{"pageNumber":"2202","pageRowStart":"55025","pageSize":"25","recordCount":68892,"records":[{"id":43235,"text":"ofr80174 - 1980 - Land use and land cover and associated maps for Breton Sound, Louisiana","interactions":[{"subject":{"id":43234,"text":"ofr75246 - 1975 - Ozarks land use data set; Breton Sound, La.","indexId":"ofr75246","publicationYear":"1975","noYear":false,"title":"Ozarks land use data set; Breton Sound, La."},"predicate":"SUPERSEDED_BY","object":{"id":43235,"text":"ofr80174 - 1980 - Land use and land cover and associated maps for Breton Sound, Louisiana","indexId":"ofr80174","publicationYear":"1980","noYear":false,"title":"Land use and land cover and associated maps for Breton Sound, Louisiana"},"id":1}],"lastModifiedDate":"2012-02-02T00:10:29","indexId":"ofr80174","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","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":"80-174","title":"Land use and land cover and associated maps for Breton Sound, Louisiana","language":"ENGLISH","doi":"10.3133/ofr80174","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1980, Land use and land cover and associated maps for Breton Sound, Louisiana: U.S. Geological Survey Open-File Report 80-174, 3 maps ;50 x 78 cm., https://doi.org/10.3133/ofr80174.","productDescription":"3 maps ;50 x 78 cm.","costCenters":[],"links":[{"id":172918,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b28e4b07f02db6b1692","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":531054,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":23982,"text":"ofr80413 - 1980 - Ground-water-level monitoring for earthquake prediction: A progress report based on data collected in southern California, 1976-79","interactions":[],"lastModifiedDate":"2022-09-22T18:30:57.239581","indexId":"ofr80413","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","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":"80-413","title":"Ground-water-level monitoring for earthquake prediction: A progress report based on data collected in southern California, 1976-79","docAbstract":"<p>The U.S. Geological Survey is conducting a research program to determine if groundwater-level measurements can be used for earthquake prediction. Earlier studies suggest that water levels in wells may be responsive to small strains on the order of 10 to the minus 8th power to 10 to the minus 10th power (dimensionless). Water-level data being collected in the area of the southern California uplift show response to earthquakes and other natural and manmade effects. The data are presently (1979) being made ready for computer analysis. The completed analysis may indicate the presence of precursory earthquake information.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr80413","usgsCitation":"Moyle, W.R., 1980, Ground-water-level monitoring for earthquake prediction: A progress report based on data collected in southern California, 1976-79: U.S. Geological Survey Open-File Report 80-413, Report: v, 60 p.; 1 Plate: 31.94 × 22.53 inches, https://doi.org/10.3133/ofr80413.","productDescription":"Report: v, 60 p.; 1 Plate: 31.94 × 22.53 inches","costCenters":[],"links":[{"id":407229,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_11626.htm","linkFileType":{"id":5,"text":"html"}},{"id":53170,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/0413/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":53171,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1980/0413/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":156246,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1980/0413/report-thumb.jpg"}],"country":"United States","state":"California","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -120,\n              32.519\n            ],\n            [\n              -115,\n              32.519\n            ],\n            [\n              -115,\n              36.25\n            ],\n            [\n              -120,\n              36.25\n            ],\n            [\n              -120,\n              32.519\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a96e4b07f02db65a19d","contributors":{"authors":[{"text":"Moyle, W. R. Jr.","contributorId":85938,"corporation":false,"usgs":true,"family":"Moyle","given":"W.","suffix":"Jr.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":191088,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":23423,"text":"ofr80750 - 1980 - Appraisal of ground-water resources in the San Antonio Creek Valley, Santa Barbara County, California","interactions":[],"lastModifiedDate":"2022-08-16T21:39:59.411695","indexId":"ofr80750","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","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":"80-750","title":"Appraisal of ground-water resources in the San Antonio Creek Valley, Santa Barbara County, California","docAbstract":"<p>A nearly threefold increase in demand for water in the 154-square-mile San Antonio Creek valley in California during the period 1958-77 has increased the potential for overdraft on the ground-water basin. The hydrologic budget for this period showed a perennial yield of about 9,800 acre-feet per year and an annual ground-water discharge of about 11,400 acre-feet per year, comprising net pumpage of 7,100 acre-feet, phreatophyte evapotranspiration of 3,000 acre-feet, and base streamflow of 1 ,300 acre-feet. The base flow in San Antonio Creek could diminish to zero when net pumpage reaches 13,500 acre-feet per year. The environmentally sensitive marshland area of Barka Slough may then become stressed as water normally lost through evapotranspiration is captured by pumpage. The aquifer consists of alluvial valley fill that ranges in thickness from 0 to 3,500 feet. Ground water moves seaward from recharge areas along mountain fronts to a consolidated rock barrier about 5 miles east of the Pacific coast. Upwelling of ground water just east of the barrier has resulted in the 550-acre Barka Slough. Transmissivity of the aquifer ranges from 2,600 to 34,000 feet squared per day, with the lowest values occurring in the central part of the valley where the aquifer is thickest but probably finer grained. The salinity problems are increasing in the agricultural parts of the valley, which is east of the barrier. West of the barrier, stream and ground-water quality is poor, owing to seepage of saline water from the marine shale that underlies the area at shallow depths. A proposed basinwide monitoring program includes 17 water-level sites, 12 water-quality sampling sites, 3 streamflow measuring sites, and periodic infrared aerial photography of Barka Slough. A computer model of the ground-water flow system could be developed to assess the impact of various water-management alternatives.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr80750","usgsCitation":"Hutchinson, C.B., 1980, Appraisal of ground-water resources in the San Antonio Creek Valley, Santa Barbara County, California (WRI/OFR): U.S. Geological Survey Open-File Report 80-750, iv, 48 p., https://doi.org/10.3133/ofr80750.","productDescription":"iv, 48 p.","costCenters":[],"links":[{"id":52752,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1980/0750/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":157478,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1980/0750/report-thumb.jpg"},{"id":405235,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_11757.htm","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"California","county":"Santa Barbara County","otherGeospatial":"San Antonio Creek Valley","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -120.646,\n              34.678\n            ],\n            [\n              -120.112,\n              34.678\n            ],\n            [\n              -120.112,\n              34.853\n            ],\n            [\n              -120.646,\n              34.853\n            ],\n            [\n              -120.646,\n              34.678\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","edition":"WRI/OFR","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac6e4b07f02db67a394","contributors":{"authors":[{"text":"Hutchinson, C. B.","contributorId":94655,"corporation":false,"usgs":true,"family":"Hutchinson","given":"C.