Camels Back Ridge dominates this northern section of the Great Salt Lake Desert, where high desert elevations meet the historical traces of ancient geography. The topographic survey documents a transition from the rising slopes of the ridge and the isolated peaks of the Simpson Buttes to the low-lying flats defined by the Old River Bed. This waterway trace represents a significant geological corridor through Tooele County, marking where prehistoric waters once flowed across the basin floor. Infrastructure is minimal in this arid landscape, primarily limited to the rugged Simpson Buttes Rd and the local route identified as Tc02854, which navigate the open terrain between these prominent landforms.
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1885 · Sevier Desert
USGS Topo · 1:250,000
1885 · Tooele Valley
USGS Topo · 1:250,000
1908 · Fish Springs
USGS Topo · 1:250,000
1910 · Fish Springs
USGS Topo · 1:250,000
1953 · Dugway Range NE
USGS Topo · 1:24,000
1953 · Dugway Range
USGS Topo · 1:62,500
1953 · Tooele
USGS Topo · 1:250,000
1953 · Delta
USGS Topo · 1:250,000
1954 · Dugway Proving Ground SE
USGS Topo · 1:24,000
1954 · Dugway Proving Ground NE
USGS Topo · 1:24,000