{"pageNumber":"2251","pageRowStart":"56250","pageSize":"25","recordCount":68873,"records":[{"id":5916,"text":"pp1110MDD - 1979 - The Mississippian and Pennsylvanian (Carboniferous) systems in the United States","interactions":[],"lastModifiedDate":"2024-11-18T19:20:36.551193","indexId":"pp1110MDD","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1979","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"1110","chapter":"M-DD","title":"The Mississippian and Pennsylvanian (Carboniferous) systems in the United States","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/pp1110MDD","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1979, The Mississippian and Pennsylvanian (Carboniferous) systems in the United States: U.S. Geological Survey Professional Paper 1110, 487 p., https://doi.org/10.3133/pp1110MDD.","productDescription":"487 p.","costCenters":[],"links":[{"id":247324,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/1110m-dd/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":402239,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_93477.htm","text":"Wyoming","linkFileType":{"id":5,"text":"html"}},{"id":251797,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/1110m-dd/report-thumb.jpg"},{"id":464250,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_93478.htm","text":"Idaho","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac8e4b07f02db67b8d3","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":528705,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":55497,"text":"wdrLA793 - 1979 - Water resources data for Louisiana, water year 1979, volume 3. Coastal Louisiana","interactions":[],"lastModifiedDate":"2025-05-22T19:17:35.362662","indexId":"wdrLA793","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1979","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"LA-79-3","title":"Water resources data for Louisiana, water year 1979, volume 3. Coastal Louisiana","docAbstract":"<p>Water resources data for the 1979 water year for Louisiana consist of records of stage, discharge, and water quality of streams; stage, contents, and water quality of lakes and reservoirs; and water levels and water quality of ground water. This report, in three volumes, contains records for water discharge at 78 gaging stations (including stage for 72 of these stations); stage only for 42 gaging stations and 10 lakes; contents for 1 reservoir; water quality for 146 surface-water stations (including 22 gaging stations, 52 miscellaneous sites, and 24 lakes), and 335 wells; and water levels for 685 observation wells. Also included are data for 212 crest-stage and flood profile partial-record stations. Additional water data were collected at various sites not involved in the systematic data-collection program, and are published as miscellaneous measurements. Records for a few pertinent stations in bordering States are also included in this report. These data represent that part of the National Water Data System operated by the U.S. Geological Survey and cooperating State and Federal agencies in Louisiana.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wdrLA793","collaboration":"Prepared in cooperation with the Louisiana Department of Transportation and Development and with other State and Federal agencies","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1979, Water resources data for Louisiana, water year 1979, volume 3. 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,{"id":11310,"text":"ofr791274 - 1979 - Low-flow characteristics of streams in the Pecatonica-Sugar River basin, Wisconsin","interactions":[],"lastModifiedDate":"2015-10-20T15:45:47","indexId":"ofr791274","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1979","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":"79-1274","chapter":"Pecatonica River, Sugar River","title":"Low-flow characteristics of streams in the Pecatonica-Sugar River basin, Wisconsin","docAbstract":"<p>The purpose of this report is to describe low-flow characteristics of streams in the Pecatonica-Sugar River basin, Wisconsin, where streamflow data have been collected, and to present equations for estimating low-flow characteristics at ungaged sites.</p>\n<p>Low-flow characteristics were estimated for 11 gaging stations, 25 low-flow partial-record stations, and 207 miscellaneous sites in the basin. Estimates of flow duration were made at the 11 gaging stations. Also, low-flow discharge measurements are listed for 16 miscellaneous sites where insufficient data were available to estimate low-flow characteristics.</p>\n<p>Four equations are provided to estimate low-flow characteristics at ungaged sites and at sites where one base-flow discharge measurement is available. The equations were determined from multiple-regression analyses that related low-flow characteristics at gaging stations and partial-record stations to basin characteristics. Drainage area and base-flow index were the most significant parameters for these analyses.</p>\n<p>The standard error of estimate of the 7-day, 10-year low flow was provided. The average SE-j f iQ in the basin ranged from 10 to 64 percent and was dependent on the amount of low-flow data available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr791274","collaboration":"Prepared in cooperation with the Wisconsin Department of Natural Resources","usgsCitation":"Stedfast, D., 1979, Low-flow characteristics of streams in the Pecatonica-Sugar River basin, Wisconsin: U.S. Geological Survey Open-File Report 79-1274, Report: iv, 92 p.; 2 Plates: 17.00 x 9.00 inches, https://doi.org/10.3133/ofr791274.","productDescription":"Report: iv, 92 p.; 2 Plates: 17.00 x 9.00 inches","numberOfPages":"98","onlineOnly":"N","additionalOnlineFiles":"Y","costCenters":[{"id":677,"text":"Wisconsin Water Science 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D.A.","contributorId":89520,"corporation":false,"usgs":true,"family":"Stedfast","given":"D.A.","affiliations":[],"preferred":false,"id":162909,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":10354,"text":"ofr791535 - 1979 - Water-quality data from five Oregon stream basins","interactions":[],"lastModifiedDate":"2016-09-26T12:47:34","indexId":"ofr791535","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1979","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":"79-1535","title":"Water-quality data from five Oregon stream basins","docAbstract":"<p>The U.S. Geological Survey collected water-quality data in five Oregon stream basins during summer low-flow conditions in 1977 and 1978. During the two sampling periods, a total of 18 different sites were sampled. Several sites were sampled twice in 1977, and some sites were sampled in both 1977 and 1978. Included in the sampling were diel trace of dissolved oxygen, temperature, specific conductance, pH, and solar radiation. In addition, periphyton and benthic invertebrate samples were collected and identified.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Portland, OR","doi":"10.3133/ofr791535","usgsCitation":"Miller, T.L., 1979, Water-quality data from five Oregon stream basins: U.S. Geological Survey Open-File Report 79-1535, iv, 98 p., https://doi.org/10.3133/ofr791535.","productDescription":"iv, 98 p.","numberOfPages":"104","costCenters":[{"id":518,"text":"Oregon Water Science Center","active":true,"usgs":true}],"links":[{"id":143356,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr791535.jpg"},{"id":328967,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1979/1535/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United 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,{"id":2396,"text":"wsp2060 - 1979 - Simulation analysis of the unconfined aquifer, Raft River geothermal area, Idaho-Utah","interactions":[],"lastModifiedDate":"2022-12-15T22:36:44.732243","indexId":"wsp2060","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1979","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2060","title":"Simulation analysis of the unconfined aquifer, Raft River geothermal area, Idaho-Utah","docAbstract":"<p>This study covers about 1,000 mi<sup>2</sup> (2,600 km<sup>2</sup> ) of the southern Raft River drainage basin in south-central Idaho and northwest Utah. The main area of interest, approximately 200 mi2 (520 km<sup>2</sup> ) of semiarid agricultural and rangeland in the southern Raft River Valley that includes the known Geothermal Resource Area near Bridge, Idaho, was modelled numerically to evaluate the hydrodynamics of the unconfined aquifer. Computed and estimated transmissivity values range from 1,200 feet squared per day (110 meters squared per day) to 73,500 feet squared per day (6,830 meters squared per day). Water budgets, including ground-water recharge and discharge for approximate equilibrium conditions, have been computed by several previous investigators; their estimates of available ground-water recharge range from about 46,000 acre-feet per year (57 cubic hectometers per year) to 100,000 acre-feet per year (123 cubic hectometers per year).