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NEW GUINEA

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Originally appearing in Volume V19, Page 489 of the 1911 Encyclopedia Britannica.
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NEW See also:

GUINEA , the largest See also:island (excluding See also:Greenland) in the See also:world, lying between the See also:equator and 12° S. and 130° 5o' and 1510 30' E., separated from See also:Australia by Torres ' Strait and having the Arafura See also:Sea on the See also:south-See also:west. It is divided politic-ally between See also:Britain (south-See also:east), See also:Germany (See also:north-east) and See also:Holland (west), the Dutch territory occupying about 48.6% of the whole See also:area, the See also:German 28.3% and the See also:British Territory of Papua 23.I%,. The See also:total area is estimated to be 312,329 sq. m. New Guinea was probably in See also:Miocene times, if not later, See also:united to the See also:northern See also:part of See also:Queensland. The deeply indented See also:shore of the Gulf of Papua forms the boundary of the subsided area between the two countries, and from it the See also:land stretches out for 200 to 300 M. north and west on both sides of the See also:Fly See also:river in vast plains, little elevated above sea-level. From Cape Bum westwards precipitous See also:limestone cliffs, several See also:hundred feet high, See also:face the sea and rise into See also:forest-clad mountains behind. The northern extremity of New Guinea is all but severed from the mainland by the deep MacCluer Inlet, See also:running eastwards towards Geelvink See also:Bay which deeply indents the northern See also:coast. South-wards from Geelvink Bay the north-east coast is more See also:regular than the south-western. Off its coast-See also:line, on the parallel of 6° S., lies the vast See also:Bismarck See also:Archipelago, of which New See also:Pomerania (Neu Pommern) is the most important member; and, on the parallel of io°, the d'See also:Entrecasteaux Islands, with the See also:Marshall See also:Bennett See also:group to their north-east; while stretching out from the south-east promontory of the mainland is the Louisiade Archipelago. The See also:Great Barrier See also:Reef of Australia can be traced more or less continuously See also:round the Gulf of Papua and along the south-east coast to the extremity of the Louisiades. In a See also:general way it may be said that on the west coast of New Guinea, from Cape See also:Burn to the Louisiades, the sea is shallow, while on its steeper eastern See also:side the See also:water See also:close in-shore is often too deep See also:Pro/acts for See also:union with See also:Canada. ~iP ~A'3 ,A p• •,, B =36 C ,ao D ,aa E See also:Las° F isa° G ~f Pity L R mntw .

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English See also:Miles ,5o You 90 ,m v'' A,33 B [36' C 'w0 D See also:Longitude East 144° or See also:Greenwich E t ls° F 1ss° G See also:amen, See also:Walker sc for safe anchorage. The islands on the See also:southern margin of the Louisiade Archipelago are raised See also:coral reefs, but the See also:majority are mountainous, rarely, however, exceeding 3000 ft.; all of them are richly forested, but of little agricultural value. The volcanic d'Entrecasteaux Islands are mostly larger, more elevated (the highest being 8000 ft.), and stand in deeper water than the Louisiade group. To the east of Kiriwina (Trobriand) lies a small group of uniquely formed islets, each of which is completely surrounded by a steep forest-clad marginal rampart of coral 300 to 400 ft. high, concealing a depressed inhabited central See also:plateau. Starting in the southern extremity of New Guinea from an abrupt face some 3000 ft. high, and traversing its centre nearly parallel to both coasts, run high ranges of mountains, which, if not continuous, See also:merge into each other in the same general direction. The See also:Owen See also:Stanley range-its highest See also:summit, named by See also:Huxley in 185o See also:Mount Owen Stanley, 13,120 ft.—the See also:Albert See also:Victor Mountains, the See also:Sir See also:Arthur See also:Gordon range, and the Bismarck Mountains See also:form a backbone united probably with the Sneeuw (Snowy) Mts., where perpetual See also:snow was found by Dr. Lorentz in 1909 at 14,635 ft., and the height of Mt. See also:Wilhelmina was fixed at 15,580 ft. This height may be exceeded by Mt. Carstensz. Other ranges, mostly of See also:lower See also:altitude, run parallel mainly to the east and west coasts.

