Lone Pine Peak serves as the high anchor for this central Idaho landscape, a high-desert environment defined by deep drainages and vital water sources. The topography is carved by systems like Malm Gulch and Spar Canyon, which drain into larger depressions such as Bradshaw Basin and the more localized Little Bradshaw Basin. This 2013 survey illustrates the critical nature of water in Custer County, documenting numerous specific points of interest for local historians and researchers, including Jenson Cabin Spring and Lower Bradshaw Spring. The area's transport network is limited to rugged paths like Malm Gulch Rd and Spar Canyon Rd, reflecting a landscape primarily used for ranching or resource management within the Germer Basin region. The mapping detail shows a complex network of seasonal drainages, such as Lone Pine Cr, highlighting the erratic hydrology of the Idaho backcountry.
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This is the sole edition of this map. No revisions or reprints were ever made.
1929 · Bayhorse
USGS Topo · 1:125,000
1957 · Challis
USGS Topo · 1:250,000
1960 · Challis
USGS Topo · 1:250,000
1963 · Challis
USGS Topo · 1:250,000
1963 · Bald Mountain
USGS Topo · 1:24,000
1963 · Bayhorse
USGS Topo · 1:24,000
1963 · Ziegler Basin
USGS Topo · 1:24,000
1963 · Little Antelope Flat
USGS Topo · 1:24,000
1963 · Clayton
USGS Topo · 1:62,500
1963 · Lone Pine Peak
USGS Topo · 1:62,500