Paleoseismology of Utah, Volume 19: Late Quaternary faulting in East Canyon Valley, Northern Utah (MP 10-5) Media Type:CD This guide leads you through

This guide leads you through New Mexico’s mountains

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The Harrisburg Junction quadrangle lies in the transition zone between the Colorado Plateau and Basin and Range physiographic provinces

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Paleoseismology of Utah, Volume 19: Late Quaternary faulting in East Canyon Valley, Northern Utah (MP 10-5) Media Type:CD This guide leads you throughBy: L. A. Piety, L. W. Anderson, and D. A. Ostenaa East Canyon Valley, a 25 km long by 5 km wide back valley, is on the eastern flank of the Wasatch Range about 25 km northeast of Salt Lake City and the Wasatch Front. Previous geologic mapping and the geomorphic expression of this north northeast trending valley suggest that East Canyon valley is a middle to late Cenozoic half graben bounded on the west by the East Canyon fault. The Main Canyon fault,