MLA 13-93 - Mineral Resource Investigation Of The Lime Creek Study Area, Camas And Elmore Counties, Idaho

The National Institute for Occupational Safety and Health (NIOSH)
Thomas J. Peters
Organization:
The National Institute for Occupational Safety and Health (NIOSH)
Pages:
31
File Size:
1792 KB
Publication Date:
Jan 1, 1993

Abstract

The Lime Creek study area lies 100 air km east of Boise, and 70 air km northeast of Mountain Home, Idaho. The eastern boundary of the 28,000-hectare, east-west-elongate study area lies 0.2 km west of the 3,077-m-high Smoky Dome. The area is mainly underlain by Cretaceous granitoid rocks of the Idaho batholith. No mineral resources were identified, but two mines and one prospect were found in the study area. At the President and the Last Chance mines, in the southwest corner of the study area, gold mineralization occurs along steeply dipping east-northeast-trending faults and associated quartz veins, and within adjacent Cretaceous granitic rock. The mineralized material is not rich enough to mine underground, and near surface, open-pit-mineable deposit areas could not be identified. The third prospect, the Ventura, is within altered pink granite of probable Tertiary age, but metal concentrations are very low. Geothermal activity was not observed within the study area, but hot springs do occur in the Vicinity. Bedrock observed is only suitable for the most basic high bulk and low end value applications, such as crushed aggregate. Numerous sources for crushed stone occur closer to markets. Alluvial concentrate (placer) samples did not contain free gold, and no substantial alluvial bars were seen; deposits were too small to contain resources.
Citation

APA: Thomas J. Peters  (1993)  MLA 13-93 - Mineral Resource Investigation Of The Lime Creek Study Area, Camas And Elmore Counties, Idaho

MLA: Thomas J. Peters MLA 13-93 - Mineral Resource Investigation Of The Lime Creek Study Area, Camas And Elmore Counties, Idaho. The National Institute for Occupational Safety and Health (NIOSH), 1993.

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