Coevolving edge rounding and shape of glacial erratics: the case of Shap granite, UK
<p>The size distributions and the shapes of detrital rock clasts can shed light on the environmental history of the clast assemblages and the processes responsible for clast comminution. For example, mechanical fracture due to the stresses imposed on a basal rock surface by a body of flowing g...
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| Format: | Article |
| Language: | English |
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Copernicus Publications
2024-02-01
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| Series: | Earth Surface Dynamics |
| Online Access: | https://esurf.copernicus.org/articles/12/381/2024/esurf-12-381-2024.pdf |