The most important and best-known See also:

rivers are the Amberno, in the north, discharging by a wide See also:delta at Point d'Urville; the Kaiserin See also:Augusta, which, rising in the See also:Charles See also:Louis range, and entering the Pacific near Cape della Torre, is navigable by ocean steamers for 18o m.; the Ottilien, a river of great length, which discharges into the sea a See also:short distance south of the last named; and the Mambare, navigable by See also:steam:See also:launch for 5o M. which drains the eastern aspect of Wasigororo Mountains and enters the sea near the Anglo-German boundary. Below 8° S. the narrowness of the See also:country precludes the existence of any very important rivers on either coast. The Purari, however, whose delta is 20 M. See also:long by 20 broad, is navigable for 120 M. by steam-launch, while the Fly has been traversed by the same means for 500 and by a See also:whale-See also:boat for over 600 m. The latter drains an enormous See also:tract of country, which is so little elevated above the sea-level that it can never be of any agricultural or commercial value. 'Vest of 141° E. the See also:geographical features of the coast, except in the region of MacCluer Inlet and Geelvink Bay, are very little known, and those of the interior even less. See also:Geology.—The geology of British New Guinea is best known from the See also:report of A. Gibb See also:Maitland (See also:Ann. See also:Rep., British New Guinea, 1891-1892; See also:Pall. Papers, Queansland, 1893, C.A. 1. 53-85, with 3 maps and 3 plates; bibliography, p. 85), which shows that the See also:axis of the territory is a high range, composed of slates and See also:schists of undetermined See also:age, with intrusive plutonic rocks.

In the See also:

district around See also:Port See also:Glasgow, on the south coast of the eastern See also:peninsula, are the Boioro limestones, also of unknown age; they are See also:lead-coloured, brecciated limestones with interbedded dolerites. Some Cretaceous or Upper See also:Jurassic rocks occur in the See also:basin of the Fly river. The Port Moresby beds are See also:Cainozoic. They are highly inclined, and occupy a large range of country along the south coast, and include the See also:Macgillivray Range, to the north-east of Beagle Bay. They are marine and probably Miocene; and range up to the height of 800 ft. above the sea, approximately the same limit as in See also:Victoria. The Kevori grits, and the raised coral reefs are upper Cainozoic, and perhaps See also:Pleistocene; but the reefs occur inland up to a height of 2000 ft. and their range back in See also:time has not been fixed. The volcanic See also:series include the See also:rhyolite of Nell Island, some See also:obsidian, and the sheets of basalts which form the Cloudy Mountains, Mount Dayman and Mount See also:Trafalgar (an active See also:volcano), and also See also:cover wide areas to the south and west of the Owen Stanley Range. Most of western British New Guinea consists of See also:recent superficial deposits, in the basin of the Fly river. The Louisiade and the d'Entrecasteaux Islands consist of the same slates and schists as form the See also:main axis of the eastern peninsula, and they are auriferous. The geology of the See also:rest of New Guinea is imperfectly known. It appears to consist in the main of a continuation of an axis of old schists and slates, with See also:granite intrusions, and flanked by coastal plains with Cretaceous or Jurassic, and Miocene beds, with Pleistocene sands and reefs and volcanic rocks. In the north-west See also:coal deposits occur.

See also:

Fergusson Island clearly shows remains of See also:extinct craters, and possesses numerous hot springs, saline lakes and solfataras depositing See also:sulphur and See also:alum. In lblurua (Woodlark I.) are quarries of the banded See also:quartzite from which the best See also:stone adzes found throughout south-east New Guinea are made. In Rossel Island (Roua or Arova) occur crystalline schistose and volcanic rocks, and in Misima (St Aignan) limestones and lavas in addition. Nearly all the rivers in New Guinea yield " See also:colours t' of See also:gold, but only in the Louisiade Archipelago has enough been discovered to constitute the district a See also:goldfield. No auriferous reefs have been found. See also:Black magnetic See also:iron See also:sand covers the shore in Milne Bay. Coal has been observed in the Purari sandstones. In the Gira river the valuable alloy osmiridium has been discovered. Earthquakes are rare on the mainland, but not infrequent in Bismarck and d'Entrecasteaux archipelagos. See also:Climate.—Since the mountains as a See also:rule See also:traverse the island parallel to its coasts, the eastern shores have far less See also:rain than the western. The amount which falls, chiefly at See also:night, varies from 30 in. on some parts of the coast to 130 at others, and to a far greater but unknown amount in the mountains. Throughout the dry or cool See also:season the See also:wind blows steadily and almost uninterruptedly (except for an See also:hour or so forenoon and afternoon) from the south-east.

