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Mineralization, indicated by a downstream increase in dissolved-solids concentration, was due primarily to geothermal springs that gradually decreased in the percentage of calcium, increased in the percentage of magnesium and sodium, and caused fluctuating, but overall increasing percentage of fluoride, sulfate, and chloride. Resulting water quality in Mammoth Creek was similar to that of the springs forming Hot Creek. Eutrophication was observed in Twin Lakes and the reach of Hot Creek below the fish hatchery. Twin Lakes had floating mats of algae and a high dissolved-oxygen saturation of 147 percent at a pH of 9.2. Hot Creek had excessive aquatic vascular plant and algae growth, dissolved-oxygen saturations ranging from 65 to 200 percent, algal growth potential of 30 milligrams per liter, and nitrates and phosphates of 0.44 and 0.157 milligrams per liter. Sedimentation was noted in observations of bed-material composition showing the presence of fine material beginning at Sherwin Creek Road. Fecal contamination was indicated by fecal coliform counts of 250 colonies per 100 milliliters and fecal streptococcal counts greater than 1,000 colonies per 100 milliliters. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri844060","usgsCitation":"Setmire, J.G., 1984, Water-quality appraisal, Mammoth Creek and Hot Creek, Mono County, California: U.S. Geological Survey Water-Resources Investigations Report 84-4060, vi, 50 p. :ill., map ;28 cm., https://doi.org/10.3133/wri844060.","productDescription":"vi, 50 p. :ill., map ;28 cm.","costCenters":[],"links":[{"id":123560,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1984/4060/report-thumb.jpg"},{"id":58500,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1984/4060/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":58501,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1984/4060/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e48cce4b07f02db544519","contributors":{"authors":[{"text":"Setmire, J. G.","contributorId":16818,"corporation":false,"usgs":true,"family":"Setmire","given":"J.","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":201933,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":233,"text":"wsp2262 - 1984 - Selected papers in the hydrologic sciences 1984; July 1984","interactions":[],"lastModifiedDate":"2018-10-22T18:13:33","indexId":"wsp2262","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2262","title":"Selected papers in the hydrologic sciences 1984; July 1984","docAbstract":"The rapid, accurate measurement of the oxygen content of soil gas in the unsaturated zone or dissolved oxygen in soil water in the saturated zone can be useful in wetland vegetation studies. A method has been devised and tested in the Great Dismal Swamp, a wetland with fine silt-clay and organic soils, that appears to provide good results. A 60-milliliter sample of soil gas or water is withdrawn from permanently installed chambers at various depths in the soil profile. The oxygen concentration of air samples is measured with a specially constructed analyzer cell fitted to the polarographic oxygen electrode of a portable oxygen meter. The dissolved oxygen concentration of water samples is measured directly with the oxygen electrode while stirring the sample in a 32-milliliter glass bottle with a portable magnetic stirrer. Field tests with duplicate chamber installations showed that consistent results are obtained for soil gas and water.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wsp2262","usgsCitation":"1984, Selected papers in the hydrologic sciences 1984; July 1984: U.S. Geological Survey Water Supply Paper 2262, v, 66 p. :ill., maps ;28 cm., https://doi.org/10.3133/wsp2262.","productDescription":"v, 66 p. :ill., maps ;28 cm.","costCenters":[{"id":532,"text":"Pennsylvania Water Science Center","active":true,"usgs":true}],"links":[{"id":136506,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/2262/report-thumb.jpg"},{"id":24843,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/2262/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a03e4b07f02db5f83da","contributors":{"editors":[{"text":"Meyer, Eric L.","contributorId":58619,"corporation":false,"usgs":true,"family":"Meyer","given":"Eric","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":749260,"contributorType":{"id":2,"text":"Editors"},"rank":1}]}} ,{"id":48893,"text":"ofr84358M - 1984 - Color slides of preliminary geologic maps of the central Laramie Mountains, Albany and Platte counties, Wyoming","interactions":[],"lastModifiedDate":"2012-02-02T00:10:08","indexId":"ofr84358M","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","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":"84-358","chapter":"M","title":"Color slides of preliminary geologic maps of the central Laramie Mountains, Albany and Platte counties, Wyoming","language":"ENGLISH","doi":"10.3133/ofr84358M","usgsCitation":"Snyder, G.L., 1984, Color slides of preliminary geologic maps of the central Laramie Mountains, Albany and Platte counties, Wyoming: U.S. Geological Survey Open-File Report 84-358, 13 color slides, https://doi.org/10.3133/ofr84358M.","productDescription":"13 color slides","costCenters":[],"links":[{"id":162402,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b24e4b07f02db6ae840","contributors":{"authors":[{"text":"Snyder, George L.","contributorId":6843,"corporation":false,"usgs":true,"family":"Snyder","given":"George","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":238530,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":48894,"text":"ofr84376 - 1984 - Seismicity of the Arctic and adjoining regions, 1960-1983","interactions":[],"lastModifiedDate":"2012-02-02T00:10:08","indexId":"ofr84376","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","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":"84-376","title":"Seismicity of the Arctic and adjoining regions, 1960-1983","language":"ENGLISH","doi":"10.3133/ofr84376","usgsCitation":"Espinosa, A.F., and Michael, J.A., 1984, Seismicity of the Arctic and adjoining regions, 1960-1983: U.S. Geological Survey Open-File Report 84-376, 12 maps on 1 sheet : photocopy ; each 23 x 23 cm., sheet 87 x 109 cm., https://doi.org/10.3133/ofr84376.","productDescription":"12 maps on 1 sheet : photocopy ; each 23 x 23 cm., sheet 87 x 109 cm.","costCenters":[],"links":[{"id":162403,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":85731,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1984/0376/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a09e4b07f02db5fa8c6","contributors":{"authors":[{"text":"Espinosa, A. F.","contributorId":63782,"corporation":false,"usgs":true,"family":"Espinosa","given":"A.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":238532,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Michael, J. A.","contributorId":48567,"corporation":false,"usgs":true,"family":"Michael","given":"J.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":238531,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":18806,"text":"ofr84378 - 1984 - Reconnaissance geology of the Jibal Matalli Quadrangle, sheet 27/40 D, Kingdom of Saudi Arabia","interactions":[],"lastModifiedDate":"2015-09-07T14:41:52","indexId":"ofr84378","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","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":"84-378","title":"Reconnaissance geology of the Jibal Matalli Quadrangle, sheet 27/40 D, Kingdom of Saudi Arabia","docAbstract":"

