Beagle Expedition (1831-1836); Coral reefs and islands; Geology -- South America; Islands; Volcanoes
Next, but much inferior in importance to the Porites, is the _Millepora
complanata_.[1] It grows in thick vertical plates, intersecting each
other at various angles, and forms an exceedingly strong honeycombed
mass, which generally affects a circular form, the marginal plates
alone being alive. Between these plates and in the protected crevices
on the reef, a multitude of branching zoophytes and other productions
flourish, but the Porites and Millepora alone seem able to resist the
fury of the breakers on its upper and outer edge: at the depth of a few
fathoms other kinds of stony corals live. Mr. Liesk, who was intimately
acquainted with every part of this reef, and likewise with that of
North Keeling atoll, assured me that these corals invariably compose
the outer margin. The lagoon is inhabited by quite a distinct set of
corals, generally brittle and thinly branched; but a Porites,
apparently of the same species with that on the outside, is found
there, although it does not seem to thrive, and certainly does not
attain the thousandth part in bulk of the masses opposed to the
breakers.
[1] This Millepora (Palmipora of Blainville), as well as the _M.
alcicornis_, possesses the singular property of stinging the skin
where it is delicate, as on the face and arm.
The woodcut shows the form of the bottom off the reef: the water
deepens for a space between one and two hundred yards wide, very
gradually to twenty-five fathoms (_A_ in section), beyond which the
sides plunge into the unfathomable ocean at an angle of 45°.[2] To the
depth of ten or twelve fathoms the bottom is exceedingly rugged, and
seems formed of great masses of living coral, similar to those on the
margin. The arming of the lead here invariably came up quite clean, but
deeply indented, and chains and anchors which were lowered, in the
hopes of tearing up the coral, were broken. Many small fragments,
however, of _Millepora alcicornis_ were brought up; and on the arming
from an eight-fathom cast, there was a perfect impression of an Astræa,
apparently alive. I examined the rolled fragments cast on the beach
during gales, in order further to ascertain what corals grew outside
the reef. The fragments consisted of many kinds, of which the Porites
already mentioned and a Madrepora, apparently the _M. corymbosa_, were
the most abundant. As I searched in vain in the hollows on the reef and
in the lagoon, for a living specimen of this Madrepore, I conclude that
it is confined to a zone outside, and beneath the surface, where it
must be very abundant. Fragments of the _Millepora alcicornis_ and of
an Astræa were also numerous; the former is found, but not in
proportionate numbers, in the hollows on the reef; but the Astræa I did
not see living. Hence we may infer, that these are the kinds of coral
which form the rugged sloping surface (represented in the woodcut by an
uneven line), round and beneath the external margin. Between twelve and
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