Australasia -- Description and travel; Australasia -- Discovery and exploration; Explorers -- Australasia
Borneo, Celebes, Buru, Jilolo, and the Spice Islands, Timor, Ceram,
the eastern Sunda Islands were, of course, with Java and Sumatra
on the west, New Guinea and the Bismarck Archipelago on the east,
and the Philippines on the north, _continental_ islands; that is to
say, fragments of the former prolongation of Asia towards Australia:
old lands, large or small portions of which have always risen above
the very shallow sea which now separates them from one another.
Yet MALAYSIA, like Polynesia, Melanesia, and Micronesia, is very
volcanic. Of all its islands Borneo is the least so at the present
day, in fact there is no active or recently active volcano in that
huge island; whereas the Philippines are occasionally racked with
earthquakes and have twelve active volcanoes. Java has a long range
of lofty craters--some hundred and twenty-five in all, of which at
least thirteen are active. The Lesser Sunda Islands, east of Java,
likewise contain many volcanoes: Lombok and Sumbawa are little more
than exceedingly large groups of craters, and when the Sumbawa
volcano (of which something like 6 cubic miles was blown away)
erupted in 1815, its red-hot lava and ashes killed forty thousand
of the inhabitants on its slopes. There are volcanoes in Celebes,
the Moluccas, Jilolo, and some of the islands off the west end of
New Guinea. Timor only shows traces of past volcanic activity. In
consequence of its being the most volcanic region in the world,
Malaysia is very subject to earthquakes; and these disturbances of
the earth's surface not only cause devastating tidal waves on the
seacoasts, but in some way affect the atmosphere, provoking fearful
cyclones of wind, followed by torrential rain. Similar disturbances
of the atmosphere, however, occur frequently before or after the
rainy season. Borneo is frightfully hot--perhaps hotter all the
year round than any other country--but it is less afflicted with
devastating winds. Nearly all Malaysia has a tremendous rainfall,
though one or two islands, such as Flores and parts of Timor, have
a rather drier climate, more suggestive of northern Australia. As
a rule, however, Malaysia, in consequence of its perpetual summer
under an equatorial sun, its rich alluvial soil--often of that
peculiar richness associated with volcanic materials--and its
plentiful rainfall, is clothed with a primeval forest which for
luxuriance can scarcely be matched in West Africa or Brazil. These
lands have been styled "the gardens of the sun"; "enormous forcing
houses crammed with vegetation"; "great zoological gardens, full of
rare and curious beasts". Here may be seen many species of palms:
the gloriously beautiful Cyrtostachys palm of Java, with vividly
red sheaths to the fronds and flower stalks, and bright yellow
inflorescence changing to scarlet fruit; the creeping, climbing
palms (the "rattan" or _Calamus_); stately Areca palms (which
produce the betel nut, and the smaller species the "cabbage", so
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