Beagle Expedition (1831-1836); Coral reefs and islands; Geology -- South America; Islands; Volcanoes
The object of this volume is to describe from my own observation and
the works of others, the principal kinds of coral-reefs, more
especially those occurring in the open ocean, and to explain the origin
of their peculiar forms. I do not here treat of the polypifers, which
construct these vast works, except so far as relates to their
distribution, and to the conditions favourable to their vigorous
growth. Without any distinct intention to classify coral-reefs, most
voyagers have spoken of them under the following heads:
“lagoon-islands,” or “atolls,” “barrier” or “encircling reefs,” and
“fringing” or “shore-reefs.” The lagoon-islands have received much the
most attention; and it is not surprising, for every one must be struck
with astonishment, when he first beholds one of these vast rings of
coral-rock, often many leagues in diameter, here and there surmounted
by a low verdant island with dazzling white shores, bathed on the
outside by the foaming breakers of the ocean, and on the inside
surrounding a calm expanse of water, which from reflection, is of a
bright but pale green colour. The naturalist will feel this
astonishment more deeply after having examined the soft and almost
gelatinous bodies of these apparently insignificant creatures, and when
he knows that the solid reef increases only on the outer edge, which
day and night is lashed by the breakers of an ocean never at rest. Well
did François Pyrard de Laval, in the year 1605, exclaim, “C’est une
merueille de voir chacun de ces atollons, enuironné d’un grand banc de
pierre tout autour, n’y ayant point d’artifice humain.” The
accompanying sketch of Whitsunday island, in the South Pacific, taken
from Captain Beechey’s admirable “Voyage,” although excellent of its
kind, gives but a faint idea of the singular aspect of one of these
lagoon-islands.
[Illustration]
Whitsunday Island is of small size, and the whole circle has been
converted into land, which is a comparatively rare circumstance. As the
reef of a lagoon-island generally supports many separate small islands,
the word “island,” applied to the whole, is often the cause of
confusion; hence I have invariably used in this volume the term
“atoll,” which is the name given to these circular groups of
coral-islets by their inhabitants in the Indian Ocean, and is
synonymous with “lagoon-island.”
[Illustration]
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