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Recent acquisitions of light detection and ranging (lidar) data along the Wasatch Front, and the proliferation of Structure from Motion (SfM) software present exceptional opportunities for detailed analysis of the Wasatch fault zone (WFZ). Between the Salt Lake City (SLCS) and Provo segments (PS), the WFZ takes a 7-km left bend along the Fort Canyo...
Between the Provo and Salt Lake City segments the Wasatch fault is expressed as an 8-12 Km long network of discontinuous surface breaks. At both ends of the segment boundary the trend of the fault rotates by ~90 degrees, over a distance of ~2 km, from roughly N-S to E-W. The most prominent surface breaks (Holocene surface break apparent) range from...
