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The following diagrams illustrate the method: Les cartes, planches, tableaux, etc., peuvent dtre filmds d des taux de reduction diffdrents. Lorsque le document est trop grand pour dtre reproduit en un seul cliche, il est filmd d partir de Tangle supdrieur gauche, de gauche d droite, et de haut en bas, en prenant le nombre d'images n6cessaire. Les diagrammes suivants illustrent la mdthode. by errata ned to lent une pelure, fapon d 1 2 3 1 2 3 4 5 6 32X m '!.'» -. astern ff^p^^.'mne^ •'.'r-." j , J m SCHOOL GEOGliArHY OF THE WORLD. V,Y J.4rt1-\LKIX, AM I.All, IN>,M.. h.|; MK >r| Is Fell; KIN, , s n .fNI V. PRESCRIBED BY THE COUNCIL Op PUBLIC INSTRUCTION S-ov illoc in the ilublic ^rhooK.. ACADIA COLLEGE DBkARY, WOLFYILLE. N,3. HALIFAX, N.S.: X ^ w. MACKIXLAV l.SG'l, (I^opiirigbt .^ccuvci). IIALIKAX, X P. : A. >\; \V. MACKIXLAV. I.c.VDO.V, EDJXBrRGH, AND XEW YoUK: T. NELSON * (iONS, A- ^■ TuK Am Nova ,>>e( Kiliicittio I'lir till' 1 grajiliiral I of itH lo, waiitH in to call ; j^'fiifial (staycs. First " Hints "' Tt'aclioi — the f((ll(i\v 1. Pnil Dcscriiif ; 5. Kelati\ 7. The 1» Soctidii ; I 11. Stiva 11. Clinial iiiid Aiiiiii ly. rursi; •Jl. The ( l:4. Linil r.iubo— it> It is till obsi'i'ving irt'ogrnpliici cocilin^ st(i wrvHtioii, I I! Vn nFACE TuK Amlidr wi.iiM l:iy tliis Imuk lieiWi-i' tlu' 'J'tjai'lu'i's <_>\ Novii r^cutiii as a Imnililt' triluitc to tlu' I'austi nf I'uMic Ivlncatiuii. Wliilst tlu' w.'riv may ii^it claiiu ar(,'c'[it.inL'i' I'cir tlic rt'Vi-latii)!! nt' new I'arts .u' iirincipK's in ;^'i'o- p:ra)iliifal scioufc, it is lielicvcil I hat a can'rul fxaiiiiuatinn • •i' its foatiuvs will iHsouV'T sjiecial aila|ilatinu u, ,,ur \vants in tlic sdidol-iMdni. lu this [ilace it may he well til call attciitiim to its Icailini^ i'liara(.'t('risti(s. 'I'ln' iTciui'al jilan im[ilics fnur '!i>tinL't au'l CMn^centivf stau'i-'S. First S*age — A rmMSK hk Okai, FiKssuNs, — Thf ! "Hints" ill this (Iciiartmcnt arc L;'iv('n as an ai'l tu tlir I Teadior — not tu In' stmlii'il liy tin' I'lijiil. They cniliracL' , the folliiwini; tupiis : — 1. Pdints fit' tin' Coiiiiiass; '_'. Tiaiii In Oliscivo ami ])oscrilie; H. Mainiiii.t,' ; 4. Train to .Juil-c I)istaiR'os; f). liolativc Position au'l Distance ; (>. Maji:. on a Scale ; 7. The I'lay (Jriimnl; s, Lainl Siirfacc in the Sdiodl Section; II. Waler-sheils ; 111, A'lvantaLres ot' .Mountains ; 11. Streams; ]'2. Henelits of Streams; 1:1. liakes ; M. Climate; 1;"). A Physical Map; It). Minerals, Plants, and Animals of the School Section; 17. InhaMtaiits ; 1J<. I'lirsuits; 111. Kiluration; lid. Civil llivisimis; •-'1. The County; li'J. Nova Scotia; '2:1. The W.aM; ■Jt. Laml ami Water; 'J'). Voyages; 'Hi. 'l"he Kartli a Globe— Its Motions; 'J7. Circles. It is the aim, hy this cniirse, to exercise tin- Piiiiil's ohservin.i,' powers, ami, hy shnwiii'.;' liini the nature o|' t,'eoi^ni[iliiciil Isiiowlcilge, to lay a foumlatinii I'nr the siie- cooding stages. From eonsidenilile t'N[ierieiiee ami ob- Kerviition, tlie .Xuthor is persiiaili'il that dial liessonM, >iniilar to tho>o suu''4c>teil, 'I'orm the tiii" aut'nl intrnilnction to the stmly oi (ieiiL;rHiihy. Second Stage. — This conM>ts, tir>t. of Lkssons on Nova Sciitia; ami, second, n\ a I.Iknki; \i, \'ik\v ob' Tin; ; Woiii.n, iiresi-nted by an imaginary tour. It i-. intciel.'d , to bi^ an ea>v tran>itioii iVnni oral lessons to t he I'rmal studv ical (ieoLcraphy. The twinhapters ■• Tin; Kautii AS a Pi.ankt'' and *• PiivsicAi, (InocitAi'iiv " are theiel'oie [ilaced at the be-inniiiL;' nt the n.nre sy,-temalie part oi the 1 k. I'nder •• Tin; Kautii a? a I'la-vkt " ilio following' topics are discussed ;-- FoiiM 111' the Ivutb ; Si/.K .'1 the Karlli ; I-hiiiT and l[i;\r; I'av and Nniiir ; I'lieijud i. i:\irrii oi' |)av; Clian^'O of Si:aso\s; Caii-e <<\ the Ivirth's An.mai, >' .>IoTio\ ; CiiKi.Ks; Zonks; liVTiTim;; .^I^:\s^Kl:M^:^■r of the Kartli; I.oN(irriiii: ; (lulline nf the Soi, \k Sr- ri:M ; the KAiirii \ IIk\vi:ni,v Ibmv; I'i.\M:r.-; Moon-; l''i.\ed St MIS ; the 'i'erre-liial (ii.oiu:, f I I I '• I'liYsii'Ai, (Ikoouai'Iiv ' embraees the f-llowing; — j The Karth's CitrsT — the l.NTi:i;i"K : the Tiiki; \ori;iii;,s (iLOUK — liWii. C'ltitinfiih, Isht.iilti^ S'ii-j\ii:<', Jli'ixr.if \\ 17 PREFACE. Jjiil-i'K — tlic Si;.\, its Exi'Mit, Ik'ptl', Cuiitciit^, 'JViii|)ora- tiiro, Divisions, Motions, Waves, Tides. Currents — the ATMK.-piri:!!!:, its Extent, (j'lniosition, I'rnpiM'ties, Re- llrction, licfriu'tioii, 'rcinporntiiro, Vaiiuiir, Winds, Rain. (Jliniate; T'i.ant.s, Axt>[.\t,s, IMw. Tu tliiS'' (lejiarttuonts it lias liecn tlic aim to jirocc-oil iVoni known plionoinena to prinoi[)]('s. shnuinL;- the de- jicndenee liy I'aniiliar illnstrations. 'I'iic paraurapli .i small type, (>inlivacin;j tlie more diflicuit parts, can be omitted by heninnci's, at tlu' di(icin of tin- Teaclicr. In order to secure tlte liii;lH'st practical lienefit, freipicnt '•oference i;-; made, in the succeeding cLaptcrs. to the principles of Physical (Icoyrapliy. Fourth Stage. — This embraces Xoutii Amkricv, South vSMKia-A. Krr;iirr.. A-i.v, AKiircA, and Oi t.axia. An out- line of each i;reat division is L,nvcn liel'nn^ tin' conntrie- Included in it are discussc^d. Ry tiiis coniprehiMi>Ive view the relation of (he different parts is more clearly appreliended. the Pupil cniiceivin,:^' nf them nut as isolati'd eouutrics, Imt as forniini;- one .urand wlmie. Cnnnuon features, alsci. are tlius learned once Inr ,'dl. Particular attenli'iii is invil"d io the rMi'msM aiiiianui;- Mi'.XT oi' Torn\-, liotli in the outlines and in the more detailed desei'ijitiiu of the dit'i'ercnt ee.unti'ies. Mvery- thin;:^ in thi^ part i<'( the \\nr\i is inclu'le'I under the lul- liiw iu'j,' ei^'htcen lnMrlinir> : — I. lIlSTiii;v. II. rosnii'N. III. FoiiM. IV. Coast. V. .\l;rA. VI. SllilAri;. VII. llivr.ifs. VIII. I.AKrs. IX. S..II.. X. f't.IMATi:. XI. Ml.^■^■.KAl^, XII. Plants XIII. Ammai.h. XIV. Iniiahitant.'!. XV. Pi VISIONS. XVI. Towns. -XVII. iNITSTIif. .:. XVIII. CJoVF.I!\MI-NT. These liendings will ]irovi^ ol' great service to the I'lipil in preparing liis losoiis, anil to the Teaclier in conduct- ing the vocitation. They will ho I'uund pretty exhaustive in the ui ,iter of Descriptive (leography, and will iurnish central points nroimd which nioro oxtciuleil Kiiowledgi>, derived from books or travel, will cliistcv. A consecutive ordu' has been sought after, so that ea^Oi topic might naturally arise out of the pnjccding — or at least that there shuuld bi no inversion of the true relation. With certain can>al facts obtained as dat^i, the learner largely anticipates those that are dependent. Thus the reason- ing [lowers being culled into action, the study of (ieography becomes a liigher exercise than a mere nicmnrizing of isolated facts. A systematic and unilbrni ;irrangemeiit will also greatly aid the memory, and will, at the same time train to habits of order. In the dirierent stages the s';KTeiii\(i of >:AI',s on the slate or on paper is conteniplat(>il. 'i'his ])ractice should go hand in liand with the study of (>very country. In nil other way can the l\ipil acquire so nccurate and in- di'lilile a mental picttire of the leailing physical features of a ci iiutry. The nr.i.ATivi; si/.r, or roi.NTiiiKs as cuiniiared with Nnva Sciitia will tend much to (h'linite knowledge. Areas are alsn expressed liy tiik sikk ok tiik siiCAi'E, as conveying a more definite id.ea to children than s^narc viifrs. Xumei-dus UKVIKW tiiF.STinNs are givi'u thrcuighont the work, which will tend tu excite interest and idicit thought. i']\'ery endeavnur has been made to give the nmst I'lKcKxr cuANiiKs ill tlic political relations of the various countries of the wm-ld. and aUn the latest re-ults of ex- phiiation and travel. T1h> AIai's have liceii constimctiU) with \ vii;w to roii- Ki'.cr coNCKi'Ti.'NS. Tlmse of the ,L;ri'at d'visii'iis are coliiured. to di-tingnish liighlaiul fmm lowland, (luyot's maps are taken as authority in this distinctiini. To I'oiti'.i'.cT the FALSI', iMi'iiF.ssioxs respecting the relativ(! sizes of cotmtries, arising from the use of maps on dif- ferent scales. TIIK Mai- of Nova Scotia is takkx as tup. INIT, by which all the others, drawn nccoivling to a R])epi(ie(l proportion, are lo b(> measureil. The TvrooHAi'iticAi, anh ilmstuativm auts luo laiil under tribute to embellish and add ei. .iveness to the work, ^'ariety of type has been emplnyed to catch the di topic iniLflit i )!• at least tliat relation. With learnur largely 'hiis the rcasoi\- the stii'ly of than a mere | tic and nnilbrm j eniory, and \vilL ")F >;Ai'S on the jjrai'tii'e shonid ry co\intry. In rciirat;' and in- tliysical i'eatures compared with ite knowled'.;e. THE StjCAKE, aS •en than fiqiiarc PREFACE. attention and Invalc tlw monotony .-su irk.snme to children ; and the pre]iarati.)n of lessons has not b,'en rendered un- necessirily impuMn- ;imi ,vj-n]ag,.'s I'jiysica! 'ieogvaphy; Kav's Outlin. .-. Suth rlaud's ( leo-niphy "f WE. ].: >hn.ry's I'livHcal (leo-.aphy n\' tli,. Sra ; IJaker'. AlluMt Nyanza ; ral-rave's Arabia ; A-assi/•^ 15ra/.i!; Collirr's Ijisiurics : Thum^on's Land and ihr U- luld,sh,.rshav,. his ho^t thanlc t^.r th. cheerful I IS.nk ; and various i:,.,,..rts on Trade and K iu.ati.n.. , . „...x,., .>, ,.x,, > ..,A.i, i.Aitv are .IrM-nrd f.^r rrfereiiee. I ].ippinr,,tt and Worcester are followcl, ehi..(ly, in thr prniiiuiciatidn. Th>- Anthur gladly avails himsell' of this space to .'x- liri'» his olijij^atious. Sonir of t!„. Huh.s and Ivxrrci.M's nu i!ir C],,!,,. aro takm from 'I'at,.'. Natural l')iiln>,,phy, nhich mav l„. mnsnlt-d ■'■la nn^parIng ell.,rts with whirh tliry havr exemt^k j,, the hi-hest style of art, tlieir part of th,. :v(irk. ^^ 3Ianv valuchle su^-gostions have heen n.vlv.d fnuu tur further inlurmation on the suLjcC. 1 . H. Uand, Es(i., ^r.A., Superintendent of I'.duralinu. -V large nnmher of h,,oks have keen consulted in the jnvj.aration (,f this w.n-k. Mvrh .-w^ist,,,,.,. l,a. l,..,.n do- ', Plants, Vegetable Zones. Animals, Man, Religion, Social Conditi in. NORTH AMERICA. History, &e., British America, Dominion of Canada, Nova Scotia, ... New Brunswick, (Quebec, Ontario. Prince Edward L^land, ... Newfoundland, Hudson Bay Territory and Labrador, Red River Settlement, ... ISritish Columbia and Vancouver, The United States. Walrussi.-v, Mexico, 2(5 2(5 28 28 2S 28 28 29 29 29 29 29 29 3(t So r.o -■50 80 30 31 31 31 32 32 32 3:; 34 34 35 39 40 41 45 47 50 52 54 55 5d 5(5 05 6(5 mM3 CONTENTS. Ccutial Amoriua, West Indies, Danihli America, SOUTH AMERICA. Ilistory, kc, Columbia, Ecuador, Venezuela, British Guiana, ... . . Dutch and French 'juiana, Brazil, Peru, .. Bolivia, Chili, The Argentine Ktiiulili.^ ... Para<:uay, I'ruguaj", Patagonia, EUROPE. Uibtory, &e The British Isles, England ami Wales. Scotland, Ireland, United Kingdom of Great Britain and Ireland British Empire, Norway and Sweden, Denmark, Russia, Prussia and North (iormany, Austria, South Germany, Holland, Belgium, France, Switzerland, Spain, Portugal, Italy, Greece, Tur'kev, ASIA. History, &c., Asiatic Russia, ... The Chinese Eiuinre, China Proper, Subject Territories, raoO cs 70 1- 7tJ 77 77 77 78 73 71t 7!' 71» to ?0 80 SO SI 60 87 i llllll 'I'l " 124 124 124 125 125 125 126 126 127 129 130 132 133 133 131 135 139 I 139 ! 139 I 140 I 140 140 140 141 141 141 142 142 i42 143 143 143 143 143 143 144 145 146 147 147 150 151 151 152 HINTS FOR ORAL LESSONS OX OECh.IKAPIIY 153 165 The yuuug stiuleut uiiglit i^t to fnl that iu the .sclioul-ruom he is isulatcd tVuiu the world oiUsiile. The teaclicr should Hut earry hiui, as it were, Miudfold and st-t Iiiiii down in tiie very niiilst uf the unknown, where all ou this side and on that is unfamiliar and .strange, and wiiere he ean have no recourse to knowledge already ae(iuirL'd, as a key of inter- jiretation to the new and unsolved. Ou the eontrary, wiiat- ever may be the new suljeet to whi h we are about to introduce liini, we should first ascertain what is his present standing ground, or knowleilge, relative to the iiro.siiL'etive stu]iosed to constitute single lessons ; on the eontrary, most of them will be f mnd to contain material sutHcient f 'r a nundier of Ics.sons. (iL'TLIXL: oK a Cdfll.'SK cF OUAL LI>:SSONS, ', lS"TlU>Iir draw a map upon their slates. 4. Train to Judge Distances.— Show tlie c! '.dren, by means of a string or stick, an inch, a foot, a yard, and a rod. E.\ercise them re- jieatedly in drawing upon the board or lloor lines of these various i lengths, causing them to test their skill by applying tlie measure. Vary the exercise by calling u|ion the children to judge of the length \ of lines, their own lieiglit, the lieight of doors and windows, the dis taiice between objects not very remote from caeli other — always ajipiy- ing the measure to test the accuracy of their jinlgn. '■..'. 5. Relative Position and Distance— BoundarliS.- Cause the chil ' dreu to observe tlie various objects in the school- ■■ .n ; their size, j relative position, and distance from each other. Show them that the j room is limited and its form determined by tlic walls. (Jive the term i ?/i)»/i(/(M'(/ ;— the room is bounded by the walls, (jail for a descrijition [ of the room, the objects in it, their j.osilioii and uses. Direct the 1 children to make a map of the room uu their slates. ■kfi HINTS FOR ORAL LESSOXS OX GEOGRAniY, 6. Maps Oil a Scale.— Dnr.v upon tlie V)l;iL'kiioard two maiis of tlie Rchool-ruom, one consiiicrably laru'er tlian ilie otlier. Show that both are equally eorreet ; that neither is as Iari.'e as tlie room ; ainl that it would not be possilile to make a map upori tiie hoard equal in size to the room. Show the crand point of raaintainini,' a linc pn^port'on in tlih ma)), eorrcspondlns to the relative sizes of the ol)ject3. This may lie made plain hy drawins the i)icture of a man with the arms extend- ing to the feet. The children, notinp the disproportion, will say that the arms are too lonsr. IWUv^ . ..t the idea of relative length, liy sliow- injr that the arms in the picture are not so loin.' as their own— thr.t they are too Ions; only liooause they do not correspond with the otlier liarts. Show them that in making niajis it is usual to let some definite short lenu'th rcjiresont a lon^rer one, and that this is called the urale cf the map ; toll them that the upper part of the map generally represents the north. Let them now make a map of the school-room liU some given Kcale. 7. The Play-Ground.— Direct tht children to examine the play- (.'round and the objects in it ; ti/ jndj^e of size and distance, testing by measurement; to describe the friound, Bhowing first its jiosition with respect to some prnniine'it object— as the brook, river, woods, village, and church ; to give tht .oundaries, lorth, east, snuth, and west ; to state the size of the ground, its surface, the objects in it, their position, uses, kc. Call upon some one to make a map on inc board, according to a given scale. The others criticise. Oorrect errors, etTacc the map, anil let all draw it njinti tli.^ir slates. 8. School Section— Land Surface.— (Question tlu .'..ildren as to what they have observed resiiecting the inequalities of the surface "f the iieiglil)ourhood. Some places are level, like the floor or play-ground ; in others the earth jises up in hills. Tell them of level tracts at large th.at they couli! not .see across them, and give them the term phin. Ask if they have seen a very high hill which it would take some time to climb, — wha^ they call such a hill. If there is no mountnin near, and they liavH not seen one, question them respecting the highest hill in the neighboiirhood. Some object is six or ten feet high ; how many such heights would equal that of tlie liill. Ten such hills, one upon nnother, would make a veiy high hill, which would be called a maun- tain. This would >e a low mountain ; for fur away are mountains twenty or thirty times ns high, rising above the clouds. They rise into the cold air so far that their tops are covered with iierpetual snow. Tell them that the snow collects in vast masses; ar.d they will see that, as it cannot melt, it must plip down the sides of the mountnin, forming an m-dhuichr. '.'. Water-shed. — Hy refennce to some detached hill ami lengthened r.ange, show the diH'erence between un isolated mountain and a con- tinuous rniige or ch: .i Draw from the children, that when they luive leaiheil the top or summit of a range the ground falls oil', or b1o|)CS in the opposite direction— that it is somewhat like the roof of a liou.se, sloping in two ways; that when it rajus, the high ridge along the top will seiiarate the water as it tails, throwing some in one directir.a and pome in the opposite ;— that this ridge is called a watvv- nhfil. It'. AdvantftRCS of Mour... ,13.— If the ground were i-.ll quite level the rr.in could not run off, and the earth would soon be Kiturated so that the water could no longer sink in. If the children have seen a swamp, it will fiiriiish a tine illustration. Show what would be the result with respect to the vcgetalde kingdom— muny of the most useful plants could not live; hence food would be wanting to many animals. So lunch water in the soil would cause disease miuuig men. The chiliiren have seen a ipring. Show Jiow it is formed, and ciuild not e.\ist if the 'iliole surface were a plain. Other benitilK may also be noticed, as shelter against winds, and the comparative ease with which minerals ran be olilnined fiom ihe side if a mountain, (^unlensatioii of clouds, and •'••'vr I'liniatie beiiclits, will perhaps be loo much advanced at this i>..gc. ll. Btreauil.— Taktt the blrva'i with which lliv children are i\ tl familiar— the brook where they have been accustomed to fish, or to .sail their toy ships. Is the water still ? why does it flow t Illustrate by pouring a little water upon the level lloor, and then upon the inclined desk. Show that the rapidity of the stream is .n jiroportion to the in- clination. Flowing water is called a stream— tht} brook is a stream ; very large streams are rircrs. Does the water flow along the surface '> No, but in a groove, the chiintul ;— the bottom of the channel is the Kal ; along the sides are the Uinks, the rir/lu hand and the ^'/< hand bank. What made the channel ? Illustrate by what they have .seen along the road aftc a iicavy rain ; show how the depth of the channel depends on the velorjty of the stream and the softness of the ground — how the stones in the bottom of the brook have 1" cu worn .smooth. As the children go up the stream, they oliserve smaller streams flowing inio the main stream— giving or contributing their waters ; these are trihutarkg. Followinf; up, they finally reach the Ovooklct hastening away from the sjiriii;/ which bubbles up on the side of the liiil or mountain; iliis is the nource of the stream. Now descending the stream, they find it beeoming larger as the tributaries flow in, until at length, by ^he union of many brooks, they have the rir > ; and the further the river llowr, the more tributaries it will receive and the larger it will become. Where does the river go ? If the children liavo seen the sc.i this will be readily explained ; if not, it will be necessary to give a le.sson on the vast body of salt water w hich covers three- fourths of the Kartli, into which the rivers flow. Thus, coining back to their homes, the little brook where they love to sport is hasting away to the ocean ; the water which they see in it today is not the same which they saw yesterday, and to-morrow it will be gone, ainl other water will lia-t taken its jilaee. Tell the children of some of the great rivers of the Kartli; and, by comparii^on, give them an idea of their size. 12. Benefits of Streams.— Lead the child'-en to see the dependence of springs, brooks, and rivers upon inequalities of the surface ; also how they can find the highest ground by tracing the brook to its source. Direct them to discover the julvantages arisin,. fioin sjiriiigs, brooks, and risers, taking those benefits first which are most obvious. They get water from the spring; the cattle get drink at the brouk, perhaps not far distant ; the stream turns a mill. Call their attcntiiui to the general fertility of the soil along the banks of streams ; remind them of the dependence of vegetation upon moisture, and show the absorbing power of the soil. They have seen the stream overflowing its banks in the spring, and have oli.served the deiiosit of mud. They have seen the Carrier spreading his top-dressing, .tc. Interval and marsh might also form subjccis for lessons. Show the facilities for iiilercommunic.atiou afforded by large and navigable streams. lli. Lakes. — From some pond in the neighbourhood develop the iilea of a 1,1 k(>. Tell of some the latter. This will afford an illustratiiui id' the cause of tiie varied iiower of the sun at dill'ereiit times of day, and at different seasons of the year. (Do not itttempt at this stage to c.\|>lain more minutely the cause of the seasons.) Show that the mountain is colder than the plain. This they can infer from the fact that there is often snow there when there is none upon the low grouii '.. They can also infer tlml shqie inthiences temperature, by comparing the south side of u hill with the north. Show the cooling effect of evaporation of water from the t arth. Various illustrations may tie used for this pur- pose. A bottle of water, wrapped in a cloth kept saturated with ether, may be froitcii in a lint day. (/olugiie water poured on tlie skin jiroduccs cold. It requires heat to clianKe a lii|iiid to the form of vapour, and heat is tiikeli Iroin the bottle or body for this purpose — the liquid having combined with heat, bei'omes vapour, and escajic^ into the atiuuHphere. So also tipriiiiiling water iijiou the floor un a !o.>l 1 oiiiod to linli, or to sail I flow '> Illustrate by tlieii upon tlia incliiieil II jiroportion to the iii- le brook is a stream ; low along the surface '! of the channel is the and and tlie left hand y "hat tliey havi> seen 3 depth of the clianael (ftness of the ground — re been worn smooth, mailer streams flowing lioir waters ; these are the brooklet hastening he side of the hill or Now descending the ibutaries flow in, until ave the rir.) ; and the t will receive and the ? If the children have ot, it will be necessary 3r which covers three- V. Thi's, coming back fe to sport is hasting in it today is not the V it will be gone, and le children of some of in. give them an idea of to see the dependence 's of the surface ; also icing the brook to its s arising from springs, hioh are most obvious. drink at the brook, Call their .'ittcntiini s of streams ; remind sturo, and show tlie le stream overllowinji eposil of mud. They ig, kc. Interval and how the facilities for )le streams. lood 1'.'. Education.- tJivo lessons o# the edinatioii'il eiuidition nf the Kclion ; the .idvanta^os of eilii/timi In the iiiuividual himself- personal satisfaction, etlectiven /i ol I'llmur guided by intelligence, avoidance of dangers, fn\ ; the llvaiitages of livliiK in a eoinmuiiity where all are editonted-gratKleliioii iiiil.inil. a cajic. a peninsula, v'^ic. IHvicI the jui/iif.i tn ninke a »i(i/) of till full III II. 'I'l. Nova Scotia.- Nova .^coti.i may now bo takiii up .is a 'vholo, givim; first some of the interesting points of its early history, nitlioiit rct'erring much to preei.se dates. Tell of the Indians, tlnir mode of life when the eoiiiitry was discovered— of the conditimi of the country at th.it time — of the early French settlements— the name Acadia, oivon by the I'lench— the capture by the Knglish — ditliculties of settle- ment, iVc. (live an idea of the size of Nova Smtia by cdinparison with sonic known area— give lessons on the leadiiiL' physical h'.'itiires, as nioiintains and rivers— then the I'ivil albiirs, pursuits, gov«riinient, and political nlatioiis. I tin ft I lie jiii/iituli) iimktn inapo/ I lie rmriiice nil It i/ivi II uriili . 'J!i. The World. -A IVw incidental lessons should now be given for the iiiirposo of calliiii; attention to other parts of the world. Home familiar article of foreign produce will furin a good introduction. A barii 1 of tlour. for instance, will le.ul to a lesson on Ontario, or tin.- I'nited States; a |iieei' of broadi'loth, to one mi Kiigland ; an ostrich loather, to ono on Africa ; tea, to one on ('liiiia, iSic. In this way thu children w ill see that there are many coiinlrieH with which we have intercourse, and they should point ;• t', direction in which the various countries are situated with respt i ' Nova Scoli.a. Tlitlr interest having been excited, they will be anxious to know how intercourse in carrieil on with foreign countries. This will le;id to conversation about long Viiyiii:i'S over the sea. -1. Land and Water.— Lessons may now lie given on the Kurtli, as coiisisliiig (d' lami and water— tin ir proportiniiH-lhe beiielit arising fnuii their rehitioiiship— Imw a country is lieiiefited by inlets of the sea, referring to the b-.yii and harbouis of Nova Scotia. The great divisions of land and the L'leat oceans can lie pointed out. and their niiliies given. '.'.I. Voyages. (,iuestion the pupils as to the mode of represent iiiu tho surface I if the Ivirlh by maps — show the Hemispheres as representing the whole Kiiih ; that, althoiiidi on separate sheets and apparently two Worlds, they are united Trace voyages, carrying products of ono eoiiutry to niintluM'— awaken euriosity by telling of vessels pursiiliiK geiiprally one course, and finally arriving' at the starting-point. 'J'l. The Earth a Olobo its Motions.- Show ;i globe as a correct representation of the Iviith -that this is prove'l by uoitig uniformly in I one liiructioii, and at last arriving at the stailiimpoint. (Hve other sn HINTS FOR ORAL LESSONS ON OEOGRAPHY. siraiile iiroot's. llliisirate the Eiiitli's ilaily rotation— its axis— tlie jioles— ilay ami nlL'lit. liy canyini; a ball arouuil some central object represfiitinf; the sum, ex)iiaiii the Kaith's annual nintii.ii and the seasons. It can lie shown that the sun is never directly above our head l.eyond tliu Lreadth uf a belt around the middle of the Kartli, equidis- tant from th'j jioles, and tljat the sun crosses this belt twice a year— that on account of tiie !.'l'.jliular furni of the Earth, the sun's rays fall more and more obliiiuely as we ^o from the central belt toward llie poles, and hence tlie cold incn.ases. '27. Circles. — Lessons may now be ;;iven on the enuator, the tropics, the noitliern and southern liemisplieres, the live zones, latitude and I 'Uj-'itude. The children having jiroviously been tangiit the position of the poles, the ecpiator can be shown as a circle midway between the jioles, also as dividino; in two enual jiarts the belt which tiie sun crosses twice a year. Show the iniiiortancc of knowing.' the dij,tance of a )ilace from the i'(|iiator — that the distance bitweon the equator and each ptern part of Nova Scotia earlier th.an in the western, (tive the difference in time between London and Halifax, and show how the longitude may be calculated. To pivvc nt luisiiiiiivlieiisiuu resijoctiiig the lU'ecetling Oral ExorcLscs, it iiuiy I"' \w]] tu rcprat, tliat it is desij^'iietl tiiat tlicy slidiilil 1m' ^uwiAy j>)i'/i'(r"tori/ to tlie Ry.steuiatic .study i)f o'eogi'apliy fioiu the te.vt-buolv. Great a(lvanta;,'e will aho result tVoiu uuiitimiiiig sudi exerciM'.s after the book ha.s Itecii lihurd ill till' Imtuls of the inijiil. If Ex|ilaiu liow wo s runiiinj,' iiHith ami sbiiig the ei|u;Uor at uator is huii|insf(l to ; tlit'i-e is no natural al to begin with the ISO dfgiees east and »t uu the same meri- icotia eailiei- thati in .undoM and Halifax, le procoilin^' Oral is elesi^'iied that systouiiitic .«tii(]y Viinta,i,'e will also 111' book lias lii'i'ii SCHOOL (lEOGKAPlIY. XOVA SCOTIA. IIAMI AN. Introduction.— 1. Tiiis book i.'* written ffipoijally for the cliiiilnii wliii livi' ill Xova Scotia— to tfll tlicm not only abi.iit tlit'ir own country, but nlso of many otlicr <'(Hiiitri(>s. wlicro all till- people in tlic worM live. Many of you have never been viiy far from home, and have not «een inueh of the world ; ho you should bi' j'lad to read and learn alioiit it. Yon flhonld learn tirat all you e.m altout your own in'ii;h- bourhood ; then iibnut vniir own I'oiintry ; then alioiit all tho eountriea on the Karth. ThJM study is ealled (,'<:,■ 2. I Mhnll not nndcrliiko to tencti ymi th» srcoanqihy f)f your rwn Ki'ctioiij fir you lmvi> pyn tn m-p with, iiiid nther s-'iiiie^ tn hi.lii you In Ki' knnwh'dKi', iitid ym hnvi- tVot fn entry you ororywli.TH mound hhiinf, thi.n, if you kU not know f.ir nnro al.out the hills tho valiys. tlie hrioks. tho .'<|.iin.'.<, tlio fi\'^x\<-i. th.- wild iImw.tm imd tp>..., tho l)irdnand wild aniinids tho |iiodu''t.H of the tiehlH. tho ooou|i:itlHi,f( of the |'eo|i|f, and many nlhor things of intcre.tt around you, timn a RtraiiK>.r, 3. (In nnottiii- |.,Tao in iv ni:»ii of N .va .'^Mtia. I liopc you all know soiiiothing al'uut makiiii: tiiiips, and tiiiit you will try to niako vitv jjood oiiei. I liavo seon 'luite small hoy.s and girU draw ina|iA almost an jtood a» this. You oliiMivo that til" I'mviiio" of iV iva .Se tia coMHisn of two nnturiil divisions, nciiarati'd by a iiair iw lasw^o of wati^r Allied tho Sinni uf Citnoi). i. Tho Inrsor divi«ioM, ealled Xora Sr^itin, and nomcliines Xurn Si'i'tia Pr<>i>'i\ i* ni'arly surr^ und(?i| t>y water, and lien-i.' U cilled a pfniniuht ; and the narrow n*i'k if land on ih" nnith, where tliero U no wat'r, is enlliil an i-iUniitin. The Mimlhr divi^iun, naiiiod t'li/ir Unl'iii, In i|uil« nuirounded hy wabT, and iMtheief>re ealled an itliiml. your .iciuhhourhood where knowledge can l.« gained. It is a great | Them; two dirisions form the I'nn'incc of .Vor.i .SiUi-i ....,,.,:^.mm«*,.,..mr^.:rij«;^A,ammSie^ NOVA SCOTIA. I. History.— 5. Lung ago, our lurttathers lived far away to tlie eastward beyond tlie ocean, in Europe. Nova Scotia was then inhabited by Indians, the ancestors of those wlio conic to our houses to sell baskets or to beg. They had no cultivated fields, or fine houses with gardens and orchards ; but tiiey dwelt in rude wigwams, and lived by hunting and fishing. The whole country was one dense forest, the home uf innumerable moo.se, caribou, and bears. 0. Nearly three hundred years ago, some Frenchmen, who had crossed the ocean to sec America, tlie land of the Indians, visited Nova Scotia. They were so iilea.sed with the country that they determined to make it their home, and accordingly formed a settlement on the shores of a beautiful basin, at a place now called Annapolis. This jilace, yuu will see by the map, is in the western part of Nova Scotia. Tiie French, however, diil not call the ])lace Annapolis, but Port Ji<>;/'(/. 7. To the whole country the French gave the name of Acodie, or Acuiliu, an Indian wonl said to mean ahnndaitcv. Hence the early French settlers were usually called -1 cadians. The Acadians had scarcely got well established, when the English came, claimed the country, and destroyed the settle- ment at Port Koyal. The King of Em land, wiio was a Scotcliman, gave the country to a friend of his, also a Scotchman ; so they namevl it Vom iScifi'i, which means 8. Fur more tli.in one luuuliud ye.irs it sceiiuil uiKvrtiiiii wbtthiT Fianee or liiitalii was to owu Nova Scotia, so I'lcinitiitly tliil it pass from one to tlie oilier. Hut aliuut one liuiuireil and tilty years ago it was tinaliy aekiiowleilfe'ed as l'iiiti.^li territory. Toil Koyal, at lliat time tiie most iuiiiortant jilace in tlie coiinlry, ll.en rcotiveil tlie name i{ AiiiKiiiiilis Hi'/Kil, or tlie <.'it;/ uf Queen Ainic. Tlie Acailiaiis were toll! they njiglit remain in tlie LNiintry if they wouM become liritiah butijects. J'. There Were not many Hriti.sii settlers in Nova Scotia until 17-lS', n, little more than one hundieil years ago, when Governor (.'oruwallis came with a company of oolonistsi, selecteil a situatiou by the sen, cut away tiie forest, aiul began to biiiM the city of Halifax. Y lU will liml the place markeil on the iiia|i. The Iiiiiiaiis, whu had alv^ays been friendly with the .\cadiaiis, wire I'lr many jears viry hustile to the En^'lish, (h'slroyed tluir (iroperiy, and cruelly murdered and scalped any persons w h lu they fuuud uu- protected. 10. lu those early times the Hritish and French nations were ahuost constantly at war, and they iifien sent their war vessels across the Atlaiitic to America, for the purpose of destroyint; each other's colonies. The Hriti-h colonists in Nova .'