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":190078,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":24003,"text":"ofr80574 - 1980 - Reconnaissance of the quality of surface water in the San Rafael River basin, Utah","interactions":[{"subject":{"id":24003,"text":"ofr80574 - 1980 - Reconnaissance of the quality of surface water in the San Rafael River basin, Utah","indexId":"ofr80574","publicationYear":"1980","noYear":false,"title":"Reconnaissance of the quality of surface water in the San Rafael River basin, Utah"},"predicate":"SUPERSEDED_BY","object":{"id":70043690,"text":"70043690 - 1982 - Reconnaissance of the quality of surface water in the San Rafael River basin, Utah","indexId":"70043690","publicationYear":"1982","noYear":false,"title":"Reconnaissance of the quality of surface water in the San Rafael River basin, Utah"},"id":1}],"supersededBy":{"id":70043690,"text":"70043690 - 1982 - Reconnaissance of the quality of surface water in the San Rafael River basin, Utah","indexId":"70043690","publicationYear":"1982","noYear":false,"title":"Reconnaissance of the quality of surface water in the San Rafael River basin, Utah"},"lastModifiedDate":"2016-12-17T12:51:17","indexId":"ofr80574","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","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":"80-574","title":"Reconnaissance of the quality of surface water in the San Rafael River basin, Utah","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr80574","issn":"0094-9140","usgsCitation":"Mundorff, J.C., and Thompson, K.R., 1980, Reconnaissance of the quality of surface water in the San Rafael River basin, Utah: U.S. Geological Survey Open-File Report 80-574, https://doi.org/10.3133/ofr80574.","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":157494,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"country":"United States","state":"Utah","otherGeospatial":"San Rafael River","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -111.5,\n              38.4\n            ],\n            [\n              -111.5,\n              39.75\n            ],\n            [\n              -110,\n              39.75\n            ],\n            [\n              -110,\n              38.4\n            ],\n            [\n              -111.5,\n              38.4\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a62e4b07f02db636a58","contributors":{"authors":[{"text":"Mundorff, J. C.","contributorId":63374,"corporation":false,"usgs":true,"family":"Mundorff","given":"J.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":191128,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Thompson, Kendall R.","contributorId":100854,"corporation":false,"usgs":true,"family":"Thompson","given":"Kendall","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":191129,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":2003,"text":"wsp2064 - 1980 - Relationships between basic soils-engineering equations and basic ground-water flow equations","interactions":[],"lastModifiedDate":"2012-02-02T00:05:22","indexId":"wsp2064","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","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":"2064","title":"Relationships between basic soils-engineering equations and basic ground-water flow equations","docAbstract":"The many varied though related terms developed by ground-water hydrologists and by soils engineers are useful to each discipline, but their differences in terminology hinder the use of related information in interdisciplinary studies. Equations for the Terzaghi theory of consolidation and equations for ground-water flow are identical under specific conditions. A combination of the two sets of equations relates porosity to void ratio and relates the modulus of elasticity to the coefficient of compressibility, coefficient of volume compressibility, compression index, coefficient of consolidation, specific storage, and ultimate compaction. Also, transient ground-water flow is related to coefficient of consolidation, rate of soil compaction, and hydraulic conductivity. Examples show that soils-engineering data and concepts are useful to solution of problems in ground-water hydrology.","language":"ENGLISH","publisher":"U.S. Dept. of the Interior, Geological Survey ;\r\nFor sale by Supt. of Docs., U.S. Govt. Print. Off.,","doi":"10.3133/wsp2064","usgsCitation":"Jorgensen, D.G., 1980, Relationships between basic soils-engineering equations and basic ground-water flow equations: U.S. Geological Survey Water Supply Paper 2064, vi, 40 p. :ill. ;23 cm., https://doi.org/10.3133/wsp2064.","productDescription":"vi, 40 p. :ill. ;23 cm.","costCenters":[],"links":[{"id":138385,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/2064/report-thumb.jpg"},{"id":27447,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/2064/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a5fe4b07f02db6346b3","contributors":{"authors":[{"text":"Jorgensen, Donald G.","contributorId":19537,"corporation":false,"usgs":true,"family":"Jorgensen","given":"Donald","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":144511,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":26930,"text":"wri80106 - 1980 - A technique for estimating flood heights on small streams in the city of Charlotte and Mecklenburg County, North Carolina","interactions":[],"lastModifiedDate":"2017-01-27T09:32:27","indexId":"wri80106","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","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":"80-106","title":"A technique for estimating flood heights on small streams in the city of Charlotte and Mecklenburg County, North Carolina","docAbstract":"A method for estimating the height reached by floods having recurrence intervals of 10, 20, and 100 years is defined for unregulated streams in Charlotte and Mecklenburg County draining areas of less than 1.0 square mile. Flood heights, defined as the vertical distance between the streambed at riffles and the floodwater surface, can be used to estimate flood elevations on small streams where flood profiles and flood inundation maps are not available. An illustrative example is given of how the method can be used with streambed elevation data and topographic maps to estimate flood elevations and delineate inundated areas.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri80106","usgsCitation":"Eddins, W.H., and Jackson, N., 1980, A technique for estimating flood heights on small streams in the city of Charlotte and Mecklenburg County, North Carolina: U.S. Geological Survey Water-Resources Investigations Report 80-106, iv, 16 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri80106.","productDescription":"iv, 16 p. :ill., maps ;28 cm.","costCenters":[{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true}],"links":[{"id":158457,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"country":"United States","state":"North Carolina","county":"Mecklenburg County","city":"Charlotte","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-80.7823,35.5113],[-80.7867,35.5031],[-80.7889,35.4949],[-80.7831,35.4836],[-80.7819,35.475],[-80.7779,35.4668],[-80.7778,35.4614],[-80.7744,35.4578],[-80.7549,35.423],[-80.7525,35.4148],[-80.7553,35.4125],[-80.7638,35.4134],[-80.7693,35.402],[-80.7551,35.3944],[-80.7364,35.3786],[-80.7187,35.3624],[-80.704,35.3552],[-80.6983,35.3507],[-80.6822,35.3131],[-80.6677,35.2705],[-80.6214,35.2499],[-80.5954,35.2369],[-80.5485,35.2108],[-80.6245,35.1487],[-80.7328,35.0627],[-80.7645,35.0375],[-80.7684,35.0348],[-80.7746,35.0329],[-80.7858,35.0315],[-80.7892,35.0314],[-80.8009,35.0286],[-80.8155,35.0204],[-80.8194,35.019],[-80.8216,35.018],[-80.8216,35.0167],[-80.8288,35.0098],[-80.835,35.0061],[-80.8405,35.0016],[-80.8604,35.0246],[-80.8854,35.0535],[-80.9016,35.0716],[-80.9312,35.1049],[-80.9373,35.1018],[-81.0383,35.0452],[-81.0419,35.0432],[-81.0447,35.0468],[-81.0464,35.0482],[-81.0483,35.0507],[-81.0503,35.0527],[-81.0528,35.0557],[-81.0548,35.0582],[-81.0568,35.0611],[-81.0577,35.0636],[-81.0586,35.067],[-81.0582,35.0722],[-81.0577,35.0788],[-81.0566,35.0834],[-81.0554,35.0868],[-81.0541,35.0904],[-81.0533,35.0927],[-81.0523,35.0956],[-81.0503,35.0975],[-81.0487,35.099],[-81.0462,35.1003],[-81.0437,35.1014],[-81.042,35.1022],[-81.0391,35.1027],[-81.0369,35.1036],[-81.0352,35.1054],[-81.0344,35.1072],[-81.0341,35.1095],[-81.0341,35.1136],[-81.0358,35.1186],[-81.0363,35.1213