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.

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TOP25487905

Source:

達志影像

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RM

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須由TPG 完整授權

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