Pat O'Hara Mountain dominates this portion of Park County, serving as the high point for a drainage network that defines the local topography. This 2012 survey illustrates a landscape primarily shaped by water and elevation, where the Pat O'Hara Basin collects runoff that feeds into Pat O'Hara Cr and its various tributaries. The northern reaches are marked by the Natural Corral and the headwaters of Paint Cr, while the eastern terrain drops toward the distinct geological formation of Oxyoke Canyon. Human movement through this high country is limited to a few specific corridors, most notably Monument Hill Rd in the south. The arrangement of seasonal waterways like the Dry Fork and Blaine Cr suggests a region defined by sharp changes in relief and spring snowmelt, typical of the Wyoming high country.
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This is the sole edition of this map. No revisions or reprints were ever made.
1949 · Pat O'Hara Mountain
USGS Topo · 1:62,500
1949 · Cody
USGS Topo · 1:62,500
1950 · Clark
USGS Topo · 1:62,500
1950 · Deep Lake
USGS Topo · 1:62,500
1951 · Cody
USGS Topo · 1:62,500
1955 · Cody
USGS Topo · 1:250,000
1958 · Cody
USGS Topo · 1:250,000
1962 · Cody
USGS Topo · 1:250,000
1980 · Cody
USGS Topo · 1:100,000
1987 · Jim Mountain
USGS Topo · 1:24,000