{"pageNumber":"2112","pageRowStart":"52775","pageSize":"25","recordCount":68919,"records":[{"id":8486,"text":"ofr82853 - 1982 - Time of travel of the Flint River, Utah Dam to highway M-13, Michigan, August 4-8, 1981","interactions":[],"lastModifiedDate":"2016-09-22T12:50:27","indexId":"ofr82853","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"82-853","title":"Time of travel of the Flint River, Utah Dam to highway M-13, Michigan, August 4-8, 1981","docAbstract":"<p>Tracing of rhodamine WT dye has provided time-of-travel data for waste-load allocation studies of a 42.8-mile reach of the Flint River at low flow. A discharge equaled or exceeded about 90 percent of the time was measured at Grand Traverse Street in Flint before dye injection. Dye was injected at two locations in Flint--at Utah Dam and at Grand Traverse Street, From Utah Dam to Grand Traverse Street, the mean velocity of flow was about 0.1 foot per second; time-of-travel was 35.3 hours. From Grand Traverse Street to Highway M-13, mean velocity was about 0.7 foot per second; time-of-travel was 78.8 hours. Time-of-travel for the reach between Utah Dam and Highway M-13 was thus 114 hours. </p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Lansing, MI","doi":"10.3133/ofr82853","collaboration":"Prepared in cooperation with the U.S. Environmental Protection Agency","usgsCitation":"Cummings, T.R., and Miller, J.B., 1982, Time of travel of the Flint River, Utah Dam to highway M-13, Michigan, August 4-8, 1981: U.S. Geological Survey Open-File Report 82-853, Document: vi, 21 p.; Plate: 12.97 x 7.78 inches, https://doi.org/10.3133/ofr82853.","productDescription":"Document: vi, 21 p.; Plate: 12.97 x 7.78 inches","costCenters":[{"id":382,"text":"Michigan Water Science 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Ray","contributorId":20722,"corporation":false,"usgs":true,"family":"Cummings","given":"T.","email":"","middleInitial":"Ray","affiliations":[],"preferred":false,"id":157798,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Miller, John B.","contributorId":37304,"corporation":false,"usgs":true,"family":"Miller","given":"John","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":157799,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":8493,"text":"ofr82364 - 1982 - An evaluation of suspended sediments and turbidity in Cow Creek, Oregon","interactions":[],"lastModifiedDate":"2012-02-02T00:06:24","indexId":"ofr82364","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"82-364","title":"An evaluation of suspended sediments and turbidity in Cow Creek, Oregon","docAbstract":"During a 6-month period from December 1980 through May 1981, samples were collected from Cow Creek near Azalea, Oreg., and analyzed for suspended sediment, particle-size distribution, and turbidity. Of the estimated suspended-sediment discharge of 4,270 tons for the 1981 water year, 95 percent (4,050 tons) was transported during a major storm event, December 2-4, 1980. The 1981 water year suspended-sediment discharge of 4,270 tons is well below the average annual suspended-sediment discharge of 22,000 tons reported earlier by Curtiss (1974). \r\n\r\nA clay-sediment transport curve was used in conjunction with the flow-duration curve to estimate average annual clay discharge of 3,700 tons for Cow Creek near Azalea. \r\n\r\nTurbidity in Cow Creek near Azalea is estimated to be equal to or less than 15 NTU (nephelometric turbidity units) 90 percent of the time. \r\n\r\nA method for predicting turbidity values in a hypothetical impoundment is presented in this report. This method utilizes a suspended-sediment transport curve of the fine (<0.002 mm) material and measures residual-turbidity values. This method probably could be used to assess the impact of proposed reservoirs on stream turbidities in basins similar to that of Cow Creek basin.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82364","usgsCitation":"Curtiss, D.A., 1982, An evaluation of suspended sediments and turbidity in Cow Creek, Oregon: U.S. Geological Survey Open-File Report 82-364, v, 26 p. :ill. ;28 cm., https://doi.org/10.3133/ofr82364.","productDescription":"v, 26 p. :ill. ;28 cm.","costCenters":[],"links":[{"id":143423,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0364/report-thumb.jpg"},{"id":36065,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0364/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad8e4b07f02db68489e","contributors":{"authors":[{"text":"Curtiss, D. A.","contributorId":27862,"corporation":false,"usgs":true,"family":"Curtiss","given":"D.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":157813,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":8519,"text":"ofr82369 - 1982 - Hydrologic monitoring in the area of the proposed Yazoo River navigation project, west-central Mississippi, 1978-80","interactions":[],"lastModifiedDate":"2023-01-30T19:31:23.74711","indexId":"ofr82369","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"82-369","title":"Hydrologic monitoring in the area of the proposed Yazoo River navigation project, west-central Mississippi, 1978-80","docAbstract":"<p>The ground—water level data presented in this report were collected in conjunction with a study of the Mississippi River Valley alluvial aquifer in part of the Yazoo River Basin. Funding for the collection of water—level data was provided by the Vicksburg District, Corps of Engineers, who also drilled the observation wells and surveyed elevations of the top of the casing of each well. The wells were drilled to obtain data on seasonal changes in ground—water levels, areas of recharge and/or discharge, and on direction of movement of water in the alluvial aquifer. This report is intended to document the data.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr82369","collaboration":"Prepared in cooperation with U. S. 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,{"id":8538,"text":"ofr82362 - 1982 - Hydrologic data from test wells and low-flow investigations in the middle reach of the Eagle River valley, Alaska; 1980-81","interactions":[],"lastModifiedDate":"2012-02-02T00:06:15","indexId":"ofr82362","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"82-362","title":"Hydrologic data from test wells and low-flow investigations in the middle reach of the Eagle River valley, Alaska; 1980-81","docAbstract":"Test wells and low-flow investigations in the Eagle River valley , Alaska, were used to evaluate the feasibility of developing ground water for a public supply. Aquifers capable of supplying large yield wells were not indicated in any of the drilling areas. The data include: results of low-flow seepage investigations at 22 river sites; geologic materials logs of eight test wells; water-quality data from two observation wells, two springs, and two river sites; and water level and temperature information for the observation wells and streams. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82362","usgsCitation":"Deeter, G., and George, R., 1982, Hydrologic data from test wells and low-flow investigations in the middle reach of the Eagle River valley, Alaska; 1980-81: U.S. Geological Survey Open-File Report 82-362, iii, 16 p., ill., maps ;28 cm., https://doi.org/10.3133/ofr82362.","productDescription":"iii, 16 p., ill., maps ;28 cm.","costCenters":[],"links":[{"id":141694,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0362/report-thumb.jpg"},{"id":36117,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0362/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa7e4b07f02db66712e","contributors":{"authors":[{"text":"Deeter, Gary","contributorId":60216,"corporation":false,"usgs":true,"family":"Deeter","given":"Gary","email":"","affiliations":[],"preferred":false,"id":157901,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"George, R.S.","contributorId":12854,"corporation":false,"usgs":true,"family":"George","given":"R.S.","email":"","affiliations":[],"preferred":false,"id":157900,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":8541,"text":"ofr8215 - 1982 - South Atlantic summary report 2: A revision of Outer Continental Shelf oil and gas activities in the South Atlantic (U.S.) and their onshore impacts, a summary report, July 1980","interactions":[],"lastModifiedDate":"2022-09-19T22:20:37.299269","indexId":"ofr8215","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"82-15","title":"South Atlantic summary report 2: A revision of Outer Continental Shelf oil and gas activities in the South Atlantic (U.S.) and their onshore impacts, a summary report, July 1980","docAbstract":"<p>The search for oil and gas on the Outer Continental Shelf (OCS) in the South Atlantic Region began in 1960, when geophysical surveys of the area were initiated. In 1977, a Continental Offshore Stratigraphic Test (COST) well was drilled in the Southeast Georgia Embayment. In March 1978, the first lease sale, Sale 43, was held, resulting in the leasing of 43 tracts. Approximately a year later, in May 1979, the first exploratory drilling began, and by February 1980, six exploratory wells had been drilled by four companies. Hydrocarbons were not found in any of these wells.