</p><p>Simulation modeling of equilibrium conditions represented by 1952 water levels suggests: (1) recharge to the water-table aquifer is about 63,000 acre-feet per year (77 cubic hectometers per year); (2) a significant volume of ground water is discharged through evapotranspiration by phreatophytes growing on the valley bottomlands; (3) the major source of recharge may be from upward leakage of water from a deeper, confined reservoir; and (4) the aquifer transmissivity probably does not exceed about 12,000 feet squared per day (3,100 meters squared per day). Additional analysis carried out by simulating transient conditions from 1952 to 1965 strongly suggests that aquifer transmissivity does not exceed about 7,700 feet squared per day (700 meters squared per day). The model was calibrated using slightly modified published pumpage data; it satisfactorily reproduced the historic water-level decline over the period 1952-65.</p>","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/wsp2060","usgsCitation":"Nichols, W., 1979, Simulation analysis of the unconfined aquifer, Raft River geothermal area, Idaho-Utah: U.S. Geological Survey Water Supply Paper 2060, iv, 46 p., https://doi.org/10.3133/wsp2060.","productDescription":"iv, 46 p.","numberOfPages":"51","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":139196,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/2060/report-thumb.jpg"},{"id":28374,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/2060/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":410592,"rank":2,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_25431.htm","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Idaho, Utah","otherGeospatial":"Raft River geothermal area","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -113.5,\n              42.325\n            ],\n            [\n              -113.5,\n              41.9\n            ],\n            [\n              -113.208,\n              41.9\n            ],\n            [\n              -113.208,\n              42.325\n            ],\n            [\n              -113.5,\n              42.325\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adbe4b07f02db685aac","contributors":{"authors":[{"text":"Nichols, William D.","contributorId":98296,"corporation":false,"usgs":true,"family":"Nichols","given":"William D.","affiliations":[],"preferred":false,"id":145132,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":40752,"text":"ofr791122 - 1979 - Coal resource occurrence map of the Mesa de los Toros quadrangle, McKinley County, New Mexico","interactions":[],"lastModifiedDate":"2022-11-30T20:07:26.161668","indexId":"ofr791122","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1979","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":"79-1122","title":"Coal resource occurrence map of the Mesa de los Toros quadrangle, McKinley County, New Mexico","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr791122","usgsCitation":"Water Resources Division, U.S. Geological Survey, and Berge Exploration Inc., 1979, Coal resource occurrence map of the Mesa de los Toros quadrangle, McKinley County, New Mexico: U.S. Geological Survey Open-File Report 79-1122, Report: ii, 24 p.; 12 Plates: 29.32 × 22.88 inches or smaller, https://doi.org/10.3133/ofr791122.","productDescription":"Report: ii, 24 p.; 12 Plates: 29.32 × 22.88 inches or smaller","costCenters":[],"links":[{"id":78029,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1979/1122/plate-05.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":78027,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1979/1122/plate-03.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":78026,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1979/1122/plate-02.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":78036,"rank":411,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1979/1122/plate-12.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":78033,"rank":408,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1979/1122/plate-09.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":78031,"rank":406,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1979/1122/plate-07.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":409887,"rank":15,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_39574.htm","linkFileType":{"id":5,"text":"html"}},{"id":78035,"rank":410,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1979/1122/plate-11.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":78034,"rank":409,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1979/1122/plate-10.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":78032,"rank":407,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1979/1122/plate-08.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":78028,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1979/1122/plate-04.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":78025,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1979/1122/plate-01.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":175772,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1979/1122/report-thumb.jpg"},{"id":78030,"rank":405,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1979/1122/plate-06.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":78037,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1979/1122/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"New Mexico","county":"McKinley County","otherGeospatial":"Mesa de los Toros quadrangle","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -107.75,\n              35.625\n            ],\n            [\n              -107.75,\n              35.5\n            ],\n            [\n              -107.875,\n              35.5\n            ],\n            [\n              -107.875,\n              35.625\n            ],\n            [\n              -107.75,\n              35.625\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b25e4b07f02db6af46b","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":530397,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Berge Exploration Inc.","contributorId":128031,"corporation":true,"usgs":false,"organization":"Berge Exploration Inc.","id":530396,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":24055,"text":"ofr791485 - 1979 - Sample descriptions for test wells penetrating deep aquifers in Dallas and Sumpter counties, Alabama","interactions":[],"lastModifiedDate":"2024-07-30T18:15:11.708098","indexId":"ofr791485","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1979","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":"79-1485","title":"Sample descriptions for test wells penetrating deep aquifers in Dallas and Sumpter counties, Alabama","docAbstract":"<p>Test wells in Dallas and Sumter counties, Alabama penetrated deep Cretaceous aquifers that are sources of future ground-water withdrawals. The test well in Dallas County was drilled to a depth of 1,460 feet, and the test well in Sumter County was drilled to a depth of 2,311 feet. The deep aquifers in Sumter County are in an area of future residential and industrial development along the Tennessee-Tombigbee Waterway. Descriptions of drill cuttings are given in the report.