],[-81.038,35.124],[-81.0408,35.1267],[-81.0425,35.1281],[-81.0454,35.1289],[-81.0476,35.1295],[-81.0499,35.1302],[-81.051,35.1313],[-81.0521,35.1335],[-81.0523,35.1365],[-81.0517,35.1392],[-81.0501,35.142],[-81.0476,35.1463],[-81.0448,35.1494],[-81.0238,35.1486],[-81.0176,35.1536],[-81.0109,35.1532],[-81.0076,35.1569],[-81.0088,35.165],[-81.0049,35.1728],[-81.0045,35.1814],[-81.0046,35.1864],[-81.0063,35.1923],[-81.0064,35.1973],[-81.0054,35.2055],[-81.0071,35.2109],[-81.0129,35.2231],[-81.0113,35.2309],[-81.012,35.2349],[-81.0082,35.2509],[-81.0139,35.2585],[-81.0152,35.2685],[-81.0143,35.2876],[-81.0133,35.293],[-81.0105,35.2944],[-81.0033,35.3017],[-81.0022,35.3045],[-80.9961,35.3113],[-80.9938,35.3132],[-80.9894,35.3205],[-80.9844,35.3237],[-80.9805,35.3287],[-80.9823,35.3341],[-80.984,35.3373],[-80.9818,35.3446],[-80.9706,35.3501],[-80.9656,35.3506],[-80.9593,35.3489],[-80.9537,35.3521],[-80.9442,35.3521],[-80.9374,35.3572],[-80.9285,35.3614],[-80.9268,35.3627],[-80.9296,35.3636],[-80.9432,35.3658],[-80.9505,35.3675],[-80.9563,35.3738],[-80.9597,35.3756],[-80.9625,35.3756],[-80.9647,35.3738],[-80.9669,35.3688],[-80.9697,35.3669],[-80.9742,35.3642],[-80.9776,35.3646],[-80.9844,35.3695],[-80.9868,35.38],[-80.9846,35.3822],[-80.9806,35.3823],[-80.9761,35.3828],[-80.9632,35.3901],[-80.9554,35.3925],[-80.9549,35.4006],[-80.959,35.4133],[-80.9569,35.4288],[-80.9587,35.436],[-80.9527,35.446],[-80.9465,35.4524],[-80.9421,35.457],[-80.9432,35.4602],[-80.9506,35.4656],[-80.9518,35.4701],[-80.948,35.481],[-80.947,35.486],[-80.951,35.4942],[-80.9612,35.4986],[-80.9664,35.509],[-80.9637,35.5131],[-80.9586,35.5163],[-80.9569,35.5177],[-80.7823,35.5113]]]},\"properties\":{\"name\":\"Mecklenburg\",\"state\":\"NC\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b17e4b07f02db6a5cf8","contributors":{"authors":[{"text":"Eddins, William H.","contributorId":65119,"corporation":false,"usgs":true,"family":"Eddins","given":"William","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":197266,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Jackson, N.M. Jr.","contributorId":19600,"corporation":false,"usgs":true,"family":"Jackson","given":"N.M.","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":197265,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":26988,"text":"wri8043 - 1980 - A statistical analysis of the quality of surface water in Nebraska","interactions":[],"lastModifiedDate":"2018-11-08T16:06:19","indexId":"wri8043","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","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":"80-43","title":"A statistical analysis of the quality of surface water in Nebraska","docAbstract":"<p>This report provides descriptive statistics for 29 chemical or biological constituents for 109 stream sites in Nebraska sampled by the U.S. Geological Survey beginning in 1946. Also provided for each site are regression equations relating specific conductance to each of 12 chemical constituents and a regression equation relating specific conductance to stream discharge. </p><p>The descriptive statistics are presented by river basins. Water leaving these basins that has the lowest mean specific conductance (266 umho/cm) is from the Niobrara River at Verdel, and water that has the highest (1,890 umho/cm) is from the South Platte River at Roscoe. Statewide, the principal cations in streamflow are calcium and sodium, and the principal anions are bicarbonate and sulfate. Calcium and bicarbonate usually predominate where mean specific conductance is less than 1,000 umho/cm, and sodium and sulfate predominate where the mean exceeds 1,000 umho/cm. </p><p>Based on regression equations, dissolved solids, hardness, calcium, magnesium and bicarbonate, with some exceptions, correlate well with specific conductance for all stream sites. </p><p>Illustrations of how regression equations may be used to estimate water quality of streamflow are given and are compared with values from actual analyses.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri8043","usgsCitation":"Engberg, R., 1980, A statistical analysis of the quality of surface water in Nebraska: U.S. Geological Survey Water-Resources Investigations Report 80-43, v, 277 p., https://doi.org/10.3133/wri8043.","productDescription":"v, 277 p.","numberOfPages":"287","costCenters":[{"id":595,"text":"U.S. Geological 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,{"id":25020,"text":"pp1107 - 1980 - Erosion, sediment discharge, and channel morphology in the upper Chattahoochee River basin, Georgia, with a discussion of the contribution of suspended sediment to stream quality","interactions":[{"subject":{"id":21771,"text":"ofr78576 - 1978 - Erosion, sediment discharge, and channel morphology in the Upper Chattahoochee River basin, Georgia","indexId":"ofr78576","publicationYear":"1978","noYear":false,"title":"Erosion, sediment discharge, and channel morphology in the Upper Chattahoochee River basin, Georgia"},"predicate":"SUPERSEDED_BY","object":{"id":25020,"text":"pp1107 - 1980 - Erosion, sediment discharge, and channel morphology in the upper Chattahoochee River basin, Georgia, with a discussion of the contribution of suspended sediment to stream quality","indexId":"pp1107","publicationYear":"1980","noYear":false,"title":"Erosion, sediment discharge, and channel morphology in the upper Chattahoochee River basin, Georgia, with a discussion of the contribution of suspended sediment to stream quality"},"id":1}],"lastModifiedDate":"2017-01-05T12:28:04","indexId":"pp1107","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","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":"1107","title":"Erosion, sediment discharge, and channel morphology in the upper Chattahoochee River basin, Georgia, with a discussion of the contribution of suspended sediment to stream quality","docAbstract":"The 3,550 square miles of the Upper Chattahoochee River basin is an area of diverse physiographic and land-use characteristics. The headwater areas are mountainous with steep, relatively narrow channels. Land in the headwater areas is heavily forested, but small towns and farms are common in the valleys of large streams. Downstream, the basin is characterized by low hills and wider stream channels. Land in this part of the basin is also predominantly forested; however, large agricultural and urban areas are common. Urban land use is particularly intensive within the Atlanta Metropolitan Area. ","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/pp1107","usgsCitation":"Faye, R.E., Carey, W.P., Stamer, J., and Kleckner, R., 1980, Erosion, sediment discharge, and channel morphology in the upper Chattahoochee River basin, Georgia, with a discussion of the contribution of suspended sediment to stream quality: U.S. Geological Survey Professional Paper 1107, 85 p., https://doi.org/10.3133/pp1107.","productDescription":"85 p.","costCenters":[{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true}],"links":[{"id":122566,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/1107/report-thumb.jpg"},{"id":54022,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/1107/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Georgia","otherGeospatial":"Upper Chattahoochee River basin","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -84.21295166015629,\n              34.24245948736849\n            ],\n            [\n              -84.13604736328122,\n              34.56764471968292\n            ],\n            [\n              -83.98223876953124,\n              34.768691457552706\n            ],\n            [\n              -83.726806640625,\n              34.75740963726004\n            ],\n            [\n              -83.50982666015624,\n              34.70775131553933\n            ],\n            [\n              -83.47412109374999,\n              34.54954921593403\n            ],\n            [\n              -83.47137451171875,\n              34.51334640147576\n            ],\n            [\n              -84.00009155273438,\n              33.970697997361654\n            ],\n            [\n              -84.36538696289062,\n              33.87041555094183\n            ],\n            [\n              -84.4793701171875,\n              33.73804486328907\n            ],\n            [\n              -84.53430175781247,\n              