Off-road vehicular destabilization of hill slopes: the major contributing factor to destructive debris flows in Ogden, Utah, 1979
By: John K. Nakata
Edited by: Robert H. Webb and Howard G. Wilshire
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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.
Study Area
| Publication type | Book chapter |
|---|---|
| Publication Subtype | Book Chapter |
| Title | Off-road vehicular destabilization of hill slopes: the major contributing factor to destructive debris flows in Ogden, Utah, 1979 |
| DOI | 10.1007/978-1-4612-5454-6_18 |
| Volume | Part IV |
| Year Published | 1983 |
| Language | English |
| Publisher | Springer |
| Description | 11 p. |
| Larger Work Type | Book |
| Larger Work Subtype | Monograph |
| Larger Work Title | Environmental Effects of Off-Road Vehicles |
| First page | 343 |
| Last page | 353 |
| Country | United States |
| State | Utah |
| City | Ogden |
| Online Only (Y/N) | N |
| Additional Online Files (Y/N) | N |