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This document summarizes the geological history and geotechnical properties of marine clays in Drammen, Norway. The clays were deposited as glaciers retreated after the last ice age, with late-glacial clays being fairly homogeneous and of low plasticity. As the climate warmed, post-glacial clays with higher plasticity and organic matter were deposited. Isostatic rebound continued to raise the land, changing the landscape from a fjord to a river valley. Various processes over time have changed the geotechnic

Author

Anonymous GnfGTw

Language

EN