33.6031820405205\n            ],\n            [\n              -84.70733642578124,\n              33.447484889088855\n            ],\n            [\n              -84.6551513671875,\n              33.351179088043494\n            ],\n            [\n              -84.7540283203125,\n              33.284619968887675\n            ],\n            [\n              -84.76226806640624,\n              33.18353672893615\n            ],\n            [\n              -84.84191894531249,\n              33.100745405144245\n            ],\n            [\n              -84.8583984375,\n              32.9372338139709\n            ],\n            [\n              -85.02044677734375,\n              32.858825196463854\n            ],\n            [\n              -85.177001953125,\n              32.857671610787456\n            ],\n            [\n              -85.27313232421878,\n              32.88996633815203\n            ],\n            [\n              -85.30746459960939,\n              33.04781007347206\n            ],\n            [\n              -85.26214599609375,\n              33.167444534375925\n            ],\n            [\n              -85.1708221435547,\n              33.23983613293645\n            ],\n            [\n              -85.16738891601562,\n              33.31905344502012\n            ],\n            [\n              -85.07812500000003,\n              33.46810795527894\n            ],\n            [\n              -84.99092102050781,\n              33.49445251114961\n            ],\n            [\n              -84.83230590820312,\n              33.67063988581374\n            ],\n            [\n              -84.70184326171875,\n              33.7597402884442\n            ],\n            [\n              -84.55490112304689,\n              33.91487347147951\n            ],\n            [\n              -84.43130493164067,\n              34.025347738147936\n            ],\n            [\n              -84.35302734375003,\n              34.07882486401267\n            ],\n            [\n              -84.21295166015629,\n              34.24245948736849\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ee4b07f02db5fdf58","contributors":{"authors":[{"text":"Faye, Robert E.","contributorId":92221,"corporation":false,"usgs":true,"family":"Faye","given":"Robert","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":193063,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Carey, W. P.","contributorId":105749,"corporation":false,"usgs":true,"family":"Carey","given":"W.","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":193064,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Stamer, J. K.","contributorId":47753,"corporation":false,"usgs":true,"family":"Stamer","given":"J. K.","affiliations":[],"preferred":false,"id":193061,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Kleckner, R.L.","contributorId":70744,"corporation":false,"usgs":true,"family":"Kleckner","given":"R.L.","email":"","affiliations":[],"preferred":false,"id":193062,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":2971,"text":"wsp1535Q - 1980 - The effect of dissolution of volcanic glass on the water chemistry in a tuffaceous aquifer, Rainier Mesa, Nevada","interactions":[],"lastModifiedDate":"2012-02-02T00:05:41","indexId":"wsp1535Q","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","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":"1535","chapter":"Q","title":"The effect of dissolution of volcanic glass on the water chemistry in a tuffaceous aquifer, Rainier Mesa, Nevada","docAbstract":"Geochemistry of ground water associated with the Tertiary tuffs within Rainier Mesa, southern Nevada, was investigated to determine the relative importance of glass dissolution in controlling water chemistry. Water samples were obtained both from interstitial pores in core sections and from free-flowing fractures. Cation com- positions showed that calcium and magnesium decreased as a function of depth in the mesa, as sodium increased. The maximum effect occurs within alteration zones containing clinoptilolite and montmorillonite, suggesting these minerals effectively remove bivalent cations from the system. \r\n\r\nComparisons are made between compositions of ground waters found within Rainier Mesa that apparently have not reacted with secondary minerals and compositions of waters produced by experimental dissolution of vitric and crystalline tufts which comprise the principal aquifers in the area. The two tuff phases have the same bulk chemistry but produce aqueous solutions of different chemistry. Rapid parabolic dissolution of sodium and silica from, and the retention of, potassium within the vitric phase verify previous predictions concerning water compositions associated with vitric volcanic rocks. Parabolic dissolution of the crystalline phase results in solutions high in calcium and magnesium and low in silica. Extrapolation of the parabolic dissolution mechanism for the vitric tuff to long times successfully reproduces, at com- parable pH, cation ratios existing in Rainier Mesa ground water. Comparison of mass- transfer rates of the vitric and crystalline tuffs indicates that the apparent higher glass-surface to aqueous-volume ratio associated with the vitric rocks may account for dominance of the glass reaction.","language":"ENGLISH","publisher":"U.S. Govt. Print. Off. :\r\nfor sale by the Supt. of Docs., GPO,","doi":"10.3133/wsp1535Q","usgsCitation":"White, A.F., Claassen, H., and Benson, L.V., 1980, The effect of dissolution of volcanic glass on the water chemistry in a tuffaceous aquifer, Rainier Mesa, Nevada: U.S. Geological Survey Water Supply Paper 1535, iv, 34 p. :ill. ;23 cm., https://doi.org/10.3133/wsp1535Q.","productDescription":"iv, 34 p. :ill. ;23 cm.","costCenters":[],"links":[{"id":139275,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1535q/report-thumb.jpg"},{"id":29708,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1535q/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e2e4b07f02db5e4cfa","contributors":{"authors":[{"text":"White, Art F.","contributorId":8607,"corporation":false,"usgs":true,"family":"White","given":"Art","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":146070,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Claassen, H.C.","contributorId":74028,"corporation":false,"usgs":true,"family":"Claassen","given":"H.C.","affiliations":[],"preferred":false,"id":146071,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Benson, Larry V. lbenson@usgs.gov","contributorId":1655,"corporation":false,"usgs":true,"family":"Benson","given":"Larry","email":"lbenson@usgs.gov","middleInitial":"V.","affiliations":[{"id":5044,"text":"National Research Program - Central Branch","active":true,"usgs":true}],"preferred":true,"id":146069,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":26242,"text":"wri8035 - 1980 - Water-quality assessment of the Cypress Creek watershed, Warrick County, Indiana","interactions":[],"lastModifiedDate":"2019-11-27T09:48:42","indexId":"wri8035","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","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":"80-35","title":"Water-quality assessment of the Cypress Creek watershed, Warrick County, Indiana","docAbstract":"<p>The U.S. Soil Conservation Service needs chemical, biological, microbiological, and hydrological data to prepare an environmental evaluation of the water quality in the Cypress Creek watershed, Warrick County, Ind., before plans can be devised to (1) improve water quality, (2) minimize flooding, (3) reduce sedimentation, and (4) provide adequate outlets for drainage in the watershed. The U.S. Geological Survey obtained these data for the Soil Conservation Service in a water-quality survey of the watershed from March to August 1979. Past and present surface coal mining is the factor having the greatest impact on water quality in the watershed. The upper reaches of Cypress Creek receive acid-mine drainage from a coal-mine waste slurry during periods of intense rainfall. All the remaining tributaries, except Summer Pecka ditch, drain mined or reclaimed lands. The general water type of Cypress Creek and most of its tributaries is calcium and magnesium sulfate. In contrast, the water type at background site 21 on Summer Pecka ditch is calcium sulfate. Specific conductance