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Les cartes, planches, tsbieaux, etc., peuvent Atre filmte A des taux de reduction diffArents. Lorsque le document est trop grand pour Atre reproduit en un seul clich6, 11 est film* A partir de I'angle supArieur gauche, de gauche h drolte, et de haut en bas, en prenant le nombre d'images nAcessaire. Les diagrammes suivants illustrent la mAthode. 1 2 3 4 6 6 C' \ X, -1K- '■mm M •/ \ \, L'>«l U: no iiK C^ • • t?r i? 1/ \. >•- CKK lOU Ilf> I;.')) lAO 11'" rrAr/nyiW a c= "■ T N.^ I hu):ksj riiiiHifii 1. IV llarrtw ¥ ■ '■■* ItftI litO KtO LW IKO "O / / ■f. ■w\ V u I ' ) f^^ MISSION OV TIIK NORTH AMERICAN PEOPLE, GEOGRAPHICAL, SOCIAL, AND POLITICAL. ILLUSTRATED BY SIX (HARTS DELINEATING THE TIIYSICAL ARCIIITECTURE AND THERMAL LAWS OF ALL THE CONTINENTS. BY WILLIAM GILPIN, I.ATK GOVKItXOIl OP COLOH.VDO. P H I L A D E li P n I A : J. B. LIPPIXCOTT & CO. 1873. J.//,S-^"2' Entered, aceorilinj; to Act of Coii(;i'eci<, in the year ISTJ!, by WILLIAM (ill-l'IX, In the Office of tlie Liliniiiiin of I^Jii^^rc.'s at \Vii>hiii;;l()n. DeN'VEB, Juill INTRODUCTION. This voluiiu! is tlic nprodiittion nf its i)reclcceHHor, which nppcareil in IHIIO. Tiiis short interval, aitliinij;h olieciicred by war, is ilhmiinated by stupendous achievements in the direction wliithcr the encrj^ies of the people were invited. The vivacity with which hdor, intcUij^encc, and n'oderation, in concert and ulliance, march and expand in force and volume, is amazinj; and <;;lorious. Nothinjr in sijrht jiredicts any serious check to this fufal flood, on which is borne every department and detail of I'ltodUESS. The aim hcj'e is to {?rasp facts as they arc ; to reject delusions which have grown senile. No special chapter is here assigned I :> the Wcstmi Cvrv\ Nditc — lia.^in uftlio Culdiacld— Canon of the Colo- rado — liasiii of the Salt Lake — l>asin of tlio Coliiiiiliia — llasiii of !•' razor's Hivi'r — DeliciiHis Cliinatc of the I'laloau — ^Its Ki'riility — Coiilillcra of tlu' Aiiili's — Pacific .Maritiiiio Kroiit 1.') CIIArTKK II. THE CORDILLERA OF THE SIERRA MADRE — THE EASTERN CORDILLERA. LLiAM Gilpin. M'Uiitain S_\ ritom of tin- (lloln — Tlu' Andes — Tlu'ir Icnjrth. aKitmle. unci aiirilVrous vealtli — Chain of the Mollicr .Monntain — Its Uivcrs — Caiions — Mesas — liules — jlanos — liiiyoiis or Pares — Klcvation — lireadth — Wiml lUver Moiintiiin — South )ass — Tlic Alps and their ])ass — Lava IMain of Snake Kiver — liowl of the Yel- Iwstone — Plain of tlie South Pass — Sweetwater lliver — Tahle iMouutain — Pla- ors of jjolcl and |ireeious stones^Xortlu'ru Pare or Bull-iien — Favorite winter liuue of tra)i|iers — Streams, meadows, flowers, i;roves, ete. — .Middle Pare — M)uutain simrs. rocky streams, cloudy atinos|ihere, snow-clail summits — liOUfj's Puk — Southern Pare — Pike's Peak — Mountain harrier — Xo transit — liayou Pm Luis — Suhlinie scenery, luxuriant fertility, ajjricultural seasons — Valley of Cashmere — Secondary mesas, or '• LIiiuiih" — Levid surface, jioor soil, rainless atiiivsidiere — -Perjdexity of [uililic mind — Llano Kslacado and Llano of the lial- sifcta — A continual terrace — Kansas Basin 21 CHAPTER III. THE PLATEAU OF NORTH AMERICA. rts area nd chnrnetorislies — The column of central iiro<,'ress — Plateaux of tlie OM AVorld-PIateau of American Talile Lands not underst(vod — Its basins — Climaf." uniforlly vernal— Fertility of soil— (Jrasses nnike natural hay — Immense herds f cattle — Auriferous f,'ranite and }rold placers — Irrijration — I'repared for an mmediate dense population — Its physical characteristics — (U'olojrical formatiii— Mineralogical resources— Zone id' civilization — Lino (d' progress 10 TABLE OF COX TEXTS. CIIArTKR IV. THE SilEKRA SAX JUA.V. VKQT. Till' gdlil mill silver ]ini(hicliiiii of tlio wmlil — AiirifciMiis or i;i)lil-l)caring forinn- tinii — ChIi'iiiciius I'liiiiiiitioii — Iniii, ciiiiiicr, Icml — KimmI I'liliiiiiiiitinns of thi; Sii'iia Mailn — Pike's I'lak — Tlu- Sirna Miinlni's — Miinn;; in thi" AinlfS — Slii|icMilcins ffl'futs iif till' inti'iiial vult-aiiir iiuwcr.-' of llii' j^lolii' — Aljiiiiilanci' of tliu ]irci.'ii)iis iiii'lals — (.'afmii of the ColinaiUi — (iorgcous variety of seenery — I'liiloiiuiiliy of inetiilliferiius ileiiosits — "tireut Xorth Amprieiin iJcHert" does not exist — Itiinibolilt's views — The (iieat IMateau tlie peat of cmjiire of the ancient Jlexieans — Heniaikalile foeal eiilniinatiun of the Siena Minilires in tho Biena San Ji mi — The colunin of jiioneers npon its tliiesliuiil 4-' CIIArTKR V. THE SOITII PASS OF AMKHIfA. Rontc from Paris to Pekin — Distance ami time reiliueil — Tlic Plateau and two Por- ililleras the only im|i"iliments — liasin of the .Mciliserranean and liasin of the JIississi]i|ii — The former .salt water — The hitter rich, calcareou)', iinil iiralilo 8iiil — The former sii]i|iorteil a |io|inhitionof one liniiilreil anil thirty-one millions — The latter cajiahlc- of twelve hnnilreil millions — l!olh the .«eats of cmiiire in their r(s|ieetivc continents — liotli traverseil hy the zmliac of civilization — The South Pass — Its slia]ie, size, ami surface — Distance from Astoria ami St. Louis — The only jiass throu;;li the Mountain Formation hence to Tehuantcjiec — The j^rcnt trail of the butValo |iasse.s throu;;li it — Uiiiiiterrn)itc(l ]iassa}fe hy the bed of great rivers both to the Atlantic and Pacific — I'niforniity of climate from sea to sea — The great Continental line of empire here — The Pillars of Washington 54 CHAPTER YI. THE GHEAT ItASlX ol' THE JllSSISSiri'I. It3 great river — It? surface n r-ch and deep sediment — Its climate — Line of tinibr — Line of grasses — Capacity for ]ioiiulatioi. iJcographical centre of the ]!aui and North American Continent at same point — Hetwcen and e(|nidistinf from the l.'.V.l,Om).non iio|)uhitioii of Kurope and the O.'id.OdO.fKIO population of Asia and Polynesia — Surfaeo of Europe descends outwards trom its cent)! — Also of .\sia — Surface of Xorth America like a bowl, gathering and cenral- izing whatever enters within its rim — The Basin of the Mississijiju the aiuihi- theatre of the world C4 CHAPTER VII. I'ASTORAT, A.MEKIfA. Great Plains of America md deserts — The I'astoral Ciardcn of the woid — Tts surface a gentle slope to the east — Abounds in rivers — Covered witi thick TABLE OF COX TENTS. 11 PAOC. Iicaring forinn- latidiis of tliL' 1 the Andes — -Abmidanee of y of si'i'ner.v — n llcsert" 'Iocs ciniiiri' of tlie Miiii))re» in the nutritious grasses and swarming with animal life — Soil not sandy, hut a flno calcareous mould — Convenient to navigation — (.'limato dry, and temperature even — Herbage perennial, edible, and nutritious throughout the year, and cured into natural hay upon the ground — Sujipnila one huiulicd iiiilUuna of iiild catlle — Xo tires as in j)rairies— Turkeys, chickens, water-fowl, fish, and game in great variety, abundant — Ample proportion of arable land for farms, fuel, building materials, etc.— t'linnite favorable to health an' rtli America — Traufactcd and I'niransactcd Mission of the North American People — Conclusion 117 APPENDIX. MEXICAN WAR. Remarks of Slajor AVilliam Giljjin, at the Barbecue given the Cole Infantrj', at Jefferson City, Thursday, August 10,1847 125 II. SFEECII OF COLONEL WILLIAM CIILI'IX ON THE SUBJECT OF THE PACIFIC RAILWAY. First S]ioken at the Canij) ol' Fin: Thnnmind California Kmigrants at WnhcruHa (now the City of Kawrenee . Kansas, l{e]ieiited at Indejiendence, Missouri, at a Mass Meeting of Ihe Citizens of Jackson County, held November 6, 18411 136 TABLE OF CONTENTS. 13 III. PROCEEDIN(iS OF A MASS MEETING OF THE CITIZENS OF JACKSON COUNTT, PAOE. At Indcpeiidi'iu^o, iin llic .'ith of November, IS 11), to ri'ijioiid to the Action of the Great N'litioniil Hiiilroiid Convention, held in St. Louis on tho V.A\\ day of October, Is 19 165 IV. pike's I'EAK and THE SIERRA SAN JUAN', Extracts fro;i un Address l)y Colonel William (iilpin, delivered at Kansas City, November 15, 1858; on the Gold I'rodnetion of America and the Sierra San Juan 168 V. OEOGRAMIICAL MEMORANDA ON THE PACIFIC RAILROAD. Reproduced from the Pamphlet of 1S50 178 VI. THE nEMP-GROWING REGION. Reproduced from tho Pamphlet of 1856 202 VII. AN ORATION. Spoken by Honorable William Gilpin, to tho Quests of tho Fenian Brotherhood, at Denver, Colorado, July 4, 1868 209 olc Infantry, at OF THE PACIFIC LIST OF MAPS. MAT OF NORTH AMERICA. Hilinpiitinj,' Iho " Momitniii Sy.^tciii" and its d'-tnih, Tlio "Great Calcareous Plain' as a unit, auJ tLu euutiiiuous eiiciiulirij; " Maritime yelvage." II. MAP OF XORTU AMERICA. In which are delineated the "Mountain System" as a unit, The "Great Calcareous Plain" and its dttaiix, and the continuous encircling " Maritime Selvage." III. THERMAL MAP OF NORTH AMERICA. Delineating the Isothermal Zodiac, the Isothermal Axis of Intensity, and its ex- pansions uji and down the " Plateau." IV. MAP ILLUSTRATING THE SYSTEM OF THE PARCS And the domestic relations of the "Great Plains," the " North American Andes," and the Pacific " Maritime Front." Y. MAP OF THE WORLD. Pclineatint; the Contrasted LonijiUnIiiKil and Lntiluiliiial Forms of the Continents, thi Isothermal Zodiac and Axis of Intensity, round the World, and the Line of the Cosmopolitan Railway and its Longitudinal Feeders. YI. MAP OF THE SYSTEM OF THE PARCS OF COLORADO. 14 P s. eat Calcareous Plain" bo "Groat Calcareous Sclvago." ntensity, and its cs- ARCS rth American Andes," ms of the Continent?, , and the Line of the )RADO. * r ^^..J~l~^ — ' .« K.I I U \M> II". III! I ,."> l;ii IJ." I.'(» ll.l no III.*. IttO l»,-| !Mt ll.l (lO 7.'> 70 ll.'. (.o .V. .Hi l.-| hi .1.. C L L r S V C R A^f.^"^ ^ - u u - r . . N u .III ^.^' ,^.,J '• (/"•I ii.i»iU / N H r M f V o N 1 >.•!»' 1 J » .. I r ' Pis XJ^'--^ •*VJ »rV- '■^Vir*.^— .*■ ft ■"^■*WWBKIJfJ!«5SiS£i« ■aill—illiiii ii'iik^. of our sl'oteh w This IS I appi degree occupy, and syiii 3Iorcovei tlieni to graphic recur wli of count! condeiisii guarded TIio ni of its an I'acific THE MISSION 'Si OP T II K NORTH AMERICAN PEOPLE. CHAPTER I. THE iMOUNTAIN FORMATION OF NORTH A.MKUICA — TlIK CORDILLERAS — THE PLATEAU — THE NORTH AMERICAN AXUES. I HAVE elsewhere given a sketch of one of the cardinal subdivisions of our continent and country, the Great Plains. I now proceed to s'.ri'tch what is beyond them, and fills the sjiace out to the Pacific f^ea. This is the immense Mountain Formation of North A.mkrica. I approach the attempt to classify and set down this region with a degree of trepidation which I find it difficult to master. During the years of war and exploration which I have passed among them, every hour has kept alive the awe inspire' by the immensity of the space tlu y occup3', the grandeur of their bidk and altitude, and the sublime order and symmetry which pervade them as a .system, and in the detail.'