</p><p>Lease Sale 56, the second lease sale in the South Atlantic Region, was held in August 1981. The sale resulted in the leasing of 47 tracts. Most of the leased tracts are in deep water along the Continental Slope off North Carolina. To date, no drilling has occurred on these tracts, but it is likely that two wells will be drilled or will be in the process of being drilled by the end of 1982. Reoffering Sale RS-2 is scheduled for July 1982, and it will include tracts offered in Lease Sale 56 that were not awarded leases. Lease Sale 78 is scheduled to be held in July 1983.</p><p>The most recent (March 1982) estimates of risked resources for leased lands in the South Atlantic OCS are 27 million barrels of oil and 120 billion cubic feet of gas.</p><p>To date, onshore impacts resulting from OCS exploration have been minimal, and they were associated with Lease Sale 43 exploratory activities. Tenneco, using existing facilities, established a support base in Savannah, Georgia; Getty, Transco, and Exxon used a support base established for them by the city of Brunswick, Georgia. The port at Morehead City, North Carolina, is expected to provide the onshore facilities for exploration in the near future on Lease Sale 56 tracts. Arrangements for the use of these facilities are currently being negotiated.</p><p>In June 1981, the South Atlantic Regional Technical Working Group prepared a Regional Transportation Management Plan for the South Atlantic OCS. The plan is principally an integration of regulatory frameworks, policies, and plans that are applicable to pipeline siting from each of the South Atlantic coastal States and Federal agencies with jurisdiction in the area.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr8215","collaboration":"Prepared for the U.S. Department of the Interior, Minerals Management Service, in cooperation with the U.S. Geological Survey","usgsCitation":"Deis, J.L., Kurz, F.N., and Porter, E.O., 1982, South Atlantic summary report 2: A revision of Outer Continental Shelf oil and gas activities in the South Atlantic (U.S.) and their onshore impacts, a summary report, July 1980: U.S. Geological Survey Open-File Report 82-15, viii, 50 p., https://doi.org/10.3133/ofr8215.","productDescription":"viii, 50 p.","costCenters":[],"links":[{"id":407021,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0015/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":141696,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0015/report-thumb.jpg"}],"country":"United States","otherGeospatial":"Outer Continental Shelf, South Atlantic","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -81.298828125,\n              25.48295117535531\n            ],\n            [\n              -76.46484375,\n              25.48295117535531\n            ],\n            [\n              -76.46484375,\n              36.66841891894786\n            ],\n            [\n              -81.298828125,\n              36.66841891894786\n            ],\n            [\n              -81.298828125,\n              25.48295117535531\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e6e4b07f02db5e7510","contributors":{"authors":[{"text":"Deis, Jeffrey L.","contributorId":10423,"corporation":false,"usgs":true,"family":"Deis","given":"Jeffrey","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":157905,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kurz, Frederick N.","contributorId":47785,"corporation":false,"usgs":true,"family":"Kurz","given":"Frederick","email":"","middleInitial":"N.","affiliations":[],"preferred":false,"id":157906,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Porter, Elizabeth O.","contributorId":104491,"corporation":false,"usgs":true,"family":"Porter","given":"Elizabeth","email":"","middleInitial":"O.","affiliations":[],"preferred":false,"id":157907,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":8590,"text":"ofr82486 - 1982 - Survey of helium in natural water wells and springs in southwest Montana and vicinity, and Imperial Valley, California; Part IV, Jan. 1-Dec. 31, 1981","interactions":[],"lastModifiedDate":"2012-02-02T00:06:09","indexId":"ofr82486","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"82-486","title":"Survey of helium in natural water wells and springs in southwest Montana and vicinity, and Imperial Valley, California; Part IV, Jan. 1-Dec. 31, 1981","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82486","usgsCitation":"Doering, W.P., and Friedman, I., 1982, Survey of helium in natural water wells and springs in southwest Montana and vicinity, and Imperial Valley, California; Part IV, Jan. 1-Dec. 31, 1981: U.S. Geological Survey Open-File Report 82-486, 33 p. ill., maps ;28 cm., https://doi.org/10.3133/ofr82486.","productDescription":"33 p. ill., maps ;28 cm.","costCenters":[],"links":[{"id":141071,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0486/report-thumb.jpg"},{"id":36184,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0486/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae1e4b07f02db688807","contributors":{"authors":[{"text":"Doering, W. P.","contributorId":7270,"corporation":false,"usgs":true,"family":"Doering","given":"W.","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":157995,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Friedman, Irving","contributorId":90664,"corporation":false,"usgs":true,"family":"Friedman","given":"Irving","email":"","affiliations":[],"preferred":false,"id":157996,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":8606,"text":"ofr82501 - 1982 - Ground water and geology of Marquette County, Michigan","interactions":[],"lastModifiedDate":"2016-09-22T14:26:12","indexId":"ofr82501","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"82-501","title":"Ground water and geology of Marquette County, Michigan","docAbstract":"<p>Ground-water resources of Marquette County are about evenly divided between bedrock aquifers and aquifers in glacial deposits. In the northern and the extreme southern parts of the county, most wells are completed in bedrock at depths less than 100 feet. In the central part, most wells are completed in glacial deposits; some of these wells are as deep as 200 feet. Yields, in some places as high as 300 gallons per minute, are generally greatest from wells completed in glacial deposits. Most well water is hard and has iron concentrations ranging from ﻿&lt;0.1 mg/L to about 5.0 mg/L. Both ground water and surface water sources are used in municipal water systems.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Lansing, MI","doi":"10.3133/ofr82501","collaboration":"Prepared in cooperation with the Michigan Department of Natural Resources","usgsCitation":"Doonan, C.J., and Van Alstine, J.L., 1982, Ground water and geology of Marquette County, Michigan: U.S. Geological Survey Open-File Report 82-501, Document: vi, 46 p.; Plate: 27.03 x 34.96 inches, https://doi.org/10.3133/ofr82501.","productDescription":"Document: vi, 46 p.; Plate: 27.03 x 34.96 inches","costCenters":[{"id":382,"text":"Michigan Water Science Center","active":true,"usgs":true}],"links":[{"id":141059,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0501/report-thumb.jpg"},{"id":36203,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0501/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":36204,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0501/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Michigan","county":"Marquette 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sgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ab0e4b07f02db66dc6a","contributors":{"authors":[{"text":"Doonan, C. J.","contributorId":62592,"corporation":false,"usgs":true,"family":"Doonan","given":"C.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":158023,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Van Alstine, J. L.","contributorId":85962,"corporation":false,"usgs":true,"family":"Van Alstine","given":"J.