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,{"id":26057,"text":"wri854210 - 1985 - Cost effectiveness of the stream-gaging program in South Carolina","interactions":[],"lastModifiedDate":"2017-01-24T10:52:02","indexId":"wri854210","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1985","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"85-4210","title":"Cost effectiveness of the stream-gaging program in South Carolina","docAbstract":"The cost effectiveness of the stream-gaging program in South Carolina was documented for the 1983 water yr. Data uses and funding sources were identified for the 76 continuous stream gages currently being operated in South Carolina. The budget of $422,200 for collecting and analyzing streamflow data also includes the cost of operating stage-only and crest-stage stations. The streamflow records for one stream gage can be determined by alternate, less costly methods, and should be discontinued. The remaining 75 stations should be maintained in the program for the foreseeable future. The current policy for the operation of the 75 stations including the crest-stage and stage-only stations would require a budget of $417,200/yr. The average standard error of estimation of streamflow records is 16.9% for the present budget with missing record included. However, the standard error of estimation would decrease to 8.5% if complete streamflow records could be obtained. It was shown that the average standard error of estimation of 16.9% could be obtained at the 75 sites with a budget of approximately $395,000 if the gaging resources were redistributed among the gages. A minimum budget of $383,500 is required to operate the program; a budget less than this does not permit proper service and maintenance of the gages and recorders. At the minimum budget, the average standard error is 18.6%. The maximum budget analyzed was $850,000, which resulted in an average standard error of 7.6 %. (Author 's abstract)","language":"ENGLISH","publisher":"U.S. Geological Survey, WRD,","doi":"10.3133/wri854210","usgsCitation":"Barker, A., Wright, B., and Bennett, C., 1985, Cost effectiveness of the stream-gaging program in South Carolina: U.S. Geological Survey Water-Resources Investigations Report 85-4210, vi, 77 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri854210.","productDescription":"vi, 77 p. :ill., maps ;28 cm.","costCenters":[{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true}],"links":[{"id":54838,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1985/4210/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":123640,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1985/4210/report-thumb.jpg"}],"country":"United States","state":"South 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Carolina\",\"nation\":\"USA  \"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0de4b07f02db5fd24a","contributors":{"authors":[{"text":"Barker, A.C.","contributorId":42258,"corporation":false,"usgs":true,"family":"Barker","given":"A.C.","email":"","affiliations":[],"preferred":false,"id":195726,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wright, B.C.","contributorId":72416,"corporation":false,"usgs":true,"family":"Wright","given":"B.C.","email":"","affiliations":[],"preferred":false,"id":195727,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Bennett, C.S.","contributorId":13273,"corporation":false,"usgs":true,"family":"Bennett","given":"C.S.","email":"","affiliations":[],"preferred":false,"id":195725,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":20572,"text":"ofr85414 - 1985 - Publications of the U.S. Geological Survey, Water Resources Division, for Puerto Rico and the U.S. Virgin Islands, 1946-1985","interactions":[{"subject":{"id":20571,"text":"ofr84229 - 1984 - Publications of the U.S. Geological Survey, Water Resources Division, for Puerto Rico and the U.S. Virgin Islands, 1946-1984","indexId":"ofr84229","publicationYear":"1984","noYear":false,"title":"Publications of the U.S. Geological Survey, Water Resources Division, for Puerto Rico and the U.S. Virgin Islands, 1946-1984"},"predicate":"SUPERSEDED_BY","object":{"id":20572,"text":"ofr85414 - 1985 - Publications of the U.S. Geological Survey, Water Resources Division, for Puerto Rico and the U.S. Virgin Islands, 1946-1985","indexId":"ofr85414","publicationYear":"1985","noYear":false,"title":"Publications of the U.S. Geological Survey, Water Resources Division, for Puerto Rico and the U.S. Virgin Islands, 1946-1985"},"id":1}],"lastModifiedDate":"2012-02-02T00:07:36","indexId":"ofr85414","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1985","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":"85-414","title":"Publications of the U.S. Geological Survey, Water Resources Division, for Puerto Rico and the U.S. Virgin Islands, 1946-1985","language":"ENGLISH","publisher":"U.S. Dept. of the Interior, Geological Survey ;\r\nOpen-File Services Section, Western Distribution Branch,","doi":"10.3133/ofr85414","usgsCitation":"Quinones-Marquez, F., and Rivera, E., 1985, Publications of the U.S. Geological Survey, Water Resources Division, for Puerto Rico and the U.S. Virgin Islands, 1946-1985: U.S. Geological Survey Open-File Report 85-414, iii, 21 p. :ill. ;28 cm., https://doi.org/10.3133/ofr85414.","productDescription":"iii, 21 p. :ill. ;28 cm.","costCenters":[],"links":[{"id":152654,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1985/0414/report-thumb.jpg"},{"id":50093,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1985/0414/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a90e4b07f02db655eb7","contributors":{"authors":[{"text":"Quinones-Marquez, F.","contributorId":97501,"corporation":false,"usgs":true,"family":"Quinones-Marquez","given":"F.","affiliations":[],"preferred":false,"id":182871,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Rivera, Elba","contributorId":89558,"corporation":false,"usgs":true,"family":"Rivera","given":"Elba","email":"","affiliations":[],"preferred":false,"id":182870,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":16630,"text":"ofr85307 - 1985 - Proceedings of the Workshop on methods and techniques for digitizing cartographic data","interactions":[],"lastModifiedDate":"2012-02-02T00:07:12","indexId":"ofr85307","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1985","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":"85-307","title":"Proceedings of the Workshop on methods and techniques for digitizing cartographic data","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr85307","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1985, Proceedings of the Workshop on methods and techniques for digitizing cartographic data: U.S. Geological Survey Open-File Report 85-307, iv, 85 p. :ill. ;28 cm., https://doi.org/10.3133/ofr85307.","productDescription":"iv, 85 p. :ill. ;28 cm.","costCenters":[],"links":[{"id":149794,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1985/0307/report-thumb.jpg"},{"id":45669,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1985/0307/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9ee4b07f02db6603ce","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":528989,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":16454,"text":"ofr85567 - 1985 - Potential hydrologic effects of ground-water withdrawals from the Dakota Aquifer, southwestern Kansas","interactions":[{"subject":{"id":16454,"text":"ofr85567 - 1985 - Potential hydrologic effects of ground-water withdrawals from the Dakota Aquifer, southwestern Kansas","indexId":"ofr85567","publicationYear":"1985","noYear":false,"title":"Potential hydrologic effects of ground-water withdrawals from the Dakota Aquifer, southwestern Kansas"},"predicate":"SUPERSEDED_BY","object":{"id":2894,"text":"wsp2304 - 1989 - Potential hydrologic effects of ground-water withdrawals from the Dakota Aquifer, southwestern Kansas","indexId":"wsp2304","publicationYear":"1989","noYear":false,"title":"Potential hydrologic effects of ground-water withdrawals from the Dakota Aquifer, southwestern Kansas"},"id":1}],"supersededBy":{"id":2894,"text":"wsp2304 - 1989 - Potential