
Snake River canyon walls define this stretch of Idaho, where the porous volcanic rock releases an extraordinary volume of water at Thousand Springs. This 1949 survey illustrates the mid-century development of the region's unique geothermal and hydraulic resources. The Banbury Natatorium and nearby Hot Water Wells signify the era's commercial interest in natural hot springs, while the Powerhouse near the springs captures the industrial harnessing of the river's descent. In the higher agricultural lands, the Lucerne School serves the rural community of Melon Valley. The terrain is marked by dramatic geological formations like Box Canyon and Blind Canyon, which feed into the main canyon alongside Salmon Falls Creek. Navigation and irrigation are prominent themes, evidenced by the numerous ditches and the turbulent waters of Devil's Washbowl Falls and Kanaka Rapids.
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7 editions found
1949 · Thousand Springs
USGS Topo · 1:24,000
1949 · Tuttle
USGS Topo · 1:24,000
1949 · Hagerman
USGS Topo · 1:24,000
1950 · Hagerman
USGS Topo · 1:24,000
1950 · Niagara Springs
USGS Topo · 1:24,000
1950 · Jerome
USGS Topo · 1:62,500
1951 · Thousand Springs
USGS Topo · 1:24,000
1951 · Tuttle
USGS Topo · 1:24,000
1951 · Clover
USGS Topo · 1:24,000
1954 · Thousand Springs
USGS Topo · 1:24,000