Massive erratics left by ice-age Rhone Glacier near Solothurn, Switzerland. The two large erratics contain granite from the Mont Blanc area. Both rest on a pedestal of limestone about 40 cm high. The pedestal formed because the erratics protect the underlying limestone bedrock from precipitation and, therefore, erosion.
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Details
Creative#:
TOP25487883
Source:
達志影像
Authorization Type:
RM
Release Information:
須由TPG 完整授權
Model Release:
No
Property Release:
No
Right to Privacy:
No
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