{"pageNumber":"540","pageRowStart":"13475","pageSize":"25","recordCount":16500,"records":[{"id":66199,"text":"i856J - 1983 - Well yields and chemical quality of water from water-table aquifers in the greater Denver area, Front Range urban corridor, Colorado","interactions":[],"lastModifiedDate":"2025-08-13T17:47:22.743757","indexId":"i856J","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":320,"text":"IMAP","code":"I","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"856","chapter":"J","title":"Well yields and chemical quality of water from water-table aquifers in the greater Denver area, Front Range urban corridor, Colorado","docAbstract":"<p>Knowledge of the well yields and chemical quality of water from water-table aquifers is useful to State and local officials in making decisions on land use and in locating water supplies in the rapidly urbanizing greater Denver are. This report presents the results of a 2-year investigation to obtain this knowledge and to relate the results to urban planning in the greater Denver area. The report is one of a series of geologic and hydrologic reports prepared by the U.S. Geological Survey to demonstrate the usefulness of Earth-science information in urban planning.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/i856J","usgsCitation":"Hillier, D.E., Schneider, P.A., and Hutchinson, E., 1983, Well yields and chemical quality of water from water-table aquifers in the greater Denver area, Front Range urban corridor, Colorado: U.S. Geological Survey IMAP 856, Cover sheet: 1 p.; 2 Plates: 36.32 x 33.61 inches and 37.61 x 33.20 inches, https://doi.org/10.3133/i856J.","productDescription":"Cover sheet: 1 p.; 2 Plates: 36.32 x 33.61 inches and 37.61 x 33.20 inches","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":494045,"rank":5,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_9747.htm","linkFileType":{"id":5,"text":"html"}},{"id":255696,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/imap/0856j/report-thumb.jpg"},{"id":255695,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/imap/0856j/report.pdf","text":"Cover sheet","size":"27.58 KB","linkFileType":{"id":1,"text":"pdf"},"description":"Cover sheet"},{"id":255694,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/0856j/plate-2.pdf","text":"Plate 2","size":"16.90 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Plate 2"},{"id":255693,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/0856j/plate-1.pdf","text":"Plate 1","size":"15.71 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Plate 1"}],"country":"United States","state":"Colorado","city":"Denver","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -104.625,\n              39.375\n            ],\n            [\n              -104.625,\n              40\n            ],\n            [\n              -105.375,\n              40\n            ],\n            [\n              -105.375,\n              39.375\n            ],\n            [\n              -104.625,\n              39.375\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e2e4b07f02db5e4b03","contributors":{"authors":[{"text":"Hillier, D. E.","contributorId":78386,"corporation":false,"usgs":true,"family":"Hillier","given":"D.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":274151,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Schneider, P. A. Jr.","contributorId":18771,"corporation":false,"usgs":true,"family":"Schneider","given":"P.","suffix":"Jr.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":274149,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hutchinson, E. C.","contributorId":26373,"corporation":false,"usgs":true,"family":"Hutchinson","given":"E. C.","affiliations":[],"preferred":false,"id":274150,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":68543,"text":"ha670 - 1983 - Predevelopment and 1980 water table in the northern high plains of Colorado; and water-level changes, predevelopment to 1980, and 1975 to 1980","interactions":[],"lastModifiedDate":"2012-02-02T00:13:40","indexId":"ha670","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":318,"text":"Hydrologic Atlas","code":"HA","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"670","title":"Predevelopment and 1980 water table in the northern high plains of Colorado; and water-level changes, predevelopment to 1980, and 1975 to 1980","language":"ENGLISH","doi":"10.3133/ha670","usgsCitation":"Borman, R.G., 1983, Predevelopment and 1980 water table in the northern high plains of Colorado; and water-level changes, predevelopment to 1980, and 1975 to 1980: U.S. Geological Survey Hydrologic Atlas 670, 3 maps on 1 sheet :col. ;30 x 65 cm. and smaller, sheet 79 x 71 cm., folded in envelope 30 x 24 cm., https://doi.org/10.3133/ha670.","productDescription":"3 maps on 1 sheet :col. ;30 x 65 cm. and smaller, sheet 79 x 71 cm., folded in envelope 30 x 24 cm.","costCenters":[],"links":[{"id":186208,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":90161,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/670/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"500000","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49fbe4b07f02db5f4821","contributors":{"authors":[{"text":"Borman, Ronald G.","contributorId":69944,"corporation":false,"usgs":true,"family":"Borman","given":"Ronald","email":"","middleInitial":"G.","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":278428,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":68545,"text":"ha669 - 1983 - Geology, altitude, and depth of the bedrock surface beneath the Ogallala Formation in the northern High Plains of Colorado","interactions":[],"lastModifiedDate":"2012-02-10T00:11:11","indexId":"ha669","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":318,"text":"Hydrologic Atlas","code":"HA","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"669","title":"Geology, altitude, and depth of the bedrock surface beneath the Ogallala Formation in the northern High Plains of Colorado","language":"ENGLISH","doi":"10.3133/ha669","usgsCitation":"Borman, R.G., and Meredith, T.S., 1983, Geology, altitude, and depth of the bedrock surface beneath the Ogallala Formation in the northern High Plains of Colorado: U.S. Geological Survey Hydrologic Atlas 669, 2 maps on 1 sheet :col. ;sheet 79 x 84 cm., folded in envelope 30 x 24 cm., https://doi.org/10.3133/ha669.","productDescription":"2 maps on 1 sheet :col. ;sheet 79 x 84 cm., folded in envelope 30 x 24 cm.","costCenters":[],"links":[{"id":190301,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":90173,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/669/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"500000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -104,38 ], [ -104,41 ], [ -102.68333333333334,41 ], [ -102.68333333333334,38 ], [ -104,38 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67c6ba","contributors":{"authors":[{"text":"Borman, Ronald G.","contributorId":69944,"corporation":false,"usgs":true,"family":"Borman","given":"Ronald","email":"","middleInitial":"G.","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":278433,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Meredith, Thomas S.","contributorId":21156,"corporation":false,"usgs":true,"family":"Meredith","given":"Thomas","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":278432,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":68189,"text":"ha661 - 1983 - Channel changes of Powder River, 1938-78, Powder River County, Montana","interactions":[],"lastModifiedDate":"2012-02-10T00:11:30","indexId":"ha661","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":318,"text":"Hydrologic Atlas","code":"HA","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"661","title":"Channel changes of Powder River, 1938-78, Powder River County, Montana","language":"ENGLISH","doi":"10.3133/ha661","usgsCitation":"Martinson, H.A., and Meade, R.H., 1983, Channel changes of Powder River, 1938-78, Powder River County, Montana: U.S. Geological Survey Hydrologic Atlas 661, 11 maps on 3 sheets :col. ;17 x 95 cm., on sheets 99 x 102 cm., folded in envelope 30 x 24 cm., https://doi.org/10.3133/ha661.","productDescription":"11 maps on 3 sheets :col. ;17 x 95 cm., on sheets 99 x 102 cm., folded in envelope 30 x 24 