hydrologic effects of ground-water withdrawals from the Dakota Aquifer, southwestern Kansas","indexId":"wsp2304","publicationYear":"1989","noYear":false,"title":"Potential hydrologic effects of ground-water withdrawals from the Dakota Aquifer, southwestern Kansas"},"lastModifiedDate":"2013-01-08T13:49:54","indexId":"ofr85567","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1985","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":"85-567","title":"Potential hydrologic effects of ground-water withdrawals from the Dakota Aquifer, southwestern Kansas","docAbstract":"A study was conducted to evaluate the effects of potential development of the Dakota aquifer on the layered aquifer system above Permian rocks in a 5,000 sq mi area of southwestern Kansas. Transmissivity of the Dakota aquifer, determined from analyses of pumping tests, ranges from 100 to 7,100 sq ft/day. Water in the Dakota aquifer is a calcium bicarbonate type water, similar to water in the High Plains aquifer, in the subcrop area. However, in areas distant from the subcrop, water in the Dakota aquifer is a sodium bicarbonate type water with dissolved solids concentrations in excess of 500 mg/L. Gradual declines in the potentiometric surface of the Dakota aquifer have occurred since the onset of pumpage in the 1960's; however, water levels in some wells have risen during the late 1970's. A digital computer model of 3-D groundwater flow was developed to simulate hydrologic conditions of a five-layer hydrologic system for 1975-82 conditions. The major components of the simulated 1975-82 water budget were well discharge from the High Plains aquifer and loss of ground water from storage in the High Plains aquifer. Although downward leakage from the High Plains aquifer in the study area represented only 18,000 acre-ft of the 1,365 ,000 acre-ft discharged from the High Plains aquifer during 1982 , it was a major source of inflow to the Dakota aquifer. Changes in storage in the Dakota aquifer in the study area during 1982 were about 5,000 acre-ft. A base-line projection was made using 1982 simulated hydraulic heads from the calibrated model and 1982 rates of pumpage from both the High Plains and the Dakota aquifers for comparison with eight additional projection simulations in which maximum pumpage from the Dakota aquifer at the end of the projections ranged from about 78,000 to 294,000 acre-ft/yr. The results from the projections indicate that: (1) pumpage from the Dakota aquifer will have a limited effect on hydraulic heads in the High Plains aquifer, (2) drawdown in the hydraulic heads in the Dakota aquifer will result in conversion of much of the Dakota aquifer to unconfined conditions, (3) change in storage will become the major water-budget component for the Dakota aquifer, (4) continuation of 1982 rates of withdrawal from the High Plains aquifer will result in dewatering of a substantial part of the aquifer in the study area. (Lantz-PTT)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr85567","usgsCitation":"Watts, K.R., 1985, Potential hydrologic effects of ground-water withdrawals from the Dakota Aquifer, southwestern Kansas: U.S. Geological Survey Open-File Report 85-567, x, 72 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr85567.","productDescription":"x, 72 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":149092,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1985/0567/report-thumb.jpg"},{"id":265398,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1985/0567/report.pdf"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1ae4b07f02db6a878b","contributors":{"authors":[{"text":"Watts, Kenneth R.","contributorId":43783,"corporation":false,"usgs":true,"family":"Watts","given":"Kenneth","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":172878,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":16492,"text":"ofr85182 - 1985 - Statistical summary of water-quality data collected from selected wells and springs in the Edwards Aquifer near San Antonio, Texas","interactions":[],"lastModifiedDate":"2016-08-12T13:33:42","indexId":"ofr85182","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1985","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":"85-182","title":"Statistical summary of water-quality data collected from selected wells and springs in the Edwards Aquifer near San Antonio, Texas","docAbstract":"<p>Statistical summaries of available water-quality data collected from 90 wells and 3 springs in the Edwards aquifer near San Antonio, Texas, are presented. The statistical summaries provide information on the range in values for each water-quality constituent as well as the mean value, the standard deviation about the mean; and for those constituents with five or more analyses, the percentage of observations in which values were equal to or less than the specified values are presented.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Austin, TX","doi":"10.3133/ofr85182","usgsCitation":"Wells, F.C., 1985, Statistical summary of water-quality data collected from selected wells and springs in the Edwards Aquifer near San Antonio, Texas: U.S. Geological Survey Open-File Report 85-182, Report: iii, 162 p.; Plate: 17.63 x 11.67 inches, https://doi.org/10.3133/ofr85182.","productDescription":"Report: iii, 162 p.; Plate: 17.63 x 11.67 inches","numberOfPages":"163","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":45458,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1985/0182/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":45459,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1985/0182/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":148810,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1985/0182/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49dce4b07f02db5e12c9","contributors":{"authors":[{"text":"Wells, Frank C.","contributorId":80664,"corporation":false,"usgs":true,"family":"Wells","given":"Frank","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":172938,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":16510,"text":"ofr85677 - 1985 - Hydrologic hazards in karst terrain (water fact sheet)","interactions":[],"lastModifiedDate":"2012-02-02T00:07:09","indexId":"ofr85677","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1985","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":"85-677","title":"Hydrologic hazards in karst terrain (water fact sheet)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr85677","usgsCitation":"Whallon, A., and Crawford, N., 1985, Hydrologic hazards in karst terrain (water fact sheet): U.S. Geological Survey Open-File Report 85-677, 2 p. :ill. ;28 cm., https://doi.org/10.3133/ofr85677.","productDescription":"2 p. :ill. ;28 cm.","costCenters":[],"links":[{"id":148357,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1985/0677/report-thumb.jpg"},{"id":45487,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1985/0677/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a1ae4b07f02db606a8d","contributors":{"authors":[{"text":"Whallon, A.J.","contributorId":10663,"corporation":false,"usgs":true,"family":"Whallon","given":"A.J.","email":"","affiliations":[],"preferred":false,"id":172970,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Crawford, N.C.","contributorId":50779,"corporation":false,"usgs":true,"family":"Crawford","given":"N.C.","email":"","affiliations":[],"preferred":false,"id":172971,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":16552,"text":"ofr85345 - 1985 - Ground-water flow in the Central Valley, California","interactions":[],"lastModifiedDate":"2018-01-30T19:22:56","indexId":"ofr85345","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1985","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":"85-345","title":"Ground-water flow in the Central Valley, California","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr85345","usgsCitation":"Williamson, A.K., Prudic, D.E., and Swain, L.A., 1985, Ground-water flow in the Central Valley, California: U.S. Geological Survey Open-File Report 85-345, ix, 203 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr85345.","productDescription":"ix, 203 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":45543,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1985/0345/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":148865,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1985/0345/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aafe4b07f02db66cd8b","contributors":{"authors":[{"text":"Williamson, A. K.","contributorId":57872,"corporation":false,"usgs":true,"family":"Williamson","given":"A.","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":173049,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Prudic, David E. deprudic@usgs.gov","contributorId":3430,"corporation":false,"usgs":true,"family":"Prudic","given":"David","email":"deprudic@usgs.gov","middleInitial":"E.","affiliations":[{"id":465,"text":"Nevada Water Science Center","active":true,"usgs":true}],"preferred":true,"id":173047,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Swain, Li. A.","contributorId":28258,"corporation":false,"usgs":true,"family":"Swain","given":"Li.