The Geography of Strabo, Volume 1 (of 3): Literally Translated, with NotesStrabo
History
The Geography of Strabo, Volume 1 (of 3): Literally Translated, with Notes
Strabo
Geography -- Early works to 1800
we denominate springs and fountains, are by other channels drawn towards
the depths of the sea, and raise it, so as to produce a flood-tide; when
the expiration is sufficient, they leave off the course in which they
are then flowing, and again revert to their former direction, when that
again takes a change.[1294]
8. I cannot tell how it is that Posidonius, who describes the Phœnicians
as sagacious in other things, should here attribute [CAS. 173] to them
folly rather than shrewdness. The sun completes his revolution in the
space of a day and night, being a portion of the time beneath the earth,
and a portion of the time shining upon it. Now he asserts that the
motion of the sea corresponds with the revolution of the heavenly
bodies, and experiences a diurnal, monthly, and annual change, in strict
accordance with the changes of the moon. For [he continues] when the
moon is elevated one sign of the zodiac[1295] above the horizon, the sea
begins sensibly to swell and cover the shores, until she has attained
her meridian; but when that satellite begins to decline, the sea again
retires by degrees, until the moon wants merely one sign of the zodiac
from setting; it then remains stationary until the moon has set, and
also descended one sign of the zodiac below the horizon, when it again
rises until she has attained her meridian below the earth; it then
retires again until the moon is within one sign of the zodiac of her
rising above the horizon, when it remains stationary until the moon has
risen one sign of the zodiac above the earth, and then begins to rise as
before. Such he describes to be the diurnal revolution. In respect to
the monthly revolution, [he says] that the spring-tides occur at the
time of the new moon, when they decrease until the first quarter; they
then increase until full moon, when they again decrease until the last
quarter, after which they increase till the new moon; [he adds] that
these increases ought to be understood both of their duration and speed.
In regard to the annual revolution, he says that he learned from the
statements of the Gaditanians, that both the ebb and flow tides were at
their extremes at the summer solstice: and that hence he conjectured
that they decreased until the [autumnal] equinox; then increased till
the winter solstice; then decreased again until the vernal equinox; and
[finally] increased until the summer solstice. But since these
revolutions occur twice in the four-and-twenty hours, the sea rising
twice and receding twice, and that regularly every day and night, how is
it that the filling and failing of the well do not frequently occur
during the ebb and flow of the tide? or if it be allowed that this does
often occur, why does it not do so in the same proportion? and if it
does so in the same proportion, how comes it that the Gaditanians are
not competent to observe what is of daily occurrence, while they are
nevertheless competent to the observing of revolutions which occur but
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