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
Eusebius relates two testimonies on the subject of deluges: one of
which is Melo, who says that the plains of Syria had formerly been
laid under water; the other is Abydenus, who says, that in the time
of King Sisithrus there was a great deluge, which had been predicted
by Saturnus, Plutarch _De Solestia Animalium_. Ovid, and other
mythologists, speak of the deluge of Deucalion, which, according to
them, was in Thessaly, about 700 years from the universal deluge. It is
also asserted that there had been one more ancient in Attica, in the
time of Ogiges, about 230 years before that of Deucalion.
In the year 1095 there was a deluge in Syria, which drowned a number
of people.[BE] In 1164 there was so considerable a one in Friezeland,
that all maritime coasts were covered, and several thousands of the
inhabitants drowned.[BF] In 1218 there was another inundation which
destroyed near an hundred thousand people. There are a multitude of
other examples of great inundations, like that of 1604 in England, and
many more.
[BE] See Alsted. Chron. chap. 25.
[BF] See Krank, Lib. 5, cap. 4.
A third cause of the change on the surface of the globe, are impetuous
winds. They not only form downs and hills on the sea shores, but they
often stop and choak up rivers, and change their directions; they tear
up cultivated land, destroy trees, overthrow edifices, and cover entire
countries with sand. We have an example of these inundations of sand on
the coasts of Britany in France: the history of the Royal Academy at
Paris, anno 1722, makes mention of it in the following terms.
"In the environs of St. Paul de Leon, in Lower Britany, there is a
quarter near the sea, which before the year 1666, was inhabited; but
is so no longer, by reason of a sand which covers it to the height of
more than twenty feet, and which gains ground every year. Reckoning
from that time it has proceeded upwards of six leagues into the
country, and is now not more than about half a league from St. Paul, so
that according to all appearance that town must soon be deserted. The
tops of some steeples and chimnies are still seen peeping out of this
sea of sand; the inhabitants of the interred villages have always had
sufficient time to quit their houses in safety.
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.
Elsewhere in the archive
Join the Discussion
Join the discussion
Sign in to leave a comment or review.
Sign InorCreate an account