Although valley glaciations would have been extensive in the Late Pleistocene, most evidence of this has been severely modified due to fluvial erosion and talus deposition. The ski area consists of approximately 80% of this scree with the remaining cover being alpine vegetation.
Glacial influence would have been widespread in the Late Pleistocene, but most signs of this have been significantly altered due to riverine action and debris accumulation. The ski area primarily comprises roughly 80% scree, with the remaining cover being alpine plant life.