^cotia became very much ithirmed, le-l the Acadians should join the French to do them harm; for the Acadians naturally liked their owu couinruucn and king better than any other. II, Accoidiiiijly, the Governor *ent soldiers who seized all the Acadians that tliey cmild find, put them on board vessels, and sent theiu out of the country, 8evvral thousands of these iioor people were thus taken fioin their beautiful Mttlemeiits of Ur and I're and Canard, in the east uf KIuk's County. It was very hard to be forced away friuu ilitir Cue farms, houses, and orchaids, and set down destitute in a stran;;e laud. A few ran aw.ay and hid in the w oods until the danger was ovL-r. 12. The French still held the Island of Cape Breton, and they h.iJ built, ou the south-east coast, a very strong town called Loaisburj. The British touk this town in 1753, a little over one hundred years aj;o, and they have owned the island ever since. II. Position.— 13. Nova Scutia lies on the west side of a great ocean called the Atlantic. It is bounded on the north-west by the Bay of Fundy ; on the north, by New Brunswick, Northumberland Strait, and the Gulf of St. Lawrence ; and on the other sides by the Atlantic Ocean. Eiij;laiid is so far tast that the sun rises there four hours earlier th.iu ill Nova Scotia. III. Form. — 14. The Peninsula of Nova Scutia is like a trunnjle, with the base mi the Atlantic, and the apex at the isthnuis. The Island of Cape Breton is somewiuit ovate, or fj;/- fhajitd, with a triangle jutting out on the north. EXERCISE.— Draw upon your slates the general form of Nova Scotia aud Cape Breton, IV. Coast.— 15. The land bordering on the sea is called the cuUff. People who live near the sea liave the best means of sending their produce to market, and ','f obtaining such tldngs as they need from otiier countries ; for goods can lie carried in vessels clieaper than in any other way. The length of ctiast is therefore a matter of much importance. Y'ou will see by the map that Nova Scotia is lonu and narrow ; that it is nearly surrounded by water ; and that the sea often runs up into the land, forming ''((.".i aiid huriuurs. K;. Let us take an imaginary tour around Nova Scotia. We set out at Ilai/ Viite, on the north, from which wo enter ^'of' Ihiimlerland .itrait. tt iiig eist, we pass J'lii/icatli, Wallace, and Txtuiitiiiiourltc harbours; also, Malu'jdnh I'yiiiit and VajiC John. See I'irf'U /flami, with its light house. Hero are vessels coming out of J'iiiiiu IJarbuitr, laden with coal fur Quebec or Slontreal ; in a few weeks they will return with tlour. Yonder also comes the steamer from Charlottetown. A little farther east is Meriijumiiik J/arboiir, Cajie .Sf. O'eonjc, St, (i'io)';/( j( A'l/,'/, and the .Sirait af <.'((ic id to he 111"! Ctet ire (re(|ninlly cast 'ijii/.i Ai '(()((/. It tu tend the liffhts (i /'('(( /ji'in il'Or, is the Iiilaiiil of -liDid tiie ehauuels .1 i. inhmd "ater» AT1K.\— SrHFAPE. S have several branches ; as, East Dai/, West Bay, ^t. Denis Basin, Barra Strait, St. I'atrick's CItannel, and U'hi/koUinunjh. They extend nearly across the island, leavini; only a narrow neck uf land, abuut hulf a wile in breadth, called St. I'ltcr's hthmus. 19. Passing south from Little liras d'Or, we come to Siidm ii Ifarlvur, which is said to be one of the best harbours in the world. Here we shall find many vessels loading with coal for Halifax, Quebec, Mont- real, and the United States. Perhaps, al-o, we may see the i-teamer from Newfoundland, which tails here on her way to Halifax. Cual is very jjlentiful near this coast, and vessels are luading with it at Limjan, Olace Bay, anil Cow Boy. Here is Mire Bay, and yonder is Si.'.darl Island, wlit-re the li.«her- men cure their fish. '20. We come now to Lonishunj Harbour, where stood the old town iiuilt by tiie French. A few fishermen's houses occupy the site. We pass Gat.arus Bay and come to I^le Madame, on the north of which is Lcnno.c I'assaijc, and on the east St. I'itir's Bay, from whicii liie Iieople are making a canal across tlie istiinius to the iJras d'Or waters. On the south of Madame is C/udabucto Bay, nuttd for its mackciel ti.>:hery. Ou this coast we shall see many fishing ve.--sels, whose head- quaiters are at Aricliat, on Isle Madame. 21. Here is Cape Caiiso, near which there was an important settle- ment in the early history of tlie country. Away to the south-east is Sable Island, surrounded by dangerous shoals, on which vessels have often been cast away. Mtn are statiuned upon ditferenl parts of the island to give relief to the sliip-w racked. There are also druves of w iM ponies ou Sable Island. 22. As we go south-west, along the Atlantic cuast of Nova Scotia, we shall pass a great many fine liarbours, too numerous even to give all their names. This cuas; also abound.s in tish, and we shall see many fi^hing vessels and boats. Here is HiUiJ'a.c Harbour, which is very deep, Kir^e, and wtll )iro- tected from winds. The upper part of the harbour is calkd Bid/orU Basin. Halifax is on the west side uf the harbour, and Dartmouth is I'll the east side. Here are shijis from various parts of the worlil ; — Iroin England, with 'oitoiia, woollens, silks, and various manufactured g ods; from the United States, with dour; and frcim the West hulies, with sugar and molasses. 23. P'orther wxst are Manjanl's Boy and .Malr and Cape Split ; but uh we come rund Cape ItUonidim, which liscii boldly near 60(1 feet, the waters widen out into Minas Basin. The shore on our right, along the basin, is (|uite low, and we piiHs the iiiouths of seveial sniall riviis. Tliose scho iierM coming down the rivers fioni Cuunini/, Canard, auil I'ort Willtanis, aiu cairying I otiitocs anbberving awhile, you would perceive that there is a regular rise for six hours, and tlien a falling' away for the same time, as if another sea wtre )ioiired in and tiieii !■ lil' d out again. This rising and falling is called the tide. The head waters of Cobe([uid Bay and Cnml'crhuid llasin are re- markable for very high tiiles — the ditl'ereiice between the kvol of low water iuul high water being 00 (jr 70 feet. EXERCISE You mtiy now trace the coast line of Nova Scotia and Cape Breton ou your map slate, marking the names of the bays, harbours, straits, capes, and islands. V. Area.— 20. If we could change the .shaiio uf Xova Sco.ia so as to make it a iwrfrft Ki(ntain,*, The land whicli seeniM aost level has a slope ; and where there is a nrook, you can tell by its course the drcction of thu slope. l.S Mllc^. *M-smwsmimf9ii!^,$i, ■I' ' NOVA SCOTIA. 31. A ridge of laud slupiiit! in oiiijosite directions, like tiie rocf of a house, is called a u-atcr-shcd. If you look on the niaji, you will see that there is a water-shed runnin:; throucii the middle of Xova Sooiia, froin one end to the other, from which streams are tlowing in oiiprpsite directions. Tiiis we may call the backbone of Xova Scotia. 32. The liii^licst mountains are in the nortli of Cajie Breton ; but even liore they are not very higli, not exceeding lialf a mile. The Cobe'/xid Mountains, ahing tlie nortli of Mina.s Basin and Cobequid Bay, are about one-fifth of a mile in height. They form a wator-slied, throwing streams to the north and to the soutli. In the western jiart of Xova Scotia are tiie .South Moun- tains, forming the western l]'.i!f of tlie backbone. "We have one other mountain range, called the Sovih Mountain, whi'^h foims a wall along the south of the Bay of Fundy, from Blomidon to Brier Island. lletwcen the Nnrtli and ."^onth Jlountains is a hcauiiful and fertile valley, from 5 to 10 miles liroad. it forms two gentle tlojes, one un the west and one on the eas'. 33. You have .sonieliines seen sn'iw upon tlie nioiiiitains when tlier-^ was none on the lowlands. This is because it is cidder on tiie niountains. In some countries the mnnnt.-iins are so hi^h that they are covered with snow all the year, and no (me can live uji'in them. EXERCISE.— Mark th. mount.iins and water-sheds tipoii your outline map, VII. Rivers.— 34. ]\[ii(li of tlie rain whidi falls sinks inti^ the earth ami forms springs. The springs send forth small streams, which, uniting as tliry fluw over the cuiuitry, form brooks and rivers. The water-sheds in Xova Scotia run lengthwise, so that tuost of the streams are thrown across the cnuntry, and very sonn re.ich tiie sea. The rivers, therefore, are quite small. In some countiies the rivers are «o larce and Ion::, that ves els can go up into the land fr luuulreds of miles. The longest in X"va .'^cotia are not inue-h over ;"iO miles in Icngtii. 3"). The following are the cliicf rivi is of Xova Scotia ; — On the south of the central water-shod— Oiw^^v/ZArr'^oz/r, St, Maiifs, Liscomh, MiilJ/'' li'ir' r, Mn.iqnoi/oboit, ,S irkril/i , Goi<\ La Have, Prtilr, I'ort Medu'dn, LivrvpooJ, ,/oi'ilaii, lioseway, Clijih', Tudil, and Si.i.tifioo, . , On th(! ntirth of the central water-shed — Annapolis, Jjnav, Af/tn, J/ahitant, Canarfirn>i, Avon, St. Cvoix, KnnnHi'i'ok, I'l/if'', Slnih,naraili<; Sti'iriavki', Miihfh' Jfivfi' of Pictoit, Kant J'iv'V, Sntfu'rlanii, I'vnrli llarnif, Rirjhl's, Wfst, South, ntnl Pomkit. On the north of the f'obeiiuids— //''/cr'. Marran, Xa/ian, La J'lanr/n, Mis.fa'inash, Skimmivas, J'/tiUji, Pu[in\uh, Wallace, Wahijh, and John. 0.1 tiic south of the Cobeiiuids — Paitriiliie Jslanil /'irn; Great Villaiie, Folh/, Dn /iert,C/iiijnnois,Sort/i,n\n\Salui Harbour Lake, in Nova Scotia ; and Ainslle, in Cape Bretnu. The.se lakes are iiem 10 to l.j miles in length. In some countries there are lakes nearly twice as large as all Xova Scotia. EXERCISE.— Lay down the principal rivers and lakes on the out- line map. IX. Soil.— 37. AVe see the farmers plougiiinii-. casting in their seed, and afte.' a few months storing their harvest. The ground which tiny cultivate is called sod. Sume soil is rocky, or cold and wet. and unthing will gncv on it ; other S(i;l is fertile, and yields larue crops. If we were to travel through Xova Scotia, we should find, generally, the best farms in that jiart of the country which lies north of tlie ^eniral water-shed. In all parts if the Province, the soil along the margins of the rivers is ferti'e. X. Climate.— 3'^. Snme countries far to the south, as the West Indies, are very hot, so that frost and snow are un- knowii ; others away to the north, as Labrador, are so cold that the gn-nnd is always fruzfii or covered witii snnw. In some countries, as Brazil, there is a great deal of rain ; in others, lil:( Kgypt. none at all. In Sdiiie the air is jiure and healthful ; in others it is poi.soiious. In speaking of those things, we use the W(ird climate, and say that a country has a cold or a hot climate, a moist or a drii climate. 30. As we have neither the great heat of southern countries, nor Ihi severe coM of those in the north, we say that X"va Scotia has n frifi- prraic climate. Our climate is also V'ny healthful, so tliat jieople live to be as (lid in Nova Scotia as in any other part of the worM. XI. Minerals.- 40. The s'unes wlii<'li you see lying about the fields iire called mineral substances. CJuld, silver, iron, and real are also minerals. Some of the most useful and valuable niinernls nro Iniricd deep in the earth, and men will are employed in digging f.ir tlum are called miners Miners often go very deep, diggiiig under fields and citie,-. ami even under the sea. 41. The most important minerals fouml in Xova Scotia are. coal, iron, f/old, fii/iisuni, lime, granite, flale, and tjrinil-ston<:, SI 42. Scotia. Coiintv colliers beneat! vv here eive lij where tub am would !•■ ; have to sun fur fill both xn. a count heat, I) water, best in 44. A native i These f( oak, are houses, i There all, no d spring, oft emblem of 45. Th baeJnt'hea raise iche^ certain. In the valley bet large orch XIII. i ous than with fore.' afraid of I as lie niig tigers, and 47. The Scot;:i, liv caribou ia The bear, weaker an Jioiiltry. There are tt'iil'', rahin, , fi'ivrv, (liirl:, Insects. »hicl ■IM. I„ |,„t Thu huge boil M fey 1 "tt^r. ■ r.'i- Middlt, i>t. Ut'iis, ^lountains, the b'rearas s into a basin-like any lakes in Novu particuliivly on tliu at they arc often in ince are — Rossi'jno/, Nova Scotia ; ami are if n; 10 to LJ ee as large as all Nova s aud lakes on the out- iilougliinL'. eastin;.' in torins their harvest. oil .<"(','. Sfime soil i^ ill Livii-.v tin it ; other i-e sliouM fiinl, coiierally, Iwliicli lies north nf the ineo, tlio s^'il along the to the south, as the st anil sniiw are nn- ihrailor. are so coM reil wit it snnw. In eat (Iral of rain ; in the air is juire ami II speakini; of these that a country has eliniate. ihorn oimiitrii's, nor tho N^iva Sooti:\ inn a trw- hful. so that veoi>le live of tho "oiM. yon see lyini,' abotit Guhl, silver, iron, hi' must useful nn^l the cartli, and men I are ealhil miners er tiehls and citie.-. Il in Xova Scotia are. litf, nml ijrinil-aioiif. I PLAXTS— DIVISIONS. 42. Coal is very jdentiful in the casltru :ind imrtitrh parts of Xova Scotia. It would be intere.stiui,' to vi.'^it tlio Ai'Ann Mines \n Pietoa County, or some of the other coal mines, and see whi-re the bii.sy colliers, all black with diist, arc peckin;; away at the coal seams, far beneath the surface. It wuuld seen, a j;looiny jilace to stay v.'ry lon^, \. here i-he sun never shines, and there is nothin;; but the dim lamp to eive li^'ht. It is probable that nijst of you would be afraid to go down where the men are at work. You would require to ^,et into s\ sort of tub and be let throujih a small opening:, much in the same way as you would 1ft down a bucket into a well, only mm h furtlu.-r. In some countries the miners are very jiour, and their children hive to work in the mines. .Some of them do not see the li,i;hi lif tlie sun fur months, and ;.'mw up in i;.'norance. You should be very tliank- ful both for the sunliu'ht and the li|:ht of knowlud.:,'e. X[[. Plants.— 4,3. The trees, Howcrs, and other plants of a country depend on the climate ami soil. Some love i,'reat heat, others cold; .^omo cannot live witliout aluindancc of water, others arc killed liy .so much moisture ; smue Hourish best in stiff clay, others in lij^ht sand. 44. A large part of Nova Scotia is still covered with the native forests which once overspread the wlude country. These forests of pine, si>ruce, hendoek, maple, beech, and oak, are very usefid, giving us fuel and material for our houses, ships, aud many other tilings. There are many beautiful wild flowers in Nova Scotia. You havi> all. no doubt, seen the lovely Mit>l-Jio(atu(S, and turnips. Tiiey also raise wheat aud Indian cum ; but these crops are more un- certain. In the western p.art of Nova Scotia, particularly in the valley between the North and South Mountains, there are large orchards. XIII. Animals. -4(1. Wild animals are luuch hss nunirr- ous than they were wlien the whole country was covered with ft)rest. None are very feroeious, so that one is not afraid of being turn in jiieces wiu'i- he goes into the forest, as he miglit be in some countries where tluie me lions, tigers, and panthers. 47. The moou, whiih is the largest wild aniniid in Nova Seotic, lives wholly on vegetable food, like the o.v. Tiie ctirifiDii. is a smaller animal, and has now become very rare. The bear, /ii,r, and fiiri/ii- mc tlcsh-onters, preying upon weaker animjils, mid .sonietiinrs eafehing our shcrp and poultry. There are many dilTereiit kinds of birds, as the rmilr, hunk, mrl, Ci-oii; n>''iii, ninilhiir, irooiliirrkrr. ^Hivlri'lijf. vmiir, mtipr, inmilcnrk, |)'oro', iliirk-, and (/ow, .Some birds are very usoful in destroyiiiu Inscets, which would do proat injury in the (j.irdoim and fifilds. 4''. In hot countries there are many larte and venonions ncrpeni^ l"hu huge boa is iible to ornsli an v. to death, and then swallow him. The reptiles of Nova Scotia are the harmless .■f/s. The yoiiiij; of the froj;, calleil tiidjiclts, nre like fish, swimmiui; about ill the frof^jionds. As they grow lar,^er they change their form, and hop on the land. It is very interesting; to notice how the form of an animal is adapted to its mode of life. Look at those birds like the crane, with their Ion;,' necks and Ion;,' legs, so nicely tittiiij; them for obtaining their food from shallow water; or tbserve the toe.s of the w.'odpecker, made for climbiiii;, and its beak and tonj,'iie fur piercing. XIV. Inhabitants.