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430 AUSTRALASIA.the surface rise the rocky walls of the encircling hills, through whose fissures areprecipitated several sparkling waterfalls.All the New Zealand fiords offer a general resemblance in the length, narrowness,and great depth of their troughs, which present as a rule but few ramifications.Nevertheless several are connected by lateral branches, which thus formislands of regular outline along the seaboard. In the central parts these inlets havean average depth of over 700 feet, while Milford Sound, deepest of all, averages1,180 feet. All without exception have a sill or bar at the entrance, like the "seabridges" of the Norwegian fiords, and the seaboard is everywhere washed byrelatively shallow waters. Depths equal to those of the sounds are not met in theopen sea within CO miles of the coast.Is this phenomenon due to the vast quantities of refuse formerly brought downby the glaciers from the uplands ? Or are the submarine banks the remnants ofmountain ranges first destroyed and then redistributed in regular layers ? Or arethey to be referred to geological agencies more potent than the glaciers ? Thegeneral form of the coast, disposed in regular convex curves between the fiordestuaries, seems to point at the action of a powerful current, by which the oldbeach was eroded and the debris deposited far seawards. On the east side, on thecontrary, the land has encroached on the marine waters, the rivers with theirsedimentary matter developing vast alluvial plains protected at two points fromerosion by volcanic promontories. One of these is Cape Saunders, under the shelterof which Otago harbour has been opened ; the other is th6 much bolder BanksPeninsula, a superb and completely isolated mountain mass indented with severaldeep-water creeks and bays, such as Akaroa Harbour, Pigeon Bay, Port Levy, andPort Cooper. The south side of Banks Peninsida is connected with the mainlandby a strip of marine sands enclosing an extensive m\iddy lagoon. The wholeformation presents a surprising resemblance to Monte Argentaro on the Italiancoast. Excluding the minor indentations and windings of the seaboard, Thomsonestimates the whole New Zealand coast-line at over 3,000 miles.Physical Features of North Island.Despite the deep gap caused by Cook Strait, the eastern ridges of South Islandare continued on the opposite side by low parallel crests disposed in the samenormal direction from south-west to north-east. But while in the south the Alpinesystem skirts the west coast, in North Island the ranges are developed along theeast side, or at least within 50 miles of the shoi'e. The foundation on which theyrest forms almost a separate region, a long quadrilateral terminating in the southwestand north-east in massive peninsulas, and attached to the rest of the mainlandby extensive plains and rocky ridges, which south of Lake Taupo rise to a height ofabout 3,000 feet. In this eastern region, the culminating point is Mount Ilikurang(5,550 feet), which is situated not far from East Cape. The short Kaimawanachain, whose wooded slopes are often snow-clad to the summit, belongs to the sameorographic system in its general disposition and the character of its old rocks,schists, sandstones, and quartz interspersed with veins of diorite. The crests of
NEW ZEALAND—NORTH ISLAND. 431K;iimawana, which lies near the centre of the ishiiid, attain an altitude of 5,900feet."West of these uplands the rest of the island is occupied by volcanic masses,disposed for the most part without a^jparent order and separated from one anotherFig.186.— Cook Stkait.Scale 1 : 3,000,000.t jtskor Cr-eenw chDepthsby lakes and deep valleys. Mount Euapehu, highest in North Island, forms awhole cluster of 'cones whose common bpse, resting on a plateau over 3,000 feethigh, has a circuit of no less than GO miles. From the two snowy points of theloftiest pyramid, nearly 9,000 feet high, the eye sweeps over a vast horizon
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:y£.:^ >M'%m
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OF THE•JNIVERSITV of ILLINOIS.
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^5 \onrNTED BY J. S. VI'iTUR AND CO
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•ivCONTENTS.CHAP.VI. New Guinea a
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: . . .LIST OF ILLUSTRATIONS.LISTOF
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1*1— ii'^ ixB- , a.•'-'\\• '
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2 AUSTEALASIA.great oceanic depress
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4 AUSTRALAMA.Sumatra to Tasmania, a
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OCEANIC EXPLOEATION. 7110 less than
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LIBRARYOF THEMNIVEftSITYofltUNOlS.