The Jibal Matalli quadrangle lies along the northern boundary of the Arabian Shield about 90 km west-southwest of Ha'il. The quadrangle consists of about 45 percent Precambrian bedrock, 50 percent Quaternary deposits, and 5 percent sedimentary cover rocks. The Precambrian rocks include volcaniclastic and volcanic rocks that are slightly metamorphosed and various granitic plutons. The volcaniclastic and volcanic rocks are correlated with the Hulayfah group and the Hadn formation. The older Hulayfah is principally basalt of probably submarine origin that has locally been metamorphosed to greenschist facies. The Hadn is composed of submarine and subaerial deposits. These consist of volcanic-derived sandstone and siltstone and lesser amounts of chiefly rhyolite volcanic rocks. In most areas, the Hadn shows little in the way of metamorphic effects, but locally it too has been metamorphosed to greenschist facies. The volcanic rocks of the Hadn include ash-flow tuffs; some appear to be water-laid, but others are subaerial. The oldest pluton is diorite, those of intermediate age are monzogranite and syenogranite, and the youngest are alkali feldspar granites. The largest pluton, a metaluminous, low-calcium, biotite monzogranite, occupies much of the southern part of the quadrangle. The alkali feldspar granites are mostly peralkaline; the two youngest are particularly so. The latter two are located in the southwest and southeast corners of the quadrangle, and both contain arfvedsonite and kataphorite. The pluton in the southeast grades outward from a peraluminous core to a peralkaline, comenditic peripheral zone and is inferred to be genetically related to a spectacular, west-trending comendite dike swarm in the southern half of the quadrangle.