- 41). There me not fewer than .350, (MH) peopli' in Nova Scotia. How long wuuld you be in counting them, suppose you count IdO in a minute J You have, no doubt, observed that the people who live in Nova Seotia are of three ditfereiit colours. JMost of them are w/iiti', and are, generally, descendants of men and women who eanie from I'^ngland, Scotland, and Ireland. .Some of the white jicoplt are di'set'iidants of the old Acadiaiis, and otluM's of Oeiniaiis. I!ut we have al.so a few tlmu.sands iif b/ack people iu Nova Scotia. Their forefathers were brought from Africa as slaves. Then we have the rxf men, or Indians, who.se forefathers were living here when t'le French discovered tho country. They number about l.')(in .'JO. There are some men and women in Nova Scotia who .are un- able to read, and cannot write their own names. Now that we have free schools, no boy or girl should grow up in this sad state. Three-fourths nf the people in the woild have not the liible, and do not know the true Nisii AnlU'oliMi, ISVKKNKSS |'(irt lldod. \'iei"iiiA Diidilcck. I'Ai'K liKKTov Mydnvy. liii MMosK Arlelmt EXERCISE.- Lay down tho counties and comity town* upon your maps. S>E.*SS^^- .11 I I 6 NOVA SCOTIA. XVI. Towns.— 53. In towns, the houses and shops stand very close t(j,(KiO inhabitants. The laws are made in Halifax, and the Governor resides there. It is called the capital of Nova Scotia. XVII. Industries.— 56. It is the duty of every one to be diligent at some honest lal)our. You have observeil that men do not all follow the same business. It is be.st that each should have some one trade or occupation, and keep to that, as he will thus become more skilful, lose less time, and be at less expense for tools. 57. In Nova Scotia, those engaged in tilling the soil, called fannei'!<, are the most numerous class. Tii'jii chief products are ditierent kinds of grain, potatoes, turnips, butter, cheese, and apples. Many of the inhabitants, particularly on the Atlantic coast and in Cape Bri;ton, are ^fixJi^'.rmcii. A large number in the cou.ties of Cai)e Breton, Pictou, and Cumberland, are coal-uiners; a few hunv^'- / / "^•wW/i ILU t^lM kv^ ^ "N-/- /""~- --/^ ^' •?,<«<<»■<£,» /. I ,.!• >\ '*». 5 \ '^JfcA, i'>f--#!'_';j^ /.. / r I f- »T!0» "II,., C >''"■' c,.i'Ai'' i (SUhrit /?;, ■ L 0^_ _ 1*0 1^ l|o Ml i^> i|o i^_ lou Ilk) itMOU 'ixp^l^ ^ V,-.ie""" ', .H .'. V fr' 1 \' V' ,/' ■'^"' ■■■ '-+ ' ! ^ ^ ■'"'■" \ \ <. (' ,. U—--^' ' ■ I ' •"""/'•"•'•"'.rf* ft ■•■ii'^' 1 frllf THEOKLD iliUii-l^HLLiiifo;,,,, ■»-'?Bi*:i&S!-" thinks I 'liistry a! ;^ We, ther security. seas of I Jamaica ; l)orliaps tl 67. It wo Irinds; but t p-eat deal ol oiir kuo«le<] wiiich we us ( theinselve nade the te; m.„:.-<-^-^*^mmm^ DOMINION OF CANADA. thinks best. In sucli countrifs tlieiv oaii be in' iuiiir'VLiui.ui. Iii- ihistry and economy only reniler a man a riclier prey fa' the jilumlerer. We, then, have j,'reat cause for th;iiikfiihiess fur the jiroteoliun of a trooil L'overnraent, to enable us to enjoy the blessiiii;s v{ our country, in security. fi.j. The heiul orticcr in the yoveriinu'iit of Xuva Scutiu in culled tlie Govenior. The hiw-s are made by the L>-;ii.<:/<(t'ire, which consists of tlie Gocnior, Lefjislalive C'txiiciU and House of Assemhly. A GLANCE AT THE WORLD. Things from Abroad. — GG. Xova Seotians use many things that conic from other conntries. Thus, iierhaiis, at the breakfast table we may see the i>rodncts of several ditJ'erent countries far distant from Nova yeotia. The bread is nuuh', it may be, of Hour wiiieh came finm (>ntario, or the United States; the tea came f'nim China; the cutlee fi'iiin the East or West Indies: the herrini;- from the cold lir 'iliiif.' sun, ly the I'Oor African, far from tiic land of his fatliers, and Ijerhajis a vlavt. Bird's Eye View.— 0^. Xova Scotia is but a small part of the wurld. \Vc have .seen tliat it is nearly surrounded by water; but if we cross the water in almost any direction, "e shall come to land — to smne one of the many countries whost' jiroduets we use. Turn to the Hemispheres and tind Nova Scotia, and you will see that this is the ^.ase. 0'.'. Tlic \V>-"// C/c/Zc/n-, we enter another cou.itry, called Qwbec, which also has vast forests. The railroad now runs along the bank of a great river, the .St. Lawrence. Large ships are coming (h»wn the river, some laden with lumber, some with flour; and others are going up, carrying coal from Pictou. Here is Quebec Citij, the capital, situated on a high blurt' beside the river— the oldest city in British America. Going on further west, we cross the river by the Victoria IJrid'je, which is nearly two miles ill Iiiiu'tli. ITtTi', "ii o!' islaml, is MiDifrnif, a Imiui' city ('iiiitaiiiinj; lU'iiily a lliiid as many inlialiitauts as all Nova Scotia. 72. We will now j^o up tlie Ot/aini Itiver to Otlnwa Cifif. On tlio west side of tlic river is tlic J'roriiuy at' Onfario, wiiich is one of the i^roatcst grain countries in tlie workl. In tlio neiphhomlioocl of Ottawa arc immense forosl.<, mid large (jimntitiea of liiuil' r me brnnglit liown tlie ri"cr in rafts. 73. Hut yonder are several Nnva Si'otioii>. enterini; tliat lar^'o liiiildlng. Yes; 'liey are memliers of I'arliaiui^nt. You remember tliat Nova Scotia, Now Iininswii'k, Q .ebee, and Ontario now firm one j;i('at fiiuntry, called tlie l)(imiiiiadii. Ottawa i.s tlicrii/i/ri/. Ou tlie .south and wot of Uiitai i' are va.st lakes. Uctwecn Lake^ Ei ic and Ontario arc llie celeliratoil \i- u;e river rushes down a precipice of 100 feet. British America.— 74. Far to the west of Ontariw, Leyond '<■ tlio lofty Kocky Aroiinlain.s, is lirithh Columhin, with rich I Oi\t:irio now firm nne Ottawa '\!i t.\\i-'riii>it'il. ». ]'n.twtcii L:iki's Kill' are the oelclnali'ii .\i- , wlicre a l:ir;;e livoi !i jirt'oiiiico of ICU foci. America.— 74. Ftir (if Ontariu, licyoiiil lucky MdiiiitMiiis, in htmlnii, with licli Tdll.Vcii) n.AST pi'M iiiiiios; iiinl on tlie iiorrli ^A' Ontario ami Qiiclioc is Ihiihon's JiiMj Territori/, a very cdld country, wlitTc ^iiiiii will not ;,'ro\v, and the few inhaliitaiits live liy Imntini.'. Coniiiiu' to (lie cast coast, in the Gulf of St. Lav. u'lici' we find the Island of Xeivfoiiudhnul, near which are the ;;reat- e.st cod fisheries in the world. Kiirtlier south, separated from Nova Scotia by Northiiuiberland Strait, is J'riiio' J-.'ihr'ird IsldiiiL All these countries- the Doiiiinion of Canada, Ihiti-h Cuhuniiia, llinlson's Bay Territory, Newfoundland, and Trinie Kdward Island -I'orni llritish Awric'i. North America.- 7r). <»n the south of liritish America is a lar^e country caUed y/c Ciiilfil Sfaffs. It has ^,'reat variety of climate and jirodiictfl. In the north-east, manu- facturitu; is a very imiiortaiit business; in the middle and west, wheat, cori\, and tobiicco arc raised in ureat abundance ; niid in the south, cotton, rice, and snuar-canc. 70. Mfwiro lies south of the United States. Slill furtluM' poiith, where the laml is narrow, is Ciiifrnl Aiiicrira, from which we obtain lou'wood and maIiiiL;aMy. Tiio coasts of Mexico ami Cc. itral America are jnw, hot, and uidicalthy; In the interior are hi^di plains, calii'd tnhb-l'iiitl, wliere the climate is more auri'eable. Mexico has loHi,' been tamed for its silver mines. The story of the eon(Hiest of IMexiro, three hundred and fifty years a^o, by the Kretdy Simniards, is very iiiti'restin^'. British America, tlir I'liiicd Stales, ]\b'\ico, and Ci'iitral America, form a yrcat division of the llarth ciUcd Xaith A mrrii'i\. The Western Continent.- 77. <>ii the map of the West- ern llemispheru ymi will see North America; and on the .south, bi'yiind the Isthmus of Tanama, S^)ntli Aiiirrli',!. These two divisions form the Wi'Ktnn ('iDititifiil. South America is j;cnera!iy a wariii, moist country, yii'ld- Mii; colfci', tobacco, rice, cotton, oraiiLjcs, pine-apples, and many other fine fniit.s. 7m. Heie, on the east side, is the Aimrjiii, an immense river, the largest in the world. It tlows throuiili a llat country, hundreds and hundreds of miles. On each sidi> of the river tire marshes covered ritli tall reeds; and beyond the uuirshes are vast dense forests, abmuidiim in dye woods, ornament.al woods, the india-ruliber tree, and many other valuable trees. 7'.'. I'lli' nf till' Ili.iSt liealltiflll |i|;ltltrii'!l in till! 17c. I»ri,t Itiiiiii, II 1,'irL,'" wiittT-lily wliicli jjoiw-s ;il(iri',' tlu' iMr.l.-rs ,.|' ilio •. !■ TnlirA lOKU Aiiuijiiii. Its laicp NtroiiL' li'iiviiH, five iir hIx f ci liii.ii.l. tli.il mi iKi' NMtti'r, mill in llio iniilst nf thoiii iiiu tliu roB>>.i«liii|inl il'>\i(.r«, lur^vr tliitii tlic crown of II iiiairH h.it. 10 A GLANCE AT THE WORLD. 80. In otlitT jiiu-ts of .Soutii Vniurica there arc iinineiise [ilain.s c'uvercd with tail grass, where roam countless herds of wild cattle. Along the west of the country is a great mountain range, called the Andes, the summits of which are covered with jieriietual snow. IL're ami theie, cone-shaped peaks rise far aliove the surrounding }ieights, tlirowing out volumes of ViiLiASO IN ASDEH. smoke, like tlie eliinincys of some great factory. Tiie.se are V'l/ctnnun or Inu'iiim: mountains. Crossing the Atlantic — ^L We will now take an imaginary tour eastward. "Wo leave Halifax in a largo steamer bound for T-iverpool in England. We are soon out of sight of lanur ship, which looked so lame beside the smaller vessels i)i the harbour, now seems very small, ns it is tossed up and down over the broail, higli waves. W'v. see no path, nor any signs to direct us; but the cajitain, by his knowledge c'" navigation, with hi.s com- pass and chart, can take us as directly across the patiiless ocean ns if lie followed a beaten trn<'k. 82, Yonder, risiiiir almve tlie wnter, nre tlie iimsts of veHScls. A« we conic nciiror, the liulis licoonie vi' to the other. There nre two men on the lonk-ont, nii'l the steiiiiiwhistle is Mowinu, to winn imy vi -sels that may he neio' to keep out of the «ny, lest we should run iiilo them. The tipj.' hes elose to the sut; for wleii we lonk up, we jt't (ilii'ipses of the olear sky. The wnter bero ii i|uite wavni. and the enptnin snys w'e are in the (yu//.S7;Y((ni, which flows like a L'reat river through the ocean from llie (Jnlf of Mexico. The fog is caused by the steam which rises from the warm water. As we jiass on, the fog clears aw.ay and we can apain see far over the ocean. That huge glittering object in the distance, like a mountain ot glass, is an icf>icv;/. It looks very lar^'e, yet only oneci^rhth pat t of it is above the wnter. It has floated d iwn from the cold regiijus of the north and will soon melt in these warm waters. Great Britain.— ^4. It is now nine days since we left Halifax. "Laud ahoy I" shouts a sailor from the mast-head. We on deck cannot see it yet, owing to the curved surface of the ocean. Soon it comes in sight and we get our tirst view of /rdmi'l, the green isle of the sea. We call at (.,>ueenstown to leave passengers and tiie mail. We tiien pa.ss tip St. George's Channel and iu'rcss the Iiisli Sea to Liverpocil. f-:>. We are now in A'lij/tiin/, wliich with Soil/'Uhf and U'ti/is forms the Js/oik/ /i /s/ts. Here is tiie home of our forefathers, the central and mother country of 'J'/ie /Iritinh Kmiurey to which Nova Scotia ami the rest of Dritish America belong. Si), Knt'Iiind is a beautiful c'nuntry. Its rich areen mendowt nre eiieloseil wiih thorn hcdiios, which are miii'li prettier than the crouked f> lu'es we so (fteii see in Nova Scutia. It has very rich mines of coal, iron, lead, and tin. It is alson u'eal niannfactiirim; country, t'nr cottons, broail cloth n, cuilety, and crockery nre made here. Cotton does not i:row in Hnkdaiid, but is bioiuht in a raw state from the Tniied States of Aineiicn nnd other warm countries, 87. There nre ninny Inr^e cities in Kiiudaiid, LoNiioM, the inraest and richei I city in the wurld. Is the capital of the enipire. It stands on both sides of the Hiver Tlialies, v\liicli is like a forest of lunstB, there lire so many ships fruin all pails of the world. There are several large bridges ovit the river; ainl there is also n rond under the river, which ii called the Thnmit Tunml. m ougli tlie ocean t'roui tlie iiu which rises from the an afrain see far over the ance, like a luouutaiu of uily oncfi^'htli part of it III tlie C(>K1 regions of the (l;iys fiinco we left Voiii tlie iiiast-liead. till' curvi'd siirthce 111 \Vf p't (lur first ' sea. We cull nt le mail. We tlieii .■'.s tlie Iii.sh Sea to with Scotliinil and nn. fJreiit I'ritaiii itar tlii'iii, are calltd (nir furefatliers, the s/i Kiiipire, to wliieh liiii belling. ii'h ffvovn tncrnhnvn aro ri'ttiiM' than the croMki'il vi'ry rich niiiu's of coal, ■tiiriiii,' eountry. tiiir II' iiiaili' here. Cotton i\ liiw Htiito fiiiiii the ilrii"'. I^wNl'iiN, thi' hiru'Cft ilic ('ni|iirr. It Ktfiiiils liko II fiU'VNt of lUllHtH, III- xvnil.l. Thi-re arc H iiIko n ronil uiiuii^KiM.i:i. At Md'Hriltm, in the iotitli of Fruiiee, we tlnd n stontni r a^||,^ t,i lllllAII''K itKI/.^li IIV A l.\<<\ The inliftMtants in I lie interior of Africa aio very iunnrant and liarharous. They wnj;u fiurcu wars with one unoilier lo ulitain eaptives ('■r slavcu. 111'. Uiit here we are at .'l/''.m«r//'i(/, an old city, founded more than two thousand years le^o. It onee iiad a line liKmry, which was luiriied hy tiie .Mnhamniedans, We iKiw u'o hy railroad to t'aii", tlir capital of Ki;ypt. and the larycHt city in Africa. It docM led minli fcNeinlile any city wo I'ver saw liel'ore. The stieeti :ire very narrow 12 A GLANCE AT THE WOItLD. and ilaik. Tlio limisi's di not seem to liuve any wiiulciwe; hut if we well' to enter them, \vc would find tiie windows Iookinj4 iiut upon an opun scjuare in tiie middle, called a eoiirt. Amid tall palm trees and orange j^roves, t' c mos(]ues, or the Mohanimeilan places of worsliip, rise with their j^ilded minarets ahove the surrounding liiiil(hn,L;s. 93. Tills is Kuypt, tlio liiml into which Josi'iih was soKl as a slave, ami wliL're lie nfterwanls became so unat. Yonder is tlie /liviv .Xilc, lieside which Muses was liidileii by his parents, in tiie ark of huiiushes, It never rains in Knypt. Water is tal;en from the Nile to water tlie ticlils, Tlie river also overflows its hanks ilin in^; three or four months in the year, and covers the whole country with water. 94. Not far from Cairo are the Piiramidn, whicii were Imilt four thousand years a|.'o, anil have been tlio wonder of all Kncoee ling n^es. The lar^'est is (juite a little mountain, bein;; lOl feet liin'i and cover- inn eleven acres of niimmi. \>ti. We now i;o by railroad from Cairo to Sur:, on the (liilf af Siirr, the tt.'iter thruuuh wliii'h the Israelites passed uM dry ;;reuud. Here we take our leave of Afrioft, Asia.- 111!. As wc sail down tin; ( iulf of Suez, we pass on our left the desert in which the I8raelit08 wniidered forty yeiirc, and M"iiiil iSiiiat wliore (Joil gnve the law to Mose.^. Further nortli \x I'nlintiiu; the l'r(imise(l r,anil, in wliidi the Israelites settled after they came out of the desert. AMa resembles Africa in havinn a lai'Kc part of its surfucc covered with rainless sandy plaitm or desorls. The enniel i.n one of the most useful ,'iniiimls in these legiotis, for it I'an endure thirst a loiii: lime. It is much used us i\ lieast of biiiihti by travellers in tln' deNvrlR. !17. Passing down the lud Sea, tlirough the Strait of Bab-el-Mandeh and tiie G'u/f <]f Aden, crossing the Arah'utn Sea and the Ikxy. of Jienr/al, wo arrive at Calcutta, a large eity in India. There arc many sliijis here from various ]iarts of the world, some of which, from America, arc laden with huge hlock.