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Landslides in weakly cemented glaciolacustrine sediments, Morkill River valley, British Columbia
Download2001
Abstract: Slopes in weakly cemented glaciolacustrine sediments in the Morkill River valley in the Canadian Rocky Mountains stand at up to 70 degrees. Based on field and laboratory observations it appears that a contributing factor to instability is the softening of the soils by frost action and...
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