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236 AUSTEALASIA.abj'sses of over a thousand fathoms ; on the north and north-west occur troughs oftwo thousand fathoms ; southwards, a chasm of fifteen hundred fathoms yawnsbetween Obi and the Southern Moluccas ;lastly, towards the east, depths of fivehundred fathoms, with a sill of over two hundred and fifty fathoms, mark the partingline between the insular world and the islands depending on Papuasia. TheNorthern Moluccas are mainly disposed longitudinally north and south, whereasthe southern group runs east and west. The total area exceeds 6,000 square miles ;but with the exception of the so-called "Little Moluccas" (Ternate, Tidor, Makjan,Motir, Kayoa) none of the islands are thickly peoijled, whileno permanent residents at all.some even haveThe two islands of Tifuri and Mayu, which dependpolitically on Ternate, may be included in this group, although rising in deepwaters to the east of Minahassa.The term Molucos was originally restricted by the Portuguese to tJie " LittleMoluccas " of modern geographers, but has gradually been extended to all theeastern islands producing spices.Igneous energy is far more active in the northern than in the southern group,and a whole range of active craters skirts the western edge of the archipelago.In the northern section of Batjan (Batchian) occur hot springs, and a gej'ser which,like those of Iceland, contains much silica. Farther north, beyond the basaltrocks of Kayoa (Kajoa) rises the Makjan volcano, which was partly blown awayduring the eruption of 1616. Motir also (1,020 feet) forms a burning mountain,which was still active down to the close of the last century. The southern portionof Tidor, a little farther north, consists of a perfectly regular cone, thehighest in the Moluccas (5,720 feet), which emits vapours from time to time. Itsneighbour, Ternate, somewhat lower and of less symmetrical form, is one of themost restless volcanoes in the whole of Indonesia ; from the Dutch occupation atthe beginning of the seventeenth century down to1862 no less than eighty-foureruptions were recorded ; the mountain is fissured in all directions, and vapours areconstantly emitted from the seven craters opened on its flanks. Earthquakes arealso frequent, and the town lying at its base has scarcely recovered from onedisaster when it is overtaken by another.Farther north, the volcanic axis of the Little Moluccas strikes the projectingcoast of Halmahera, and here also rise three eruptive cones visible from Ternate.In the same direction follow other centres of igneous activity, such as the GunongTarakan (Tafelberg), and Tolo, facing the island of Morotai (Mortai), whose scorioeforming barriers across the marine inlets have converted them into completeland-locked lakes.Halmahera, or the " Great Land," presents in its outlines a curious resemblanceto Celebes, consisting, like that island, of four 'mountainous peninsulas rooted ina central nucleus, and all disposed in similar directions. The trachytic island ofMorotai, with the adjacent clusters, which appear to have beenformerly attachedto the northern peninsula, also correspond to the Minahassa region of NorthCelebes, while the southern and south-eastern peninsulas are similarly prolongedby the islands of Damar and Gebe.
THE NORTHERN MOLUCCAS. 237Tlie Xorthern Moluccas, where tlic iiolitical ascendency is centred in tlie twovolcanic islets of Tidor and Ternatc, are distinguished, even more than the southerngroup, by their iêculiarly specialised local forms. Thus Morotai possesses characteristicbirds unknown in Ilalmahera, from which it is separated only by an islandsluddcdstrait twenty-four miles wide. The fauna, both of Morotai in the extremenorth and of Damar in the extreme south, is much more allied to that of the remotePapuasia than the JMoluccas. Specially remarkable is the fauna of Batjan, inFig. 101.—Ejipihes of Teen'ate issn Tidoe.Scale 1 : 20,0:0,000.^'taslj oFGreenwtcb
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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
Page 245 and 246: TOPOGHAPHY OF JA^'A. 193remains of
Page 247 and 248: ADinNISTEATION OF JAVA. 195for the
Page 249 and 250: BALI. 197all rapacious beasts, exce
Page 251 and 252: BALI. 199Public instruction stands
Page 253 and 254: LOMBOK. 201A table of all the provi
Page 255 and 256: LOMBOK.—SUMBAWA. 203Mataram, the
Page 257 and 258: SUMBAWA. 205these debris represente
Page 259 and 260: FLOEES. 207tain is at present quies
Page 261 and 262: SUMBA. 209entirely of limestone cli
Page 263 and 264: TIMOR. 211fourteentli century, and
Page 265 and 266: TnroE. 213vegetable zones of the Su
Page 267 and 268: TIMOR. 215fall asleep, and are not
Page 269 and 270: —TENIin?EE. 217On the other hand
Page 271 and 272: CELEBES.»219praus, which are expor
Page 273 and 274: [ 1—iiCELEBES. 221wLicb, however,
Page 275 and 276: CELEBES.223reaclnug the sea.Thus th
Page 277 and 278: —CELEBES. 226cultured coastlauder
Page 279 and 280: CELEBES. 227Topography ofCelebes.Th