\n

Two northeast-trending buried right-lateral faults are inferred in the quadrangle; one in the southeast and one in the northwest. The one in the northwest probably offsets the comendite dike swarm about 3 km. This fault appears to be part of a broad right-lateral fault and flexure zone that juxtaposes the Hadn formation on the west against the Hulayfah group on the east.

","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr84378","usgsCitation":"Ekren, E.B., 1984, Reconnaissance geology of the Jibal Matalli Quadrangle, sheet 27/40 D, Kingdom of Saudi Arabia: U.S. Geological Survey Open-File Report 84-378, ii, 38 p. . :ill., maps ;28 cm., https://doi.org/10.3133/ofr84378.","productDescription":"ii, 38 p. . :ill., maps ;28 cm.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":152954,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1984/0378/report-thumb.jpg"},{"id":48176,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1984/0378/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":48177,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1984/0378/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"Saudi Arabia","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n 40,\n 27\n ],\n [\n 40,\n 28\n ],\n [\n 41,\n 28\n ],\n [\n 41,\n 27\n ],\n [\n 40,\n 27\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a6fe4b07f02db6409ad","contributors":{"authors":[{"text":"Ekren, E. B.","contributorId":14371,"corporation":false,"usgs":true,"family":"Ekren","given":"E.","middleInitial":"B.","affiliations":[],"preferred":false,"id":179775,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":32585,"text":"pp1309 - 1984 - Upper Proterozoic and Cambrian rocks in the Caborca region, Sonora, Mexico; physical stratigraphy, biostratigraphy, paleocurrent studies, and regional relations","interactions":[],"lastModifiedDate":"2012-02-02T00:09:17","indexId":"pp1309","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"1309","title":"Upper Proterozoic and Cambrian rocks in the Caborca region, Sonora, Mexico; physical stratigraphy, biostratigraphy, paleocurrent studies, and regional relations","language":"ENGLISH","doi":"10.3133/pp1309","usgsCitation":"Stewart, J., McMenamin, M., and Morales-Ramirez, J.M., 1984, Upper Proterozoic and Cambrian rocks in the Caborca region, Sonora, Mexico; physical stratigraphy, biostratigraphy, paleocurrent studies, and regional relations: U.S. Geological Survey Professional Paper 1309, 36 p., https://doi.org/10.3133/pp1309.","productDescription":"36 p.","costCenters":[],"links":[{"id":119432,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/1309/report-thumb.jpg"},{"id":60411,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/1309/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a1ae4b07f02db606649","contributors":{"authors":[{"text":"Stewart, John H.","contributorId":14383,"corporation":false,"usgs":true,"family":"Stewart","given":"John H.","affiliations":[],"preferred":false,"id":208734,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"McMenamin, M.A.S.","contributorId":92311,"corporation":false,"usgs":true,"family":"McMenamin","given":"M.A.S.","email":"","affiliations":[],"preferred":false,"id":208736,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Morales-Ramirez, J. M.","contributorId":69616,"corporation":false,"usgs":true,"family":"Morales-Ramirez","given":"J.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":208735,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":33814,"text":"b1382E - 1984 - Gold in the Black Pine mining district, southeast Cassia County, Idaho","interactions":[],"lastModifiedDate":"2022-09-21T18:18:30.070344","indexId":"b1382E","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":306,"text":"Bulletin","code":"B","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1382","chapter":"E","title":"Gold in the Black Pine mining district, southeast Cassia County, Idaho","docAbstract":"

No abstract available.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/b1382E","usgsCitation":"Brady, B., 1984, Gold in the Black Pine mining district, southeast Cassia County, Idaho: U.S. Geological Survey Bulletin 1382, iii, 15 p., https://doi.org/10.3133/b1382E.","productDescription":"iii, 15 p.","costCenters":[],"links":[{"id":407148,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_21489.htm","linkFileType":{"id":5,"text":"html"}},{"id":61723,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/1382e/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":167790,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/1382e/report-thumb.jpg"}],"country":"United States","state":"Idaho","county":"Cassia County","otherGeospatial":"Black Pine mining district","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n 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