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 LOW ARCHIPELAGO.—This group consists of about eighty atolls: it
will be quite superfluous to refer to descriptions of each. In
D’Urville and Lottin’s chart, one island (_Wolchonsky_) is written with
a capital letter, signifying, as explained in a former chapter, that it
is a high island; but this must be a mistake, as the original chart by
Bellinghausen shows that it is a true atoll. Captain Beechey says of
the thirty-two groups which he examined (of the greater number of which
I have seen beautiful MS. charts in the Admiralty), that twenty-nine
now contain lagoons, and he believes the other three originally did.
Bellinghausen (see an account of his Russian voyage, in the “Biblioth.
des Voyages,” 1834, p. 443) says, that the seventeen islands which he
discovered resembled each other in structure, and he has given charts
on a large scale of all of them. Kotzebue has given plans of several;
Cook and Bligh mention others; a few were seen during the voyage of the
_Beagle_; and notices of other atolls are scattered through several
publications. The _ Actæon_ group in this archipelago has lately been
discovered (_Geograph. Journ._, vol. vii, p. 454); it consists of three
small and low islets, one of which has a lagoon. Another lagoon-island
has been discovered (_Naut. Mag._, 1839, p. 770), in 22° 4′ S., and
136° 20′ W. Towards the S.E. part of the group, there are some islands
of different formation: _ Elizabeth_ Island is described by Beechey (p.
46, 4to ed.) as fringed by reefs, at the distance of between two and
three hundred yards; coloured red. _Pitcairn_ Island, in the immediate
neighbourhood, according to the same authority, has no reefs of any
kind, although numerous pieces of coral are thrown up on the beach; the
sea close to its shore is very deep (see “Zool. of Beechey’s Voyage,”
p. 164); it is left uncoloured. _Gambier_ Islands (see Plate I Fig. 8),
are encircled by a barrier-reef; the greatest depth within is
thirty-eight fathoms; coloured pale blue. _Aurora_ Island, which lies
N.E. of Tahiti close to the large space coloured dark blue in the map,
has been already described in a note (), on the authority of Mr.
Couthouy; it is an upraised atoll, but as it does not appear to be
fringed by living reefs, it is left uncoloured.
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