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LIBRARYOF THEJNIVERSITV of ILLINOIS,
NEW ZEALAND—SOUTH ISLAND. 427by the sedimentary matter washed down with the mountain torrents. Withoutcounting numerous sparkling ponds or tarns less than a square mile in extent,South Island contains about sixty basins, some of which cover an area of over 40square miles and fill cavities 300 feet and upwards deep. Nearly all these greatreservoirs are grouped in the southern part of the island and on the east slope ofthe mountains. Rising abniptlj' above the western seaboard, the New Zealand Alpshave too precipitous a slope on this side to allow the running waters to collect inlarge basins. But the opposite decKvity and the plains stretching thence to theeast coast present numerous depressions where the glaciers have been replaced bylakes, most of which have been formed in the intermediate zone between theuplands and the plains. A straight line drawn across the chief flooded basinsfrom north-east to south-west for a distance of about 200 miles would run parallelto the main Alpine chain, and would represent the direction of the axis of thesouthern island.The northern group of lakes east of the highest section of the Alps appears tobe merely the remains of a labyrinth of inland waters, which formerly occupiedthe vast llackenzie Plains, and which are now disposed in countless secondarycavities by moraines, heaps of erratic boulders, dams and sedimentary dejDosits.These basins—Te Kapo, Pukaki, Ohau—were formerly much deeper, and are nowrapidl}' silting up, just as those farther north have already been filled in whichwere at one time traversed by the river Walmakariri. The dav may be predictedwhen the glacial waters of the Waitaki, which now issue in a crystal stream fromthe flooded depressions, will roll down in a tiu'bid current to the plains. Althoughits course scarcely exceeds 120 miles in length, the Waitaki is none the less a greatriver, according to W. N. Blair five times more voluminous than the Thames,although this writer gives no data in support of his statement.*Farther south the Clutha, which receives the overflow of the central gi-oup oflakes, is a much larger watercourse, being compared by the same author with theNile. It is certainly the first river in New Zealand both for size and A'olume, itscatchment basin exceeding 8,000 square miles in extent. The Clutha has alsobeen more thoroughly explored than any other stream in South Island, thanks tothe rich gold-fields, which since the year 1862 have attracted thousands of minersto the region about its headwaters. "Wakatipu,' one of the lakes belonging to thissj'stem, is no less than 50 miles long, but only from 1 to 3 miles wide. It thuspresents the aspect of a winding river, without visible current, with a mean depthof no less than 1,200 feet, and in its profoundest chasms sinking to 1,400 feet.both sides the encircling hills jjlunge abruptly into these abysmal watci's.Te Anau, largest of all New Zealand lakes, lies beyond the Clutha basin at thehead of the Waiau, a short stream flowing to the south coast. The lake fills a longvalley and several tributary branches for a space of <strong>14</strong>0 square miles, and in itsdeepest part the soimding line has measured 940 feet. Te Anau is separated by anarrow isthmus from Manapuri (ilanipori), another lacustrine basin, which is alsosaid to be very deep, and which branches into numerous creeks and buys, winding* Scottish Geographical Magazine, Xovemlier, 1887.On
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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
Page 107 and 108:
FLORA OF I>rDONT:SIA. 71whole of ll
Page 109 and 110:
FAUNA OF IXDOXESIA. 73the other isl
Page 111 and 112:
FAUXA OF INDONESIA. 75At the same t
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IXHABITANTS OF INDONESIA. 77In the
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INHABITANTS OF INDONESIA. 79black,
Page 117 and 118:
SUMATRA. 81The Siimatran mountain s
Page 119 and 120:
SUMATRAN HIGHLAXDS. 83wealth of the
Page 121 and 122:
SUMATEAN HIGHLANDS. 85chasm visited
Page 123 and 124:
onKEAKATAU. 87Krakai'au.Till recent
Page 125 and 126:
KEAKATAU. 89ashes and pumice was es
Page 127 and 128:
SUMATRAN ElYERS. 91alluvial lands a
Page 129 and 130:
SUMATEAN ISLANDS. 93to the west the
Page 131 and 132:
IXHABITAXTS OF SUMATRA. 95camphor,
Page 133 and 134:
'.=INHABITANTS OF SUMATEA. 97dant h
Page 135 and 136:
IXUAEIT.VXTS OF SUMATRA. 99The lang
Page 137 and 138:
IXHABITANTS OP SUMATRA. 101On the d
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IN'HABITANTS OF SUMATRA. 103neighbo
Page 141 and 142:
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
Page 162 and 163:
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
Page 182 and 183:
142 AUSTRALASIA.The little port of
Page 184 and 185:
144 AUSTRALASIA.Labuan.At the time
Page 186 and 187:
146 AUSTRALASIA.annual surplus devo
Page 188 and 189:
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
Page 236 and 237:
LiotiARYOF THEUNIVERSITY of nUNOIS.
