Beagle Expedition (1831-1836); Coral reefs and islands; Geology -- South America; Islands; Volcanoes
_Cosmoledo;_ “this group consists of a ring of coral, ten leagues in
circumference, and a quarter of a mile broad in some places, enclosing
a magnificent lagoon, into which there did not appear a single opening”
(Horsburgh, volume i., page 151); coloured blue. Thirdly, _Aldabra;_ it
consists of three islets, about twenty-five feet in height, with red
cliffs (Horsburgh, volume i., page 176) surrounding a very shallow
basin or lagoon. The sea is profoundly deep close to the shore. Viewing
this island in a chart, it would be thought an atoll; but the foregoing
description shows that there is something different in its nature; Dr.
Allan also states that it is cavernous, and that the coral-rock has a
vitrified appearance. Is it an upheaved atoll, or the crater of a
volcano?—uncoloured.
COMORO GROUP.—_Mayotta_, according to Horsburgh (volume i., page 216,
4th edition), is completely surrounded by a reef, which runs at the
distance of three, four, and in some places even five miles from the
land; in an old chart, published by Dalrymple, a depth in many places
of thirty-six and thirty-eight fathoms is laid down within the reef. In
the same chart, the space of open water within the reef in some parts
is even more than three miles wide: the land is bold and peaked; this
island, therefore, is encircled by a well-characterised barrier-reef,
and is coloured pale blue.—_Johanna;_ Horsburgh says (volume I. page
217) this island from the N.W. to the S.W. point, is bounded by a reef,
at the distance of two miles from the shore; in some parts, however,
the reef must be attached, since Lieutenant Boteler (“Narr.” volume i.,
page 161) describes a passage through it, within which there is room
only for a few boats. Its height, as I am informed by Dr. Allan, is
about 3,500 feet; it is very precipitous, and is composed of granite,
greenstone, and quartz; coloured blue.—_Mohilla;_ on the S. side of
this island there is anchorage, in from thirty to forty-five fathoms,
between a reef and the shore (Horsburgh, volume i., page 214); in
Captain Owen’s chart of Madagascar, this island is represented as
encircled; coloured blue.—_Great Comoro Island_ is, as I am informed by
Dr. Allan, about 8,000 feet high, and apparently volcanic; it is not
regularly encircled; but reefs of various shapes and dimensions, jut
out from every headland on the W., S., and S.E. coasts, inside of which
reefs there are channels, often parallel with the shore, with deep
water. On the north-western coasts the reefs appear attached to the
shores. The land near the coast is in some places bold, but generally
speaking it is flat; Horsburgh says (volume i., page 214) the water is
profoundly deep close to the _shore_, from which expression I presume
some parts are without reefs. From this description I apprehend the
reef belongs to the barrier class; but I have not coloured it, as most
of the charts which I have seen, represent the reefs round it as very
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