Off-Road Vehicular Destabilization of Hill Slopes: The Major Contributing Factor to Destructive Debris Flows in Ogden, Utah, 1979
The Wasatch Mountains in northern Utah are a north-south trending range with steep slopes caused by faulting less than 10,000 years ago. Through the natural processes of rain, frost-wedging, gravity, and earthquakes these slopes are slowly being eroded. A geologic history of instability is recorded at the base of the range in the form of landslide deposits, debris flows, and rock-fall deposits.
KeywordsDebris Flow Diurnal Temperature Range Hill Slope Landslide Deposit Surge Tank
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