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr791485","collaboration":"Prepared in cooperation with Geological Survey of Alabama","usgsCitation":"Newton, J.G., 1979, Sample descriptions for test wells penetrating deep aquifers in Dallas and Sumpter counties, Alabama: U.S. Geological Survey Open-File Report 79-1485, iii, 24 p., https://doi.org/10.3133/ofr791485.","productDescription":"iii, 24 p.","costCenters":[],"links":[{"id":431628,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1979/1485/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":156220,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1979/1485/report-thumb.jpg"}],"country":"United States","state":"Alabama","county":"Dallas County, Sumpter County","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -88.38159110622885,\n              32.64390677077685\n            ],\n            [\n              -88.38159110622885,\n              31.405673585368433\n            ],\n            [\n              -86.65749089365087,\n              31.405673585368433\n            ],\n            [\n              -86.65749089365087,\n              32.64390677077685\n            ],\n            [\n              -88.38159110622885,\n              32.64390677077685\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ee4b07f02db5fde4c","contributors":{"authors":[{"text":"Newton, John G.","contributorId":22323,"corporation":false,"usgs":true,"family":"Newton","given":"John","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":191228,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":42616,"text":"ofr791348 - 1979 - Preliminary lithologic and water quality data from test wells on Koehn Dry Lake, Kern County, California","interactions":[],"lastModifiedDate":"2012-02-02T00:10:29","indexId":"ofr791348","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1979","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":"79-1348","title":"Preliminary lithologic and water quality data from test wells on Koehn Dry Lake, Kern County, California","language":"ENGLISH","doi":"10.3133/ofr791348","usgsCitation":"Dockter, R.D., 1979, Preliminary lithologic and water quality data from test wells on Koehn Dry Lake, Kern County, California: U.S. Geological Survey Open-File Report 79-1348, 5 well logs ;97 x 99 cm. or smaller., https://doi.org/10.3133/ofr791348.","productDescription":"5 well logs ;97 x 99 cm. or smaller.","costCenters":[],"links":[{"id":172817,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":80387,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1979/1348/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":80388,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1979/1348/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":80389,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1979/1348/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":80390,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1979/1348/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":80391,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1979/1348/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afee4b07f02db69771f","contributors":{"authors":[{"text":"Dockter, Roger D.","contributorId":81875,"corporation":false,"usgs":true,"family":"Dockter","given":"Roger","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":226829,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":41513,"text":"ofr791474 - 1979 - Aeromagnetic map of southern Nevada","interactions":[],"lastModifiedDate":"2021-10-26T19:28:24.732973","indexId":"ofr791474","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1979","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":"79-1474","title":"Aeromagnetic map of southern Nevada","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr791474","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1979, Aeromagnetic map of southern Nevada: U.S. Geological Survey Open-File Report 79-1474, 1 Plate: 32.25 × 35.19 inches, https://doi.org/10.3133/ofr791474.","productDescription":"1 Plate: 32.25 × 35.19 inches","costCenters":[],"links":[{"id":170993,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":390979,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_11161.htm"},{"id":79237,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1979/1474/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Nevada","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -116.69677734375,\n              34.867904962568716\n            ],\n            [\n              -113.88427734374999,\n              34.867904962568716\n            ],\n            [\n              -113.88427734374999,\n              37.03763967977139\n            ],\n            [\n              -116.69677734375,\n              37.03763967977139\n            ],\n            [\n              -116.69677734375,\n              34.867904962568716\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afee4b07f02db6973a0","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":530441,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":24151,"text":"ofr79556 - 1979 - Water-quality reconnaissance of lakes in Voyageurs National Park, Minnesota","interactions":[],"lastModifiedDate":"2016-05-17T14:37:33","indexId":"ofr79556","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1979","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":"79-556","title":"Water-quality reconnaissance of lakes in Voyageurs National Park, Minnesota","docAbstract":"<p>Water samples were collected from three lakes in Voyageurs National Park to assess chemical and biological water quality in March and August 1977. Bottom material samples were also collected and analyzed for chemical quality. Results of the analyses show that the water system was dilute; specific conductance ranged from 32 to 111 micromhos. Blue-green algae, particularly <i>Oscillatoria</i>, were the most common phytoplankton in the samples. Differences in water quality, shown particularly by concentrations of nutrients and dissolved solids, were detected between samples collected in different areas of the park. The collected data were used to design a monitoring program to assess eutrophication that may occur during the development of the park.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"St. Paul, MN","doi":"10.3133/ofr79556","issn":"0094-9140","collaboration":"Prepared in cooperation with National Park Service, Department of the Interior","usgsCitation":"Payne, G.A., 1979, Water-quality reconnaissance of lakes in Voyageurs National Park, Minnesota: U.S. Geological Survey Open-File Report 79-556, 40 p., https://doi.org/10.3133/ofr79556.","productDescription":"40 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":392,"text":"Minnesota Water Science 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A.","contributorId":62190,"corporation":false,"usgs":true,"family":"Payne","given":"G.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":191407,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":40933,"text":"ofr79986 - 1979 - Potentiometric surface map of the Floridan Aquifer in the St. Johns River water management district and vicinity, Florida, September 1978","interactions":[],"lastModifiedDate":"2022-03-15T16:29:58.32134","indexId":"ofr79986","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1979","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":"79-986","title":"Potentiometric surface map of the Floridan Aquifer in the St. Johns River water management district and vicinity, Florida, September 1978","docAbstract":"<p>No abstract available.