
The Continental Divide terrain at the border of Park and Chaffee counties is defined by high alpine summits and intensive resource exploration. High points like West Buffalo Peak and East Buffalo Peak anchor the northern landscape within the Buffalo Peaks Wilderness, while Marmot Peak stands to the south. The drainage patterns of Buffalo Creek, Salt Creek, and several forks of Brush Creek suggest a landscape shaped by significant seasonal runoff, managed in part by an Aqueduct cutting through the San Isabel National Forest. Evidence of historical industry is scattered throughout the slopes, with numerous Mines and Prospect sites located near the Lenhardy Cutoff. These labels reflect the region's long-standing connection to mining and transit through the high passes between the Pike and San Isabel forests.
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This is the sole edition of this map. No revisions or reprints were ever made.
1889 · Leadville
USGS Topo · 1:125,000
1891 · Leadville
USGS Topo · 1:125,000
1942 · Leadville
USGS Topo · 1:125,000
1953 · Denver
USGS Topo · 1:250,000
1954 · Pueblo
USGS Topo · 1:250,000
1955 · Buena Vista
USGS Topo · 1:62,500
1956 · Garo
USGS Topo · 1:24,000
1956 · Antero Reservoir
USGS Topo · 1:24,000
1956 · Montrose
USGS Topo · 1:250,000
1957 · Denver
USGS Topo · 1:250,000