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10 AUSTEALASIA.group discovered by
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12 AUSTEALASIA.as a god, but soon a
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14 AUSTRALASIA.where he'came close
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IGAUSTRALASIA.enterprise the seriou
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18 AUSTEALARIA.,few hundred fathoms
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20 AUSTRALASIA.everywhere a clay fo
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OCEANIC AEEIAL CUEEEXTS. 21ing as t
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M-VEIXE CUBEEXTS. 23of the conflict
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MARINE CUREKXTS. 25consequently rel
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DIUFT ICE. 27drifting northwards wi
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VOLCANIC AGEXCIES. 29Ze;ilanrl, com
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CORALLINE FORMATIONS. 31sequently i
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CORAL FORMATIONS. 83so the reef con
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# .^1'.' k
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OCE.\KIC FLOEA. 35than a hundred di
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OCEANIC FAUNA. 37Old World except i
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INHABITANTS OF THE OCEANIC REGIONS.
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THE M/\.SCAEENHAS. 41in winter, and
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MAUEITIUS. 4:3swept away seventy-tw
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h•, J
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MAUEITITTS. 45aloe fibre, and cocoa
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EEUNIOX. 47highest point of the isl
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4t>*«#. .^,#^
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REUNION. 49standing its fertility,
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OF THEUNIVERSITY of ILLINOIS,
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52 AUSTEALAPTA.Galets, St. Denis, t
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54 AUSTEAI.ASIAoa the banks of Rodr
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5CAUSTRALASIA.are the cocoanut palm
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58 AUSTEAT-ASIA.and Athens in the n
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OF THEUNIVERSITY of ILLINOIS,i
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60 AUSTRALASIA.buffeted by fierce g
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62 AUSTRALASIA.Formerly the island
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CHAPTER III.HE EASTEEN ARCHIPELAGO
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IXDONESIA.6SI.ndo-Malaya andAustro-
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INDONESIA.G7and their conquests hav
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IXDONESIA. 69fortune * some years a
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FLORA OF I>rDONT:SIA. 71whole of ll
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FAUNA OF IXDOXESIA. 73the other isl
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FAUXA OF INDONESIA. 75At the same t
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IXHABITANTS OF INDONESIA. 77In the
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INHABITANTS OF INDONESIA. 79black,
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SUMATRA. 81The Siimatran mountain s
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SUMATRAN HIGHLAXDS. 83wealth of the
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SUMATEAN HIGHLANDS. 85chasm visited
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onKEAKATAU. 87Krakai'au.Till recent
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KEAKATAU. 89ashes and pumice was es
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SUMATRAN ElYERS. 91alluvial lands a
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SUMATEAN ISLANDS. 93to the west the
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IXHABITAXTS OF SUMATRA. 95camphor,
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'.=INHABITANTS OF SUMATEA. 97dant h
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IXUAEIT.VXTS OF SUMATRA. 99The lang
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IXHABITANTS OP SUMATRA. 101On the d
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IN'HABITANTS OF SUMATRA. 103neighbo
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INHABITANTS OF SUJIATRA. 105all spe
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TOPOGRAPHY OF SUMATRA. 107thousand
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TOPOGEAPIIY OP SUMATRA 109about £6
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TOPOGEAPHY OF SUMATRA.Illlocal sayi
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LlSfiARYOF THEiNIVERSITV of ILLINOI
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114 AUSTRALASIA.contribute to swell
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noAUSTRALASIA.coast. Belonging geol
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118 AUSTEALASIA.not disposed in rid
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120 AUSTRALASIA.same geological for
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122 AUSTEALASIA.Permanent European
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124 AUSTRALASIA.ubruptly, the pass
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] 20 AUSTRALASIA.Several ofthe summ
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128 AUSTRALASIA.gradually diminisli
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130 AUSTEiiLASIA.Kiijang, the ScbuT
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182 AUSTRALASIA.and rosins. On the
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134 AUSTRALASIA.The great bulk of t
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136 AUSTRALASIA.people in the whole
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ILIBRARYOF THE'NIVERSITV of ILLINOI
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133 AUSTBAIASIA.Dajâks, and toward
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InoAUSTRM.ASIA.and backwaters. Here
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142 AUSTRALASIA.The little port of
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144 AUSTRALASIA.Labuan.At the time
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146 AUSTRALASIA.annual surplus devo
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118 AUSTEALASLV.mouth of the Kina-B
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150 AUSTRALASIA.north-westwards tow
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152 AUSTRALASIA.feet) was still act
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One of these volcanoes,the Malabar,
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15GAUSTRALASIA.ground caual which d
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158 AUSTRALASIA.the west. Neverthel
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160 AUSTRALASIA.The Arjuno chain is
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LIBRARYOF THEJNlVERSITYofltLlNOlS,
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162 AUSTRALASIA.crater, is encircle
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164 AUSTRALASIA.natural depression
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J1G(5 AUSTEALA8IA.about a Iniiulved
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•invading-J108 AUSTRALASIA.and to
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170 AUSTRALASIA.Javanese aborigines
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J]7-2 AUSTRALASIA,Although less mun
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174 AUSTRALASIA.Economic Coxiiition
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17C> AUSTRALASIA.them absolutely ;
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178 AUSTRALASIA.Java ranks next to
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180 AUSTRALASIA.these is the kapok
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182 AUSTRALASIA.raw sugars in excha
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184 AUSTRALASIA.quite recent founda
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LONDON. J, SVi\Telolvli Betoen^SU N
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TOPOGRAPHY OF JAVA. 185west of the
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LiotiARYOF THEUNIVERSITY of nUNOIS.