ranged from 470 to 4,730 micromhos per centimeter at 25 degrees Celsius, and pH ranged from 1.2 to 8.8. Specific conductance, hardness, and concentrations of major ions and dissolved solids were highest in tributaries affected by mining. The pH was lowest in the same tributaries. Concentrations of iron, manganese, and sulfate in water samples and chlordane, DDT, and PCB 's in streambed samples exceeded water-quality limits set by the U.S. Environmental Protection Agency. (USGS)</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wri8035","usgsCitation":"Bobo, L.L., and Peters, C.A., 1980, Water-quality assessment of the Cypress Creek watershed, Warrick County, Indiana: U.S. Geological Survey Water-Resources Investigations Report 80-35, iv, 67 p. , https://doi.org/10.3133/wri8035.","productDescription":"iv, 67 p. ","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":346,"text":"Indiana Water Science Center","active":true,"usgs":true}],"links":[{"id":157630,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1980/0035/report-thumb.jpg"},{"id":369706,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1980/0035/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Indiana","county":"Warrick","otherGeospatial":"Cypress Creek","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-87.3169,38.2459],[-87.2981,38.246],[-87.2985,38.2319],[-87.073,38.2323],[-87.0728,38.2065],[-87.0166,38.2063],[-87.0165,38.1215],[-87.0733,38.1222],[-87.0727,38.1181],[-87.0727,38.1167],[-87.072,38.1072],[-87.0761,38.1049],[-87.0761,38.1022],[-87.0737,38.1013],[-87.0743,38.0977],[-87.0748,38.0963],[-87.0789,38.0936],[-87.0818,38.0899],[-87.0853,38.089],[-87.0882,38.0849],[-87.0894,38.084],[-87.0911,38.0799],[-87.0928,38.0749],[-87.0928,38.0686],[-87.0974,38.0609],[-87.0979,38.0568],[-87.0938,38.0559],[-87.0909,38.0555],[-87.0879,38.0527],[-87.0885,38.0491],[-87.0926,38.0491],[-87.0949,38.0482],[-87.1019,38.0468],[-87.1148,38.0472],[-87.1253,38.0439],[-87.1271,38.0476],[-87.1312,38.0498],[-87.133,38.0552],[-87.1476,38.0592],[-87.1534,38.0547],[-87.151,38.0461],[-87.1568,38.0401],[-87.1562,38.037],[-87.1538,38.0356],[-87.1544,38.032],[-87.1573,38.0297],[-87.1597,38.0329],[-87.1631,38.032],[-87.1661,38.0301],[-87.166,38.0279],[-87.1543,38.0257],[-87.1526,38.0239],[-87.1531,38.0193],[-87.1572,38.017],[-87.1695,38.0183],[-87.1694,38.0129],[-87.1729,38.0097],[-87.1752,38.007],[-87.1833,38.0028],[-87.1862,37.9965],[-87.192,37.9928],[-87.1949,37.9887],[-87.2123,37.9777],[-87.2216,37.9723],[-87.2239,37.9727],[-87.2303,37.9654],[-87.2285,37.9627],[-87.2296,37.9572],[-87.2313,37.9523],[-87.2336,37.9509],[-87.2383,37.9504],[-87.2406,37.9527],[-87.2464,37.9454],[-87.2499,37.9435],[-87.2678,37.9257],[-87.2684,37.8754],[-87.2767,37.8813],[-87.2884,37.8889],[-87.3002,37.8956],[-87.3027,37.8967],[-87.3058,37.8979],[-87.3205,37.9046],[-87.3312,37.9094],[-87.3374,37.9111],[-87.3434,37.9128],[-87.3668,37.9258],[-87.3759,37.9309],[-87.384,37.9349],[-87.3899,37.9375],[-87.3943,37.9392],[-87.4166,37.9442],[-87.4193,37.9443],[-87.4324,37.9445],[-87.446,37.9416],[-87.4512,37.9394],[-87.4501,38.0373],[-87.4729,38.0371],[-87.4711,38.1242],[-87.4676,38.1242],[-87.4676,38.1655],[-87.4663,38.2035],[-87.3557,38.2048],[-87.317,38.2051],[-87.3167,38.2314],[-87.3169,38.2459]]]},\"properties\":{\"name\":\"Warrick\",\"state\":\"IN\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e5e4b07f02db5e6eb4","contributors":{"authors":[{"text":"Bobo, Linda L.","contributorId":104053,"corporation":false,"usgs":true,"family":"Bobo","given":"Linda","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":196046,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Peters, Charles A. capeters@usgs.gov","contributorId":214,"corporation":false,"usgs":true,"family":"Peters","given":"Charles","email":"capeters@usgs.gov","middleInitial":"A.","affiliations":[],"preferred":true,"id":196045,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":56896,"text":"wdrGA801 - 1980 - Water resources data for Georgia, water year 1980","interactions":[],"lastModifiedDate":"2025-08-19T14:25:11.67895","indexId":"wdrGA801","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","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":"GA-80-1","title":"Water resources data for Georgia, water year 1980","docAbstract":"<p>Water resources data for the 1980 water year for Georgia consists of records of stage, discharge, and water quality of streams; stage and contents of lakes and reservoirs; and ground-water levels. This report contains discharge records for 105 gaging stations; stage for 9 gaging stations; stage and contents for 17 lakes and reservoirs; water quality for 22 continuous stations, 129 periodic stations and miscellaneous sites; peak stage and discharge only for 109 crest-stage partial-record stations and 15 miscellaneous sites; measurements of discharge at 108 low-flow partial-record stations and 69 miscellaneous sites; and water levels of 28 observation wells. These data represent that part of the National Water Data System collected by the U.S. Geological Survey and cooperating State and Federal agencies in Georgia.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wdrGA801","collaboration":"Prepared in cooperation with the State of Georgia and with other Federal agencies","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1980, Water resources data for Georgia, water year 1980: U.S. Geological Survey Water Data Report GA-80-1, xii, 455 p., https://doi.org/10.3133/wdrGA801.","productDescription":"xii, 455 p.","costCenters":[{"id":13634,"text":"South Atlantic Water Science 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,{"id":57524,"text":"wdrAZ791 - 1980 - Water resources data for Arizona, water year 1979","interactions":[],"lastModifiedDate":"2022-11-30T18:45:50.268544","indexId":"wdrAZ791","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","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":"AZ-79-1","title":"Water resources data for Arizona, water year 1979","docAbstract":"<p>Water resources data for the 1978 water year for Arizona consist of records of stage, discharge, and water quality of streams; stage, contents, and water quality of lakes and reservoirs; measurements of ground-water levels; and quality of water from selected wells. Also included are discharge data for crest-stage partial-record stations and water-quality data for partial-record stations. Locations of the gaging stations are shown in figures 4, 6, and 7, and of water-quality stations in figures 5 and 6. Additional water data were collected at various sites, which are not part of the systematic data-collection program, and are published as miscellaneous measurements or miscellaneous water-quality analyses. 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 Arizona.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wdrAZ791","collaboration":"Prepared in cooperation with the State of Arizona and with other agencies","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1980, Water resources data for Arizona, water year 1979: U.S. Geological Survey Water Data Report AZ-79-1, xiii, 614 p., https://doi.org/10.3133/wdrAZ791.","productDescription":"xiii, 614 p.","costCenters":[],"links":[{"id":409876,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/1979/az-79-1/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":185382,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wdr/1979/az-79-1/report-thumb.jpg"}],"country":"United 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 \"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0de4b07f02db5fd18a","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":533131,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":57537,"text":"wdrAL792 - 1980 - Water resources data for Alabama, water year 1979; Volume 2. Tombigbee, Mobile, Dog, Pascagoula, and Tennessee River Basins","interactions":[],"lastModifiedDate":"2022-11-21T18:50:28.642726","indexId":"wdrAL792","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","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":"AL-79-2","title":"Water resources data for Alabama, water year 1979; Volume 2. Tombigbee, Mobile, Dog, Pascagoula, and Tennessee River Basins","docAbstract":"<p>Water resources data for the 1979 water year consist of records of stage, discharge, and water quality of streams; stage and contents of lakes and reservoirs; and water levels and water quality of ground-water wells. This report contains records for water discharge at 51 gaging stations; stage only at 7 gaging stations; stage and contents of 4 lakes and reservoirs; water quality at 34 gaging stations, 103 partial-record stations; and water levels at 44 observation wells. Also included are data for 9 low flow, 5 crest-stage and 3 flood hydrograph partial-record stations. Location of these sites are shown on figures 4-7. Additional water data were collected at various sites, not involved in the systematic data-collection program, and are published as miscellaneous measurements and analyses. Discharge 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 collected by the U.S. Geological Survey and cooperating State and Federal agencies in Alabama.