Date of Award:
Master of Science (MS)
Civil and Environmental Engineering
John D. Rice
John D. Rice
The Skunk Hollow Landslide (located 1 mile north of Mantua, UT along US-89) was instrumented with an automated monitoring system to aid in the determination of the triggering mechanism of slow moving landslides. Data was transmitted wirelessly through telecommunications to allow year-round, real-time monitoring of the site. Measurements were recorded and analyzed for the first season of landslide movement (fall 2009 to spring 2010) to better understand the correlations between snowmelt and movement initiation. Based on the first year of data, it appears that the Skunk Hollow Landslide is controlled by water infiltrating into the slide mass through cracks and fissures. Snowmelt is a function of many meteorological variables and future years of observation will create a better understanding of the interaction of these variables with landslide initiation.
Randall, Brent P., "A Study of Cause and Effect Relationships of Snowmelt-Induced Movement for the Skunk Hollow Landslide" (2010). All Graduate Theses and Dissertations. 740.
Copyright for this work is retained by the student. If you have any questions regarding the inclusion of this work in the Digital Commons, please email us at .