Tule Valley defines this arid landscape in western Utah, where isolated water sources and subtle terrain features provided the only reliable points of navigation. As documented in this 2011 survey, the area is characterized by sparse, intermittent hydrology, with the Coyote Spring standing out as a critical natural landmark on the western edge of the valley. The presence of the East Tule Bench Reservoir indicates modern efforts to manage and capture water in a region otherwise dominated by the dry elevations of the Coyote Knolls. This map reflects the quiet, unpopulated character of the Great Basin, where human infrastructure is limited to a few remote 4WD tracks and local roads traversing the desert floor between these isolated water points.
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This is the sole edition of this map. No revisions or reprints were ever made.
1908 · Fish Springs
USGS Topo · 1:250,000
1910 · Fish Springs
USGS Topo · 1:250,000
1953 · Delta
USGS Topo · 1:250,000
1958 · Delta
USGS Topo · 1:250,000
1959 · Cowboy Pass
USGS Topo · 1:62,500
1960 · Granite Mountain
USGS Topo · 1:62,500
1962 · Delta
USGS Topo · 1:250,000
1967 · Sand Pass
USGS Topo · 1:24,000
1967 · Sand Pass SE
USGS Topo · 1:24,000
1972 · Swasey Peak SW
USGS Topo · 1:24,000