The periglacial origin of the drifts at Morfa‐Bychan, near Aberystwyth
Abstract The superficial deposits at Morfa‐bychan have previously been interpreted as deposited by Welsh ice. A reconsideration, including: stone orientation analysis, suggests however that they consist of screes and solifluction deposits with subordinate rain‐wash gravels, and a thin loess—the whol...
| Published in: | Geological Journal |
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| Main Authors: | , |
| Format: | Article in Journal/Newspaper |
| Language: | English |
| Published: |
Wiley
1967
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| Subjects: | |
| Online Access: | http://dx.doi.org/10.1002/gj.3350050212 https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fgj.3350050212 https://onlinelibrary.wiley.com/doi/pdf/10.1002/gj.3350050212 |
| Summary: | Abstract The superficial deposits at Morfa‐bychan have previously been interpreted as deposited by Welsh ice. A reconsideration, including: stone orientation analysis, suggests however that they consist of screes and solifluction deposits with subordinate rain‐wash gravels, and a thin loess—the whole laid down under periglacial conditions, when the Irish Sea ice no longer reached the area. There is no direct evidence for dating but their volume and field relations suggest they represent the deposits of the last glaciation. |
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