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
This east wind continually blowing under the line, is the cause, that
sailing from Europe to America, the course of the vessel is directed
from the north to the south, along the coasts of Spain and Africa, to
within 20 degrees of the equator, where this east wind is met with,
which carries them directly to the coasts of America. The voyage from
Acapulco to the Philippine islands, is made in two months by the favour
of this east wind: but the return from them to Acapulco is longer and
more difficult. At 28 or 30 degrees on this coast from the line, the
western wind is nearly as constant, which is the reason that vessels
returning from the East Indies to Europe, do not follow the same track
as in going; those from New Spain sail north along the coasts till they
arrive at the Havannah, and from thence they continue northward, until
they meet with the westerly winds which carry them to the Azores and
afterwards to Spain. So likewise in the South Sea, those which return
from the Philippines, or China, to Peru, or Mexico, sail north as far
as Japan, and navigate under that parallel to a certain distance from
California, from whence, coasting along New Spain, they arrive at
Acapulco. These winds do not always blow from one point, but in general
from the south-east from April to November, and from the north-east
from November to April.
The east wind, by its action, increases the general motion of the
sea from east to west; it also produces currents which are constant,
some flowing from east to west, others from west to east; and from
the east to the south-west or north-west, following the direction of
the eminencies and chains of mountains at the bottom of the sea, the
vallies that divide them serving as channels to these currents. The
alternative winds which blow sometimes from the east, and sometimes
from the south, produce also currents which change their direction at
the same time with these winds.
The winds which blow continually for some months, are generally
followed by contrary winds, and therefore mariners are obliged to wait
for that which is favourable to their voyage. When these winds change,
a calm or dangerous tempest generally ensues, and which continues for
several days, sometimes a month, and has been known for more than two.
Public-domain text, read in full here on John Shaqi.
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