{"pageNumber":"2306","pageRowStart":"57625","pageSize":"25","recordCount":68867,"records":[{"id":43127,"text":"ofr7717 - 1977 - Land use and land cover and associated maps for Port Townsend, Washington","interactions":[],"lastModifiedDate":"2012-02-02T00:05:01","indexId":"ofr7717","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1977","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":"77-17","title":"Land use and land cover and associated maps for Port Townsend, Washington","language":"ENGLISH","doi":"10.3133/ofr7717","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1977, Land use and land cover and associated maps for Port Townsend, Washington: U.S. Geological Survey Open-File Report 77-17, 5 maps ;56 x 75 cm., https://doi.org/10.3133/ofr7717.","productDescription":"5 maps ;56 x 75 cm.","costCenters":[],"links":[{"id":135568,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b26e4b07f02db6afc02","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":530977,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":64713,"text":"i1012 - 1977 - Leasable mineral and waterpower land classification map of the Choteau 1° x 2° quadrangle, Montana","interactions":[{"subject":{"id":46366,"text":"ofr74169 - 1974 - Leasable mineral and waterpower land classification map, Choteau Quadrangle, Montana, showing lands withdrawn, classified, and valuable prospectively for leasable minerals and occurrences of other selected minerals, lands withdrawn or classified for waterpower and reservoir sites","indexId":"ofr74169","publicationYear":"1974","noYear":false,"title":"Leasable mineral and waterpower land classification map, Choteau Quadrangle, Montana, showing lands withdrawn, classified, and valuable prospectively for leasable minerals and occurrences of other selected minerals, lands withdrawn or classified for waterpower and reservoir sites"},"predicate":"SUPERSEDED_BY","object":{"id":64713,"text":"i1012 - 1977 - Leasable mineral and waterpower land classification map of the Choteau 1° x 2° quadrangle, Montana","indexId":"i1012","publicationYear":"1977","noYear":false,"title":"Leasable mineral and waterpower land classification map of the Choteau 1° x 2° quadrangle, Montana"},"id":1}],"lastModifiedDate":"2021-11-01T21:14:21.530942","indexId":"i1012","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1977","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":"1012","title":"Leasable mineral and waterpower land classification map of the Choteau 1° x 2° quadrangle, Montana","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/i1012","usgsCitation":"Bateman, A., and Lutz, G.A., 1977, Leasable mineral and waterpower land classification map of the Choteau 1° x 2° quadrangle, Montana: U.S. Geological Survey IMAP 1012, 1 Plate: 32.78 × 23.32 inches, https://doi.org/10.3133/i1012.","productDescription":"1 Plate: 32.78 × 23.32 inches","costCenters":[],"links":[{"id":391238,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_8884.htm"},{"id":255148,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/imap/1012/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":255149,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/imap/1012/report-thumb.jpg"},{"id":255147,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/1012/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"250000","country":"United States","state":"Montana","otherGeospatial":"Choteau 1° x 2° quadrangle","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -114,47 ], [ -114,48 ], [ -112,48 ], [ -112,47 ], [ -114,47 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1ae4b07f02db6a87d3","contributors":{"authors":[{"text":"Bateman, A. F. Jr.","contributorId":24411,"corporation":false,"usgs":true,"family":"Bateman","given":"A. F.","suffix":"Jr.","affiliations":[],"preferred":false,"id":272027,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lutz, G. A.","contributorId":71604,"corporation":false,"usgs":true,"family":"Lutz","given":"G.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":272028,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":3474,"text":"cir767 - 1977 - Current oil and gas production from North American Upper Cretaceous chalks","interactions":[],"lastModifiedDate":"2012-02-02T00:05:36","indexId":"cir767","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1977","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":307,"text":"Circular","code":"CIR","onlineIssn":"2330-5703","printIssn":"1067-084X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"767","title":"Current oil and gas production from North American Upper Cretaceous chalks","docAbstract":"Production of oil and natural gas from North American chalks has increased significantly during the past five years, spurred by the prolific production from North Sea chalks, as well as by higher prices and improved production technology. Chalk reservoirs have been discovered in the Gulf Coast in the Austin Group, Saratoga and Annona Chalks, Ozan Formation, Selma Group, Monroe gas rock (an informal unit of Navarro age), and other Upper Cretaceous units. In the Western Interior, production has been obtained from the Cretaceous Niobrara and Greenhorn Formations. Significant, though subcommercial, discoveries of natural gas and gas condensate also have been made in the Upper Cretaceous Wyandot Formation on the Scotian Shelf of eastern Canada. \r\n\r\nAll North American chalk units share a similar depositional and diagenetic history. The chalks consist primarily of whole and fragmented