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":173048,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":16080,"text":"ofr85189 - 1985 - Selected hydrologic data from a wastewater spray disposal site on Hilton Head Island, South Carolina","interactions":[],"lastModifiedDate":"2016-12-14T14:09:09","indexId":"ofr85189","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1985","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":"85-189","title":"Selected hydrologic data from a wastewater spray disposal site on Hilton Head Island, South Carolina","docAbstract":"This study presents data collected during a study of the effects on the water table aquifer from wastewater application at rates of up to 5 inches per week on a wastewater spray disposal site on Hilton Head Island, South Carolina. The study was conducted from April 1982 through December 1983. The disposal site covers approximately 14 acres. Water level and water quality data from organic, inorganic, and nutrient analyses from the water table aquifer to a depth of 30 ft and similar water quality data from the wastewater treatment plant are included. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr85189","usgsCitation":"Speiran, G., and Belval, D., 1985, Selected hydrologic data from a wastewater spray disposal site on Hilton Head Island, South Carolina: U.S. Geological Survey Open-File Report 85-189, v, 34 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr85189.","productDescription":"v, 34 p. :ill., maps ;28 cm.","costCenters":[{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true}],"links":[{"id":150331,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1985/0189/report-thumb.jpg"},{"id":45012,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1985/0189/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"South Carolina","otherGeospatial":"Hilton Head Island","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -80.94932556152344,\n              32.01273389791075\n            ],\n            [\n              -80.94932556152344,\n              32.34574191355548\n            ],\n            [\n              -80.57441711425781,\n              32.34574191355548\n            ],\n            [\n              -80.57441711425781,\n              32.01273389791075\n            ],\n            [\n              -80.94932556152344,\n              32.01273389791075\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a06e4b07f02db5f8977","contributors":{"authors":[{"text":"Speiran, G. K.","contributorId":83534,"corporation":false,"usgs":true,"family":"Speiran","given":"G. K.","affiliations":[],"preferred":false,"id":172204,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Belval, D.L.","contributorId":52186,"corporation":false,"usgs":true,"family":"Belval","given":"D.L.","affiliations":[],"preferred":false,"id":172203,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":19594,"text":"ofr85327 - 1985 - Background hydrologic information in potential lignite mining areas in north-central Mississippi, August 1984","interactions":[],"lastModifiedDate":"2012-02-02T00:07:29","indexId":"ofr85327","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1985","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":"85-327","title":"Background hydrologic information in potential lignite mining areas in north-central Mississippi, August 1984","docAbstract":"The U.S. Geological Survey, in cooperation with the Mississippi Department of Natural Resources, Bureau of Geology, is conducting a hydrologic data collection program in potential lignite-producing areas in Mississippi. During the last two weeks of August 1984, hydrologic data were collected at 15 stream sites that drain potential lignite mining areas in Lafayette, Calhoun, and Yalobusha Counties. Main channel widths ranged from approximately 60 feet at three streams (Coon Creek near Toccopula, Muckaloon Creek near Tula, and Hurricane Creek near Velma) to approximately 120 feet at two streams (Potlockney Creek near Tula, and Savannah Creek near Bruce). Maximum water depths ranged from less than 1.0 foot at most streams to over 5.0 feet at sites on Potlockney Creek near Tula and McGill Creek near Sarepta. Stream discharge ranged from 0.32 cubic feet per second in Persimmon Creek near Bruce to 18.5 cubic feet per second in Puskus Creek near Etta. The specific conductance of stream water ranged from 25 to 160 microsiemens and dissolved solids concentrations ranged from 22 to 91 mg/L (milligrams per liter). Most major ion concentrations were less than 10 mg/L with the exception of calcium (11 mg/L), sodium (12 mg/L) and sulfate (18 mg/L) in the water of Persimmon Creek near Bruce. Dissolved oxygen concentrations were greater than 5.0 mg/L at all but one site. Turbidity values were generally less than 50 units. Nitrate plus nitrite concentrations were equal to or less than 0.10 mg/L in all streams except in Potlockney Creek near Tula where the concentration was 0.11 mg/L. Copper and selenium concentrations in the water at all sampling sites ranged from below the detection limits (1 microgram/g) to 4 micrograms/g (micrograms per gram) and mercury concentrations in bottom material samples ranged from less than 0.01 microgram/g to 0.15 microgram/g. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nOpen-File Services Section, Western Distribution Branch, U.S. Geological Survey [distributor],","doi":"10.3133/ofr85327","usgsCitation":"Kalkhoff, S., 1985, Background hydrologic information in potential lignite mining areas in north-central Mississippi, August 1984: U.S. Geological Survey Open-File Report 85-327, iv, 18 p. :ill. ;29 cm., https://doi.org/10.3133/ofr85327.","productDescription":"iv, 18 p. :ill. ;29 cm.","costCenters":[],"links":[{"id":151969,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1985/0327/report-thumb.jpg"},{"id":49062,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1985/0327/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a80e4b07f02db6496b9","contributors":{"authors":[{"text":"Kalkhoff, S. J.","contributorId":28967,"corporation":false,"usgs":true,"family":"Kalkhoff","given":"S. J.","affiliations":[],"preferred":false,"id":181181,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":18242,"text":"ofr85405 - 1985 - Water-quality data from selected surface coal mines in West Virginia","interactions":[],"lastModifiedDate":"2012-02-02T00:07:26","indexId":"ofr85405","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1985","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":"85-405","title":"Water-quality data from selected surface coal mines in West Virginia","language":"ENGLISH","publisher":"U.S. Geological Survey, WRD ;\r\nCopies of this report can be purchased from Open-File Services Section, Western Distribution Branch,","doi":"10.3133/ofr85405","usgsCitation":"Bragg, R., 1985, Water-quality data from selected surface coal mines in West Virginia: U.S. Geological Survey Open-File Report 85-405, i, 76 p. :map ;28 cm., https://doi.org/10.3133/ofr85405.","productDescription":"i, 76 p. :map ;28 