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wdrAL792","collaboration":"Prepared in cooperation with the Geological Survey of Alabama, the Alabama Highway Department, and with other State, municipal, and Federal agencies","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1980, Water resources data for Alabama, water year 1979; Volume 2. Tombigbee, Mobile, Dog, Pascagoula, and Tennessee River Basins: U.S. Geological Survey Water Data Report AL-79-2, x, 454 p., https://doi.org/10.3133/wdrAL792.","productDescription":"x, 454 p.","costCenters":[],"links":[{"id":182163,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wdr/1979/al-79-2/report-thumb.jpg"},{"id":409506,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/1979/al-79-2/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United 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,{"id":25890,"text":"wri806 - 1980 - The potential for developing ground-water supplies in the Pescadero area, San Mateo County, California","interactions":[],"lastModifiedDate":"2022-11-08T15:08:51.222669","indexId":"wri806","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","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":"80-6","title":"The potential for developing ground-water supplies in the Pescadero area, San Mateo County, California","docAbstract":"<p>Adequate supplies of ground water for municipal use generally are not available within a 3-mile radius of Pescadero, San Mateo County, California. The required quantity of 100 gallons per minute probably could be obtained from one or more wells in the alluvium along Pescadero Creek; however, the quality of the water probably would deteriorate with time and might not be suitable for public supply for more than 20 or 30 years. Sand and gravel beds below 60 feet in the alluvium near the junction of Honsinger and Pescadero Creeks offer the best potential for developing domestic water supplies.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wri806","usgsCitation":"Akers, J.P., 1980, The potential for developing ground-water supplies in the Pescadero area, San Mateo County, California: U.S. Geological Survey Water-Resources Investigations Report 80-6, iii, 8 p., https://doi.org/10.3133/wri806.","productDescription":"iii, 8 p.","costCenters":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true}],"links":[{"id":158544,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1980/0006/report-thumb.jpg"},{"id":365516,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1980/0006/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"California","county":"San Mateo County","otherGeospatial":"Pescadero area","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -122.4254857433479,\n              37.36201737722473\n            ],\n            [\n              -122.4254857433479,\n              37.16890736555864\n            ],\n            [\n              -122.0913656434631,\n              37.16890736555864\n            ],\n            [\n              -122.0913656434631,\n              37.36201737722473\n            ],\n            [\n              -122.4254857433479,\n              37.36201737722473\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a71e4b07f02db641d5d","contributors":{"authors":[{"text":"Akers, J. P.","contributorId":82678,"corporation":false,"usgs":true,"family":"Akers","given":"J.","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":195429,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":65675,"text":"i1262 - 1980 - Controlled photomosaic of the Thaumasia Northeast Quadrangle of Mars","interactions":[],"lastModifiedDate":"2012-02-02T00:13:14","indexId":"i1262","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","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":"1262","subseriesTitle":"NONE","title":"Controlled photomosaic of the Thaumasia Northeast Quadrangle of Mars","language":"ENGLISH","doi":"10.3133/i1262","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1980, Controlled photomosaic of the Thaumasia Northeast Quadrangle of Mars: U.S. Geological Survey IMAP 1262, 1 remote-sensing image ;53 x 60 cm., on sheet 86 x 67 cm., folded in envelope 30 x 24 cm., https://doi.org/10.3133/i1262.","productDescription":"1 remote-sensing image ;53 x 60 cm., on sheet 86 x 67 cm., folded in envelope 30 x 24 cm.","costCenters":[],"links":[{"id":189135,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":260784,"rank":900,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/1262/plate-1.pdf"}],"scale":"2000000","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae0e4b07f02db6881bb","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":534067,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":25124,"text":"cir840 - 1980 - Catalog of selected offices of the Office of Surface Mining, Bureau of Land Management, and Geological Survey relating to coal, 1981","interactions":[],"lastModifiedDate":"2012-02-02T00:08:15","indexId":"cir840","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":307,"text":"Circular","code":"CIR","onlineIssn":"2330-5703","printIssn":"1067-084X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"840","title":"Catalog of selected offices of the Office of Surface Mining, Bureau of Land Management, and Geological Survey relating to coal, 1981","language":"ENGLISH","doi":"10.3133/cir840","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1980, Catalog of selected offices of the Office of Surface Mining, Bureau of Land Management, and Geological Survey relating to coal, 1981: U.S. Geological Survey Circular 840, 41 p., https://doi.org/10.3133/cir840.","productDescription":"41 p.","costCenters":[],"links":[{"id":156886,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1980/0840/report-thumb.jpg"},{"id":54104,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1980/0840/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f3e4b07f02db5ef372","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":529179,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":27182,"text":"wri8063 - 1980 - Ground water in the Thousand Oaks area, Ventura County, California","interactions":[],"lastModifiedDate":"2019-07-10T09:57:35","indexId":"wri8063","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","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":"80-63","title":"Ground water in the Thousand Oaks area, Ventura County, California","docAbstract":"The ground-water basin beneath the city of Thousand Oaks, Calif. , corresponds closely in area with the surface-water drainage basin of Conejo Valley. Before World War II there was little ground-water development. After World War II, urban development put a stress on the ground-water basin; many wells were drilled and water levels in wells were drawn down as much as 300 feet in places. Beginning in 1963, imported water replaced domestic and municipal ground-water systems, and water levels rapidly recovered to predevelopment levels or nearly so. Most of the ground water in the Thousand Oaks area is stored in fractured basalt of the middle Miocene Conejo Volcanics. Depending on the degree of occurrence of open fractures and cavities in the basalt, recoverable ground water in the upper 300 to 500 feet of aquifer is estimated to be between 400,000 and 600,000 acre-feet. The yield of water from wells in the area ranges from 17 to 1,080 gallons per minute. Most of the ground-water in the eastern part of the valley is high insulfate and has a dissolved-solids