Author:
Cruden D.M.,Thomson S.,Kim H.J.,Peterson A.E.
Abstract
Observations over 20 years of three contiguous translational slides on the west wall of a 100 m deep valley in the Interior Plains document their evolution into advancing, composite, slow earth-flow earth-slides involving over a million cubic metres of displaced material. Colluvial deposits downslope of the apparent toes of the flows are moving. The reactivation of the abandoned slides in the Upper Cretaceous sedimentary rocks was likely triggered by years of higher than average precipitation following clearing of brush behind the crest of the slope. Back analysis is consistent with fully softened rock in the crowns of the slides and displaced materials at residual strength. Key words : landslide, rock-slide, earth-flow, earth-slide, Interior Plains.
Publisher
Canadian Science Publishing
Subject
Civil and Structural Engineering,Geotechnical Engineering and Engineering Geology
Cited by
7 articles.
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