
The Cerbat Mountains dominate the southwestern corner of this Arizona landscape, dropping sharply into the broad, arid expanse of the Hualapai Valley (Depression). Surveyed in the late 1960s, the terrain is defined by its drainage patterns, where seasonal waters carve through Cane Spring Wash, Twentysix Wash, and Truxton Wash. These desert washes radiate from the mountain foothills toward the low-lying valley center, illustrating the hydraulic character of the Mohave desert floor. Human presence is marked primarily by infrastructure for livestock and travel. Stockton Hill Road winds through the foothills, connecting various water sources critical to the region, including Big Well, Canyon Tank, and White Tank. This network of tanks and wells underscores the historical reliance on scattered water points for ranching and transit across this portion of the Cerbat range.
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2 editions found
1886 · Diamond Creek
USGS Topo · 1:250,000
1886 · Camp Mohave
USGS Topo · 1:250,000
1892 · Diamond Creek
USGS Topo · 1:250,000
1892 · Camp Mohave
USGS Topo · 1:250,000
1939 · Chloride
USGS Topo · 1:48,000
1942 · Camp Mohave
USGS Topo · 1:250,000
1944 · Chloride
USGS Topo · 1:62,500
1947 · Kingman
USGS Topo · 1:250,000
1948 · Kingman
USGS Topo · 1:250,000
1948 · Williams
USGS Topo · 1:250,000