Beagle Expedition (1831-1836); Coral reefs and islands; Geology -- South America; Islands; Volcanoes
series, beginning with fragments of unaltered coral, and ending with
others, where it was impossible to discover with the naked eye any
trace of organic structure. In some specimens I was unable, even with
the aid of a lens, and by wetting them, to distinguish the boundaries
of the altered coral and spathose limestone. Many even of the blocks of
coral lying loose on the beach, had their central parts altered and
infiltrated.
The lagoon alone remains to be described; it is much shallower than
that of most atolls of considerable size. The southern part is almost
filled up with banks of mud and fields of coral, both dead and alive,
but there are considerable spaces, between three and four fathoms, and
smaller basins, from eight to ten fathoms deep. Probably about half its
area consists of sediment, and half of coral-reefs. The corals
composing these reefs have a very different aspect from those on the
outside; they are very numerous in kind, and most of them are thinly
branched. Meandrina, however, lives in the lagoon, and great rounded
masses of this coral are numerous, lying quite or almost loose on the
bottom. The other commonest kinds consist of three closely allied
species of true Madrepora in thin branches; of _Seriatapora subulata;_
two species of Porites[4] with cylindrical branches, one of which forms
circular clumps, with the exterior branches only alive; and lastly, a
coral something like an Explanaria, but with stars on both surfaces,
growing in thin, brittle, stony, foliaceous expansions, especially in
the deeper basins of the lagoon. The reefs on which these corals grow
are very irregular in form, are full of cavities, and have not a solid
flat surface of dead rock, like that surrounding the lagoon; nor can
they be nearly so hard, for the inhabitants made with crowbars a
channel of considerable length through these reefs, in which a
schooner, built on the S.E. islet, was floated out. It is a very
interesting circumstance, pointed out to us by Mr. Liesk, that this
channel, although made less than ten years before our visit, was then,
as we saw, almost choked up with living coral, so that fresh
excavations would be absolutely necessary to allow another vessel to
pass through it.
[4] This Porites has somewhat the habit of _P. clavaria_, but the
branches are not knobbed at their ends. When alive it is of a yellow
colour, but after having been washed in fresh water and placed to dry,
a jet-black slimy substance exuded from the entire surface, so that
the specimen now appears as if it had been dipped in ink.
Public-domain text, read in full here on John Shaqi.
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