Page 282 and 283: LISRARVOF THEUNlVERSlTy of ILLINOIS
Page 284 and 285: 230 AtrSTEAlASIA.reefs appearing ab
Page 286: 232 AUSTRALASIA.Guinea. Those of Bu
Page 289 and 290: —THE SOUTHERN MOLUCCAS. 238region
Page 291 and 292: iMPiMliBiiiiiiSliS
Page 293: —THE SOUTHEEN MOLUCCAS. 285with t
Page 297 and 298: THE NORTHEEX MOLUCCAS. 289Nearly al
Page 299 and 300: THE NOETHEllX MOLUCCAS. 241The capi
Page 301 and 302: ;CHAPTEE IV.THE PHILIPPINES.HE term
Page 303 and 304: THE PIIILIPriXKS. 245ridge is also
Page 306 and 307: LIBRARYOF THEUNIVERSITY of ILUNOIS1
Page 308 and 309: 248 AUSTRALASIA.whose slopes occupy
Page 310 and 311: 250 AUSTBAI.ASIA.to its modified en
Page 312: 252 AUSTRALASIA.60 miles from its m
Page 315 and 316: lyilABITANTS OF THE PHILIPPIXES. 25
Page 317 and 318: some places, and especially Luzon,
Page 319 and 320: —IXHABITAXTS OF THE PHILIPPINES.
Page 321 and 322: INHABITANTS OP THE rillLlITINES. 25
Page 323 and 324: IXITAF.ITAXTS OF THE PHILIPPIXES.2f
Page 326 and 327: LiBRARYOF THEUNIVERSITYefliLlNOIS.
Page 328 and 329: ;264 AUSTRATiASIA.occupies ono of t
Page 330 and 331: 260 AITSTEALASIA.two miles from eac
Page 332 and 333: '268 AUSTRALASIA.populous member of
Page 334 and 335: 270 AUSTRALASIA.Administratioxof th
Page 336 and 337: —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
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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
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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
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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
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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
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—884 AUSTRALASIA.progress of Chri
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—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
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392 AUSTRALASIA.the colonief? with
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391 AUSTRALASIA.was adequately repr
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—390 AUSTRALASIA.spaces from the
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;898•AUSTRALASIA.were discovered
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—400 AUSTRALASIA.where is coiitre
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—402 AUSTRALASLV.to the prosperit
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404 AUSTRALASIA.1859. But altliougt
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-100 AUSTRALASIA.2fari/boroi(gh occ
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;408 AUSTRALASIA.development o£ th
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L13RASYOF THE
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SYDNEYA^C to IGfe*T. !atc3:f*LONDON
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LiSRARYOF THEiVERSITV of ILLINOIS.
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;410 AUSTRALASIA.clearing at the ex
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412 AUSTRALASIA.most densely people
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411 AUSTRALASIA.Norfolk, over five
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VICTOEIA. 415place of little import
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LI3RAKVOF THEUNIVERSITV of ILLINOIS
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418 AUSTRALASIA.precious metal. Sin
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TASMANIA. 419about a reaction, and
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LIBRARYOF THEJNIVERSITV of ILLINOIS
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422•AUSTRALASIA.Pahiii, and which
Page 516 and 517:
424 AUSTRALASIA.brian pouinsula, wb
Page 518:
—'42GAUSTEAI.ASIA.On the west sid
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NEW ZEALAND—SOUTH ISLAND. 427by t
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—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
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LIBRARYOF THE'INIVERSITV of ILLINOI
Page 532 and 533:
43GAUSTE.VLASIA.siijjpbire tints of
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438 AUSTEALASIA.disappear as if by
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440 AUSTRALASIA.and tailless, of wh
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442 AUSTRAT.ASIA.warlike expedition
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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
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FIJI.4G3raw. He also amused himself
Page 568 and 569:
LIBRARYOF THEDIVERSITY of ILLINOIS,
Page 570 and 571:
CHAPTER XLEQUATORIAL POLYNESIA.'OLY
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—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
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—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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