The high-elevation landscape of the Ashley National Forest is defined here by the rugged transitions between Dyer Mtn and the Taylor Mountain Plateau. In the center of this terrain lies Bullionville, a location deeply tied to the region's mineral and water history, supported by nearby sources like Bullionville Spring and Iron Spring. The map documents a complex network of forest access routes, including the Ashley Driveway and the Pine Hollow Jade Ram Loop, which navigate the steep drainage systems of Big Brush Gorge and Dodds Hollow. Water management and natural springs are prominent throughout, ranging from the Oaks Park Reservoir in the northwest to secluded points like Parson City Spring and Gartell Spring, illustrating the critical role of water resources in this high-altitude Utah environment.
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This is the sole edition of this map. No revisions or reprints were ever made.
1885 · Ashley
USGS Topo · 1:250,000
1906 · Marsh Peak
USGS Topo · 1:125,000
1908 · Marsh Peak
USGS Topo · 1:125,000
1950 · Burnt Cabin Gorge
USGS Topo · 1:24,000
1950 · Dyer Mountain
USGS Topo · 1:24,000
1954 · Vernal
USGS Topo · 1:250,000
1958 · Vernal
USGS Topo · 1:250,000
1960 · Vernal
USGS Topo · 1:250,000
1963 · East Park Reservoir
USGS Topo · 1:24,000
1963 · Elk Park
USGS Topo · 1:24,000