Borneo, next in size to New Guinea, is a noble island, divided into two
nearly equal parts by the equator, and traversed through its whole
length by magnificent chains of mountains, which end in three branches
at the Java Sea. Beautiful rivers flow from them to the plains, and
several of these spring from a spacious lake on the table-land in the
interior, among the peaks of Keni-Balu, the highest point of the island.
Diamonds, gold, and antimony are among its minerals; gums, gutta percha,
precious woods, and all kinds of spices and tropical fruits are among
its vegetable productions.
Situate in the centre of a vast archipelago, and in the direct line of
an extensive and valuable commerce, it will in the course of time become
the seat of a great nation, whose civilization and prosperity will hand
down to posterity the name of the enterprising, philanthropic Sir James
Brooke, Rajah of Sarawak, with the highest honour to which man can
aspire. The climate is healthy, tempered by sea-breezes, and in some
parts even European; and its appendage, the small island of Labuan, rich
in coal, is happily situate in the route of steam-vessels between India
and China.
A volume might be written on the beauty and riches of the Indian
Archipelago. Many of the islands are hardly known; the interior of the
greater number has never been explored, so that they offer a wide field
of discovery to the enterprising traveller, and they are now of easier
access since the seas have been cleared of pirates by the exertions of
the Honourable Captain Keppel, and other officers of Her Majesty’s Navy.
They have become of much importance since our relations with China have
been extended, on which account surveys of their coasts have been
already made, and are going on, under the able direction of the
Hydrographer of the Navy, Sir F. Beaufort. The great intertropical
islands of the Pacific, likewise other large islands, as Ceylon and
Madagascar, in the Indian Seas, which by the way do not differ in
character from the preceding, are really continents in miniature, with
their mountains and plains, their lakes and rivers; and in climate they
vary, like the main land, with the latitude, only that continental
climates are more extreme both as to heat and cold.
It is a singular circumstance, arising from the instability of the crust
of the earth, that all the smaller tropical pelasgic islands in the
Pacific and Indian Oceans are either volcanic or coralline, except New
Caledonia and the Seychelles; and it is a startling fact, that in most
cases where there are volcanos the land is rising by slow and almost
imperceptible degrees above the ocean, whereas there is every reason to
believe that those vast spaces, studded with coral islands or atolls,
are actually sinking below it, and have been for ages.[76]
Public-domain text, read in full here on John Shaqi.
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