cm.","costCenters":[],"links":[{"id":185564,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":89514,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/661/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":89515,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/661/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":89516,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/661/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"24000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -105.91666666666667,45 ], [ -105.91666666666667,45.6175 ], [ -105.25,45.6175 ], [ -105.25,45 ], [ -105.91666666666667,45 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e4e4b07f02db5e6307","contributors":{"authors":[{"text":"Martinson, Holly A.","contributorId":50215,"corporation":false,"usgs":true,"family":"Martinson","given":"Holly","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":277807,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Meade, Robert H. 0000-0002-4965-3040 rhmeade@usgs.gov","orcid":"https://orcid.org/0000-0002-4965-3040","contributorId":2744,"corporation":false,"usgs":true,"family":"Meade","given":"Robert","email":"rhmeade@usgs.gov","middleInitial":"H.","affiliations":[{"id":5044,"text":"National Research Program - Central Branch","active":true,"usgs":true}],"preferred":true,"id":277806,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":68132,"text":"ha649 - 1983 - Development of irrigation in the Central Valley of California","interactions":[],"lastModifiedDate":"2012-02-10T00:11:29","indexId":"ha649","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":318,"text":"Hydrologic Atlas","code":"HA","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"649","title":"Development of irrigation in the Central Valley of California","language":"ENGLISH","doi":"10.3133/ha649","usgsCitation":"Nady, P., and Larragueta, L.L., 1983, Development of irrigation in the Central Valley of California: U.S. Geological Survey Hydrologic Atlas 649, 2 maps :col. ;sheets 129 x 89 cm. and 129 x 74 cm., folded in envelope 30 x 24 cm., https://doi.org/10.3133/ha649.","productDescription":"2 maps :col. ;sheets 129 x 89 cm. and 129 x 74 cm., folded in envelope 30 x 24 cm.","costCenters":[],"links":[{"id":186675,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":89432,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/649/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":89433,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/649/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"500000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -12.333333333333334,35 ], [ -12.333333333333334,40 ], [ -12.5,40 ], [ -12.5,35 ], [ -12.333333333333334,35 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9be4b07f02db65decd","contributors":{"authors":[{"text":"Nady, Paul","contributorId":26703,"corporation":false,"usgs":true,"family":"Nady","given":"Paul","email":"","affiliations":[],"preferred":false,"id":277702,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Larragueta, Lori L.","contributorId":30298,"corporation":false,"usgs":true,"family":"Larragueta","given":"Lori","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":277703,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":58005,"text":"ofr83764 - 1983 - Hydrologic monitoring in the area of the Tennessee-Tombigbee Waterway, Mississippi-Alabama : fiscal year 1982","interactions":[],"lastModifiedDate":"2012-02-02T00:12:31","indexId":"ofr83764","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-764","title":"Hydrologic monitoring in the area of the Tennessee-Tombigbee Waterway, Mississippi-Alabama : fiscal year 1982","language":"ENGLISH","doi":"10.3133/ofr83764","usgsCitation":"Morris, F., 1983, Hydrologic monitoring in the area of the Tennessee-Tombigbee Waterway, Mississippi-Alabama : fiscal year 1982: U.S. Geological Survey Open-File Report 83-764, iv, 189 leaves : ill., map ; 29 x 40 cm., https://doi.org/10.3133/ofr83764.","productDescription":"iv, 189 leaves : ill., map ; 29 x 40 cm.","costCenters":[],"links":[{"id":182250,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a1ae4b07f02db606700","contributors":{"authors":[{"text":"Morris, Fred","contributorId":54197,"corporation":false,"usgs":true,"family":"Morris","given":"Fred","affiliations":[],"preferred":false,"id":258133,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":29754,"text":"wri834202 - 1983 - Hydrology of an abandoned coal-mining area near McCurtain, Haskell County, Oklahoma","interactions":[],"lastModifiedDate":"2012-02-02T00:08:51","indexId":"wri834202","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-4202","title":"Hydrology of an abandoned coal-mining area near McCurtain, Haskell County, Oklahoma","docAbstract":"Water quality was investigated from October 1980 to May 1983 in an area of abandoned coal mines in Haskell county, Oklahoma. Bedrock in the area is shale, siltstone, sandstone, and the McAlester (Stigler) and Hartshorne coals of the McAlester Formation and Hartshorne Sandstone of Pennsylvanian age. The two coal beds, upper and lower Hartshorne, associated with the Hartshorne Sandstone converge or are separated by a few feet or less of bony coal or shale in the McCurtain area. Many small faults cut the Hartshorne coal in all the McCurtain-area mines. The main avenues of water entry to and movement through the bedrock are the exposed bedding-plane openings between layers of sandstone, partings between laminae of shale, fractures and joints developed during folding and faulting laminae of shale, fractures and joints developed during folding and faulting of the brittle rocks, and openings caused by surface mining--the overburden being shattered and broken to form spoil. Water-table conditions exist in bedrock and spoil in the area. Mine pond water is in direct hydraulic connections with water in the spoil piles and the underlying Hartshorne Sandstone.\r\nSulfate is the best indicator of the presence of coal-mine drainage in both surface and ground water in the Oklahoma coal field. Median sulfate concentrations for four sites on Mule Creek ranged from 26 to 260 milligrams per liter. Median sulfate concentrations increased with increased drainage from unreclaimed mined areas. The median sulfate concentration in Mule Creek where it drains the reclaimed area is less than one-third of that at the next site downstream where the stream begins to drain abandoned (unreclaimed) mine lands.\r\n\r\nWater from Mule Creek predominantly is a sodium sulfate type. Maximum and median values for specific conductance and concentrations of calcium, magnesium, sodium, sulfate, chloride, dissolved solids, and alkalinity increase as Mule Creek flows downstream and drains increasing areas of abandoned (unreclaimed) mining lands. Constituent concentrations in Mule Creek, except those for dissolved solids, iron, manganese, and sulfate, generally do not exceed drinking-water limits. Reclamation likely would result in decreased concentrations of dissolved solids, calcium, magnesium, sodium, sulfate, and alkalinity in Mule Creek in the vicinity of the reclaimed area.\r\n\r\nGround water in the area is moderately hard to very hard alkaline water with a median pH of 7.2 to 7.6. It predominately is a sodium sulfate type and, except for dissolved solids, iron manganese, and sulfate, constituent concentrations generally do not exceed drinking-water limits. Ground-water quality would likely be unchanged by reclamation.\r\n\r\nThe quality of water in the two mine ponds is quite similar to that of the shallow ground water in the area. Constituents in water from both ponds generally do not exceed drinking-water limits and the water quality is unlikely to be changed by reclamation in the area.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri834202","usgsCitation":"Slack, L.J., 1983, Hydrology of an abandoned coal-mining area near McCurtain, Haskell County, Oklahoma: U.S. Geological Survey Water-Resources Investigations Report 83-4202, v, 117 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri834202.","productDescription":"v, 117 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":124782,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1983/4202/report-thumb.jpg"},{"id":58548,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1983/4202/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":58549,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1983/4202/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49dee4b07f02db5e2ef3","contributors":{"authors":[{"text":"Slack, L. J.","contributorId":44157,"corporation":false,"usgs":true,"family":"Slack","given":"L.