{"pageNumber":"2060","pageRowStart":"51475","pageSize":"25","recordCount":68919,"records":[{"id":8448,"text":"ofr84450 - 1984 - Geohydrologic data for test well UE-25p1, Yucca Mountain area, Nye County, Nevada","interactions":[],"lastModifiedDate":"2012-02-02T00:06:05","indexId":"ofr84450","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"84-450","title":"Geohydrologic data for test well UE-25p1, Yucca Mountain area, Nye County, Nevada","docAbstract":"This report presents the following data for test well UE-25p 1 in Nye County, Nevada: drilling operations, lithology, availability of borehole geophysical logs, water levels, future availability of core analyses, water chemistry, pumping tests, borehole-flow surveys, and packer-injection tests. The well is one of a series of test wells drilled in and near Yucca Mountain adjacent to the Nevada Test Site in cooperation with the U.S. Department of Energy. These investigations are part of the Nevada Nuclear Waste Storage Investigations to identify suitable sites for underground storage of high-level radioactive wastes. Test well UE-25p 1 was the first in the Yucca Mountain area to penetrate rocks of Paleozoic age. To a depth of 1,244 meters, the rocks are predominantly ash-flow tuffs of Tertiary age. From 1,244 meters to a total depth of 1,805 meters, the rock is dolomite of Paleozoic age. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr84450","usgsCitation":"Craig, R.W., and Johnson, K., 1984, Geohydrologic data for test well UE-25p1, Yucca Mountain area, Nye County, Nevada: U.S. Geological Survey Open-File Report 84-450, vi, 70 p. :ill., map ;28 cm., https://doi.org/10.3133/ofr84450.","productDescription":"vi, 70 p. :ill., map ;28 cm.","costCenters":[],"links":[{"id":140524,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1984/0450/report-thumb.jpg"},{"id":36021,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1984/0450/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1be4b07f02db6a8f12","contributors":{"authors":[{"text":"Craig, R. W.","contributorId":40984,"corporation":false,"usgs":true,"family":"Craig","given":"R.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":157732,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Johnson, K. A.","contributorId":46518,"corporation":false,"usgs":true,"family":"Johnson","given":"K. A.","affiliations":[],"preferred":false,"id":157733,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":18698,"text":"ofr84422 - 1984 - Survey of helium in natural water wells and springs in Southwest Montana and Imperial Valley, California; Part VI, Jan. 1 - Dec. 31, 1983","interactions":[],"lastModifiedDate":"2012-02-02T00:07:30","indexId":"ofr84422","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"84-422","title":"Survey of helium in natural water wells and springs in Southwest Montana and Imperial Valley, California; Part VI, Jan. 1 - Dec. 31, 1983","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr84422","usgsCitation":"Doering, W.P., and Friedman, I., 1984, Survey of helium in natural water wells and springs in Southwest Montana and Imperial Valley, California; Part VI, Jan. 1 - Dec. 31, 1983: U.S. Geological Survey Open-File Report 84-422, 30 p. :ill. ;28 cm., https://doi.org/10.3133/ofr84422.","productDescription":"30 p. :ill. ;28 cm.","costCenters":[],"links":[{"id":152023,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1984/0422/report-thumb.jpg"},{"id":48055,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1984/0422/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae1e4b07f02db688787","contributors":{"authors":[{"text":"Doering, W. P.","contributorId":7270,"corporation":false,"usgs":true,"family":"Doering","given":"W.","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":179579,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Friedman, Irving","contributorId":90664,"corporation":false,"usgs":true,"family":"Friedman","given":"Irving","email":"","affiliations":[],"preferred":false,"id":179580,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":30053,"text":"wri834174 - 1984 - A water-quality study of the Russian River basin during the low-flow seasons, 1973-78, Sonoma and Mendocino Counties, California","interactions":[],"lastModifiedDate":"2022-01-21T19:40:32.854093","indexId":"wri834174","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"83-4174","title":"A water-quality study of the Russian River basin during the low-flow seasons, 1973-78, Sonoma and Mendocino Counties, California","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri834174","usgsCitation":"Sylvester, M.A., and Church, R.L., 1984, A water-quality study of the Russian River basin during the low-flow seasons, 1973-78, Sonoma and Mendocino Counties, California: U.S. Geological Survey Water-Resources Investigations Report 83-4174, vii, 106 p., https://doi.org/10.3133/wri834174.","productDescription":"vii, 106 p.","costCenters":[],"links":[{"id":394682,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_35824.htm"},{"id":58863,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1983/4174/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":122184,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1983/4174/report-thumb.jpg"}],"country":"United States","state":"California","county":"Mendocino County, Sonoma County","otherGeospatial":"Russian River basin","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -123.417,\n              38.333\n            ],\n            [\n              -122.667,\n              38.333\n            ],\n            [\n              -122.667,\n              39.417\n            ],\n            [\n              -123.417,\n              39.417\n            ],\n            [\n              -123.417,\n              38.333\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b15e4b07f02db6a4d7d","contributors":{"authors":[{"text":"Sylvester, M. A.","contributorId":10838,"corporation":false,"usgs":true,"family":"Sylvester","given":"M.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":202599,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Church, R. L.","contributorId":61078,"corporation":false,"usgs":true,"family":"Church","given":"R.