Distinguishing between debris flows and hyperconcentrated flows: an example from the eastern Swiss Alps

Author:

Calhoun Nancy C.12,Clague John J.1ORCID

Affiliation:

1. Department of Earth Sciences; Simon Fraser University; 8888 University Drive Burnaby BC V5A 1S6 Canada

2. Oregon Department of Geology & Mineral Industries; 800 NE Oregon Street, Suite 965 Portland OR 97232 USA

Funder

Natural Sciences and Engineering Research Council of Canada

Publisher

Wiley

Subject

Earth and Planetary Sciences (miscellaneous),Earth-Surface Processes,Geography, Planning and Development

Reference59 articles.

1. Large rockslides: Their causes and movement on internal sliding planes;Abele;Mountain Research and Development,1994

2. Rockslide movement supported by the mobilization of groundwater-saturated valley floor sediments;Abele;Zeitscrift für Geomorphology,1997

3. Die Wurzelregion der helvetischen Decken im Hinterrheingebiet und die Überschiebung der Bündnerschiefer südlich von Bonaduz;Arbenz;Verhanglungen der Naturforschenden Gesellschaft in Zürich,1910

4. Bagnold RA 1966 An Approach to the Sediment Transport Problem from General Physics

5. Calhoun NC 2015 LiDAR and Geomorphic Characterisation of Landslide-induced Liquefaction deposits in the Eastern Swiss Alps

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