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188 AUSTRALASIA.estuai-y accessible
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190 AUSTRALASIA.affluent of the Sol
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192 AUSTEALASIA.The ruins of the Hi
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TOPOGHAPHY OF JA^'A. 193remains of
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ADinNISTEATION OF JAVA. 195for the
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BALI. 197all rapacious beasts, exce
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BALI. 199Public instruction stands
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LOMBOK. 201A table of all the provi
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LOMBOK.—SUMBAWA. 203Mataram, the
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SUMBAWA. 205these debris represente
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FLOEES. 207tain is at present quies
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SUMBA. 209entirely of limestone cli
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TIMOR. 211fourteentli century, and
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TnroE. 213vegetable zones of the Su
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TIMOR. 215fall asleep, and are not
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—TENIin?EE. 217On the other hand
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CELEBES.»219praus, which are expor
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[ 1—iiCELEBES. 221wLicb, however,
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CELEBES.223reaclnug the sea.Thus th
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—CELEBES. 226cultured coastlauder
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CELEBES. 227Topography ofCelebes.Th
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LISRARVOF THEUNlVERSlTy of ILLINOIS
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230 AtrSTEAlASIA.reefs appearing ab
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232 AUSTRALASIA.Guinea. Those of Bu
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—THE SOUTHERN MOLUCCAS. 238region
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iMPiMliBiiiiiiSliS
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—THE SOUTHEEN MOLUCCAS. 285with t
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THE NORTHERN MOLUCCAS. 237Tlie Xort
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THE NORTHEEX MOLUCCAS. 289Nearly al
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THE NOETHEllX MOLUCCAS. 241The capi
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;CHAPTEE IV.THE PHILIPPINES.HE term
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THE PIIILIPriXKS. 245ridge is also
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LIBRARYOF THEUNIVERSITY of ILUNOIS1
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248 AUSTRALASIA.whose slopes occupy
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250 AUSTBAI.ASIA.to its modified en
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252 AUSTRALASIA.60 miles from its m
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lyilABITANTS OF THE PHILIPPIXES. 25
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some places, and especially Luzon,
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—IXHABITAXTS OF THE PHILIPPINES.
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INHABITANTS OP THE rillLlITINES. 25
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IXITAF.ITAXTS OF THE PHILIPPIXES.2f
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LiBRARYOF THEUNIVERSITYefliLlNOIS.