cm.","costCenters":[],"links":[{"id":150797,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1985/0405/report-thumb.jpg"},{"id":47599,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1985/0405/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e3e4b07f02db5e56e4","contributors":{"authors":[{"text":"Bragg, R.L.","contributorId":67905,"corporation":false,"usgs":true,"family":"Bragg","given":"R.L.","email":"","affiliations":[],"preferred":false,"id":178766,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":21033,"text":"ofr85332 - 1985 - Alaska index; streamflow and water-quality records to September 30, 1983","interactions":[],"lastModifiedDate":"2012-02-02T00:07:57","indexId":"ofr85332","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1985","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":"85-332","title":"Alaska index; streamflow and water-quality records to September 30, 1983","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nOpen-File Services Section [distributor],","doi":"10.3133/ofr85332","usgsCitation":"Still, P.J., and Jones, K.V., 1985, Alaska index; streamflow and water-quality records to September 30, 1983: U.S. Geological Survey Open-File Report 85-332, iv, 174 p. :maps ;28 cm., https://doi.org/10.3133/ofr85332.","productDescription":"iv, 174 p. :maps ;28 cm.","costCenters":[],"links":[{"id":155429,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1985/0332/report-thumb.jpg"},{"id":50624,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1985/0332/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae2e4b07f02db688dc9","contributors":{"authors":[{"text":"Still, Patsy J.","contributorId":27077,"corporation":false,"usgs":true,"family":"Still","given":"Patsy","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":183720,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Jones, Karen V.","contributorId":48996,"corporation":false,"usgs":true,"family":"Jones","given":"Karen","email":"","middleInitial":"V.","affiliations":[],"preferred":false,"id":183721,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":16702,"text":"ofr83943 - 1985 - Ground-water data, Green River basin, Wyoming","interactions":[],"lastModifiedDate":"2012-02-02T00:07:05","indexId":"ofr83943","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1985","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":"83-943","title":"Ground-water data, Green River basin, Wyoming","docAbstract":"Hydrologic and geologic data collected by the U.S. Geological Survey as part of energy-related projects in the Green River basin of Wyoming are compiled from the files of the Geological Survey and the Wyoming State Engineer as of 1977. The data include well and spring location, well depth, casing diameter, type of lifts, type of power, use of water, rock type of producing zone, owner, and discharge for more than 1,600 sites. Analyses for common chemical constituents, trace elements, and radioactive chemicals are tabulated as well as water temperature and specific conductance measurement data. Lithologic logs of more than 300 wells, test holes, and measured sections constitute much of this report. County maps at a scale of 1:500 ,000 show the locations. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr83943","usgsCitation":"Zimmerman, E.A., and Collier, K.R., 1985, Ground-water data, Green River basin, Wyoming: U.S. Geological Survey Open-File Report 83-943, v, 511 p. :maps ;28 cm., https://doi.org/10.3133/ofr83943.","productDescription":"v, 511 p. :maps ;28 cm.","costCenters":[],"links":[{"id":148944,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0943/report-thumb.jpg"},{"id":45774,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0943/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aafe4b07f02db66cefe","contributors":{"authors":[{"text":"Zimmerman, Everett Alfred","contributorId":18729,"corporation":false,"usgs":true,"family":"Zimmerman","given":"Everett","email":"","middleInitial":"Alfred","affiliations":[],"preferred":false,"id":173319,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Collier, K. R.","contributorId":36152,"corporation":false,"usgs":true,"family":"Collier","given":"K.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":173320,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":16354,"text":"ofr84712 - 1985 - Revised water budget for the Fernley area, west-central Nevada, 1979","interactions":[],"lastModifiedDate":"2012-02-02T00:07:12","indexId":"ofr84712","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1985","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":"84-712","title":"Revised water budget for the Fernley area, west-central Nevada, 1979","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr84712","usgsCitation":"Van Denburgh, A.S., and Arteaga, F., 1985, Revised water budget for the Fernley area, west-central Nevada, 1979: U.S. Geological Survey Open-File Report 84-712, vii, 17 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr84712.","productDescription":"vii, 17 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":149455,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1984/0712/report-thumb.jpg"},{"id":45276,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1984/0712/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a14e4b07f02db602ce5","contributors":{"authors":[{"text":"Van Denburgh, A. S.","contributorId":23928,"corporation":false,"usgs":true,"family":"Van Denburgh","given":"A.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":172714,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Arteaga, F.E.","contributorId":50918,"corporation":false,"usgs":true,"family":"Arteaga","given":"F.E.","affiliations":[],"preferred":false,"id":172715,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":4495,"text":"cir970 - 1985 - 1985 annual report on Alaska's mineral resources","interactions":[],"lastModifiedDate":"2012-02-02T00:05:48","indexId":"cir970","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1985","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":307,"text":"Circular","code":"CIR","onlineIssn":"2330-5703","printIssn":"1067-084X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"970","title":"1985 annual report on Alaska's mineral resources","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/cir970","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1985, 1985 annual report on Alaska's mineral resources: U.S. Geological Survey Circular 970, iii, 58 p. :ill., maps ;26 cm.26 cm., https://doi.org/10.3133/cir970.","productDescription":"iii, 58 p. :ill., maps ;26 cm.26 cm.","costCenters":[],"links":[{"id":121706,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1985/0970/report-thumb.jpg"},{"id":31555,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1985/0970/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53cd4913e4b0b290850eedd7","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":528223,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":4695,"text":"twri03A16 - 1985 - Measurement of discharge using tracers","interactions":[{"subject":{"id":9805,"text":"ofr84136 - 1984 - Measurement of discharge using tracers","indexId":"ofr84136","publicationYear":"1984","noYear":false,"title":"Measurement of discharge using tracers"},"predicate":"SUPERSEDED_BY","object":{"id":4695,"text":"twri03A16 - 1985 - Measurement of discharge using tracers","indexId":"twri03A16","publicationYear":"1985","noYear":false,"title":"Measurement of discharge using tracers"},"id":1}],"lastModifiedDate":"2012-02-02T00:05:31","indexId":"twri03A16","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1985","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":336,"text":"Techniques of Water-Resources Investigations","code":"TWRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"03-A16","title":"Measurement of discharge using tracers","docAbstract":"The development of fluorescent dyes and fluorometers that can measure these dyes at very low concentrations has made dye-dilution methods practical for measuring discharge. These methods are particularly useful for determining discharge under certain flow conditions that are unfavorable for current meter measurements. These include small streams, canals, and pipes where\r\n1. Turbulence is excessive for current-meter measurement but conducive to good mixing.