^. 3Ioreover, no one, not even IIuMnoLDT, has ever attempted to reduce them to a classic system, or assented to what I have done in the hydro- graphic map of 1845. These indelibly-graved impre.ss'ons perpetually recur whenever my memory reverts to that time, and warn me to s| cak of countries so novel to a public little curious and uninformed, only after condensing their portrait with the maturest meditation and with nicely- guarded caution. The mountain formation of Xorth America is that distinct subdivision of its area which occupies the whole space from the Great Plains to the Pacific Sea, and covers two-sevenths of the continent. In its superficial 16 MOVKTAIN FORMATION OF XORTII AMLltlCA, FTC. contents, bulk, nunibor und variety of the niimntaiu niafIadro between Cape Horn and the Arctic Sea. It is lierc that a profound and distressing error pervades all the existing charts and delineations of our continental geography. These, omitting the great Sierra .Madre for (iOO or 700 miles of its Icngtli, and assigning its name to the Sierra Minibres, locate the Rio del Xorte and its vast basin with the .system of Atlantic rivers. Yet the Sierra Mimhres abounds in pedrigals of lava, craters, and volcanic phenomena, and the geological altitude, configuration, and a thousand pal- pal)le characteristic features of the ba.sin of tlie Del Norte, locate thi'm upon the Plateau of the Table Lands. This blunder of transposition is more foolish than to construct a map of Europe and forget the Alps, or to draw for the people a ])ine-trce growing erect in the middle of the ocean, whilst doli)hins graze upon a mountain slope ! The vast basin of the 0el Norte is then tlie third in order of the mountain basins of the Plateau. The Western Cordillera continues to traverse Sonora, and, passing round the Gulf of California, rea])pears in sight of the ocean in the State of California. Opposite San Bernardo another numntain chain branches from its eastern flank, traverses the Table Lands by a northern cour.se, dividing the waters of the Colorado and Great Salt Lake, and plunges into the Sierra Madre between the .sources of Green River and Snake River. This is theyoHr^/t great moiuitain chain of the Table Lands, is 1000 miles in length, and is the Sieura Wasatch. Between it and the Sierra Mimbres is included tlie immense Mountain Basin of tiik Colokado, which is tho fourth subdivisicm of the area of the Table Lands. This basin has an immense area, great altitude, an infinite perplexity of mountains, and is redundant in striking and wonder- ful novelties. The Rio Verde, Rio Grande of the West, and Rio San Juan, collect its upper waters, and, uniting against the inner flank of the Cordillera of the Snowy Andes, gorge it diagonally through and through, and escape into the Gulf of California. This sublime gorge is 557 miles in length, and is known as the " Canon of the Colonido.'' It is through- out a narrow mountain chasm, traversing, without interruption, the very bowels of the Andes, having perpendicular mural .sides, often many thou- sand feet in altitude. Other important aflluents of the Cohn-ado (the Mohabe, the Little Colo- rado, and the Gila) force their way into it by an infinite labyrinth of gorges, similarly scooped through the bowels of the mountain mass. These two remarkable basins, then, — the Del Norte and Colorado, — lie linst the Sierra Mimbres, as a back!) )ne. The waters of tlie first uortre the Eastern Cordillera to the Gulf of Mexico; those of the second the 20 MOfSTMN FOllMAl'lOy OF SOHTIl AMh'ltlVA, ETC. Wt'storii Cortlillora to the Gulf of California ; but no yorjr'e unites them tliiouj,^! the .Siona Miuibn s, wliiuli is uniierfoiatoil. Tlu'si- lia.sin.s arc both lonjiitutlinal in shajic and jiosition ; thoy overlap one another, anii\vth chain of mountains, break- ing oft" from the eastern flank of the Western Cordillera, traverses tlie Table Lands by a due northern course, and sinks into the Eastern Cor- dillera, closely enveloj)ing the sources of the Columbia Iiiver. This is called the Uk?;n.\aua\ ^Iolntains, and divides the waters of the Colnndjia from those of Frazer's Kiver. The Basin of the CoLUiiiUA is the sixth in order of the basins of the Table Lands. It is the most admirable ol" them all. A splendid circular configuration and two primary rivers. Its size, position, and con- figuration, relatively to the Mississijipi Valley and the Pacific Ocean, make it the elite of them all. It extends all across the Table Lands from rim to rim, as do both its great rivers — the Snake Iiiver and the Colum- bia — which, uniting, gorge the Western Cordillera at the Cascades, j)cnc- trating through them to the Pacific in 4(5^ l\)'. They run from east to west, and connect exactly by convenient and single pa.s.ses across tlie East- ern Cordillera, with the great rivers flowing down to tlie Atlantic. It partakes of all the cardinal characteristics of the other basins, liaving, in addition, mighty forests, navigation, a larger share of arable qualities, and a superior economy in its topographical siuface and position. Such are the six primary basins and mountain chains v;hieh checker i IL'/tlt'A, ETC. MOUSTAIN FOliMATION OF XOIITII AMERICA, ETC. 'A IK) j;(H miles in length, accomplishes at once its exit into the maritime region and its descent from the '^Plateau of thr. Tabh: Lands." This gorge, impracticable for common uses, is the only water curnnit by which the Sierra Madre is perforated anywhere between the extremities of the continent. I have elsewhere .spokcM of this canon, together with that of the Colorado and that of the Columbia, as the three remarkable and only water-gaps whereby the plateau discharges its surplus waters to the seas. The Cordilleva of the Sierra Madre enters our territory in latitude 29°, ■ju !.■>! ID MAP OF NORTH xVMERICA ill which ar(MU'liiu'aU>cl IIk' MOUNTAIN SYSTEM ASA UNIl WuiAWAl ( AL( AllKOrSlMAlN and ils DETAILS, f//n/ Ihc t on /inor.s nirirri i n fi MAR VV i .V( i'", v^ b\ i, \\\ I> l-'. . 1 t no 10.-. 26 THE CORDILLERA OF THE SIERRA MADRE. longitude 103°, antl passes beyond the 49th degree, in longitude 114°. Its length, then, witliin these linnts, exceeds IGOO miles. It nuiintain.s an avenige distance from tlie Mississijipi Kiver exceeding 10(10 miles, and has the same distance from the beach of the Pacific Ocean ; it forms, therefore, a continuous sunmiit crest parallel to and midway between them. All the varieties of formation which distinguish the mountain chains of tlie continents here follow one another, or are blended in groups, and exist on a Titanic .scale of magnitude. Mrs(i>i exist, being mountains of immen.se base and perpendicular walls, whose summits have the level surface and smoothness of a table : Bntis, which are conical peaks wrought into perfect .symmetry of contour by the corroding power of the atmosphere: JJimmit crest at the forty-ninth degree, from hence to follow its sinuous 'jdge to the south, to skim from point to point of the .serrated jmitile, and, from this elevation, to extend the vision outward on either flank to where it subsides into the general foundation of the continent. From such a position the eye continually overlooks the " Pfatcau of the Tabic Lands" on the west, the '' Bas'n of (lie Misumijijir on the east. The average elevation of the crest is 12,000 feet above the sea ; that of the broad pediment, from whose longitudinal axis it rises, 0000 feet ; the breadth across is 300 miles; so stupendous in area, bulk, and solidity, is the mass of the Sierra Madre ! Every one has built card houses in childhood, having a second story over the centre ; such a structure illustrates a cross section of the Sierra Madre in its primeval form. This regularity of form has disappeared under the corroding influences 'iA MADIiE. THE CORDILLERA OF TI/E SIERRA MADRE. 27 r the corrodiim' iiifluencca of the atmosphere, operating durinjj; countless ages, and the abrading powers of a tliou.sand rivers, carrying down their attritions to the sea. What is left presents an immense labyrinth of mountain summits, under- mined and channeled to a profound depth by the yawning gorges of the streams. Advancing then along the Mother crest in the direction indicated, the whole eastern flank to the 4;}d° of latitude, and lOOth" of longitude {the Sutitli Push), is striped with the rivers which converge to form the Mis- souri proper and the Yellowstone. These are the 3[ilk Kiver, the Mis- souri, the Wisdom, Jefferson, IMadison, and Gallatin forks, all converging into the Mis.souri ; the Yellowstone proper, the Wind, I'okeagie, and Powder Rivers, all converging into the Yellowstone. These rivers, each having its complement of aflluents, are all of great length, and pour down an immense volume of waters. A very small pro- portion reaches the sea, for where they debouch from the mountains at the lowe.st altitude, these waters are consumed by evaporation, rising to qu'"i'h che thirst of the arid atmosphere and surface of the great prairie ocean. But down the western flank, within the same limits, descend rivers of equal number and magnitude, going to traverse the elevated " liasin of the Cohimhid ;" these are the Columbia proper, the Cottonais, the Fliitbow, Pcnd-oreilles, Spokan, Salmon, and Snake Rivers. These rivers have a more immediate descent to the sea than those upon the east ; the mountain spurs between them are, therefore, more numer- ous, abrupt, and of greater altitude. It is easily discernible that over this serrated crest, whence so many rivers radiate as from u single knife-edge, there are many depressions or passes, liaving every variety of altitude and accessibility. The gorges which lead outward from these passes, all eventually converge to the Mis- souri and to the Columbia. The more southern portion of this mountain crest, where it divides the waters of the Yellowstone and Snake Rivers, and is seen from the great road of the Soutli Pass traveled by our people, has the local name of "Wind River Mountain." Tlie mountain crest, curving to the east, and describing a semicircle, envelops the whole basin of the Yellowstone as in a ciit-(Ir-s(u; and, subsiding gradually in altitude, disappears upon the bank of the Mis.souri. It is by this jteculiar configuration that the mountain crest here practi- cally disajipears, and leaves the open depression of die South Phhh, into which we gain access by the Sweetwater on the east, and by Snake River on the west, pa.ssing, by this means, coun)letely around the arc described by the Wind River Mountain crest. 