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Geochemical characteristics of hydrothermally altered black shales of the southern Oquirrh Mountains and relationships to Mercur-type gold deposits (OFR-161)By: P. N. Wilson and W. T. Parry Alteration of the Manning Canyon and Long Trail Shales in the southern Oquirrh Mountains has resulted in (1) oxidation of organic matter and pyrite; (2) replacement by phyllosilicates; (3) silicification; (4) porphyroblast growth; (5) fossil replacement...
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Wood Ranch thermal anomaly, Iron County, Utah (MP 91-4)By: H. P. Ross, R. E. Blackett, and M. A. Shubat Isolated locations within the Escalante Valley of southwestern Utah exhibit higher than normal ground-water temperatures. The sources of geothermal fluid, which cause the elevated temperatures, are not well understood. Because of this uncertainty...
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Guidelines for preparing hydrogeologic and soil reports addressing suitability for alternative wastewater disposal systems in Weber County, Utah (C-102)By: M. Lowe and D. Sorensen Many lots in Weber County presently cannot be developed because adverse site characteristics (such as soil that percolates outside of acceptable rate ranges or shallow ground water) make them unsuitable for conventional wastewater disposal systems (septic tank soil-absorption...
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Preliminary hydrogeologic framework characterization - ground-water resources along the western side of the northern Wasatch Range, eastern Box Elder County, Utah (C-101)By: H. A. Hurlow This report summarizes the bedrock geology of the western part of the northern Wasatch Range in eastern Box Elder County, Utah , and its relation to ground-water resources. The southern part of the northern Wasatch Range is herein informally designated...
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High-temperature geothermal resources of Utah (B-123)By: D. R. Mabey and K. E. Budding Numerous thermal springs and shallow wells in western Utah are near-surface evidence of geothermal systems containing heat energy that can be produced and put to beneficial use. The seven known geothermal systems in Utah that contain...
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