coccoliths with subordinate planktonic and benthonic Foraminifera, inoceramid prisms, oysters, and other skeletal grains. Most have between 10 and 35 percent HCl-insoluble residue, predominantly clay. Deposition was principally below wave base in tens to hundreds of meters of water. \r\n\r\nThe diagenetic history of a chalk is critical in determining its reservoir potential. All chalk has a stable composition (low-Mg calcite) and very high primary porosity. With subsequent burial, mechanical and chemical (solution-transfer) compaction can reduce or completely eliminate pore space. The degree of loss of primary porosity in chalk sections is normally a direct function of the maximum depth to which it has been buried. Pore-water chemistry, pore-fluid pressures, and tectonic stresses also influence rates of cementation. Oil or gas reservoirs of North American chalk fall into three main groups: \r\n\r\n1. Areas with thin overburden and significant primary porosity retention (for example, Niobrara Formation of Kansas and eastern Colorado). \r\n\r\n2. Areas with thicker overburden but considerable fracturing. Here primary porosity has been largely lost but secondary (fracture) porosity provides some storage capacity and greatly improves permeability (for example, Austin Group of the Pearsall field, Texas). \r\n\r\n3. Areas with thick overburden in which marine pore fluids have been retained, or where hydrocarbons (including biogenically generated methane) were introduced early in the diagenetic history. \r\n\r\nIn these settings, primary porosity is reduced to a lesser degree than in group two, and adequate reservoir properties can be maintained to depths approaching 2,000 m (6,600 ft) (for example, Scotian Shelf of Canada). \r\n\r\nContinued small-scale oil and gas discoveries can be expected from these types of reservoirs in North America. The prolific production of oil and gas from North Sea chalk reservoirs will not be matched in North America unless deeply buried, overpressured chalks can be located. It is the early formation of overpressures and (or) early oil input into North Sea chalks that have preserved porosities as high as 40 percent at 3,000- to 3,500-m (9,800- to 11,500-ft) depths and provided the outstanding reservoir capacity of those chalks.","language":"ENGLISH","publisher":"Dept. of the Interior, Geological Survey,","doi":"10.3133/cir767","usgsCitation":"Scholle, P.A., 1977, Current oil and gas production from North American Upper Cretaceous chalks: U.S. Geological Survey Circular 767, iv, 51 p. :ill., maps ;26 cm. , https://doi.org/10.3133/cir767.","productDescription":"iv, 51 p. :ill., maps ;26 cm. ","costCenters":[],"links":[{"id":126710,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1977/0767/report-thumb.jpg"},{"id":30485,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1977/0767/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4acce4b07f02db67ec52","contributors":{"authors":[{"text":"Scholle, Peter A.","contributorId":48954,"corporation":false,"usgs":true,"family":"Scholle","given":"Peter","email":"","middleInitial":"A.","affiliations":[{"id":218,"text":"Denver Federal Center","active":false,"usgs":true}],"preferred":false,"id":146992,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":57421,"text":"wdrOH762 - 1977 - Water Resources Data for Ohio, Water Year 1976--Volume 2. St. Lawrence River Basin","interactions":[],"lastModifiedDate":"2012-02-02T00:12:07","indexId":"wdrOH762","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1977","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":"OH-76-2","title":"Water Resources Data for Ohio, Water Year 1976--Volume 2. St. Lawrence River Basin","language":"ENGLISH","doi":"10.3133/wdrOH762","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1977, Water Resources Data for Ohio, Water Year 1976--Volume 2. St. Lawrence River Basin: U.S. Geological Survey Water Data Report OH-76-2, 216 p., 2 fig., https://doi.org/10.3133/wdrOH762.","productDescription":"216 p., 2 fig.","costCenters":[],"links":[{"id":182098,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ce4b07f02db5fcab2","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":533090,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":4723,"text":"twri05A5 - 1977 - Methods for determination of radioactive substances in water and fluvial sediments","interactions":[],"lastModifiedDate":"2013-11-19T16:19:24","indexId":"twri05A5","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1977","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":336,"text":"Techniques of Water-Resources Investigations","code":"TWRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"05-A5","title":"Methods for determination of radioactive substances in water and fluvial sediments","docAbstract":"Analytical methods for the determination of some of the more important components of fission or neutron activation product radioactivity and of natural radioactivity found in water are reported. The report for each analytical method includes conditions for application of the method, a summary of the method, interferences, required apparatus and reagents, analytical procedures, calculations, reporting of results, and estimation of precision. The fission product isotopes considered are cesium-137, strontium-90, and ruthenium-106. The natural radioelements and isotopes considered are uranium, lead-210, radium-226, radium-228, tritium, and carbon-14. A gross radioactivity survey method and a uranium isotope ratio method are given. When