calvert, to obtain all subsidies, by the assent of the people-hence, the second Charles introduced the same principle, in the grant of Pennsylvania-hence, they, and the Carterets, and the Berkeleys, and the minor Proprietaries, were compelled to their liberal charters. All were results of improvement in the moral condition of our species, which individuals might promote, but could scarce retard. We are guilty, therefore, of the worst species of idolatry-of man-worship, when we give to individuals the praise of creating measures, of which they could'only be the servants.. Our plaudits for their concurrence in the good work, are, however, due; and should be frankly and fully paid, as the just incentive to virtuous actions. In this spirit, we adopt the expressions of a late writer upon colonial history:-" A North American may feel grateful exultation in avowing himself the native of no ignoble land-but of a land which has yielded as great an increase of glory to God, and happiness to man, as any other portioi of the world, since the first syllable of recorded time, has had the honour of producing. A nobler model of human character could hardly be proposed to the inhabitants of the North American States, than that which their own early history supplies. It is, at once, their interest and their honour, to preserve, with sacred care, a model so richly fraught, with the instructions of wisdom and the incitements of duty."* No portion of the history of this' great country is more filled with cause for this "grateful exultation," than the State of New Jersey-none can boast greater purity in its origin-none more wisdom, more happiness in its growth. To develope her unpretending, but instructive story, is the object of the following pages; in which, however, we must, necessarily, blend a portion of that of the adjacent states, which for half a century were identified with her. II. Soon after the discovery of America, by Columbus, the Spaniards and Portuguese explored the northern Atlantic coast, as high as Labrador; to which, the latter gave its (present name. As they approached 'by the West Indies, they may have visited the shores of the Delaware and Hudson rivers; but possessed of the fine climates, and richer countries of the south, they had no inducement to make permanent settlements in regions less attractive. Florida' was occupied by the Spaniards, in 1512; and its boundaries, as * Grahame's History of the American Colonies. 4 HISTORY OF NEW JERSEY. given by the charter of Philip II. to Menendez, extended from Newfoundland to the 22d degree of northern latitude. III. To the genius of the Italian navigators, the world is deeply indebted, as well for the early exploration, as for the discovery, of America. John de Verrazano, and the enterprising and skilfulCabots, were the worthy successors of Columbus and Americus Vespucius. Verrazano, whilst in the service of Francis I. of France, visited, it is supposed, the bay of New York.* It is certain, that, in 1523,'he coasted the American continent, from the 30th to the 50th degree of north latitude, landing and communicating with the natives in several places; and that by virtue of discoveries made by him, and some French navigators, Henry IV. gave to Des Monts, the lands lying between the 40th and 46th degrees of north latitude.t The loss of Verrazano, with his vessel and crew, on a subsequent voyage, (1524) procrastinated, for ten years, the efforts of the French to establish colonies in America. The voyages and discoveries of Quartier, in 1535, directed their attention, particularly, to the shores of the bay and river of St. Lawrence. IV. Under the patronage of Henry VII. of England, Sebastian Cabot discovered the islands of Newfoundland and St. Johns, and explored the coast of the continent, from the 38th to the 67th degree of north latitude4, But no fruit was, immediately, derived from his labours. During the reigns of the voluptuary, Henry VIII., of his son, Edward VI., and daughter, the bigoted Mary, no effort was made to prosecute these interesting discoveries. It was reserved for the maritime enterprise of Elizabeth's reign, to give to the English nation a fuller knowledge of the new world, and a proper sense of the advantages which might be drawn from it. Encouraged by the Earl of Warwick, Martin Frobisher, in three successive voyages, visited the shores of Labrador and Greenland.~ Sir Humphrey Gilbert, in 1580, made two unsuccessful attempts to establish a colony in North America, in the last of which, he perished. V. But the fate of Gilbert did not deter his half-brother, Sir Walter Raleigh, alike distinguished for 'his genius and courage, from pursuing the same object; which, indeed, had taken strong hold of the affections of the principal men of the kingdom. He formed a company, under a charter, obtained from the queen,II granting them all the lands they-should discover between the 33d and 40th degrees of north latitude. Two vessels despatched by them, under captains Armidas and Barlow,"* visited Pamptico Sound, and, Roanoke Bay; and on their return, reported so favourably of the beauty and fertility of the country, that the company were excited to new exertions; and Elizabeth