Mechanics of a small landslide block, Wattener Lizum, Austria
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Abstract
A small landslide block left a trail about 81 meters long on an 11½-degree slope in the Tuxer Voralpen, Austria. The movement is explained in terms of fluid pressure mechanics; hypothetically, the requisite pore pressure was caused by the loading of contiguous saturated segments of the slide path during rapid sliding.
Study Area
Publication type | Article |
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Publication Subtype | Journal Article |
Title | Mechanics of a small landslide block, Wattener Lizum, Austria |
Series title | GSA Bulletin |
DOI | 10.1130/0016-7606(1962)73[1277:MOASLB]2.0.CO;2 |
Volume | 73 |
Issue | 10 |
Year Published | 1962 |
Language | English |
Publisher | GSA |
Contributing office(s) | Geology, Minerals, Energy, and Geophysics Science Center |
Description | 4 p. |
First page | 1277 |
Last page | 1280 |
Country | Austria |
Other Geospatial | Wattener Lizum |