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;264 AUSTRATiASIA.occupies ono of t
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260 AITSTEALASIA.two miles from eac
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'268 AUSTRALASIA.populous member of
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270 AUSTRALASIA.Administratioxof th
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—272 AUSTRALASL^.and its iraportu
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—CHAPTER V.MICKONESIA.I.The Maria
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;270 AUSTRALASIA.Exposed during the
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—THE MAEIANAS. 277although baptis
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THE PELEW ISLAISTDS. 279together, a
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THE CAEOLIXES. 281Eocha readied the
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THE CAEOLIXES. 283also affords shel
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THE CAEOLES'ES 285purchase hatcliet
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THE CAEOLINES. 287tions associated
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—EASTERN MiCEONESIA. 289times eve
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EASTERN MICEOXESIA. 291by breezes f
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CHAPTER VI.NEW GUINEA AND ADJACENT
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NKW GUINEA. 295the great island ass
Page 363 and 364:
PHYSICAL FEATUEES OF NEW GUINEA. 29
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—rrTTSIC.\L FEATUEES OP NEW GITIN
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—CLIMATE OF NEW GUINEA. 801windin
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FAUNA OF NEW GUINEA. 303these are r
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LIBRARYOF THEIKIVERSITYoflLUNOlS.i
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806 AUSTRALASIA.out ever founaering
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H08AUSTRALASIA.frequented market in
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310 AUSTRALASIA.Along the whole of
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812 AUSTRALASIA.time of the discove
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314 AUSTEALASIA."palace," barracks,
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misAUSTRALASIA." Monsieur," as they
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—CHAPTER VII.MELANESIA.LL the isl
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3iOAUSTRALASIA.Hermit and Admiralty
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822 AUSTEALASIA.central part of the
Page 392:
324 AUSTEALASIAPolynesian are inter
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NOETH MELA^ÊSIA. 325Maklaj' to the
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NORTH MELANESIA. 327As a rule the s
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NOKTH MELANESIA. 329west, and which
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—SAXTA-C'RUZ.—NEW HEBRIDES. 331
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SAXTA-CEUZ.—NEW HEBRIDES. 833Clim
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SANTA-CEUZ.—NEW HEBEIDES. 335inla
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—FREXCH MELANESIA. 387remarkably
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—FRENCH MELANESIA. 339In New Cale
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FRENCH MELANESIA. 341brooks apiêar
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—FEEXC'II MELANEf^FA.343Imiaiutan
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FRENCH MELANESIA.3i580 many clans,
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LIBRARYOF THEUNIVERSITY of ILLlNGi.
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—348 AUSTRALASIA.New Ciik'clonia
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850 AUSTRALASIA.the surrounding far
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CHAPTER VIII.AUSTRALIA AND TASMANIA
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AUSTRALIATASMAr
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AUSTRALIA. .353alluvial plains, dee
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—EXPLORATION OF AUSTEALIA. 355isl
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—EXPLORATIOX OF AUSTE.ILIA. 357Th
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THE AUSTRALIAN ALPS. 859which lie w
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LIBRARYOF THEINIVERSITV of ILLINOIS
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362 AUSTEALASIA.heat and cold, wind
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3G1AUSTRALASIA.from shoals, begins
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366 AUSTRALASIA.notwithstanding the
Page 446 and 447:
3(J8 AUSTRALASIA.islands ;at anotli
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870 AUSTRALASIA.regions. Neverthele
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872 AUSTRALASIA.The splendour and e
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37iAUSTEALASIA.least three-fourths
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876 AUSTRALASIA.resembled the Malay
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;378 AUSTEALASIA.Australian languag
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—380 AUSTRALASIA.The most charact
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B82AUSTRiVLASIA.towards the rising
Page 462 and 463:
—884 AUSTRALASIA.progress of Chri
Page 464 and 465:
—886 AUSTRALASIA.year to ye:ir th
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338 AUSTRAIASIA.respect even bffore
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SCOAUSTRALASIA.limited uuuiber of w
Page 470 and 471:
392 AUSTRALASIA.the colonief? with
Page 472 and 473:
391 AUSTRALASIA.was adequately repr
Page 474 and 475: —390 AUSTRALASIA.spaces from the
Page 476 and 477: ;898•AUSTRALASIA.were discovered
Page 478 and 479: —400 AUSTRALASIA.where is coiitre
Page 480 and 481: —402 AUSTRALASLV.to the prosperit
Page 482 and 483: 404 AUSTRALASIA.1859. But altliougt
Page 484 and 485: -100 AUSTRALASIA.2fari/boroi(gh occ
Page 486 and 487: ;408 AUSTRALASIA.development o£ th
Page 488 and 489: L13RASYOF THE
Page 490 and 491: SYDNEYA^C to IGfe*T. !atc3:f*LONDON
Page 492 and 493: LiSRARYOF THEiVERSITV of ILLINOIS.