\r\n2. Moving rocks and debris may damage instruments placed in the flow.\r\n3. Cross-sectional areas or velocities are indeterminate or changing.\r\n4. The flow is unsteady, such as the flow that exists with storm-runoff events on small streams and urban storm-sewer systems.\r\n5. The flow is physically inaccessible or unsafe.\r\nFrom a practical standpoint, such methods are limited primarily to small streams, because of the excessively long channel-mixing lengths required for larger streams. Very good accuracy can be obtained provided that\r\n1. Adequate mixing length and time are allowed.\r\n2. Careful field and laboratory techniques are used.\r\n3. Dye losses are not significant.\r\nThis manual describes the slug-injection and constant-rate injection methods of performing tracer-dilution measurements. Emphasis is on the use of fluorescent dyes as tracers and the equipment, field methods, and laboratory procedures for performing such measurements. The tracer-velocity method is also briefly discussed.","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/twri03A16","issn":"0565-596X","usgsCitation":"Kilpatrick, F.A., and Cobb, E.D., 1985, Measurement of discharge using tracers: U.S. Geological Survey Techniques of Water-Resources Investigations 03-A16, x, 52 p. :ill. ;26 cm., https://doi.org/10.3133/twri03A16.","productDescription":"x, 52 p. :ill. ;26 cm.","costCenters":[],"links":[{"id":139096,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":287,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/twri/twri3-a16/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a1ae4b07f02db606aa0","contributors":{"authors":[{"text":"Kilpatrick, F. A.","contributorId":22319,"corporation":false,"usgs":true,"family":"Kilpatrick","given":"F.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":149633,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Cobb, Ernest D.","contributorId":25139,"corporation":false,"usgs":true,"family":"Cobb","given":"Ernest","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":149634,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":4700,"text":"twri03A17 - 1985 - Acoustic velocity meter systems","interactions":[],"lastModifiedDate":"2012-02-02T00:05:31","indexId":"twri03A17","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1985","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":336,"text":"Techniques of Water-Resources Investigations","code":"TWRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"03-A17","title":"Acoustic velocity meter systems","docAbstract":"Acoustic velocity meter (AVM) systems operate on the principles that the point-to-point upstream traveltime of an acoustic pulse is longer than the downstream traveltime and that this difference in traveltime can be accurately measured by electronic devices. An AVM system is capable of recording water velocity (and discharge) under a wide range of conditions, but some constraints apply:\r\n1. Accuracy is reduced and performance is degraded if the acoustic path is not a continuous straight line. The path can be bent by reflection if it is too close to a stream boundary or by refraction if it passes through density gradients resulting from variations in either water temperature or salinity. For paths of less than 100 m, a temperature gradient of 0.1' per meter causes signal bending less than 0.6 meter at midchannel, and satisfactory velocity results can be obtained. Reflection from stream boundaries can cause signal cancellation if boundaries are too close to signal path.\r\n2. Signal strength is attenuated by particles or bubbles that absorb, spread, or scatter sound. The concentration of particles or bubbles that can be tolerated is a function of the path length and frequency of the acoustic signal.\r\n3. Changes in streamline orientation can affect system accuracy if the variability is random.\r\n4. Errors relating to signal resolution are much larger for a single threshold detection scheme than for multiple threshold schemes.\r\nThis report provides methods for computing the effect of various conditions on the accuracy of a record obtained from an AVM. The equipment must be adapted to the site. Field reconnaissance and preinstallation analysis to detect possible problems are critical for proper installation and operation of an AVM system.","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/twri03A17","issn":"0565-596X","usgsCitation":"Laenen, A., 1985, Acoustic velocity meter systems: U.S. Geological Survey Techniques of Water-Resources Investigations 03-A17, viii, 38 p. :ill. ;26 cm., https://doi.org/10.3133/twri03A17.","productDescription":"viii, 38 p. :ill. ;26 cm.","costCenters":[],"links":[{"id":139114,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":292,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/twri/twri3-a17/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b0fe4b07f02db6a03bb","contributors":{"authors":[{"text":"Laenen, Antonius","contributorId":107673,"corporation":false,"usgs":true,"family":"Laenen","given":"Antonius","email":"","affiliations":[],"preferred":false,"id":149642,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":8067,"text":"ofr85168 - 1985 - Historical water-quality data for the Clark Fork (river) and the mouths of selected tributaries, western Montana","interactions":[],"lastModifiedDate":"2012-02-02T00:06:12","indexId":"ofr85168","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1985","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":"85-168","title":"Historical water-quality data for the Clark Fork (river) and the mouths of selected tributaries, western Montana","docAbstract":"The Clark Fork, occupying a major drainage area in western Montana, leaves the state of Montana 's largest river. This report is a compilation of recent historical water-quality data collected by the U.S. Geological Survey on the Clark Fork and near the mouths of major tributaries. Included in the report are water-quality data collected during various time intervals since 1969 at 18 surface-water stations. Because of the large amount of streamflow and water-temperature data collected at these 18 stations and at other sites in the study area, the data are not included in the report. However, station numbers and corresponding periods of record are listed and the availability of the data is identified. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr85168","usgsCitation":"Brosten, T., and Jacobson, M., 1985, Historical water-quality data for the Clark Fork (river) and the mouths of selected tributaries, western Montana: U.S. Geological Survey Open-File Report 85-168, v, 99 p. :map ;28 cm., https://doi.org/10.3133/ofr85168.","productDescription":"v, 99 p. :map ;28 cm.","costCenters":[],"links":[{"id":142260,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1985/0168/report-thumb.jpg"},{"id":35643,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1985/0168/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a54e4b07f02db62c0b3","contributors":{"authors":[{"text":"Brosten, T.M.","contributorId":92669,"corporation":false,"usgs":true,"family":"Brosten","given":"T.M.","email":"","affiliations":[],"preferred":false,"id":157092,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Jacobson, M.A.","contributorId":7279,"corporation":false,"usgs":true,"family":"Jacobson","given":"M.A.","email":"","affiliations":[],"preferred":false,"id":157091,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":4160,"text":"cir904C - 1985 - Geologic and hydrologic characterization and evaluation of the Basin and Range Province relative to the disposal of high-level radioactive waste: Part III, Geologic and hydrologic evaluation","interactions":[{"subject":{"id":18097,"text":"ofr83756 - 1983 - Geologic and hydrologic characterization and evaluation of the Basin and Range Province relative to the disposal of high-level radioactive waste: Part III, Geologic and hydrologic evaluation","indexId":"ofr83756","publicationYear":"1983","noYear":false,"title":"Geologic and