Condensed Geology: Wyoming Mountains
Wyoming has mountians that originate from different kinds of tectonic processes.
![]() Figure 1 Normal Fault. Crust extension creates a steep fault; one side slides up, another down. Example: Teton Range. |
![]() Figure 2 Thick-skinned Compression. Crust compression pops up a block along a pair of steep faults. Example: Wind River Range. |
![]() Figure 3 Thin-skinned Compression. Crust compression creates a stack of slabs sliding along oblique faults. Example: Hoback Range. |
David R. Lageson, Darwin R. Spearing Roadside Geology of Wyoming (Roadside Geology Series) Mountain Press Publishing Company, 1991, ISBN: 0-87842-216-1
© November 26, 2014, Yuri Wolf / YuriKira.com