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Updated: May 8, 2025
When long-weathered lands mantled with deep, well-oxidized waste are uplifted by a gradual movement of the earth's crust, and the mantle is rapidly stripped off by the revived streams, the uprise is recorded in wide deposits of red and yellow clays and sands upon the adjacent ocean floor.
The ice sheet, therefore, both scraped up the mantle of long-weathered waste which covered the coun try before its coming, and also ground heavily upon the sound rock underneath, and crushed and wore to rock flour the fragments which it carried. The color of unweathered till depends on that of the materials of which it is composed.
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