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":202062,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":45925,"text":"ofr82522 - 1983 - Hydrologic quadrangles, Bithlo, Florida","interactions":[],"lastModifiedDate":"2012-02-02T00:10:58","indexId":"ofr82522","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"82-522","title":"Hydrologic quadrangles, Bithlo, Florida","language":"ENGLISH","doi":"10.3133/ofr82522","usgsCitation":"Tibbals, C.H., Wood, W., and Snell, L.J., 1983, Hydrologic quadrangles, Bithlo, Florida: U.S. Geological Survey Open-File Report 82-522, 3 maps :photocopy ;72 x 55 cm., on sheets 84 x 77 cm., https://doi.org/10.3133/ofr82522.","productDescription":"3 maps :photocopy ;72 x 55 cm., on sheets 84 x 77 cm.","costCenters":[],"links":[{"id":168525,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a19e4b07f02db6056c4","contributors":{"authors":[{"text":"Tibbals, C. H.","contributorId":76316,"corporation":false,"usgs":true,"family":"Tibbals","given":"C.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":232304,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wood, W.D.","contributorId":31799,"corporation":false,"usgs":true,"family":"Wood","given":"W.D.","email":"","affiliations":[],"preferred":false,"id":232303,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Snell, Leonard J.","contributorId":89897,"corporation":false,"usgs":true,"family":"Snell","given":"Leonard","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":232305,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":43565,"text":"ofr82630 - 1983 - Hydrology of the Hamilton lakes and vicinity, Polk County, central Florida","interactions":[],"lastModifiedDate":"2022-04-18T16:27:21.394867","indexId":"ofr82630","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"82-630","title":"Hydrology of the Hamilton lakes and vicinity, Polk County, central Florida","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr82630","usgsCitation":"Anderson, W.G., and Simonds, E., 1983, Hydrology of the Hamilton lakes and vicinity, Polk County, central Florida: U.S. Geological Survey Open-File Report 82-630, 1 Plate: 41.63 x 26.84 inches, https://doi.org/10.3133/ofr82630.","productDescription":"1 Plate: 41.63 x 26.84 inches","costCenters":[],"links":[{"id":398943,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0630/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":169337,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0630/report-thumb.jpg"}],"country":"United States","state":"Florida","county":"Polk County","otherGeospatial":"Hamilton Lakes","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -81.67579650878906,\n              28.03380393108653\n            ],\n            [\n              -81.62326812744139,\n              28.03380393108653\n            ],\n            [\n              -81.62326812744139,\n              28.082582442997595\n            ],\n            [\n              -81.67579650878906,\n              28.082582442997595\n            ],\n            [\n              -81.67579650878906,\n              28.03380393108653\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a13e4b07f02db601e6d","contributors":{"authors":[{"text":"Anderson, Warren G.","contributorId":88807,"corporation":false,"usgs":true,"family":"Anderson","given":"Warren","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":228395,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Simonds, Edward P.","contributorId":24838,"corporation":false,"usgs":true,"family":"Simonds","given":"Edward P.","affiliations":[],"preferred":false,"id":228394,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":43566,"text":"ofr82759 - 1983 - Hydrology of Lake Padgett, Saxon Lake, and adjacent area, Pasco County, Florida","interactions":[],"lastModifiedDate":"2013-01-24T07:35:04","indexId":"ofr82759","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"82-759","title":"Hydrology of Lake Padgett, Saxon Lake, and adjacent area, Pasco County, Florida","language":"ENGLISH","doi":"10.3133/ofr82759","usgsCitation":"Henderson, S., 1983, Hydrology of Lake Padgett, Saxon Lake, and adjacent area, Pasco County, Florida: U.S. Geological Survey Open-File Report 82-759, 1 map :col. ;47 x 34 cm., on sheet 76 x 112 cm., folded in envelope 30 x 23 cm., https://doi.org/10.3133/ofr82759.","productDescription":"1 map :col. ;47 x 34 cm., on sheet 76 x 112 cm., folded in envelope 30 x 23 cm.","costCenters":[],"links":[{"id":169338,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":266350,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0759/plate-1.pdf"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a17e4b07f02db6048f3","contributors":{"authors":[{"text":"Henderson, S.E.","contributorId":70806,"corporation":false,"usgs":true,"family":"Henderson","given":"S.E.","email":"","affiliations":[],"preferred":false,"id":228396,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":28741,"text":"wri824071 - 1983 - Selected hydrologic characteristics of the South Platte River in the vicinity of the proposed Narrows Reservoir near Fort Morgan, Colorado","interactions":[],"lastModifiedDate":"2012-02-02T00:08:48","indexId":"wri824071","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"82-4071","title":"Selected hydrologic characteristics of the South Platte River in the vicinity of the proposed Narrows Reservoir near Fort Morgan, Colorado","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri824071","usgsCitation":"Minges, D., 1983, Selected hydrologic characteristics of the South Platte River in the vicinity of the proposed Narrows Reservoir near Fort Morgan, Colorado: U.S. Geological Survey Water-Resources Investigations Report 82-4071, iv, 25 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri824071.","productDescription":"iv, 25 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":159402,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1982/4071/report-thumb.jpg"},{"id":57593,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1982/4071/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a06e4b07f02db5f8c07","contributors":{"authors":[{"text":"Minges, D.R.","contributorId":31387,"corporation":false,"usgs":true,"family":"Minges","given":"D.R.","affiliations":[],"preferred":false,"id":200321,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":44505,"text":"wri834063 - 1983 - Identification and classification of perennial streams of Arkansas","interactions":[],"lastModifiedDate":"2023-12-12T21:53:14.81486","indexId":"wri834063","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-4063","title":"Identification and classification of perennial streams of Arkansas","docAbstract":"Perennial streams are identified in a map and classified according to the relative magnitude of their 7-day, 10-year low flows. Perennial streams are identified for the entire State of Arkansas with the exception of the Mississippi Alluvial Plain. Also presented are the 7-day, 10-year low flow values at continuous-record and low-flow partial-record stations statewide. Perennial streams are defined in this report as having 7-day, 10-year low flows greater than zero. The perennial stream drainage was delineated using data from continuous-record and low-flow partial-record stations, and reconnaissance-site observations. The reconnaissance was conducted during the unusually dry summer of 1980. In analysis, the State was divided into hydrologic regions; they were used in conjunction with index stations to establish the recurrence intervals of flow observed, during the reconnaissance. When necessary, relations were developed by region to adjust observed flow to 10-year recurrence interval flows. (USGS)","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Little Rock, AR","doi":"10.3133/wri834063","collaboration":"Prepared in cooperation with the Arkansas Geological Commission","usgsCitation":"Hunrichs, R., 1983, Identification and classification of perennial streams of Arkansas: U.S. Geological