The Castle Peaks Wilderness Study Area (CDCA266) comprises approximately 45,000 acres in the northern New York Mountains, San Bernardino County, California. At the request of the Bureau of Land Management, 39,303 acres of the wilderness study area were studied. The area was investigated during 1982-1985 using combined geologic, geochemical, and geophysical methods. are considered preliminarily suitable for wilderness deignation. There are no mineral reserves or identified resources in the study area. Fluorspar, occurring in sparse veins, has moderate resource potential, as do silver and lead in fault zones, and gold and silver in sparse, high-grade veins and fault breccia. Each area of moderate resource potential encompasses less than one square mile. These same commodities have low resource potential in similar occurrences throughout much of the study area. In addition, there is low resource potential for gold in placer deposits, uranium in altered breccia and gouge, and rare-earth elements in pegmatite dikes. There is no resource potential for oil and gas resources over most of the study area, but the potential is unknown along its western margin. In this report, the area studied is referred to\"the wilderness study area\", or simply \"the study area.\"
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a plotting program for the IBM PC using Lotus 1-2-3 and a Hewlett-Packard plotter: U.S. Geological Survey Open-File Report 86-569, 10 p. :ill. ;28 cm., https://doi.org/10.3133/ofr86569A.","productDescription":"10 p. :ill. ;28 cm.","costCenters":[],"links":[{"id":149317,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1986/0569a/report-thumb.jpg"},{"id":44865,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1986/0569a/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49d6e4b07f02db5de579","contributors":{"authors":[{"text":"Schumann, R.R.","contributorId":14429,"corporation":false,"usgs":true,"family":"Schumann","given":"R.R.","email":"","affiliations":[],"preferred":false,"id":171850,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":15040,"text":"ofr86578 - 1986 - Strength measurements of heated illite gouge at low and high pore pressures","interactions":[],"lastModifiedDate":"2012-02-02T00:07:06","indexId":"ofr86578","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1986","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"86-578","title":"Strength measurements of heated illite gouge at low and high pore pressures","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr86578","usgsCitation":"Moore, D., Summers, R., and Byerlee, J., 1986, Strength measurements of heated illite gouge at low and high pore pressures: U.S. Geological Survey Open-File Report 86-578, 28 p. :ill. ;28 cm., https://doi.org/10.3133/ofr86578.","productDescription":"28 p. :ill. ;28 cm.","costCenters":[],"links":[{"id":149046,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1986/0578/report-thumb.jpg"},{"id":43953,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1986/0578/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b15e4b07f02db6a4c68","contributors":{"authors":[{"text":"Moore, Diane E. 0000-0002-8641-1075","orcid":"https://orcid.org/0000-0002-8641-1075","contributorId":106496,"corporation":false,"usgs":true,"family":"Moore","given":"Diane E.","affiliations":[],"preferred":false,"id":170466,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Summers, R.","contributorId":65483,"corporation":false,"usgs":true,"family":"Summers","given":"R.","email":"","affiliations":[],"preferred":false,"id":170464,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Byerlee, J.D.","contributorId":69982,"corporation":false,"usgs":true,"family":"Byerlee","given":"J.D.","affiliations":[],"preferred":false,"id":170465,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":15930,"text":"ofr8649 - 1986 - Results of the Second Western Task Force Round Robin Soil and Overburden Analysis Program","interactions":[],"lastModifiedDate":"2012-02-02T00:07:14","indexId":"ofr8649","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1986","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"86-49","title":"Results of the Second Western Task Force Round Robin Soil and Overburden Analysis Program","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr8649","usgsCitation":"Severson, R.C., and Fisher, S., 1986, Results of the Second Western Task Force Round Robin Soil and Overburden Analysis Program: U.S. Geological Survey Open-File Report 86-49, [2], 30 p. :ill. ;28 cm., https://doi.org/10.3133/ofr8649.","productDescription":"[2], 30 p. :ill. ;28 cm.","costCenters":[],"links":[{"id":149047,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1986/0049/report-thumb.jpg"},{"id":44900,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1986/0049/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a18e4b07f02db60558a","contributors":{"authors":[{"text":"Severson, R. 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It is a Cambrian sandstone that overlies the granites of the Precambrian basement complex. The basal sandstone is a poorly known resource defined only by 14 data points (wells) for the entire state of Tennessee. Because the aquifer occurs at depths of more than 5 ,500 feet below land surface, and is overlain by about 1,000 feet of low permeability Paleozoic carbonates and shales. Consequently vertical recharge to the aquifer is probably very small per unit area. Data from two sampling sites indicate that the basal sandstone aquifer has low porosity and permeability. The concentrations of dissolved solids in water from the basal sandstone aquifer range from less than 10,000 mg/L to more than 200,000 mg/L. It is believed that some of the values above 50 ,000 mg/L are due to contaminants from nearby disposal wells. This aquifer is not being used as a source of drinking water because of its great depth, the presence of shallower sources, suspected low yields, and possible concentrations of more than 10,000 mg/L dissolved solids. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82762","usgsCitation":"Brahana, J., Bradley, M.W., Macy, J.A., and Mulderink, D., 1986, Delineation and description of the regional aquifers of Tennessee; basal sandstone aquifer west of the Valley and Ridge Province: U.S. Geological Survey Open-File Report 82-762, iv, 21 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr82762.","productDescription":"iv, 21 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":146129,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0762/report-thumb.jpg"},{"id":40380,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0762/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adae4b07f02db685704","contributors":{"authors":[{"text":"Brahana, J. V.","contributorId":32926,"corporation":false,"usgs":true,"family":"Brahana","given":"J. 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A.","contributorId":10047,"corporation":false,"usgs":true,"family":"Macy","given":"J.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":165543,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Mulderink, Dolores","contributorId":64667,"corporation":false,"usgs":true,"family":"Mulderink","given":"Dolores","email":"","affiliations":[],"preferred":false,"id":165546,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":12226,"text":"ofr82338 - 1986 - Delineation and description of the regional aquifer systems of Tennessee; Cumberland Plateau aquifer system","interactions":[],"lastModifiedDate":"2012-02-02T00:06:50","indexId":"ofr82338","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1986","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"82-338","title":"Delineation and description of the regional aquifer systems of Tennessee; Cumberland Plateau aquifer system","docAbstract":"The Cumberland Plateau aquifer system consists of Pennsylvanian sandstones, conglomerates, shales, and coals which underlie the Cumberland Plateau in Tennessee. Major water-bearing zones occur within the sandstones and conglomerates in interconnected fractures. The water-bearing formations are separated by shale and siltstone that retard the vertical circulation of ground water, The Pennington Formation serves as the base of this aquifer system and is an effective confining unit, \r\n\r\nThe Cumberland Plateau aquifer system is an important water source for the Cumberland Plateau, wells and springs from the aquifer system supply most of the rural domestic and public drinking-water supplies, water from wells drilled into the Cumberland Plateau aquifer system is generally of good to excellent quality. Of the 32 water-quality analyses on file from this aquifer. only 2 had dissolved-solids concentrations greater than 500 milligrams per liter, and about three-fourths had less than 200 milligrams per liter dissolved solids, However, no samples from depths greater than 300 feet below land surface have been recorded. 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