Beagle Expedition (1831-1836); Coral reefs and islands; Geology -- South America; Islands; Volcanoes
ADMIRALTY GROUP.—From the accounts by Bougainville, Maurelle,
D’Entrecasteaux, and the scattered notices collected by Horsburgh, it
appears, that some of the many islands composing it, are high, with a
bold outline; and others are very low, small and interlaced with reefs.
All the high islands appear to be fronted by distant reefs rising
abruptly from the sea, and within some of which there is reason to
believe that the water is deep. I have therefore little doubt they are
of the barrier class.—In the southern part of the group we have
_Elizabeth Island_, which is surrounded by a reef at the distance of a
mile; and two miles eastward of it (Krusenstern, “Append.” 1835, page
42) there is a little island containing a lagoon.—Near here, also lies
_Circular-reef_ (Horsburgh, “Direct.” volume i., page 691, 4th
edition), “three or four miles in diameter having deep water inside
with an opening at the N.N.W. part, and on the outside steep to.” I
have from these data, coloured the group pale blue, and _circular-reef_
dark blue.—the _Anachorites_, _Echequier_, and _Hermites_, consist of
innumerable low islands of coral-formation, which probably have
atoll-like forms; but not being able to ascertain this, I have not
coloured them, nor _Durour_ Island, which is described by Carteret as
low.
The CAROLINE ARCHIPELAGO is now well-known, chiefly from the
hydrographical labours of Lutké; it contains about forty groups of
atolls, and three encircled islands, two of which are engraved in
Figures 2 and 7, Plate I. Commencing with the eastern part; the
encircling reef round _Ualen_ appears to be only about half a mile from
the shore; but as the land is low and covered with mangroves (“Voyage
autour du Monde,” par F. Lutké, volume i., page 339), the real margin
has not probably been ascertained. The extreme depth in one of the
harbours within the reef is thirty-three fathoms (see charts in “Atlas
of ‘Coquille’s’ Voyage”), and outside at half a mile distant from the
reef, no bottom was obtained with two hundred and fifty fathoms. The
reef is surmounted by many islets, and the lagoon-like channel within
is mostly shallow, and appears to have been much encroached on by the
low land surrounding the central mountains; these facts show that time
has allowed much detritus to accumulate; coloured pale blue.—
_Pouynipète_, or _Seniavine_. In the greater part of the circumference
of this island, the reef is about one mile and three quarters distant;
on the north side it is five miles off the included high islets. The
reef is broken in several places; and just within it, the depth in one
place is thirty fathoms, and in another, twenty-eight, beyond which, to
all appearance, there was “un porte vaste et sur” (Lutké, volume ii.,
page 4); coloured pale blue.—_Hogoleu_ or _Roug_. This wonderful group
contains at least sixty-two islands, and its reef is one hundred and
thirty-five miles in circuit. Of the islands, only a few, about six or
eight (see “Hydrog.
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