
Carico Lake Valley serves as the central drainage for this high-altitude basin, flanked by the Shoshone Range to the west and the Red Mountains to the east. The landscape is defined by its arid hydrology, most notably the seasonal Carico Lake (Dry) and several vital water sources like Elephant Head Spring, Placer Gulch Spring, and Wholey Spring No. 2. Evidence of resource exploration is scattered throughout the terrain in the form of multiple prospect sites, particularly along the slopes of Stone Cabin Basin and the eastern ridges. Deep incisions such as Stone Cabin Canyon and Rattlesnake Canyon illustrate the erosional patterns of the Great Basin, while Hall Creek meanders toward the valley floor, tracing the natural contours of this remote high-desert environment.
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This is the sole edition of this map. No revisions or reprints were ever made.
1926 · Roberts Mountains
USGS Topo · 1:250,000
1929 · Roberts Mountains
USGS Topo · 1:250,000
1932 · Sonoma Range
USGS Topo · 1:250,000
1939 · Sonoma Range
USGS Topo · 1:250,000
1955 · Millett
USGS Topo · 1:250,000
1955 · Winnemucca
USGS Topo · 1:250,000
1956 · Hall Creek
USGS Topo · 1:62,500
1958 · Winnemucca
USGS Topo · 1:250,000
1959 · Millett
USGS Topo · 1:250,000
1961 · The Cedars
USGS Topo · 1:62,500