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During filling of reservoir in Kauner Valley in Austria 20 million cu m of debris started to move; measurements and rheological investigations provide information about behavior of this unstable slope; conclusions can be evaluated as large-scale test; slope movements appeared in moraine; mass displacement which followed as consequence of reservoir-filling was compensated by corresponding slope movements; it was found that small reduction of shear stress was sufficient to bring movement to halt; this behavior can be traced back to resolidification of moraine; it was possible to control rate of sliding and to hold it within limits by filling reservoir in stages.
During filling of reservoir in Kauner Valley in Austria 20 million cu m of debris started to move; measurements and rheological investigations provide information about behavior of this unstable slope; conclusions can be evaluated as large-scale test; slope movements appeared in moraine; mass displacement which followed as consequence of reservoir-filling was compensated by corresponding slope movements; it was found that small reduction of shear stress was sufficient to bring movement to halt; this behavior can be traced back to resolidification of moraine; it was possible to control rate of sliding and to hold it within limits by filling reservoir in stages.
Dynamics of landslide produced by filling reservoir
Int Congress Large Dams
Breth, H. (author)
9th International Congress on Large Dams ; 1967 ; Turkey , Istanbul
1967
9 pages
Conference paper
English
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