gave, to the newly discovered region, the name of Virginia, as a memorial that it was discovered in the reign of a virgin queen. But the subsequent efforts of this company proved abortive. A colony was, indeed, planted at Roanoke, in 1585; but, having been reduced to distress by the delay of supplies, they returned to Europe, in the following year, with Sir Francis Drake; who touched at their island on his way home, from a successful cruise against the Spaniards. Undiscouraged by this ill success, Raleigh despatched another colony to the same place, under the direction of captain John White,tt which perished by famine, or the sword of the natives; having been deprived, by the preparations of the Spaniards, for invading England, of the succour which White had returned to seek. * Dr. Miller's Discourse, 1 vol.--N. Y. Historical Collection. t 2 Hackluyt's, 1. N. Y. Historical Collection. Williamsoi's History of North Carolina, vol. i. 15. Moulton's History of New York, vol: i. 134. t 1498.1 A Mr. Hare is said to have followed Cabot, and to have brought to Henry VIII, some Indians from North America. ~ In 1576, 1577, 1678. 1I 26th March, 1584. * Sailed, 27th April, returned, 15th September, 1584. tt March, 1590. HISTORY OF NEW JERSEY.,5 5 VI. Between the years 1590 and 1603, the English do not appear to have made any voyage for thi^purpose of settlement. In the latter year, Bartholomew Gosnold, abandofning the circuitous route hitherto pursued by all navigators, discovered, by steering due west, a more direct course to the northern continent. He visited, and gave names to Cape Cod, and the islands of Elizabeth, and Martha's Vineyard; and taught his countrymen, that there were many attractions, far north of the lands they had attempted to colonize. His favourable reports, at first disbelieved, were confirmed by persons who sailed, thither, in the service of some merchants of Bristol, the Earl of Southampton, and Lord Arundel, of Wardour. By the zeal of Richard Hackluyt, prebendary of Westminster, to whom England was more indebted than to any man of his age, for her American possessions, an association, embracing men of rank and men of business, was formed, with a view to colonization.* To this company, James I., on the 10th of April, 1606, granted letters patent, dividing that portion of the continent which stretches from the 34th to the 46th degrees of north latitude, into two, nearly equal, districts. The one, called the first, or south colony of Virginia, was allotted to Sir Thomas Gates, Richard Hackluyt, and their associates, mostly residents of London; the other, to sundry knights, gentlemen and merchants, of Bristol, Plymouth, and other parts of the west of England. Each company was empowered to appropriate to itself, fifty miles each way, along the coast, from the point of its settlement, and one hundred miles of interior extent. From the places at which the colonial councils were respectively established, were derived the titles of the London and Plymouth Colonies.t" Under this and another charter, to the Plymouth company, given in 1620, whose, provisions were not the most friendly to political freedom, nor the best adapted to promote the objects for which they were designed, the permanent settlement of Virginia and New England was commenced and prosecuted. It forms, however, no part of our present plan, to trace the various fortune which attended their growth, from weak and sickly plants, to deeprooted and umbrageous trees. VII. The hope of discovering a north-west passage from Europe to Asia, which no disappointment seems to have power to extinguish, was the motive of several voyages made by Henry Hudson, a distinguished English mariner. In his third voyage, failing to open a northern route, he explored the eastern coast of America, with the view of determining, whether a passage, to the Pacific Ocean, might not be found through the continent.4 He ranr down the coast, from Newfoundland, to 350 41', northern latitude; and,returning by the same course, entered the Delaware bay, on the 28th of August, 1609,but finding the water shoal, and the channel impeded by bars of sand, he did not venture to explore it. Following the eastern shore of New Jersey, he anchored his ship, the Half-Moon, on the 3d of September, within Sandy Hook. He spent a week in examining the neighbouring shores, and in communication with the natives; during which, one of his seamen, named John Coleman, was killed. The boat in which he and several others had passed the Kills, between Bergen Neck and Staten Island, being attacked by two canoes, carrying twenty-six Indians, the unfortunate sailor was shot, by an arrow, through the throat. Thus it would seem, that in the intercourse * 2 Purchas, 5. Belknap's American Biography.-N. A. R., (new series) vol. vi. p. 36. f Modern Universal History, vol. xxx. Hazard's State Papers, 1. Stith, Beverly, Robertson. t Voyages undertaken by the Dutch East India Company. Hudsoc's Journal. Purchas, I-N. Y. Hist. Col. 81, 162. 