Survey Water-Resources Investigations Report 83-4063, 1 Plate: 53.05 inches x 36.42 inches, https://doi.org/10.3133/wri834063.","productDescription":"1 Plate: 53.05 inches x 36.42 inches","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":423460,"rank":3,"type":{"id":36,"text":"NGMDB Index 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A.","contributorId":89208,"corporation":false,"usgs":true,"family":"Hunrichs","given":"R. A.","affiliations":[],"preferred":false,"id":229898,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":26696,"text":"wri834047 - 1983 - Hydrologic conditions in the Wheatland Flats area, Platte County, Wyoming","interactions":[],"lastModifiedDate":"2017-09-20T16:32:01","indexId":"wri834047","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-4047","title":"Hydrologic conditions in the Wheatland Flats area, Platte County, Wyoming","docAbstract":"The area includes about 260 square miles in central Platte County that consists of Wheatland Flats and a border region. Wheatland Flats is an area of about 100 square miles that is bounded by Chugwater Creek on the east, the Laramie River on the north, and Sybille Creek on the west. The southern boundary is approximately the southernmost limit of alluvial terrace deposits. Surface water diverted from the Laramie River along with ground water from wells is used to irrigate about 57,000 acres most of which are on and adjacent to Wheatland Flats. More than 200 wells are used for irrigation, industrial, and municipal supplies. The wells are completed in an upper aquifer consisting primarily of shallow alluvial deposits of Quaternary age and a lower aquifer, the Arikaree Formation of early Miocene age. Net water-level decline after approximately 20 years (1958-60 to 1979) generally is less than 10 feet in each aquifer , although declines of as much as 13 feet have occurred in the Airkaree Formation at specific locations. A digital model was used to simulate hydrologic conditions in the Wheatland Flats area. The model indicated that ground-water discharge to streams decreased by 10 percent from 1971 to 1978. Stream-discharge measurements are not available to verify the loss. However, it is reasonable to assume, on the basis of hydraulic-head decline in the aquifers, that there has been some ground-water contribution to the stream. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri834047","usgsCitation":"Crist, M.A., 1983, Hydrologic conditions in the Wheatland Flats area, Platte County, Wyoming: U.S. Geological Survey Water-Resources Investigations Report 83-4047, v, 41 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri834047.","productDescription":"v, 41 p. :ill., maps ;28 cm.","costCenters":[{"id":5050,"text":"WY-MT Water Science Center","active":true,"usgs":true}],"links":[{"id":123554,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1983/4047/report-thumb.jpg"},{"id":55562,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1983/4047/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":55563,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1983/4047/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":55564,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1983/4047/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":55565,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1983/4047/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a28e4b07f02db6113ae","contributors":{"authors":[{"text":"Crist, M. A.","contributorId":84799,"corporation":false,"usgs":true,"family":"Crist","given":"M.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":196845,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":25719,"text":"wri824099 - 1983 - Preliminary appraisal of the hydrology of the Stigler area, Haskell County, Oklahoma","interactions":[],"lastModifiedDate":"2012-02-02T00:08:15","indexId":"wri824099","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"82-4099","title":"Preliminary appraisal of the hydrology of the Stigler area, Haskell County, Oklahoma","docAbstract":"Bed rock in the Stigler area of southeastern Oklahoma consists principally of shale, siltstone, and sandstone of the McAlester, Savanna, and Boggy Formations of Pennsylvanian age. These rocks have been folded to form the Stigler syncline on the north and the Antioch anticline on the south. An area of several square miles is underlain by terrace deposits, mostly sandy silt, as much as 25 feet thick. Alluvium along the streams is 5 to 10 feet thick and consists mainly of sandy silt. Neither the terrace deposits nor the alluvium are hydrologically significant.\r\nWater in the bedrock is under artesian conditions. Well depths range from 34 to 235 feet and average 95 feet. The water level in most wells is less than 30 feet below the land surface. Because the rocks have minimal permeability, well yields probably are less than 5 gallons per minute. Much of the area is provided with water by a rural water district. Based on specific-conductance measurements, dissolved-solids concentrations in ground water are estimated to range from 200 to 2,500 milligrams per liter. Nor relationship between variations in specific conductance and well depth, geographic distribution, or geologic formation is apparent.\r\n\r\nStreams in the area are ephemeral and extended periods of no flow can be expected. During much of the period of record, streamflow in Taloka Creek was maintained by water pumped from an active coal mine. Water upstream from the mine area had a mean dissolved-solids concentration of 72 milligrams per liter whereas water downstream from the mine area had a mean concentration of 1,323 milligrams per liter. At times, downstream concentrations of some toxic metals exceeded the standards for drinking water set by the U.S. Environmental Protection Agency. Samples of water collected from Taloka Creek since mining ceased did not have excessive concentrations of toxic metals. Maximum suspended-sediment discharge of Taloka Creek was about 1,660 tons per day. Silt-clay particles (diameters less than 0.062 millimeter) were the dominant grain size.\r\n\r\nObserved and measured effects of surface mining for coal on the hydrologic system include (1) creation of additional water storage in the surface mine pond, (2) disruption of drainage in an area of about 1 square mile, and (3) increased mineralization of water in Taloka Creek. Other possible effects include (4) changes in permeability and storage of water in mine spoil, (5) minor changes in streamflow and runoff characteristics, and (6) temporary increase in the sediment load of Taloka Creek.","language":"ENGLISH","publisher":"U.S. Dept. of the Interior, U.S. Geological Survey,","doi":"10.3133/wri824099","usgsCitation":"Marcher, M., Huntzinger, T., Stoner, J., and Blumer, S.P., 1983, Preliminary appraisal of the hydrology of the Stigler area, Haskell County, Oklahoma: U.S. Geological Survey Water-Resources Investigations Report 82-4099, iv, 41 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri824099.","productDescription":"iv, 41 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":156905,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1982/4099/report-thumb.jpg"},{"id":54484,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1982/4099/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":54485,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1982/4099/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":54486,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1982/4099/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":54487,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1982/4099/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67cb61","contributors":{"authors":[{"text":"Marcher, M.V.","contributorId":9267,"corporation":false,"usgs":true,"family":"Marcher","given":"M.V.","affiliations":[],"preferred":false,"id":194785,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Huntzinger, T.L.","contributorId":67503,"corporation":false,"usgs":true,"family":"Huntzinger","given":"T.L.","email":"","affiliations":[],"preferred":false,"id":194788,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Stoner, J.D.","contributorId":58261,"corporation":false,"usgs":true,"family":"Stoner","given":"J.D.","email":"","affiliations":[],"preferred":false,"id":194787,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Blumer, S. P.","contributorId":23938,"corporation":false,"usgs":true,"family":"Blumer","given":"S.","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":194786,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":48750,"text":"ofr811182 - 1983 - Historical changes to Lake Washington and route of the Lake Washington Ship Canal, King County, Washington","interactions":[],"lastModifiedDate":"2015-10-01T15:01:07","indexId":"ofr811182","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"81-1182","title":"Historical changes to Lake Washington and route of the Lake Washington Ship Canal, King County, Washington","docAbstract":"<p>Lake Washington, in the midst of the greater Seattle metropolitan area of the Puget Sound region (fig. 1), is an exceptional commercial, recreational, and esthetic resource for the region . In the past 130 years, Lake Washington has been changed from a \" wild \" lake in a wilderness setting to a regulated lake surrounded by a growing metropolis--a transformation that provides an unusual opportunity to study changes to a lake's shoreline and hydrologic characteristics -resulting from urbanization.