Description and origin of some talus‐foot debris accumulations, Aghla Mountains, Co. Donegal, Ireland
The morphology and site characteristics of talus‐foot debris accumulations in the Aghla Mountains, Ireland, suggest that these landforms are fossil protalus ramparts and talus‐derived rock glaciers. The ramparts are linear or arcuate ridges or benches located within 45 m of the talus foot. The rock...
| Published in: | Permafrost and Periglacial Processes |
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| Format: | Article in Journal/Newspaper |
| Language: | unknown |
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| Online Access: | https://doi.org/10.1002/ppp.3430040305 |