A Sequence Of Glacial Deformation, Erosion, And Deposition At The Ice–Rock Interface During The Last Glaciation: Cranbrook, British Columbia, Canada
Abstract A comparison of bedrock fractures with orientation of structures and fabric in the overlying late Pleistocene basal till indicates a sequence of common glacial origin. The deformations in bedrock and till, and the deposition of the till layer, were accomplished by two glacial flows that wer...
| Published in: | Journal of Glaciology |
|---|---|
| Main Authors: | , , |
| Format: | Article in Journal/Newspaper |
| Language: | English |
| Published: |
Cambridge University Press (CUP)
1979
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| Subjects: | |
| Online Access: | http://dx.doi.org/10.1017/s0022143000029907 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000029907 |