Page 494 and 495: ;410 AUSTRALASIA.clearing at the ex
Page 496 and 497: 412 AUSTRALASIA.most densely people
Page 498: 411 AUSTRALASIA.Norfolk, over five
Page 501 and 502: VICTOEIA. 415place of little import
Page 504 and 505: LI3RAKVOF THEUNIVERSITV of ILLINOIS
Page 506: 418 AUSTRALASIA.precious metal. Sin
Page 509 and 510: TASMANIA. 419about a reaction, and
Page 512 and 513: LIBRARYOF THEJNIVERSITV of ILLINOIS
Page 514 and 515: 422•AUSTRALASIA.Pahiii, and which
Page 516 and 517: 424 AUSTRALASIA.brian pouinsula, wb
Page 518: —'42GAUSTEAI.ASIA.On the west sid
Page 521 and 522: NEW ZEALAND—SOUTH ISLAND. 427by t
Page 523: —NEW ZEALAND—SOUTH ISLAND. 429i
Page 527 and 528: NEW ZEALAND—NORTH ISLAND. 433is 1
Page 530 and 531: LIBRARYOF THE'INIVERSITV of ILLINOI
Page 532 and 533: 43GAUSTE.VLASIA.siijjpbire tints of
Page 534 and 535: 438 AUSTEALASIA.disappear as if by
Page 536 and 537: 440 AUSTRALASIA.and tailless, of wh
Page 538 and 539: 442 AUSTRAT.ASIA.warlike expedition
Page 540 and 541: 444 AUSTEALASIA.two tribes in 1884.
Page 542 and 543: 446 AUSTRALASIA.Nevertheless, tiiia
Page 544 and 545: U8AUSTllALASIA.Topography of New Zk
Page 546 and 547: 450 AUSTEALASIA.to navigation.Thank
Page 548: 452 AUSTRALASIA.very remarkable col
Page 551 and 552: TorOGRAPHT OF NEW ZEALAND. 453the e
Page 553 and 554: NEW ZEALAND.—ADJACENT ISLANDS. 45
Page 555: LISRAKVOF THEUNlVERSITVofllLlNOiS
Page 559 and 560: CIIArTER X.TIIK FIJI ISLANDS.1
Page 561 and 562: FIJI. 459from Vanua-Levu by the nar
Page 563 and 564: FIJI.IGleven with the gods, making
Page 565 and 566: FIJI.4G3raw. He also amused himself
Page 568 and 569: LIBRARYOF THEDIVERSITY of ILLINOIS,
Page 570 and 571: CHAPTER XLEQUATORIAL POLYNESIA.'OLY
Page 572 and 573: —4G8AUSTRALASIA.the last Polj'nes
Page 574 and 575:
470 AUSTEALASIA.Samoa, -wliich is r
Page 576 and 577:
—472 AUSTRALASIA.tropical vegetat
Page 579 and 580:
EQUATORIAL POLYXESIA. 473zone of pl
Page 581 and 582:
EQUATOEIAJ. POLTNESIx\.. 475pletel}
Page 583 and 584:
EQUATORIAL POLYNESIA. 477covering t
Page 585 and 586:
—EQUATORIAL POLYNESIA. 479supreme
Page 587 and 588:
, , 1EQUATOEIAL POLTXE-IA. 481tions
Page 589 and 590:
EQUATOELVI. POLYXESIA. 483changes o
Page 591 and 592:
—EQUATORIAL POLYNESIA. 485The who
Page 594 and 595:
LiSRARYOF THEJNlVERSlTYofttLlNOtS,i
Page 596 and 597:
—483 AUSTR.VLASIA.the gi-adual an
Page 598 and 599:
—400 AUSTRALASIA.for the highest
Page 600 and 601:
—402 AIISTRATiASIA.islets, whicli
Page 602 and 603:
494 AUSTRALASIA.in Honolulu, whore,
Page 604:
4'JGAUSTEAIjASIA.Anglicans, Metliod
Page 607 and 608:
HAWAH. 497a province of the great r
Page 609 and 610:
APPENDIX. 499Riouw and Lingga Archi
Page 611 and 612:
—ArrENDix. 501NoETHEEX Moluccas :
Page 613 and 614:
APPENDIX.Anibrym......-.Vate (Sandw
Page 615 and 616:
INDEX.Abang Volcano, 196Abong-Abons
Page 617 and 618:
INDEX. 507Deli Town, 96, 113Demak,
Page 619 and 620:
4INDEX. 509Malu Mountain, 124Mamauu
Page 621 and 622:
'INDEX. 511Salak Mountain, 151, 1S2
Page 626:
UNIVERSITY OF I1-UNOI3-URBANA
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