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
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, vol. i, p. 151); coloured blue. Thirdly, _Aldabra_; it
consists of three islets, about twenty-five feet in height, with red
cliffs (Horsburgh, vol. i, p. 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 (vol. i, p. 216, 4th
ed.), 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 (vol. i, p. 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.” vol. i, p. 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, vol. i, p. 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 (vol. i, p. 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 much less
extensive than round the other islands in the group.
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