hydrologic characterization and evaluation of the Basin and Range Province relative to the disposal of high-level radioactive waste: Part III, Geologic and hydrologic evaluation"},"predicate":"SUPERSEDED_BY","object":{"id":4160,"text":"cir904C - 1985 - Geologic and hydrologic characterization and evaluation of the Basin and Range Province relative to the disposal of high-level radioactive waste: Part III, Geologic and hydrologic evaluation","indexId":"cir904C","publicationYear":"1985","noYear":false,"chapter":"C","title":"Geologic and hydrologic characterization and evaluation of the Basin and Range Province relative to the disposal of high-level radioactive waste: Part III, Geologic and hydrologic evaluation"},"id":1}],"lastModifiedDate":"2019-11-07T12:10:42","indexId":"cir904C","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1985","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":307,"text":"Circular","code":"CIR","onlineIssn":"2330-5703","printIssn":"1067-084X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"904","chapter":"C","title":"Geologic and hydrologic characterization and evaluation of the Basin and Range Province relative to the disposal of high-level radioactive waste: Part III, Geologic and hydrologic evaluation","docAbstract":"<p>This report describes the first phase in evaluating the geology and hydrology of the Basin and Range Province for potential suitability of geohydrologic environments for isolation of high-level radioactive waste. The evaluation of the Province applies the guidelines, discussed in Part I (Bedinger, Sargent, and Reed, 1983) of this report to the geologic and hydrologic information compiled for the Province in Part II (Sargent and Bedinger, 1983).</p><p>The geologic and hydrologic factors considered in the Province evaluation include distribution of potential host rocks, tectonic conditions and data on ground-water hydrology. Potential host media considered include argillaceous rocks, tuff, basaltic rocks, granitic rocks, evaporites, and the unsaturated zone. The tectonic factors considered are Quaternary faults, late Cenozoic volcanics, seismic activity, heat flow, and late Cenozoic rates of vertical uplift. Hydrologic conditions considered include length of flow path from potential host rocks to discharge areas, interbasin and geothermal flow systems and thick unsaturated sections as potential host media.</p><p>The Basin and Range Province was divided into 12 subprovinces; each subprovince is evaluated separately and prospective areas for further study are identified. About onehalf of the Province appears to have combinations of potential host rocks, tectonic conditions, and ground-water hydrology that merit consideration for further study.</p><p>The prospective areas for further study in each subprovince are summarized in a brief list of the potentially favorable factors and the issues of concern. Data compiled for the entire Province do not permit a complete evaluation of the favorability for high-level waste isolation. The evaluations here are intended to identify broad regions that contain potential geohydrologic environments containing multiple natural barriers to radionuclide migration.</p>","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/cir904C","usgsCitation":"Bedinger, M.S., Sargent, K., and Brady, B., 1985, Geologic and hydrologic characterization and evaluation of the Basin and Range Province relative to the disposal of high-level radioactive waste: Part III, Geologic and hydrologic evaluation: U.S. Geological Survey Circular 904, iv, 27 p., https://doi.org/10.3133/cir904C.","productDescription":"iv, 27 p.","numberOfPages":"34","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":335937,"rank":4,"type":{"id":22,"text":"Related Work"},"url":"https://pubs.usgs.gov/publication/cir904B","text":"Circular 904-B","linkHelpText":"Part II, Geologic and hydrologic characterization"},{"id":335936,"rank":3,"type":{"id":22,"text":"Related Work"},"url":"https://pubs.usgs.gov/publication/cir904A","text":"Circular 904-A","linkHelpText":"Part I, Introduction and guidelines"},{"id":31270,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1985/0904c/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":118366,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1985/0904c/report-thumb.jpg"}],"country":"United States","state":"Arizona, California, Idaho, Nevada, New Mexico, Oregon, Texas","otherGeospatial":"Basin and Range Province","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -115.6640625,\n              32.65787573695528\n            ],\n            [\n              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S.","contributorId":65452,"corporation":false,"usgs":true,"family":"Bedinger","given":"M.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":148319,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Sargent, Kenneth A.","contributorId":15998,"corporation":false,"usgs":true,"family":"Sargent","given":"Kenneth A.","affiliations":[],"preferred":false,"id":148318,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Brady, Bruce T.","contributorId":8059,"corporation":false,"usgs":true,"family":"Brady","given":"Bruce T.","affiliations":[],"preferred":false,"id":148317,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":3375,"text":"cir926 - 1985 - Bibliography of borehole geophysics as applied to ground-water hydrology","interactions":[],"lastModifiedDate":"2012-02-02T00:05:30","indexId":"cir926","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1985","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":307,"text":"Circular","code":"CIR","onlineIssn":"2330-5703","printIssn":"1067-084X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"926","title":"Bibliography of borehole geophysics as applied to ground-water hydrology","docAbstract":"Most of the references on borehole geophysics that are relevant to ground-water hydrology are contained in this bibliography, but it does not include every reference that is available under each subject heading; the literature is much too extensive to compile a complete listing. \r\n\r\nSome of the references may appear under more than one subject heading because the references commonly relate to more than one main topic. Many articles have been cross-referenced in order to assist the reader in locating an article. For example, the article entitled, 'Application of the acoustic televiewer to the characterization of hydraulic fractures in geothermal wells' is listed under both 'Acoustic televiewer,' and 'Geothermal'. \r\n\r\nThe bibliography is intended to lead the reader to other articles on borehole-geophysical logging and related subjects, because each article cited also will have a list of references, which may be more specialized, covering many subjects with related applications, such as physics, mathematics, chemistry, geology, electronics, acoustics, hydrology, and surface geophysics. However, not all of these related subject headings could be included in this bibliography.