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. | |
Lizenzart: | Lizenzpflichtig |
Credit: | Science Photo Library / Alean, Dr. Juerg |
Bildgröße: | 7882 px × 4434 px |
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Eigentums-Rechte: | nicht erforderlich |
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