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This paper summarizes research on quick clays found in eastern Canada along the St. Lawrence and Ottawa Rivers. The clays have a similar mineral composition to other glacial marine clays but often have an unusually low salt content. There is evidence that overconsolidated deposits have strong rigid bonds between particles that break when loaded, which can lead to large volume changes or exceptional strength loss if drainage is not allowed. Studies have examined the clays

Author

kika bouba

Language

EN