Abstract
The composition of erratic assemblages depends to a large extent on the specific gravity of the particular erratic boulders. The observed dependence may be explained as a result of a selection within an erratic assemblage by glacifluvial waters. The index is the ratio of the Aland erratics (acid - hence lighter ones) to the basic and ultrabasic ones (heavier). -after Author
Original language | English |
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Pages (from-to) | 65-69 |
Number of pages | 5 |
Journal | Quaternary Studies in Poland |
Volume | 1 |
State | Published - 1979 |