&nbsp;</p>","language":"ENGLISH","doi":"10.3133/ofr79986","collaboration":"Prepared in cooperation with the St. Johns River Water Management District, Brevard, Lake, Orange, Seminole, Sumter and Volusia Counties Bureau of Water Resources Management, Florida Department of Environmental Regulation, South Florida Water Management District, Southwest Florida Water Management District, City of Gainesville and Cocoa, Lake County Water Authority-Pollution Control and Planning Departments, Reedy Creek Improvement District","usgsCitation":"Watkins, F.A., Laughlin, C.P., and Hayes, E.C., 1979, Potentiometric surface map of the Floridan Aquifer in the St. Johns River water management district and vicinity, Florida, September 1978: U.S. Geological Survey Open-File Report 79-986, 1 Plate: 30.53 x 45.53 inches, https://doi.org/10.3133/ofr79986.","productDescription":"1 Plate: 30.53 x 45.53 inches","costCenters":[],"links":[{"id":171440,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1979/0986/report-thumb.jpg"},{"id":397120,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1979/0986/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"500000","country":"United States","state":"Florida","otherGeospatial":"St. Johns River","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -82.1502685546875,\n              29.156958511360703\n            ],\n            [\n              -81.2109375,\n              29.156958511360703\n            ],\n            [\n              -81.2109375,\n              30.500750980290693\n            ],\n            [\n              -82.1502685546875,\n              30.500750980290693\n            ],\n            [\n              -82.1502685546875,\n              29.156958511360703\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad4e4b07f02db68312f","contributors":{"authors":[{"text":"Watkins, F. A.","contributorId":17649,"corporation":false,"usgs":true,"family":"Watkins","given":"F.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":224203,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Laughlin, C. P.","contributorId":107741,"corporation":false,"usgs":true,"family":"Laughlin","given":"C.","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":224204,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hayes, E. C.","contributorId":120899,"corporation":false,"usgs":true,"family":"Hayes","given":"E.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":224202,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":11426,"text":"ofr79704 - 1979 - Chemical analyses of waters from geysers, hot springs, and pools in Yellowstone National Park, Wyoming, from 1974 to 1978","interactions":[],"lastModifiedDate":"2025-12-11T17:54:12.128604","indexId":"ofr79704","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1979","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":"79-704","title":"Chemical analyses of waters from geysers, hot springs, and pools in Yellowstone National Park, Wyoming, from 1974 to 1978","docAbstract":"<p>Waters from geysers, hot springs, and pools of Yellowstone National Park have been analyzed by numerous investigators extending back nearly ten decades. Large compilations of complete major ion analyses of the thermal waters have been reported by Gooch and Whitfield (1888) 38 analyses; Allen and Day (1935) 94 complete and 127 partial major ion analyses, Rowe and others (1973) 166 analyses including many previous chemical analyses of the same feature; and Thompson and others (1975) 242 complete and 299 partial major ion analyses. Smaller compilations of the thermal water chemistry have been reported by Douglass (1939) 12 analyses; White and others (1963) 6 analyses; and Scott (1964) 10 analyses. Partial chemical analyses have been reported by White and others (1956) and by Morey and others (1961) for dissolved silica; Noguichi and Nix (1963) for dissolved silica and major anions; Araki and Noguichi (1969) for dissolved silica, molybdenum, vanadium, and major anions. Here we report 422 complete major ion analyses from 330 different locations of geysers, hot springs, and pools, collected from 1974 to 1978. Many of the analyses from Upper, Midway, Lower, and Norris Geyser Basin are recollections of features previously reported.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr79704","usgsCitation":"Thompson, J., and Yadav, S., 1979, Chemical analyses of waters from geysers, hot springs, and pools in Yellowstone National Park, Wyoming, from 1974 to 1978: U.S. Geological Survey Open-File Report 79-704, 53 p., https://doi.org/10.3133/ofr79704.","productDescription":"53 p.","costCenters":[],"links":[{"id":144292,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1979/0704/report-thumb.jpg"},{"id":497342,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1979/0704/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Wyoming","otherGeospatial":"Yellowstone National Park","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": 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M.","contributorId":77142,"corporation":false,"usgs":true,"family":"Thompson","given":"J. M.","affiliations":[],"preferred":false,"id":163120,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Yadav, Sandhya","contributorId":8847,"corporation":false,"usgs":true,"family":"Yadav","given":"Sandhya","email":"","affiliations":[],"preferred":false,"id":163119,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":2129,"text":"wsp2057 - 1979 - Hydrology and surface morphology of the Bonneville Salt Flats and Pilot Valley Playa, Utah","interactions":[{"subject":{"id":10049,"text":"ofr7818 - 1977 - Hydrology and surface morphology of the Bonneville Salt Flats and Pilot Valley playa, Utah","indexId":"ofr7818","publicationYear":"1977","noYear":false,"title":"Hydrology and surface morphology of the Bonneville Salt Flats and Pilot Valley playa, Utah"},"predicate":"SUPERSEDED_BY","object":{"id":2129,"text":"wsp2057 - 1979 - Hydrology and surface morphology of the Bonneville Salt Flats and Pilot Valley Playa, Utah","indexId":"wsp2057","publicationYear":"1979","noYear":false,"title":"Hydrology and surface morphology of the Bonneville Salt Flats and Pilot Valley Playa, Utah"},"id":1}],"lastModifiedDate":"2017-09-03T10:07:56","indexId":"wsp2057","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1979","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2057","title":"Hydrology and surface morphology of the Bonneville Salt Flats and Pilot Valley Playa, Utah","docAbstract":"<p>The Bonneville Salt Flats and Pilot Valley are in the western part of the Great Salt Lake Desert in northwest Utah. The areas are separate, though similar, hydrologic basins, and both contain a salt crust. The Bonneville salt crust covered about 40 square miles in the fall of 1976, and the salt crust in Pilot Valley covered 7 square miles. Both areas lack any noticeable surface relief (in 1976, 1.3 feet on the Bonneville salt crust and 0.3 foot on the Pilot Valley salt crust).</p><p>The salt crust on the Salt Flats has been used for many years for automobile racing, and brines from shallow lacustrine deposits have been used for the production of potash. In recent years, there has been an apparent conflict between these two major uses of the area as the salt crust has diminished in both thickness and extent. Much of the Bonneville Racetrack has become rougher, and there has also been an increase in the amount of sediment on the south end of the racetrack. The Pilot Valley salt crust and surrounding playa have been largely unused.</p><p>Evaporite minerals on the Salt Flats and the Pilot Valley playa are concentrated in three zones: (1) a carbonate zone composed mainly of authigenic clay-size carbonate minerals, (2) a sulfate zone composed mainly of authigenic gypsum, and (3) a chloride zone composed of crystalline halite (the salt crust). Five major types of salt crust were recognized on the Salt Flats, but only one type was observed in Pilot Valley. Geomorphic differences in the salt crust are caused by differences in their hydrologic environments. The salt crusts are dynamic features that are subject to change because of climatic factors and man's activities.</p><p>Ground water occurs in three distinct aquifers in much of the western Great Salt Lake Desert: (1) the basin-fill aquifer, which yields water from conglomerate in the lower part of the basin fill, (2) the alluvial-fan aquifer, which yields water from sand and gravel along the western margins of both playas, and (3) the shallow-brine aquifer, which yields water from near-surface carbonate muds and crystalline halite and gypsum. The shallow-brine aquifer is the main source of brine used for the production of potash on the Salt Flats.