Skip to main content
U.S. Department of Energy
Office of Scientific and Technical Information

Thermal springs in the Salmon River basin, central Idaho

Technical Report ·
DOI:https://doi.org/10.2172/5224505· OSTI ID:5224505
The Salmon River basin within the study area occupies an area of approximately 13,000 square miles in central Idaho. Geologic units in the basin are igneous, sedimentary, and metamorphic rocks; however, granitic rocks of the Idaho batholith are predominant. Water from thermal springs ranges in temperature from 20.5/sup 0/ to 94.0/sup 0/ Celsius. The waters are slightly alkaline and are generally a sodium carbonate or bicarbonate type. Dissolved-solids concentrations are variable and range from 103 to 839 milligrams per liter. Estimated reservoir temperatures determined from the silicic acid-corrected silica, sodium-potassium-calcium, and sulfate-water isotope geothermometers range from 30/sup 0/ to 184/sup 0/ Celsius. Tritium concentrations in sampled thermal waters are near zero and indicate the waters are at least 100 years old. Stable-isotope data indicate it is unlikely that a single hot-water reservoir supplies hot springs in the basin. Thermal springs discharged at least 15,800 acre-feet of water in 1980. Associated convective heat flux is 2.7 x 10/sup 7/ calories per second.
Research Organization:
Geological Survey, Boise, ID (USA)
OSTI ID:
5224505
Report Number(s):
USGS-OFR-82-104; ON: DE84900487
Country of Publication:
United States
Language:
English