Southward across mouth of Mill Creek Canyon, Wasatch Range. Salt Lake County, Utah. No Date.
Summary
Southward across mouth of Mill Creek Canyon, Wasatch Range. The canyon wall is craggy; the face of the range, seen in profile, is smooth - the facet of an escarpment created by faulting. At base of the facet are cliffs of Bonneville shore line. The rock of the foreground at right is a quartzite breccia, the shear zone of the frontal fault of the range. Compare 1825 and 3461. Utah.n.d. Published as plate 4-B in U.S. Geological Survey. Professional paper 153. 1928.
Summary
Southward across mouth of Mill Creek Canyon, Wasatch Range. The canyon wall is craggy; the face of the range, seen in profile, is smooth - the facet of an escarpment created by faulting. At base of the facet are cliffs of Bonneville shore line. The rock of the foreground at right is a quartzite breccia, the shear zone of the frontal fault of the range. Compare 1825 and 3461. Utah.n.d. Published as plate 4-B in U.S. Geological Survey. Professional paper 153. 1928.
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