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deluge, as well as of Deucalion and Pyrrha, as a commencement
of the account of the great catastrophe, which, according to the
priests of Sais, destroyed the Atalantis; but in this brief
mention, he speaks of the deluge in the singular number, as if it
was one only; and even expressly says, a little farther on, that
the Greeks knew but of one. He places the name of Deucalion
immediately after that of Phoronæus, the first man, without
even adverting to Ogyges; thus, to the extent of his knowledge,
it was a general event, a completely universal deluge, and the
only one that occurred. He looked upon it as identical with that
of Ogyges. Aristotle (Meteor. i. 14,) seems to have been the
first who considered this deluge as only a partial inundation,
which he placed near Dodona and the river Achelous, but this
was the Achelous and Dodona of Thessaly.
Apollodorus (Bibl. i. §7,) gives to the deluge of Deucalion all
its magnitude and mythological character: it happened at the
epoch of the interval between the age of brass and the iron age.
Deucalion is made the son of the Titan Prometheus, the
fabricator of man: he recreates the human race with stones; and
yet Atlas, his uncle, Phoroneus, who lived before him, and
many other antecedent personages, leave large posterities.
The nearer we come down to more recent authors, the more
facts and details do we meet with coinciding with the Mosaic
account of the deluge. Thus Apollodorus gives Deucalion a
chest as his means of safety; Plutarch mentions the pigeons by
which he endeavoured to ascertain the abatement ot the waters;
and Lucian alludes to the animals of every species which he had
embarked with him, &c.
As to the coincidences of traditions and hypotheses, by which
it has recently been sought to prove that the rupture of the
Thracian Bosphorus was the cause of the deluge of Deucalion,
and even of the opening of the Pillars of Hercules, by causing
the Euxine sea to discharge its waters into the Archipelago,
which were, prior to this event, much higher and more extended
than they have since been, it is needless to occupy ourselves in
detailing; since it has been ascertained by the observations of
M. Oilvier, that if the Black sea had been as high as is
supposed there would have been many channels for its waters,
by hills and plains not so high as the present shores of the
Bosphorus; and by those of M. le Comte Andreossy, that had
it fallen any day by this new
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