Glaciotectonically deformed gneiss bedrock exposed in a former ice-marginal channel. The bedrock is strongly fractured and the distinct planes dipping to the left (glacierwards) are thrusts. |
Glaciotectonically deformed gneiss bedrock exposed in a former ice-marginal channel. The bedrock is strongly fractured and the distinct planes dipping to the left (glacierwards) are thrusts. |