Abstract: Slope stability in the critical zone: The relative influence of long vs. short-time scale soil and vegetation properties on debris-flow initiation during a catastrophic rainfall. (2016 AGU Fall Meeting)

Slope stability in the critical zone: The relative influence of long vs. short-time scale soil and vegetation properties on debris-flow initiation during a catastrophic rainfall.

Francis K Rengers¹, Luke McGuire², Jeffrey A. Coe³, Jason W Kean³, Rex L Baum³, Dennis M Staley⁴ and Jonathan Godt⁵, (1)U.S. Geological Survey, Geologic Hazards Science Center, Golden, United States, (2)USGS Geologic Hazards Science Center, Golden, CO, United States, (3)USGS Central Region Offices Denver, Denver, CO, United States, (4)USGS, Baltimore, MD, United States, (5)U.S. Geological Survey, Denver, CO, United States
Scientific Team Name: USGS Landslide Hazards Team

Back to: The Architecture and Workings of Earth's Critical Zone II