The temperature has an extreme range of-from 72° to 95° F., with a mean of about 8o°. At an See also:

elevation of 3000 ft. the climate is pleasantly cool; at 13,000 ft. See also:ice forms in the night, but disappears with the See also:heat of the See also:sun. No snow is known certainly to fall, though it is alleged to have been seen from the sea lying on the summits of the Charles Louis range. See also:Fever is very prevalent on the coasts, and even in the interior at 2000 ft. above the sea. Though generally of a mild See also:character, it is persistently recurrent, and slowly saps and wears out the constitution; too often it is virulent and rapidly fatal. See also:Fauna.—New Guinea shares in the poverty in mammals of the Australian sub-region. Monotremes (2 See also:species) and marsupials (4 families and 44 species) predominate, but are not abundant. Among the latter two genera, Distaechurus and Dorcopsis, are See also:peculiar. A See also:pig (Sus papuensis), a See also:dingo, several species of mice (of which Chiruromys is a peculiar genus), a few squirrels, and a considerable number of See also:Chiroptera (bats) inhabit the country. The island is specially remarkable for the number and beauty of its birds. The most recent lists See also:record over Soo species as found in the Papuan area, and of these between 50 and 6o genera are peculiar to it. The birds of See also:paradise, which are confined to the sub-region, give See also:special celebrity to its fauna.

Between 70 and 8o species have already been described, many of them the most gorgeously adorned, and others, such as the Pteridophora albertisi, the most wonderful of feathered creatures. They are absent from the Louisiades, but species occur in the d'Entrecasteaux Islands which have not been seen on the mainland opposite. The See also:

zoology of the Bismarck Archipelago is little known. The species of birds so far described from it number 178 (referable to 38 families), of which 74 are peculiar to it, though closely allied to Papuan forms. It contains, however, no Paradiseidae. The See also:Amphibia, to which the sea is a barrier, are almost exclusively of Australian See also:affinities. Turtles and tortoises are plentiful on the coast. Ceratochelys insculpla of the Fly river, a chelonian peculiar to New Guinea, is remarkable in having its nearest affinities (as have the Papuan tortoises) with South See also:American species. Of the lizards, 3 of the 6 species of Varanidae, 16 of the 30 Scincidae, 8 Geckonidae, and 8 out of the it Agamidae are peculiar. Salamanders, toads and frogs are numerous, and crocodiles abound. Only 4 genera and 5 species of See also:snakes are peculiar to New Guinea, many of them poisonous. Butterflies, moths and bees are very abundant, the former being remarkable for their See also:size and splendid coloration; but these See also:groups have not been investigated exhaustively enough to afford a correct See also:idea of their number or their true affinities.

Although the See also:

list of See also:Coleoptera already known is long, it represents only a fraction of the species remaining to be discovered. The land molluscs show relationship with the See also:Indian and the Malayan sub-regions; but many forms have here their centre, and have spread hence into Australia and the Pacific islands. See also:Flora.—Most of the foreshores of New Guinea are See also:eucalyptus-dotted grass lands; in the interior dense forests prevail to a height of many thousand feet. Vast tracts of the country have been, how-ever, deforested by See also:fire, and these are covered by the tall ineradicable grass, Imperata arundinacea. So far the highest altitudes yet botanically investigated are those of the Owen Stanley range and the mountains in Kaiser Wilhelms Land, but of the flora of the highest range of all—the Charles Louis mountains—nothing is known. The vascular See also:plants already described number about 1500 species. In the See also:low and sub-mountainous lands the flora is a mixture of Malayan, Australian and Polynesian forms. There are, according to See also:Muller, twice as many palms known from New Guinea as from Australia. The alpine flora, beginning at 6000 ft., is specially characterized by its rhododendrons, pines (See also:Araucaria and Libocedrus), and palms, by numerous superb species of Agapetes (See also:Ericaceae), and on the summits by an extraordinary association of species characteristically See also:European (Rubus, See also:Ranunculus, Leontodon, Aspidium), Himalayan, New Zealandian (See also:Veronica), See also:Antarctic and South American (Drymus, Libocedrus). See also:Good pasture See also:grasses are numerous, but pasture lands are limited. The usual tropical See also:food-plants are cultivated. See also:Tobacco has been found growing in the interior, and may be indigenous, as is in some districts the See also:Kava See also:pepper (See also:Piper methysticum).