28 THE CORDILLERA OF THE SIERRA MADRE. A similar configuration to this exists, on a small scale, in the Alps dividing France fifim Italy, which may be mentioned here on account of the aptness of the illustration and the familiarity with which history has for twenty centuries invested it. It is where the Alpine crest, under the successive names of Savoy Alps, IMount Ccnis, and Maritime Alps, sweeps round in a regular arc from Geneva to Genoa, and thence subsiding into the Apennines, bisects Italy lengthwise to the sea. Within this arc is embraced the basin of the Po, oalled once Liguria, but now Piedmont. Around this arc marched the armies of Brennus and Hannibal ; those of the Romans passing into Gaul by the plain of the Rhone ; and here also still pass the armies and people of France and the modern J]uropeans. Upon Snake River is developed the most northern of the pares. As thi;. river descends from the Sierra Mndre, it debouches into and bisects an immense plain of the most novel and remarkable features. This is the Lara Plain. It is an elliptical bowl, embraced between the Salmon River and Snake River Mountains, 325 miles in length and 95 in breadth. It is a uniform pedrigal or flat surface of vitrified basalt, melted by volcanic fires, and congealed as into a lake of cast iron. Along its longitudinal axis stand isolated peaks, known as the '• Three Butes " which erect themselves to the snow line, like volcanic cones pro- truding above the sea. Cracks of profound depth traverse this plain, whose blasted surface is without vegetation or water. It is traversed beneath by subterranean streams, which issue from natural tunnels in the wall of Snake River, plunging into its bed by magnificent cascades. Bald nakedness, rather than sterility, is the extreme characteristic of this \Tonderful plain, which has around i\s rim a fringe of little " oases" upon the streams bubbling from the mountain base, of exquisite fertility and of the most perfect romantic beauty. When we call to memory the interest attracted in every age to the diminutive formations of crystalline basalt upon the north of Ireland, near the city of jMcxico, and in Southern Italy, we are struck with awe at the repetition here of these same phenomena, on a scale of stupendous grandeur. Upon the alternate flank of the Sierra Madrc, the bowl of the Yellow- stone properly classifies itself as the second in order of the pares, having its oval ft)rm streaked longitudinally with many parallel and narrow moun- tain ridges gorged by parallel rivers. This pare is very fertile, of the grandest scenery, and a delightful climate. Such is a partial sketch of the Cordillera of the Sierra Madre, from the 49th° to the 4i{d° of latitude. .V few denominating features only are I A MA DUE. THE CORDILLERA OF THE SIERRA MADRE. 29 pointed out ; the serrateJ crests, altenuitoly rising into peaks and mesas above the snows, and depressed by passes ; tlie flanks gorged by descend- ing rivers or branching out into mountain spurs between them — the pares; the general direction is south-southeast. I omit to speak of the regions around the liigher sources of the Mis- souri and Columbia, and still onward to the noi-th, not because they are less interesting and attractive, but because I have not myself seen them, and because they are of identical features, and are as yet remote from the coUunn of progressing empire. The third Jim c is the plain of the South Pass. Although adjacent to the other two, it is in perfect contrast to them in all its characteristic features. Its surface of clay has the perfect smoothness of a water plain, over which tlie eye ranges without interruption, llain is rare, and the vegetation of grass and artcmisia .scanty and uniform. Upon its south front rises again the Cordillera, under the local name of Table Mountain. This forms an immense arc, similar to the Wind Kiver Mountain, but in the opposite direction, for, turning to the southwest, it subsides to the Rio Verde, which is the great Colorado. These two arcs approach one another within thirty miles, forming a double corner over the gorge through which the Sweetwater escapes. To mark the conti- nuity of the mothei crest, a gentle crown traverses the plain from one mountain corner to the other, only traceable by tb-^ perfect division which it makes between the waters of the Atlantic and Pacific Oceans. In the Table Mountiiin the ConU/leni rises agiiin. It resumes its direc- tion, configuration, and altitude, which it preserves with uninterrupted uniformity clear through the continent to Tehuantepec. As far as the 38th degree of latitude it sheds the waters of the greo.t Colorado from its western flank ; those of the Platte and Arkansas Rivers from its eastern flank. I am admonished here to pause and fix attention on the number, gran- deur, and variety of the physical elements combined around this culmi- nating ] oint of the mountains and the rivers of our continent. Nature liere, more perfectly than at any other point upon the globe, unites into one grand coup-iVml all her grandest features, which, liaimo- niously grouped, present to the mind a combination of superlative sub- limity. These contrasted pares, so different, yet so close together ! the intense massiveness of the Cordillera ! the number and proximity of great rivers ! the brilliancy and .serenity of the atmosphere in which they shine ! the awful storms whicli at long intervals brew among and shatter the iced mountain tops ! the graphic conviction ever present to the mind of the immediate presence and presiding omnipotence of the Creator ! 30 THE COnniLLERA OF THE SIEItliA MADUE. The impression left with mo, ami made by the peculiar irrit and appear- ance of the soil which overlays the plain of the South l*ass. is of a '• placer of kaoline," resembling- the biscuit from which porcelain is burned. This is disintegrated, and washed down from the bald mountain flanks of porj)hyritic jxranite. Whether there may be also here concealed immense placers of jrold anh the separation of the Platte and Arkansas, con- denses into the snowy promontory of Pike's Peak, and terminates in an abrupt precipice to the Great Plains. At both of these remarkable focal points, nature seems to have insti- tuted a primeval conflict between the abrading power of the rivers and the stubborn resistance of the porphyritic durability of the mountain barrier. At the northern focus, the triumph of the rivers presents a com- plete harmony of the pas.ses, which enter at all points upon the plain of the South Pass, and connect across it. At the southern focus, the unscathed impenetrability of the mountain porphyry presents on every front its mural precipice of undiminished altitude ; here, then, the aus- tere rigidity of the mountain mass triumphs and admits no transit direct through. To complete the perfect counterpart resemblance between these foci, opens from the western flank of the mother crest, the Bayou San Luis, which is the seventh pare. This is, in physical formation and in every detail, the exact twin counterpart of the pare of the " Plain of the South Pass.' The Sierra Mimbres bounds its western edge, along whose base flows the Ilio Bravo del Norte. Elliptical in shape, level as the sea, equal to the third pare in area, encoinpas.sed by the sublimest scenery, abundantly irrigated by streams, 6500 feet in altitude, it has an alluvial soil of luxuriant fertility, and seasons eminently propitious to agriculture. It is in this delicious " Bai/ of the Sirrrns' that the current flow of time will find renewed, identified, and developec' all the charms with which Oriental narrative and .song have invested the lovely Valley of Kashmere ! The Spanish Peaks outflank the mountain crest under the 158th degree of latitude. From hence to the 2'Jth degree it .sheds the waters of the Rio Bravo del Norte from its western flank ; from the eastern flank descend the Arkansas and the Red River, flowing to the Mississippi, and the rivers of Texas, flowing directly to the Gulf. The whole front is masked towards the east with a screen of secondary 7H(',sv(s (tables) termed distinctively Unnos. These are immense triangular terraces, of half the altitude of the Sierra, resting against its flank, pro- 32 THE CORDILLERA OF THE SIERRA MADRE. truditi}^ uutward many hundred miles, gradually dwarfing in breadth until they terminate in an acute angle. They have an uninterrupted level surface of calcareous soil, a scanty herbage, and rainless atmosphere, an imperceptible dip towards their ter- minations, where they present an abrupt wall of many thousand leet in altitude, suspended above the Great Plains. All al(jng these mural flanks come out innumerable streams, which go to form the Arkansas, the Red Kivcr, and all tiic rivers which traverse Texa.«. Thus is explained the coui'usion which perplexes the public mind, struggling to arrange the physictd configuration of this immense region, as yet only partially explored. To the Mexican people who inhabit the higher mountain region, this is known as the lower plain ; by the people of the maritime region, who see from below its ragged front, it is designated as the Guadaloupe .Moun- tains, and by other names. But this system of llanos, seen most distinctly in Texas as the LImio Eatiicudo and the Lhtno of the liaki/ata, has an extent and magnitude on a scale commensurate with all the other distinctive formations. It is the coiitinu(jus screen or Piedmont which graduates the immen.se declina- tion in altitude from the summit crest of the Cordillera to the smooth expanse of the Great Plains. It ajipears from above as a depressed mesa ; from below as a series of ragged mountain chains. Geologically it is, as it were, a continental terrace or steppe, or bench of the sulphate of lime (plaster of Paris), elevated iibove the Great Plains, which are carbonate of lime ; deprc.s.sed below the Curdllkra, which is porphyritic granite. I may with propriety pause here to speak of the Basin of the Kansas, both on account of the fitness of the opportunity, and because this delicious country, surrounding the very navel of our continent and embracing its geographical centre, has from that fact a perpetual and paramount interest. The Kansas River has its extreme sources beneath the roots of Pike's Peak, where they have ceased to interrupt the plains. The Platte and Arkansas envelop it; and form a line of drainage between it and the Cor- dillera. But in front of the Kansas Basin the screen of the Piedmont is interrupted and disappears, so that the Great Plains stretch up to the base of the naked Cordillera, which reveals at one sight the towering masses of Pike's and Longs Peaks, and the curtain of snowy mountains which connects them. A similar coup-iToeil is seen, as presents itself to an Italian standing upon the Po above Milan, whose eye sweeps the Plain of Lombardy, and ascends to the snowy summits of the highest Alps, without any interven- ing objects to interrupt the vision. A similar resemblance to the Alpine THE CORDILLERA OF THE SIERRA MADRE. 