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The subterranean channels of waters, like those which exist between
the air and the earth, are those which unceasingly wear away and
deepen the beds of their currents.
The origin of the sand in rivers (977. 978).
9
77.
A river that flows from mountains deposits a great quantity of large
stones in its bed, which still have some of their angles and sides,
and in the course of its flow it carries down smaller stones with
the angles more worn; that is to say the large stones become
smaller. And farther on it deposits coarse gravel and then smaller,
and as it proceeds this becomes coarse sand and then finer, and
going on thus the water, turbid with sand and gravel, joins the sea;
and the sand settles on the sea-shores, being cast up by the salt
waves; and there results the sand of so fine a nature as to seem
almost like water, and it will not stop on the shores of the sea but
returns by reason of its lightness, because it was originally formed
of rotten leaves and other very light things. Still, being
almost--as was said--of the nature of water itself, it afterwards,
when the weather is calm, settles and becomes solid at the bottom of
the sea, where by its fineness it becomes compact and by its
smoothness resists the waves which glide over it; and in this shells
are found; and this is white earth, fit for pottery.
798
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