</p><p>Recharge to that part of the shallow-brine aquifer north of Interstate Highway 80 on the Salt Flats is mainly by infiltration of precipitation and wind-driven floods of surface brine. Discharge was mainly by evaporation at the playa surface and withdrawals from brine-collection ditches. Some water was transpired by phreatophytes, and some leaked into the alluvial fan along the western edge of the playa.</p><p>Salt-scraping studies indicate that the amount of halite on the Salt Flats is directly related to the amount of recharge through the surface (which causes re-solution of halite) and the amount of evaporation at the surface (which causes crystallization of halite). Evaporation rates through sediment-covered salt crust and the gypsum surface were estimated at between 3x10<sup>-4</sup> and 4x10<sup>-3</sup> inches per day during the summer and fall of 1976. Evaporation rates through the surface of thick perennial salt crust were much higher.</p><p>The concentration of dissolved solids in brine in the shallow-brine aquifer varies, but it generally increases from the edges of the playas toward areas of salt crust. Dissolved-solids concentration in the shallow brine ranges from less than 100,000 to more than 300,000 milligrams per liter on both playas. The increase in salinity toward areas of salt crust reflects the natural direction of brine movement through the aquifer toward the natural discharge area.</p><p>On the Salt Flats, the percentages of dissolved potassium chloride and magnesium chloride in the shallow-brine aquifer generally increase from the edge of the playa to- ward the salt crust. The relative enrichment in potassium and magnesium reflects the many years of subsurface drainage toward the main discharge area (the salt crust) prior to man's withdrawal of brine. By artificially extracting brines from the carbonate muds, the percentages of potassium and magnesium have decreased while brine salinity has been maintained by re-solution of the salt crust.</p><p>The configuration of the density-corrected potentiometric surface in the fall of 1976 indicates that brine in the shallow-brine aquifer under the Bonneville Racetrack was draining toward brine-collection ditches or a well field to the west. Ground-water divides have no effect on the movement of dissolved salt across the surface in wind-driven floods, and salt in surface brine was carried from the racetrack into the area of influence of the ditches by such surface movement. During 1976 on the Salt Flats, some brine was moving through the shallow-brine aquifer across lease and property boundaries.</p><p>An evaluation of suggested remedial measures indicates that none will completely eliminate the conflict between uses or transform the Bonneville Salt Flats to its original state prior to man's activities in the area.</p>","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/wsp2057","collaboration":"Prepared in cooperation with the U.S. Bureau of Land Management","usgsCitation":"Lines, G.C., 1979, Hydrology and surface morphology of the Bonneville Salt Flats and Pilot Valley Playa, Utah: U.S. Geological Survey Water Supply Paper 2057, vii, 107 p., https://doi.org/10.3133/wsp2057.","productDescription":"vii, 107 p.","numberOfPages":"117","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":138280,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/2057/report-thumb.jpg"},{"id":27729,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/2057/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Utah","otherGeospatial":"Bonneville Salt Flats, Pilot Valley Playa","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4acce4b07f02db67e898","contributors":{"authors":[{"text":"Lines, Gregory C.","contributorId":50502,"corporation":false,"usgs":true,"family":"Lines","given":"Gregory","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":144712,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
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 \"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e2e4b07f02db5e4e29","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":529098,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":55220,"text":"wdrIA781 - 1979 - Water resources data for Iowa, water year 1978","interactions":[],"lastModifiedDate":"2016-02-29T11:58:49","indexId":"wdrIA781","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1979","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"IA-78-1","title":"Water resources data for Iowa, water year 1978","docAbstract":"<p>This report was prepared by personnel of the Iowa district of the Water Resources Division of the U.S. Geological Survey under the supervision of S. W. Wiitala, District Chief, and Alfred Clebsch, Jr., Regional Hydrologist, Central Region. It was done in cooperation with the State of Iowa and with other agencies. This report is one of a series issued by Iowa. General direction for the series is by J. S. Cragwall, Jr., Chief Hydrologist, U.S. Geological Survey, and G. W. Whetstone, Assistant Chief Hydrologist for Scientific Publications and Data Management.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wdrIA781","collaboration":"Prepared in cooperation with the Iowa Geological Survey and with other State and Federal agencies","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1979, Water resources data for Iowa, water year 1978: U.S. Geological Survey Water Data Report IA-78-1, x, 256 p., https://doi.org/10.3133/wdrIA781.","productDescription":"x, 256 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":351,"text":"Iowa Water Science 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,{"id":18483,"text":"ofr791290 - 1979 - Ground-water levels and quality data for Georgia, 1978","interactions":[],"lastModifiedDate":"2022-01-10T20:36:32.204256","indexId":"ofr791290","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1979","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":"79-1290","title":"Ground-water levels and quality data for Georgia, 1978","docAbstract":"Mean water levels in wells across Georgia were from 0.25 foot higher to 11.4 feet lower in 1978 than in 1977, and in some areas were the lowest on record. Water levels in the principal artesian aquifer underwent a long-term decline during the period 1969-78. In some areas water levels dropped more than 10 feet. Wells tapping the Clayton Limestone in the Albany area showed a long-term decline during the period 1969-78, and in some wells water levels dropped more than 20 feet. Water levels in the Cretaceous aquifer system showed little fluctuation during 1978; however, in a well located in Chattahoochee County, water levels declined 4.4 feet during 1969-78. In the Piedmont area mean water levels remained the same to 2.2 feet lower in 1978 than in 1977, and showed no long-term trend. Chloride concentrations in the principal artesian aquifer in the Savannah area remained stable and in the Brunswick area continued to rise during 1978. Daily mean water-level fluctuations and trends for 1978 and fluctuations of the monthly mean water level for the previous 10 years are shown in hydrographs of 33 selected observation wells in Georgia. Chloride concentrations in 11 wells in the Savannah and Brunswick areas are shown in graphs of monthly values over the previous 10 years. A short narrative explains fluctuations and trends in each of the hydrographs and chloride concentration graphs shown. (Woodard-USGS)","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr791290","collaboration":"Prepared in cooperation with the Georgia Department of Natural Resources Georgia Geologic Survey","usgsCitation":"Clarke, J., Hester, W., and O’Byrne, M.P., 1979, Ground-water levels and quality data for Georgia, 1978: U.S. Geological Survey Open-File Report 79-1290, vi, 94 p., https://doi.org/10.3133/ofr791290.","productDescription":"vi, 94 