{"pageNumber":"5117","pageRowStart":"127900","pageSize":"25","recordCount":184617,"records":[{"id":7414,"text":"ofr84556 - 1984 - A Possible new source of natural gas in the eastern West Virginia Panhandle","interactions":[],"lastModifiedDate":"2012-02-02T00:06:08","indexId":"ofr84556","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":"84-556","title":"A Possible new source of natural gas in the eastern West Virginia Panhandle","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr84556","usgsCitation":"Pohn, H., 1984, A Possible new source of natural gas in the eastern West Virginia Panhandle: U.S. Geological Survey Open-File Report 84-556, 21 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr84556.","productDescription":"21 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":141381,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1984/0556/report-thumb.jpg"},{"id":34813,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1984/0556/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53cd4963e4b0b290850ef1dd","contributors":{"authors":[{"text":"Pohn, H. A.","contributorId":6912,"corporation":false,"usgs":true,"family":"Pohn","given":"H. A.","affiliations":[],"preferred":false,"id":155514,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":8267,"text":"ofr84627 - 1984 - Stability of slopes below the Sherwood Uranium Mine, Spokane Indian Reservation, northeastern Washington","interactions":[],"lastModifiedDate":"2012-02-02T00:05:59","indexId":"ofr84627","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":"84-627","title":"Stability of slopes below the Sherwood Uranium Mine, Spokane Indian Reservation, northeastern Washington","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr84627","usgsCitation":"Chleborad, A., and Schuster, R.L., 1984, Stability of slopes below the Sherwood Uranium Mine, Spokane Indian Reservation, northeastern Washington: U.S. Geological Survey Open-File Report 84-627, ii, 55 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr84627.","productDescription":"ii, 55 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":140096,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1984/0627/report-thumb.jpg"},{"id":35880,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1984/0627/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":35881,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1984/0627/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e2e4b07f02db5e49a2","contributors":{"authors":[{"text":"Chleborad, A.F.","contributorId":17990,"corporation":false,"usgs":true,"family":"Chleborad","given":"A.F.","affiliations":[],"preferred":false,"id":157456,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Schuster, R. L.","contributorId":19135,"corporation":false,"usgs":true,"family":"Schuster","given":"R.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":157457,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":64605,"text":"i1502 - 1984 - Reconnaissance geologic map of southwestern Misheguk Mountain Quadrangle, Alaska","interactions":[{"subject":{"id":7132,"text":"ofr82611 - 1982 - Reconnaissance geologic map of southwestern Misheguk Mountain quadrangle, Alaska","indexId":"ofr82611","publicationYear":"1982","noYear":false,"title":"Reconnaissance geologic map of southwestern Misheguk Mountain quadrangle, Alaska"},"predicate":"SUPERSEDED_BY","object":{"id":64605,"text":"i1502 - 1984 - Reconnaissance geologic map of southwestern Misheguk Mountain Quadrangle, Alaska","indexId":"i1502","publicationYear":"1984","noYear":false,"title":"Reconnaissance geologic map of southwestern Misheguk Mountain Quadrangle, Alaska"},"id":1}],"lastModifiedDate":"2012-02-10T00:10:52","indexId":"i1502","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":"1502","subseriesTitle":"NONE","title":"Reconnaissance geologic map of southwestern Misheguk Mountain Quadrangle, Alaska","language":"ENGLISH","doi":"10.3133/i1502","usgsCitation":"Curtis, S., Ellersieck, I., Mayfield, C., and Tailleur, I., 1984, Reconnaissance geologic map of southwestern Misheguk Mountain Quadrangle, Alaska: U.S. Geological Survey IMAP 1502, 1 map and 3 cross sections on 2 sheets :col. ;102 x 66 cm., sheets 145 x 106 cm. and 81 x 102 cm., folded in envelope 30 x 24 cm., https://doi.org/10.3133/i1502.","productDescription":"1 map and 3 cross sections on 2 sheets :col. ;102 x 66 cm., sheets 145 x 106 cm. and 81 x 102 cm., folded in envelope 30 x 24 cm.","costCenters":[],"links":[{"id":106769,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_9263.htm","linkFileType":{"id":5,"text":"html"},"description":"9263"},{"id":187358,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"63360","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -162,68 ], [ -162,68.58333333333333 ], [ -161,68.58333333333333 ], [ -161,68 ], [ -162,68 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a73e4b07f02db643730","contributors":{"authors":[{"text":"Curtis, S.M.","contributorId":16823,"corporation":false,"usgs":true,"family":"Curtis","given":"S.M.","email":"","affiliations":[],"preferred":false,"id":271710,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ellersieck, Inyo","contributorId":34914,"corporation":false,"usgs":true,"family":"Ellersieck","given":"Inyo","affiliations":[],"preferred":false,"id":271711,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Mayfield, C.F.","contributorId":95467,"corporation":false,"usgs":true,"family":"Mayfield","given":"C.F.","email":"","affiliations":[],"preferred":false,"id":271713,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Tailleur, I.L.","contributorId":59027,"corporation":false,"usgs":true,"family":"Tailleur","given":"I.L.","email":"","affiliations":[],"preferred":false,"id":271712,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":29493,"text":"wri834135 - 1984 - Regional geohydrology of the northern Louisiana salt-dome basin, part II, geohydrologic maps of the Tertiary aquifers and related confining layers","interactions":[],"lastModifiedDate":"2021-12-21T20:26:28.18915","indexId":"wri834135","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":"83-4135","title":"Regional geohydrology of the northern Louisiana salt-dome basin, part II, geohydrologic maps of the Tertiary aquifers and related confining layers","docAbstract":"

Regional geohydrologic maps show the altitude of the base and the thickness of the aquifers of Tertiary age and related confining layers in the northern Louisiana salt-dome basin. The limit of freshwater in aquifers is also shown. The basin has an area of about 3,000 square miles, and four geologic units of Tertiary age contain regional aquifers. From oldest (deepest) to youngest, the aquifers are in the Wilcox Group, Carrizo Sand, Sparta Sand, and Cockfield Formation. As the Wilcox is hydraulically interconnected with the overlying Carrizo, they are treated as one hydrologic unit, the Wilcox-Carrizo aquifer. The aquifers are separated by confining layers that retard water movement. In the northwestern part of the area, the Wilcox-Carrizo aquifer is separated from the underlying sand facies of the Nacatoch Sand (Cretaceous age) by a confining layer composed of the Midway Group (Tertiary age) and the underlying Arkadelphia Marl and an upper clay and marl facies of the Nacatoch Sand (both of Cretaceous age). In the remainder of the area, the Wilcox-Carrizo aquifer is separated from an underlying Cretaceous aquifer comprised of the Tokio Formation and Brownstown Marl by the Midway Group and several underlying Cretaceous units which in order of increasing age are the Arkadelphia Maril, Nacatoch Sand, Saratoga Chalk, Marlbrook Marl , and Annona Chalk. The Wilcox-Carrizo aquifer is separated from the Sparta aquifer by the overyling Cane River Formation. The Sparta aquifer is separated from the Cockfield aquifer by the overlying Cook Mountain Formation. 

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri834135","usgsCitation":"Ryals, G., 1984, Regional geohydrology of the northern Louisiana salt-dome basin, part II, geohydrologic maps of the Tertiary aquifers and related confining layers: U.S. Geological Survey Water-Resources Investigations Report 83-4135, Report: iii, 6 p.; 7 Plates: 21.40 × 22.74 inches or smaller, https://doi.org/10.3133/wri834135.","productDescription":"Report: iii, 6 p.; 7 Plates: 21.40 × 22.74 inches or smaller","costCenters":[],"links":[{"id":58338,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1983/4135/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":58337,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1983/4135/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":58336,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1983/4135/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":393241,"rank":10,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_35797.htm"},{"id":58342,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1983/4135/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":58335,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1983/4135/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":159716,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1983/4135/report-thumb.jpg"},{"id":58341,"rank":406,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1983/4135/plate-7.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":58340,"rank":405,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1983/4135/plate-6.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":58339,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1983/4135/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Louisiana","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -93.75,\n 31.536\n ],\n [\n -91.603,\n 31.536\n ],\n [\n -91.603,\n 33.433\n ],\n [\n -93.75,\n 33.433\n ],\n [\n -93.75,\n 31.536\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a2be4b07f02db613575","contributors":{"authors":[{"text":"Ryals, G.N.","contributorId":47374,"corporation":false,"usgs":true,"family":"Ryals","given":"G.N.","email":"","affiliations":[],"preferred":false,"id":201605,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":29949,"text":"wri844298 - 1984 - Water-quality investigations of the Jordan River, Salt Lake County, Utah, 1980-82","interactions":[],"lastModifiedDate":"2012-02-02T00:08:54","indexId":"wri844298","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":"84-4298","title":"Water-quality investigations of the Jordan River, Salt Lake County, Utah, 1980-82","docAbstract":"Water-quality studies were conducted on the Jordan River, Utah, to investigate specific problems: dissolved oxygen, toxic substances, sanitary quality, and turbidity and suspended sediment. The dissolved oxygen decreased from 8 milligrams per liter at the Jordan Narrows to less than 5 milligrams per liter at 500 North Street. Chemical oxygen demand increased about 23 percent and biochemical oxygen demand increased 90 percent. Nearly 78 percent of the water samples analyzed for total mercury exceeded the State intended-use standard of 0.05 microgram per liter. Concentrations of ammonia, cadmium, copper, lead, and zinc exceeded the standards periodically. The pesticides DDD, DDE, DDT, dieldrin, methoxychlor, and 2,4-D were occasionally detected in bottom materials. Most were present in quantities of less than 15 micrograms per kilogram. Concentrations of three indicator bacteria (total coliform, fecal coliform, and fecal streptococcus) increased in a downstream direction. Concentrations of total coliform bacteria often exceeded 5,000 colonies per 100 milliliters and concentrations of fecal coliform bacteria often exceeded 2,000 colonies per 100 milliliters. The primary sources of turbidity in the Jordan River are Utah Lake and discharges from the wastewater-treatment plants. Large values of turbidity were measured at the Jordan Narrows with a summer mean value of 88 nephelometer turbidity units (NTU) and a winter mean value of 43 NTU. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri844298","usgsCitation":"Stephens, D.W., 1984, Water-quality investigations of the Jordan River, Salt Lake County, Utah, 1980-82: U.S. Geological Survey Water-Resources Investigations Report 84-4298, viii, 45 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri844298.","productDescription":"viii, 45 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":125066,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1984/4298/report-thumb.jpg"},{"id":58770,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1984/4298/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e3e4b07f02db5e551a","contributors":{"authors":[{"text":"Stephens, D. W.","contributorId":68335,"corporation":false,"usgs":true,"family":"Stephens","given":"D.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":202412,"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":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":"

No abstract available.

","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":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":7209,"text":"ofr84605 - 1984 - Ground-water data for Georgia, 1983","interactions":[],"lastModifiedDate":"2016-12-14T13:53:15","indexId":"ofr84605","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":"84-605","title":"Ground-water data for Georgia, 1983","docAbstract":"Continuous water-level records from 134 wells and more than 700 water-level measurements made in Georgia during 1983 provide the basic data for this report. Selected wells illustrate the effects that changes in recharge and pumping have had on the various ground-water resources in the State. Daily mean water levels are shown in hydrographs for 1983. Monthly means are shown for the 10-year period 1974-83. Mean annual water levels ranged from 9 feet higher to 6 feet lower in 1983 than in 1982. Water-quality samples are collected periodically throughout Georgia and analyzed as part of areal and regional ground-water studies. Along the coast, chloride concentrations in the upper and lower water-bearing zones of the Floridan aquifer system generally remained steady in the Brunswick and Hilton Head Island areas. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr84605","usgsCitation":"Clarke, J., Peck, M., Longsworth, S., and McFadden, K., 1984, Ground-water data for Georgia, 1983: U.S. Geological Survey Open-File Report 84-605, xiv, 145 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr84605.","productDescription":"xiv, 145 p. :ill., maps ;28 cm.","costCenters":[{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true}],"links":[{"id":34610,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1984/0605/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":140821,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1984/0605/report-thumb.jpg"}],"country":"United 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Iowa"},"lastModifiedDate":"2012-02-02T00:10:28","indexId":"ofr83946","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":"83-946","title":"Bedrock topography of central Iowa","language":"ENGLISH","doi":"10.3133/ofr83946","usgsCitation":"Hansen, R., 1984, Bedrock topography of central Iowa: U.S. Geological Survey Open-File Report 83-946, 1 map on 2 sheets :photocopy ;98 x 139 cm., on sheets 127 x 77 and 132 x 88 cm. +1 pamphlet (9 leaves ; 28 cm), https://doi.org/10.3133/ofr83946.","productDescription":"1 map on 2 sheets :photocopy ;98 x 139 cm., on sheets 127 x 77 and 132 x 88 cm. +1 pamphlet (9 leaves ; 28 cm)","costCenters":[],"links":[{"id":172808,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a58e4b07f02db62eea7","contributors":{"authors":[{"text":"Hansen, R.E.","contributorId":57109,"corporation":false,"usgs":true,"family":"Hansen","given":"R.E.","email":"","affiliations":[],"preferred":false,"id":226156,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":39664,"text":"pp1317 - 1984 - Possible correlations of basement rocks across the San Andreas, San Gregorio-Hosgri, and Rinconada-Reliz-King City faults, California","interactions":[],"lastModifiedDate":"2012-02-02T00:09:56","indexId":"pp1317","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","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":"1317","title":"Possible correlations of basement rocks across the San Andreas, San Gregorio-Hosgri, and Rinconada-Reliz-King City faults, California","language":"ENGLISH","doi":"10.3133/pp1317","usgsCitation":"Ross, D.C., 1984, Possible correlations of basement rocks across the San Andreas, San Gregorio-Hosgri, and Rinconada-Reliz-King City faults, California: U.S. Geological Survey Professional Paper 1317, 37 p., https://doi.org/10.3133/pp1317.","productDescription":"37 p.","costCenters":[],"links":[{"id":123194,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/1317/report-thumb.jpg"},{"id":67385,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/1317/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad5e4b07f02db683ba5","contributors":{"authors":[{"text":"Ross, D. C.","contributorId":103681,"corporation":false,"usgs":true,"family":"Ross","given":"D.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":221939,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":8076,"text":"ofr84768 - 1984 - Selected references on the geology of the Danforth Hills coal field, Moffat and Rio Blanco counties, Colorado","interactions":[],"lastModifiedDate":"2012-02-02T00:06:13","indexId":"ofr84768","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":"84-768","title":"Selected references on the geology of the Danforth Hills coal field, Moffat and Rio Blanco counties, Colorado","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr84768","usgsCitation":"Brownfield, M.E., and Johnson, E.A., 1984, Selected references on the geology of the Danforth Hills coal field, Moffat and Rio Blanco counties, Colorado: U.S. Geological Survey Open-File Report 84-768, 31 p. :ill., map ;28 cm., https://doi.org/10.3133/ofr84768.","productDescription":"31 p. :ill., map ;28 cm.","costCenters":[],"links":[{"id":142068,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1984/0768/report-thumb.jpg"},{"id":35683,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1984/0768/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a03e4b07f02db5f82f2","contributors":{"authors":[{"text":"Brownfield, Michael E. 0000-0003-3633-1138","orcid":"https://orcid.org/0000-0003-3633-1138","contributorId":7250,"corporation":false,"usgs":true,"family":"Brownfield","given":"Michael","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":157101,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Johnson, E. A.","contributorId":87893,"corporation":false,"usgs":true,"family":"Johnson","given":"E.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":157102,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":29560,"text":"wri824102 - 1984 - Seasonal patterns of alkalinity in the San Francisco Bay estuarine system, California, during 1980","interactions":[],"lastModifiedDate":"2016-07-27T11:33:22","indexId":"wri824102","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":"82-4102","title":"Seasonal patterns of alkalinity in the San Francisco Bay estuarine system, California, during 1980","docAbstract":"

Salinity and alkalinity were measured in the near-surface waters of San Francisco Bay estuarine system at two-week intervals during 1980. Results are presented in figures and as numerical values, and the analytical methods are detailed. The transport of alkalinity to the Bay from the delta during 1980 was 3.8 x 10 to Ohe 10th power equivalents; this estimate is based on the freshwater alkalinity concentrations predicted by the north San Francisco Bay salinity-alkalinity distributions. North San Francisco Bay distributions are primarily the result of conservative mixing of freshwater from the Delta with Pacific Ocean water. Nonlinear distributions are the consequence of alkalinity variations in the freshwater rather than the effects of in-estuary processes or sources. Seasonal inflow of agricultural waste water is a major cause of freshwater alkalinity variations. South San Francisco Bay salinity-alkalinity distributions show the effects of variations in Delta outflow rate, local streams, and municipal waste-water inflows. (USGS)

