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New Real-Time Landslide Monitoring System in Polish Carpathians Read chapter Read first chapter

2013 | OriginalPaper | Chapter

Resolving Landslide-Bedrock Interaction by Nanoseismic Monitoring

Authors : Marco Walter, Manfred Joswig

Published in: Landslide Science and Practice

Publisher: Springer Berlin Heidelberg

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Abstract

Applying high-resolution Nanoseismic Monitoring to different slope instabilities in the Alps, we were able to observe the existence of fracture processes that resolve the creeping of slope material into sequences of discrete ‘slide quake’ events. At Heumoes slope, Austria, the locations of slide quakes are clustered in the mid-part of the slope exhibiting lower displacement rates than the remaining slope. In contrast, at the mudslide in Super-Sauze, France, the epicenters of located slide quakes correlates well with areas of highest displacement rates. These different behaviors are caused by the completely different layout of bedrock topography which directly influences dilatation and stress relief within the slope material.

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previous chapter Rapid Assessment of Landslide Activity in Emilia Romagna Using GB-InSAR Short Surveys
next chapter SAR Interferometry for Landslides Risk Assessment at Local Scale: The Case Study of Castagnola (Northern Apennines, Italy)
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Metadata
Title
Resolving Landslide-Bedrock Interaction by Nanoseismic Monitoring
Authors
Marco Walter
Manfred Joswig
Copyright Year
2013
Publisher
Springer Berlin Heidelberg
Book
Landslide Science and Practice

Print ISBN: 978-3-642-31444-5

Electronic ISBN: 978-3-642-31445-2

Copyright Year: 2013

DOI
https://doi.org/10.1007/978-3-642-31445-2_52