Cliff Lake and Wade Lake dominate this high-elevation landscape within the Beaverhead National Forest, illustrating a complex network of glacial and volcanic terrain features. The survey highlights a series of distinctive geological benches and ridges, including Wade Lake Bench, Bogus Bench, and Island Ridge, which frame the deep basins of the lakes. The Madison River flows through the northeastern sector, joined by tributaries such as Butte Creek and Curlew Creek. Notable for its ecological preservation, the Cliff Lake RNA encompasses significant portions of the shoreline. Human infrastructure is limited to primitive access routes and ranch-related landmarks like Morgans Salt Box and Elk Meadows Ranch Rd, reflecting the area's primary use for timber management and wilderness recreation. The presence of numerous springs, such as 11S01E13DBB_01 Spring, underscores the vital hydrography that sustains the local ecosystem and the West Fork Madison River.
68 named features on this map. Tap any name to fly to it.
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This is the sole edition of this map. No revisions or reprints were ever made.
1950 · Cliff Lake
USGS Topo · 1:62,500
1950 · Hebgen Dam
USGS Topo · 1:62,500
1950 · Upper Red Rock Lake
USGS Topo · 1:62,500
1955 · Ashton
USGS Topo · 1:250,000
1958 · Ashton
USGS Topo · 1:250,000
1960 · Ashton
USGS Topo · 1:250,000
1964 · Targhee Peak
USGS Topo · 1:24,000
1964 · Henrys Lake
USGS Topo · 1:62,500
1988 · Granite Mountain
USGS Topo · 1:24,000
1988 · Hidden Lake Bench
USGS Topo · 1:24,000