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":158024,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":8625,"text":"ofr811021 - 1982 - Water resources of the Gig Harbor Peninsula and adjacent areas, Washington","interactions":[],"lastModifiedDate":"2012-02-02T00:06:22","indexId":"ofr811021","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"81-1021","title":"Water resources of the Gig Harbor Peninsula and adjacent areas, Washington","docAbstract":"The study area is a remnant of a glacial-drift plain nearly surrounded by marine embayments. A water-resources appraisal was made because the area is experiencing rapid population growth. Additional ground water is available for use in the study area. At least 11 cubic feet per second, five times the 1978 rate of use, can probably be obtained. Ground-water quality is generally very good, with minor problems of excess iron, manganese, dissolved solids, chloride, and coliform bacteria. Total flow through the hydrologic system is at an average rate of 254 cubic feet per second, which includes 93 cubic feet per second of ground-water recharge. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr811021","usgsCitation":"Drost, B., 1982, Water resources of the Gig Harbor Peninsula and adjacent areas, Washington: U.S. Geological Survey Open-File Report 81-1021, vii, 154 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr811021.","productDescription":"vii, 154 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":142332,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/1021/report-thumb.jpg"},{"id":36223,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/1021/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":36224,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/1021/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f4e4b07f02db5f0537","contributors":{"authors":[{"text":"Drost, B. W.","contributorId":38526,"corporation":false,"usgs":true,"family":"Drost","given":"B. W.","affiliations":[],"preferred":false,"id":158047,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":8637,"text":"ofr82168 - 1982 - Report of the annual yield of the Arkansas River basin for the Arkansas River Basin Compact, Arkansas-Oklahoma, 1981 water year","interactions":[],"lastModifiedDate":"2012-02-02T00:06:28","indexId":"ofr82168","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"82-168","title":"Report of the annual yield of the Arkansas River basin for the Arkansas River Basin Compact, Arkansas-Oklahoma, 1981 water year","docAbstract":"The computed annual yield and deficiency of the subbasins as defined in the Arkansas River Compact, Arkansas-Oklahoma, 1980, are presented. Actual runoff from the subbasins and depletion caused by major reservoirs in the compact area are also given. Monthly, maximum, minimum, and mean discharges are shown for the 14 streamflow stations used in computing annual yield. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82168","usgsCitation":"Ducret, G., 1982, Report of the annual yield of the Arkansas River basin for the Arkansas River Basin Compact, Arkansas-Oklahoma, 1981 water year: U.S. Geological Survey Open-File Report 82-168, 27 p. :map ;28 cm., https://doi.org/10.3133/ofr82168.","productDescription":"27 p. :map ;28 cm.","costCenters":[],"links":[{"id":144086,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0168/report-thumb.jpg"},{"id":36242,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0168/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a28e4b07f02db61125a","contributors":{"authors":[{"text":"Ducret, G.L. Jr.","contributorId":107703,"corporation":false,"usgs":true,"family":"Ducret","given":"G.L.","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":158067,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":8664,"text":"ofr82442 - 1982 - Data management system for USGS/USEPA urban hydrology studies program","interactions":[],"lastModifiedDate":"2012-02-02T00:06:11","indexId":"ofr82442","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"82-442","title":"Data management system for USGS/USEPA urban hydrology studies program","docAbstract":"A data management system was developed to store, update, and retrieve data collected in urban stormwater studies jointly conducted by the U.S. Geological Survey and U.S. Environmental Protection Agency in 11 cities in the United States. The data management system is used to retrieve and combine data from USGS data files for use in rainfall, runoff, and water-quality models and for data computations such as storm loads. The system is based on the data management aspect of the Statistical Analysis System (SAS) and was used to create all the data files in the data base. SAS is used for storage and retrieval of basin physiography, land-use, and environmental practices inventory data. Also, storm-event water-quality characteristics are stored in the data base. The advantages of using SAS to create and manage a data base are many with a few being that it is simple, easy to use, contains a comprehensive statistical package, and can be used to modify files very easily. Data base system development has progressed rapidly during the last two decades and the data managment system concepts used in this study reflect the advancement made in computer technology during this era. Urban stormwater data is, however, just one application for which the system can be used. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82442","usgsCitation":"Doyle, W., and Lorens, J., 1982, Data management system for USGS/USEPA urban hydrology studies program: U.S. Geological Survey Open-File Report 82-442, vi, 278 p. ill. ;28 cm., https://doi.org/10.3133/ofr82442.","productDescription":"vi, 278 p. ill. ;28 cm.","costCenters":[],"links":[{"id":141155,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0442/report-thumb.jpg"},{"id":36263,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0442/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac7e4b07f02db67b3d1","contributors":{"authors":[{"text":"Doyle, W.H. Jr.","contributorId":59029,"corporation":false,"usgs":true,"family":"Doyle","given":"W.H.","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":158114,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lorens, J.A.","contributorId":15201,"corporation":false,"usgs":true,"family":"Lorens","given":"J.A.","email":"","affiliations":[],"preferred":false,"id":158113,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":8693,"text":"ofr82852 - 1982 - Ground-water levels in Arkansas, spring 1982","interactions":[],"lastModifiedDate":"2012-02-02T00:06:16","indexId":"ofr82852","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"82-852","title":"Ground-water levels in Arkansas, spring 1982","docAbstract":"The report contains about 640 ground-water level measurements made in observation wells in Arkansas in the spring of 1982. In addition, the report contains potentiometric-surface maps and well hydrographs relating to the alluvial aquifer and the Sparta Sand, the most important aquifers with respect to ground-water availability and use in Arkansas.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82852","usgsCitation":"Edds, J., 1982, Ground-water levels in Arkansas, spring 1982: U.S. Geological Survey Open-File Report 82-852, v, 56 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr82852.","productDescription":"v, 56 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":141772,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0852/report-thumb.jpg"},{"id":36280,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0852/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b01e4b07f02db698599","contributors":{"authors":[{"text":"Edds, Joe","contributorId":48532,"corporation":false,"usgs":true,"family":"Edds","given":"Joe","email":"","affiliations":[],"preferred":false,"id":158168,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":8700,"text":"ofr82923 - 1982 - Definitions of components of the Water Data Sources Directory maintained by the National Water Data Exchange","interactions":[{"subject":{"id":9852,"text":"ofr791541 - 1980 - Definitions of components of the Water Data Sources Directory maintained by the National Water Data Exchange","indexId":"ofr791541","publicationYear":"1980","noYear":false,"title":"Definitions of components of the Water Data Sources Directory maintained by the National Water Data Exchange"},"predicate":"SUPERSEDED_BY","object":{"id":8700,"text":"ofr82923 - 1982 - Definitions of components of the Water Data Sources Directory maintained by the National Water Data Exchange","indexId":"ofr82923","publicationYear":"1982","noYear":false,"title":"Definitions of components of the Water Data Sources Directory maintained by the National Water Data Exchange"},"id":1}],"lastModifiedDate":"2012-02-02T00:06:16","indexId":"ofr82923","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"82-923","title":"Definitions of components of the Water Data Sources Directory maintained by the National Water Data Exchange","docAbstract":"This report contains a definition and description of each component of the Water Data Sources Directory data base maintained by the National Water Data Exchange (NAWDEX). It is intended, primarily, to assist those persons using the Water Data Sources Directory in understanding information obtained from the data base. The Water Data Sources Directory is a computerized data base maintained and operated using the System 2000 data base management system. It contains information about organizations that collect, store, and disseminate water data. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82923","usgsCitation":"Edwards, M.D., 1982, Definitions of components of the Water Data Sources Directory maintained by the National Water Data Exchange: U.S. Geological Survey Open-File Report 82-923, vi, 126 p. :ill. ;28 cm., https://doi.org/10.3133/ofr82923.","productDescription":"vi, 126 p. :ill. ;28 cm.","costCenters":[],"links":[{"id":141790,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0923/report-thumb.jpg"},{"id":36286,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0923/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":36287,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0923/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":36285,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0923/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9be4b07f02db65e0d1","contributors":{"authors":[{"text":"Edwards, Melvin D.","contributorId":94305,"corporation":false,"usgs":true,"family":"Edwards","given":"Melvin","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":158178,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":8704,"text":"ofr82921 - 1982 - Identification codes for organizations listed in computerized data systems of the U.S. Geological Survey","interactions":[{"subject":{"id":8705,"text":"ofr81904 - 1981 - Identification codes for organizations listed in computerized data systems of the U.S. Geological Survey","indexId":"ofr81904","publicationYear":"1981","noYear":false,"title":"Identification codes for organizations listed in computerized data systems of the U.S. Geological Survey"},"predicate":"SUPERSEDED_BY","object":{"id":8704,"text":"ofr82921 - 1982 - Identification codes for organizations listed in computerized data systems of the U.S. Geological Survey","indexId":"ofr82921","publicationYear":"1982","noYear":false,"title":"Identification codes for organizations listed in computerized data systems of the U.S. Geological Survey"},"id":1}],"lastModifiedDate":"2012-02-02T00:06:16","indexId":"ofr82921","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"82-921","title":"Identification codes for organizations listed in computerized data systems of the U.S. Geological Survey","docAbstract":"This report contains codes for the identification of public and private organizations listed in computerized data systems. These codes are used by the U.S. Geological Survey 's National Water Data Exchange (NAWDEX), National Water Data Storage and Retrieval System (WATSTORE), National Cartographic Information Center (NCIC), Office of Water Data Coordination (OWDC). The format structure of the codes is discussed and instructions are given for requesting new codes. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82921","usgsCitation":"Edwards, M.D., and Josefson, B.M., 1982, Identification codes for organizations listed in computerized data systems of the U.S. Geological Survey: U.S. Geological Survey Open-File Report 82-921, vi, 119 p. ;28 cm., https://doi.org/10.3133/ofr82921.","productDescription":"vi, 119 p. ;28 cm.","costCenters":[],"links":[{"id":141833,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0921/report-thumb.jpg"},{"id":36288,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0921/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67c83e","contributors":{"authors":[{"text":"Edwards, Melvin D.","contributorId":94305,"corporation":false,"usgs":true,"family":"Edwards","given":"Melvin","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":158183,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Josefson, Beverly M.","contributorId":94306,"corporation":false,"usgs":true,"family":"Josefson","given":"Beverly","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":158184,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":8725,"text":"ofr82252 - 1982 - Production and decomposition of forest litter fall on the Apalachicola River flood plain, Florida","interactions":[{"subject":{"id":8725,"text":"ofr82252 - 1982 - Production and decomposition of forest litter fall on the Apalachicola River flood plain, Florida","indexId":"ofr82252","publicationYear":"1982","noYear":false,"title":"Production and decomposition of forest litter fall on the Apalachicola River flood plain, Florida"},"predicate":"SUPERSEDED_BY","object":{"id":1310,"text":"wsp2196B - 1982 - Production and decomposition of forest litter fall on the Apalachicola River flood plain, Florida: Chapter B, Apalachicola River quality assessment","indexId":"wsp2196B","publicationYear":"1982","noYear":false,"chapter":"B","title":"Production and decomposition of forest litter fall on the Apalachicola River flood plain, Florida: Chapter B, Apalachicola River quality assessment"},"id":1}],"supersededBy":{"id":1310,"text":"wsp2196B - 1982 - Production and decomposition of forest litter fall on the Apalachicola River flood plain, Florida: Chapter B, Apalachicola River quality assessment","indexId":"wsp2196B","publicationYear":"1982","noYear":false,"title":"Production and decomposition of forest litter fall on the Apalachicola River flood plain, Florida: Chapter B, Apalachicola River quality assessment"},"lastModifiedDate":"2022-08-22T20:46:09.58696","indexId":"ofr82252","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"82-252","title":"Production and decomposition of forest litter fall on the Apalachicola River flood plain, Florida","docAbstract":"<p>Measurements of litter fall (leaves and other particulate organic material) and leaf decomposition were made on the bottom-land hardwood swamp of the Apalachicola River flood plain in 1979-80. Litter fall was collected monthly from nets located in 16 study plots. The plots represented five forest types in the swamp and levee areas of the Apalachicola River flood plain. Forty-three species of trees, vines, and other plants contributed to the total litter fall, but over 90 percent of the leaf material originated from 12 species. Nonleaf material comprised 42 percent of the total litter fall. Average litter fall was determined to be 800 grams per square meter per year, resulting in an annual deposition of 360,000 metric tons of organic material in the 454-square-kilometer flood plain.</p><p>The levee communities have lower tree biomass but higher tree diversity than swamp communities. The levee vegetation, with lower tree biomass, produces slightly more litter fall per ground surface area than the swamp vegetation. The swamps are dominated by three genera: tupelo (Nyssa), cypress (Taxodium), and ash (Fraxinus). These genera account for over 50 percent of the total leaf fall in the flood plain but they are the least productive, on a weight-per-biomass basis, of any of the 12 major leaf producers.</p><p>Decomposition rates of leaves from five common flood-plain tree species were measured using a standard leaf-bag technique. Leaf decomposition was highly species-dependent. Tupelo (Nyssa spp.) and sweetgum (Liquidambar styraciflua) leaves decomposed completely in 6 months when flooded by river water. Leaves of baldcypress (Taxodium distichum) and diamond-leaf oak (Quercus laurifolia) were much more resistant. Water hickory (Carya aquatica) leaves showed intermediate decomposition rates. Decomposition of all species was greatly reduced in dry environments. Carbon and biomass loss rates from the leaves were nearly linear over a 6-month period, but nitrogen and phosphorus leaching was nearly complete within 1 month. Much of the organic substance may be recycled in the forest ecosystem, but annual flooding of the river provides an important mechanism for mobilization of the litter-fall products.