
Whistler Mountain dominates the western half of this Nevada landscape, transitioning sharply into the wide, flat expanse of Diamond Valley to the east. The terrain is defined by a sparse but essential network of water sources, including Stinking Spring, Hash Spring, and Trap Corral Spring, which likely served as critical hubs for regional livestock and travel. An Old RR Grade cuts through the southeastern corner of the valley, signaling the area's historical connection to early mining or transport infrastructure. The valley floor is dotted with numerous wells and a notable Slough, indicating a reliance on groundwater in this arid environment. Several prospects and a Gravel Pit appear along the mountain's lower slopes, documenting the persistent search for mineral wealth that characterized this part of Eureka County during the late 20th century.
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1926 · Roberts Mountains
USGS Topo · 1:250,000
1929 · Roberts Mountains
USGS Topo · 1:250,000
1949 · Garden Valley
USGS Topo · 1:62,500
1951 · Garden Valley
USGS Topo · 1:62,500
1953 · Eureka
USGS Topo · 1:62,500
1955 · Millett
USGS Topo · 1:250,000
1956 · Whistler Mtn
USGS Topo · 1:62,500
1956 · Ely
USGS Topo · 1:250,000
1957 · Diamond Springs
USGS Topo · 1:62,500
1959 · Ely
USGS Topo · 1:250,000