33 formation which characterizes the parti.'.lly-explored masses immediately to the west, has acquired for them the local name of " TIelvetiaii Mountains." From these two peaks, — Loiijr's Peak to the nortli. and Tike's Peak to the south, — as from twin radiating points, the riedniont expands from the eastern flank of the Cordillera, like a half-ojien fan. Towards the north are the Medieine-Pow 3Iountain and the Laramie Plain ; towards the south, the U.itono Mountain, the Llano Balsiffeta. and the Llano Estaeado. Such is an effurt to delineate and ela.ssify the ]>roniinent physieid features of the Miilhir (^>r(/iflrrn of our country; the .serrated axis which forms its core; the system of pares; the system of river.s and mountain spurs; the jieaks and mc.sas ; the system of llanos. Its m.'iterial mass is primeval granite. Volcanoes, active or extinct, craters and their i, H ■'f'n<-ir^u ..I'l'' ^#* :%' Un,l,l,l> M f E ^/, •^vv *»ll •Vr. "■U- T''^ H-. "'/'• m /J f/ >, ^ — -v->^-- f N C. 'iSte. ;i^, Oak f'l-/rlf/. ft .ii jijL./.' \ *. brAXJCTMN 0> o ^ ^ iiTVAri. r r WIS .>. 111 an('liu'i» pTT?nu"''"''^ 1 nusfl A iu«\; ,lw,v-.iii i»;. K, H — ._. i.Kci '^.7^^^' )^,v-»^V's" ilcinocrnf IKIVclty V I'latoan, : Messes elm fii tliO tii'y thi.s ; iiri'l (Icino jiowcr in t A sill (;oi Kurojp,. Jill The inn ♦iiicnf. exfi is iiK^loscfJ liraeini.' flii Ciisfiian ,Se; flow ill to til This t,'rcii Jiiiineval in I.ifituiie.s ;J5 niilcs. Such is tj filjre is inijJ fill. WekJ hiirharians |J to the seas, These cojivj of Europe, Sueh is a I for the higj I'ojiiWations.l The Pf,A Seas : the ij large rivers,] ranean. It Here is inspired civ| systems of 'vligion, trii^ Porpetuate el the earth anl THE i'i..\TF..\r OF yoirrif amkukw. 35 ili'tnocrntlc einjiirc co-ctiual with tho area of tlu> CDntiiiciit. Tl..- utiiihI iKiVflty wliii'li rises in t'nmt. is tlic /'/ufimi nf flir Tulilr Luiulx. Tliis I'latiMU, iiiL'losi'd widiiii tlu- ('unlilli'ras nf tlio Muiiiitaiii Foniiatinii, pns- HosHtw eliaraftcristics now to niankiiid, and about to arre;*t the attention and sway the mental enerjiieH of Anieriea. Ill tli(! first jilacc, it is necessary, l>y reference and coniiiarison, to ideji- tity tiiis Pliilidii ; to discover wnat and whiTC it is; and tlience to tro un and demonstrate its area, its climate, itH capacity, and its ^'eofrrajihical jiower in the world. Asia contains two jilateaux ; Smith America, one; Noiih A»nerica. one. Europe and Africa have jixeat mountain chains, ])ut no jilateau. Tiie immense I'lnfpnii of Asni oecupies the central rejrion of that con- tinent, cxtendin}; ea.st and west from the I'ontic Sea to Middle Chiiin. It is iiurloscd hetween the Himalaya IMountains and those of Siheria, em- hracinii the uiiper and lower jilains of Thihet anil the prcat lakes, the Casjiian Sea, the Sea of Aral, and the IJalkash Sea, witli the rivers that flow iiito them. This !j;rcat space is fenced im])erviously from the oceans by a circuit of ]irimi'val mountains: it extends cast and west 4S(I() miles, between the latitudes ;{5° and r)0°. Its average breadth, north and south, is 1200 miles. Such is the immense cimtinental plateau of Asia, of which our knowl- edge is imperfect, as to its po]iulation and the grade of civilization they fill. We know that from jirimcval time, periodical swarms of conquering barbarians have descended down its flanks and delngcd all the continents to the seas, convulsing cmjiires and disjilacing all organized societies. These convidsions have extended to the extremities of China, of India, of Kurope, and into Africa. Such is a short and significant memorandum of this plateau, remarkable for the high antiquity, the numbers, and the uniform barbarism of its populations. It is entirely north of tlu' isothermal temperate zone. The Phifcait of Syria occupies the .space between the Vcrsian and Keil Seas : the Dead Sea is within it and the peninsula of Araliia : it has no large rivers, but is flanked by the Euphrates, the Nile, and the Mediter- ranean. It lies across the Isothermal temperate zone from edge to edge. Here is the original birthplace and cradle of human history ami inspired civilization. Down its flanks have descended all the ethereal systems of the world, which enter the heart of men and inspire true religion, true knowledge, political liberty, and which erect, enlarge, and perjietuate civilized .society. Hence have gone forth to the extremities of the earth and to the human i-ace throughout all time, the genuine oracles 36 Tin: PLATEAU OF XOllTIf AMKIUCA. (){' < 111(1 ri'vcaliiif: rclipmi and lihcrty. to acliiovo tho eonqufst uf iJolatry anil Ijaiharism, and disjilace tlu'ni from tlie luiman heart. IJcncath tho e((iiator, upon the summit of the Peruvian mountains, is the I'/iifidii (if thr Aii(ff- ilcrc was tlic delicate empire and system of the Incas, wlneh w'''.iered before I'izarro and tlie Spaniards as a vine before the tropical siroc. It contains ilie Laki, of Titicaca, ami is witliout larjre rivers. Of excessive elevation and aridity, small in area, arduous of access, and approachable only thnui^h torrid lieats which .surround its base and flanks, this Plateau is entirely vithoiif the belt of the isothermal temjierate zone. Such are the three other I*lateaux. We now approach the fourth — our own — the P/oterin of Xorth America. I have heretofore written of this Plateau : " I speak witli preat diffi- dence : but of all the departments into which science has arranged the physical geography of the globe, this appears to me the most interesting, the most crowded with various and attractive features, and the most cer- taiidy destined eventually 'o contain the most powerful and enlightened empire of the world. •' ^\t present it is no more known or comprehended, ns it is, by the Ameri- can peojile, than was America it.self by the poet ITomcr. It is to them as much a myth as was then the continent of Atalanta. Nevertheless, it is of such great area as to contain within itself three great rivers which rank with the Nile, the (Janges, and the Danube in length, and five great ranges of primary mountains." The A ndes. where it issues from the Isthmus of Tehuantepee, divides into tlie two Cordilleras of the north. The one pursues the shores of the Mexican Gulf; the other, the .shores of the Pacific Ocean. The Cordil- leras, .ontinuing to open from one another, run, with gre^it uniformity of I'v.!!: :!n;l altitude, through to the Polar Sea. At the 48d degree of lati- tnile they are 1 400 miles a.«under, which is here the breadth of the Plateau. 'i'he riiafirii CanUVcra is the Sierra JIadre (the ^lother Mountain); the in.tfmi CordilJvra is the Sierra Nevada de los Andes (the Snowy Andes \ T' i ;. ili(>n. the whole immense area encased within the Cordilleras from Tehuaritepee to tlie Polar Sea, is the I'lateau of Nfirth America ! The Cordiiloras have a general altitude of 12,000 feet ; the Plateau, of (JOOO. The I'la'oau is 4000 miles in lengili. having its direction from .southeast to nortliN^e.st ; its superficial area is 2,000.000 sfpuire miles. The portion within our territories is one-third of the whole country. Such. then, are the geographical position, the t.rea, and the altitude of the I'/dtuni. Its lo)iffitv(h'nnl position is remarkable, having its extremi- THE PLATEAU OF XOHTJf AMERICA. 'M y^^{ of idolatry n mountains, is ami system of liarils as a vine , aii'l is without in area, arduous Icii surround its 1" the isotlicrmal the fourth— our with ?rrcat difli- has arranged the most interesting, ind the most cer- and enlightened t ,\ by the Ameri- cr. It is to them Nevertheless, it rreat rivers whith gth, and five great huantepec, divides the shores of the can. The Covdil- re-it uniformity of 43(1 degree of lati- idth of the Plateau. Mother Mountain); \ndes (the Snowy ,c Cordilleras from th America! The , Plateau, of (3000. tion from southeast miles. The portion •y. •inrojiress was forcibly interdicted. Abruptly stopped by an Indian barrier and Draconic code, and forced to recoil for forty years, the flanks have come up to an even front upon the rijjrht and upon the left. Science has recently very ])erfectly established, by observation, this axh of the isothermal temperate zone. It reveals to the world this .>^hining fact, that alonjr it civilization has traveled, as by an inevitable instinct of nature, since creation's dawn. Finm this line has radiated intellijience of mind to the north and to the ■ to despair. They invite and receive the white man as a new divinity, and then recoil, to shun him with hate implacable till death. This is my understanding of the Plateau of America, condensed to a general but a compact view. At my first entrance upon it in 1843, my impressions were far otherwise. Everywhere appeared novel phenomena ; nature wore an impenetrable complexity of features alternately fantastic, sublime, bizarre, and incomprehensible. Time, reiterated exploration, study, and meditation, have revealed it to me as it is, — in architecture transcendent, in an:itoiny symmetrical and con- sistent in every detail. It is necessary to ponder long before we may pene- trate the deep designs of Providence, or be permitted to comprehend the austere and perfect order with which natuvc is everywhere replete. hi CHAPTER IV. THE SIERRA SAN JUAN. i To command the gold and silver production of the world, and combine this with an intelligent policy, is to rule the world. The present ability of the American people to do this, will become manifest so soon as the geography of the North American continent shall become correctly under- stood by tliem, ar.d its economical development made a systematic policy. A few standard facts in physical geography and geology being currently grafted in to guide the popular mind, the ease with which the people of America will rise to the pinnacle of power and empire, and the necessity inc'imbent upon them to do so, become both simple and luminous of comprehension. I have in a former chapter defined to itself the " Great Plateau of the Table Lands," and enumerated the primary mountain chains, the rivers, and the elevated basins (seven in number) which checker its immense area. This whole aroa, together with the great flanking Cordilleras, is of the primeval, auiiferous formation. Although immense sa-idstone and cal- careous formations are frequent, and elsewhere igneous rocks have over- flowed thousands of square miles, these overlay a luiiform pediment of porphyritic granite, as uniformly yielding gold. The primeval gold-bearing formation, therefore, very equally divides the area of the continent, half and half, with the calcareous formation, which latter abounds with the base metals. Thus, within the present tfritorics of the American people, the precious stones and precious metals, pla.inum, gold, silver, quicksilver, exist in tl:e im yet partially deveit (i^l aalf, with the same abundance and universality ofdistrilution as do tl . ^'ate metals, minend fuel, and calcareous rocks, within the States. Investigation within " the great calcareous plain" has so far progressed, that we trace along its diagontd axis a metallif 'lous band traversing con- tinuously from the neighborlniod of Mior, en the Kio Bravo del Norte, to the junction of Coppermine IJivcr with the Arctic Sea. This band, reseuibliiig a .