The Natural History of Pliny, Volume 1 (of 6)Pliny, the Elder
History
The Natural History of Pliny, Volume 1 (of 6)
Pliny, the Elder
Natural history -- Pre-Linnean works
[626] This circumstance is noticed by most of the ancients, as by
Aristotle, Meteor. ii. 1; by Seneca, Nat. Quæst. iv. 2; and by Strabo.
It has, however, no relation to the tide, but depends upon the quantity
of water transmitted into the Euxine by the numerous large rivers that
empty themselves into it.
[627] It has been suggested, with some plausibility, that the greater
height of the tides at this period will cause a greater quantity of
matter to be cast on shore. This circumstance is referred to by Seneca,
Nat. Quæst. iii. 26; and by Strabo.
[628] Alexandre observes on this supposed fact, “Algarum molles
quædam species intelligendæ sunt, quæ convolutæ et marcidæ in littus
ejiciuntur.” Lemaire, i. 432.
[629] It may cause some surprise to find that such an opinion has been
entertained even in modern times; but more correct observation has
shown it to be without foundation. Lemaire.
[630] “Spiritus sidus;” “Quod vitalem humorem ac spiritus in corporibus
rebusque omnibus varie temperet.” Hardouin in Lemaire, i. 433.
[631] “Terras saturet;” as Alexandre interprets it, “succo impleat;”
Lemaire.
[632] This circumstance is alluded to by Cicero, De Divin. ii. 33, and
by Horace, Sat. ii. 4, 30. It is difficult to conceive how an opinion
so totally unfounded, and so easy to refute, should have obtained
general credence.
[633] Lib. xviii. chap. 75.
[634] Aristotle, Meteor. ii. 1, remarks, that as the sun is continually
evaporating the water of the sea, it must eventually be entirely
dried up. But we have reason to believe, that all the water which is
evaporated by the solar heat, or any other natural process, is again
deposited in the form of rain or dew.
[635] “Terræ sudor;” according to Aristotle, Meteor. ii. 4: this
opinion was adopted by some of the ancients.
[636] The commentators discuss at considerable length the relative
merits of the three hypotheses here proposed, to account for the
saltness of the ocean; all of which are equally unfounded. See Hardouin
in Lemaire, i. 434, 435. Aristotle’s opinion on this subject is
contained in his Meteor.
[637] It is not easy to ascertain the origin of the very general
opinion respecting the peculiar physical action of the moon. The
alleged facts are, for the most part, without foundation, and I am
not aware of any circumstance which could, originally, have made them
a part of the popular creed of so many nations, ancient as well as
modern. Perhaps some of the effects which have been ascribed to the
specific action of the moon, may be explained by the lower temperature
and greater dampness of the air, during the absence of the sun.
[638] There appears to be some doubt respecting the history of the
person here referred to: according to the account of Hardouin, Fabianus
was a naturalist, who enjoyed a high reputation; he lived in the time
of Tiberius: see Lemaire, i. 188.
[639] This would be a depth of 3125 yards, not very far short of two
miles; see Adam’s Rom. Antiq. p. 503.
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