Buffon's Natural History, Volume 01 (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 01 (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
What we have now said on the great eminences of the earth, may also be
observed on the greatest depths of the sea. The vast and highest seas
are nearer the equator than the poles; and there results from this
observation, that the greatest inequalities of the globe are in the
southern climate. These irregularities on the surface of the earth, are
the causes of an infinity of extraordinary effects: for example, between
the Indus and the Ganges, there is a large peninsula, which is divided
through its middle, by a chain of high mountains called the Gate, and
which extends from north to south, from the extremities of Mount
Caucasus to Cape Comorin; on one is the coast of Malabar, and the other
Coromandel; on the side of Malabar, between this chain of mountains and
the sea, the summer season lasts from September to April, during which
the sky is serene and dry; on the other side the Coromandel the above
period is their winter, and it rains every day plentifully and from the
month of April to the month of September is their summer, whereas it is
winter in Malabar; insomuch, that in many places, which are scarcely 20
miles distant, we may, by crossing the mountains, change seasons. It is
said that the same thing takes place at Razalgat in Arabia, and at
Jamaica, which is divided through its middle by a chain of mountains,
whose direction is from east to west, and that the plantations to the
south of these mountains feel the summer heat, at the time those to the
north endure the rigor of winter.
Peru, which is situated under the line, and extends about a thousand
leagues to the south, is divided into three long and narrow parts; these
the natives call Lanos, Sierras, and Andes. The Lanos, which comprehends
the plains, extends along the coast of the South Sea: the Sierras are
hills with some vallies, and the Andes are the famous Cordeliers, the
highest mountains that are known. The Lanos is about ten leagues in
breadth; in many places the Sierras are twenty leagues broad, and the
Andes in some places more and in some less. The breadth is from east to
west, and the length from north to south. This part of the world is
remarkable for the following particulars: first, in the Lanos the wind
almost constantly blows from the south-west, which is contrary to what
happens in the torrid zone: secondly, it never rains nor thunders in the
Lanos, although there is plenty of dew: thirdly, it almost continually
rains in the Andes: fourthly, in the Sierras, between the Lanos and the
Andes, it rains from September to April.
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