At Dorey a See also:

cotton plant (G. vitifolium) grows See also:wild, and is also cultivated. Natives.—So large an area of New Guinea remains unexplored that it is impossible, except approximately, to See also:state the number of its inhabitants, but probably 600,000 is under rather than over the See also:mark. The See also:people are broken up into numerous isolated tribes differing greatly in feature, See also:colour and See also:language. Ethnically they belong as a whole to the Melanesian See also:division of the Indo-Pacific races. The predominant tribe are the See also:Papuans (q.v.), who are found here in their greatest racial purity and occupy practically the whole island except its eastern extremity. The New Guinea native is usually of a See also:negroid type with See also:fine physique, but in the Arfak mountains in the north-west, and at points on the west and north coasts and adjacent islands, the very degraded and stunted Karons are found, with hardly the elements of social organization (possibly the aboriginal See also:race unmixed with See also:foreign elements), and resembling the Aetas or See also:Negritos of the Philippines, and other kindred tribes in the See also:Malay Archipelago. On the See also:banks of the Fly river d'Albertis observed at least two widely differing types, those on its upper course bearing some resemblance to the tribes-of theeastern coast. Here, wedged in among the ruder Papuans, who reappear at the extremity of the peninsula, a very different-looking people are found, whom competent observers, arguing from See also:appearance, language and customs, assert to be a See also:branch of the See also:fair Polynesian race. But they are obviously of mixed See also:blood. On the west coasts there is a semi-See also:civilization, due to intercourse with See also:Malays and See also:Bugis, who have settled at various points, and carry on the, See also:trade with the neighbouring islands, in some of which, while the coast See also:population is Malay or mixed, that of the interior is identical with the people of the mainland of New Guinea. On the west coasts, See also:Mahommedan teaching has also some civilizing effect. Many of, the tribes at the west end of New Guinea are, at all events in See also:war time, See also:head-hunters, and in the mountains cannibals.

See also:

Cannibalism, in fact, is practised here and there throughout New Guinea. The. frequent hostility and mistrust of strangers are partly due to slave-, See also:hunting raids and See also:ill-treatment by traders, but the different tribes vary much in character. Thus in the mountains of the north-west the Karons live by See also:plunder, or by disposal of slaves or See also:bird skins: while their neighbours the Kebars are a peaceful agricultural people.; The See also:mountain tribes are usually despised by their coast neighbours, but in the south of west New Guinea the coast people live in per-' petual terror of their inland neighbours. At See also:Humboldt Bay the people are ready to trade, as are the tribes. at See also:Astrolabe Bay; here the See also:Russian Miklucho Maclay lived for some time, and was favourably impressed by the natives. Still farther east, the plateaus of the Finisterre ranges are highly cultivated and artificially irrigated by a comparatively fair people. Many tribes in the south-west seem to be migratory. At Princess Marianne Straits tribes much wilder than those farther west, naked:. and painted, swarm like monkeys in the trees, the stems of which are? submerged at high See also:tide. But the Torres Straits islanders are employed by Europeans in the See also:pearl See also:shell See also:fishery, and are good labourers;' and in some of the Kei and Aru Islands the Papuan inhabitants form orderly See also:Christian communities. The people of the south-east peninsula are generally far from ferocious. Englishmen, wandering_ inland and losing their way, have been found and brought back by them. Their See also:manners are more courteous, their See also:women better treated, than is usual with Papuans, but they show perhaps less ingenuity and See also:artistic See also:taste. Their See also:children, in the See also:mission See also:schools, show much intelligence.

Exploration and See also:

Annexation.—Though probably sighted by See also:Antonio d'Abreu, 1511, New Guinea was apparently first visited either by the Portuguese See also:Don Jorge de Meneses, driven on his way from See also:Goa to See also:Ternate in 1526 to take shelter at " See also:Isla Versija " (which has been identified with Warsia, a See also:place on the N.W. coast, but may possibly be the island of Waigeu), or by the Spaniard Alvaro de See also:Saavedra two years later. The name of " New Guinea " was probably given by Ortiz de Retez, or Roda, who in 1546 first laid down several points along the north coast. In the same and the two following centuries, though the coasts were visited by many illustrious navigators, as Willem Schouten and See also:Jacob Lemaire, See also:Abel See also:Tasman, See also:William See also:Dampier, L. V. de Torres, L. A. de See also:Bougainville and See also:James See also:Cook, little additional knowledge was gained. This' was due first to the difficulties of the See also:navigation, next to the exclusiveness of the Dutch, who, holding the Spice Islands, prevented all See also:access to places east of them, and lastly to the stream of enterprise being latterly diverted to the more temperate regions farther south. The Dutch barrier was broken down by the arrival of Dampier and other " interlopers " from the east, and of emissaries from the (English) East See also:India See also:Company in See also:search of spice-bearing lands. The voyage of See also:Thomas See also:Forrest (1774) in the " See also:Tartar See also:galley " of ro tons, and his See also:account of New Guinea (Voyage to New Guinea and the See also:Moluccas, See also:London, 178o), are still full of See also:interest. New Guinea was actually annexed in 1793 by two commanders in the East India Company's service, and the island of Manasvari in Geelvink Bay was held for some months by their troops. After the See also:peace of 1815 Dutch See also:surveying expeditions to the west coasts became numerous, and in later times scientific explorers penetrated many of the unknown parts of Dutch New Guinea, such as A. R. See also:Wallace (1856-1863), Odoardo Beccari (1871, 1875 and 1876), and Maria d'Albertis (1871-1878).