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr82252","usgsCitation":"Elder, J.F., and Cairns, D.J., 1982, Production and decomposition of forest litter fall on the Apalachicola River flood plain, Florida: U.S. Geological Survey Open-File Report 82-252, vii, 73 p., https://doi.org/10.3133/ofr82252.","productDescription":"vii, 73 p.","costCenters":[],"links":[{"id":405411,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0252/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":141040,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0252/report-thumb.jpg"}],"country":"United States","state":"Florida","otherGeospatial":"Apalachicola River flood 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,{"id":8747,"text":"ofr82910 - 1982 - Selected ground-water data, Sevier Desert, Utah, 1935-82","interactions":[],"lastModifiedDate":"2020-06-16T21:17:15.316532","indexId":"ofr82910","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"82-910","title":"Selected ground-water data, Sevier Desert, Utah, 1935-82","docAbstract":"<p>No abstract available.<br data-mce-bogus=\"1\"></p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr82910","collaboration":"Prepared in cooperation with the Utah Department of Natural Resources, Division of Water Rights","usgsCitation":"Enright, M., and Holmes, W.F., 1982, Selected ground-water data, Sevier Desert, Utah, 1935-82: U.S. Geological Survey Open-File Report 82-910, Report: iv, 59 p. 1 Plate: 23.38 x 22.00 inches, https://doi.org/10.3133/ofr82910.","productDescription":"Report: iv, 59 p. 1 Plate: 23.38 x 22.00 inches","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":142877,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0910/report-thumb.jpg"},{"id":375647,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0910/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":375646,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0910/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Utah","otherGeospatial":"Sevier 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,{"id":8777,"text":"ofr82775 - 1982 - Hydrology of the Arbuckle Mountain area, south-central Oklahoma","interactions":[{"subject":{"id":8777,"text":"ofr82775 - 1982 - Hydrology of the Arbuckle Mountain area, south-central Oklahoma","indexId":"ofr82775","publicationYear":"1982","noYear":false,"title":"Hydrology of the Arbuckle Mountain area, south-central Oklahoma"},"predicate":"SUPERSEDED_BY","object":{"id":70046124,"text":"70046124 - 1990 - Hydrology of the Arbuckle Mountains area, south-central Oklahoma","indexId":"70046124","publicationYear":"1990","noYear":false,"title":"Hydrology of the Arbuckle Mountains area, south-central Oklahoma"},"id":1}],"supersededBy":{"id":70046124,"text":"70046124 - 1990 - Hydrology of the Arbuckle Mountains area, south-central Oklahoma","indexId":"70046124","publicationYear":"1990","noYear":false,"title":"Hydrology of the Arbuckle Mountains area, south-central Oklahoma"},"lastModifiedDate":"2017-09-29T07:50:47","indexId":"ofr82775","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"82-775","title":"Hydrology of the Arbuckle Mountain area, south-central Oklahoma","docAbstract":"<p>Rocks that make up the Arbuckle-Simpson aquifer crop out over about 500 square miles in the Arbuckle Mountains province in south-central Oklahoma. The aquifer consists of limestone, dolomite, and sandstone of the Arbuckle and Simpson Groups of Late Cambrian to Middle Ordovician age and is about 5,000 to 9,000 feet thick. The rocks were subjected to intensive folding and faulting associated with major uplift of the area during Early to Late Pennsylvanian time. </p><p>Water in the aquifer is confined in some parts of the area, while in other parts it is unconfined. The average saturated thickness of the aquifer is about 3,500 feet in the outcrop area. Water levels measured in wells fluctuated from 8 to 53 feet each year, primarily in response to recharge from rainfall. </p><p>Recharge to the aquifer is estimated at about 4.7 inches per year. </p><p>The average storage coefficient of the aquifer is estimated at 0.008, and the average transmissivity is estimated at 15,000 feet squared per day. Based on an average saturated thickness of about 3,500 feet and a storage coefficient of 0.008, the volume of ground water contained in the 500-square-mile outcrop area is about 9 million acre-feet. An undetermined amount of fresh water probably exists in the aquifer around the periphery of the aquifer outcrop. </p><p>Base flow of streams that drain the aquifer accounts for about 60 percent of the total annual runoff from the outcrop area and is maintained by numerous springs. The close hydraulic connection between streams in the outcrop area and the aquifer is shown by a close correlation between base flow in Blue River and the fluctuation of ground-water levels in five wells in the Blue River basin. This correlation also exists between the discharge by Byrds Mill Spring and the fluctuation in water level in a nearby observation well; increase and decrease in spring discharge correspond to rise and fall of the water level in the well. </p><p>The chemical quality of water from the Arbuckle-Simpson aquifer is suitable for most industrial and municipal uses. The water is hard and of the bicarbonate type; the average hardness is about 340 milligrams per liter, and the average dissolved-solids concentration is about 360 milligrams per liter. Because springs issue from the aquifer and discharge to streams in the area, the quality of water from springs and base flow in streams is similar to that of ground water. The average dissolved-solids concentration of stream water is slightly less than that of water from wells and springs.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr82775","usgsCitation":"Fairchild, R.W., Hanson, R.L., and Davis, R.E., 1982, Hydrology of the Arbuckle Mountain area, south-central Oklahoma: U.S. Geological Survey Open-File Report 82-775, 156 p., https://doi.org/10.3133/ofr82775.","productDescription":"156 p.","numberOfPages":"170","costCenters":[],"links":[{"id":346189,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0775/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":143402,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0775/report-thumb.jpg"}],"country":"United States","state":"Oklahoma","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -97.37182617187499,\n              34.16295449004889\n            ],\n            [\n              -96.41189575195312,\n              34.16295449004889\n            ],\n            [\n              -96.41189575195312,\n              34.73484137177769\n            ],\n            [\n              -97.37182617187499,\n              34.73484137177769\n            ],\n            [\n              -97.37182617187499,\n              34.16295449004889\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a13e4b07f02db601ee9","contributors":{"authors":[{"text":"Fairchild, Roy W.","contributorId":79155,"corporation":false,"usgs":true,"family":"Fairchild","given":"Roy","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":158313,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hanson, Ronald L.","contributorId":65054,"corporation":false,"usgs":true,"family":"Hanson","given":"Ronald","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":158311,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Davis, Robert E.","contributorId":10403,"corporation":false,"usgs":true,"family":"Davis","given":"Robert","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":158312,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":8787,"text":"ofr82156 - 1982 - Effects of Late Cretaceous and Cenozoic faulting on the geology and hydrology of the coastal plain near the Savannah River, Georgia and South Carolina","interactions":[],"lastModifiedDate":"2016-12-14T12:22:31","indexId":"ofr82156","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"82-156","title":"Effects of Late Cretaceous and Cenozoic faulting on the geology and hydrology of the coastal plain near the Savannah River, Georgia and South Carolina","docAbstract":"Geologic and hydrologic investigations by the U.S. Geological Survey have defined stratigraphic and hydraulic anomalies suggestive of faulting within Coastal Plain sediments between the Ogeechee River in east-central Georgia and the Edisto River in west-central South Carolina. Examination of borehole cuttings, cores, and geophysical logs from test wells indicate that Triassic rocks and Upper Cretaceous and lower Tertiary Coastal Plain sediments near the Barnwell-Allendale County line near Millett, South Carolina, are offset by a northeast-trending fault downthrown to the northwest. The location of this suspected Coastal Plain fault generally coincides with the location of an inferred fault in basement rocks as interpreted from aeromagnetic surveys. Apparent vertical offsets range from about 700 feet at the base of Upper Cretaceous sediments to about 20 feet in strata of Late Eocene age. As a result, the Upper Cretaceous Middendorf Formation which directly overlies crystalline and Triassic rocks updip (northwest) of this fault, is absent immediately downdip of the fault. The thickness of Tipper Cretaceous sediments is also sharply reduced from about 700 feet to about 180 feet across the fault.