-j of ice. 98. India belongs to Great Uritain. It is a, very warm, fruitful country, yielding rice, sugarcane, cotton, silk, opium, indigo, colfee, cinnamon, pine apples, und other line fruits and spices. Along the north arc mountains five and a half miles high— the high- est in the world. On the southorn slo]ies are vast forests, abounding with elephants, lions, tigers, and other largo wild beasts. !)f). Leaving Calcutta we ssail south-east through the Strait of Malacca, and then north-east over tlie Cltina Sea, to Canton, a port of the great country called China. Here wo sec ships from America and Europe, taking in lea, silk, and rice, which are tin- important products of the country. China is s:iid to contain one-third the iuliahitaiits of the Earth. The soil is carefully cultivated, and the hill-sides are formed into terraei^s, on winch tea, coti'ee, and otiier products are raised. In many places the rivers me covered with lloating L'ardens, which an' forineil l\y covering a raft of fimhcr with earth. In the gnnleiis are little houses, \W. Asia ig larger than North and South America together, It ijontains two-thirds of the human nice. Nearly nil its inhabitants art heathens, destitute of Cliristinnily. In the central ]i;irt of Asia there aie vnsl high plains unlit fur cultivation. The irihabilanis possc-s many lnuses, cattle, and sheep; and they waniler from place to place, i H 1 ^•. O 1^ u ^E c. cy3; ! ^ ' s O r ^ ■J i 1 I , •> [:« 'Jl 1 i ■ 3 t igli the at rait of issiiig the Ai\tlii(tit t Calcutta, a larj^t! ii'i'o from variiiiis ^iiu'rica, are laden very wnriii, fruitful Hiiuiii, imligo, colfee, piocs. liles hi)^li— the liipli- (t fnrests, aboumliii;,' beasts. • ■ast tlinuij^h tin' T the (liina Sea, (tl ('/ii)ia. Here ikiiij,' ill lea, silk, .s of the country, lahitauts of the iiMJ the hill-Hides ill'ee, and other ivers are covered ly enveriiiu a rat't it tie hniiBL'S. li'a tt'Ki'tliur. It its inlialijlaiitfi arc I |iiirt iif Asia then' inliiiliitaiits piiRsoM! from plaeu In place, I I, 102. T to a CiiMii iiciu- Clir licio. Tlio nr. C(],5fl'S to t of South which th which hii; with fur I Aiistial niul iiiryo 103, V I'dcijic C imist no ( nurse ii( OCEANIA— HOME\f ARU. 13 TEA ri.ANTATlDX. in search of pasturage. Tliey are notorious rolihers, and tiavelitrs st'i('.om ventuvo into their country. Kurope, Africa, ami A.sia arc ail coiinectet), ami taken together form the Eastern Coiilinoit. Oceania.— Idl. The only leiniiiiiinc! portions of the world to lie seen are the Islands (.>f tiie Ocean, sometiniea called Occmia. "We sail Houtii amid the hot and fertile AW Inilin Islands, who.se choice sjiices scent the air far around. Anion^' the rich jirodiicts of these island.", are coeoa-niit.s, ciiuiamon, nutine^s, and cloves. We cross the Iinfinn Ori-nn, |.a.ssin<,' the west and south coaata of Ausfi-alia. Tills is the lar<,'est island on the Ivirth, and forms a j)art of the wide-siiread British Km|iire. 102. There are many thiiiu's in Australia ■vhich npppar very stranirf to a Canailian. Tin- .^nn is nortii of us nt ni.on; and ahlmnuh it is near Christmas, wiicn we iiave winter at liinie, it is midsununcr here. Tlie native trees are niailv all evergreens, and iire.«ent their tiiin cd.^cs to the sun ; so that the forests are n.a shady and dark like those of South America. Alany of the aninialH liave a pouch or sack in which they carry their younp. Tliero is one >ery I'loiiois animal "liich has tiie feit and bill of a duck and lajs vn^s, hut i.s covered with fur anil suckkii 'is yonn.' like a cat. Anstialia lias very rich j;nld mines. Many nf ihe people tend hlieep, and larj^e i|iiantilics df wiml are exported to lOnjilanil. 103, We shall cnutiniU' our courst! caslward aciuss the I'acijic Ocean, which is the larnest of all the oceans. You must now turn to the \Ve>itcru Hemisphere and mark our course north-easterly, PiUong the numerous groups of islands. ACSTKAMAN I'r.ANlS Most of the islands of the I\icifie are very beautiful and fertile, yieldiuj,' the finest fruits. ]0J. Some of tiiese islands are inhaliited hy savajies, and it would be danu'ennis to land anion;;st llieni ; in others, the natives have been tau;;ht the principles of t'liri.stianity by missionaries from liritain anil .America. Yon ,-,ee a pmup called the Sew llfhivlcn, where there are several missiunaries from Nova Scotia. The inliabitiint.s were once very fierce, and cruelly murdered Mr. Gordon and his wife, who went from Nova Scotia to teach them the way In heaven. Further on are the Sdinliricli /,^/nn<^.^, win ic (,'aptain Co.ik, the great navi^'ator, was killed by savages, nearly a Inmdied \earsa>;i). Homeward. -1(1."). Ilaviii',' crossed the Paeific, we tr.ivel over the Isthmus uf Panama in the rail-cjirs, and at As/,iii- tr'i//, on the Cariliheau «ca, t.ilce a steamer for New York, the larL'cst city in .\mcrica. We (;ome to Boston and thence to Ilalifa.v Conclusion.— im;. Ilnw stran-c' We set out at Halifax, fravcllcij an easterly course, and lii'n; wd are at Hiilitax aiiain I The fact is. the Earth is a ureat b.dl. and we Iia\c made a jnurncy mund the world. This explains why wo always saw the masts nf a ilislant ship lirsr. If you now trace our course on the K'ob.', which represents the Kaith belter than a map, you will iniderstainl how we tiavelled cuie stantly in the name direcliini, and at len^lh arrived at the place fro:u which we started. THE EARTH AS A PLANET. The Form of the Earth. — 1. R'dple (nue bclievid tlwt tlio Eiirth was an cxttiKlr'l iilaiK'. There aiu many lu'ool's that this is nut tht: case. 2. Xaviuatoi'j have often. Ly sailing constantly in the .same ilireetion, arrived at the plaee from wliieh tiiey .set out. Tlie first voj-iige arouiul the wuilil w.is made between luVJ and loiiii, under the cominund of Ala^'ellan. 3. When a ship comes in sii^ht, we first see tlie top-masts and the rii'ging, histiy tlie hidl, as if it were coining over a i'i,-.rANr snirs. convex surface; and when the sailor leaves the sliore, low oliji'cts are the first to disajipear — the last seen are the luountaiii U)\)s. 4. If a man six feet high were to stand hy the .sea-shore when the water is smooth, he coidd see a boat three miles distant; if he were to stand on a high rock, so as to be ele- vatc'd twenty-four feet, a boat would be visible six miles distant. 5. For these and various tdlier reasons, all intelligent persons now believe that the Earth is a vast ball. It does not appear round, because it is so large that there is but little curvature in any portion of the surface which we can see at one time. If we were to ascend in a balloon far above tiie Earth, we wuiuld see much more of its surface' at one view, and it would appear curved, as a ball. 6. An observer on the Earth's surface, or at any elevation above it, always finds that his view is bounded by a circle ; and that this circle, which is callcil the iSensihle Horizon, is eidarged in proportion to his elevation. Could he rise sufH- cicntly high, he woidd see half the Earth's surface, when the circle bounding \m view wuuhl be called the Jiatiomd Horizon. 7. One might suppose, at first, that the unevcniic.ported, it falls, because it is pulled down by this force. 12. The weight of a body is the measure of the force witli which it is attracted by the Earth. Attraction is mutual in all bodies, and in proportion to the quantity of matter they contain. Thus the stiiie, in juoportion to its matter, attracts the Earth, as well as the Earth the stone, 13. The attractive power of the Earth acts in a right line drawn from the Earth's centre to tiie body attracted; and this power diininislies as the scpuire if the distance frurii the centre increases. If tiie Earth, without any increase of matter, were swelled out to twice its present size, a body which now weighs a pound upon its surface, would weigh only oue fourth of a pound. E;irtli is so lai;:,'(', mure witli its yuiiu- tlie riml with tlie but is slightly flut- ; I'oles, tiiul bulnid iiijjc resembles that Liition of the Earth. n a iieifect sphere, tteiieil. Ill a i;lulie :he poles would not of au inch. I'ical form. ■oiiuitiniialiy earlier or come in view, wliil.st liicli i.s the invariable Dt' eiylit inches in tlii.' vtl. . wiiit towards either uulJ rise uniforiuly quite the case ; for St be passed over to ar. Ik'iice we inter :ni,L,' a stone from •ereume the re-sist- This resistanee, le Earth's altrac- Earth's surface ia stotic and leave it iwn by this furce. I'liroe with which it n all bodies, and in Thus the stune, in >cll as the Karlh the iuht line drawn tVcni is [lovver diminishes uses. If the Earth, to twice its present lurlace, would weigh MOTIONS OF THE EAKTII. 14. As a body weighs nearly the same in all places on the Earth, the surface must be everywhere nearly the same distance from the centre. Hence we h.ive an additional proof of the Earth's spherical form. A body weighs sliuhtly more near Uie pules, which is a further proof that those parts of the Earth are flattened. The term oblate .^phti'oid expresses the exact form of the Eartli. Cause of the Spheroidal Form.— 1.^. When we pour water upon a revolving grind-stone, the water tlies olf in proportion to the raiiidity of the motion; also a wagi^on-wlieel throws more mud when we drive rapidly. If a iiiece of soft putty, in the firm of a sphere, bo made tn revolve rapidly on an axis, the poles will become flattened, while the middle, or equator, will bulge out. liy supposing that the Earth, whilst in a semi-fluid state, revolved around a line pa'^sing from one pole to the other, we can account for its sjiberoidal form. Size of the Earth.— Ifi. A railway train, movini,' at the rate oi' (JtJ miles au hour, would go around the Earth in about seventeen days. The distance arou: '^ the Earth is called its rircumfi'vence, and is equal to 24,860 miles. The area of the Earth's surface is 10,590 times greater than that of Nova Scotia, or it is equal to a square of 14,035 miles. The pillar diameter of the Earth is 7898 miles; the equatorial dia- meter is 7924 miles. Light and Heat. — 17. The Sun is the great source of light and heat. Without this luminary the Earth woidd be wiiolly uninhabitable; every animal ami i)lant would perish, anil all the water upon the Earth would be congealed to the hardest ice. The Sun is so Air removed from us, that, by travelling (JO lailes an hour, it would take one hundred and eighty years to travel an equal distance. Light moves so rajjidly, that it occupies oidy about eight minutes in coming to us from the Sun. 18. The Sun is 1,400.000 times larger than the Earth ; liut, bcin- less dense, it is only 3130,000 times heavier. Its diameter is 883,OUO miles, and it is 91,72.'i,000 miles distant from the Earth. Day and Night.— id. Place a lighted lamp beside th(> glolte, so that it will shine from pole to pole, and turn the glol)e uptm its axis. A fly standing on any jiart of the globe will have light and darkness in succession. In like manner, day and night follow each other in turn, by the rotation of the Earth. The Earth turns aroiuid an imaginary lino called the n.ri)^. Tiie N(wlh I'ofc is at one extremity of the axis, the Smit/i J'ole at the other. 20. A light shinine uimn a spherical body illuminates juit onehalf of its surface at once. The Sun is always shining upon the Earth; therefore nne-half the Earth's surface is in the light, the other in the dark. The boundary line between the light and dark hemispheres is called the Ciirlc of lUuminatiDn. A.i the Earth rotates, this circle is ever changing its position. 21. When moving rapidly in a rail-car we seem to be at rest, and 'he objects along the track to be gliding past us in the opposite direc- tion. The rotation of the Earth from west to east, gives the Sun an apparent motion from east to west. It was once thought that the Earth w.as stationary, and that the Sun revolved around it. According to this theory, the Sun must, every twenty-four hours, describe a circle having a diameter equal to twice tlie distance of the Sun from the Earth ; and the stars, wliich are In- conceival)ly more remote, must travel correspondingly faster in order to comjilete their revolution in the same time. 22. The most direct proof of the Earth's rotation is furnished by an interesting experiment with the pendulum. Unequal Length of Day. ^2:5. In the siunmer we have long days and short niglit.s ; in the winter, the reverse ; so that light and darkness in the course of the year are exactly eiiual. The longest day is the 21.st of Junc, the shortest the 21st of December. Twice in the year— the 2()th of March and the 23d of September — day and night are eijual, twelve hours each. At the Equator ihiy and niu;lit are always equal, and the inequality is greatest near the poles. 24. At mid-summer, when the day is longest, the Sun at noon is high up in the heaven.s, and much more nearly over-head than in winter. Tin's is only an ai>]tarent shifting of the Sun's position— the real change is in the Earth. The Earth not oidy rotates \\\w\\ its axis, it also moves around the Sun in a vast circle. The path in whicli the Earth re- volves around the Sun is called the Enrtlts Ovh'd. Illustration — 2.'). ri.ico a l.imp on the floor, to represent the Sun, and witli tlie oliiilk ilraw a larije circle around it for tlio Kartti's orliit. I'l.-vco the plolio in the orbit, on the east side of the lamp, with the north polo pointiiii? to the reilin^' in the northern jmrt of the rocim, in such a manner that the axis shall he parallel In the east side of the room, and inelined towards the nortliern wall ahout one-fimrtli tin.' distanee lietween a vertical line and a horizontal * The lanqi will now hiiie from iiole to poli?. and if the j?lohe he tur ed on its axis, it will illnstrate the eiinality of day and night in the spring. Without chanKinij tlie inclination of the axis or its jiarallel position with respect to the east wall, move the jjlohe thron^'h one-fourth the orbit, so that it shall stand on the sonth .side! of the lanij). The rays of light will extend beyond the north pole, illumi latin.; more than half the northern hemisphrre, and less than half the Houtliern, We have here the position of the Kartli at niid-sninnier liy movintr the globe in the same manner to the west and north sides, we shall have the Karth's position in the autumn and at mid-winter. jn. The E;irtli thus makes a revolution around the Siin once a year, uuriiig whieh it presents dillerent paits of its surface directly to the /'',/. 1, nw AMI Niiinr i-i^'ai,, ^Vtrih 2o(/i ./111/ Siiili-mhir 'lArd ' It should be Inclined 2Hi denrees from the purpondlcular. i(„ 10 THE EARTH AS A PLANET. Sun. Hence llie ililliieiice In ilie leiigtii of day and niglit. Tlie accom- panying di.igraras represent the Earth in its relation to the Sun at diflferent times of year. In figure 1, the Sun is vertical at the Equator; in figure 2, it is vertical at tlie Tropic of Cancer ; and iu figure 3, at the Fl'j. 2. ■ -.y LONil DAVS AND SHORT NKIHTS IS THE XOUTUEllN llEMI.srilEUE, Juni: ilii. Tropic of Capricorn. In figure 2, the whole space within the Arctic Circle has constant day ; iu figure 3, it has constant night. Fiij. 3. .•';^'7jT^''Z\ SUOllT DAVS AND LONU MdllTS IN THE NiiliTHEIiN HEMISl'HEUE, UiccmliLr ilst. 27. An imaginary -^lane, e.xtendiiig from all parts of the Earth's orhit to the centre of the Sun, is called the Plane of the Earth's Orbit. If the Earth revolved around the Sun with its axis perpendicular to the plane, the plane would cut tiie Earth at the Equator, and the Sun would always be vertical at the Equator, as in figure 1. lUit the axis is in- clined 23.J degrees from the perpendicular, and this inclination causes the circle described on the Eartii, by tlie plane, to cut the Equator at an angle of 23.^ degrees. This circle is called the JCc/iptic. As tiie Sun appears to move in the opposite edge of the plane, its annual path is also called the Ecliijtic. 28. The axis of the Eartli always maintains the same position, so that iu any part of the orbit it is parallel with itself in every other part. A star situated in the northern heavens, to wiiich the Nirth Pole is directed, is called the )iorllt st(tr. 29. Tho plane of the Karth's orbit may lie ilhistratod by a birgo circular .sheet of tin with a hole in the middli;, tlirnuKh wliicli a lani)) i» placed so that half tho flame is above the plate ami half liclow. A ball with a wire thrnuKli tho middle, rciirosentinB tho Kavlli and its axis, can now be carried round tho outer imIro of tUo tin, keepinR the proper inclination of tho a\h. Apparent Motion of the Sun, —30. In the spring and autumn tiie Sun is vertical at tho Equator. It then appears to describe a circle in the heavens directly over the Equator. This circle is called the AV/m'- iioctial (equa now, iqual niij)d), because day and night are then equal at all places. In pursuing its apparent annual path in the Ecliptic, the Sun during our summer is north of the Equinoctial; during our winter, south. The Sun, therefore, crosses the Equinoctial twice during the year. The points in which the Ecliptic and Equinoctial cut each otlior are called Equinoxes— 1\\6 Vernal and Autumnal Equinox. The Sun's position each side of the PJquiiioctial is called the Hun'a Declina- tion, which is either north or south. 