concentration greater than 1,000 milligrams per liter. In the western part of the valley the ground-water is mostly of a bicarbonate type, and the dissolved-solids concentration is less than 800 milligrams per liter. In most areas of Conejo Valley, ground-water is a viable resource for irrigation of public lands and recreation areas. (USGS)","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wri8063","usgsCitation":"French, J.J., 1980, Ground water in the Thousand Oaks area, Ventura County, California: U.S. Geological Survey Water-Resources Investigations Report 80-63, iv, 40 p. , https://doi.org/10.3133/wri8063.","productDescription":"iv, 40 p. ","costCenters":[],"links":[{"id":157965,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1980/0063/report-thumb.jpg"},{"id":365430,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1980/0063/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"California","county":"Ventura County","otherGeospatial":"Thousand Oaks","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -118.91326904296874,\n              34.14136162745489\n            ],\n            [\n              -118.75396728515625,\n              34.14136162745489\n            ],\n            [\n              -118.75396728515625,\n              34.2004447595411\n            ],\n            [\n              -118.91326904296874,\n              34.2004447595411\n            ],\n            [\n              -118.91326904296874,\n              34.14136162745489\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ab0e4b07f02db66d749","contributors":{"authors":[{"text":"French, James J.","contributorId":103651,"corporation":false,"usgs":true,"family":"French","given":"James","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":197702,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":25615,"text":"wri8010 - 1980 - Investigation of acidity and other water-quality characteristics of Upper Oyster Creek, Ocean County, New Jersey","interactions":[],"lastModifiedDate":"2012-09-12T17:16:23","indexId":"wri8010","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","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":"80-10","title":"Investigation of acidity and other water-quality characteristics of Upper Oyster Creek, Ocean County, New Jersey","docAbstract":"Water-quality data collected in the upper Oyster Creek drainage basin, Ocean County, N.J., indicate that the stream has excellent water quality except for a persistently low pH. The mean concentrations of the major inorganic ions were all less than 6.0 milligrams per liter. Mean concentrations of total nitrogen and total phosphorus were 0.15 mg/L and 0.01 mg/L, respectively. Dissolved oxygen averaged 8.7 mg/L and 81% saturation. Low pH levels are typical of streams draining cedar swamps. In Oyster Creek, the pH tended to decrease downstream due to chemical and biological processes. The pH levels in swamps were one-half unit or more lower than the pH levels in the adjacent stream. Sharp declines in stream pH were noted during runoff periods as the result of the mixing of poorly-buffered stream water with more highly acidic water from surrounding swamp areas. The quality of ground water within the study area was similar to the quality of streamflow, except for higher iron and ammonia-nitrogen concentrations and a higher pH range of 4.9 to 6.5. Precipitation represented a major source of many chemical constituents in the ground- and surface-waters of the Oyster Creek basin. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wri8010","collaboration":"Prepared in cooperation with the State of New Jersey, Department of Environmental Protection, Division of Fish, Game, and Shell Fisheries","usgsCitation":"Fusillo, T.V., Schornick, J., Koester, H., and Harriman, D., 1980, Investigation of acidity and other water-quality characteristics of Upper Oyster Creek, Ocean County, New Jersey: U.S. Geological Survey Water-Resources Investigations Report 80-10, v, 30 p. :ill., maps; 28 cm., https://doi.org/10.3133/wri8010.","productDescription":"v, 30 p. :ill., maps; 28 cm.","numberOfPages":"35","costCenters":[{"id":470,"text":"New Jersey Water Science Center","active":true,"usgs":true}],"links":[{"id":157523,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/wri_80_10.gif"},{"id":261850,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/wri/wri80-10/","linkFileType":{"id":5,"text":"html"}},{"id":261851,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/wri80-10/pdf/wrir80-10.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"New Jersey","county":"Ocean County","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e486ce4b07f02db50b66c","contributors":{"authors":[{"text":"Fusillo, Thomas V.","contributorId":106097,"corporation":false,"usgs":true,"family":"Fusillo","given":"Thomas","email":"","middleInitial":"V.","affiliations":[],"preferred":false,"id":194420,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Schornick, J.C. Jr.","contributorId":49003,"corporation":false,"usgs":true,"family":"Schornick","given":"J.C.","suffix":"Jr.","affiliations":[],"preferred":false,"id":194419,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Koester, H.E.","contributorId":26323,"corporation":false,"usgs":true,"family":"Koester","given":"H.E.","email":"","affiliations":[],"preferred":false,"id":194417,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Harriman, D.A.","contributorId":27860,"corporation":false,"usgs":true,"family":"Harriman","given":"D.A.","email":"","affiliations":[],"preferred":false,"id":194418,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":67647,"text":"l108 - 1980 - Land use and land cover, 1976-77, Winston-Salem, North Carolina; Tennessee, Virginia","interactions":[],"lastModifiedDate":"2012-02-10T00:11:30","indexId":"l108","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","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":"108","title":"Land use and land cover, 1976-77, Winston-Salem, North Carolina; Tennessee, Virginia","language":"ENGLISH","doi":"10.3133/l108","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1980, Land use and land cover, 1976-77, Winston-Salem, North Carolina; Tennessee, Virginia: U.S. Geological Survey Land Use and Land Cover 108, -, https://doi.org/10.3133/l108.","productDescription":"-","costCenters":[],"links":[{"id":186538,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":260952,"rank":900,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/l/108/plate-1.pdf"}],"scale":"250000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -82,36 ], [ -82,37 ], [ -80,37 ], [ -80,36 ], [ -82,36 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b23e4b07f02db6ae062","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":534393,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":67637,"text":"l183 - 1980 - Land use and land cover, 1974, Dickinson, North Dakota","interactions":[],"lastModifiedDate":"2012-02-10T00:11:29","indexId":"l183","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","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":"183","title":"Land use and land cover, 1974, Dickinson, North Dakota","language":"ENGLISH","doi":"10.3133/l183","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1980, Land use and land cover, 1974, Dickinson, North Dakota: U.S. Geological Survey Land Use and Land Cover 183, -, https://doi.org/10.3133/l183.","productDescription":"-","costCenters":[],"links":[{"id":186473,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":260942,"rank":900,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/l/183/plate-1.pdf"}],"scale":"250000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -104,46 ], [ -104,47 ], [ -102,47 ], [ -102,46 ], [ -104,46 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b24e4b07f02db6ae43d","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":534383,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":41532,"text":"ofr80831 - 1980 - Aeroradioactivity map of the Manistique Lakes area, Michigan","interactions":[],"lastModifiedDate":"2012-02-02T00:10:32","indexId":"ofr80831","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","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":"80-831","title":"Aeroradioactivity map of the Manistique Lakes