Boudinage in rodonite dyke crossing serpentinite near Trockener Steg, Zermatt canton Valais, Switzerland. The outcrop has been polished by glacier ice flowing over it; the glacier recently has receded from this position. The orange colour is caused by the mineral hessonite, an orange-yellow type of garnet.
px | px | dpi | = | cm | x | cm | = | MB |
Details
Creative#:
TOP25487905
Source:
達志影像
Authorization Type:
RM
Release Information:
須由TPG 完整授權
Model Release:
N/A
Property Release:
N/A
Right to Privacy:
No
Same folder images: