The Escalante River carves a complex, winding path through this corner of Southern Utah, defining the primary drainage for a landscape shaped by ancient water action. As it meanders southeast, it is joined by Moody Creek, a tributary that drains the northern reaches of the quadrangle. The topography is dominated by dramatic canyon systems, including the deeply etched profiles of Middle Moody Canyon and East Moody Canyon, which converge toward the river valley. Further south, the namesake Scorpion Gulch provides a narrow passage through the high desert terrain. This 2011 survey illustrates a region where the natural geology remains the primary feature, with no roads or settlements interrupting the intricate network of canyons and riparian corridors that characterize the Escalante basin.
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This is the sole edition of this map. No revisions or reprints were ever made.
1886 · Escalante
USGS Topo · 1:250,000
1886 · Henry Mountains
USGS Topo · 1:250,000
1892 · Henry Mountains
USGS Topo · 1:250,000
1953 · Circle Cliffs 4 NW
USGS Topo · 1:24,000
1953 · Mt Pennell 3 NW
USGS Topo · 1:24,000
1953 · Mt Pennell 3 SW
USGS Topo · 1:24,000
1953 · Circle Cliffs 4 NE
USGS Topo · 1:24,000
1953 · Circle Cliffs 4 SW
USGS Topo · 1:24,000
1953 · The Rincon
USGS Topo · 1:62,500
1953 · Hall Mesa
USGS Topo · 1:62,500