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
The surface of the Earth, like that of Jupiter, is not divided by bands
alternative and parallel to the equator; on the contrary, it is divided
from one pole to the other, by two bands of earth, and two of sea; the
first and principal is the ancient continent, the greatest length of
which is found to be in a line, beginning on the east point of the
northern part of Tartary, and extending from thence to the land which
borders on the gulph of Linchidolkin, where the Muscovites fish for
whales; from thence to Tobolski, from Tobolski to the Caspian sea, from
the Caspian sea to Mecca, and from Mecca to the western part of the
country inhabited by the Galli, in Africa; afterwards to Monoemuci or
Monomotapa, and at last to the Cape of Good Hope; this line, which is
the greatest length of the old continent, is about 3600 leagues, Paris
measure; it is only interrupted by the Caspian and Red seas, the
breadths of which are not very considerable, and we must not pay any
regard to these interruptions, when it is considered, the surface of the
globe is divided only in four parts.
This greatest length is found by measuring the old continent diagonally;
for if measured according to the meridians, we shall find that there are
only 2500 leagues from the northernmost Cape of Lapland to the Cape of
Good Hope; and that the Baltic and Mediterranean cause a much greater
interruption than is met with in the other way. With respect to all the
other distances that might be measured in the old continent under the
same meridian, we shall find them to be much smaller than this; having,
for example, only 1800 leagues from the most southern point of the
island of Ceylon to the northernmost coast of Nova Zembla. Likewise, if
we measure the continent parallel to the equator, we find that the
greatest uninterrupted length is found from Trefna, on the western coast
of Africa, to Ninpo, on the eastern coast of China, and that it is about
2800 leagues. Another course may be measured from the point of Brittany
near Brest, extending to the Chinese Tartary; about 2300 leagues. From
Bergen, in Norway, to the coast of Kamschatka, is no more than 1800
leagues. All these lines have much less length than the first, therefore
the greatest extent of the old continent, is, in fact, from the eastern
point of Tartary to the Cape of Good Hope, that is about 3600 leagues.
There is so great an equality of surface on each side of this line,
which is also the longest, that there is every probability to suppose it
really divides the contents of the ancient continent; for in measuring
on one side is found 2,471,092-3/4 square leagues, and on the other
2,469,687.
Agreeable to this, the old continent consists of about 4,940,780 square
leagues, which is nearly one-fifth of the whole surface of the globe,
and has an inclination towards the equator of about 30 degrees.
Public-domain text, read in full here on John Shaqi.
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