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr811182","usgsCitation":"Chrzastowski, M.J., 1983, Historical changes to Lake Washington and route of the Lake Washington Ship Canal, King County, Washington: U.S. Geological Survey Open-File Report 81-1182, Report: 9 p.; Plate: 33.53 x 57.12 inches, https://doi.org/10.3133/ofr811182.","productDescription":"Report: 9 p.; Plate: 33.53 x 57.12 inches","numberOfPages":"9","onlineOnly":"N","additionalOnlineFiles":"Y","costCenters":[],"links":[{"id":161892,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr811182.jpg"},{"id":309454,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/1182/report.pdf","text":"Report","linkFileType":{"id":1,"text":"pdf"}},{"id":309455,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/1182/plate-1.pdf","text":"Plate 1","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Washington","county":"King County","otherGeospatial":"Lake Washington","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -122.46871948242186,\n              47.30903424774781\n            ],\n            [\n              -122.46871948242186,\n              47.96510025611191\n            ],\n            [\n              -121.40991210937499,\n              47.96510025611191\n            ],\n            [\n              -121.40991210937499,\n              47.30903424774781\n            ],\n            [\n              -122.46871948242186,\n              47.30903424774781\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae1e4b07f02db6885d0","contributors":{"authors":[{"text":"Chrzastowski, Michael J.","contributorId":28643,"corporation":false,"usgs":true,"family":"Chrzastowski","given":"Michael","email":"","middleInitial":"J.","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":238152,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":25718,"text":"wri834013 - 1983 - Preliminary appraisal of the hydrology of the Rock Island area, Le Flore County, Oklahoma","interactions":[],"lastModifiedDate":"2012-02-02T00:08:15","indexId":"wri834013","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-4013","title":"Preliminary appraisal of the hydrology of the Rock Island area, Le Flore County, Oklahoma","docAbstract":"Bed rock in the Rock Island area of northeastern Le Flore County in southeastern Oklahoma consists of shale, siltstone, and sandstone of the McAlester, Hartshorne, and Atoka Formations of Pennsylvanian age. The area is on the south flank of the Backbone anticline; the rocks dip to the south at 5o-45o. Alluvium along James Fork consists of sandy and clayey silt and may be as much as 30 feet thick.\r\nWater in bedrock is under artesian conditions. The depth to water in most wells is less than 20 feet below the surface; a few wells flow. Yields of most wells probably are less than 5 gallons per minute. Water from nine wells was a sodium carbonate or sodium mixed anion type; dissolved-solids concentrations ranged from 294 to 1,250 milligrams per liter. No relationship between variations in chemistry of ground water and well depth, geographic distribution, or geologic formation is apparent.\r\n\r\nJames Fork has flow most of the time and discharge exceeds 25 cubic feet per second about one-half the time. The mean dissolved-solids concentration in James Fork water ranged from 224 milligrams per liter near Williams, Oklahoma, to 332 milligrams per liter near Hackett, Arkansas. Water in James Fork is a calcium magnesium sulfate type about 75 percent of the time. Maximum suspended sediment discharge was 2,720 tons per day. Silt-clay particles (diameters less than 0.062 millimeter) are the dominant sediment size.\r\n\r\nPotential hydrologic effects of surface mining for coal include: (1) Creation of additional water storage in surface-mine ponds, (2) changes in rock permeability and ground-water storage, (3) changes in runoff and streamflow characteristics, (4) changes in drainage patterns, and (5) changes in the chemical quality and sediment load of James Fork. Although mining may increase the quantities of sediment and dissolved minerals added to James Fork, detection of these increases would be difficult because the potentially mineable area is very small in proportion to the total area of the basin.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri834013","usgsCitation":"Marcher, M., 1983, Preliminary appraisal of the hydrology of the Rock Island area, Le Flore County, Oklahoma: U.S. Geological Survey Water-Resources Investigations Report 83-4013, iv, 39 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri834013.","productDescription":"iv, 39 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":156904,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1983/4013/report-thumb.jpg"},{"id":54480,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1983/4013/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":54481,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1983/4013/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":54482,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1983/4013/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":54483,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1983/4013/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67ca7e","contributors":{"authors":[{"text":"Marcher, M.V.","contributorId":9267,"corporation":false,"usgs":true,"family":"Marcher","given":"M.V.","affiliations":[],"preferred":false,"id":194784,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":25717,"text":"wri834166 - 1983 - Preliminary appraisal of the hydrology of the Red Oak area, Latimer County, Oklahoma","interactions":[],"lastModifiedDate":"2012-02-02T00:08:15","indexId":"wri834166","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-4166","title":"Preliminary appraisal of the hydrology of the Red Oak area, Latimer County, Oklahoma","docAbstract":"Bed rock in the Red Oak area consists of shale, siltstone, and sandstone of the McAlester and Savanna Formations of Pennsylvanian age. Water in bedrock occurs in bedding planes, joints, and fractures and is confined. The potentiometric surface generally is less than 20 feet below the land surface. Wells yield enough water for domestic and stock use, but larger amounts of ground water are not available. Ground water commonly is a sodium or mixed cation carbonate/bicarbonate type with dissolved-solids concentrations ranging from 321 to 714 milligrams per liter. Although variable in quality, ground water generally is suitable for domestic use. No relationship between water chemistry and well depth or location is apparent.\r\nBrazil Creek, the principal stream in the area, has no flow 15 percent of the time, and flow is less than 1 cubic foot per second about 25 percent of the time. Water in Brazil Creek is a mixed cation carbonate/bicarbonate type. Dissolved-solids concentrations in Brazil Creek upstream from areas of old and recent mining ranged from 31 to 99 milligrams per liter with a mean of 58 milligrams per liter, whereas concentrations downstream from the mine areas ranged from 49 to 596 milligrams per liter with a mean of 132 milligrams per liter. Water in Brazil and Rock Creeks had concentrations of cadmium, chromium, lead, and mercury that exceeded maximum contaminant levels established by the U.S. Environmental Protection Agency at least once during the 1979-81 water years. Maximum suspended-sediment discharge, in tons per day, was 2,500 for Brazil Creek and 3,318 for Rock Creek. Silt-clay particles (diameters less than 0.062 millimeter) were the dominant sediment size.