
Spring Valley dominates this eastern Nevada landscape, where the wide basin floor meets the rising elevations of the Snake Range. The hydrology of the valley is defined by its namesake springs and intermittent drainages like Cleve Cr which flow from the higher terrain to the west. A notable geological feature, the Osceola Arch, sits on the western flank of the range, highlighting the unique limestone and quartzite formations of the district. Human infrastructure is relatively sparse, represented primarily by White Pine Co Road 37 and 6 50, which facilitate movement between the basin's ranching interests and the rugged eastern peaks. At the heart of the lower terrain, the namesake South Bastian Spring serves as a vital water source in this arid environment, illustrating the critical role of groundwater for settlement and livestock in the high desert.
13 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.
1952 · Ely
USGS Topo · 1:125,000
1956 · Ely
USGS Topo · 1:250,000
1959 · Ely
USGS Topo · 1:250,000
1959 · Sacramento Pass
USGS Topo · 1:62,500
1959 · Connors Pass
USGS Topo · 1:62,500
1959 · Schell Peaks
USGS Topo · 1:62,500
1963 · Ely
USGS Topo · 1:250,000
1981 · Majors Place
USGS Topo · 1:24,000
1981 · South Schell Peak
USGS Topo · 1:24,000
1981 · Cave Mountain
USGS Topo · 1:24,000