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
In America there are a great number of volcanos, particularly in the
mountains of Peru and Mexico; that of Arequipa is one of the most
famous; it often causes earthquakes, which are more common in Peru
than in any other country in the world. The volcano of Carrappa and
that of Malahallo are, according to the report of travellers, the most
considerable, next to that of Arequipa; but there are many others in
these parts of which we have no exact knowledge. M. Bouguer, in his
voyage to Peru, published in the Memoirs of the Academy of the year
1744, mentions two volcanos, called Cotopaxi and Pichincha; the first
at some distance from, the other near the town of Quito; he was witness
of a conflagration of Botopaxi in 1742, and of the orifice which was
made in that mountain; this eruption did no other damage than melting
the snow and producing such torrents of water, that in less than three
hours inundated a tract of country 18 leagues in extent, and overthrew
all they met with in their way.
At Mexico the most considerable volcanos are Popochampeche, and the
Popoatepec; it was near this last that Cortes passed in his voyage
to Mexico; some of the Spaniards ascended to the top, where they saw
the mouth, which was about half a league in circumference. Sulphurous
mountains are also met with at Guadaloupe, Tercera, and other islands
of the Azores; and, if we were to consider as volcanos all those
mountains which smoke, or emit flames, we might reckon more than sixty;
we have only spoken of those formidable volcanos, near which no person
dares to inhabit.
These volcanos which are in such great numbers in the Cordeliers, as I
have formerly said, cause almost continual earthquakes, which prevent
the natives from building with stone above one story high, and to
construct the upper stories of their houses with reeds and light wood.
In these mountains are also many precipices and large vents, the sides
of which are black and burnt, as in the precipice of Mount Ararat, in
Armenia, which is called the Abyss; these abysses are the mouths of
extinguished volcanos.
There was lately an earthquake at Lima, the effects of which were
dreadful. The town of Lima and Port Callao were almost entirely
swallowed up; but the evil was still greater at Callao. The sea rose
and covered every building in that town, drowned all the inhabitants,
and left only one single tower remaining. Of twenty-five ships that
were in this port, four were carried a league upon land, and the rest
were swallowed up by the sea. At Lima, which was a large town, there
remains only twenty-seven houses standing; a great number of persons
were buried in the ruins, particularly monks and religious persons, as
their buildings were higher and constructed of more solid materials
than the other houses. This misfortune happened at night, in October
1746; the shock remained fifteen minutes.
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