6 HISTORY OF NEW JERSEY. between the European and Indian, in this part of America, the Indian committed the first homicide. The shores of the Delaware and Raritan bays were, probably, the first lands of the middle States trodden by European feet. On the 12th of September, Hudson entered New York Bay, through the Narrows. He spent the time between that day and the 19th of the same month, in exploring the North river.* He ascended, with his ship, as high as the spot where the city of Albany now stands; and his boat proceeded to the sites of Waterford and Lansingburg. The decreasing volume of the stream, and the shoals which obstructed his further way, depriving him of all hope of reaching the Pacific Ocean by this route, he prepared to retrace his steps. Commencing his return on the 22d of September, heslowly descended the river, and on the 4th day of October, put to sea. He reached England on the 7th of November, 1609. His vessel, and part of the crew, returned- to Holland; but the jealousy of the king, James the First, forbade him, and his English sailors, to revisit that country.t In the following year, Hudson re-entered the service of the London company, in which he had made his two first northern voyages; designing to seek again, a north-west passage, through Davis' Straits; but his crew mutinied, and abandoned him, his only son, and some half-dozen of his men, who continued faithful, to perish amid the fields of ice, in the vicinity of the bay which bears his name.t Whilst in the North river, Hudson had much intercourse with the natives. Near the coast, they were fierce and inimical--at a distance from the sea, mild and hospitable. But the superior power of the Europeans was exercised upon friend and foe without mercy. Of the former, one was shot to death, for a petty theft-and of the latter, nine were more deservedly slain, in an attack which they made upon the vessel. The first visit of the white man, therefore, to the shores of the Hudson, was signalized by the violent death of ten of the aboriginal inhabitants. VIII. The Dutch East India Company, although disappointed in the main design of Hudson's voyage, found in the fur trade he had opened, sufficient inducement to cherish commercial intercourse with the Americans. 'A second voyage, under their authority, in 1610, proving successful, was repeated; but the competition of private adventurers reducing their profits, they endeavoured to monopolize the trade, by a decree of the States-General, granting to all persons who had discovered, or might discover, any bays, rivers, harbours, or countries before unknown, the right, beside other advantages, to the exclusive trade therein, for four successive voyages.~ Under this edict the Amsterdam Licensed Trading rWest India Company was formed; proposing to maintain the acquisitions on the Hudson and to explore the circumjacent country. In the service of this company, Adrian Blok and Hendrick Christianse sailed in the year 1614. Blok arrived first at Mannahattan, where, his ship having been accidentally burned, he built a small vessel, with which he passed into Long IslaAd Sound. He fell in with Christianse near Cape Cod. Together, they discovered Rhode Island and Connecticut river; and proceeding to Mannahattan Bay, they erected a fort on Castle Island, and four dwellings on the Greater Island. In the preceding year, a small trading house was built upon an island below Albany; and in the following, a redoubt was thrown up on the right bank of the river, probably, at the present Jersey City * Hudson's Journal. See Note (A.)-Appendix. t Lambrechsten, Moulton, Ebeling. t June 21, 1611. ~ De Laet, March 27, 1614; or as it is said 1611, 1612. Moulton, 340. HISTORY OF NEW JERSEY. 7 Point.* The most important event of this period, however, was the alliance by formal treaty, between the Dutch and the Five Nation confederacy of Indians; at the execution of which, it is supposed, the Lenape tribes were also present, and by the united instances of the Dutch and Iroquois, consented to the fatal assumption of the character of the woman, in the manner we shall narrate hereafter.t The Hollanders, directing their efforts at colonization, to their Asiatic, African and South American possessions, and restrained, perhaps, by the claim of the English, to the greater part of North America, had hitherto made little effort to people the shores of the Hudson. It has been asserted, however, that between the years 1617 and 1620, settlements were made at Bergen, in New Jersey, in the vicinage of the Esopus Indians, and at Schenectady; and it would seem, that Sir Thomas Dale and Sir Samuel Argal, in the year 1614, returning from an expedition against the French at Acadie, visited Mannahattan, and compelled the Dutch to acknowledge the English title, and to contribute to the payment of the expenses of their voyage. It would further seem, from the authorities cited in the margin, but which should be received with some allowance, that in 1620, the Dutch West Indian Company, upon application to James the First, of England, obtained leave to build some cottages upon the Hudson river, for the convenience of the ships, touching there for fresh water and provisions, in their voyage to Brazil; under colour of which license, the company established a colony; and that, upon complaint to Charles I. of these proceedings, he remonstrated with the States-General, who