Spring Valley dominates the western half of this Lincoln County landscape, showing a broad alluvial expanse that contrasts sharply with the verticality of the Limestone Hills to the east. The geography is defined by significant drainage and transit features, including the eponymous Wells Summit and the carved path of Daves Canyon. This area of eastern Nevada serves as a textbook example of Basin and Range morphology, where the flat valley floor meets the steep, north-south trending ridges. Small intermittent water features like Hyde Wash illustrate the arid hydrology of the region. The map preserves the township and range grid system across several sections, including t9n r68e and t8n r69e, providing a clear record of land division in this part of the state during the early 21st century.
11 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.
1956 · Lund
USGS Topo · 1:250,000
1960 · Lund
USGS Topo · 1:250,000
1972 · Rosencrans Knolls
USGS Topo · 1:24,000
1972 · Hyde Well
USGS Topo · 1:24,000
1972 · Big Springs
USGS Topo · 1:24,000
1973 · Horse Corral Pass
USGS Topo · 1:24,000
1973 · Atlanta
USGS Topo · 1:24,000
1973 · Indian Springs Knolls
USGS Topo · 1:24,000
1973 · Red Ledges
USGS Topo · 1:24,000
1973 · Wells Summit
USGS Topo · 1:24,000