\r\n\r\nSediments of the basal Coastal Plain aquifer are largely truncated by uplifted Triassic rocks at the fault near Millett, South Carolina. Lateral ground-water flow near the Savannah River Is consequently disrupted updip of the fault and ground water is transferred vertically into overlying sediments and possibly into the Savannah River. At several locations, abrupt changes in potentiometric head occur across this fault. Computed transmissivity of the basal Coastal Plain aquifer is also radically reduced downdip of the fault, sharply reversing a downdip trend of rapidly increasing aquifer transmissivity. \r\n\r\nOther anomalous potentiometric data along a northeast-trending line between Statesboro, Georgia, and Fairfax, South Carolina, suggest the possibility of similar faulting in correlative geologic units. The location of the suspected fault near Statesboro, Georgia, generally coincides with the eastward extension of the Gulf Trough, a regional potentiometric anomaly in central Georgia.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82156","usgsCitation":"Faye, R., and Prowell, D., 1982, Effects of Late Cretaceous and Cenozoic faulting on the geology and hydrology of the coastal plain near the Savannah River, Georgia and South Carolina: U.S. Geological Survey Open-File Report 82-156, 85 p., 8 over-size sheets, ill., maps ;28 cm., https://doi.org/10.3133/ofr82156.","productDescription":"85 p., 8 over-size sheets, ill., maps ;28 cm.","costCenters":[{"id":13634,"text":"South Atlantic Water Science 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,{"id":8793,"text":"ofr82324 - 1982 - Radioactivity and geochemistry of selected mineral-spring waters in the Western United States; basic data and multivariate statistical analysis","interactions":[],"lastModifiedDate":"2012-02-02T00:06:19","indexId":"ofr82324","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"82-324","title":"Radioactivity and geochemistry of selected mineral-spring waters in the Western United States; basic data and multivariate statistical analysis","docAbstract":"Multivariate statistical analyses were performed on data from 156 mineral-spring sites in nine Western States to analyze relationships among the various parameters measured in the spring waters. Correlation analysis and R-mode factor analysis indicate that three major factors affect water composition in the spring systems studied: (1) duration of water circulation, (2) depth of water circulation, and (3) partial pressure of carbon dioxide. An examination of factor scores indicates that several types of hydrogeologic systems were sampled. Most of the samples are (1) older water from deeper circulating systems having relatively high salinity, high temperature, and low Eh or (2) younger water from shallower circulating systems having relatively low salinity, low temperature, and high Eh. The rest of the samples are from more complex systems. Any of the systems can have a relatively high or low content of dissolved carbonate species, resulting in a low or high pH, respectively. Uranium concentrations are commonly higher in waters of relatively low temperature and high Eh, and radium concentrations are commonly higher in waters having a relatively high carbonate content (low pH) and, secondarily, relatively high salinity. \r\n\r\nWater samples were collected and (or) measurements were taken at 156 of the 171 mineral-spring sites visited. Various samples were analyzed for radium, uranium, radon, helium, and radium-228 as well as major ions and numerous trace elements. On-site measurements for physical properties including temperature, specific conductance, pH, Eh, and dissolved oxygen were made. All constituents and properties show a wide range of values. Radium concentrations range from less than 0.01 to 300 picocuries per liter; they average 1.48 picocuries per liter and have an anomaly threshold value of 171 picocuries per liter for the samples studied. Uranium concentrations range from less than 0.01 to 120 micrograms per liter and average 0.26 micrograms per liter; they have an anomaly threshold value of 48.1 micrograms per liter. Radon content ranges from less than 10 to 110,000 picocuries per liter, averages 549 picocuries per liter and has an anomaly threshold of 20,400 picocuries per liter. Helium content ranges from -1,300 to +13,000 parts per billion relative to atmospheric helium; it averages +725 parts per billion and has an anomaly threshold of 10,000 parts per billion. Radium-228 concentrations range from less than 2.0 to 33 picocuries per liter; no anomaly threshold was determined owing to the small number of samples. All of the anomaly thresholds may be somewhat high because the sampling was biased toward springs likely to be radioactive. \r\n\r\nThe statistical variance in radium and uranium concentrations unaccounted for by the identified factors testifies to the complexity of some hydrogeologic systems. Unidentified factors related to geologic setting and the presence of uranium-rich rocks in the systems also affect the observed concentrations of the radioactive elements in the water. The association of anomalous radioactivity in several springs with nearby known uranium occurrences indicates that other springs having anomalous radioactivity may also be associated with uranium occurrences as yet undiscovered.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82324","usgsCitation":"Felmlee, J., and Cadigan, R.A., 1982, Radioactivity and geochemistry of selected mineral-spring waters in the Western United States; basic data and multivariate statistical analysis: U.S. Geological Survey Open-File Report 82-324, ii, 107 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr82324.","productDescription":"ii, 107 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":142733,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0324/report-thumb.jpg"},{"id":36377,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0324/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a60e4b07f02db634cbd","contributors":{"authors":[{"text":"Felmlee, J.K.","contributorId":106114,"corporation":false,"usgs":true,"family":"Felmlee","given":"J.K.","email":"","affiliations":[],"preferred":false,"id":158341,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Cadigan, R. A.","contributorId":57844,"corporation":false,"usgs":true,"family":"Cadigan","given":"R.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":158340,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":8796,"text":"ofr82265 - 1982 - Selected hydrogeologic data from southern Sweet Grass County, south-central Montana","interactions":[],"lastModifiedDate":"2012-02-02T00:06:19","indexId":"ofr82265","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"82-265","title":"Selected hydrogeologic data from southern Sweet Grass County, south-central Montana","docAbstract":"Selected hydrogeologic data from Sweet Grass County south of the Yellowstone River have been compiled to show baseline ground-water conditions. Included are records from a 1981 onsite inventory of 94 water wells and 30 springs. Chemical analyses of water show the major cation and anion concentrations for 40 wells and 14 springs. Concentrations of 17 trace elements in water from 12 of the wells and 9 of the springs were determined by an argon coupled emission spectrometer. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82265","usgsCitation":"Feltis, R., and Wood, W., 1982, Selected hydrogeologic data from southern Sweet Grass County, south-central Montana: U.S. Geological Survey Open-File Report 82-265, 17 p., 1 over-size sheet, ill., maps ;28 cm., https://doi.org/10.3133/ofr82265.","productDescription":"17 p., 1 over-size sheet, ill., maps ;28 cm.","costCenters":[],"links":[{"id":142754,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0265/report-thumb.jpg"},{"id":36380,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0265/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":36381,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0265/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a07e4b07f02db5f933b","contributors":{"authors":[{"text":"Feltis, R.D.","contributorId":93467,"corporation":false,"usgs":true,"family":"Feltis","given":"R.D.","affiliations":[],"preferred":false,"id":158347,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wood, W.A.","contributorId":6048,"corporation":false,"usgs":true,"family":"Wood","given":"W.A.","email":"","affiliations":[],"preferred":false,"id":158346,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":8822,"text":"ofr82354 - 1982 - Chemical and physical characteristics of water in estuaries of Texas, October 1976-September 1978","interactions":[],"lastModifiedDate":"2016-08-11T14:46:56","indexId":"ofr82354","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"82-354","title":"Chemical and physical characteristics of water in estuaries of Texas, October 1976-September 1978","docAbstract":"<p>The Texas Water Plan (1968) proposes development and utilization of water resources in Texas and includes provision for the use and preservation of water in the estuaries of the State. Management of estuarine waters requires knowledge of the hydrodynamics and of the continuing changes in the chemical and physical characteristics of water in the estuaries.</p>\n<p>In September 1967, the U.S. Geological Survey and the Texas Department of Water Resources began a cooperative water-resources investigation of the principal estuaries along the Texas coast (fig. 1) except the Rio Grande estuary,&nbsp;which is under the jurisdiction of the International Boundary and Water Commission, United States and Mexico.</p>\n<p>The objectives of the investigation are to define: (1) The occurrence, source, and distribution of nutrients; (2) the physical, organic, and inorganic water-quality constituents and their areal distribution and time variations; (3) the chemical and physical characteristics of Gulf water that enters the estuaries; (4) the occurrence, quality, quantity, and dispersion of drainage entering the estuarine systems; and (5) the current patterns, directions, and rates of water movement.</p>\n<p>The coastal waters of Texas are not classical estuaries, but are similar to them in ecosystems and mixing phenomena. A description of various types of estuaries is presented in \"Estuaries\" edited by Lauff (1967, p. 3-11). The term estuary as used in this report, refers to concomitant water bodies in which streamflow mixes with seawater.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Austin, TX","doi":"10.3133/ofr82354","usgsCitation":"Fisher, J., 1982, Chemical and physical characteristics of water in estuaries of Texas, October 1976-September 1978: U.S. Geological Survey Open-File Report 82-354, Report: 213 p.; 3 Plates: 9.90 x 14.91 inches or smaller, https://doi.org/10.3133/ofr82354.","productDescription":"Report: 213 p.; 3 Plates: 9.90 x 14.91 inches or smaller","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":141691,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0354/report-thumb.jpg"},{"id":36397,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0354/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":36398,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0354/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":36399,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0354/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":36400,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0354/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e1e4b07f02db5e47f9","contributors":{"authors":[{"text":"Fisher, J.C.","contributorId":99974,"corporation":false,"usgs":true,"family":"Fisher","given":"J.C.","email":"","affiliations":[],"preferred":false,"id":158389,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":8829,"text":"ofr82888 - 1982 - Origin of the Mariano Lake uranium deposit, McKinley County, New Mexico","interactions":[],"lastModifiedDate":"2020-04-30T16:28:14.587118","indexId":"ofr82888","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"82-888","title":"Origin of the Mariano Lake uranium deposit, McKinley County, New Mexico","docAbstract":"<p>The Mariano Lake uranium deposit, hosted by the Brushy Basin Member of the Jurassic Morrison Formation, occurs in the trough of an east-west trending syncline at the western end of the Smith Lake-Mariano Lake group of uranium deposits near Crownpoint, New Mexico. The orebody, which contains abundant amorphous organic material, is situated on the reduced side of a regional reduction-oxidation (redox) interface. The presence of amorphous organic material suggests the orebody may represent a tabular (primary) deposit, whereas the close proximity of the orebody to the redox interface is suggestive that uranium was secondarily redistributed by oxidative processes from pre-existing tabular orebodies. Uranium contents correlate positively with both organic carbon and vanadium contents. Petrographic evidence and scanning electron microscope-energy dispersive analyses point to uranium residence in the epigentically introduced amorphous organic material, which coats detrital grains and fills voids. Uranium mineralization was preceded by the following diagenetic alterations: precipitation of pyrite (ẟ<sup>34</sup>S values ranging from-11.0 to-38.2 per mil); precipitation of mixed-layer smectite-illite clays; partial dissolution of some of the detrital feldspar population; and precipitation of quartz and adularia overgrowths. Alterations associated with uranium mineralization include emplacement of amorphous organic material (possibly uranium bearing); destruction of detrital iron-titanium oxide grains; coprecipitation of chlorite and microcrystalline quartz, and precipitation of pyrite and marcasite (ẟ<sup>34</sup>S values for these sulfides ranging from -29.4 to -41.6 per mil). After mineralization, calcite, dolomite, barite, and kaolinite precipitated, and authigenic iron disulfides were replaced by ferric oxides and hydroxides. Geochemical data (primarily the positive correlation of uranium content to both organic carbon and vanadium contents) and petrographic observations (epigentically introduced amorphous organic matter and uranium residence in this organic matter) indicate that the Mariano Lake orebody is a tabular-type uranium deposit. Oxidative processes have not noticeably redistributed and reconcentrated primary uranium in the immediate vicinity of the deposit nor have they greatly modified geochemical characteristics in the ore. Preservation of the Mariano Lake deposit may not only be related to its position along the synclinal trough, where oxidative destruction of the orebody has been inhibited by stagnation of oxidizing ground waters by the structure, but also due to the deflection of ground waters (resulting from low orebody porosity) around the orebody.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr82888","usgsCitation":"Fishman, N.S., and Reynolds, R.L., 1982, Origin of the Mariano Lake uranium deposit, McKinley County, New Mexico: U.S. Geological Survey Open-File Report 82-888, iii, 52 p., https://doi.org/10.3133/ofr82888.","productDescription":"iii, 52 p.","costCenters":[{"id":318,"text":"Geosciences and Environmental Change Science Center","active":true,"usgs":true}],"links":[{"id":141608,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0888/report-thumb.jpg"},{"id":36405,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0888/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"New Mexico","county":"McKinley County","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-109.0452,36.006],[-108.7687,36.0063],[-108.3738,36.0044],[-108.2646,36.0038],[-108.1559,36.0027],[-108.1468,36.0028],[-108.1411,36.0029],[-108.1224,36.0028],[-107.8738,36.0034],[-107.8351,36.0035],[-107.6776,36.0031],[-107.66,36.0034],[-107.6423,36.0032],[-107.6247,36.0034],[-107.6213,36.003],[-107.6042,36.0032],[-107.5866,36.003],[-107.5718,36.0027],[-107.5541,36.0025],[-107.5513,36.0026],[-107.5161,36.0026],[-107.4421,36.0008],[-107.4068,36.0007],[-107.3875,36.0009],[-107.3397,36.0006],[-107.317,36.0008],[-107.3056,36.0005],[-107.3054,35.991],[-107.3058,35.9765],[-107.3055,35.9311],[-107.3051,35.8744],[-107.3049,35.8295],[-107.3047,35.8168],[-107.3053,35.7864],[-107.3054,35.7573],[-107.3057,35.7419],[-107.3049,35.7301],[-107.3052,35.7151],[-107.305,35.6997],[-107.3053,35.6852],[-107.305,35.6707],[-107.3048,35.6552],[-107.3046,35.6439],[-107.3041,35.6139],[-107.3032,35.5277],[-107.3035,35.4787],[-107.3025,35.4247],[-107.3016,35.3021],[-107.518,35.3036],[-107.5231,35.3036],[-107.6183,35.3059],[-107.6229,35.3059],[-107.6231,35.3159],[-107.6243,35.3485],[-107.7287,35.3489],[-107.7295,35.3366],[-107.7288,35.3062],[-107.7812,35.3063],[-107.8111,35.3063],[-107.8297,35.3065],[-107.8336,35.3064],[-107.9159,35.3065],[-107.9351,35.3066],[-107.9396,35.3065],[-107.974,35.3064],[-107.992,35.3066],[-108.0473,35.307],[-108.143,35.3057],[-108.151,35.307],[-108.2558,35.3077],[-108.364,35.3065],[-108.4661,35.3081],[-108.4644,35.2214],[-108.4659,35.1623],[-108.4661,35.1355],[-108.4673,35.0501],[-108.4678,34.9597],[-108.497,34.96],[-108.52,34.96],[-108.7809,34.9595],[-109.0458,34.9611],[-109.0458,35.166],[-109.0457,35.1796],[-109.0457,35.1941],[-109.0457,35.2078],[-109.0457,35.2228],[-109.0457,35.2359],[-109.0456,35.3531],[-109.0457,35.6637],[-109.0452,36.006]]]},\"properties\":{\"name\":\"McKinley\",\"state\":\"NM\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a61e4b07f02db635e15","contributors":{"authors":[{"text":"Fishman, Neil