The Mineral Mountains define the central topography of this section of the Utah desert, where the peaks are bisected by Pinnacle Pass. This corridor serves as a significant natural landmark along the county line between Millard and Beaver counties. The landscape is shaped by the desert's hydrological patterns, featuring ephemeral drainages like Negro Mag Wash and Cunningham Wash that carry seasonal runoff. Water management for local use is evident in the presence of Salt Cove Reservoir and the more natural Hodgsen Pond to the north. These features, along with Salt Spring, indicate the historical reliance on scattered water sources in an otherwise arid environment. The road network, including TV Hill Rd and Geothermal Rd, suggests modern utility and infrastructure development amidst the high-altitude terrain of Antelope Mtn.
20 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.
1885 · Beaver
USGS Topo · 1:250,000
1953 · Richfield
USGS Topo · 1:250,000
1958 · Richfield
USGS Topo · 1:250,000
1958 · Beaver
USGS Topo · 1:62,500
1958 · Adamsville
USGS Topo · 1:62,500
1958 · Ranch Canyon
USGS Topo · 1:24,000
1962 · Cove Fort
USGS Topo · 1:62,500
1973 · Pinnacle Pass
USGS Topo · 1:24,000
1973 · Antelope Spring
USGS Topo · 1:24,000
1973 · Black Rock
USGS Topo · 1:24,000