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/cir926","usgsCitation":"Taylor, T.A., and Dey, J.A., 1985, Bibliography of borehole geophysics as applied to ground-water hydrology: U.S. Geological Survey Circular 926, iii, 62 p. ;26 cm., https://doi.org/10.3133/cir926.","productDescription":"iii, 62 p. ;26 cm.","costCenters":[],"links":[{"id":123179,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1985/0926/report-thumb.jpg"},{"id":30385,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1985/0926/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a50e4b07f02db6296dd","contributors":{"authors":[{"text":"Taylor, Ticie A.","contributorId":74736,"corporation":false,"usgs":true,"family":"Taylor","given":"Ticie","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":146744,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Dey, Joyce A.","contributorId":88335,"corporation":false,"usgs":true,"family":"Dey","given":"Joyce","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":146745,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":4256,"text":"cir878C_1985 - 1985 - Codes for the identification of aquifer names and geologic units in the United States and the Caribbean outlying areas","interactions":[],"lastModifiedDate":"2012-02-02T00:05:38","indexId":"cir878C_1985","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1985","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":307,"text":"Circular","code":"CIR","onlineIssn":"2330-5703","printIssn":"1067-084X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"878-C","title":"Codes for the identification of aquifer names and geologic units in the United States and the Caribbean outlying areas","docAbstract":"This standard provides codes to be used for the identification of aquifer names and geologic units in the United States, the Caribbean and other outlying areas. Outlying areas include Puerto Rico, the Virgin Islands, American Samoa, the Midway Islands, Trust Territories of the Pacific Islands, and miscellaneous Pacific Islands. Each code identifies an aquifer or rock-stratigraphic unit and its age designation. The codes provide a standardized base for use by organizations in the storage, retrieval, and exchange of ground-water data; the indexing and inventory of ground-water data and information; the cataloging of ground-water data acquisition activities; and a variety of other applications.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/cir878C_1985","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1985, Codes for the identification of aquifer names and geologic units in the United States and the Caribbean outlying areas: U.S. Geological Survey Circular 878-C, iii, C1-C8 p. ;28 cm. (A. U.S. Geological Survey Data Standard), https://doi.org/10.3133/cir878C_1985.","productDescription":"iii, C1-C8 p. ;28 cm. (A. U.S. Geological Survey Data Standard)","costCenters":[],"links":[{"id":118224,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1985/0878c/report-thumb.jpg"},{"id":31369,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1985/0878c/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b24e4b07f02db6ae9ab","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":528173,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":3027,"text":"wsp2256B - 1985 - Effects of low-level dams on the distribution of sediment, trace metals, and organic substances in the lower Schuylkill River basin, Pennsylvania","interactions":[],"lastModifiedDate":"2017-06-06T14:02:12","indexId":"wsp2256B","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1985","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":"2256","chapter":"B","title":"Effects of low-level dams on the distribution of sediment, trace metals, and organic substances in the lower Schuylkill River basin, Pennsylvania","docAbstract":"Heavy use of the Schuylkill River for municipal water supplies and a history of accidental spills and discharges of trace metals and organic substances have been a concern of State and local officials for many years. The U.S. Geological Survey, as part of their River Quality Assessment Program, developed a study to assess the occurrence and distribution of trace substances that pose a threat to human health and aquatic life. This report presents the results of the part of the study that evaluates the effects of low-level dams in the lower basin on the distribution and transport of sediment and trace substances. \r\n\r\nA combination of historical and current data were used in the assessment. Suspended-sediment data collected at several mainstem and tributary sites from 1954 to 1979 and sedimentation surveys of the six pools in the lower basin were used to define the sediment-transport characteristics of the river. These data provided a base for assessing the transport of trace substances, which are associated closely with riverbed sediments and suspended particles. Water and riverbed samples were collected for analyses of trace substances at numerous sites in the lower basin from 1978 to 1980. \r\n\r\nThe six dams on the river between Pottstown and Philadelphia have had a significant effect on the transport of sediment and trace substances. Between 1954 and 1970, more than 4.7 million cubic yards of sediment accumulated in the pools formed by the dams. The quantity of sediment deposited in the pools ranged from 150,000 cubic yards in Plymouth Pool to 1.6 million cubic yards in Fairmount Pool. The rate of accumulation in the pools was a function of pool size and geometry and the frequency of storms. About 35 percent of the total sediment discharged by the river was stored in the six pools from 1954 to 1970. Since 1970, the net change in sediment accumulation has been minimal. More than 24 percent of the sediment in Fairmount Pool in 1970 was scoured from the pool during Hurricane Agnes in 1972; however, total sediment accumulation returned to the 1970 level within 2 years. \r\n\r\nAnalyses of water samples showed that some trace substances are associated closely with particulate material transported by the river. The concentration of suspended and total cadmium, chromium, copper, lead, nickel, and zinc correlated well with the concentration of suspended sediment and suspended organic carbon. The average annual discharge of metals in suspension as a percentage of total average annual discharge ranged from 46 percent for nickel to 94 percent for lead for the Schuylkill River at Manayunk. The average annual discharge of each metal remained about the same or decreased between Pottstown and Philadelphia. Synoptic sampling of the inflow and outflow of several pools during storm runoff showed that the pools limit the transport of trace metals. More than 50 percent of the suspended copper transported by the river at Pottstown was deposited in Vincent Pool during the storm of May 12-15, 1980. Similar reductions were observed between Port Kennedy and Manayunk as the storm runoff passed through Norristown, Plymouth, and Flat Rock Pools. \r\n\r\nAnalyses of riverbed sediments showed that concentrations of trace substances were higher in sediments that included all particles finer than 0.062 millimeter than in sediments that included only particles finer than 0.016 millimeter. This suggests that medium and coarse silt particles or conglomerates of finer particles sorb as much or more trace constituents as the individual fine silts and clay particles. Concentrations of trace metals were as much as 90 percent higher in the sediments that included coarse silt. Concentrations of trace organic substances were several times higher in the sediments that included coarse silt than in sediments consisting of only fine silt or clay. \r\n\r\nSurficial and core samples of riverbed sediments were used to define the present and historical distribution of trace substances in ","language":"English","publisher":"U.S. Government Printing Office","doi":"10.3133/wsp2256B","usgsCitation":"Yorke, T.H., Stamer, J.K., and Pederson, G.L., 1985, Effects of low-level dams on the distribution of sediment, trace metals, and organic substances in the lower Schuylkill River basin, Pennsylvania: U.S. Geological Survey Water Supply Paper 2256, vii, 53 p. :ill., maps ;28 cm., https://doi.org/10.3133/wsp2256B.","productDescription":"vii, 53 p. :ill., maps ;28 cm.","costCenters":[{"id":532,"text":"Pennsylvania Water Science Center","active":true,"usgs":true}],"links":[{"id":29858,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/2256b/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":139513,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/2256b/report-thumb.jpg"}],"country":"United States","state":"Pennsylvania","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4acce4b07f02db67ecc5","contributors":{"authors":[{"text":"Yorke, Thomas H.","contributorId":83109,"corporation":false,"usgs":true,"family":"Yorke","given":"Thomas","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":146169,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Stamer, John K.","contributorId":104481,"corporation":false,"usgs":true,"family":"Stamer","given":"John","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":146170,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Pederson, Gary