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
The Red Sea does not receive any river whose motion
might oppose the tides, whereas the Persian Gulph receives three very
considerable ones in its most projecting extremity. It appears very
apparently that the Red Sea has been formed by an eruption of the
ocean, for the bearing of the lands are exactly similar, the coasts
on each side of the straits follow the same direction,, and evidently
appear to have been cut by waters.
At the extremity of the Red Sea is that famous neck of land called the
Isthmus of Suez, which forms a barrier to the Red Sea, and prevents
its communication with the Mediterranean. In a preceding article we
noticed the reasons which inclined us to think that the Red Sea is
higher than the Mediterranean, and that if the Isthmus of Suez was
cut, an inundation and an augmentation of the latter might ensue. To
which we shall subjoin, that if even it should not be agreed that the
Red Sea is higher than the Mediterranean, it cannot be denied that
there is neither flux nor reflux in the Mediterranean, adjoining to
the mouths of the Nile; and that, on the contrary, in the Red Sea the
tides are very considerable, and raise the water several feet, which
circumstance alone would suffice to send a quantity of water into the
Mediterranean if the Isthmus was broken. Besides, we have an example on
this subject quoted by Varenius, who says in page 100 of his Geography:
"Oceanus Germanicus, qui est Atlantici pars, inter Frisiam & Hollandium
se effundens, efficit sinum, qui et si parvis sit respectu celebrium
sinum maris, tamen & ipse dicitur mare, alluitque Hollandiæ emporium
celeberrimum, Amstelodamum. Non procul inde abest lacus Harlemensis,
qui etiam mare Harlemense dicitur. Hujus altitudo non est minor
altitudine sinus illius Belgici, quem diximus & mittit ramum ad urbem
Leidam, ubi in varias fossas divaricatur. Quoniam itaque nec lacus
his, neque sinus ille Hollandici maris inundant adjacentes agros (de
naturali constitutione loquor, non ubi tempestatibus urgentur, propter
quas aggeres facti sunt) pater inde, quod non sint altiores quam agri
Hollandiæ. At vero Oceanum Germanicum esse altiorem quam terras hasce,
experti sunt Leidenses, cum suscepissent fossam seu alveum ex urbe sua
ad Oceani Germanici littora, prope Cattorum vicum perducere (distantia
est duorum milliarum) ut, recepto per alveum hunc mari, possent
navigationem instituere in Oceanum Germanicum, & hinc in varias terræ
regiones. Verumenimvero cum magnam jam alvei port em perfecissent,
desistere coacti sunt, quoniam turn demum per observationem cognitem
est, Oceani Germanici aquam esse altiorem quam agrum inter Leidam et
litus Oceani istius; unde locus ille, ubi fodere desierunt dicitur,
_Het malle Gat_. Oceanus itaque Germanicus est aliquantum altior quam
sinus ille Hollandicus, &c." Therefore, as the German Sea is higher
than that of Holland, there is no reason why we should not believe the
Red Sea may be higher than the Mediterranean. Herodotus and Diodorus
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.
Join the Discussion
Join the discussion
Sign in to leave a comment or review.
Sign InorCreate an account