31. During the three months succeeding the Vernal Equinox, the Sun's northern declination is constantly increasing, acquiring its maxi- mum on the 21st of June — 23.J degrees. The Sun now appears to be stationary for a little, then to turn back towards the Equator. The northern point in the Ecliptic is called the Hummer Solstice [Sol, the li'ni; and sto, to stand). In like manner, the point marking the greatest declination south is called the Winter Solstice. The circles which the Sun describes 23.^ degrees each side of the Equator, are called Tropics {trepo, to turn) — the Tropic of Cancer on the north, and the Tropic of Capricorn on the south. 32. When the Sun is vertical at either troi'ic, the rays fall 23^ degrees beyond the pole on the same side of the Equator. The polar circles are supposed to be drawn at this distance from the. poles — the Arctic Circle at the north, and the Antarctic Circle at the south. Change of Seasons.— 33. If we hold a board upright before tlie fire, so that the rays fall periieiidicularly iiiion its surface, it will receive much more heat than when we incline it away from the fire. In the former case more rays fall upon a given space than iu the latter. This is illustrated in the annexed diagram. The rays a h, which fall periieu- dicularly on c d, are spread over a space three times as long by falling obliquely on zone in which it is situated. We often wish to bo more definite, and it is both natural and conveniont to give the distance from the Equator. This distance is called hditude. If a place is on the north of the Equator, it has nnvth liditnde ; if oil the south, muOi latitude. The di.stancc from the Equator to either pole is 90°, which is the iiigtiest latitude any place can have. 46. Latitude ia indicated on maps and glohes by lines or circles 18 THE EAKTIL AS A PEAXET. i-:' Ciilled pardlth of latitude, wliicli are (iiiiwn east ami west betwean the equator and tlie jjoles. Degrees of latitude are num- bered on lines ninning noith and south, or alon;; the aides (if the map. 4". The most simple mode of Hndini; latitude in the north- ern hemisphere is by t<\liinf; the altitude of the north star. At the Eipiator this stiir is al- ways in the northern liorizon, and as we travel north it rises rei,'ularly in jiroportion to tlie 90 '■' distance travelled, until at the Fiii. 8. North Pole it is directly over- rAiiAi.LK.Ls. liead. That is, at the Equator the altitude is ; at the polo 00 ' ; and at all intermediate places it i.s exactly equal tu the latitude of the place. Tiius at Halifax the altitude of the north star is 44° 38', which is the latitude. 48. Latitude can also be determined from the meridian altitude of the Sun — that is, tlie height at nodii. When the Sun i.s in the Kquinoc- tial, the meridian altitude at the K(]uator is 90°, and the altitude be- comes less as til' latitude increases, until at the jwle the Sun appears in the horizon. Therefore, to ubtain the latitude, wj subtract the alti- tude from 90'. 49. When 'he Sun is not in the Kquinoctial, and we are on the oppo- site side, we dd the declination to the altitude, and subtract the sum from 90°, for *he latitude ; if we are on tlie same side as the Sun, wo first subtract the declination from tlie altitude and then subtract the re- mainder from 90". The Sun'.s altitude at Halifax on the 21st of Juno is (1S° 52' ; from tliis subtract 29.^', the deolinatinn north on that day, and we have 45° 22'; subtract this from 90°, and the remainder, 44° ?i.s', is the latitude. Measurement of the Earth. -r.n. i!y obsorvatinn, we should fmd that tlic eleviitidn ef tlie i)nl;ir ai-.w at Halifax is 41 ;!8' ; if we go ;!S', we sliall have travelled one degree of the Kartli's cireuiiifereiiee. AVe would find liy measurement, that the distance travelled was i!ll|'^ Knglish miles: wliieh inultii>lied hy iiliO-tln' numlier of degrees around the Earth - give '24,87!) To determine our distance east or west of London, that is, our longitude, we compare London time with our own. A nicely constructed time-piece, called a chronometer, shows the time at London, and we are one 7.'.15 (;(i.(i,5 05 25,.S0 20,16 20 co,;is (i4,S4 70 20,. 12 23,00 2.") .'■vt.as (i2,.'-);! 75 I6,r).{ 17,S0 ;jo r>\.Wi 60,75 80 10,42 11,08 •^-^ 4i>,l,') 6fi,.61 85 5,23 0,00 ■10 4,".,ll(i 62,85 1)0 0,00 0,00 4'. 42, 4S 48,78 OUTLINE OF THE SOLAR SYSTEM. The Earth a Heavenly Body.— Gl. During a portion of the year r. lar-e and beautiful star may be seen in the western he.avens, shortly after sunset. This evening star is the planet Venus. Tiie Earth is very much such a tiody as this star. It is about the same size, and, if viewed from the same distance, would probably look much like it. Equator in csti- ural line at which it and west. We I name it the frsl ian is called lonr/i- m the same meri- tish Empire, and :h passes through ;e is said to have s meridian which liat which passes IS, the first nierklian circle, on tlie oi>i)Osite ! greatest longitude a ed on the equator of ,om of otlier maps, will be seen that they ie becomes constantly ; rather greater than I Equator slightly ex- 1 west to cast, once in ound the Earth in the n thus traverses 360° Therefore for every ater in coming to our our in the day, will vill be earlier. tanco cast or west of n time with onr own. ter, sliows the time at London for every four e chronometer, of longitude in differ- OUTI.INE OF THE SOLAR SYS'L'K.M. 19 iphjcl Khtliil, iCS Illlll-.1. t.r)7 44.3.'; ,41 S^..-'.^ ,00 34,riO ..■il) 20,1-, i,.V2 23,00 .r,:i 17,80 ,42 11,08 ,2;{ 0,00 ,00 0,00 SYSTEM. irtion of the year a ;rn heavens, shortly ;nus. The Earth is he same size, and, if look much like it. •:! AsiruMi.iuers inform us tliat Venus, like the Earth, i-otaiBS upon it.s a.\;s and revolves around the Sun. Planets. --t)2. Tliere are many other celestial bodies similar to tiie Earth and Venus, which revolve around tlie Sun. All such bodies are call'd I'UiiitU. Some of the jilaneta are smaller than the Earth, and S'imeare \L-ry much larger ; some are much neaierthe Sun, others are greatly iii ae remote. All are Mpaque bodies. 63. The following are the eight largtist pl.inets, in the onler of their distance from the Sun ; — Mcrcuri/, \'inu.i<, the llartit, Man, Juj'iUr, Hutufii, L'ranus, and Xtjftuiu: soi.AU svsrt.M. Their orbits form coneentric circles, as in llic iliiiL'rain. Ixtween the orbits of Mars and Jupiter are ni;iny small pl.intts, usually called ;/?,oi;s 3 4.. wo 42,000 37,000.000 ti'.l,"00,WO 01,72.-i,OOiJ M 1.000,000 404,000.0110 11110,000,0 10 1.^22.000,(100 2. >( .',1,000.000 22.-. 3l-.> (i.^7 4.3:;:i lo.7.'iO 3(1, (W7 U0,02,"> 1 4 Fi.xed Stars.- co. The Solar Sy.stem eiimprises only a few of the celestial bodies. The nthers are called KL^ed Star.i, and are distin^uished liy their silvery twinklhii.' liglit. They are suppnsed to be suns forming centri'.s of .sy.stems like the solai system. Light eomes from the .Sun to us in atmut eight minutes ; but 1 d nearest fixed star is .so remote that light is 3] years in travelling from it to the Karth. EXERCISES. 70. Till' I'ollowiiiy Exercises will test tlio jtupH's ict to the Sun's rays has the Northern Hemisphere over the Southern, and why? ■■ "<«»iipv-.;s^ft^j/. Ill .1 1 '20 THE EARTH AS A PLANET. THE TERRESTRIAL GLOBE. 71. Tlio Terrorstrial Globe i.s a representation of the Eartli, sliowinir its forn), rotatory m " >n, tlie parallels, meridians, and relative situation of jilace.?. It al.so enables us to illus- trate many important prineijjles respecting the Earth in its relations to the Sun. The Wooden Horizon. — 72. The irLibe is .suspendcil in a wood.*- riiifr, c.illeil tliC Wiwilni llnrizon, \vliii;h ie|ircscnts the liitioiiiil Iiorizon nnd (li.-idcs the nl'j'ie into tlio u)ipi.'r and I'lwcr licnHs]ilii.Mo.s. Tlie upper RurlUco of the wooden liori/.ou ia divided into six concontrie oiicles, one of wiiieh {.'ivcs the 32 points nf the conipas.s. 7H. Tlip Innermost circle of the wnmlin liorizon slinw-i the iniii^lilitil'' uf the liu;»veii!y Imclios ; tliat is, the arc nf tlie leirizon lying lictween tlie point wlii-re ii lioily rises or sets iind tlic east or west jioinls nf tlie horizon The second circle sliows the nzimiitli of the celestial hoilies. or the arc nf the horizon between a vertical circle passing' Ihrouyh the body and the north or .south jinints of the horizon. The third circle pivos the jioints of the crnnpas.s ; the fnurtli. the ]'2 sii'ns of t'le zodiac ; the liftli, tlie iiioiiths and d.iys cnrresiinniling to the .signs and degrees ; and the si.\lh, the \1 calendar nmntli.-i. The Brazen Meridian.— 71. A circle of brass, passins round the {jlobc at rir'ht aii;;le.s to thiMipiator, is called the Drazen Meridian, and soinetiu)e.stlie I'niversiil .Meridian. It i.s divided into four diuai jiarts, or quadrants, taeh f,'iaduated from to !»U'. Two of thecpiadrants are nuinbcred from the equator to the poles, fir .showing the latitude ; and two from the poles to the ec|uat'ir, eiiablini,' us to elevate the poles t ■ any reipiired hei:^h(. The Quadrant of Altitude.— 75. A thin slip of br.iss, coi'eaponding in its graduation to the bra'cn meridian, is called the Quadrant of Altitude. It is numbeied from to KO", to enable us to find the distance between places; and also from to 18^. for finding the dura- lion of twilij;lit. The Hour Circle.— 70. This is a circle, either of brass or marked upon liie (.jlobe, around tiie north pole. It is divided into 24 equal parts, rcpresentiu); honrs. It enables I's to find the ditlereiiee uf time between places, and also the len(;tli of the day. PROBLEMS. I. To find the latitude and longitude of any place :— 77. BrinR tlio given place to the graduated edge of the brazen meri- dian ; tin; degree marked over it is the latitude ; and the degree on the equator, cut by the same edge of the brazen meridian, is the longitude. EXERCISES. -7'^. Find (lie latitude and longitmL' of the followii i? places : — In.Kilc I.oiijllii.l' Halifax \>i>. ii ;!>■ N.; (1;^ 30' W. Ottawa ■»r)'2.V N. ; 7.V 4,^■ W Cliarlollctuwn U\' 14' N. ; 03' Jo' W. Quebec 40" 4 H' N. ; 71" 13' W, St. John 45' 14' N. ; 00' 3' W, London ra" 30' N. ; Lon. Paris 48' fill' N. ; 2" -'o' K, Cairo 30' '.>' N.; 31" IT/ K. (':ipo Town 'Yi" fill' M. ; la" '.'S' K, .•aloutla 22" 33' N.; fS'' lU' K, NV.isliiiigtfin ; Jeru.saluin ; North Pole; NowOrleamii (^nito ; Mcliiourm . II. The latitude and longitude being given, to find the place : - 70. Find the given meridian on the eqnator and brluK it to the brazen meridian ; find the given latitude on the brazen meridian, and beneath it is the required place. When the place is found, all others having the s.aiue longitude can be found, by tracing along the ed^'e of the brazen moridian from pole to pole; and by turning the globe, all jilaces having the same latitude will pass under the same degree on the brazen tneridian. EXERCISES.— 80. Find the places situated as follows :— (1.) N. lat. 41- 54' and fi. lon. 12'' 27' Ans. Rome. (2.) N. lat. 39° andW. lon. 2S° Azores. (3.) S. lat. 55' 58' and W. Inn. 07" 11' Cape Horn. (4.) S. lat. 33° 50' and E. Ion. 1,S° 2S' ("ape Tuwu, III. To find the distance b'Hween two places :— 81. Find the nnmber of degrees between the places with the quadrant of altitude ; and multiply by CO for geographical miles, or by C9,'n for English miles. If the distance is more than II'V, nieasiiro it with a tliiead, and lind the iiunilier of degrees by apidyinj the thread to tlie eijuator. EXERCISES.— 82. Find the distance in English miles between the fnlliiwiiig places : — (I.) Halifax and Montreal \ii.f. 41)0 Eng. miles. (2.) (.'ape Iliirn and Cape of (iood Ilo|ie 4140 ,, (3.) Newfonndiand and Ireland 1830 ,, (4.) Newfoundland and Vancouver Island 2'JOO ,, (5.) A shi|) snails from Halifax to Liverpool in England; thence to New York; thence to Ilio Janeiro; thence to Halifax: what is the whole distance 1 IV. Two places given and the time at one, to find the time at the other ;— 83. Bring the place at which the time is given to the brazen meridian; set the hour circle or index to the given time; turn the gloue until the other place is brought to the brazen meridian; -the hour circle will sliow the required time. EXERCISES.— 84. The followin,' can bo verified by calculation :— (I.) When it is 12 o'clock noon V London, what is thetiiueat Halifax ! Aii.^. 7h. 40in. a.m. (2.) When it is 1 o'clock in the afterncoa at Ale.vandria, what time ia it at 1 iiiladelphia I An:'. A.M. (3.) Wiien it is 1) o'clock in the morning in Halifax, what ia the time at Ottawa ! Aiis. 8li. r2m. a.m. (4.) When it is 4 o'clock in the afternoon at London, what is the t'lne at St. IVters'iurg ? Aim. I'.M. (5.) When :' is noon at Halifax, what time is it at Melb nirne ! Aim. Ih. 54in. A.M. V. To find the antipodes, or place directly opposite: — 35. Set the poles of the globe on the horizon ; turn the globe until the given place comes to the eastern horizon ; observe the number of degrees the place is north or south of the eastern point of the hcizon -the antipodes will be the same number of degrees on the opposite side of the western point, EXERCISES,- 80, Find the anlipndcH of the following places :— U.) LoniloM l/i.^ .Vntipodes I.iland (nearly). (2.) Halifax... 41* 38" S. lat. ; 116' 24' E. Ion. (3.) The llerniudai The south-west .<( AuHtiali.i. (4.) C.'ipe lloin The uasl of Lake ilaikai. VI. To rectify the globe for a given 'niace:— 8". Elevate the pole on the same side of the equator, as many degrees above the wocdcu horizon as lu'c equal to the latitude uf the place. When the kIoIm' I* I. 'titled, if the given plaoo b« brntubt to the brasou meridian wooden 1 EXEK Halila (,'alcutt! VII. or the as mediate THE TERRESTRIAL GLOBE. 21 B brazen meridian, same longituJe can meridian from pole ^ tlie suuio latiluilo iilian. jljows : — lis. Rome. Azores. Cape Horn. Cape Town. places :— e places with the eographical miles, a t!ire:ul, and lind i equator. iiiilt's between tlie .f. VM) Eus. miles. ....414(5 ...1830 „ ....2y0() wiglaiid; thence to lifax ; what is tlie ne, to find the 'en to the brazen en time; turn the n meridian; -the )y calculation ;— le time ut Halifax I idria, wlmt time is , what is the time what is the t'Uio I at AK'lljdurne ? ly opposite : - II the Klobe until vi> the number of rn point of the )f dcjifrees on the iriK plaees :— nearly ). C':'.r ]•;. Ion. Aiistlali.i. taikil. i:— uator, an many L> latitude of the iitlit to tlio bratuii rrr^j iii.riilian, it will Ijc in the zenitli or hi(,'iipst part of the globe, and the w ooden horizon will become the true horizon of the place. EXERCISES.-88. Rectify the nlobe fur the foUowinc; places :— Halifax, St. .lolin, Mexico, Juan Fernandez, St. Helena, Quito, (.'alcutta. VIL To illustrate the three positions of the sphere, or the aspect of tlie lieaveiis ut llie eqiiatur, lliu jiolcs, and any inter- mediate place ; — '1.) At the Equator.- s;» place the pnlcs in tlie horizon. It will he seen, liy turning the globe, that the equator and p.iralk'l.'i ahviiys out the horizon at right angles ; that whatever nt.ay be the Sun'n ileeliiiation, he will rut the horizon at right angles at sunrise and sun.set : and that as thi^ iiarallels are all divided enually by the horizon, day and nij.'lit must be e^iual throughout the year. This is the aspect to one situated at the Kiiuator.and isoalli d the rhj},f .ijiluri-, (2.' At the Polo. - !)0 Elevate the north pole llir, Tlie equator now corre- ppond.s with the horizon, and all the iiarallel.s are parallel with it. It is manifest that all the celestial bodies north of the eqiiinoi'tial must be eon. s antly visible anil move around in eireles, as the Karlli revolve.'', the size of the circle defending on their elevation. 01. The Sun will eonie above the liori>on at the vernal eipiinox, and will move around the horizon in a kind of s|iiral, rising higher every day. until hi.' attains his extreme elevation iit tlie suininer solstiee, when ln' will ile- .seenil, until he sets at the autumnal equinox, not to apjuar again for six nionilis. Suci. Is the aspect at the North I'olo. It Is called the iimnlh i .s/./o nr (.3.) Between the Kquator and thd Pole.- !»■.'. Ity taking dlii'erLnt posi- tions on the glolie, as 10", 'Jo , liir, nnd reotifyiiig the globe to the several 1 ititudes, we shall find that as we ap|iroaeh the pole, the equator, iiarallels of latitude, anil the Sun at his rising and setting, cut the horizon more obliquely. Any .such iiosition is ealleil an / '■/17".' c/i/oti'. IKS. To illustrate further, elevate the north pole ^!