Coral Reefs; Volcanic Islands; South American Geology — CompleteDarwin, Charles
Science
Coral Reefs; Volcanic Islands; South American Geology — Complete
Darwin, Charles
Beagle Expedition (1831-1836); Coral reefs and islands; Geology -- South America; Islands; Volcanoes
The coast of _Malacca, Tenasserim_ and the coasts northward, appear in
the greater part to be low and muddy: where reefs occur, as in parts of
_Malacca Straits_, and near _ Singapore_, they are of the fringing
kind; but the water is so shoal, that I have not coloured them. In the
sea, however, between Malacca and the west coast of Borneo, where there
is a greater depth from forty to fifty fathoms, I have coloured red
some of the groups, which are regularly fringed. The northern _Natunas_
and the _Anambas_ Islands are represented in the charts on a large
scale, published in the “Atlas of the Voyage of the _ Favourite_,” as
fringed by reefs of coral, with very shoal water within
them.—_Tumbelan_ and _Bunoa_ Islands (1° N.) are represented in the
English charts as surrounded by a very regular fringe.—_St. Barbes_ (0°
15′ N.) is said by Horsburgh (vol. ii, p. 279) to be fronted by a reef,
over which boats can land only at high water.—The shore of _Borneo_ at
_Tunjong Apee_ is also fronted by a reef, extending not far from the
land (Horsburgh, vol. ii, p. 468). These places I have coloured red;
although with some hesitation, as the water is shallow. I might perhaps
have added _Pulo Leat_, in Gaspar Strait, _Lucepara_, and _Carimata_;
but as the sea is confined and shallow, and the reefs not very regular,
I have left them uncoloured.
The water shoals gradually towards the whole west coast of _ Borneo_: I
cannot make out that it has any reefs of coral. The islands, however,
off the northern extremity, and near the S.W. end of _Palawan_, are
fringed by very distant coral-reefs; thus the reefs in the case of
_Balabac_ are no less than five miles from the land; but the sea, in
the whole of this district, is so shallow, that the reefs might be
expected to extend very far from the land. I have not, therefore,
thought myself authorised to colour them. The N.E. point of Borneo,
where the water is very shoal, is connected with Magindanao by a chain
of islands called the _Sooloo Archipelago_, about which I have been
able to obtain very little information; _Pangootaran_, although ten
miles long, entirely consists of a bed of coral-rock (“Notices of E.
Indian Arch.” p. 58): I believe from Horsburgh that the island is low;
not coloured.—_Tahow Bank_, in some old charts, appears like a
submerged atoll; not coloured. Forrest (“Voyage,” p. 21) states that
one of the islands near Sooloo is surrounded by coral-rocks; but there
is no distant reef. Near the S. end of _ Basselan_, some of the islets
in the chart accompanying Forrest’s “Voyage,” appear fringed with
reefs; hence I have coloured, though unwillingly, parts of the Sooloo
group red. The sea between Sooloo and Palawan, near the shoal coast of
Borneo, is interspersed with irregular reefs and shoal patches; not
coloured: but in the northern part of this sea, there are two low
islets, _ Cagayanes_ and _Cavilli_, surrounded by extensive
coral-reefs; the breakers round the latter (Horsburgh, vol. ii, p. 513)
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