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":202600,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":30306,"text":"wri844263 - 1984 - AQUIFEM-SALT; a finite-element model for aquifers containing a seawater interface","interactions":[],"lastModifiedDate":"2012-02-02T00:09:02","indexId":"wri844263","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","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":"84-4263","title":"AQUIFEM-SALT; a finite-element model for aquifers containing a seawater interface","docAbstract":"Described are modifications to AQUIFEM, a finite element areal ground-water flow model for aquifer evaluation. The modified model, AQUIFEM-SALT, simulates an aquifer containing a freshwater body that freely floats on seawater. Parts of the freshwater lens may be confined above and below by less permeable units. Theory, code modifications, and model verification are discussed. A modified input data list is included. This report is intended as a companion to the original AQUIFEM documentation. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri844263","usgsCitation":"Voss, C., 1984, AQUIFEM-SALT; a finite-element model for aquifers containing a seawater interface: U.S. Geological Survey Water-Resources Investigations Report 84-4263, iv, 37 p. :ill. ;28 cm., https://doi.org/10.3133/wri844263.","productDescription":"iv, 37 p. :ill. ;28 cm.","costCenters":[],"links":[{"id":119473,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1984/4263/report-thumb.jpg"},{"id":59099,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1984/4263/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b15e4b07f02db6a4969","contributors":{"authors":[{"text":"Voss, C.I.","contributorId":79515,"corporation":false,"usgs":true,"family":"Voss","given":"C.I.","email":"","affiliations":[],"preferred":false,"id":203027,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":65873,"text":"i1646 - 1984 - Shaded relief map of the Casius Quadrangle of Mars","interactions":[],"lastModifiedDate":"2012-02-02T00:13:08","indexId":"i1646","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","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":"1646","subseriesTitle":"NONE","title":"Shaded relief map of the Casius Quadrangle of Mars","language":"ENGLISH","doi":"10.3133/i1646","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1984, Shaded relief map of the Casius Quadrangle of Mars: U.S. Geological Survey IMAP 1646, 1 remote-sensing image :col. ;46 x 69 cm., on sheet 76 x 78 cm., folded in envelope 30 x 24 cm., https://doi.org/10.3133/i1646.","productDescription":"1 remote-sensing image :col. ;46 x 69 cm., on sheet 76 x 78 cm., folded in envelope 30 x 24 cm.","costCenters":[],"links":[{"id":189803,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":260822,"rank":900,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/1646/plate-1.pdf"}],"scale":"5000000","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49fbe4b07f02db5f480b","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":534227,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":29973,"text":"wri834223 - 1984 - Estimate of self-supplied domestic water use in Oklahoma during 1980","interactions":[],"lastModifiedDate":"2012-02-02T00:08:59","indexId":"wri834223","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"83-4223","title":"Estimate of self-supplied domestic water use in Oklahoma during 1980","docAbstract":"Reported or measured water-use data for the domestic self-supplied user were not available for Oklahoma; therefore estimates of water use within this classification were derived. The total self-supplied population in Oklahoma during 1980 was estimated to be 343,615, which was 11.4 percent of the total 1980 State population. The rate of water use by this group was estimated to be 56 gallons per capita per day. The estimated annual domestic self-supplied water use by county ranged from 10 to 1,180 acre-feet, with a total statewide use of 21,610 acre-feet.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri834223","usgsCitation":"Stoner, J., 1984, Estimate of self-supplied domestic water use in Oklahoma during 1980: U.S. Geological Survey Water-Resources Investigations Report 83-4223, iii, 20 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri834223.","productDescription":"iii, 20 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":122749,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1983/4223/report-thumb.jpg"},{"id":58785,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1983/4223/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ee4b07f02db5fdd9c","contributors":{"authors":[{"text":"Stoner, J.D.","contributorId":58261,"corporation":false,"usgs":true,"family":"Stoner","given":"J.D.","email":"","affiliations":[],"preferred":false,"id":202463,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":65677,"text":"i1600 - 1984 - Controlled photomosaic of the Thaumasia Southeast Quadrangle of Mars M 2M -56/75 CM, MC-25 SE","interactions":[],"lastModifiedDate":"2012-02-02T00:13:14","indexId":"i1600","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","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":"1600","subseriesTitle":"NONE","title":"Controlled photomosaic of the Thaumasia Southeast Quadrangle of Mars M 2M -56/75 CM, MC-25 SE","language":"ENGLISH","doi":"10.3133/i1600","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1984, Controlled photomosaic of the Thaumasia Southeast Quadrangle of Mars M 2M -56/75 CM, MC-25 SE: U.S. Geological Survey IMAP 1600, 1 remote-sensing image ;52 x 59 cm., on sheet 86 x 67 cm., folded in envelope 30 x 24 cm., https://doi.org/10.3133/i1600.","productDescription":"1 remote-sensing image ;52 x 59 cm., on sheet 86 x 67 cm., folded in envelope 30 x 24 cm.","costCenters":[],"links":[{"id":251393,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/imap/1600/report.pdf","size":"28","linkFileType":{"id":1,"text":"pdf"}},{"id":251394,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/1600/plate-1.pdf","size":"9174","linkFileType":{"id":1,"text":"pdf"}},{"id":252251,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/imap/1600/report-thumb.jpg"}],"scale":"2000000","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adce4b07f02db686673","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":534069,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":29639,"text":"wri844118 - 1984 - Hydrology of the Tertiary-Cretaceous aquifer system in the vicinity of Fort Rucker Aviation Center, Alabama","interactions":[],"lastModifiedDate":"2012-02-02T00:08:56","indexId":"wri844118","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","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":"84-4118","title":"Hydrology of the Tertiary-Cretaceous aquifer system in the vicinity of Fort Rucker Aviation Center, Alabama","docAbstract":"Fort Rucker Aviation Center, built in 1941-42, uses ground water for its water supply. The demand for water began to exceed the capacity of the well field in 1976. The Tertiary-Cretaceous aquifer system in the Fort Rucker area consists of an upper and lower aquifer. The upper aquifer consists of the basal part of the Tuscahoma Sand, the Nanafalia and Clayton Formations, and the upper part of the Providence Sand. The lower aquifer consists of the lower part of the Providence Sand and the Ripley Formation. Most large capacity (greater than 100 gal/min (gallons per minute)) wells in the Fort Rucker area are developed in one of these aquifers, and produce 500 gal/min or more. An aquifer test made at Fort Rucker during the study indicates that the transmissivity of the upper aquifer is about 7,000 ft sq/d (feet squared per day). This test and a potentiometric map of the area indicate that wells spaced too closely together is a major problem at pumping centers in the study area. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri844118","usgsCitation":"Scott, J.C., Law, L., and Cobb, R., 1984, Hydrology of the Tertiary-Cretaceous aquifer system in the vicinity of Fort Rucker Aviation Center, Alabama: U.S. Geological Survey Water-Resources Investigations Report 84-4118, v, 221 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri844118.","productDescription":"v, 221 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":122685,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1984/4118/report-thumb.jpg"},{"id":58462,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1984/4118/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ee4b07f02db5fdb2b","contributors":{"authors":[{"text":"Scott, J. C.","contributorId":75901,"corporation":false,"usgs":true,"family":"Scott","given":"J.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":201863,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Law, L.R.","contributorId":71596,"corporation":false,"usgs":true,"family":"Law","given":"L.R.","email":"","affiliations":[],"preferred":false,"id":201862,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Cobb, Riley","contributorId":107325,"corporation":false,"usgs":true,"family":"Cobb","given":"Riley","email":"","affiliations":[],"preferred":false,"id":201864,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":43272,"text":"ofr8434 - 1984 - Land use and land cover and associated maps for Midland, Michigan","interactions":[],"lastModifiedDate":"2012-02-02T00:10:26","indexId":"ofr8434","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"84-34","title":"Land use and land cover and associated maps for Midland, Michigan","language":"ENGLISH","doi":"10.3133/ofr8434","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1984, Land use and land cover and associated maps for Midland, Michigan: U.S. Geological Survey Open-File Report 84-34, maps :photocopy ;45 x 73 cm., https://doi.org/10.3133/ofr8434.","productDescription":"maps :photocopy ;45 x 73 cm.","costCenters":[],"links":[{"id":172418,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b27e4b07f02db6b0d2c","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":531080,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":65674,"text":"i1602 - 1984 - Controlled photomosaic of the Thaumasia northeast Quadrangle of Mars","interactions":[],"lastModifiedDate":"2012-02-02T00:13:14","indexId":"i1602","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","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":"1602","subseriesTitle":"NONE","title":"Controlled photomosaic of the Thaumasia northeast Quadrangle of Mars","language":"ENGLISH","doi":"10.3133/i1602","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1984, Controlled photomosaic of the Thaumasia northeast Quadrangle of Mars (Rev. in June 1983.): U.S. Geological Survey IMAP 1602, 1 photomosaic ;53 x 59 cm., on sheet 86 x 66 cm. folded in envelope 30 x 24 cm., https://doi.org/10.3133/i1602.","productDescription":"1 photomosaic ;53 x 59 cm., on sheet 86 x 66 cm. folded in envelope 30 x 24 cm.","costCenters":[],"links":[{"id":251391,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/imap/1602/report.pdf","size":"25","linkFileType":{"id":1,"text":"pdf"}},{"id":251392,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/1602/plate-1.pdf","size":"10022","linkFileType":{"id":1,"text":"pdf"}},{"id":252250,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/imap/1602/report-thumb.jpg"}],"scale":"2000000","edition":"Rev. in June 1983.","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adce4b07f02db68667e","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":534066,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":12492,"text":"ofr84803 - 1984 - Water-Level Measurements for the Coastal Plain Aquifers of South Carolina Prior to Development","interactions":[],"lastModifiedDate":"2016-12-14T13:56:15","indexId":"ofr84803","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"84-803","title":"Water-Level Measurements for the Coastal Plain Aquifers of South Carolina Prior to Development","docAbstract":"Tabulations of water-level measurements for the Coastal Plain aquifers of \r\nSouth Carolina representing water levels prior to man-made development are \r\npresented. Included with the tabulations are local well number, location, \r\nland-surface altitude, well depth, screened interval, depth to water, water- \r\nlevel altitude, and date measured. These water-level measurements were used \r\nin compiling regional potentiometric maps for the Coastal Plain aquifers. \r\nThis data set will be useful in the planning for future water-resource \r\ndevelopment.","language":"ENGLISH","publisher":"Geological Survey (U.S.)","doi":"10.3133/ofr84803","usgsCitation":"Aucott, W.R., and Speiran, G.K., 1984, Water-Level Measurements for the Coastal Plain Aquifers of South Carolina Prior to Development: U.S. Geological Survey Open-File Report 84-803, 42 p. **PUBLICATION PAGES ARE IN INCORRECT ORDER**, https://doi.org/10.3133/ofr84803.","productDescription":"42 p. **PUBLICATION PAGES ARE IN INCORRECT ORDER**","costCenters":[{"id":13634,"text":"South Atlantic Water Science 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,{"id":41773,"text":"ofr84648 - 1984 - Aeromagnetic map of part of the Springfield 1 degree x 2 degree Quadrangle, Missouri","interactions":[],"lastModifiedDate":"2012-02-02T00:10:27","indexId":"ofr84648","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"84-648","title":"Aeromagnetic map of part of the Springfield 1 degree x 2 degree Quadrangle, Missouri","language":"ENGLISH","doi":"10.3133/ofr84648","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1984, Aeromagnetic map of part of the Springfield 1 degree x 2 degree Quadrangle, Missouri: U.S. Geological Survey Open-File Report 84-648, 1 map :photocopy ;49 x 75 cm., https://doi.org/10.3133/ofr84648.","productDescription":"1 map :photocopy ;49 x 75 cm.","costCenters":[],"links":[{"id":173087,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":79483,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1984/0648/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afee4b07f02db6978c1","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":530610,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":55733,"text":"wdrNJ832 - 1984 - Water-resources data for New Jersey, water year 1983, Volume 2. Delaware River Basin and tributaries to Delaware Bay","interactions":[],"lastModifiedDate":"2019-11-07T14:02:45","indexId":"wdrNJ832","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","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":"NJ-83-2","title":"Water-resources data for New Jersey, water year 1983, Volume 2. Delaware River Basin and tributaries to Delaware Bay","docAbstract":"<p>No abstract available.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wdrNJ832","usgsCitation":"Bauersfeld, W., Moshinsky, E., Pustay, E., and Schaefer, F., 1984, Water-resources data for New Jersey, water year 1983, Volume 2. Delaware River Basin and tributaries to Delaware Bay: U.S. Geological Survey Water Data Report NJ-83-2, vii, 195 p., https://doi.org/10.3133/wdrNJ832.","productDescription":"vii, 195 p.","costCenters":[],"links":[{"id":369054,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/1983/nj-83-2/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":174342,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wdr/1983/nj-83-2/report-thumb.jpg"}],"country":"United States","state":"New Jersey","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -75.3497314453125,\n              38.91668153637508\n            ],\n            [\n              -73.9874267578125,\n              38.91668153637508\n            ],\n            [\n              -73.9874267578125,\n              40.534676780615406\n            ],\n            [\n              -75.3497314453125,\n              40.534676780615406\n            ],\n            [\n              -75.3497314453125,\n              38.91668153637508\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e2e4b07f02db5e4ee4","contributors":{"authors":[{"text":"Bauersfeld, W.R.","contributorId":72451,"corporation":false,"usgs":true,"family":"Bauersfeld","given":"W.R.","email":"","affiliations":[],"preferred":false,"id":254160,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Moshinsky, E.W.","contributorId":104972,"corporation":false,"usgs":true,"family":"Moshinsky","given":"E.W.","email":"","affiliations":[],"preferred":false,"id":254162,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Pustay, E.A.","contributorId":62604,"corporation":false,"usgs":true,"family":"Pustay","given":"E.A.","affiliations":[],"preferred":false,"id":254159,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Schaefer, F. L.","contributorId":91085,"corporation":false,"usgs":true,"family":"Schaefer","given":"F. L.","affiliations":[],"preferred":false,"id":254161,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":13157,"text":"ofr84829 - 1984 - Platform margin and deep water carbonates","interactions":[],"lastModifiedDate":"2012-02-02T00:06:48","indexId":"ofr84829","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"84-829","title":"Platform margin and deep water carbonates","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr84829","usgsCitation":"Cook, H.E., 1984, Platform margin and deep water carbonates: U.S. Geological Survey Open-File Report 84-829, 248 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr84829.","productDescription":"248 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":146086,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1984/0829/report-thumb.jpg"},{"id":41558,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1984/0829/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad9e4b07f02db684f7e","contributors":{"authors":[{"text":"Cook, H. E.","contributorId":18782,"corporation":false,"usgs":true,"family":"Cook","given":"H.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":167325,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":43242,"text":"ofr84531 - 1984 - Land use and land cover and associated maps for Caliente, Nevada","interactions":[],"lastModifiedDate":"2012-02-02T00:10:26","indexId":"ofr84531","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"84-531","title":"Land use and land cover and associated maps for Caliente, Nevada","language":"ENGLISH","doi":"10.3133/ofr84531","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1984, Land use and land cover and associated maps for Caliente, Nevada: U.S. Geological Survey Open-File Report 84-531, 5 maps :photocopy ;45 x 71 cm., on sheets 77 x 107 cm., https://doi.org/10.3133/ofr84531.","productDescription":"5 maps :photocopy ;45 x 71 cm., on sheets 77 x 107 cm.","costCenters":[],"links":[{"id":173538,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b28e4b07f02db6b1712","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":531061,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":29656,"text":"wri834272 - 1984 - Reconnaissance of the shallow-unconfined aquifer in Salt Lake Valley, Utah","interactions":[],"lastModifiedDate":"2012-02-02T00:08:56","indexId":"wri834272","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"83-4272","title":"Reconnaissance of the shallow-unconfined aquifer in Salt Lake Valley, Utah","docAbstract":"The shallow-unconfined aquifer in Salt Lake (Jordan) Valley, Utah, seldom is used for domestic or industrial purposes because it yields water slowly and is readily contaminated. The water in the aquifer, however, can flood basements and is a potential source of contamination to other water supplies. In about one-half of the valley, water in the shallow-unconfined aquifer is less than 10 feet below land surface. The general direction of flow in the shallow aquifer is toward the Jordan River. Water levels in the north part of the valley and along the Jordan River are highest in March or April and in the south part of the valley are highest in late summer. The smallest concentrations of dissolved solids in water from wells along the east side of the valley, and the greatest concentrations are in the northwest part of the valley near the Great Salt Lake. Large dissolved-solids concentrations are found near some landfills and tailings areas. Nitrate-nitrogen concentrations ranged from less than 0.1 to 86 milligrams per liter and nitrate-nitrogen concentrations from less than 0.02 to 0.85 milligram per liter. Some of the largest nitrate-nitrogen concentrations were found in water wells near animal pens. The greatest concentrations of trace elements generally came from wells near landfills and tailings area. The greatest measured concentration of cadmium was 200 microgram per liter, of mercury 0.1 microgram per liter, of lead 46 micrograms per liter, of iron 37,000 micrograms per liter and of arsenic 360 micrograms per liter. Synthetic organic chemicals were found in water from several wells. The greatest measured concentration of benzene was 400 micrograms per liter, of phenol 660 micrograms per liter, of 1,1 dichloroethane 20 micrograms per liter, of tichloroethylene 8 micrograms per liter , and of chloroethylene, 11 micrograms per liter. The greatest concentrations were in water from wells near landfills. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri834272","usgsCitation":"Seiler, R.L., and Waddell, K., 1984, Reconnaissance of the shallow-unconfined aquifer in Salt Lake Valley, Utah: U.S. Geological Survey Water-Resources Investigations Report 83-4272, 37 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri834272.","productDescription":"37 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":159831,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1983/4272/report-thumb.jpg"},{"id":58476,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1983/4272/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":58477,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1983/4272/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":58478,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1983/4272/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":58479,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1983/4272/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e48cfe4b07f02db546080","contributors":{"authors":[{"text":"Seiler, R. L.","contributorId":87546,"corporation":false,"usgs":true,"family":"Seiler","given":"R.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":201906,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Waddell, K.M.","contributorId":59009,"corporation":false,"usgs":true,"family":"Waddell","given":"K.M.","email":"","affiliations":[],"preferred":false,"id":201905,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":65864,"text":"i1511 - 1984 - Shaded relief map of the Lunae Palus Quadrangle of Mars","interactions":[],"lastModifiedDate":"2012-02-02T00:13:08","indexId":"i1511","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","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":"1511","subseriesTitle":"NONE","title":"Shaded relief map of the Lunae Palus Quadrangle of Mars","language":"ENGLISH","doi":"10.3133/i1511","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1984, Shaded relief map of the Lunae Palus Quadrangle of Mars: U.S. Geological Survey IMAP 1511, 1 remote sensing image :col. ;37 x 53 cm., on sheet 86 x 67 cm., folded in envelope 30 x 24 cm., https://doi.org/10.3133/i1511.","productDescription":"1 remote sensing image :col. ;37 x 53 cm., on sheet 86 x 67 cm., folded in envelope 30 x 24 cm.","costCenters":[],"links":[{"id":189701,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":260815,"rank":900,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/1511/plate-1.pdf"}],"scale":"5000000","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49fbe4b07f02db5f463f","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":534218,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":65879,"text":"i1475 - 1984 - Shaded relief map of the Cebrenia Quadrangle of Mars","interactions":[],"lastModifiedDate":"2012-02-02T00:13:18","indexId":"i1475","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","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":"1475","subseriesTitle":"NONE","title":"Shaded relief map of the Cebrenia Quadrangle of Mars","language":"ENGLISH","doi":"10.3133/i1475","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1984, Shaded relief map of the Cebrenia Quadrangle of Mars: U.S. Geological Survey IMAP 1475, 1 photomosaic :col. ;49 x 69 cm., on sheet 86 x 79 cm., folded in envelope 30 x 24 cm., https://doi.org/10.3133/i1475.","productDescription":"1 photomosaic :col. ;49 x 69 cm., on sheet 86 x 79 cm., folded in envelope 30 x 24 cm.","costCenters":[],"links":[{"id":190280,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":260827,"rank":900,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/1475/plate-1.pdf"}],"scale":"5000000","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49fbe4b07f02db5f4789","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":534233,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":29690,"text":"wri834271 - 1984 - Shallow ground-water flow and drainage characteristics of the Brown ditch basin near the East Unit, Indiana Dunes National Lakeshore, Indiana, 1982","interactions":[],"lastModifiedDate":"2012-02-02T00:08:57","indexId":"wri834271","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"83-4271","title":"Shallow ground-water flow and drainage characteristics of the Brown ditch basin near the East Unit, Indiana Dunes National Lakeshore, Indiana, 1982","docAbstract":"Brown ditch drains wetlands between three parallel ridges of sand dunes near the East Unit of Indiana Dunes National Lakeshore in Poter County, Indiana. Dune and lacustrine sands form a surficial aquifer that is the source of base flow to the ditch. Profiles established in July and August 1982 show that the average streambed slope of the ditch in the Lakeshore (0.19 percent) is six times that of the upstream east reach in the adjacent town, The Pines (0.03 percent). Although the ditch contains debris and vegetation, the reach in the Lakeshore seems to convey all the base flow it receives. In contrast, the upstream east arm contains several ponded sections where flow is sluggish. Digital model simulations show that dredging to form a uniformly graded streambed and eliminate ponding in the upstream east arm of the ditch south of The Pines could lower the water table 0.2 to 2.0 feet in The Pines. Lowering the ditch stage in the Lakeshore by 0.5 to 1.0 foot would cause additional water-table decline of less than 0.5 foot in The Pines. Lowering the ditch stage both in the Lakeshore and in The Pines could lower the water-table in the Lakeshore by nearly 1.0 foot. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri834271","usgsCitation":"Shedlock, R.J., and Harkness, W.E., 1984, Shallow ground-water flow and drainage characteristics of the Brown ditch basin near the East Unit, Indiana Dunes National Lakeshore, Indiana, 1982: U.S. Geological Survey Water-Resources Investigations Report 83-4271, iv, 37 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri834271.","productDescription":"iv, 37 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":159674,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1983/4271/report-thumb.jpg"},{"id":58514,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1983/4271/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49d6e4b07f02db5de58c","contributors":{"authors":[{"text":"Shedlock, R. J.","contributorId":91510,"corporation":false,"usgs":true,"family":"Shedlock","given":"R.