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Alpine topography of many high- and mid-latitude mountain ranges gives the qualitative impression that glaciers have been highly efficient erosive agents during the Quaternary. Glacial retreat leave slopes in an unstable state, highly susceptible to
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::2624340674dbf3300677a2755ddc5e82
https://doi.org/10.5194/egusphere-egu23-8531
https://doi.org/10.5194/egusphere-egu23-8531
