
Coyote Spring and its surrounding desert topography define this portion of Lincoln County, where water sources dictated the movement of both people and livestock. The expansive corridor of Coyote Wash dominates the central landscape, acting as a natural drainage artery that flows toward the south. This modern survey illustrates the persistent importance of isolated water points in the Great Basin, highlighting features like Stonewall Spring and the Upper Reservoir that anchor the otherwise arid terrain. To the southeast, the geography transitions into the broad expanse of Dry Lake Valley, a characteristic desert sink. The map provides a detailed view of the ephemeral water systems of the region, including Silverhorn Wash and Fairview Wash, showing how these intermittent flows have shaped the basin floor over time.
12 named features on this map. Tap any name to fly to it.
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This is the sole edition of this map. No revisions or reprints were ever made.
1885 · Pioche
USGS Topo · 1:250,000
1886 · Pioche
USGS Topo · 1:250,000
1915 · Bristol Range
USGS Topo · 1:62,500
1916 · Highland
USGS Topo · 1:62,500
1917 · Bristol Range
USGS Topo · 1:62,500
1918 · Highland
USGS Topo · 1:62,500
1954 · Caliente
USGS Topo · 1:250,000
1956 · Lund
USGS Topo · 1:250,000
1959 · Caliente
USGS Topo · 1:250,000
1960 · Lund
USGS Topo · 1:250,000