The Three Voyages of Captain Cook Round the World. Vol. I. Being the First of the First Voyage.Cook, James
History
The Three Voyages of Captain Cook Round the World. Vol. I. Being the First of the First Voyage.
Cook, James
Cook, James, 1728-1779 -- Travel; Explorers -- Great Britain -- Biography; Voyages around the world -- History -- 18th century
During this excursion, Mr. Banks had an excellent opportunity to examine
the rocks, which were almost every where naked, for minerals; but he
found not the least appearance of any. The stones every where, like
those of Madeira, showed manifest tokens of having been burnt; nor is
there a single specimen of any stone, among all those that were
collected in the island, upon which there are not manifest and
indubitable marks of fire; except, perhaps, some small pieces of the
hatchet-stone, and even of that, other fragments were collected which
were burnt almost to a pumice. Traces of fire are also manifest in the
very clay upon the hills; and it may, therefore, not unreasonably be
supposed, that this and the neighbouring islands are either shattered
remains of a continent, which some have supposed to be necessary in this
part of the globe, to preserve an equilibrium of its parts, which were
left behind when the rest sunk by the mining of a subterraneous fire, so
as to give a passage to the sea over it; or were torn from rocks, which,
from the creation of the world, had been the bed of the sea, and thrown
up in heaps, to a height which the waters never reach. One or other of
these suppositions will perhaps be thought the more probable, as the
water does not gradually grow shallow as the shore is approached, and
the islands are almost every where surrounded by reefs, which appear to
be rude and broken, as some violent concussion would naturally leave the
solid substance of the earth. It may also be remarked upon this
occasion, that the most probable cause of earthquakes seems to be the
sudden rushing in of water upon some vast mass of subterraneous fire, by
the instantaneous rarefaction of which into vapour the mine is sprung,
and various substances, in all stages of vitrification, with shells, and
other marine productions, that are now found fossil, and the strata that
covered the furnace, are thrown up; while those parts of the land which
were supported upon the broken shell give way, and sink into the gulf.
With this theory the phænomena of all earthquakes seem to agree: pools
of water are frequently left where land has subsided; and various
substances, which manifestly appear to have suffered by the action of
fire, are thrown up. It is indeed true, that fire cannot subsist without
air; but this cannot be urged against there being fire below that part
of the earth which forms the bed of the sea; because there may be
innumerable fissures by which a communication between those parts and
the external air may be kept up, even upon the highest mountains, and at
the greatest distance from the sea-shore.
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