>', the position near tlio middle of Nova Seotip,. The polar .tar has here an elevation of 4.'i''. and all the stars within that ilistanee of the jiolar star will Im- constantly above the horizon, luovlng urounil in eireles. It will be seen that the horizon divides the equator I i|ually. and all the piirallels uneqiiiilly, and hence that when the Sun is in the eqninoetlal. day and iii;.'ht must be ei|ual, and at all other times un- equal , also, that from the vern.il to the antumn.il eqiiinov. when tlie Suii is In the Northi'rn Hemisphere, the iliiys will be lon;.'rr than the ni^dlts, ai'd during the other halt of tlie yeiir sliorler. 04. We e;in see, ton how twilL'lit is h.nger In hli'h hitlludes than neiir the Kquator, for a |ilaoo unn have twilight only when the .sun Is within la uf tliu horizon. VIII. To find the length of a degree of longitude in aiy given latitude : - 05. With the qnadraut of altitude take the distance between any two meridians along 'he ijiven parallel, and multiply by 4, for ((eographical miles. Vo convert Kcojfraphical to English miles, multiply by C91, and divide by GO, The miTldlans are laid ih wn upon the globe l.'i" ap.irt, nmki'ig Jl In all, (iUe for eiieli .lOiir in the dillereiin of time. K\i'relses e;in be tiikeii from the tiilih', p.i.-e Is IX. To find the Sur/s place in the ecliptic on any given day:— 90. Find thcdayof the Month on the wooden hori«on, and opposite to it in the circle coutalnli k the sittus of the zodiac are the si){n and decree in which the Sun is situated on that day ; lind the same slffn and detfroc of the ecliptic on ii.v> globe, which is the Suns place. EXERCISES, 07. Find the Hun'n I'laee on the following dny» 1— (1.1 March ;|0 Ann. Arlen. (■J 1 Miiy n Id* 'JUl doKice of Tiiiiiu* (M. AuKuitt in (4 ' DeerinliiM' 'i\ (6 I'ehruary 4 X. To find the Sun's declination on any given day :— Dd, Find the Sun » place iu the ecliptic for the given day, and biing that place to the brazen meridian ; -the degree marked over it is the declination. I'.y turning the globe, all places to which the Sun is then vertical will j. i^s under that degree. EXERCISES —;«t Find the Sun's declination on the following days, .and tlie places to which lie will then be virtieal : — (l.)May 10 1 U.S. 17" .'to' (2.) June 21 1 /OS. 23" 27' X September 21 '4. .lanuary lo XI. To find the hour at which the Sun rises and sets at a given place on a given day :— 100. Rectify the globe for the latitude of the place ; find the Sun's place in the ecliptic, and bring it to the brazen meridian. Set the hour circle to 12 ; turn the globe till the Sun's place comes to the eastern edge of the wooden horizon, and the hour circ'.,' will show the time at which the Sun rises. Turn the j;lobc till the Sun's place comes to the western horizon, and the hoi>r circle will show the time of sunset. Having the time of mnrise and sunset, the leimlli of the day can readily be fouml Also, the :iiiiplilnde of the Sun can be found by nb.serving the point cut In the horizon by the Sun's place In the ecliplie. EXERCISES. 101 Find the time at which the Sun rises and sets ; als.i • lie length of the day and the amplilnile of the Sun on the 21st of .luiie and the 21st of Kei'einber, at the following places : - 1 Halifax ; 2 London : :t Canton ; 4 I'lipe Town ; ,''1 Lima ; li (Quebec. /Iii.i. 1. Hises, 21st.liine, 4h. Um ; sets, 7h 4*ni Alls, ['i.) Rises. 21st Deeember, 71i. 4,''iin. ; sets, 4h. I.'iiii. XII. To find the duration of twilight at a given place on a given day : 111-'. Rectify the globe fur the latitude of the place; bring the Sun's place iu the ecliptic, on the given day, lo the brazen meridian : set the hour circle to 12 ; fasten the quadrant of altitude upon the brazen meridian, over the given latitude ; turn the globe till the Sun's place comes to the western id^'e of the wooden horizon. The hoiir circle will now show the time of the Sun's setting, or the be- ginning of twilight. Continue the motion of the globe we>tward until the Sun's place coincides with 18' on the quadrant of altitude below the horizon, aim the hour circle will then show the tiiue at which twilight ends. EXERCISES. ■ 10:1 I'Ind the duration .,f IwiliL'lit on the " i|h Maieli, 21st .Mine, 2Hril Se]itenil er, and 21sl December, at tli" follnulng plaeeil : I. Nova Scoti.i piriillel of 4.'i ; 2. Orkney islands; ;i. Noiwuy (i;il* ilo j 4 The Kqmilor A11.1. The length of twilight at the iibnve pliees, on '.!iMli Minh mid 2: rd s. picudier, is I Ih :ioni ; 2 2h l.'iiii. ; :i :ili l.'.m. , I Hi IJiii XIII. To find the length of the longest day and the longest night \t any given place in the North Frigid Zone :— liM. Rectify the globe to the latitude of the place; bring the hk- cendiuR signs of the ecliptic that is. those going before Cancer 10 the north point of the horizon, and observe what degree of the ecliptic is cut by that point; lind on the wooden horizon Ww, day and month corresponding to that degree, which will be the commencement of the longtst da) Friiig the desoemliug sii,'ns those after Canter to the north point of tlie horizon, and observe what degieo uf tho ecliptic Is cut by that point ; the corresponding day on tho woodou horizon will show th ' time of Hiinset. The beginning and end of the loiigciit nl.:lit can be found, by pioi ling In the siiine manner with the ■ouHurn point of the horUoii EXERCISK. lo.'i Find tlic 71 :io N 1,1 Ann Heveiily s .v.qi di.>« 'I'hi I IhetWlh of.luly. length of Hie Imigest ility nt < ipe Nmlli, SUII rliieii ou the llthnf ,M,;y. and li-tn on PHYSICAL GEOGRAPHY. EXTERIOR AND INTERIOR. --ti MOirXT IIKCI.A. Tho Earth's Crust.- 1. TIio outer portion of tlip Earth is cilloil till' cnisf. Near tlic mirfiico we UKiially find loose niatcrials, calli'il soil, cartlis, jiravol, and stones. On di^'^init tlirouuli tlieso we eonie to solid roek. Miners linvn poni'tnti'il intn (lip RartliV crust nrnrly 40cn ii nbout 2000 feet, in Vr\\K»\ix. 1!. The inntoriftls fnrmins tlie Kfiriti'n prnnt nrp ilivlilcd into .Siw;i/i' nnA ('"mi'OKiiil. All ('iiniiKiniul bmlici vt\\\ W .ifpiiriitcil into two <'i' in Imillpi". (i', I'pi'mikc it cnnnnt lie I'PKolveil into ok'inentary |mrt», H'li^r in ii poiniiound sul)stanop, lip- p.iuse it pon bp sp|mrntcil into tliP eloinpntR o.vfififti nnd Inidroiifii. Tlip nnmbpr of ilpniPiits, or Riniplo snlmlnncPH, of wliicli cvor^tliim: is potnposcd, po fur ns dispovrry liiin (Irtoriniiii'.l, iit iil>ont. si.xly. Tlioy (irp KonictiniPH fonml in lliiii- Hini|iip stato ; but nimi' fii'ipipntiy I wo or inniv ail' poinliiniii, tlois t'ornnn;.' tlio nmt('ii;il of wlii'li rvoiytliiiijj niinrriil, vpl'c lal'lp. nnil iininm! is p(iiii|ios(i|, !!, Tlii:< mutoiiiil )ir;lit Mmli'r the )iohpi- of vouctiiblp or animal life is pallril Oriiniiic Moltci'. It kopuib dtranup lliat tlio l)paulit'iil iiihI fnic'ant rosp, ntul pvpn oi\r bodips, il oil the coast id' Iceland ; and one in ISIil on the count of .*^icily. Uolli these islands siil)sei)nently di.sap]jeaied. ^7. Many islands, ptirticidarly in the trojiicul parts of the PaeiHi>, owe tlieii' crk'iii tn the coral insect. Tlieso little creatures secrete lime niiil other siihstiuiees from the ndter, wliich they form into roi^k. They cannot live in deep water or on dry html. They therefore com- mence operations on lucks and shoals within two hundieil feel of the surface, and cease on reachin;; the level of the sea. Ceiallinu islands are HomelimeB fiii titer elevated by volcuiiiu force, but they uru uaually low. 18. The islatidn of the Pacific often prewnt a highly pictureBtitie appearance. Some of llicni, as Whitsunday, coiiHist of a rinn of low land with II la^;ooii in the centre; others, like Tiihiti, are snrrounded hy a huooii which is Hcparated from the ocean by a coral leef. Surface.- lO. '''he hind j.s cNceeiliii.i^ly vnrietl in respeet to eli'Viuiidi above tiie sea. Sometimes the iLseent from the water's edge is ;;entle; in other iilaeeH, tlit^ shore line is pre- (■i|iitoHH, varying in height from a few feet to Kcvenil liiintlred feet. The highest land is usutilly in the inlcrior. Tracts itf land arc ealled jdaiuf!, plateaus, hlUs, yiountains, and vaUetjs according to their elevation. Although the land is generally higher than the level of the sea, there ate di.stricts where it is otherwise. The most remarkable ile- [iiessions are in Western Asia, near the Caspian and Dead Seas. The surface of the Dead .Sea is 1312 feet below the ocean level. 2i). Tiiere are inanj extensive Jiiid comparatively level tnict.'i, varying in elevation from a few feet to tlireo miles aliove the se;i,. Wiieii under 500 or GdO ft^et high, they are called phtinf, when more eleviite-l, /iluteaits or table-lands. riiitcaus arc often rainless deserts, destitute of vegetation. A great desert extends nearly across the Eastern Continent from west to east, passing through Northern Africa and Central Asia. The most extensive jdains in tip; Western Continent are in the middle of North America from the Arctic Ocean to the Crulf of Mexico, and on the east of South Americti ; tin; most extensive in tiie Ivistern Continent are in the north ot Europe and Asiti. 21. The mountain ranges, witii few cxception.s, run in the direction of the greatest length of the land. They are also freiiuently on one side of the ctamtry, presenting a loiiu and gentle slope towtirds the more distttut ocean r-s/iftl between streams ilowing in opposite directions. The Rocky Mountains ami Andes are water-shed.s. Some important water-sheds are iiuito low ridges or mere swells in the surface. Thu souives of tliu AlissJNNippi and Volga are cxampleH. JStreanis often make their way through miMintain ranges by deep gorges. 27. On mountains and table-lauds thu cold rapidly in- crea.ses with the elevation. i I *■, ami valUiji ;vel of the sea, reiiiiukHble de- lead Seas. The ratively level three miles liiyli, they are r table-land''. jf vegetation, 'I'll Continent n Africa anil Continent are rctic Ocean to America ; tlio 1 the north ot ns, run in tlie Tiioy are also ng a long and md an abrupt jutii America, eat divisions ; .'nu; heiglit. n Ceet, is the traced than nw ridges, but iiisiiig two or int a moderate 'rt:iiii jiai'tf, it iiitunu level, it lirnnuitiiij; tlie iiiial streams. hpriiigK aliiii)! she.i, exhaliiiK '1 rivers. tinjr K''i"lf"l :e directionu. .4. nicro bwcIIk in are exaiii|iluii. iiuc'it by deep rapidly in- RIVERS— LA KF.S. 25 It is a singular illustration of the adaptation of the Earth to its inhabitants, that liii;hlands occur most frequently wliere tlie sun's rays are most vertical. If the northern part of the continents were tahle- hinds, they would be uninhabitable throu^rh intense cold. 23. Mountains were probably formed by ujtheavals caused by the expandinji power of the great iicat in the interim r of the hearth. The same cause is still at work, gradually producing similar results. In various parts of the Earth the subterranean tires ha\ okcn through the crust in volcanoes, where vast fpiantities ot i.iva are poured out. About a century ago, the volcano of Jorullo burst forth from a plateau of Mexico and in a single night raised a mountain over 4U"0 feet high. In 1S22, a portion of the coast of (Jhili was elevated three f.ct. A portion of Sweden, along the Haltic, is being gradually elevatdl at the rate of a foot in twenty-live years. Volcanoes are usually near the sea, either on islands or maritime parts of the continents. Some of the most noted volcanoes are Vuto- IKixi, in South America; E(ua, in Sicily; and llcda, in Iceland. 20, Earthiiuakes are movements of the ground, varying in degree from slight tremors to the most violer.t concussions. They are ninsi common in volcanic regions, and are supposed lo ne occasiuned by the i-.ime causes as volcanoes. Sometimes ihe ground rises and falls, like the waves of the sea; and sometimes It has a circular motion, like that causi-d by throwing a stone into still water. In the great earthquake of 1757, which lasted about six uiinutes, almost every building iu Lisbon was laid in ruins, and 60,000 persons lost their lives. CaracMS was destroyed iu ISl'J, and 10,000 persons were killed in less tli,"i a luinuto. Rivers.— 30. If all the rain wliich fails uium the Eartii wore to run off innncdiatcly almiL; the .surface, tiic lowlands would in the wet season he inundated, ami in seasons ot drought wo would iiavc no water — neitlier streams, s])riHgs, nor wells. A large jiortion of tiie rain anil melted sno v .sinks into the ground, until bi.'ing arre.-^h'd in its cour.so by rocks or clay, it makes its way to tlio surface again in t'le i'onn of springs. Springs give rise to brot)k3 and are tlie primary sources of rivers. Some rivers iiave tlieir origin in hikes; otlicrs are formed by the melting of snow and ice on iiigii niotmtain.s. Some of the leading features to be noted vesiiecling rivers are tlieir ronrtic, length, volmnr, iuid C'lucil//. 31. The course of a river depends on the hlopo of the land. Hosi Those uliii'h rtfiUis .itnaiug, htit liiitr no fi.siUc oiitlit. (4.) Those nhich both riuivc niid mud out xtmtinn. "7. Lakes of the first class are often found in the craters of extinct Volcanoes; they, as well as those of the second class, are usually small and derive their supply fruiii springs. 33. Lakes of the third class discharge tleir surplus waters by evaporation. Tiny are all salt except /.(tki. Tthud, in Africa. Such lakes are most nunicrnus in Asia. Tlie (Ai.ijiiitn, Anil, and Jtcnd .s'l'd.i, and (inut .S(i/< /.akc of North America, belong to this class, 3'J. Lakes of the fourth class are the most nunieious, oecurrinij aloiiij the courses of rivers, particularly in northuni latitudes. The great lakes of North America and of Oeiitral Africa are the largest fresh-water lakes. 40. The /trad Sea. 1312 feet bi,l.,w the r-oa l.vel, is the lowest l.ike known; Sir-ikol, in iJiiitial A.sia, l.'i.tioo tVot above the sea, is the most elevated, TiitMai, iu South Aluericu, has .iu elvvalioii uf 12,S60 feel. THE SEA. Extent. 11. The nca cuvers iilmut thne inurtlis uf the I'l.irtii's Hurl'ace. Its area is computed to be i'i|uiil tu a si|Uare uf over 12,li(iO miles. Dopth,— 42. The lieifof the Ken has all the irregtilaritici of HUrface which we see on the land. Hence the depth varies greatly in ditlerent parts, it is nuppuHcd that tho greatest depths are not less than eight ur ..iuu mik'8. llu* i^^msuaam 26 PHYSICAL GEOGRAPHY. WIIAI.IC HSIII.VO. liiililo iiieasuromeuts have been made to the Jeptli of about five miles. Tlio pressure on the lower waters of the sea is very sre.it. If ;i ooiked liottle be letdown empty, tlie cork >vill be forocil in. Contents.— 1:5. Soa water contains several mintjral sul)- stauees, as common salt, lime, magnesium, potassium, and iodine. Some of those substances arc extracted from tlio water, in large quantities, by marine animals, in tlie formation of sliells and coral. New supplies are contributed liy the rivers, so that the composition of bea water remains unchanged. Temperature.— 44. The sea maintains a more uniform temperature than tin; land. The waters of the ocean are ever ehanpinR place — flowing back and firth between the jiolar and C(|uatorial rcf-'ions, so that the same water is not exposed for a long time to intense lieat or cold. Also, in warm regions evaporation is very copious, liy which the accumulation of heal is prevented ; and iu cold regions water parts with its heat less readily than laud. Divisions. — 4,^', Althom;]! the ocean forms one iireat con- nected I'ody, it is usual to consider it as separated into five lirinciiml divisions: — 27ie Atlantic, Pucijic, Indutn, Arctic, and Antarctic Oceans. Branil"* of fiiese oceans, extending,' into the land, lake various uumoa, va seas, bays, gn(fs, channels, and straits. id. The Atlantic lies on tho east of America, which it separates from Europe and Africa. The Polar Circles are its northern and southern limits, and the Ecjuator divides it into North and Soiah AVnittic. The principal branches of the Atlantic are, on the American side, Davis' ,Stmit, finffin's Bay, Iliuhon's Bay and Strait, the Gulf of St. Lawrence, Bay of Fumly, Half of Mexico, and tlte Caribbean Sea; on the eastern side, the Xortli Sea, Baltic Sea, Bvijlish Channel, Bay of Biscay, Mediterranean Sea, and the Gulf of Uuinet 47. The Atlantic varies in l)rea(ltli from 000 to 4000 miles It is of gre.it importance in a ctiumiercial point of view, forming tlie Brcat liigliway hu- tween America and Kurope A 6ul)niarino plateau in tlio North Atlantic forms tho bed of tlie telegrapli cables botwoeu Newfoundland and IrelaniL 48. The Pacific is on the .vest of America, separating it from Asia and Australia, and it extends from Behring's Stiait, on the north, to the Ant,arctic Circle. It is divided into North and South Pacific by the Equator. The chief branches of the Pacific are the Qnlf of California, on the American side; Behriny Strait, the Sea of Kamchatka, Sea of Okhotsk, .Sea of Japan, Ydloin Sea, and China Sea, on the coast of A.sia. llehring Strait, connecting the Pacilic with tho Arctic Ocean, is about thirty-si.