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":201957,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Harkness, W. E.","contributorId":19176,"corporation":false,"usgs":true,"family":"Harkness","given":"W.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":201956,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":8094,"text":"ofr8465 - 1984 - Floods in south-central Oklahoma and north-central Texas, October 1981","interactions":[],"lastModifiedDate":"2017-06-14T14:30:00","indexId":"ofr8465","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"84-65","title":"Floods in south-central Oklahoma and north-central Texas, October 1981","docAbstract":"<p>Heavy rains fell over south-central Oklahoma and north-central Texas during October 11-14, 1981, causing record flooding in both States. Six lives were lost, many people were temporarily left homeless, and damages amounted to nearly $115 million. The maximum rainfall of 23 inches occurred 5 miles north of Clyde, Texas, in about 34 hours.</p>\n<p>Flood discharges along the East Fork Little Wichita River in Texas and along the Blue River, Clear Boggy Creek, and part of Muddy Boggy Creek in Oklahoma in the Red River basin exceeded those previously known. The Red River near Gainesville, Texas, had a record stage. Severe flooding also occurred along the West Fork and Elm Fork Trinity Rivers in Texas. The Brazos River experienced record flooding along tributaries in Abilene and Breckenridge, Texas, and the Brazos River near Glen Rose had a record stage that was almost 1.5 feet higher than any previous flood.</p>\n<p>Substantial reductions in peak stages and discharges on the West Fork Trinity River downstream from Eagle Mountain Reservoir were attained as a result of reservoir storage. All floodwater on the Elm Fork Trinity River was contained by reservoir storage thus preventing a potentially devastating flood downstream on the Trinity River. Maximum stages and discharges and/or contents were recorded during and after this major flood at 83 gaging stations, crest-stage stations, reservoir stations, and a miscellaneous site.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr8465","usgsCitation":"Buckner, H.D., and Kurklin, J.K., 1984, Floods in south-central Oklahoma and north-central Texas, October 1981: U.S. Geological Survey Open-File Report 84-65, v, 112 p., https://doi.org/10.3133/ofr8465.","productDescription":"v, 112 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":141339,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1984/0065/report-thumb.jpg"},{"id":35693,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1984/0065/report.pdf","text":"Report","size":"3.67 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Report"}],"country":"United States","state":"Oklahoma, Texas","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -96.17431640625,\n              36.049098959065645\n            ],\n            [\n              -101.14013671875,\n              32.879587173066305\n            ],\n            [\n              -99.931640625,\n              31.42866311735861\n            ],\n            [\n              -94.98779296875,\n              34.831841149828655\n            ],\n            [\n              -96.17431640625,\n              36.049098959065645\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b28e4b07f02db6b118c","contributors":{"authors":[{"text":"Buckner, Harold D.","contributorId":173633,"corporation":false,"usgs":false,"family":"Buckner","given":"Harold","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":157135,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kurklin, Joanne K.","contributorId":173634,"corporation":false,"usgs":false,"family":"Kurklin","given":"Joanne","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":157136,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":43241,"text":"ofr8442 - 1984 - Land use and land cover and associated maps for Burns, Oregon","interactions":[],"lastModifiedDate":"2012-02-02T00:10:26","indexId":"ofr8442","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"84-42","title":"Land use and land cover and associated maps for Burns, Oregon","language":"ENGLISH","doi":"10.3133/ofr8442","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1984, Land use and land cover and associated maps for Burns, Oregon: U.S. Geological Survey Open-File Report 84-42, maps :photocopy ;45 x 66 cm., on sheet 77 x 107 cm., https://doi.org/10.3133/ofr8442.","productDescription":"maps :photocopy ;45 x 66 cm., on sheet 77 x 107 cm.","costCenters":[],"links":[{"id":173435,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b28e4b07f02db6b168c","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":531060,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":7205,"text":"ofr83928 - 1984 - Glacial aquifer systems in the northeastern United States; a plan for study","interactions":[],"lastModifiedDate":"2012-02-02T00:06:00","indexId":"ofr83928","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"83-928","title":"Glacial aquifer systems in the northeastern United States; a plan for study","docAbstract":"The U.S. Geological Survey project designed to study the availability and quality of water in glacial aquifers in the States of Maine, New Hampshire, Vermont, Massachusetts, Rhode Island, Connecticut, New York, New Jersey, Pennsylvania, and Ohio is scheduled for completion in 1986. It will focus on general principles that define aquifer geometry, hydraulic properties of sediments, recharge, discharge, physical-chemical properties of water, rock and water-rock interactions, and mechanisms for mixing of water from multiple sources. Planned project activities include compilation and analysis of available data for a regionwide analysis of glacial-aquifer systems, studies of selected system components such as recharge and chemical processes, classification of aquifers with regard to water-supply potential, and construction of generalized ground-water models to predict responses of types of aquifer systems to pumping and climatic stress. This report describes the general characteristics of glacial aquifer systems in the Northeastern United States and of planned work elements of the study. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr83928","usgsCitation":"Lyford, F.P., Dysart, J., Randall, A., and Kontis, A., 1984, Glacial aquifer systems in the northeastern United States; a plan for study: U.S. Geological Survey Open-File Report 83-928, v, 64 p. :maps ;28 cm., https://doi.org/10.3133/ofr83928.","productDescription":"v, 64 p. :maps ;28 cm.","costCenters":[],"links":[{"id":140190,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0928/report-thumb.jpg"},{"id":34604,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0928/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac5e4b07f02db679c57","contributors":{"authors":[{"text":"Lyford, F. P.","contributorId":30223,"corporation":false,"usgs":true,"family":"Lyford","given":"F.","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":154756,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Dysart, J.E.","contributorId":23939,"corporation":false,"usgs":true,"family":"Dysart","given":"J.E.","affiliations":[],"preferred":false,"id":154755,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Randall, A. D.","contributorId":81077,"corporation":false,"usgs":true,"family":"Randall","given":"A. D.","affiliations":[],"preferred":false,"id":154758,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Kontis, A.L.","contributorId":69542,"corporation":false,"usgs":true,"family":"Kontis","given":"A.L.","affiliations":[],"preferred":false,"id":154757,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":43729,"text":"ofr84540 - 1984 - Land use and land cover and associated maps for Emory Peak, Texas","interactions":[],"lastModifiedDate":"2012-02-02T00:04:52","indexId":"ofr84540","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"84-540","title":"Land use and land cover and associated maps for Emory Peak, Texas","language":"ENGLISH","doi":"10.3133/ofr84540","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1984, Land use and land cover and associated maps for Emory Peak, Texas: U.S. Geological Survey Open-File Report 84-540, maps :photocopy ;44 x 77 cm., https://doi.org/10.3133/ofr84540.","productDescription":"maps :photocopy ;44 x 77 cm.","costCenters":[],"links":[{"id":134909,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b28e4b07f02db6b1372","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":531330,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":30440,"text":"wri844055 - 1984 - Effects of October 1981 flood on the quantity and quality of water in selected streams and reservoirs in the Brazos River basin, Texas","interactions":[],"lastModifiedDate":"2016-08-09T14:12:28","indexId":"wri844055","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","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":"84-4055","title":"Effects of October 1981 flood on the quantity and quality of water in selected streams and reservoirs in the Brazos River basin, Texas","docAbstract":"<p>The storm that moved across north-central Texas during October 11-13, 1981, produced intense rainfall along a line extending from east of Abilene, Texas to Breckenridge, Texas to north of Mineral Wells, Texas. Rainfall in excess of 20 inches was recorded near Clyde. Texas and in several locations near Breckenridge, Texas.</p>\n<p>The large quantity of rainfall in the Hubbard Creek drainage basin caused the water level in Hubbard Creek Reservoir to rise by 13.33f feet and the storage contents of the reservoir to increase from 233,000 to 441,000 acre-feet during 56 hours.</p>\n<p>Large quantities of inflow into Possum Kingdom Lake from the Brazos River, Big Cedar Creek basin, and ungaged inflow from the Big Caddo Creek basin, and Rock Creek basin caused the water level to rise 7.54 feet and the storage contents to increase from 505,000 to 653,000 acre-feet during 48 hours.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Austin, TX","doi":"10.3133/wri844055","usgsCitation":"Wells, F.C., Schertz, T.L., and Flugrath, M.W., 1984, Effects of October 1981 flood on the quantity and quality of water in selected streams and reservoirs in the Brazos River basin, Texas: U.S. Geological Survey Water-Resources Investigations Report 84-4055, ix, 119 p., https://doi.org/10.3133/wri844055.","productDescription":"ix, 119 p.","numberOfPages":"128","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":121665,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1984/4055/report-thumb.jpg"},{"id":59218,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1984/4055/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4ae4b07f02db625025","contributors":{"authors":[{"text":"Wells, Frank C.","contributorId":80664,"corporation":false,"usgs":true,"family":"Wells","given":"Frank","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":203254,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Schertz, Terry L. tschertz@usgs.gov","contributorId":188,"corporation":false,"usgs":true,"family":"Schertz","given":"Terry","email":"tschertz@usgs.gov","middleInitial":"L.","affiliations":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"preferred":true,"id":203255,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Flugrath, Marvin W.","contributorId":173557,"corporation":false,"usgs":false,"family":"Flugrath","given":"Marvin","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":203256,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":29851,"text":"wri844086 - 1984 - Appraisal of the surficial aquifers in the Pomme de Terre and Chippewa River Valleys, western Minnesota","interactions":[],"lastModifiedDate":"2018-04-02T11:06:56","indexId":"wri844086","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","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":"84-4086","title":"Appraisal of the surficial aquifers in the Pomme de Terre and Chippewa River Valleys, western Minnesota","docAbstract":"<p>The surf icial sands in the Pomme de Terre and Chippewa River valleys in Grant, Pope, Stevens, and Swift Counties have been studied to determine the occurrence, availability, and quality of ground water in these aquifers.</p>\n<p>In the northern part of the Pomme de Terre and Chippewa River valleys, the aquifers consist of coarse sand and gravel ranging from 0 to 100 feet in thickness; transmissivities range from 0 to 35,000 feet squared per day in narrow, steep-sided erosional valleys. In the north, well yields commonly exceed 1,000 gallons per minute and may be as much as 4,000 gallons per minute locally. Farther south, the deposits are medium to fine grained, range from 0 to 90 feet thick, and reach a maximum width of 10 miles near Benson, Minnesota. Transmissivities range from 0 to 25,000 feet squared per day. Wells may yield as much as 1,500 gallons per minute locally. Southeast of Clontarf, well yields generally do not exceed 500 gallons per minute because the deposits are thinly saturated and fine grained.