-word-belt suspended from the shoulder and knotted upon the hip, faver.^cs Texas in a direction ni'rth-nortlicast ; crosses Arkansas .-'.ud iSuuthcrn MiH:«ouri diagonally ; Noitliern Illinois, 44 THE SIERRA SAX JUAN. 45 rid, and combine le present ability 3t so soon tis the > correctly under- jystenuitic policy. ^ being currently ich tb.e people of and the necessity and luminous of at Plateau of the ha ins, the rivers, it^ immense area, ddleras, is of the idstone and cal- rocks have over- inn pediment of quilly divides the formaUon, which present tcritories melals, plaanum, ,xu [" 'I half, with lo tl : 'xii-e metals, ;o far progressed, id traversing con- avo del Norte, to the shoulder and 1 iKirth-iiortheiuit ; Xdrtlieni lUiiiois, Wisconsin, and Minnesota, and, brusliiiig the extreme shores of Lake Superior and Hudson's Bay, sinks into the Arctic Sea near the Magnetic Pole. Everywhere within this band the calcareous rocks and soils are )iemie- iiteJ with veins and native masses of the base metals, existing in a pleni- tudi' and purity . ufficient to snjiply the world forever. AVhat is seen and known upon the .'iiirface, indicates a sy.stcmatic order throughout in the relative jto.sitions of the dift'crent metals and their accompanying rocks and earths, as also in the localities where each exists in excess and may be said to culminate. Thus in the State of Misi^ouri iron appears protruding above the general level, over an immense area, attracting extlu&ive attention and the appella- tion of Iron Mountains, by reason of the immense formation of this metal, which displays itself for many hundred sfjuarc miles above and below the surface, la mass miu In ponltion. '"Jojiiier may likewise be said to cul.ni- nate, where it displays itself around the extreme waters of the St. Law- rence, in mam and in position. Thus likewise of lead, where it appears in indefinite abundainte by itself, in Wisconsin, Misi^ouri, and Arkansas. Tbe existence nf tiu- base nu'tals of native jmrity in ?«a.s.< mid in pnsifion, on an imnu'n.^i! scale and within the calcareous fovnuition of the basins of the Mississippi and St. Lawrence, is now become established. Tbe ques- tion arises, tberi.forc, whether there exists within the primeval formation any jarallel phenomenon, or any possibility of the existence, accessible to hu Man research, of tiie precious stones, of gold, silver, and tlie kindred j.rccious rif^tals, in mass and in position. Tiie po.ssibility, and, even more, the prohability of .such a develojimcnt resulting from persevering exploration among the sieiras of the Plateau of the Table Lands, becomes distinct as their geological configuration is ' evealed, We have seen, in a former chapter, that the Cordillera of the Sierra Madre presents within our territory tW(.> ri'inarkable foca) culminations, — the one grouped around the Wind River ^lountain, the other surrounding Pike's Peak. These are about four hundred miles apart; th^y are con- nected by the continuous chain of the Cordillera, as by a curtain. Either one, contenijdated by itself, fills the same significant place upon our contiuent, as does the Alpine gror;- surrounded by tin; kingdoms of Europe, in the topography of that continent. A parallel altitude, grander bulk, larger rivers, the sublimest scenery, a rainless atmosphere, and a foundation of bro.'ub'r and more •iriHddini'iisions, distinguish our 'ontinent. Tnd tlie gre:'.t phans in the iwighborhood of the 39th degree of latitude, tbe snow-crested mu.-s of Pike's Peak, 15,000 feet in 'li! 1 1? ,'M r^' N c. ■'- - - *, ''^ •>*, ^ y \*.. 0>^V y /, k/ ijTA.virt'd.v l»niiij»il"''f*<»''' ""T" ^ '- S ft, A S K A J I O ' W. *;v.. y^V ^-0 . O V^.J'"'* V •^-A Sau^lWviuo *^W. >.l*jA', J SEW .9 ^||UkyJ KT'" 1 ^ [--^Wm. BPR fcfcSi^^. *c^ .-I- >:mM Kir .%:(Ai" 01'' N OUT 11 AMKllU A ih^liiM^aliiKk ilii* MOryiMX SrSTIJM xynnsniTArLS, WW (»1U:AT ( AL( AUKOl S plain as a IMT, hy and geology. The founders of these sciences have reared them by hiving the slowly-developed details of nature, collected by exhausting patience within the small basins surrounding the cities of their residences. Thu within the small basins of the Thames, the Seine, the Arno ; upon the flanks of the Alps, the Apennines ; in Calabria, and around Fingals Cave, have heretofore been found the most popular illustrations to nurse the infancy of these sciences. More than si.xty yeare of intense meditation has inspired the cosmo- politan genius of IIi'.AiiJOLDT to scan the terrestrial globe with an expanded vision. He only has s])oken worthily of America to her own peojjle. In him we recognize the intrepid pioneer who invites us to understand the gigantic proportions of our own great country, its order, its s^ynimctry, and itx grand simidicity of configuration. As Columbus led forth navigation and commerce, from its lengthened tutelage in the Mediterranean Sea, to expand itself over all the oceans and to every continental and every island shore; so now, this venerable pioneer of phj-sical science and the arts, marshals us on to penetrate the arcatin of the land, to fit .society to the broad foundation of the continents, and rear a comity ol" civilization coe([ual with the globe. It is in Europe that CoLUMnus and IIu.mbo'.dt have had their nativity and their residence. It is for America that t.i^y have lived ; to us they belong ; apostolic citizens of our destiny ! The area of the department of the Platrnti of the Tahh Land, embracing the three elevated basins of the Salt Ijake, the Colorado, and the Rio Bravo del Norte, is ef|uivalent to France. Austria, Switzerland, and Cisalpine Italy combined ; its rivers are equal to the Danube, Rhine. Rhono, and Po : its metalliferous mountains are pre-eminent in bulk, number, and granileur. In rcadiiivss to receive and ability to sustain in perpetuity a dense |io])ulation. it is more favored than Kurope. Fertility of soil of the high- est order is the dominant and unil'orm characteristic of this immense THE iilEUHA SAX JViN. 51 wander — ^but region. The mouni-iins are rarely abrupt or rugged. Tliov are sur- mounted by mesas, descending by giijantic terraces called tiwuMiK. The densely crystalline primeval rock'* yield but slightly to atmospheric corro- sion in the regnlarity of a continental climate and seclusion from the sea. It is the decay of lava, selcnite, and carboniferou.xlinu stone ilmt forms the soil. The pastoral fertility is developed by nature, which sustain* its aborigi- nal herds as fish in the rivers and in the sea. The arable fertility needs the care of man, and awaits the economical development of artificial irri- gation. For the reception of this system, the whole structure and contour of the surface is fitted, and the natural waters abundant. Reflection will recfdl to memory the magnificent empires of peopie. possessing a highly-advanced, but imperfectly-organized, civilization, found established along the .summit of this Plateau, con(|nered by Ct)RTEZ. .•Vlvau.vdo, and 1'izarro. On the summit of the Southern Andes, in Chili. Peru, and around Quito, on the Northern Andt's. in Central America, and Mexico, dwelt twenty millions of popnlati,)n in the aggreg-ate. Three centuries of subjugation have dwarfed this aboriginal people to one-half of their original numbers, and radically altered their religion, their lancruasje. and traditional manners. Tliev have touched the lowe.«'t point of decadence, from which they will again slowly ascend. This peojile had no fixed science in physics, religion, or politics, to prop and protect their system from the shocks of time; no na'igation. no prin- ciple of perpetuity. Tlu..«e have now come to them with the EiirojH'at! column, bringing with it the ark of regeneration. The peciUiar agricul- tural and social sy.stem of the Mexicans under the Montezunias, extended up the basin of the Rio Bravo dci \ort«' to the ba.se of the Sierra San Juan. Our people are marching to the same | oint fnnn an opposite diiec- tion, bringing with them the social habits of the isothermal zone and a maritime climate. I have spoken of this remarkable focal culmination of f lie Eastern Cor- dillera, fronnvhich two snowy promontories protrude, back to back ; Pikes Peak to the northeast beetles over and subsides into the Plains; the Sierra San Juan, to the south, beetles over the Plateau, and subsides into the Sierra Mimbres. Radiant mountains and streams diverge from this point in every direc- tion, and form abundant pas.ses, direct and practicable, to and fro, betwet-n the basin of the Missisisipjii and the Plateau. The three reniarkable purrs — the Middle Pare, the Rayou Salado. and the Mayou San T.uis — all approach close together the dividing crest of the Easti'rn Cordillera, over whoso summit they imujedialely communicate. i 52 THE SIERRA SA\ JVAS. I know not hew adequaU;ly to delineate this knotted group of all the colossal elements of nature. To subujit the unenibellislied facts is all that is necessary, were this possible, where the elements in "ompact contiguity are so many, so varied, and each of such colossal granuour. To exag- gerate is far from my intention ; to enumerate the detiiiis t)f nature, as I have seen them, with austere simplicity, is my aim. Heboid, then, to the right, the Mississippi Basin; to the left, the Plateau of the Table Lands ; beneath, the family of Pares ; around, the radiating backs of the primeval mountains ; the primary rivers, starting to the seas; a uniform elevation of 8(MI() feet; a translucent atmosphere, a thousand miles removed from the ocean and its influences ; a checkered landscape, in which no clcnunt of sublimity is left oat , fertility and food upon the surface ; metals beneath ; uninterrupted facility of transit ! Behold the sublime panorama which crowns the middie region of our Union, fans the fire of patriotism, and beckons on the energetic host of our people. The American j>eople number fifty millions in strength. Two millions change annually tb.eir place of residence. The oracular instinct of conquest burns in every heart ; this is the continental mission of '7ti, proclaimed from the traditions of Jamestown and of Plymouth Rock, and thence becjueathed to posterity ! The column of pioneers (engaged during several years in planting the St^ite of the Kansjis basin) has pas.sed over the rim of the Calcareous I'lain, and debouched upon the base of the primeval mountains. Gold has been found at the fii-st trial and upon the threshold at Cherry Creek, upon the eastern flank of Pike's Peak, and elsewhere. A few seasons have sufticed for them to ascend, by the Arkansas and the Bayou Solodo, to the mother crest of the Cordillera, whence the basins and sierras of the Plateau expand beyond : " The I'loHils nl'Pve us to the whifo Alps fond, And wo must j ieroo them, and survey whate'er Mny be permitto i . ns our steps we bend Ti) that most great nud growing region, where Tho earth to her embrace compels the powers of air." Let us here pause to reflect whether the traditional history of our race does not, on its very front, ilhistrate what ])roniinence awaits this Imiffi- tv(h'ueck, upon the ave sufficed for to the mother i)f the Plateau oiy of our race aits this longi- rraees into the AVOSt ! Incas exhibits joriginal people ids, as universal All around the head of the Mediterranean Sea, where it penetrates the Asiatic continent, its basin is encircled by a j)latca\i. or amphitheatre of elevated plains extending round from Suez, ((tntiiiuously through Syria, Asia Minor, and into Greece. This descends by terraces to the sea-slth. The Plateau of the Tahle Lands. 