L.","contributorId":81084,"corporation":false,"usgs":true,"family":"Pederson","given":"Gary","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":146168,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":8082,"text":"ofr84802 - 1985 - Hydrogeologic data from a test well in east-central Duval County, Florida","interactions":[],"lastModifiedDate":"2012-02-02T00:06:07","indexId":"ofr84802","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1985","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":"84-802","title":"Hydrogeologic data from a test well in east-central Duval County, Florida","docAbstract":"A 2,112-foot test well was drilled in east-central Duval County, Florida, to obtain geologic, hydrologic, and water chemistry data. Drill cuttings and water samples were collected, and water-level measurements and lithologic and geophysical logs were made. Deposits to a depth of 575 feet consist of sand, clayey sand, phosphatic sandy clay, coquina, sandy limestone, and dolostone. Below 575 feet, the deposits consist of fragmented and granular limestone, dolomitic limestone, and massive to finely crystalline dolostone, which comprise the Floridan aquifer system in the area. Water levels were measured near or at the bottom of the drill hole through the drill stem and in the annular space between the drilled hole and drill stem at the well head as drilling progressed from 770 to 2,112 feet in depth. Water levels measured through the drill stem ranged from 1.17 feet above land surface at a depth of 2,107 feet to 15.0 feet above land surface at a depth of 1,574 feet. Water levels measured in the annular space ranged from 7.5 feet above land surface at a depth of 770 feet to 14.9 feet at various depths from 1,574 to 1,721 feet. Chloride concentrations of water sampled through the drill stem from a depth of 711 to 1 ,616 feet ranged from 22 to 150 milligrams per liter at 1,648 feet. Chloride concentrations then ranged from 345 to about 800 milligrams per liter to a depth of 2,071 feet and then increased to a maximum of 5,450 milligrams per liter at 2,107 feet. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr84802","usgsCitation":"Brown, D., Johnson, R., and Broxton, R., 1985, Hydrogeologic data from a test well in east-central Duval County, Florida: U.S. Geological Survey Open-File Report 84-802, iv, 67 p. :ill., map ;28 cm., https://doi.org/10.3133/ofr84802.","productDescription":"iv, 67 p. :ill., map ;28 cm.","costCenters":[],"links":[{"id":141482,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1984/0802/report-thumb.jpg"},{"id":35686,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1984/0802/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4de4b07f02db6273e5","contributors":{"authors":[{"text":"Brown, D.P.","contributorId":95881,"corporation":false,"usgs":true,"family":"Brown","given":"D.P.","email":"","affiliations":[],"preferred":false,"id":157113,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Johnson, R.A.","contributorId":93864,"corporation":false,"usgs":true,"family":"Johnson","given":"R.A.","email":"","affiliations":[],"preferred":false,"id":157112,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Broxton, R.A.","contributorId":36934,"corporation":false,"usgs":true,"family":"Broxton","given":"R.A.","email":"","affiliations":[],"preferred":false,"id":157111,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":5654,"text":"pp1054C - 1985 - Hydrothermal alteration in research drill hole Y-3, Lower Geyser Basin, Yellowstone National Park, Wyoming","interactions":[],"lastModifiedDate":"2019-05-16T09:21:10","indexId":"pp1054C","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1985","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":"1054","chapter":"C","title":"Hydrothermal alteration in research drill hole Y-3, Lower Geyser Basin, Yellowstone National Park, Wyoming","docAbstract":"Y-3, a U.S. Geological Survey research diamond-drill hole in Lower Geyser Basin, Yellowstone National Park, Wyoming, reached a depth of 156.7 m. The recovered drill core consists of 42.2 m of surficial (mostly glacial) sediments and two rhyolite flows (Nez Perce Creek flow and an older, unnamed rhyolite flow) of the Central Plateau Member of the Pleistocene Plateau Rhyolite. Hydrothermal alteration is fairly extensive in most of the drill core. The surficial deposits are largely cemented by silica and zeolite minerals; and the two rhyolite flows are, in part, bleached by thermal water that deposited numerous hydrothermal minerals in cavities and fractures. Hydrothermal minerals containing sodium as a dominant cation (analcime, clinoptilolite, mordenite, Na-smectite, and aegirine) are more abundant than calcium-bearing minerals (calcite, fluorite, Ca-smectite, and pectolite) in the sedimentary section of the drill core. In the volcanic section of drill core Y-3, calcium-rich minerals (dachiardite, laumontite, yugawaralite, calcite, fluorite, Ca-smectite, pectolite, and truscottite) are predominant over sodium-bearing minerals (aegirine, mordenite, and Na-smectite). Hydrothermal minerals that contain significant amounts of potassium (alunite and lepidolite in the sediments and illitesmectite in the rhyolite flows) are found in the two drill-core intervals. Drill core y:.3 also contains hydrothermal silica minerals (opal, [3-cristobalite, chalcedony, and quartz), other clay minerals (allophane, halloysite, kaolinite, and chlorite), gypsum, pyrite, and hematite. The dominance of calcium-bearing hydrothermal minerals in the lower rhyolitic section of the y:.3 drill core appears to be due to loss of calcium, along with potassium, during adiabatic cooling of an ascending boiling water.","language":"English","publisher":"U.S. Government Printing Office","doi":"10.3133/pp1054C","usgsCitation":"Bargar, K.E., and Beeson, M.H., 1985, Hydrothermal alteration in research drill hole Y-3, Lower Geyser Basin, Yellowstone National Park, Wyoming: U.S. Geological Survey Professional Paper 1054, p. C1-C23, https://doi.org/10.3133/pp1054C.","productDescription":"p. C1-C23","costCenters":[],"links":[{"id":32151,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/1054c/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":124513,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/1054c/report-thumb.jpg"}],"country":"United States","state":"Wyoming","otherGeospatial":"Yellowstone National Park","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ce4b07f02db5fc654","contributors":{"authors":[{"text":"Bargar, Keith E.","contributorId":9643,"corporation":false,"usgs":true,"family":"Bargar","given":"Keith","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":151372,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Beeson, Melvin H. mbeeson@usgs.gov","contributorId":5017,"corporation":false,"usgs":true,"family":"Beeson","given":"Melvin","email":"mbeeson@usgs.gov","middleInitial":"H.","affiliations":[{"id":617,"text":"Volcano Science Center","active":true,"usgs":true}],"preferred":true,"id":151371,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":4825,"text":"pp1200KS - 1985 - The National Gazetteer of the United States of America; Kansas 1984","interactions":[],"lastModifiedDate":"2012-02-02T00:05:50","indexId":"pp1200KS","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1985","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":"1200","chapter":"KS","title":"The National Gazetteer of the United States of America; Kansas 1984","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/pp1200KS","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1985, The National Gazetteer of the United States of America; Kansas 1984: U.S. Geological Survey Professional Paper 1200, 326 p., https://doi.org/10.3133/pp1200KS.","productDescription":"326 p.","costCenters":[],"links":[{"id":117416,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/1200ks/report-thumb.jpg"},{"id":31768,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/1200ks/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac7e4b07f02db67b159","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":528384,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
]}