Off-road vehicular destabilization of hill slopes: the major contributing factor to destructive debris flows in Ogden, Utah, 1979

John K. Nakata

doi:10.1007/978-1-4612-5454-6_18

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Off-road vehicular destabilization of hill slopes: the major contributing factor to destructive debris flows in Ogden, Utah, 1979

John K. Nakata

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Abstract

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.

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Source-reported bounding extent: 41.05087733907939° to 41.340215943707705° latitude; -112.12371826171875° to -111.84288024902344° longitude. This indicates report coverage, not an exact sampling location. View area on OpenStreetMap.

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John K. Nakata. 1983. Off-road vehicular destabilization of hill slopes: the major contributing factor to destructive debris flows in Ogden, Utah, 1979. https://doi.org/10.1007/978-1-4612-5454-6_18

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