\ miles wide. 41). Tho extreme breadth of the raclftc Is about 10,000 miles, or nearly halt the clreumfiTt^ieo of tlio lOartli. It is noted for the number of iU island: 'rhi.'t Kreat oci'iiii was: unltniiwn to lOurapeaiis uiifil IT)!;), when It wiis dis- covered liy a Spaniard nanuil llallioa, wlio eron.ted the Isthmus of I'auania. The part of Hie nceaii scrn from the iiioimtiiiiis of tlin istliinui lay on tho Boulh. from which the raeidc rceiivcd tho name of thn South Soa. MaReilan, who crossed tliis ocean in If.^l, ealliil it the I'aeiHe, bt auso ha unuountuied no stormii on Ida voyaKu 50. The Indian Ocean lies south of Asia, having Afriwi on the west and Australia on tho east. Tho Antarctic Circle is tho sontliern limit. Its branches arc Mozaml'iiur Channel, Bed Sea, .\rabian Hca, Persian Uulf, and the Bay uf Bengal. ft' m a? hicli il si.'paiatea its nortliern and Xortli and Soutli ! B Atiieiican side, tiie Gulf of St. Caribbean Sea; 'sh Channel, Bay It is of great rent lilRhwiiy be- Ncith Atlantic iiiul Hiid IrulaniL ng it from Asia ' on the nortii, to "iouth Pacific by I difornia, on tlie ' Sea of Ok/iotak, iif Asia. ii'ctic Ocean, is Ics, or nearly IiaK iif it.i islaiidf v;\h:\\ it WHS dis- iniH of I'luinnia. liiim:) lay on the III Sea ille, Ik auno ha -ioa on the west I Boiitlicrn limit. Arabian Sea, TIIE SEA. L'7 61. The Arctic or Northern Ocean is on the nortii of America, Europe, and Asia, witliin tlie Arctic Circle. Its principal branches in the Eastern Hemisphere are tlie White Sea, Sea of Kara, and the Gtdf of Obi. It is much broken by islands on tiie north of America. Tiiroughout a long winter this ocean is covered with ice of prcal thickness, wiiich breaks up in the spring and drifts down in vast masses, called icbcrgf, into tlie North Atlantic. 52. A navigable route from the Atlantic to the Pacinc. through the Arctic Ocean, was long sought witli great ardour. The most memorable and disa.s- trous expedition for the discovery of Vic Nnrtli-Wcd Ponsiirii: as the route on the north of America was called, was that commanded by sir .lohn I'rankiin, who sailed from England in 184.1 with two sliip.s and VMi men. None of the party ever returned. One of the crew was a Nova Scotian .OS. Whilst in the search fur Franklin, Captain M'Clure, entering by Behring Strait, m.ade the whnle pass.age on the north of America to the Atlantic; but he was compelled to leave his vessel frozen fast, and to go pp.rt of the way over the ice. Navigators have often m.ade unsuccessful attempts to reach the North Pole. The nearest point yet reached is 82' 4;')', by Captain Parry. t4. The Antarctic Ocean is situated within tiie Antarctic Circle. Tlio colli is even more severe than in the Arciic, and tiio ico extends furtlier from the pole. The highest latitude reached in this direction is 7S' 4', I'y Sir, Tames Ross. In 1841, Kir .Tames Tioss discovered an extensive tract of land in the Antarctic Ocean, tn which bo gave the name fif Victoria Land. He .-il-o di.scovered a lofty volcano, 12,400 feet in height, which he called iMdinit Erebus. Tiio Arctic and Antnrctio Oceans are tlio favourite resort of wlirijes, .a the capture of whicii many vessels are engaged. Motions of the Sea.— ;")5. TIio wator.^^ of tlio dccui Iiave three kinds of movements, arisincr from distinct c'lnso.s— waves, tides, and currepts. Y>\ tlic unceasing .ijiitation of its waters the ocean is preserved from putrefaction. Waves.— .'iO. Waves are a.tritations of tlie surface water, usually occasioned l»y the wind. Except in shallow water, and when the wind is very stronir, there is iid onward How of water; hut each wave communicates its motion to the iie.\t. .17. It is tliouglit th.Tt oven by the i ost vident \\ iiids the water is not distnrlicd to a greater dejilh tiian iyw feet. Tiie higliest waves are found in tlie Atlantic, oil' the Cape of (J.mkI Hope, where, from the hollow or trouiik of the sea to the crcd nf the wave, the height is sou'Ctimes forty feet. The rise of waves is (distrucled by ice-c;ikes or sea-weed fi lating on the water, and by dcn«f fog.s. Throwing oil iip^n the surface will al.-o prevent the rise of waves. Tides. — 58. Tiie ocean is ever clian!;iii;; its level. The waters rise for about six iioiirs, tind then fall fur the same time. This alternate risiiii; and fallini.' of the ocean is called t/ieddc. When the water is rising,' we call it jhiod tUh' ; when it is falling;, cW (iile. 6P. In the open ocean the height n; l.io tide- thai is, the difTeroncc if level between hni! water and hi'jh water— \n from three to si.>t feel ; but when the water is furced up narrow liays, the tide is much hi.'her. in the Hristol (Jhannel tlie height is from forty to fifty feet, and in the bend waters of the Hay of Kundy sivly or seventy feet. In inlaii'l seas like the C;ispian, Illack Sea, and IJaltic. there are no tides. 00. The tides nre caused principully by the attraction of the moon. They are .also considerably modified by the attraction of the sun. This liody beirg more remote, is thought to exert only about one-third the influence of the moon. t1l. Water having but little cohesion among its particles is easily dis|ilaced by any force acting upon it ; and as the attraction is strongest directly beneath the moon, or where the moon is vertical, the water is drawn to that meridian from either side to the distance of 00°. The whole body of the sidid e.arth is also drawn towards the moon, whilst the waters on the opposite side remain behind, f rming another convex ridge.* Thus there are two meridians 180° apart, at which it is high water simultaneously, and ether two intermediate, and the same dis- tance from each otlier, .at which it is low water. This is shown in the diagram. It is liigh water at a and li, low w.ater at c and (/. >■.. N\ A -. M .S] 3-.-. I M /■•",. II. NK.AI' HITS. At the meni's quarters the sun and moon net at right angles, ns shown in this diagram. They are then said to be in ij.iilit)n. as I he sun jiarlially counteiiu'ts the moon's inlliience. It is high water nl (( and b, but the ti'h-s are low, and are called neap tides. ' The above U the common explanation of thu oppoiiltu llilu, but it Is open to obJectloDi, sritisd TinKs. Now, as the Earth turns upon its a.xis from west to east, the two convex ridges of water, rei^resented at a and '), move round the Earth as immense tidal waves from east to west, bringing high water to all places twice every day. G'2. If the moon were stationary, the time between one iiigli water and another would be exactly twelve iiours ; Imt in consequence of the moon's progress in its orbit, it is a little later ea^h day in coming to any ('articular meridian ; hence the time between two consecutive tides is about twelve and a half hours. The greatest elevation of the tide is a little after the moon has passed the meridian. 63. Sometimes the sun's influence is combined with the moon's, when the two Iwdics are said to be in eonjiinrliini. This occurs at new moon, when the siiti and moon are on the same side of the Kanh, as shown in figure 12; it also occurs at full moon, when they are on op] Obile sides of the Euth. At such times the tides are very high, and are called s/iriaij tide.*. # 2H PHjSICAL GEOGRArilY, G4. Tlic foreftoinR theory of tlie tides is on the supposition that the Earth's mrface is wholly coifered with water. It requires considerable modiUciition, ill cnnsequence of the interference of the land It will be seen, by reference to the map of Nova Scotia, that Halifax Harbour and the mouth of the Shul)Bnacadie are nearly on the sar 3 meri- dian. It might I)e supposed that they would liave high water at \ .le same time. But it must l)e remembered that the tidal wave pas.ies around the llarth from east to west. The Bay of Fiindy opens to the ocean on the west, and the wave cannot flow in until it lias passed the extreme west of the province. Its mution ujp the Bay is then from west to cast As the Bay liecomes narrow near its head, the water is crowded; the tide rises higher, and flows more rapidly. Currents. — 05. Broad currents, like vast rivers, arc ever Howiiig tluuii;,'li tlic sea. An excliangc of waters is tlius kept u]) between tlie Eqiiator and tlie poles, and among the (lift'erent ocean.s. A current ilowinj; from the polar towards tiie equatorial regions acquires a westerly tendency, and one flowing in the opposite direction becomes more and more easterly as it advances. (16. Navigators arc in the habit of throwing bottles into the sea, containing slips of paper stating where they were cast out, and when. The bottles course along with the current. Every navigator who falls in with them iiote.g the place and time on the paper, and sends them on their voyage. Tiie products of tlie West Indies are often cast upon the phores of the Azores and Ireland ; the products of Ciiiua are curried to the Aleutian Isles; and drift-wood is carried from Xortherii Europe to Iceland. Tlicse are some of the jiioofs of the existence and direction of ocean current.^. G7. The following ai'c the iiviiicipal Currents ; — {"[,) IlumlohU's Ctiviriit, (lowing' nortlicnstii-ly froui tlic AiitJU'ctio Ocean into tlie Pacific, along the west ciast of Souili A'liioiica. (2.) The JCqi(at(}rial Current of the Pacific, tlowiiig we.stei-iy fivmi the vest Coast of America to Asia aiiil Aiistiaiia. (3.) The Mozuwli'iiie Viirrcnt. wliicli is ]U'opeily a contiiination "f (lie preoeclini: aero^.s tlie Indian O.'oaii to tlie east co;i.-?t of Africa, where it tlows soutlierly tliroiigh .AIiizaiiil'i(iiie Cliaiinel to the C'a|ie of tiood Hope. (1.) 7'/.c Equatorial Cvrrent of the Atlantic, flowiii^r from the Ant- arctic Ocean to tiie west coast of Africa, ami thence westerly to Soiilh A inerica. (T). ) The ('III/ Strerim, flowing iioith-easiei'ly from the (lulf of Mexico to Northern Europe. (0.) The I'lilar Current, sotting down from the coasts of (Ireenlar.il, R mlherly helweeii the (iiilf Slreaiu ami the coa^t of Nortli Aiiierica. (7.) 7'he Japan Current, flowing north-easterly across the Pacific from the Indian Ocean to the north-west of North America. (8.) The Okh'it.ik- Current, (lowing southerly along the cast coa.'^t of Asia inside the Japan Current. (.8. A current Hows from the .\ll;intic into the Mediterranean; anotlicr from the Indian Ocean into the \Ui\ Sea. There arc many other currents, cnnie constant, ollicrs viiriuble, in illtfcrent jiarts of tlie ocean. Also, it has I'cen kIiowii that where surfiice currents llow in one direction, counter currents llow in the (ip|ioKite direction. Thus an under current Hows from the Mediterranean to tlie Atlantic. GO. The Uulf Stream is the tuo.st rcinaikatile ainl iiiiportant of all the currents. An immense volume of water, eight or ten degrees warmer than the surrounding ocean, passes through Florida Strait with a velocity of four miles an hour. As it proceeds northerly it be- comes broader, but diminishes in velocity and temperature. Near Newfoundland it turns to the east, and, whilst crossing the Atlantic, it divides into two branches — one passing nnitherly to the British Islands, the other southerly along the coast of Northern Africa. 70. The triangular space lietween the Azores, Canaries, and Cape Verd Islands, forms the centre of a great whirl of waters. It is called the Sar- gasso .Sen, and is covered with matted sea-weed, whicli greatly obstructs navigation. 71. The effects of ocean currents are very important. They speed the navigator in his distant voyages, and they exercise a marked in- fluence on climate. The Gulf Stream warms the coasts of Northern Europe, and the Japan Current has a similar effect on the western shores of North America. Humboldt's Current liatlies the hot shores of Chili with the cold waters of the Antarctic Ocean, The Polar Current from the Arctic is le.s.^ genial on the eastern coast of Jiritisli America, retarding, with its chilly north-east winds, the advance of spring. 72. All tlie eau.ses on vhich ocean currents dejiend arc not well known. It is probable that the two prineiiial causes are the Kaith's rotation on its axis, aniuatori;il ng influence, by us the Kqiiutu- continetits, are led towards the n the parts of more and more 'apiiii Current, iulluence on urt/'s '• I'lnisi- we liroiltlie, fnify-live or iitidii mi its y of a mixture 'f 7!' of nitr 1- s n uniull frao- ry VMpniir, tllliuil<' itd THE ATMOSPHERE. W liaiticles that it is eiisily displaced, and wo move about in it without feeling the slightest obstruction. Except when laden with condensed vapour, the atmosjiherc is perfectly transparent, so that objects are seen through it with the greatest clearness. It is not, however, quite colour- less ; for when we look through a large volume of it, as up- wards into the sky, or at a distant mountain, it appears of a biue tint. Air is exceedingly elastic. If we nearly exhaust it from a closed vessel, the little that remains will expand and fill the whole space. 78. The air has iveigki. Its pressure at the level of tlie sea is nearly 15 jiounds to the square inch. A column of air of the full height of the atmosphere is equal in weiglit to a column of water of equal base 34 feet higli, or to a column of mercury 30 inches in height. 70. Tiy means of atmnsjilieric pressure water rises in the p\inip to the height of al)Out ;U feet ; also, tlie mercury is sustahied in tlie tulie of the barometer to the height of about '.M inches. Tlie pre.ssure varies witliiu certain narrow limits, according to the temperature, humidity, and elec- trical state of tlie air, causing a corresponding variatimi in the heiirlit .if the mercury in the barometer. This instrument, therefore, becoiiies an index of the condition of the atmosphere. 80. As we rif,e above the sea-level, the density and pres.sure of the air rapidly diminish. At the heiu'ht of 20,000 feet, the pressure is re- duced less than half. Thus the barometer is use 1 for determining the elevation of mountains. In conseipionce of the diminished pressure, water, mercury, and other liquids, boil at a lo.ver temperature on mountains. The density and pressure of the atmosiihere are essential to iuiimal life. On high mountains breatiiing i.s ditiicult, and the blood bui'sts from nnse, eyes, .and cars. 81. The oxygen of the air is the great supporter of combustion : hence where there is a scanty siqiply of air, the lire goes out or burns feebly. Air is also essential to animal and vegetable life. The Creator has wonderfully provided that tlie two great classes of oruaiiic exist- ences shall each give to the atmosphere greater adaptation to the wauls of the other. Carbonic .acid, which is highly poisonous to animal iil'o. and is cojiionsly thrown from tl'.e lungs in brcTlhiiig, is absorbed by the plant as the most nutritious food. Reflection.— 82. Objects become visible by the light which passes from them to the eye. Some bodies, like the sun, are luminous, emitting light of their own ; others are dark, and are seen by rcllect- ing or throwing olV the light which they receive from some luminous body. The atmosiphere reflects the light of the stin. ami thus dilVu.scs the r.iys over the Karlli. Were it not f'r this jiower of the atmosphere the sun would appear as a bright spot in the licavens, whilst all el-e would be as dark as night. 8:!. Twilight Is also dependent on the same eatise When the sun i.i not more than Is below the horizon, the r.ays of light wlili'h strike the hiirhrr 'egions of the aliiios|ilii'ie are tlu'iiee relleeted to the Karlh. As more rays thus lliul their way to the P'arth when the sun Is near the horlzou, day and night come on gradually. iSiv Karlh