\r\n\r\nA significant hydrologic effect of surface mining is creation of additional water storage in mine ponds; one such pond supplies water for the town of Red Oak. Other effects or potential effects of surface mining include changes in rock permeability and ground-water storage, changes in drainage patterns, and changes in the chemical quality and sediment loads of streams.","language":"ENGLISH","publisher":"U.S. Geological Survey, Water Resources Division,","doi":"10.3133/wri834166","usgsCitation":"Marcher, M., Bergman, D.L., Stoner, J., and Blumer, S.P., 1983, Preliminary appraisal of the hydrology of the Red Oak area, Latimer County, Oklahoma: U.S. Geological Survey Water-Resources Investigations Report 83-4166, iv, 44 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri834166.","productDescription":"iv, 44 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":156903,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1983/4166/report-thumb.jpg"},{"id":54476,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1983/4166/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":54477,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1983/4166/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":54478,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1983/4166/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":54479,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1983/4166/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67ca70","contributors":{"authors":[{"text":"Marcher, M.V.","contributorId":9267,"corporation":false,"usgs":true,"family":"Marcher","given":"M.V.","affiliations":[],"preferred":false,"id":194780,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bergman, D. L.","contributorId":93038,"corporation":false,"usgs":true,"family":"Bergman","given":"D.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":194783,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Stoner, J.D.","contributorId":58261,"corporation":false,"usgs":true,"family":"Stoner","given":"J.D.","email":"","affiliations":[],"preferred":false,"id":194782,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Blumer, S. P.","contributorId":23938,"corporation":false,"usgs":true,"family":"Blumer","given":"S.","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":194781,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":29330,"text":"wri824081 - 1983 - Limnological study of Shasta Lake, Shasta County, California, with emphasis on the effects of the 1977 drought","interactions":[],"lastModifiedDate":"2012-02-02T00:08:45","indexId":"wri824081","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"82-4081","title":"Limnological study of Shasta Lake, Shasta County, California, with emphasis on the effects of the 1977 drought","docAbstract":"An intensive limnological study of Shasta Lake was made in conjunction with the California Department of Water Resources during the 1977 drought. Water-quality data were collected from March 1977 through September 1978 at six lake stations and four lake tributary stations. Data collected during and after the drought were compared. Lake water quality is described as a function of lake morphometry, climate, hydrology, and reservoir hydraulics. Results indicate Shasta Lake is a warm monomictic lake. Tributary inflow to the lake and outflow through the dam generate density currents which promote mixing at depth and the development of an extensive metalimnion. During the drought, record low lake levels resulted in the exposure of an extensive nearshore sediment zone. Resuspended sediments caused a deterioration of water quality. The most notable effects, in comparison with post-drought conditions, were decreased light penetration, increased dissolved-solids concentration and specific conductance, decreased dissolved-oxygen concentrations, and elevated nutrient levels. A hypolimnetic anoxic condition was observed at the upstream stations of the lake. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri824081","usgsCitation":"Rettig, S., and Bortleson, G.C., 1983, Limnological study of Shasta Lake, Shasta County, California, with emphasis on the effects of the 1977 drought: U.S. Geological Survey Water-Resources Investigations Report 82-4081, vii, 66 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri824081.","productDescription":"vii, 66 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":122755,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1982/4081/report-thumb.jpg"},{"id":58168,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1982/4081/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b16e4b07f02db6a5220","contributors":{"authors":[{"text":"Rettig, S.A.","contributorId":104105,"corporation":false,"usgs":true,"family":"Rettig","given":"S.A.","email":"","affiliations":[],"preferred":false,"id":201357,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bortleson, Gilbert C.","contributorId":57472,"corporation":false,"usgs":true,"family":"Bortleson","given":"Gilbert","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":201356,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":25715,"text":"wri834238 - 1983 - Precipitation-runoff modeling system; user's manual","interactions":[],"lastModifiedDate":"2012-02-02T00:08:15","indexId":"wri834238","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-4238","title":"Precipitation-runoff modeling system; user's manual","docAbstract":"The concepts, structure, theoretical development, and data requirements of the precipitation-runoff modeling system (PRMS) are described. The precipitation-runoff modeling system is a modular-design, deterministic, distributed-parameter modeling system developed to evaluate the impacts of various combinations of precipitation, climate, and land use on streamflow, sediment yields, and general basin hydrology. Basin response to normal and extreme rainfall and snowmelt can be simulated to evaluate changes in water balance relationships, flow regimes, flood peaks and volumes, soil-water relationships, sediment yields, and groundwater recharge. Parameter-optimization and sensitivity analysis capabilites are provided to fit selected model parameters and evaluate their individual and joint effects on model output. The modular design provides a flexible framework for continued model system enhancement and hydrologic modeling research and development. (Author 's abstract)","language":"ENGLISH","publisher":"U.S. Geological Survey, Water Resources Division,","doi":"10.3133/wri834238","usgsCitation":"Leavesley, G., Lichty, R., Troutman, B., and Saindon, L., 1983, Precipitation-runoff modeling system; user's manual: U.S. Geological Survey Water-Resources Investigations Report 83-4238, vii, 207 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri834238.","productDescription":"vii, 207 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":156896,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1983/4238/report-thumb.jpg"},{"id":54474,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1983/4238/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4abae4b07f02db671f67","contributors":{"authors":[{"text":"Leavesley, G.H.","contributorId":93895,"corporation":false,"usgs":true,"family":"Leavesley","given":"G.H.","email":"","affiliations":[],"preferred":false,"id":194774,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lichty, R.W.","contributorId":46987,"corporation":false,"usgs":true,"family":"Lichty","given":"R.W.","affiliations":[],"preferred":false,"id":194772,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Troutman, B.M.","contributorId":73638,"corporation":false,"usgs":true,"family":"Troutman","given":"B.M.","email":"","affiliations":[],"preferred":false,"id":194773,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Saindon, L.G.","contributorId":103281,"corporation":false,"usgs":false,"family":"Saindon","given":"L.G.","email":"","affiliations":[],"preferred":false,"id":194775,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":45939,"text":"ofr82519 - 1983 - Hydrologic quadrangles, Sanford, SW, Florida","interactions":[],"lastModifiedDate":"2012-02-02T00:10:57","indexId":"ofr82519","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"82-519","title":"Hydrologic quadrangles, Sanford, SW, Florida","language":"ENGLISH","doi":"10.3133/ofr82519","usgsCitation":"Tibbals, C.H., Wood, W., and Snell, L.J., 1983, Hydrologic quadrangles, Sanford, SW, Florida: U.S. Geological Survey Open-File Report 82-519, 3 maps :photocopy ;72 x 55 cm., on sheets 84 x 77 cm., https://doi.org/10.3133/ofr82519.","productDescription":"3 maps :photocopy ;72 x 55 cm., on sheets 84 x 77 cm.","costCenters":[],"links":[{"id":167998,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a19e4b07f02db605667","contributors":{"authors":[{"text":"Tibbals, C. H.","contributorId":76316,"corporation":false,"usgs":true,"family":"Tibbals","given":"C.