disowned the acts of the company.4 IX. But, although the Dutch did not immediately, themselves, colonize the New Netherlands, (the name given to the country from the Delaware Bay to Cape Cod,) they were well disposed to aid others in such design; encouraging the Puritans, who, under the care of the Rev. John Robinson, had fled to, the low countries from England, to seek a safe and more commodious asylum in the New World; notwithstanding these sectarians avowed an intention to preserve their national character, and to hold the title for the lands they should inhabit, in dependence on the English government. This germ of the Plymouth colony, planted in 1620, was designed for the country between New York Bay and the western line of Connecticut. But the season at which the adventurers arrived on the coast, adverse winds and currents, with the discovery of a portion of the country, whence the aborigines had been lately swept, providentially, as the pilgrims supposed, by pestilence, induced them to land at a place, they termed Plymouth.~ The allegation, therefore, that Capt. Jones, with whom they sailed, had faithlessly, in consequence of a bribe from the Dutch, landed them at a distance from the Hudson, is not entitled to credence. X. In 1621 the great West India Company was formed in Holland, and endowed with the wealth and power of the States-General. The Licensed Trading Company which had hitherto conducted commercial operations in the Hudson, confining themselves to one river and a small portion of the coast, was merged in the new company, to whom we may properly ascribe the first efforts of the Dutch to plant colonies in North America.l1 They immediately despatched a number of settlers duly provided with the means of subsistence, trade, and defence, under the command of Cornelius * De Laet, Moulton. t Heckewelder. t Beauchamp Plantagenet's description of New Albion-Moulton-British Empire in Aimerica-Ogilby's America-Elizabethtown Bill in Chancery. ~ Robertson. Dudley's letter. Moulton. |j See charter of this company in Hazard's Col. 8 HISTORY OF NEW JERSEY. Jacobse Mey; who, with more enterprise and industry than his predecessors, visited the coast from Cape Cod to the Delaware river, where he proposed to establish his own residence. He called the bay of New York, Port May; that of the Delaware, New Port May; its northern cape, Cape May; and its southern, Cape Cornelius. He built Fort Nassau at Techaacho, upon Sas. sackon, now Timber Creek, which empties into the Delaware, a few miles below the city of Camden. During the same year the forts New Amsterdam and Orange, were also erected upon the sites, of the now great cities, of New York and Albany. The administration of the affairs of New Netherlands, was committed to Peter Minuit; with whom came a colony of Walloons, who settled, 1624-5, at the Walbocht, a bend of the Long Island shore, opposite to New Amsterdam. In 1626, Minuit opened a friendly and commercial intercourse with the Plymouth pilgrims; and prosecuted the fur trade with great advantage to the company. XII. In 1629 the West India Company endeavoured to excite individual enterprise, to colonize the country; granting by charter to the patroon or founder of,a settlement, exclusive property, in large tracts of land, with extensive manorial and seignorial rights.* Thus encouraged, several of the directors, for whose use, probably, the charter was designed, among whom Goodyn, Bloemart, Pauuw and Van Renselaer were most distinguished, resolved to make large territorial acquisitions; and they sent out Wooter Van Twiller, of Niewer Kerck, a clerk of the Amsterdam department, of the company, to assume the management of its public affairs, and to select lands for the individual directors. One of the three ships which came over in 1629, visited an Indian village on the south-west corner of Delaware Bay; and the agents on board, purchased from the three chiefs of the resident tribe, in behalf of the Herr Goodyn, a tract of land, extending from Cape Henloop, in length thirtytwo, and breadth two, English miles. In the succeeding year, several other extensive tracts were purchased; for Goodyn and Bloemart, of nine Indian chiefs, sixteen miles square, on the peninsula of Cape May; for the director Pauuw, Staten Island, and a large plat on the western side of the Hudson, in the neighbourhood of Hoboken; and for Van Renselaer, a considerable territory, along the Hudson, in the vicinity of Fort Orange.t The impolicy of these great and exclusive appropriations was, subsequently, discovered and condemned; and their ratification seems to have been obtained, only, by admitting other directors to participate in them. XIII. In prosecution of their plans, these directors formed an association,.to which they admitted, on equal terms, David Pieterson de Vries, an experienced and enterprising navigator. Their immediate object was to colonize the Delaware river, to plant tobacco and grain, and to establish a whale and sea) fishery. The command of the vessel appointed to carry out the colonists was given to De Vries; who left the Texel on the 12th Dec. 1630, and arrived in the Delaware bay in the course of the winter. The country was deserted by the Europeans, who had preceded him. Fort Nassau was in possession of the Indians; Captain Mey having left it, bearing with him the affectionate regrets of the natives, who long cherished his memory. De Vries selected a spot for his settlement, on Lewis Creek, called by the Dutch, on account of the prostitution of the Indian women here, Hoornekill; where, unimpeded by the season, which was uncommonly mild, he erected a trading * See the charter in Moulton's History of New York. t See Moulton's History of New York. The territory of Goodyn was denominated Swanwendael; that of Pauuw, Pavonia; and that of Van Renselaer, Renselaerwick HISTORY OF NEW JERSEY. 