Adamsville serves as the focal point of this western Utah survey, situated at the confluence of the Beaver River and the northern reaches of the Minersville Reservoir. The landscape transition is stark, moving from the irrigated flats served by the Furnace Ditch and the Adamsville Bench into the steep, spring-fed elevations of the Mineral Mountains. Genealogists will find the Adamsville Cem clearly marked just east of the main settlement along E Main St. Higher elevations to the west and north are defined by numerous named features such as Harkley Mtn, Soldier Pass, and Granite Peak Reservoir. The distribution of water sources like Rock Corral Spring and Dripping Spring highlights the historical importance of localized hydrology for ranching and travel in this arid terrain, while the rugged drainage patterns of Lincoln Gulch and Granite Canyon reveal the complex topography surrounding the community.
39 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.
1885 · Beaver
USGS Topo · 1:250,000
1953 · Minersville
USGS Topo · 1:24,000
1953 · Cave Canyon
USGS Topo · 1:24,000
1953 · Richfield
USGS Topo · 1:250,000
1958 · Richfield
USGS Topo · 1:250,000
1958 · Minersville
USGS Topo · 1:62,500
1958 · Beaver
USGS Topo · 1:62,500
1958 · Adamsville
USGS Topo · 1:62,500
1958 · Ranch Canyon
USGS Topo · 1:24,000
1971 · Greenville Bench
USGS Topo · 1:24,000