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":232343,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wood, W.D.","contributorId":31799,"corporation":false,"usgs":true,"family":"Wood","given":"W.D.","email":"","affiliations":[],"preferred":false,"id":232342,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Snell, Leonard J.","contributorId":89897,"corporation":false,"usgs":true,"family":"Snell","given":"Leonard","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":232344,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":27857,"text":"wri834044 - 1983 - Evaluation of the San Dieguito, San Elijo, and San Pasqual hydrologic subareas for reclaimed water use, San Diego County, California","interactions":[],"lastModifiedDate":"2023-04-10T18:19:36.73362","indexId":"wri834044","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-4044","title":"Evaluation of the San Dieguito, San Elijo, and San Pasqual hydrologic subareas for reclaimed water use, San Diego County, California","docAbstract":"<p>A study was made to determine the suitability of three small hydrologic subareas in San Diego County, California, for reuse of municipal wastewater. Ground-water quality has been impacted by agricultural water use, imported water use, changes in natural recharge patterns, seawater intrusion, and intrusion of ground water from surrounding marine sediments; therefore, ground water is of limited value as a water-supply source. Reclaimed water use is feasible and expected to improve ground-water quality, creating a new source of water for agricultural use.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri834044","usgsCitation":"Izbicki, J., 1983, Evaluation of the San Dieguito, San Elijo, and San Pasqual hydrologic subareas for reclaimed water use, San Diego County, California: U.S. Geological Survey Water-Resources Investigations Report 83-4044, vii, 131 p., https://doi.org/10.3133/wri834044.","productDescription":"vii, 131 p.","costCenters":[],"links":[{"id":415511,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_35684.htm","linkFileType":{"id":5,"text":"html"}},{"id":56681,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1983/4044/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":120067,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1983/4044/report-thumb.jpg"}],"country":"United States","state":"Calilfornia","county":"San Diego County","otherGeospatial":"San Dieguito, San Elijo, and San Pasqual hydrologic subareas","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -117.069,\n              33.058\n            ],\n            [\n              -117.29,\n              33.058\n            ],\n            [\n              -117.29,\n              32.95\n            ],\n            [\n              -117.069,\n              32.95\n            ],\n            [\n              -117.069,\n              33.058\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a96e4b07f02db65ac22","contributors":{"authors":[{"text":"Izbicki, J. A. 0000-0003-0816-4408","orcid":"https://orcid.org/0000-0003-0816-4408","contributorId":28244,"corporation":false,"usgs":true,"family":"Izbicki","given":"J. A.","affiliations":[],"preferred":false,"id":198793,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":27663,"text":"wri834121E - 1983 - Map showing outcrops of ash-flow tuffs, Basin and Range Province and vicinity, Trans-Pecos Texas","interactions":[],"lastModifiedDate":"2017-11-21T14:37:32","indexId":"wri834121E","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-4121","chapter":"E","title":"Map showing outcrops of ash-flow tuffs, Basin and Range Province and vicinity, Trans-Pecos Texas","docAbstract":"<p>This map report is one of a series of geologic and hydrologic maps covering all or parts of the States within the Basin and Range province of the western United States, resulting from work under the U.S. Geological Survey's program for geologic and hydrologic evaluation of the Basin and Range province to identify potentially suitable regions for future study relative to isolation of high-level nuclear waste (Bedinger, Sargent, and Reed, 1984) . </p><p>The map report on the ash-flow tuffs of Trans-Pecos Texas was prepared from published maps and reports and from recent work in progress by geologists of the Texas Bureau of Economic Geology, and was compiled utilizing the project guidelines of Sargent and Bedinger (1984). The map shows the outcrops and localities of measured thicknesses of the ash-flow tuffs that resulted from silicic volcanism 38 to 28 million years ago (Henry and McDowell, 1982). Locally, however, some thin, inadequately studied tuffs of limited distribution have been excluded from the map. Such tuffs are reported in the \"lower rhyolite\" in the Eagle Mountains (Underwood, 1963), in the southern Davis Mountains (Parker, 1977), within parts of the Shely Group and Morita Ranch Formation in the Chinati Mountains (Cepeda and Henry, 1983) , and in the Rawls Formation in the Bofecillos Mountains (McKnight, 1969). The distribution of most ash-flow tuffs in the northern Davis and Wylie Mountains is not well known. The Chambers Tuff, largely tuffaceous sedimentary rocks, is reported to contain several ash-flow tuffs (Walton, 1972), but their distribution is poorly documented. Metamorphosed ash-flow tuffs of Precambrian age in the Thunderbird Group in the Franklin Mountains (Thomann, 1981) and in the Carrizo Mountain Group near Van Horn (Rudnick , 1983) were not included on the map. In some areas studied in reconnaissance, the definitive lithology of some volcanic units described as lava flows or tuffs has not been determined. </p><p>In the Description of Map Units, the general location, caldera source and volume of tuff, isotopic age, if available, lithologic data, and the reference sources for each geologic unit are described. The nomenclature of the geologic units is from published reports and does not necessarily conform to U.S. Geological Survey usage.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri834121E","collaboration":"Prepared in cooperation with the Texas Bureau of Economic Geology","usgsCitation":"1983, Map showing outcrops of ash-flow tuffs, Basin and Range Province and vicinity, Trans-Pecos Texas: U.S. Geological Survey Water-Resources Investigations Report 83-4121, Report: 8 p.; 3 Plates: 52.69 x 26.24 inches or smaller, https://doi.org/10.3133/wri834121E.","productDescription":"Report: 8 p.; 3 Plates: 52.69 x 26.24 inches or smaller","costCenters":[],"links":[{"id":349225,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1983/4121e/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":349226,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1983/4121e/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":349227,"rank":5,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1983/4121e/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":56516,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1983/4121e/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":120145,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1983/4121e/report-thumb.jpg"}],"scale":"25000","datum":"National Geodetic Datum of 1929","country":"United States","state":"Texas","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -106.5,\n              29\n            ],\n            [\n              -102,\n              29\n            ],\n            [\n              -102,\n              32\n            ],\n            [\n              -106.5,\n              32\n            ],\n            [\n              -106.5,\n              29\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b15e4b07f02db6a4890","contributors":{"compilers":[{"text":"Henry, Christopher D.","contributorId":36556,"corporation":false,"usgs":true,"family":"Henry","given":"Christopher D.","affiliations":[],"preferred":false,"id":723108,"contributorType":{"id":3,"text":"Compilers"},"rank":1},{"text":"Fisher, Gail L.","contributorId":200706,"corporation":false,"usgs":false,"family":"Fisher","given":"Gail","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":723109,"contributorType":{"id":3,"text":"Compilers"},"rank":2}]}}
