Mechanics of a small landslide block, Wattener Lizum, Austria
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.
|Publication Subtype||Journal Article|
|Title||Mechanics of a small landslide block, Wattener Lizum, Austria|
|Series title||GSA Bulletin|
|Contributing office(s)||Geology, Minerals, Energy, and Geophysics Science Center|
|Other Geospatial||Wattener Lizum|
|Google Analytics Metrics||Metrics page|