Halfway Summit stands as a central topographic marker in this desert landscape, where the Millard Co Beaver Co line divides the high-altitude terrain. The 2014 survey reveals a sparse network of water sources essential for survival in this arid region, including Beers Tunnel Spring and the Upper Pine Spring located near the base of the ridges. Transport through the area is largely dictated by the natural geology, with Ut-21 and various unnamed tracks winding around the Halfway Hills and through Beers Pass. Distinctive geological formations like The Needles and The Toad characterize the southwestern portion of the quadrangle, suggesting a landscape shaped by significant erosion. The mapping of Cottonwood Wash further illustrates the drainage patterns that define this interior basin environment between Antelope Valley and Pine Valley.
28 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.
1953 · Richfield
USGS Topo · 1:250,000
1958 · Richfield
USGS Topo · 1:250,000
1960 · Wah Wah Summit
USGS Topo · 1:62,500
1971 · Mountain Home Pass
USGS Topo · 1:24,000
1971 · Halfway Summit
USGS Topo · 1:24,000
1971 · Tunnel Spring
USGS Topo · 1:24,000
1971 · Sawtooth Peak
USGS Topo · 1:24,000
1971 · Lamerdorf Peak NW
USGS Topo · 1:24,000
1971 · Mormon Gap
USGS Topo · 1:24,000
1972 · Lopers Spring
USGS Topo · 1:24,000