p.","costCenters":[{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true}],"links":[{"id":153102,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1979/1290/report-thumb.jpg"},{"id":394131,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1979/1290/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United 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 \"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa9e4b07f02db6688b5","contributors":{"authors":[{"text":"Clarke, J.S.","contributorId":89526,"corporation":false,"usgs":true,"family":"Clarke","given":"J.S.","email":"","affiliations":[],"preferred":false,"id":179213,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hester, W.G.","contributorId":29455,"corporation":false,"usgs":true,"family":"Hester","given":"W.G.","email":"","affiliations":[],"preferred":false,"id":179212,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"O’Byrne, M. P.","contributorId":19963,"corporation":false,"usgs":true,"family":"O’Byrne","given":"M.","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":179211,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":31042,"text":"ofr791568 - 1979 - Seismic refraction profile, Kingdom of Saudi Arabia: field operations, instrumentation, and initial results","interactions":[],"lastModifiedDate":"2012-02-02T00:09:18","indexId":"ofr791568","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1979","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":"79-1568","title":"Seismic refraction profile, Kingdom of Saudi Arabia: field operations, instrumentation, and initial results","docAbstract":"In February 1978 a seismic deep-refraction profile was recorded by the USGS along a 1000-km line across the Arabian Shield in western Saudi Arabia. The line begins in Paleozoic and Mesozoic cover rocks near Riyadh on the Arabian Platform, leads southwesterly across three major Precambrian tectonic provinces, traverses Cenozoic rocks of the coastal plain near Jizan (Tihamat Asir), and terminates at the outer edge of the Farasan Bank in the southern Red Sea. More than 500 surveyed recording sites were occupied, including 19 in the Farasan Islands. Six shot points were used--five on land, with charges placed mostly below water table in drill holes, and one at sea, with charges placed on the sea floor and fired from a ship. The total charge consumed was slightly in excess of 61 metric tons in 21 discrete firings. \r\n\r\nSeismic energy was recorded by means of a set of 100 newly developed portable seismic stations. Each station consists of a standard 2-Hz vertical geophone coupled to a self-contained analog recording instrument equipped with a magnetic-tape cassette. The stations were deployed in groups of 20 by five observer teams, each generally consisting of two scientist-technicians and a surveyor-guide. On the day prior to deployment, the instruments were calibrated and programmed for automatic operation by means of a specially designed device called a hand-held tester. At each of ten pre-selected recording time windows on a designated firing day, the instruments were programmed to turn on, stabilize, record internal calibration signals, record the seismic signals at three levels of amplification, and then deactivate. After the final window in the firing sequence, all instruments were retrieved and their data tapes removed for processing. A specially designed, field tape- dubbing system was utilized at shot point camps to organize and edit data recorded on the cassette tapes. The main functions of this system are to concatenate all data from each shot on any given day onto a single shot tape, and to provide hard copy for monitoring recorder performance so that any problems can be corrected prior to the next deployment. \r\n\r\nComposite digital record sections were produced from the dubbed tapes for each shot point by a portable processing and plotting system. The heart of this system is a DEC PDP 11VO3 computer, which controls a cassette playback unit identical to those used in the recorders and dubbers, a set of discriminators, a time-code translator, a digitizer, and a digital plotter. The system was used to maintain various informational data sets and to produce tabulations and listings of various sorts during the field operations, in addition to its main task of producing digital record sections. \r\n\r\nTwo master clocks, both set to time signals broadcast by the British Broadcasting Corporation, provided absolute time for the recording operations. One was located on the ship and the other was stationed at a base camp on the mainland. The land-based master clock was used to set three additional master clocks located at the other active shot points a few days in advance of each firing, and these clocks were then used to set the internal clocks in the portable seismic stations via the hand-held tester. A master clock signal was also linked to the firing system at each shot point for determination of the absolute shot instant. \r\n\r\nIt is possible to construct a generalized crustal model from examination of the six shot point composite record sections obtained in the field. Such a model rests upon a number of simplifying assumptions and will almost certainly be modified at a later stage of interpretation. The main assumptions are that the crust consists of two homogeneous isotropic layers having no velocity inversion,, that the Mohorovicic discontinuity is sharp, and that effects of surface inhomogeneities and elevation changes can be ignored. The main characteristics of the tentative model are the following: \r\n\r\n(1) The thickness of th","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr791568","usgsCitation":"Blank, H.R., Healy, J.H., Roller, J., Lamson, R., Fisher, F., McClearn, R., and Allen, S., 1979, Seismic refraction profile, Kingdom of Saudi Arabia: field operations, instrumentation, and initial results: U.S. Geological Survey Open-File Report 79-1568, ii, 52 p. ;28 cm., https://doi.org/10.3133/ofr791568.","productDescription":"ii, 52 p. ;28 cm.","costCenters":[],"links":[{"id":163371,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1979/1568/report-thumb.jpg"},{"id":59593,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1979/1568/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":59594,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1979/1568/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":59595,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1979/1568/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":59596,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1979/1568/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":59597,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1979/1568/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":59598,"rank":405,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1979/1568/plate-6.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":59599,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1979/1568/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ae4b07f02db5fb25f","contributors":{"authors":[{"text":"Blank, H. Richard","contributorId":69541,"corporation":false,"usgs":true,"family":"Blank","given":"H.","email":"","middleInitial":"Richard","affiliations":[],"preferred":false,"id":204654,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Healy, J. H.","contributorId":48968,"corporation":false,"usgs":true,"family":"Healy","given":"J.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":204652,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Roller, John","contributorId":89948,"corporation":false,"usgs":true,"family":"Roller","given":"John","affiliations":[],"preferred":false,"id":204656,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Lamson, Ralph","contributorId":106949,"corporation":false,"usgs":true,"family":"Lamson","given":"Ralph","affiliations":[],"preferred":false,"id":204657,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Fisher, Fred","contributorId":71606,"corporation":false,"usgs":true,"family":"Fisher","given":"Fred","email":"","affiliations":[],"preferred":false,"id":204655,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"McClearn, Robert","contributorId":12534,"corporation":false,"usgs":true,"family":"McClearn","given":"Robert","email":"","affiliations":[],"preferred":false,"id":204651,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Allen, Steve","contributorId":53010,"corporation":false,"usgs":true,"family":"Allen","given":"Steve","email":"","affiliations":[],"preferred":false,"id":204653,"contributorType":{"id":1,"text":"Authors"},"rank":7}]}}