7th. The Cordillera of the Snowy Andes. 8th. The Pacific Maritime Slope, ilth. The Pacific Ocean. This route brinjrs into immediate juxtajxtsition, ii/i>ii*t ])enned, was the interval occupied by the C )rdillera of the Sierra Madre, the Plateau of the Table Lands, and the Cordillera of tlu' Sierra Nevada, which conjointly form the •' tuinmtnin fonnathtn oj North America," extending continuously from Tchuantepec to the Arctic Sea. 54 How this cc breadth, is to i lislinieiit of the them. It is b people and the that of exit oi now and in all There exists sixsijipi, a perf( prestige, and hi furnish a lumii •iVmerican peop The area in of the surface i Pontic, Propon Danube, the Ni imperfect naviad out to illuminate the whole area, both under the political sys- tem of the lloinaii J'jnpire and the religious system of tlie l{<>i»ii!! Church. It has overrun the brim, and is inherited by the mod-jin European nations who are the dispeisi'd progeny of Home. The " Basin of tlu; Mississippi" fills more perfectly the temperate zone. The counterpart of the salt water surface is a delicious, undulating plane, everywhere channelled by rivers navigaliU; to their very sources: navi!',:ulation of one hvndrea hiiii t)f hiiul, every wliero iiiterhuetl and raiiiitied with iiaviu'ahle arteries, lioiu i.re traversed centrally by the r.i)(/t'(ic (if ( injiircM within which the current of civilizatiun has fluwcd in all a;;c!< /'/■"/;( t(i:ei|uently of all coumn ice, to the !otli flow fnuii chasms in the flanks of the iniineii.se mass of the Wind Uiver Mountain, which here forma au urc fronting to the west, und issue out upon the plain. But the plain ia traversed by a gentle d!clil<\ [lanillel with the iiioiintain base, und no more distinguishable than the bevel given by eiigineeis to any ordinary street. Against this these two streams are deflected into opposite courses, the former to burrow its way around the urc of tiie moun- tain to the southeast, the other towards the no it Invest. To one who observes this from the plain, there is presented a similar miraculous configuration of the land, such us displays itself to oik^ who, naviguting the Propontic Seu, beholds the Dardanelles upon his right hand and the Bosphorus on his left. Moreover, the sky is vithout clouds and rainless, the atmosphere intensely brilliunt, temperate, .I'.id screiu-, encompussed round by scenery of the austerest sublimity. But we have seen that the elevation of the South I'ass is 75(10 feet, and that Snake River runs continuously out of it by the most direct and favorable course, of 1400 miles, to the Pacific Sea, tuiinelliiig consecu- tively the Blue or Salmon lliver range of mountains, the western Cordil- lera, and all other transverse ranges and obstructions. Here is, then, an uninterrupted water declination through and across the whole ^'^ mountain formatiou" descending by a plane dijiping Jicv J\tA to the mile ! From the adjacent eastern rim of the Plain uf tlic Sonth I'ajss runs out Sweetwater into the Platte, »¥hich, tunnelling consecutively all the out- lying ranges of the eastern Cordillera, forms a similar uninterrupted water declination, in a very straight line of 1400 miles to St. Louis, descending by thti simie average dip i>i five feet per mile. Everybody is familiar with the existing railways, which, radiating from St. Jjouis and pursuing continuously the plains of the Ohio and St. Law- rence, outflank the Alleghanies between Syracuse and Home, and descend by the Ilud.son lliver to New York. The .Mieiiees which delineate ami explain to the human understanding the details of matter, i»s it fits itself in myriads of millions of variegated forms to fill oil intt^resting to t physical geogra This line of our I^iiion fron :tt;oil miles in I ri'os.sing one ri It ]ire>eiits to II nieiicing at the and debouehiii) From the Si out. Tllcy, to; tudinal, ]iariilli a])proa(-li the .hi Hanks, which n barriers. Nowhere, wi dividing barrie; pa.ss. Nowlier crest, and a cor east and to the The South I some l.'iOO )n atmosphere is Hence an Intm tonic and .saliil Along the n time climate a .scale as the sin so nearly ap]iri ]ilenitude. Human socii periods of barl feet. Manner! opposite, as tli- this harmony buleiit force di is lo.st ; as we empire ri.se. Nature here of configuratio THE sorrn r.iss or amkiiha. « forms til till ant tln! Niipromi' onlt-r nf tlio univereo, develop nothing so iiit(;rc.stiii^ to tlitt lit'iirt of civilixcii niaii un tlii.s xiii^lf Hul)liiiie t'uet of pliysital ;;('f tliu Creator. Tliif* iiiif of gentiy-iinduiuliiig river-gradet* fiirdles tin- iiiiddif zone of our Union from sen to sea, in one sniooth, continuous and unliri>ken cord, ■'{(idd miles in iengtii. It fits t/i> Imtthtrnuil f/.r/jt of the temperate climates, crossing one river only at St. liouis, and outflanking all tin- nmuntains. It |irc.-cnts to us the counterpart of that water-line of the Old World, com- mencing at the extremity of the Kuxiiie, passing down the Mediterraiieau, and dehonching out into the ocean. From the South l'a.ss to Mexico the primary mountain ehaiim spread out. They, together with the great rivers wliich divide them, are longi- tudinal, parallel, and uiiperforated. The rivers grow deeper as they ap|iroach the .sea. increasing the altitudi and ahruptness of the niounlain flanks, which overlaji one another, and incrcjise and c(»niplicatc the mural harriers. Nowhere, within this interval, uro the mountains reduced to a single dividing harrier, nor are there jiresented anywhere the essentials of a single pa,ss. Nowhere is to he found a sufficient depression in the mountain crest, and a continuous gradation from the summit-crest, prolonged to the east and to the west, down both (h'clinations to the seas. The South Pass is elevattid 7')'MI fet^t above the seas, from whieh it ia some 1 '>(•(» miles remote. It has, then, a rontiiundil clliiuitf, whose atnio-sphere is tempered by tin? altitude and by tin; absence of moisture. Ileiiee an interne screuiti/ is the |*rominent feature, jierpetual sunshine, u tonic and .salubrious air, a vernal ». iiiperature. Along the roiitiiinittil //«rthe chHi,_'es from the continental to the mari- time climate and tire rvriid, gradual themselves with the Siime delicate scale as the surface slopes. Untfonnity u/ climate, from seu to 8e4J, is then so nearly apjiroaehed, that it actually exists ull along this line in absidute plenitude. Human society, in the current course of ages, vibrates to and fro through periods of barbarism. God and Nature endure con.stantly eternal and per- fect. Manners, religions, policies, change and becom, our farms and habitations, will traverse the hroad current of com- merce, where [la.ssenjrers and carjioes may at any tinu- or jilace emhark ujion or leave the vehicles of transiiortation. Down with the parricidal trea.son which will hani.sh it fnun the /<»;«/, from amontr they"V(y//»', to forc'c it into the /«»/•;•<•« ovcun. outside of society, thiouirh i'orei^n nations, into the torrid heats, along solitary « in nitons routes, im|irisoned for months in great sliij)s ! This i'mttnuntitl liaihrni/ is an es.sential domestic institution, more powerful and more jterniaiient than law. or popular consent or jiolitieal cnnstituiions. to thorouirhly comj)lete the great system of fluvial arteries wiiich I'raternize us into on(> people ; to hind the tim sra-lxmrdH to this one continental I'nion, like ears to the human head; to radicate the founda- tions of the I'nion so liroamory, his name, and his actions. Modern linn s. accepting the tradition, behold it stamped upon the coin of .S|)ain and the Indies, to obtuin a circulation as universal and i'amiliar as the human ra<'0. The American people pursue the planting of empire, advancing with intense celerity ; moving to the front according to a system understood and self-disciplined ; marching with the eudenco of an army of innumerable legions, uniting in one homogeneous order, with the same energies, a single aim. and rrshing to eonsuinmate a cnmmon ilestiny. .^'hining in the front of this marching hast, the pioneei and excni]il;ir. •'///-.il gave to us this sacred Union and foundeil our continental Ke|iul)lie. The xnoml has filled u]i the Atlantic half of the continent vith States, secured the maritime connections with that ocean and with Kuro|ie, and has bla/.ed for ns the way atio.ss tlie continent to the I'acitic an 1 to Asia. We, the /Am/ generation, receive I'rom them the jiious task to plant State's onward to that ocean ; to complete the zodiac of fraternal nations round the globe, and to set deep and firm to their outward dimen- sions the foundations they have laid. As we a.-^sume our task, illuminated by the example of their wisdom, energy, and glory, intent to equal them in the first and surpass them in liir rest, may we not repeat this invocation to the luminary of the universe, i.s he depiirts to usher in another day : — I ■ '■ 1 ho wcnry sun halh iiiinlc n hoMpd «<•?. AnJ, by tliu brij;lit truck itf liis fiery car, Qivos token of a gomlly ilay to-morrow !" Th h'I ,1 m CHAPTER VI. THE GREAT HASIN OF THE MISSISSIPPI. TllK most olividiisly roniiirkanlo pliysiral feature of America and of the iiiliabitt'tl j:l(il)e, is the Jinsiii of tin- MkmMlppi. Ah yet tlio pojmlar luiml doe.s not clearly comprehend its diinen.-^ion.s, and tlie underHtandinj; of it.