Island Life; Or, The Phenomena and Causes of Insular Faunas and FlorasWallace, Alfred Russel
Science
Island Life; Or, The Phenomena and Causes of Insular Faunas and Floras
Wallace, Alfred Russel
Biogeography; Glacial epoch; Island ecology
It is not yet known whether Celebes is completely separated from the
surrounding islands by a deep sea, but {453} the facts at our command
render it probable that it is so. The northern and eastern portions of the
Celebes Sea have been ascertained to be from 2,000 to 2,600 fathoms deep,
and such depths may extend over a considerable portion of it, or even be
much exceeded in the centre. In the Molucca passage a single sounding on
the Gilolo side gave 1,200 fathoms, and a large part of the Molucca and
Banda Seas probably exceed 2,000 fathoms. The southern portion of the
Straits of Macassar is full of coral reefs, and a shallow sea of less than
100 fathoms extends from Borneo to within about forty miles of the western
promontory of Celebes; but farther north there is deep water close to the
shore, and it seems probable that a deep channel extends quite through the
straits, which have no doubt been much shallowed by the deposits from the
great Bornean rivers as well as by those of Celebes itself. Southward
again, the chain of volcanic islands from Bali to Timor appears to rise out
of a deep ocean, the few soundings we possess showing depths of from 670 to
1,300 fathoms almost close to their northern shores. We seem justified,
therefore, in concluding that Celebes is entirely surrounded by a deep sea,
which has, however, become partially filled up by river deposits, by
volcanic upheaval, or by coral reefs. Such shallows, where they exist, may
therefore be due to antiquity and isolation, instead of being indications
of a former union with any of the surrounding islands.
Public-domain text, read in full here on John Shaqi.
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