,{"id":25711,"text":"wri834109 - 1983 - Potential hydrologic impacts of a tar-sand industry in 11 special tar sand areas in eastern Utah","interactions":[],"lastModifiedDate":"2012-02-02T00:08:15","indexId":"wri834109","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-4109","title":"Potential hydrologic impacts of a tar-sand industry in 11 special tar sand areas in eastern Utah","docAbstract":"About 93 percent of the Nation 's estimated 30 billion barrels of crude oil in tar sand deposits is in 11 tar-sand deposits in eastern Utah that were chosen for leasing by the Federal government. The Tar Sand Triangle area, which contains about 15 billion barrels of oil, is the largest. This area and the Sunnyside and P R Springs areas contain more than three-fourths of the Utah reserves. About 88,000 acre-feet of water per year would be required for a commercial tar-sand industry producing about 365,000 barrels per day. At this rate, most of the recoverable oil would be mined within 30 years. About 22,000 acre-feet of water per year would be required for a commercial tar-sand industry producing about 83,000 barrels per day. Impacts on local hydrology would be greatest in the Tar Sand Triangle, Sunnyside, and P R Springs areas. Impacts could be minimized with proper construction of surface facilities to decrease erosion, sediment transport, and impoundment of mining and retort water. Increases in salinity of the Colorado River at Imperial Dam, Ariz.-Calif., could be about 3 milligrams per liter, with a peak of 9 milligrams per liter, for a 365 ,000-barrel-per-day industry and less than 1 milligram per liter , with a peak of 2 milligrams per liter, for an 83 ,000-barrel-per-day industry. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri834109","usgsCitation":"Lindskov, K., 1983, Potential hydrologic impacts of a tar-sand industry in 11 special tar sand areas in eastern Utah: U.S. Geological Survey Water-Resources Investigations Report 83-4109, x, 130 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri834109.","productDescription":"x, 130 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":123362,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1983/4109/report-thumb.jpg"},{"id":54471,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1983/4109/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac8e4b07f02db67c09e","contributors":{"authors":[{"text":"Lindskov, K.L.","contributorId":91077,"corporation":false,"usgs":true,"family":"Lindskov","given":"K.L.","affiliations":[],"preferred":false,"id":194758,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":25745,"text":"wri834218 - 1983 - Regional hydrology of the Blanding-Durango area, southern Paradox basin, Utah and Colorado","interactions":[],"lastModifiedDate":"2022-12-15T21:48:06.003876","indexId":"wri834218","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-4218","title":"Regional hydrology of the Blanding-Durango area, southern Paradox basin, Utah and Colorado","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri834218","usgsCitation":"Whitfield, M., Thordarson, W., Oatfield, W.J., Zimmerman, E.A., and Rueger, B.F., 1983, Regional hydrology of the Blanding-Durango area, southern Paradox basin, Utah and Colorado: U.S. Geological Survey Water-Resources Investigations Report 83-4218, Report: vi, 88 p.; 3 Plates: 36.22 × 23.17 inches or smaller, https://doi.org/10.3133/wri834218.","productDescription":"Report: vi, 88 p.; 3 Plates: 36.22 × 23.17 inches or smaller","costCenters":[],"links":[{"id":410584,"rank":6,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_35859.htm","linkFileType":{"id":5,"text":"html"}},{"id":54507,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1983/4218/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":54506,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1983/4218/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":156738,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1983/4218/report-thumb.jpg"},{"id":54509,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1983/4218/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":54508,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1983/4218/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Colorado, Utah","otherGeospatial":"Blanding-Durango area, southern Paradox basin","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -110,\n              37.967\n            ],\n            [\n              -110,\n              37\n            ],\n            [\n              -107.873,\n              37\n            ],\n            [\n              -107.873,\n              37.967\n            ],\n            [\n              -110,\n              37.967\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a60e4b07f02db634eb4","contributors":{"authors":[{"text":"Whitfield, M.S.","contributorId":69547,"corporation":false,"usgs":true,"family":"Whitfield","given":"M.S.","email":"","affiliations":[],"preferred":false,"id":194897,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Thordarson, William","contributorId":23539,"corporation":false,"usgs":true,"family":"Thordarson","given":"William","email":"","affiliations":[],"preferred":false,"id":194894,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Oatfield, W. J.","contributorId":34531,"corporation":false,"usgs":true,"family":"Oatfield","given":"W.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":194896,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Zimmerman, E. A.","contributorId":75533,"corporation":false,"usgs":true,"family":"Zimmerman","given":"E.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":194898,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Rueger, B. F.","contributorId":27470,"corporation":false,"usgs":true,"family":"Rueger","given":"B.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":194895,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":45938,"text":"ofr82520 - 1983 - Hydrologic quadrangle, Sanford, Florida","interactions":[],"lastModifiedDate":"2012-02-02T00:10:56","indexId":"ofr82520","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"82-520","title":"Hydrologic quadrangle, Sanford, Florida","language":"ENGLISH","doi":"10.3133/ofr82520","usgsCitation":"Tibbals, C.H., Wood, W., and Snell, L.J., 1983, Hydrologic quadrangle, Sanford, Florida: U.S. Geological Survey Open-File Report 82-520, 3 maps :photocopy ;72 x 55 cm., on sheets 84 x 77 cm., https://doi.org/10.3133/ofr82520.","productDescription":"3 maps :photocopy ;72 x 55 cm., on sheets 84 x 77 cm.","costCenters":[],"links":[{"id":168794,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a19e4b07f02db6056a6","contributors":{"authors":[{"text":"Tibbals, C. H.","contributorId":76316,"corporation":false,"usgs":true,"family":"Tibbals","given":"C.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":232340,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wood, W.D.","contributorId":31799,"corporation":false,"usgs":true,"family":"Wood","given":"W.D.","email":"","affiliations":[],"preferred":false,"id":232339,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Snell, Leonard J.","contributorId":89897,"corporation":false,"usgs":true,"family":"Snell","given":"Leonard","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":232341,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
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