Fig 3 LCC Nicoll

Figure 3 A classic U-shaped valley (dashed line) is legacy of the Pleistocene glaciers emanating from Little Cottonwood Canyon. Can you denote the trim line along the northern (left) side of the valley? The multi-million dollar homes depicted happen to straddle the Wasatch fault, which remains active today. Figure credit: Kathleen Nicoll 2007.

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Geomorphic Features in Little Cottonwood Canyon, UT
http://serc.carleton.edu/vignettes/collection/25465.html

Provenance
Kathleen Nicoll, University of Utah

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