Coral Reefs; Volcanic Islands; South American Geology — Complete — John Shaqi
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
The woodcut represents a section across one of the islets on the reef,
but if all that part which is above the level of C were removed, the
section would be that of a simple reef, as it occurs where no islet has
been formed. It is this reef which essentially forms the atoll. It is a
ring, enclosing the lagoon on all sides except at the northern end,
where there are two open spaces, through one of which ships can enter.
The reef varies in width from two hundred and fifty to five
hundred yards, its surface is level, or very slightly inclined towards
the lagoon, and at high tide the sea breaks entirely over it: the water
at low tide thrown by the breakers on the reef, is carried by the many
narrow and shoal gullies or channels on its surface, into the lagoon: a
return stream sets out of the lagoon through the main entrance. The
most frequent coral in the hollows on the reef is _Pocillopora
verrucosa_, which grows in short sinuous plates, or branches, and when
alive is of a beautiful pale lake-red: a Madrepora, closely allied or
identical with _M. pocillifera_, is also common. As soon as an islet is
formed, and the waves are prevented breaking entirely over the reef,
the channels and hollows in it become filled up with cemented
fragments, and its surface is converted into a hard smooth floor (C of
woodcut), like an artificial one of freestone. This flat surface varies
in width from one hundred to two hundred, or even three hundred yards,
and is strewed with a few large fragments of coral torn up during
gales: it is uncovered only at low water. I could with difficulty, and
only by the aid of a chisel, procure chips of rock from its surface,
and therefore could not ascertain how much of it is formed by the
aggregation of detritus, and how much by the outward growth of mounds
of corals, similar to those now living on the margin. Nothing can be
more singular than the appearance at low tide of this “flat” of naked
stone, especially where it is externally bounded by the smooth convex
mound of Nulliporæ, appearing like a breakwater built to resist the
waves, which are constantly throwing over it sheets of foaming water.
The characteristic appearance of this “flat” is shown in the foregoing
woodcut of Whitsunday atoll.
Public-domain text, read in full here on John Shaqi.
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