Page 238 and 239:
188 AUSTRALASIA.estuai-y accessible
Page 240 and 241:
190 AUSTRALASIA.affluent of the Sol
Page 242:
192 AUSTEALASIA.The ruins of the Hi
Page 245 and 246:
TOPOGHAPHY OF JA^'A. 193remains of
Page 247 and 248:
ADinNISTEATION OF JAVA. 195for the
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BALI. 197all rapacious beasts, exce
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BALI. 199Public instruction stands
Page 253 and 254:
LOMBOK. 201A table of all the provi
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LOMBOK.—SUMBAWA. 203Mataram, the
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SUMBAWA. 205these debris represente
Page 259 and 260:
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
Page 271 and 272:
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
Page 282 and 283:
LISRARVOF THEUNlVERSlTy of ILLINOIS
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230 AtrSTEAlASIA.reefs appearing ab
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232 AUSTRALASIA.Guinea. Those of Bu
Page 289 and 290:
—THE SOUTHERN MOLUCCAS. 238region
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iMPiMliBiiiiiiSliS
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—THE SOUTHEEN MOLUCCAS. 285with t
Page 295 and 296:
THE NORTHERN MOLUCCAS. 237Tlie Xort
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THE NORTHEEX MOLUCCAS. 289Nearly al
Page 299 and 300:
THE NOETHEllX MOLUCCAS. 241The capi
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;CHAPTEE IV.THE PHILIPPINES.HE term
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THE PIIILIPriXKS. 245ridge is also
Page 306 and 307:
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
Page 315 and 316:
lyilABITANTS OF THE PHILIPPIXES. 25
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some places, and especially Luzon,
Page 319 and 320:
—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.
Page 328 and 329:
;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
Page 338 and 339:
—CHAPTER V.MICKONESIA.I.The Maria
Page 340:
;270 AUSTRALASIA.Exposed during the
Page 343 and 344:
—THE MAEIANAS. 277although baptis
Page 345 and 346:
THE PELEW ISLAISTDS. 279together, a
Page 347 and 348:
THE CAEOLIXES. 281Eocha readied the
Page 349 and 350:
THE CAEOLIXES. 283also affords shel
Page 351 and 352:
THE CAEOLES'ES 285purchase hatcliet
Page 353 and 354:
THE CAEOLINES. 287tions associated
Page 355 and 356:
—EASTERN MiCEONESIA. 289times eve
Page 357 and 358:
EASTERN MICEOXESIA. 291by breezes f
Page 359 and 360:
CHAPTER VI.NEW GUINEA AND ADJACENT
Page 361 and 362:
NKW GUINEA. 295the great island ass
Page 363 and 364:
PHYSICAL FEATUEES OF NEW GUINEA. 29
Page 365 and 366:
—rrTTSIC.\L FEATUEES OP NEW GITIN
Page 367 and 368:
—CLIMATE OF NEW GUINEA. 801windin
Page 369 and 370:
FAUNA OF NEW GUINEA. 303these are r
Page 372 and 373:
LIBRARYOF THEIKIVERSITYoflLUNOlS.i
Page 374 and 375:
806 AUSTRALASIA.out ever founaering
Page 376 and 377:
H08AUSTRALASIA.frequented market in
Page 378 and 379:
310 AUSTRALASIA.Along the whole of
Page 380 and 381:
812 AUSTRALASIA.time of the discove
Page 382 and 383:
314 AUSTEALASIA."palace," barracks,
Page 384 and 385:
misAUSTRALASIA." Monsieur," as they
Page 386 and 387:
—CHAPTER VII.MELANESIA.LL the isl
Page 388 and 389:
3iOAUSTRALASIA.Hermit and Admiralty
Page 390 and 391:
822 AUSTEALASIA.central part of the
Page 392:
324 AUSTEALASIAPolynesian are inter
Page 395 and 396:
NOETH MELA^ÊSIA. 325Maklaj' to the
Page 397 and 398:
NORTH MELANESIA. 327As a rule the s
Page 399 and 400:
NOKTH MELANESIA. 329west, and which
Page 401 and 402:
—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
Page 409 and 410:
—FRENCH MELANESIA. 339In New Cale
Page 411 and 412:
FRENCH MELANESIA. 341brooks apiêar
Page 413 and 414:
—FEEXC'II MELANEf^FA.343Imiaiutan
Page 415 and 416:
FRENCH MELANESIA.3i580 many clans,
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LIBRARYOF THEUNIVERSITY of ILLlNGi.
Page 420 and 421:
—348 AUSTRALASIA.New Ciik'clonia
Page 422 and 423:
850 AUSTRALASIA.the surrounding far
Page 424 and 425:
CHAPTER VIII.AUSTRALIA AND TASMANIA
Page 426 and 427:
AUSTRALIATASMAr
Page 429 and 430:
AUSTRALIA. .353alluvial plains, dee
Page 431 and 432:
—EXPLORATION OF AUSTEALIA. 355isl
Page 433 and 434:
—EXPLORATIOX OF AUSTE.ILIA. 357Th
Page 435 and 436:
THE AUSTRALIAN ALPS. 859which lie w
Page 438 and 439:
LIBRARYOF THEINIVERSITV of ILLINOIS
Page 440 and 441:
362 AUSTEALASIA.heat and cold, wind
Page 442 and 443:
3G1AUSTRALASIA.from shoals, begins
Page 444 and 445:
366 AUSTRALASIA.notwithstanding the
Page 446 and 447:
3(J8 AUSTRALASIA.islands ;at anotli
Page 448 and 449:
870 AUSTRALASIA.regions. Neverthele
Page 450 and 451:
872 AUSTRALASIA.The splendour and e
Page 452 and 453:
37iAUSTEALASIA.least three-fourths
Page 454 and 455:
876 AUSTRALASIA.resembled the Malay
Page 456 and 457:
;378 AUSTEALASIA.Australian languag
Page 458 and 459:
—380 AUSTRALASIA.The most charact
Page 460 and 461:
B82AUSTRiVLASIA.towards the rising
Page 462 and 463:
—884 AUSTRALASIA.progress of Chri
Page 464 and 465:
—886 AUSTRALASIA.year to ye:ir th
Page 466 and 467:
338 AUSTRAIASIA.respect even bffore
Page 468 and 469: 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 523 and 524: —NEW ZEALAND—SOUTH ISLAND. 429i
Page 525 and 526: NEW ZEALAND—NORTH ISLAND. 431K;ii
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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