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U.S. Department of Energy
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National Uranium Resource Evaluation: Ritzville Quadrangle, Washington

Technical Report ·
OSTI ID:5367126

The Ritzville Quadrangle, Washington, was evaluated using criteria of the National Uranium Resource Evaluation program for identifying environments and delineating areas favorable for uranium deposits. Reconnaissance and detailed investigations included the evaluation of reported uranium occurrences, geochemical sampling, and field evaluation of aerial radiometric anomalies. Detailed investigations were conducted mainly in the northeastern corner of the quadrangle where there are two producing uranium mines, the Midnite and the Sherwood. The Midnite Mine uranium deposit is hosted by Precambrian metasedimentary rocks of the Togo Formation that are favorable for allogenic uranium deposits. Metasedimentary rocks of Paleozoic age are also favorable for allogenic deposits where they underlie a small area containing the Lowley Lease occurrence. The Sherwood uranium deposit is hosted by carbonaceous basal sedimentary rocks that probably correlate to the Eocene Sanpoil Volcanics and are favorable for sandstone-type deposits. Results of surface investigations outside these mining areas indicate environments favorable for magmatic-hydrothermal and authigenic deposits. Plutonic rocks in the quadrangle that are uranium enriched and show evidence of hydrothermal processes are favorable for magmatic-hydrothermal deposits. Plutonic rocks of the Mica Mountain area are judged favorable for both magmatic-hydrothermal and authigenic deposits.

Research Organization:
Bendix Field Engineering Corp., Grand Junction, CO (USA). Grand Junction Operations
DOE Contract Number:
AC13-76GJ01664
OSTI ID:
5367126
Report Number(s):
PGJ/F-041-82; ON: DE82018206
Country of Publication:
United States
Language:
English