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Updated: May 9, 2025
During this period of depression and of subsequent re-emergence the wave-action of the Atlantic waters must have told severely on the coast and islands, wearing them into cliffs and escarpments, furrowing out channels and levelling obstructions. Such action has gone on down to the present day.
That the domain of the sea is being slowly extended over the land by incessant wave-action is well known; but in this freshly glaciated region the shores have been so short a time exposed to wave-action that they are scarcely at all wasted.
That the domain of the sea is being extended over the land by the wearing away of its shores, is well known, but in these icy regions of Alaska, and even as far south as Vancouver Island, the coast rocks have been so short a time exposed to wave-action they are but little wasted as yet.
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