Studies on flow till in Denmark
- 1 December 1973
- Vol. 2 (4) , 213-231
- https://doi.org/10.1111/j.1502-3885.1973.tb00255.x
Abstract
Profiles with till and stratified meltwater sediments have been examined. Structural and morphological conditions indicate a deposition of till in the same environment as the stratified sediments. The till is interpreted as flow till which originated from considerable amounts of supraglacial material.Keywords
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