- phy.sical characteristics is indistinct and vague. It is bi.sected througli its eemrc hy a supreme artery, which above St. Louis has received the uuuie of tlie Minsoiiri, and below, the MissigHipjii River. This is r»(l()() miles in length, and its surface is a continuous inclined plane, descending .seven inches in the mile. Into this central artery, as into a common tioiiffh, descend innumerable rivers couiing from the great mountain chains of the continent. All of the immense area thus drained, forms a single Ixisln^ of which the circuniferent mountains form the rim. It may also be called an (imphl- tlii litre, embracing 1,1215,100 sfpiare miles of surface. This has been, during the antediluvian ages, the bed of a great ocean, such as is now the Gulf of Mexico or the Mediterranean, above the surface of which the mountains jirotruded thenLsclves as islands. (Jradiially filled up by the filtration of the waters during countless iiges, it has reached its jtresent altitude above the other basins, oV(^r which the oceans now still roll, and into which the waters have retired. The " Jidxiit of the Af{itsliisi'j>pt" is, then, a j)avemcnt of calcareous rock many thousand feet in depth, formed by the .sediment of the superincum- bent water, deposited stratum upon stratum, compressed by its weight and crystallized into rock by its chenncal fermentation and ]iressiire. Jt is in exact imitation of this sublime process of the natural world, tl at every housewife ( > 'ipres-ses th(> milk of her dairy into solid cheese and butter. It is, therefore, a homogeneous, tindulating plain of the g/onii/iin/ or sedimentary formation, surmounted by a covering of soil from which springs the vegetation, as hair fnmi the external skin of an animal. Through this coating of soil, and into the soft surface strata of rock, the de.'^cending fresh waters burrow their channels, converging everywhere from the circumfi'rent rim to the lowest level and pa.ss out to the sea. In this sy.stem, which is the sanu> as the circulation of the blood in 64 animal life, the garden fountain, correspontling oi of contour in th( Such is this vi simph>, homogen The vegetation i and are mon; vai oceans, and with The in.sular si feet el(!vat*!d abo coming from the The plain of T.OOO feet above raiidess and witli Such are the ( Through the i one to the other, sensilile to a tni\ who does .so, the.> the diurnal alti>i the grasses indie palpably as tin All that porti River and th(' .' Indiana, IlliiioiH Arkan.sas, and S An irreguliir south and west i this iiue and tin ened liy .sliowers I'eyond this nourish tim!>er. narrow lines of and in thi. is!nn( and soft, arablt; of vegetation. The tcrminati the first, where about l.'iU mile tised, nor ncec.^s THE OIIKAT DASFX OF THE MISSJSS/PPr. 65 iiniiniil life, the MiKsoiiri Ilivor and the mimitoHt rill that flows from a gjirdeii roiuitaiii, lias each it.*« siieiific and c•(lns|)ieuou^ place. Heme the correspond in}^ order In the unijjiilations, the variety, and the complexity of contour in the surface and in its vej^etation. Such is this vast Basin, whose transverse diameter is 25(tO miles, and so sinipli!, homogeneous, and clear is the system of its the first, when^ t!ie rains eea.se. and the t'lnber entirely di.sapiH'ars, It is about I'lO miles in width, and witliin it artifii iai iriigatioi\ ,> not pnu - tisod, nor necessary, it being everywiiere .soft, arable, and fertile. J m Tin: tiith'AT //.1.S7.V OF riii: Mississirri. El 'l To th IS HUecci'ds till- Mil init'iisi! rin'tiffSH wh'mu onwiird to tlio niouniaiiis, cxclusivfly JiiiKtiiriil, (il'a coinjuut noil, eoiitod with the iJ\vart'ltuft"iiiojj;rii88, witliout trt'cs, aii.ied and fused into one political and social i-ysicm the /(usin nf lln Mn/ih irniititii, whose ari-a is l,l(i((,(> () sijuart n iloH. i •olli '.( o*' this they ne\('r passed, except into the corner of (Janl and Urita: lit !( •ted llicinsclvcs to the .NIe(literranean and I'oiitic Seas, to the .Vile, to the Manuhe, and (<> the Ithone. 'i'his em|iire, emiiraeing '.\ V ;i!mi\i, arc; . coi t. lined under 'I'r. .in and the Aiitoiiiues l!!! .(MMI.(IO(( of jMtpiiMi inn, .Miii lli.ii.e i.self, it; tiie gi'ograpliical centre, had a diameter (d' ;"jtl oiiie:* and !■; till. (Mill of iiiMaliilanlsI l»ii >h< Hrea oi'this Uasiii is. for the iiKisi r.irt, a salt water waste, into Avhici pHt'.riwi 'i.e |" linsiilas of Asia Minor, (ireece. Italy, and S[iaiii, tl U"ll> '1 with I mountain vertehriv, .ind al.so a i\'W islands. Spaeo for hal'/a i' i .■■ and ilie iirodiiciion of fooil is. therefc irce Th le e(piivaleiit, with us, ol' this salt surface and rugged mouiitaiusj is overywherc, an productive, Th and the front o amount and acci easily contain at inhaliitaiits ! If the eaicarec fronts, and the n Europe arid Asia. the existing hum This I'asin is ihe (Sulf, at the I produced. On th /one. Between we descend from ill posiliiiii it i the West bank o( and fertile prairii hy their confluent once of the N'ortli The circle de.^c pns,H throuirh Vd Hudson's ISay, t Cni.j. and the ci( will pa.ss throiigl therefore, thci/.-o tlie Basin of the It is also e(|u hlocked out into sites in (he iiow-e exactly in the mi tiiictly concentrat to the nnniher i occupying On'riif Europe has al wrsf dehouchinir AJii tlio niouiiiaiiis, irf buffalo ^rass, t no di'scrt (looa (lance ami niaj;- lic alisoni't' of a ; zone ; and the 1. iin ol' pahii-lcaf. ivo, till- artlut'nt n till! fist foino the rpiii'V MIh- (' Arkansas, the ri|ilc IMatto, the ' of jnrat lenj^th •f 2-2jm\ iniUvH, nl I'oast (Miual to ) oiu'-and-a-half- nil two-liftlis of ili<'(las niiniitoly m. y for ]iopiilation act. i;tli, civilization, of the lioiiiiiiis. iilniinatioii. and lilical and s'H'ial .!(i(», and productive. The rivvji-s surpass the .sea i\ir the freipulation, or l,;ilO,()00,000 of iidiahitants ! If th(! calcareous ])lain extendin/ Ut *ho .\rt^\f ^^a. the two niiirl'linc fronts, and the mountain formation, Im> •I'l/i^d. »ti4 tin- whoh' compared '/> Europe and Asia, 2,tM)U.()(M),(MM) will easily Am^ rf/Kfitt n ^.^btion d<*uW« the existin»*< the V'e/^i/<« <^ ^t^ fitt^ Zone. Ihftween the.se arc 'ourid every kin4 <»f ii>rric,«|kur.il ^> the continent. ,\'ot ft*r n^iw/^ (I'ttt the West bank of the Missouri Hiver, in the Imisohi of romarnfie '-ttt^y and fertile prairie, ia a H[K»t where the Smokyhill and I{<'publicii« Kiv«'«K. by their confluence, form (he Kan.sas. Thi* is Mu' <:eo;iraphieal centre at omc of the N'orth American continent, and of tin Hasin of the Mississippi. The circle described from this centre with a radii»^ to San Francisco ^vill pass throutrh Vimi'iinir tm the Cohnnbia, the |«>rt of Srvr/it Jliver on nud.>;on's I'ay, throujih (/n'lin-. through UtiKton, throuprh lliir'nm. Vera Cni::. and the city of Mv.rico. With a radius to flie A'M\t ilifj,.rilii This spot i«. therefore, thi' American Union, ;m it is now lilocked out into exi.stin^ States and into prospective States, to oceujiy sites in the now-existing TiTritories ! .Moreover, it is e(|uidi.stant from, and exactly in the middle between, the two halves of the huunin family, dis- tinctly eoneentrated ; the one half (Miristians, occnpyinir Western Kurope, to the luimber of :i ">!>,( MM),0(»( I of population; the other half Papins, occupying Oriental :Uia and Poh/nvsia, to the number of t!r) ! Kuro]ie ha.s all the outlets of its iidand seas and rivers towards the vent, debotwhing on to our Atlanlic front, towards which its whole surl'ace slopes. Asia similarly jire.sents to our I'acilic front an On'mtd/ s,'nj,i. containing her great rivers, the densest mas.xes of her poimlation, and detached i.slands of great area, den.se population, and intinite pro;nizcd, tii< dis- tniction of intcrvciiinther and fu.si'd into one universtJ uud convenient system of immediate relationship. Such are ,s(ime of t! •niordinary attractions presented to mankind, as a social nia.-'s. hy tlu; {xisition and conli;niralion ol' the MixHt'iisi/ijii linnni. There is anuther and superlative prospective view. This jircsciits it.self in contrastinj; the physical conlif^uration of North America with the otiier continents. Europe, tlu' smallest in area of the continents, culminates in its centre info the icy ma.sses |M' towards their ."ourct's ; nitWuation is) \,\ lUulfwlie. Art mid ommi tvc have never, durinu thiii> t-cnturii!* \itiiu-d so many suihII vulluyti. uimotvly isolat«'d hv im|K»l in n«>« lanjruac*', reli-jion, iiitor^'sts, ami hahits Thou>;h oIUmi fx-hh^^iNi/ amalpiuiatrd )>> cuit<|ue(«t. tli' apiiu rclapM' into frnpuentx. IV^iii iiMMiu i;eo^niphii ' iiicohiTeX'' u'< /iy/oti« crvi dn und tnjjifmiir^ foriu no iu«4\i enduriiit; ' ^ Thi t.ii t i «)»«•»*' nation- ' .1 ^tatjf of pei^'tual war, of mutual exu-rib itm an ip|«iilliug di»MHuti< cMUihtpie of a tew splendid xyttw iii*« er.-lun^ uiuliiiudin<>us aiitlioiivoi Hubmissive and unchronidcd H(>it«. KudH Hiniilar to Kiiidjm. though grander iu hik and {Ktpulatiou, a THE uhkat hasis of the MlSSISSiri'l. *;:« e two rof'uns, is From tli»( Htu|wiid(>UH cciifnil Imriior of the llinialiiyaM run tin- lour great rivvrs of China, duo caM, to ili.schar<;o tlu-nisclvt's umlcr tlic ri«in}r hum: towards tlie smith run tlie rivori* of Coeliin Cliina, X\w (Janp-s, anil tile Indus: towards tlu; inut, the rivers of tlie Casjiian: and hmf/i, throujrh Silu ria t« the Arctic Sea, many rivi-rs of the first ma^rnitude. I>uriiii,' fifty centuries, as now, the Alps and Himalaya Mountains have |iroved insu|)erahl(^ barriitrs to the amal;;aniation of tlu> nations around their ))atf t/ii' Misnissi'ii/ii, thus held in inn'fi/ by the American people, is a st. liawiriicc, Ilinlsdn'a Bay, ami Atlialiasia. tlu; aiii]>liilli(>ati'f of the wuilil — licir i,s Hii|ir<'incly, iiitli!i'(], the uioKt uiagiiifii-cnt (l\V('lliii niarkiil nut fiy (jod for man's aliodc. Bcholil, tlicii, ri.>-iiin now and in the ftitnic. tlir iinjui' which imhi-ilry and !-, lillldl' illlil li, iiiid wiiillicr iliu jii, tu |)liiiil u hiin- ^% .^.^. ^.^ ^\.V% IMAGE EVALUATION TEST TARGET (MT-3) 1.0 I.I 2.5 '- IP'S 1^ IM IIIII2 2 Ao nil 2.0 us 1.8 1-25 1.4 1.6 ■m 6" ► Photographic Sciences Corporation L17 V s y O "<^ V <«> 6^ ■<> ^ 23 WEST MAIN STREET WEBSTER, N.Y. 14580 (716) 872-4503 '^^ ,.'< ■V ..%^ ^^^ 47* ^- ^ :J ^ ' o » 'S) ri? pt^ nMiij»rj»#» iX -k. nAK'>S i ■i < II I ill"" (.' I'lltoxa I iT i^r ? N -4-* K X5.. O n.fc>""'«TT / P M.„l. s \Li«f?r...">-'i ^-V *f^ i*",'){'5^'"'^ / — *^ I I N O V A /< , CHOCTAW r[ 1H.ATI0 N I '^ ,..»