</p>\n<p>Ground water in the surf icial aquifer is a mixed calcium magnesium-sulf ate bicarbonate type that is chemically suitable for most uses. Concentrations of most constituents analyzed were below limits recommended by the Minnesota Pollution Control Agency for drinking water, but concentrations of manganese, iron, nitrite plus nitrate, and dissolved solids exceed recommended limits locally. Salinity, as indicated by the specific conductance (values ranged from 580 to 1,000 micromhos per centimeter) was in the medium to high range at several locations.</p>\n<p>An analytical model was used to estimate the effect on streamflow of pumpage from the surficial aquifer in the narrow, 50-mile reach of the Pomme de Terre River valley in Stevens and Grant Counties. The model indicates that the 43 existing wells pumping at maximum potential yields could reduce streamflow by 55 cubic feet per second. Addition of 23 wells also pumping at maximum potential yields could reduce streamflow by 77 cubic feet per second; this rate exceeds low base flow of the Pomme de Terre River.</p>\n<p>Finite-difference models were used to simulate flow in the surficial aquifer along the Pomme de Terre River near Appleton in Swift County and along the Chippewa River between Cyrus in Pope County and Danvers in Swift County. In the Appleton area/ model analyses indicate that pumping lowered water levels as much as 3 feet from 1973-80 and reduced streamflow by about 14 cubic feet per second. Additional regional water-level declines of 1 to 2 feet/ and up to 4 feet locally near aquifer-till boundaries, can be expected after about 4 years if pumping continues at the 1980 rate and area! recharge from precipitation is near normal. However/ simulation of increased pumping rates and decreased area! recharge during a 3-year drought indicates that water levels may decline as much as 9 feet near aquifer-till boundaries and streamflow may be reduced by about 41 cubic feet per second, which is about 95 percent of the available flow in the Pomme de Terre River at the 55-percent flow duration. Model results also suggest that/ during the first year of a drought/ the combined pumpage from wells operated during 1980 along the Pomme de Terre River in Stevens and Grant Counties and in the Appleton area could reduce streamflow to zero during base flow. Model-computed streamflow deficiencies are 48 and 60 cubic feet per second at the 55- and 70-percent flow duration/ respectively. Under such conditions/ pumping could not be sustained at the rates simulated unless there was sufficient water stored in the stream channel or streamflow was augmented.</p>\n<p>In the Cyrus-Benson area/ model results indicate that tinder 1980 development and average area! recharge/ dynamic equilibrium would be reached in less than 4 years and additional drawdown would be less than 2 feet. A 3-year drought coupled with increased pumping from irrigation wells operated during 1980 would lower water levels as much as 6 feet and reduce flow in the Chippewa River by about 26 cubic feet per second. At maximum hypothetical development in terms of the number of wells and normal area! recharge/ water levels would be lowered as much as 9 feet and streamflow would be reduced about 12 cubic feet per second. At maximum hypothetical development/ drought conditions and increased pumping would lower water levels as much as 12 feet and reduce flow in the Chippewa River by about 30 cubic feet per second/ which equals about 75 percent of available streamflow at the 70-percent flow duration.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"St. Paul, MN","doi":"10.3133/wri844086","collaboration":"Prepared in cooperation with the Pomme de Terre and Chippewa Ground-Water Study Steering Committee and the Minnesota Department of Natural Resources","usgsCitation":"Soukup, W., Gillies, D.C., and Myette, C., 1984, Appraisal of the surficial aquifers in the Pomme de Terre and Chippewa River Valleys, western Minnesota: U.S. Geological Survey Water-Resources Investigations Report 84-4086, Document: vi, 63 p.; 4 Plates: 17.05 x 37.31 inches or smaller, https://doi.org/10.3133/wri844086.","productDescription":"Document: vi, 63 p.; 4 Plates: 17.05 x 37.31 inches or smaller","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":392,"text":"Minnesota Water Science Center","active":true,"usgs":true}],"links":[{"id":58660,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1984/4086/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":58661,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1984/4086/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":124175,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1984/4086/report-thumb.jpg"},{"id":58662,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1984/4086/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":58663,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1984/4086/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":58664,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1984/4086/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Minnesota","otherGeospatial":"Pomme de Terre and Chippewa River Valleys","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -96.016667,\n              46.116667\n            ],\n            [\n              -95.75,\n              46.116667\n            ],\n            [\n              -95.75,\n              45.766667\n            ],\n            [\n              -95.633333,\n              45.766667\n            ],\n            [\n              -95.633333,\n              45.416667\n            ],\n            [\n              -95.5,\n              45.416667\n            ],\n            [\n              -95.5,\n              45.15\n            ],\n            [\n              -95.733333,\n              45.15\n            ],\n            [\n              -95.733333,\n              44.966667\n            ],\n            [\n              -95.833333,\n              44.966667\n            ],\n            [\n              -96.1,\n              45.166667\n            ],\n            [\n              -96.1,\n              45.416667\n            ],\n            [\n              -96.016667,\n              45.416667\n            ],\n            [\n              -96.016667,\n              46.116667\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac6e4b07f02db67a3e4","contributors":{"authors":[{"text":"Soukup, W.G.","contributorId":82732,"corporation":false,"usgs":true,"family":"Soukup","given":"W.G.","email":"","affiliations":[],"preferred":false,"id":202243,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Gillies, D. 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