area, Michigan","language":"ENGLISH","doi":"10.3133/ofr80831","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1980, Aeroradioactivity map of the Manistique Lakes area, Michigan: U.S. Geological Survey Open-File Report 80-831, 1 map ;178 x 153 cm. on 4 sheets., https://doi.org/10.3133/ofr80831.","productDescription":"1 map ;178 x 153 cm. on 4 sheets.","costCenters":[],"links":[{"id":173117,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":20036,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/0831/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":20037,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/0831/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":20034,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/0831/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":20035,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/0831/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae4e4b07f02db689a6e","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":530458,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":67691,"text":"l98 - 1980 - Land use and land cover, 1969-76, Quincy, Illinois; Missouri","interactions":[],"lastModifiedDate":"2012-02-10T00:11:26","indexId":"l98","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","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":"98","title":"Land use and land cover, 1969-76, Quincy, Illinois; Missouri","language":"ENGLISH","doi":"10.3133/l98","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1980, Land use and land cover, 1969-76, Quincy, Illinois; Missouri: U.S. Geological Survey Land Use and Land Cover 98, -, https://doi.org/10.3133/l98.","productDescription":"-","costCenters":[],"links":[{"id":185875,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":260998,"rank":900,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/l/098/plate-1.pdf"}],"scale":"250000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -92,39 ], [ -92,40 ], [ -90,40 ], [ -90,39 ], [ -92,39 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b24e4b07f02db6aeafb","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":534437,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":30445,"text":"wri808 - 1980 - Analysis of stream quality in the Yampa River Basin, Colorado and Wyoming","interactions":[],"lastModifiedDate":"2012-02-02T00:09:03","indexId":"wri808","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","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":"80-8","title":"Analysis of stream quality in the Yampa River Basin, Colorado and Wyoming","docAbstract":"Historic data show no significant water-temperature changes since 1951 for the Little Snake or Yampa Rivers, the two major streams of the Yampa River basin in Colorado and Wyoming. Regional analyses indicate that harmonic-mean temperature is negatively correlated with altitude. No change in specific conductance since 1951 was noted for the Little Snake River; however, specific conductance in the Yampa River has increaed 14 % since that time and is attributed to increased agricultural and municipal use of water. Site-specific relationships between major inorganic constituents and specific conductance for the Little Snake and Yampa Rivers were similar to regional relationships developed from both historic and recent (1975) data. These relationships provide a means for estimating concentrations of major inorganic constituents from specific conductance, which is easily measured. Trace-element and nutrient data collected from August 1975 through September 1976 at 92 sites in the Yampa River basin indicate that water-quality degradation occurred upstream from 3 sites. The degradation resulted from underground drainage from pyritic materials that probably are associated with coal at one site, discharge from powerplant cooling-tower blowdown water at a second site, and runoff from a small watershed containing a gas field at the third site. Ambient concentrations of dissolved and total iron and manganese frequently exceeded proposed Colorado water-quality standards. The concentrations of many dissolved and total trace elements and nutrients were greatest during March 1976. These were associated with larger suspended-sediment concentrations and smaller pH values than at other times of the year. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey, Water Resources Division,","doi":"10.3133/wri808","usgsCitation":"Wentz, D.A., and Steele, T.D., 1980, Analysis of stream quality in the Yampa River Basin, Colorado and Wyoming: U.S. Geological Survey Water-Resources Investigations Report 80-8, viii, 161 p. :ill., maps ;26 cm., https://doi.org/10.3133/wri808.","productDescription":"viii, 161 p. :ill., maps ;26 cm.","costCenters":[],"links":[{"id":124098,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1980/0008/report-thumb.jpg"},{"id":59228,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1980/0008/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4acfe4b07f02db6801c9","contributors":{"authors":[{"text":"Wentz, Dennis A. dawentz@usgs.gov","contributorId":1838,"corporation":false,"usgs":true,"family":"Wentz","given":"Dennis","email":"dawentz@usgs.gov","middleInitial":"A.","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":203266,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Steele, Timothy Doak","contributorId":88723,"corporation":false,"usgs":true,"family":"Steele","given":"Timothy","email":"","middleInitial":"Doak","affiliations":[],"preferred":false,"id":203267,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":41641,"text":"ofr80812 - 1980 - Aeroradioactivity map of Fairfax County, Virginia","interactions":[],"lastModifiedDate":"2012-02-02T00:10:51","indexId":"ofr80812","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","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":"80-812","title":"Aeroradioactivity map of Fairfax County, Virginia","language":"ENGLISH","doi":"10.3133/ofr80812","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1980, Aeroradioactivity map of Fairfax County, Virginia: U.S. Geological Survey Open-File Report 80-812, 1 map ;102 x 98 cm., https://doi.org/10.3133/ofr80812.","productDescription":"1 map ;102 x 98 cm.","costCenters":[],"links":[{"id":170712,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":20027,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/0812/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":20028,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/0812/plate-1-preview.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae4e4b07f02db689b75","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":530535,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":42878,"text":"ofr80757 - 1980 - Preliminary potentiometric-surface map showing fresh-water heads for the Lower Cretaceous rocks in the northern Great Plains of Montana, North Dakota, South Dakota, and Wyoming","interactions":[],"lastModifiedDate":"2012-02-02T00:11:06","indexId":"ofr80757","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","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":"80-757","title":"Preliminary potentiometric-surface map showing fresh-water heads for the Lower Cretaceous rocks in the northern Great Plains of Montana, North Dakota, South Dakota, and Wyoming","language":"ENGLISH","doi":"10.3133/ofr80757","usgsCitation":"Lobmeyer, D.H., 1980, Preliminary potentiometric-surface map showing fresh-water heads for the Lower Cretaceous rocks in the northern Great Plains of Montana, North Dakota, South Dakota, and Wyoming: U.S. Geological Survey Open-File Report 80-757, 1 map ;90 x 145 cm., https://doi.org/10.3133/ofr80757.","productDescription":"1 map ;90 x 145 cm.","costCenters":[],"links":[{"id":169154,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":20021,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/0757/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":20022,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/0757/plate-1-preview.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aafe4b07f02db66cc9f","contributors":{"authors":[{"text":"Lobmeyer, David H.","contributorId":85156,"corporation":false,"usgs":true,"family":"Lobmeyer","given":"David","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":227315,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
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