«" t /I: IB"'""'' fcfr^ \ • I There lias the true char; which pcrvud historic pcrio the (ipi)osite, and industry They are ( Tiu'ir positii whieh terniii on the west, tcesfern limit of!;rain of les? Arctic coasts There is ii a gentle slo)i clad thick w is not silicioii out to the n and to the T The niou between thei No portir from the mt lating and Storms are i the Rocky 1 The climi to irrigate r onts. They the basins t of the "Gi States betw( ffHf CHAPTER VII. PASTORAL AJiERICA. There has been a radical niisiipprelienslon in the poimlar mind as to the true character of the " Great Pldiiis of Aiiim'cn,'' as complete as that wliich pervaded Europe resjiecting the Atlantic (Jeean durinjj; the whole historic period jirior to CoLLMHUS. These J^LAINS a"e not th'scrls, but the opposite, and are the cardinal basis of the future empire of conmierce and industry now erecting itself upon the North American Continent. They arc calcareous, and form the Pastoral (Jarden of the world. Their position and area may be easily understood. The meridian line which terminates the States of Louisiana, Arkansas, Missouri, and Iowa on the west, forms their eastern limit, and the llocky Mountain crest their icesfern limit. Between these limits they occupy a loniritudinal parallel- ogram of less than 1(M)() miles in width, extending fnmi the Texan to the Arctic coasts. There is no timber upon them, and single trees are scarce. They have a gentle slope from the icvsf to the east, and abound in rivers. They are clad thick with nutritious grasses, and swarm with animal life. The soil is not silicious or sandy, but is a fine calcareous mould. They run smoothly out to the navigable rivers, the 3Iissouri, Mississippi, and St. Lawrence, and to the Texan coast. The mountain masses towards the Pacific form no serious barrier between them and that ocean. No portion of their whole sweep of surface is more thari lOOO miles from the most facile navigation. The prospect is everywhere gently undu- lating and graceful, being bounded, as on the ocean, by the horizon. Storms are rare, except during the melting of the snows upon the crest of the Rocky Mountains. The climate is comparatively rainiest; the rivers serve, like the Nile, to irrigate rather than drain the neighboring surface, and have few afflu- ents. They all run from iccst to east, having beds shallow and broad, a!id the basins through which they flow are flat, hmg, and narrow. The area of the " Great Plains" is e(|uivalent to the surface of the twenty-four States between the Mississippi and the Atlantic Sea. They are one homo- 71 i m :ti^; •li'i 72 PASTOIiAL AMERICA. gcncous formation, smooth, uniform, and continuous, without a single abrui)t mountain, timl)cred space, desert, or hike. From their ample dimensions and position they define themselves to he the pdntiirr-jit/ffs (if thf world. Upon them I'ASTOHAl, AOUlCLLTLllE will become :i separate grand department of continental industry. The ])astonil characteristic, being novel to our people, needs a miimte explanation. In traversing the continent from the Atlantic hcch to the South Pass, the point of greatest altitude and remoteness from the sea, we cross successively the timbered region, the prairie region of .soft soil and long annual gras.scs, and finally the Great Plains. The two first are irri- gated by the rains coming from the sea, and are araUe. The last is rainless, of a compact soil resisting the plow, and is, there- fore, 2>o-'/ore, the immense empire of pasforaf (trpicn/finr. ut the threshold of which we have arrived, has been as completely a hlank. as was the present condition of social development on the Atlantic Ocean and the American Continent, to the ordinary thoughts of the antiipie Greeks and Romans. Hence this immense world of plains and mountains ; occupying three- fifths of our continent ; so novel to them and so exactly contradictory in every feature to the existing prejudices, routine, and economy of society, is unanimously pronounced an vnlnhahltahle desert. To any reversal of such a judgment, the unanimous public opinion, the rich and poor, the wise and ignorant, the famous and obscure, agree to oppose unanimously a dogmatic and universal deafness. To them, the delineations of travellers, elsewhere intelligent, are here tinged with lunacy ; the science of geography is befogged; the sublime order of Crea- tion no longer holds, and the supreme engineering of God is at i'.tult and a chaos of blunders ! The P. .STORAL Region is longitudinal. The bulk of it is under the Tempera' J Zone, out of which it runs into the Arctic Zone on the north, and Into the Tropical Zone on the south. The parallel Atlantic andde aiA maritime region flanks it on the east ; that of the Pacific on the west. The Great Plains, then, at once separate and bind together these flanks, rounding o-it both the variety and compactness of arrangement in the ele- mentary details of society, ttJiich enables a continent to govern itself with the same ease as a single city.* *■ Such an internal adjustment of society, expanding itself uniformly over the whole area of the continent, accompanies incidentally and of necessity its grand architecture. The physical anatomy, auspicious and consistent in all its details, the intense range of variety, the neighborhood and compactne.»s of these elements so various in configu- ration, warmth, altitude, and production, all conspire to dictate fusion and order. They correct and render impossible what is hostile and opposite to them. The contciiliuiialitica which anticipate tumult will assert, establish, and perpetuate themselves. The experiences of history arm us with precedents for our guidance, and instruct our judgments. They predict for us a wholesome employment of our energies, accom- panied by a subtle and zealous dii-ciplinc competent to anticipate and to restrain disorder. rrangcmont in the ele- t to govern itself with PASTORAL AMEIlfCA. 75 Assiuninfr, then, that tlie advaiiciiijiuohiinn of progress, having roaohcil nnilt'stalilisliL'd itsolf'in force all along the easte'-n froiitof the frnnf I'/niiis, from Jjonisianu to Minnesota : having, also, junijied over and flanked them to oeeujiy California and Oregon : — Assuming that this eolnmn is ahont to dehoiich to the front and ocenpy them with tlie embodied inipulse of our y(/i'_y millions of population : liere- tufore seattere0 Sheep 21,722,220 Swine 30,334,213 Value $655,883,658 It is probable that the aggregate ahoriginal stock of the Great Plains still exceeds in amount the above table. It is all spontaneously supported by nature, as is the fish of the sea. Every kind of our domestic animals flourishes upon the Greai Plains equally Avell with the wild ones. Three tame animals may be substituted for every wild one, and vast territories re-occupied, from which the wild The ancient discordances between urban and rural populations, manners, and tem- per, will find their asperities mutually modified. Society, rectified by reflection from the propitious powers of Nature, will insensibly ascend to an exalted level, illustrating the perpetual dominance and activity of peace, industri/, and concord. I 76 PASTORAL AMRKICA. Illl stock lias been cxfenninatcd by indiseriininatc sliiuglitcr and the inc^aso of tlic Wolves. The American peo[ile are about, then, to inaugurate a novel and immense order of industrial jnoductioii : Pastoral AauiciLTUUE. — Its fields will be the (IikU /Va(';M intermediate between the oceans. Once commenced, \t will di'Veloj) very rajiidly. We trace in their history the successive inauguration and sy.stematic growth of several of these distinct orders : The tohaccn culture, the rlcn culture, the cottou culture, the innnense provision culture of cereals and VKiifs, friil/irr and uoiifj thc'/oA/ culture, ((((c/y^//'^/; external and internal, cotiiitieire ^'xternal and internal, tmnspuftdtion by land and water, the hemj) culture, t\ic Jis/teri'es, munHfuctum. Each of these has arisen as time has ripened tbe necessity for each, and noiselessly taken and fillud its appropriate place in the general economy of our iiii/imtriiil empire. This fuiHtoral property transports itself on the hoof, and finds its food ready furni.shed by nature. In these elevated countries fresh meats becoyie the preferable food for man, to the exclusion of bread, vegetables, and salted articles. The atmosjdiere of the Great Ploiiin is perpetually brilliant with sun- shine, tonic, healthy, pungent, and inspiring to the temper. It corrcsjxmds with and surpasses the historic climate of Syria and Arabia, from whence we inherit all that is ethereal and refined in our .system of civilization, our religion, our sciences, our alphabet, our numerals, our written languages, our articles of food, our learning, and our system of social manners. As the site for a great central metropolitan city of the " Basin of the Mississippi" to arise prospectively upon the developments now maturing, Kansas City, at the mouth of the Kansas Kiver, has the start, the geo- gi'aphical position, and the existing elements with which any rival will contend in vain. It is the focal point where three developments, now near ripeness, will &nd t\w\T river jwrt. 1. The pastoral development. 2. The gold, silver, and salt production of the Sierra San Juan. 3. The continental railroad from the Pacific. These great fields of enterprise will all be recognized and understood by the popular mind, and will be under vigorous headway within the mature life of the existing generation. There must be a great city here, such as antiquity built at the head of the IMediterranean and named Jerusalem, Tyre, Alexandria, and Constan- tinople ; such as our own people name New York, New Orlean3, San Fran- cisco, St. Louis. nil i ': M^m.mmtm-/! V*v/j. I ■Tr-'f"- i..->- ^'^^ ■'■i! . ( I ir^. ,.4-^- /f.i '..1 I «■« I >l^ i.^" •'«».**a*.^J*«f»-''""^sj;''?5i!,v f';^ lanif^*- ? t. t ..3Wfe,- li^^' /•.^ c- I r I •r /_ >K* i/' '•■IT'' 'i ' -r-' if 4^ ■ir ^^rj-vu... i->As.i \ ■ - ■ . • ■ f'"i r 'TIlllJ.IlM I » '" .r4iib'ijty .i<: IMiiiiuik.|'T. ..■•>l-'<'- >--. . K A -' •ji«l.-tl •" U I >|.VP^Of andnorthern portion of THE SYSTEM or PA RCS. y: • ^ /" AJ^iAi^AlJiD'i: ^D. 'j - . •-•^; ^/i- .lb >^^^ ^_ j.ff_ X ^.-.l }.». £i). ^\>»rjf^ UnMk. /•■•■ >- J. V- ^. llaiiiiTiik' \»\ lllMllH-lll) ■'^'^i:. H v^-^ r%^-,/' /f ^^-•-^ ^--■^ S rSTEM OF i»Aau\s I //if BmESM RELATIONS Of TmQmT PLAm, IHK XOin 11 AMKUICAi ANDES, UIhI lli(> PACIFIC MARATmE rtRONT. >'■ : K J B L:pp,ncoti S Co Phi ,:., II *,- 1 i Ij '- -. f» i. I ^^ n " ARAPAHOESi I .»«■; I i^: .-i :^~ '"'■., •^\.v^" w r«»»'i F.n> A l,«wr»"' s \) . ^ n feC E C \ .1^, «7.i..*»""'""* * l,,«rt>>"H ,, L^ AX8 E rV'Ji.V;,,!.,. ietual venial temperature ; intense serenity and the most gorgeous splendor. They are bisrctcil successively, through and through, by tlie o«e Iiun- drcil and sixth meridian. Each one siiii/fy is of marvellous size, excellence of form, and eminent beauty. Th(! group, as they are blended into one system, '? miraculous! This springs from its dominating continental position: from the juxtaposition: from the immediate contact : from the intense variety and supreme grace illustrating every detail and i)ervading the entire structure. Kestricted especially to the System of the Fouk Paucs of Colo- rado, the S