","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri824102","usgsCitation":"Schemel, L., 1984, Seasonal patterns of alkalinity in the San Francisco Bay estuarine system, California, during 1980: U.S. Geological Survey Water-Resources Investigations Report 82-4102, iv, 54 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri824102.","productDescription":"iv, 54 p. :ill., maps ;28 cm.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":552,"text":"San Francisco Bay-Delta","active":false,"usgs":true},{"id":5079,"text":"Pacific Regional Director's Office","active":true,"usgs":true}],"links":[{"id":160460,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1982/4102/report-thumb.jpg"},{"id":58389,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1982/4102/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ce4b07f02db5fc33c","contributors":{"authors":[{"text":"Schemel, L. E.","contributorId":89529,"corporation":false,"usgs":true,"family":"Schemel","given":"L. E.","affiliations":[],"preferred":false,"id":201717,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":29559,"text":"wri834059 - 1984 - Salinity, alkalinity, and dissolved and particulate organic carbon in the Sacramento River water at Rio Vista, California, and at other locations in the Sacramento-San Joaquin Delta, 1980","interactions":[],"lastModifiedDate":"2022-12-15T21:52:01.77773","indexId":"wri834059","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":"83-4059","title":"Salinity, alkalinity, and dissolved and particulate organic carbon in the Sacramento River water at Rio Vista, California, and at other locations in the Sacramento-San Joaquin Delta, 1980","docAbstract":"

Salinity, alkalinity, and dissolved and particulate organic carbon (DOC and POC respectively) concentrations in the Sacramento River water at Rio Vista were measured every three to five days during 1980 as part of an effort to identify time-dependent variations in the composition of the freshwater flow from the Sacramento-San Joaquin Delta to San Francisco Bay. Concentration ranges were generally small compared to the seasonal range of river flow rate; transport rates to the Delta and to the Bay varied primarily as a function of flow rate. Surface runoff from winter storms diluted salinity and alkalinity concentrations. DOC and POC were generally more concentrated during winter than during other times of the year. Variations in tributary flows resulted in sometimes-large salinity and alkalinity variations during spring through fall. Late summer concentrations were high because of large inflows of agricultural waste waters. POC and DOC concentrations were lowest during summer. 

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri834059","usgsCitation":"Schemel, L., 1984, Salinity, alkalinity, and dissolved and particulate organic carbon in the Sacramento River water at Rio Vista, California, and at other locations in the Sacramento-San Joaquin Delta, 1980: U.S. Geological Survey Water-Resources Investigations Report 83-4059, iv, 45 p., https://doi.org/10.3133/wri834059.","productDescription":"iv, 45 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":552,"text":"San Francisco Bay-Delta","active":false,"usgs":true},{"id":5079,"text":"Pacific Regional Director's Office","active":true,"usgs":true}],"links":[{"id":410585,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_35695.htm","linkFileType":{"id":5,"text":"html"}},{"id":58388,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1983/4059/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":160459,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1983/4059/report-thumb.jpg"}],"country":"United States","state":"California","city":"Rio Vista","otherGeospatial":"Sacramento River","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -121.75,\n 38.5\n ],\n [\n -121.75,\n 37.888\n ],\n [\n -121.3,\n 37.888\n ],\n [\n -121.3,\n 38.5\n ],\n [\n -121.75,\n 38.5\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a09e4b07f02db5fad26","contributors":{"authors":[{"text":"Schemel, L. 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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.

\n

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.

\n

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.

\n

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.

\n

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.

\n

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.

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Gaging stations are classified based on the type of data and number of years record as current use, long-term trend, and planning and design. Goals are established for each classification. Suggestions for program revisions include establishing crest-stage gages for high-flow and flood-profile data, defining and establishing a low-flow network, and establishing two and discontinuing one daily discharge station. 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No abstract available.

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