,{"id":49373,"text":"ofr791160 - 1979 - Land use and land cover and associated maps for Athens, Georgia, South Carolina","interactions":[],"lastModifiedDate":"2012-02-02T00:11:20","indexId":"ofr791160","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1979","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":"79-1160","title":"Land use and land cover and associated maps for Athens, Georgia, South Carolina","language":"ENGLISH","doi":"10.3133/ofr791160","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1979, Land use and land cover and associated maps for Athens, Georgia, South Carolina: U.S. Geological Survey Open-File Report 79-1160, 4 maps, https://doi.org/10.3133/ofr791160.","productDescription":"4 maps","costCenters":[],"links":[{"id":175520,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b2de4b07f02db6b3f08","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":531896,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":29695,"text":"wri78108 - 1979 - Contamination potential in the Silurian Dolomite aquifer, eastern Wisconsin","interactions":[],"lastModifiedDate":"2015-10-21T09:23:47","indexId":"wri78108","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1979","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":"78-108","title":"Contamination potential in the Silurian Dolomite aquifer, eastern Wisconsin","docAbstract":"<p>The Silurian dolomite aquifer is used for water supply in much of a 14-county area bordering Lake Michigan in eastern Wisconsin. Because of the rapidity of ground-water movement, the aquifer is susceptible to contamination by waters percolating downward from surface sources. Maps showing the distribution of permeability, the thickness of unconsolidated materials, and the depth to the water table are combined to show areas where the dolomite aquifer has the greatest contamination potential. Several areas have above-normal potential for contamination. These include the Casco-Luxemburg area of Kewaunee County, the area south of Chilton in Calumet County, a part of western Manitowoc County, drainageway areas in Sheboygan County, the Byron-Campbellsport area of Fond du Lac County, the Sussex-Lannon-Cedarburg areas of Waukesha and Ozaukee Counties, and the Racine-Burlington areas of Racine County.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri78108","usgsCitation":"Sherrill, M., 1979, Contamination potential in the Silurian Dolomite aquifer, eastern Wisconsin: U.S. Geological Survey Water-Resources Investigations Report 78-108, 2 Plates: 33.87 x 43.95 inches, https://doi.org/10.3133/wri78108.","productDescription":"2 Plates: 33.87 x 43.95 inches","onlineOnly":"N","additionalOnlineFiles":"Y","costCenters":[{"id":677,"text":"Wisconsin Water Science Center","active":true,"usgs":true}],"links":[{"id":159502,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":58518,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1978/0108/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":58519,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1978/0108/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Wisconsin","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -89.05517578125,\n              42.49640294093708\n            ],\n            [\n              -87.615966796875,\n              42.48830197960227\n            ],\n            [\n              -87.78076171875,\n              43.41302868475145\n            ],\n            [\n              -87.56103515625,\n              43.96909818325174\n            ],\n            [\n              -87.484130859375,\n              44.36313311380771\n            ],\n            [\n              -87.4951171875,\n              44.55133484083592\n            ],\n            [\n              -87.989501953125,\n              44.535674532413196\n            ],\n            [\n              -88.143310546875,\n              44.402391829093915\n            ],\n            [\n              -88.17626953125,\n              44.10336537791152\n            ],\n            [\n              -88.319091796875,\n              43.79488907226601\n            ],\n            [\n              -88.385009765625,\n              43.636075155965784\n            ],\n            [\n              -88.692626953125,\n              43.004647127794435\n            ],\n            [\n              -88.714599609375,\n              42.76314586689494\n            ],\n            [\n              -88.8134765625,\n              42.577354839557856\n            ],\n            [\n              -89.05517578125,\n              42.49640294093708\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4af4e4b07f02db691d68","contributors":{"authors":[{"text":"Sherrill, M.G.","contributorId":19945,"corporation":false,"usgs":true,"family":"Sherrill","given":"M.G.","email":"","affiliations":[],"preferred":false,"id":201964,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":9941,"text":"ofr791300 - 1979 - Water-quality investigation of the Flat Bayou watershed, Jefferson County, Arkansas","interactions":[],"lastModifiedDate":"2022-03-02T20:54:05.556074","indexId":"ofr791300","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1979","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":"79-1300","title":"Water-quality investigation of the Flat Bayou watershed, Jefferson County, Arkansas","docAbstract":"<p>The results of a 1-year study, in 1977-78, of surface-water quality in the Flat Bayou watershed, Jefferson County, Ark. are presented to document conditions before implementation of Soil Conservation Service programs. Analysis of samples collected at two sites showed that oxygen depletion, as low as 32 percent of saturation at times, and high concentrations of pesticides on the streambed were the most serious water-quality problems in the watershed. The pesticides aldrin, DDD, DDE, DDT, dieldrin, endrin, heptachlor epoxide, lindane, and toxaphene were found in samples of the bottom material. One sample of bottom material contained an unusually high toxaphene concentration of 160 micrograms per kilogram.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr791300","collaboration":"Prepared in cooperation with the U.S. Department of Agriculture, Soil Conservation Service","usgsCitation":"Lamb, T., 1979, Water-quality investigation of the Flat Bayou watershed, Jefferson County, Arkansas: U.S. Geological Survey Open-File Report 79-1300, ii, 19 p., https://doi.org/10.3133/ofr791300.","productDescription":"ii, 19 p.","costCenters":[],"links":[{"id":396674,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1979/1300/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":143213,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1979/1300/report-thumb.jpg"}],"country":"United States","state":"Arkansas","county":"Jefferson County","otherGeospatial":"Flat Bayou watershed","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -92.21923828124999,\n              33.87041555094183\n            ],\n            [\n              -91.56005859375,\n              33.87041555094183\n            ],\n            [\n              -91.56005859375,\n              34.397844946449865\n            ],\n            [\n              -92.21923828124999,\n              34.397844946449865\n            ],\n            [\n              -92.21923828124999,\n              33.87041555094183\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e3e4b07f02db5e55fd","contributors":{"authors":[{"text":"Lamb, T.E.","contributorId":58272,"corporation":false,"usgs":true,"family":"Lamb","given":"T.E.","email":"","affiliations":[],"preferred":false,"id":160547,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":44543,"text":"wri7985 - 1979 - Flow routing in the Susquehanna River Basin: Part III -- Routing reservoir releases in the Tioga and Chemung rivers system, Pennsylvania, and New York, 1977","interactions":[],"lastModifiedDate":"2017-07-07T08:34:32","indexId":"wri7985","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1979","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":"79-85","title":"Flow routing in the Susquehanna River Basin: Part III -- Routing reservoir releases in the Tioga and Chemung rivers system, Pennsylvania, and New York, 1977","docAbstract":"<p>Channel-routing models were used to route hypothetical releases from reservoirs in the upper Tioga River basin, Pennsylvania. These releases were routed northward down the Tioga River to Lindley, Erwins, and Corning, New York: combined with flows routed down the Cohocton River from Campbell to Corning, New York; and then routed southeastward down the Chemung River from Corning to Chemung, New York. The models used to route the flows of Cohocton and Chemung Rivers accounted for bank-storage discharge and streamflow depletion by well pumpage. In general, 17 water years of concurrent streamflow data were available for model calibration and verification.</p>\n<p>Three hypothetical reservoir releases were made from the reservoirs and routed to Wilkes-Barre, Pennsylvania, using the models developed in this study and models developed downstream to Wilkes-Barre in a previous study. A hypothetical makeup water requirement of 65 cubic feet per second was assumed. Two historical low-flow periods were investigated. The first hypothetical release investigated was a constant 100 cubic feet per second, and the second release was a constant 70 cubic feet per second. The third scheme was a hypothetical release of 100 cubic feet per second for three days followed by a constant 70 cubic feet per second for the duration of the period considered. Constant 100 cubic feet per second releases arrived downstream more quickly than constant 70 cubic feet per second releases for both test periods, but delivered more water than required to satisfy the assumed makeup requirement. The third release scheme was generally the most efficient of the three schemes tested.&nbsp;</p>\n<p>Although inherent modeling errors exist in all the simulated data, the accuracy of the estimated routed reservoir releases at the downstream sites is considered good.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri7985","usgsCitation":"Armbruster, J.T., 1979, Flow routing in the Susquehanna River Basin: Part III -- Routing reservoir releases in the Tioga and Chemung rivers system, Pennsylvania, and New York, 1977: U.S. Geological Survey Water-Resources Investigations Report 79-85, v, 34 p., https://doi.org/10.3133/wri7985.","productDescription":"v, 34 p.","numberOfPages":"43","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":532,"text":"Pennsylvania Water Science Center","active":true,"usgs":true}],"links":[{"id":134595,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/wri7985.jpg"},{"id":310279,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1979/0085/report.pdf","text":"Report","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"New York, Pennsylvania","otherGeospatial":"Chemung River, Tioga River","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -77.5030517578125,\n              41.176586696571015\n            ],\n            [\n              -77.5030517578125,\n              42.374778361114195\n            ],\n            [\n              -75.74523925781249,\n              42.374778361114195\n            ],\n            [\n              -75.74523925781249,\n              41.176586696571015\n            ],\n            [\n              -77.5030517578125,\n              41.176586696571015\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e488de4b07f02db51dabb","contributors":{"authors":[{"text":"Armbruster, Jeffrey T.","contributorId":37707,"corporation":false,"usgs":true,"family":"Armbruster","given":"Jeffrey","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":229970,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":67707,"text":"l75 - 1979 - Land use and land cover, 1971-73, Florence, South Carolina; North Carolina","interactions":[],"lastModifiedDate":"2012-02-10T00:11:28","indexId":"l75","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1979","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":321,"text":"Land Use and Land Cover","code":"L","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"75","title":"Land use and land cover, 1971-73, Florence, South Carolina; North Carolina","language":"ENGLISH","doi":"10.3133/l75","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1979, Land use and land cover, 1971-73, Florence, South Carolina; North Carolina: U.S. Geological Survey Land Use and Land Cover 75, -, https://doi.org/10.3133/l75.","productDescription":"-","costCenters":[],"links":[{"id":186213,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":261014,"rank":900,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/l/075/plate-1.pdf"}],"scale":"250000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -80,34 ], [ -80,35 ], [ -78,35 ], [ -78,34 ], [ -80,34 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b24e4b07f02db6aebc8","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":534453,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":57480,"text":"wdrKY781 - 1979 - Water Resources Data for Kentucky, Water Year 1978","interactions":[],"lastModifiedDate":"2012-02-02T00:12:09","indexId":"wdrKY781","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1979","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"KY-78-1","title":"Water Resources Data for Kentucky, Water Year 1978","language":"ENGLISH","doi":"10.3133/wdrKY781","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1979, Water Resources Data for Kentucky, Water Year 1978: U.S. Geological Survey Water Data Report KY-78-1, 502 p., 5 fig., 3 tab., https://doi.org/10.3133/wdrKY781.","productDescription":"502 p., 5 fig., 3 tab.","costCenters":[],"links":[{"id":181291,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0de4b07f02db5fd043","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":533117,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":48466,"text":"ofr79922 - 1979 - Preconstruction and postconstruction ground-water levels, Lock and Dam 5 and 6, Red River Valley, Louisiana","interactions":[],"lastModifiedDate":"2022-09-07T20:55:15.991638","indexId":"ofr79922","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1979","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":"79-922","title":"Preconstruction and postconstruction ground-water levels, Lock and Dam 5 and 6, Red River Valley, Louisiana","docAbstract":"Proposed construction of a series of locks and dams in the Red River in Louisiana will cause a permanent increase in average river stage. The potentiometric surface of the shallow alluvial aquifer and the water table in the fine-grained material confining the aquifer will be affected. The purpose of this study, using digital-modeling techniques, was to predict the average postconstruction potentiometric surface (steady state) and the water table (nonsteady state) so that potential effects of the water-level changes could be evaluated. Plans for lock and dam 5 at mile 243 (kilometer 390) above the mouth of the Red River call for a pool elevation of 145 feet (44 meters) and will cause an average increase in river stage of 23 feet (7.0 meters). As a result, ground-water levels in the pool area will be raised to near land surface in much of the area between the river and Bayou Pierre and as much as 2 miles (3.2 kilometers) east of the river from the dam upstream to realined mile 220 (kilometer 350). Areas of Barksdale Air Force Base where levels are now near land surface would be enlarged and extend downstream along Flat River to near Curtis. The potentiometric surface may be above land surface near Howard, Anderson Island, and Dixie Gardens. 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