S.","contributorId":106464,"corporation":false,"usgs":true,"family":"Fishman","given":"Neil","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":158404,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Reynolds, Richard L. 0000-0002-4572-2942 rreynolds@usgs.gov","orcid":"https://orcid.org/0000-0002-4572-2942","contributorId":139068,"corporation":false,"usgs":true,"family":"Reynolds","given":"Richard","email":"rreynolds@usgs.gov","middleInitial":"L.","affiliations":[{"id":318,"text":"Geosciences and Environmental Change Science Center","active":true,"usgs":true}],"preferred":true,"id":158403,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":8856,"text":"ofr82783 - 1982 - The lanthanides and yttrium in minerals of the apatite group; a review","interactions":[],"lastModifiedDate":"2012-02-02T00:06:11","indexId":"ofr82783","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"82-783","title":"The lanthanides and yttrium in minerals of the apatite group; a review","docAbstract":"More than 1000 analyses have been tabulated of the distribution of the lanthanides and yttrium in minerals of the apatite group, recalculated to atomic percentages. Average compositions have been calculated for apatites from 14 types of rocks. These show a progressive change of composition from apatites of granitic pegmatites, highest in the heavy lanthanides and yttrium, to those from alkalic pegmatites, highest in the light lanthanides and lowest in yttrium. This progression is clearly shown in plots of S (= at % La+Ce+Pr) vs the ratio La/Nd and of S vs the ratio 100Y/(Y+Ln), where Ln is the sum of the lanthanides. \r\n\r\nApatites of sedimentary phosphorites occupy a special position, being relatively depleted in Ce and relatively enriched in yttrium and the heavy lanthanides, consequences of deposition from sea water. \r\n\r\nApatites associated with iron ores are close in composition to apatites of carbonatites, alkalic ultramafic, and ultramafic rocks, being enriched in the light lanthanides and depleted in the heavy lanthanides. Their compositions do not support the hypothesis of Parak that the Kiruna-type ores are of sedimentary origin. \r\n\r\nTable 9 and Figures 1-3 show the dependence of lanthanide distribution on the nature of the host rock. Although a given analysis of the lanthanides does not unequivocally permit certain identification of the host rock, it can indicate a choice of highly probable host rocks.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82783","usgsCitation":"Fleischer, M., and Altschuler, Z., 1982, The lanthanides and yttrium in minerals of the apatite group; a review: U.S. Geological Survey Open-File Report 82-783, i, 156 p., ill. ;28 cm., https://doi.org/10.3133/ofr82783.","productDescription":"i, 156 p., ill. ;28 cm.","costCenters":[],"links":[{"id":141107,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0783/report-thumb.jpg"},{"id":36434,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0783/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e48e8e4b07f02db55334c","contributors":{"authors":[{"text":"Fleischer, Michael","contributorId":65835,"corporation":false,"usgs":true,"family":"Fleischer","given":"Michael","email":"","affiliations":[],"preferred":false,"id":158444,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Altschuler, Z. S.","contributorId":42962,"corporation":false,"usgs":true,"family":"Altschuler","given":"Z. S.","affiliations":[],"preferred":false,"id":158443,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":8866,"text":"ofr82335 - 1982 - Compilation of selected ground-water-quality data from the San Joaquin Valley, California","interactions":[],"lastModifiedDate":"2012-02-02T00:06:18","indexId":"ofr82335","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"82-335","title":"Compilation of selected ground-water-quality data from the San Joaquin Valley, California","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82335","usgsCitation":"Fogelman, R.P., 1982, Compilation of selected ground-water-quality data from the San Joaquin Valley, California: U.S. Geological Survey Open-File Report 82-335, iii, 279 p. :ill., map ;28 cm., https://doi.org/10.3133/ofr82335.","productDescription":"iii, 279 p. :ill., map ;28 cm.","costCenters":[],"links":[{"id":142809,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0335/report-thumb.jpg"},{"id":36438,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0335/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1de4b07f02db6a967c","contributors":{"authors":[{"text":"Fogelman, R. P.","contributorId":96688,"corporation":false,"usgs":true,"family":"Fogelman","given":"R.","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":158460,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":8871,"text":"ofr78556I - 1982 - Drainage areas of surface water bodies of central Maine coastal river basins","interactions":[{"subject":{"id":8871,"text":"ofr78556I - 1982 - Drainage areas of surface water bodies of central Maine coastal river basins","indexId":"ofr78556I","publicationYear":"1982","noYear":false,"chapter":"I","title":"Drainage areas of surface water bodies of central Maine coastal river basins"},"predicate":"IS_PART_OF","object":{"id":7104,"text":"ofr78556 - 1978 - Drainage areas in Maine","indexId":"ofr78556","publicationYear":"1978","noYear":false,"title":"Drainage areas in Maine"},"id":1}],"isPartOf":{"id":7104,"text":"ofr78556 - 1978 - Drainage areas in Maine","indexId":"ofr78556","publicationYear":"1978","noYear":false,"title":"Drainage areas in Maine"},"lastModifiedDate":"2026-03-06T17:41:50.444588","indexId":"ofr78556I","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"78-556","chapter":"I","title":"Drainage areas of surface water bodies of central Maine coastal river basins","docAbstract":"<p>The report contains drainage-area values for: lakes and ponds included in the MIDAS (Maine Informational Display Analysis System) File 906-Z, streams that drain an area greater than 25 square miles, dam sites, and locations where hydrologic data are available. Supplemental information includes State and Federal location systems used to identify these lake and stream sites.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr78556I","collaboration":"Prepared in cooperation with the Maine Department of Environmental Protection","usgsCitation":"Fontaine, R.A., 1982, Drainage areas of surface water bodies of central Maine coastal river basins: U.S. Geological Survey Open-File Report 78-556, v, 27 p., https://doi.org/10.3133/ofr78556I.","productDescription":"v, 27 p.","costCenters":[],"links":[{"id":422920,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1978/0556-i/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":142628,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1978/0556-i/report-thumb.jpg"}],"country":"United States","state":"Maine","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -70.14536238431826,\n              44.57917477028707\n            ],\n            [\n              -70.14536238431826,\n              43.6956341707274\n            ],\n            [\n              -68.91970281136494,\n              43.6956341707274\n            ],\n            [\n              -68.91970281136494,\n              44.57917477028707\n            ],\n            [\n              -70.14536238431826,\n              44.57917477028707\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b05e4b07f02db699dcc","contributors":{"authors":[{"text":"Fontaine, Richard A. rfontain@usgs.gov","contributorId":2379,"corporation":false,"usgs":true,"family":"Fontaine","given":"Richard","email":"rfontain@usgs.gov","middleInitial":"A.","affiliations":[],"preferred":true,"id":158466,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
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