Paleoseismology of Utah, Volume 15: Surficial-geologic reconnaissance and scarp profiling on the Colliston and Clarkston Mountain segments of the Wasatch fault zone, Box Elder County, Utah (SS-121) National and State Parks Sanpete and Emery Counties

Sanpete and Emery Counties

specific gravity

Teton Wilderness

Scenic byways are clearly marked for those wishing to take in the scenery by car

Bureau of Land Management as having oil shale development potential

Paleoseismology of Utah, Volume 15: Surficial-geologic reconnaissance and scarp profiling on the Colliston and Clarkston Mountain segments of the Wasatch fault zone, Box Elder County, Utah (SS-121) National and State Parks Sanpete and Emery CountiesBy: M. D. Hylland The Collinston and Clarkston Mountain segments, the northernmost two segments of the Wasatch fault zone in Utah, have been active during the Quaternary Period but show no evidence of Holocene surface faulting. The only fault scarps identified on Quaternary deposits along the Collinston segment are in the area of the Coldwater Canyon reentrant, which is at the segment boundary with the Brigham City segment to the south and includes