Hamlin Well serves as the central landmark in this high-desert basin near the border of Nevada and Utah. The landscape is defined by the drainage patterns of seasonal watercourses, including Wood-McCullough Creek in the northwest and the convergence of Miller Creek and Cobb Creek toward the south. To the north, the terrain rises toward the slopes of Miller Mountain, providing a stark contrast to the flatter alluvial plains where the well is situated. This 2012 survey illustrates the isolated nature of the region, where survival and settlement are dictated by the sparse water sources and topographic barriers of the Great Basin range-and-valley system.
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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
1956 · Lund
USGS Topo · 1:250,000
1958 · Richfield
USGS Topo · 1:250,000
1960 · Lund
USGS Topo · 1:250,000
1971 · Mountain Home Pass
USGS Topo · 1:24,000
1972 · Gleason Basin
USGS Topo · 1:24,000
1972 · Rosencrans Knolls
USGS Topo · 1:24,000
1972 · Hamlin Well
USGS Topo · 1:24,000
1972 · Miller Wash
USGS Topo · 1:24,000
1972 · Hyde Well
USGS Topo · 1:24,000