Beagle Expedition (1831-1836); Coral reefs and islands; Geology -- South America; Islands; Volcanoes
The SOCIETY Archipelago is separated by a narrow space from the Low
Archipelago; and in their parallel direction they manifest some
relation to each other. I have already described the general character
of the reefs of these fine encircled islands. In the “Atlas of the
‘Coquille’s’ Voyage” there is a good general chart of the group, and
separate plans of some of the islands. _Tahiti_, the largest island in
the group, is almost surrounded, as seen in Cook’s chart, by a reef
from half a mile to a mile and a half from the shore, with from ten to
thirty fathoms within it. Some considerable submerged reefs lying
parallel to the shore, with a broad and deep space within, have lately
been discovered (“Naut. Mag.” 1836, page 264) on the N.E. coast of the
island, where none are laid down by Cook. At _Eimeo_ the reef “which
like a ring surrounds it, is in some places one or two miles distant
from the shore, in others united to the beach” (Ellis, “Polynesian
Researches,” volume i., page 18, 12mo edition). Cook found deep water
(twenty fathoms) in some of the harbours within the reef. Mr. Couthouy,
however, states (“Remarks,” page 45) that both at Tahiti and Eimeo, the
space between the barrier-reef and the shore, has been almost filled
up,—“a nearly continuous fringing-reef surrounding the island, and
varying from a few yards to rather more than a mile in width, the
lagoons merely forming canals between this and the sea-reef,” that is
the barrier-reef. _Tapamanoa_ is surrounded by a reef at a considerable
distance from the shore; from the island being small it is breached, as
I am informed by the Rev. W. Ellis, only by a narrow and crooked boat
channel. This is the lowest island in the group, its height probably
not exceeding 500 feet. A little way north of Tahiti, the low
coral-islets of _Teturoa_ are situated; from the description of them
given me by the Rev. J. Williams (the author of the “Narrative of
Missionary Enterprise”), I should have thought they had formed a small
atoll, and likewise from the description given by the Rev. D. Tyerman
and G. Bennett (“Journal of Voyage and Travels,” volume i., page 183),
who say that ten low coral-islets “are comprehended within one general
reef, and separated from each other by interjacent lagoons;” but as Mr.
Stutchbury (“West of England Journal,” volume i., page 54) describes it
as consisting of a mere narrow ridge, I have left it uncoloured.
_Maitea_, eastward of the group, is classed by Forster as a high
encircled island; but from the account given by the Rev. D. Tyerman and
G. Bennett (volume i., page 57) it appears to be an exceedingly abrupt
cone, rising from the sea without any reef; I have left it uncoloured.
It would be superfluous to describe the northern islands in this group,
as they may be well seen in the chart accompanying the 4to edition of
Cook’s “Voyages,” and in the “Atlas of the ‘Coquille’s’ Voyage.”
_Maurua_ is the only one of the northern islands, in which the water
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