Buffon's Natural History, Volume 02 (of 10): Containing a Theory of the Earth, a General History of Man, of the Brute Creation, and of Vegetables, Mineral, &c. &cBuffon, Georges Louis Leclerc, comte de
History
Buffon's Natural History, Volume 02 (of 10): Containing a Theory of the Earth, a General History of Man, of the Brute Creation, and of Vegetables, Mineral, &c. &c
Buffon, Georges Louis Leclerc, comte de
Natural history
The coasts of Italy are bordered by several sorts of marble and
stone; these rocks appear at a distance as so many pillars of marble
perpendicularly divided. The coasts of France from Brest to Bourdeaux
are almost surrounded with rocks just at the water's edge, which
occasion dangerous breakers. The coasts of England, Spain, and many
others, are also bordered with rocks and hard stone; excepting some
parts which are made use of for bays, ports, and havens.
The depth of water along the coasts is in proportion to their
elevation. The inequalities at the bottom of the sea near the coasts,
correspond also with the inequalities of the surface of the ground
along the shore. A celebrated navigator has made the following
observations on this subject.
"I have constantly remarked, that where the coasts are defended
by steep rocks, the sea is there very deep, and seldom affords a
probability of anchoring; and, on the contrary, where the ground
inclines from the coast to the sea, however elevated it may be further
inland, the bottom is good there, and consequently admits of anchorage.
"According to the declivity of land, as it approaches the water's
edge, so we generally find our anchor ground, and either approach or
keep at a distance from shore agreeable to the steepness of the land;
for I never saw or heard of a coast where the land is of a continual
height, without some vallies lying intermixed with the high-lands;
they are the subsiding of low lands, and afford good anchoring, the
earth being lodged deep under water; for this reason it is we find good
harbours upon coasts which abound with steep cliffs, because the land
has subsided between them. But Where the declensions from the hills is
not within land but towards the main sea, as at Chili and Peru, and
the coasts are nearly perpendicular, as in the countries running from
the Andes, it is very deep, and has scarcely any creeks or harbours.
The coasts of Gallicia, Portugal, Newfoundland, the islands of Juan
Fernando and St. Helena, &c. are somewhat similar to those of Peru,
yet good harbours are not so scarce, as there is always good anchorage
where there are short ridges of land. In general the land under water
seems to be exactly proportioned to the rising of the contiguous part
above, and therefore, where the lands upon the shores are steep, there
is but little security for ships, they being very easily driven from
their moorings; yet although steep cliffs denote this disadvantage,
they assure us of this benefit also, that we can sail close to them
with safety, besides being able to see them at a considerable distance;
whereas low lands are frequently not discovered until we are near, and
always experience the hazard of running aground. This fact of good
anchorage where the lands on the coast are low, might be illustrated by
many instances in the bays of Campeachy, Honduras, Panama; the coasts
of Portobella, Carthagena, Guinea, Callifornia, China, Coromandel, &c.
Public-domain text, read in full here on John Shaqi.
Reviews
Reviews
No reviews yet
Be the first to share your thoughts on this work.
Join the Discussion
Join the discussion
Sign in to leave a comment or review.
Sign InorCreate an account