Death Valley National Park encompasses a significant portion of this high-desert landscape, where the sharp ridges of the Nelson Range meet the eastern slopes of the Inyo Mountains. The terrain is defined by dramatic elevation changes, notably at Conglomerate Mesa and the transition into Lee Flat. Transport through this arid corridor is traced via Cerro Gordo Rd and White Mountain Talc Rd, routes historically linked to the region's mineral extraction and early prospecting efforts. To the south, the Santa Rosa Hills overlook the northern reaches of the Mojave Desert, while seasonal drainage is marked by the winding path of Lee Wash and the descent of San Lucas Canyon. This survey documents a wilderness area where ancient geological formations and early industrial access roads remain the primary landmarks.
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1908 · Ballarat
USGS Topo · 1:250,000
1913 · Ballarat
USGS Topo · 1:250,000
1948 · Death Valley
USGS Topo · 1:250,000
1950 · Darwin
USGS Topo · 1:62,500
1950 · New York Butte
USGS Topo · 1:62,500
1950 · Ubehebe Peak
USGS Topo · 1:62,500
1951 · New York Butte
USGS Topo · 1:62,500
1951 · Darwin
USGS Topo · 1:62,500
1951 · Ubehebe Peak
USGS Topo · 1:62,500
1951 · Keeler
USGS Topo · 1:62,500