Important expeditions were those of P. See also:

van der Crab, J. E. T.eysmann, J. G. Coorengel, A. J. Langeveldt van Hemert and P. Swaan, undertaken for the -See also:Netherlands Indian See also:government 1871-1872, 1875-1876 (reports published at The See also:Hague in 1879); and of C. B. H. von Rosenberg in the Geelvink Bay districts in 1869-187o (report published at The Hague in 1875). Subsequently to the visits of J. A. d'Entrecasteaux (1793) and See also:Dumont d'Urville (1827-1840), the eastern coasts were surveyed by Captains F.P.

See also:

Blackwood (1835), Owen Stanley (1848), Charles B. See also:Yule (1864), and other British See also:officers, including J. Moresby (1874). Among other explorers in this See also:period the following may be mentioned: See also:Nicholas von Miklucho Maclay in 187o, 1877 and 1879-1881, in the Astrolabe Bay district, &c.; the missionary, Rev. S. Macfarlane (1875, Fly river, &c.); about 1876-188o the north-east coasts and adjacent islands were explored by the Rev. G. See also:Brown and by Wilfred See also:Powell, and in 1882 Dr See also:Otto Finsch, whose name is well known in connexion with scientific See also:work in New Guinea, made valuable explorations in the neighbourhood of Port Moresby and the Loluki. river. The surveys and reports of See also:Captain Moresby in 1874 brought See also:home to Queensland (and Australia generally) the dangers possible to her See also:commerce were the coasts opposite to Torres Strait and the entrance to the splendid waterway inside the Barrier Reef to fall into the See also:possession of a foreign See also:power. By authority, therefore, of Queensland, the mainland of New Guinea, opposite her shores east of the 141st See also:meridian, was annexed to that See also:colony in 1883. But this See also:action was disallowed by the British government as Yule's and Moresby's had been. Finally,. however, in 1884 a British See also:protectorate was authoritatively proclaimed by See also:Commodore See also:Erskine over the region " lying between the 141st meridian eastward as far as East Cape, with the adjacent islands as far as Kosman Island." German New Guinea was annexed on the 16th of See also:November 1884, when the German See also:flag was raised in See also:Friedrich Wilhelmshafen and a trading company was established on the north-east coast, and in 1885 the two countries agreed to See also:fix their boundaries through the then neutral areas of the country.

The result of this was the assignation to Great Britain of the portion now known as the Territory of Papua (British New Guinea), lying between the extreme limits of 5° and 12° S. and 141° and 1550 E. To Germany were assigned all the territory and islands to the north of the British boundary under the name of Kaiser Wilhelms Land, while all to the west of the 141st meridian remained under its old flag as Dutch New Guinea. Since this period explorers and investigators have been almost constantly at work. There may be mentioned the work of the Rev. J. See also:

Chalmers on the coast of the Gulf of Papua (1893), and of officers of the German New Guinea Company in the See also:ship " Ysabel " on the coasts and among the islands of the German territory; the expedition which crossed the south-eastern peninsula from Huon Gulf of which both the leaders, O. Ehlers and M. Piering, lost their lives (1895), the important German expedition under C. Lauterbach (1.896), and the various explorations carried out by or at the instigation of Sir William See also:MacGregor, including a See also:crossing of the island from the mouth of the Mambare river to that of the Vanapa, and a second crossing in the See also:reverse direction (1897). Ethnographical researches have been prosecuted by Messrs C. G. Seligmann and W.

Mersh Strong, and others. The reports of travellers and of various missionary See also:

societies have thrown a great See also:deal of See also:light on the natural See also:history of the island, on its resources, and the islanders.

End of Article: NEW GUINEA

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