
Moorman Spring (Hot) stands as a primary water source in this arid stretch of White River Valley, located within Nye County. The landscape is defined by the significant topographic variations between the floor of the valley and the elevated formations of The Cove and Lower Cove. Human presence in this high-desert environment is tied closely to scattered water points and precarious transit, represented by Riordans Well and Opu Well along the base of the mountains. A single Jeep Trail navigates the rugged transition between the valley floor and the higher basins, illustrating the era's reliance on specialized vehicles to access the Nevada interior for ranching or prospecting. The 1969 field check by the Geological Survey captures a moment before modern infrastructure altered these remote corridors.
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2 editions found
1956 · Lund
USGS Topo · 1:250,000
1960 · Lund
USGS Topo · 1:250,000
1964 · Currant
USGS Topo · 1:62,500
1964 · Forest Home
USGS Topo · 1:62,500
1969 · Sunnyside
USGS Topo · 1:24,000
1969 · Moorman Spring SE
USGS Topo · 1:24,000
1969 · Sunnyside NW
USGS Topo · 1:24,000
1969 · Moorman Spring NW
USGS Topo · 1:24,000
1969 · Moorman Spring NE
USGS Topo · 1:24,000
1980 · Duckwater
USGS Topo · 1:100,000