Bartine Ranch serves as a primary point of reference in this arid region of central Nevada, where the landscape is defined by its vital water sources and significant relief. The presence of Hot Springs and Hot Spring Hill suggests geothermal activity that has long shaped the local geography. Several seasonal and perennial watercourses, including Coils Creek, Roberts Creek, and Slough Creek, descend from the higher elevations of Lone Mountain to feed into the broader Antelope Wash. These drainages, along with Lone Mountain Spring and Clover Spring, were historically essential for ranching operations and travelers navigating the high desert. The network of tracks and roads, such as Antelope Valley Rd, illustrates the continued reliance on these natural corridors through the Great Basin terrain.
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1926 · Roberts Mountains
USGS Topo · 1:250,000
1929 · Roberts Mountains
USGS Topo · 1:250,000
1955 · Millett
USGS Topo · 1:250,000
1956 · Bellevue Peak
USGS Topo · 1:62,500
1956 · Bartine Ranch
USGS Topo · 1:62,500
1956 · Antelope Peak
USGS Topo · 1:62,500
1956 · Whistler Mtn
USGS Topo · 1:62,500
1959 · Millett
USGS Topo · 1:250,000
1978 · Summit Mountain
USGS Topo · 1:100,000
1979 · Simpson Park Mtns
USGS Topo · 1:100,000