9 house and fort, giving it the name of Oplandt. The whole plantation, within Goodyn's purchase, extended to the Liftle Tree Corner or Boompjes' Hoek.* Returning to Holland, he committed his infant colony to the care of one Giles Osset; who, in evidence of the claim and possession of the Dutch, set up the arms of the States-General, painted on tin, upon a column, in some conspicuous station. An Indian, ignorant of the object of this exhibition, appropriated the honoured symbol to his own use. The folly of the commandant construed the trespass into a grievous national insult, and he became so importunate for redress, that the harassed and perplexed tribe brought him the head of the offender. This was a result which Osset had neither wished nor foreseen, and he should justly have dreaded its consequences. In vain he reprehended the severity of the Indians, and assured them that had they brought the delinquent to him, he would have suffered a reprimand only. Though the death of the culprit had been doomed and executed by his own tribe, they beheld its cause in the exaction of the strangers, and with the vindictiveness of their character, sought a dire retribution. At a season when the greater part of the garrison was engaged in field labour, distant from the fort, the Indians entered it, under the pretence of trade, and murdered the unsuspicious Osset with the single sentinel who attended him. Thence, proceeding to the fields, they massacred every other colonist, whilst tendering to them the usual friendly salutations. This conduct, with its extenuating circumstances, as related by the aborigines themselves to De Vries, is sufficiently atrocious; but it is highly probable, that the desire of the white man's wealth was as powerful a stimulant to violence as the thirst for vengeance. In December, 1632, De Vries returned from Holland, to mourn over the unburied bodies of his friends, and the ashes of their dwelling. Attracted by the firing of cannon, the savages approached his vessel with guilty hesitation;. but at length, summoned courage to venture on board, and to detail the circumstances we have narrated. The object which De Vries had in view, led him to seek reconciliation; and he was compelled to pardon, where he could not safely punish. He formed a new treaty with the Indians; and in order to obtain provisions, ascended the river above Fort Nassau, where he narrowly escaped from the perfidy of the natives,. Pretending to comply with his request, they directed him to enter Timmerkill or Cooper's Creek, which furnished a convenient place for attack; but, the interposition of an Indian woman, so often recorded in favour of the whites, saved him from destruction. She warned him of the design of her countrymen, and that a crew of a vessel (supposed from Virginia) had been there murdered. In the mean time, Fort Nassau was filled with savages, and on the return of De Vries, forty boarded his vessel, whom he compelled to retreat; declaring that the Manitou or Great Spirit, had revealed their wickedness. But, subsequently,, with the humane and pacific policy which distinguished him, he consented to their wishes of forming a treaty of amity; which they confirmed with customary presents, declining his gifts, however, saying, that they did not now give with the view of a return.f Disappointed in obtaining provisions, De Vries, leaving part of his crew in the bay, proceeded to Virginia; where, as the first visiter from New Netherlands, he was kindly received and his wants supplied. Upon his return to the Delaware, finding the whale fishery unsuccessful, he hastened his departure, and with the other colonists proceeded to Holland, by the way of Fort Amsterdam. Thus, at the expiration of * Corrupted into Bombay Hook. De Vries, Moulton. t De Vries' Journal. Moulton. B 10 HISTORY OF NEW JERSEY. twenty-five years from the discovery of the Delaware Bay, by Hudson, not a single European remained upon its shores. XIV. It is possible, however, that the Minisink settlements- on the river, above the Blue Mountain, were made at or near this period. They extend forty miles on both sides of the river, and the tradition, as rendered by Nicholas Depuis, a descendant of an original settler is; " That, in some for"mer age, there came a company of miners from Holland, supposed to have "been rich and great people, from the labour they bestowed in opening two " mines-one on the Delaware, where the mountain nearly approaches the "lower point of Pahaquarry Flat, the other, at the north foot of some moun