
The Schell Creek Range dominates the eastern half of this terrain, where water sources like Sidehill Spring, Jasper Spring, and Cris Spring provide critical relief in the arid Lincoln County landscape. To the west, the land falls away into the Cave Valley (Depression), a vast basin defined by sparse landmarks and an emphasis on industrial and ranching infrastructure. This 1970s survey captures the region's utilitarian development, showing an Aqueduct and Water Tank positioned to manage limited water resources, alongside evidence of mineral exploration such as a Drill Hole and Gravel Pit. The presence of Ruins and a network of Jeep Trails cutting through the foothills suggests a long history of human passage and temporary habitation in these high-elevation valleys. On the far eastern edge, the Muleshoe Valley begins to unfold, emphasizing the corrugated nature of this Great Basin environment.
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This is the sole edition of this map. No revisions or reprints were ever made.
1956 · Lund
USGS Topo · 1:250,000
1960 · Lund
USGS Topo · 1:250,000
1969 · Shingle Pass
USGS Topo · 1:24,000
1969 · Shingle Pass SE
USGS Topo · 1:24,000
1971 · Cave Valley Well
USGS Topo · 1:24,000
1971 · Sidehill Pass
USGS Topo · 1:24,000
1971 · Silver King Well
USGS Topo · 1:24,000
1973 · Grassy Mtn
USGS Topo · 1:24,000
1973 · Dutch John Mtn
USGS Topo · 1:24,000
1978 · Milk Ranch Spring
USGS Topo · 1:24,000