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Bouldery |
Also found in: Encyclopedia, Wikipedia, Hutchinson | 0.03 sec. |
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Ice-contact diamictons from the Fraser Glaciation are exposed over much of the central and northern strait, evident by the rough bouldery surface (Fig. The bouldery clay 'drift' was the not the product of a tropical ice sheet but deep weathering of igneous rocks and exfoliation of core stones (Branner, 1893; Fig. |
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