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had thawed away and left the general outline of
the country nearly the same as at present; but the
climate was still so much colder, or so much more
humid than at present, that the snows which fell
upon those hills in winter was greater in quantity
than the summer sun could thaw. There was thus
a local overflow of snow, which made its way
downwards, and, lodging in the valleys, there became
compressed, thawed, and refrozen into glacier ice,
which crept along, following every slope until it
reached the sea, on the shores of which its final
work is now so abundantly and curiously visible.
Glacial Farms. |
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