two analytical methods are in routine use for an individual isotope, both methods are reported with identification of the specific areas of application of each. Techniques for the collection and preservation of water samples to be analyzed for radioactivity are discussed.","language":"English","publisher":"U.S. Government Printing Office","doi":"10.3133/twri05A5","usgsCitation":"Thatcher, L.L., Janzer, V.J., and Edwards, K.W., 1977, Methods for determination of radioactive substances in water and fluvial sediments: U.S. Geological Survey Techniques of Water-Resources Investigations 05-A5, vi, 95 p., https://doi.org/10.3133/twri05A5.","productDescription":"vi, 95 p.","numberOfPages":"94","costCenters":[{"id":343,"text":"Idaho Water Science Center","active":true,"usgs":true}],"links":[{"id":139094,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":351,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/twri/twri5a5/","linkFileType":{"id":5,"text":"html"}},{"id":279206,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/twri/twri5a5/pdf/TWRI_5-A5.pdf"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b28e4b07f02db6b12dd","contributors":{"authors":[{"text":"Thatcher, Leland Lincoln","contributorId":73985,"corporation":false,"usgs":true,"family":"Thatcher","given":"Leland","email":"","middleInitial":"Lincoln","affiliations":[],"preferred":false,"id":149684,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Janzer, Victor J.","contributorId":36119,"corporation":false,"usgs":true,"family":"Janzer","given":"Victor","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":149682,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Edwards, Kenneth W.","contributorId":61023,"corporation":false,"usgs":true,"family":"Edwards","given":"Kenneth","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":149683,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":26163,"text":"wri7787 - 1977 - Surface-water and ground-water features, Clay County, Florida","interactions":[],"lastModifiedDate":"2017-10-17T14:54:14","indexId":"wri7787","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1977","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":"77-87","title":"Surface-water and ground-water features, Clay County, Florida","docAbstract":"<p>Clay County is a rapidly growing area in northeastern Florida. Surface water largely is undeveloped except for recreational use. Black Creek is the largest fresh-water stream in the country and has an average discharge of about 515 cubic feet per second. However, excessive color, iron concentration, hardness, and pH often make the water objectionable for many uses. Water from the lakes and streams in the Etonia Creek basin in southwestern Clay County generally is of good chemical quality. </p><p>Ground water occurs in the county in a water-table aquifer, secondary artesian aquifers, and the Floridan aquifer. Large withdrawals of water from the Floridan aquifer since the 1940's, especially in nearby metropolitan Jacksonville, have caused a decline of the potentiometric surface of up to 30 feet in the northeast corner of Clay County to less than 5 feet in the western part. The rate of decline in recent years at Orange Park has been about 0.7 of a foot per year. Ground water in the county generally is of good chemical quality and is suitable for most uses. The quality has not changes noticeably in the past several years since records have been kept.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri7787","collaboration":"Prepared in cooperation with Clay County Development Authority","usgsCitation":"Bentley, C., 1977, Surface-water and ground-water features, Clay County, Florida: U.S. Geological Survey Water-Resources Investigations Report 77-87, viii, 59 p., https://doi.org/10.3133/wri7787.","productDescription":"viii, 59 p.","costCenters":[],"links":[{"id":346717,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1977/0087/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":158121,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1977/0087/report-thumb.jpg"}],"country":"United States","state":"Florida","county":"Clay County","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b15e4b07f02db6a4d5c","contributors":{"authors":[{"text":"Bentley, C.B.","contributorId":28223,"corporation":false,"usgs":true,"family":"Bentley","given":"C.B.","email":"","affiliations":[],"preferred":false,"id":195923,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":56369,"text":"wdrME761 - 1977 - Water resources data for Maine, water year 1976","interactions":[],"lastModifiedDate":"2025-07-29T14:45:57.648239","indexId":"wdrME761","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1977","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":"ME-76-1","title":"Water resources data for Maine, water year 1976","docAbstract":"<p>Water resources data for the 1976 water year for Maine consist of records of stage, discharge, and water quality of streams; stage and contents of lakes and reservoirs; and water-levels and water quality of wells. This report contains discharge records for 66 gaging stations; stage only records for 2 gaging stations; contents for 17 lakes and reservoirs; water quality for 13 gaging stations and 22 wells; and water levels for 17 observation wells. Additional water data were collected at various sites, not part of the systematic data collection program, and are published as miscellaneous measurements. These data represent that part of the National Water Data System operated by the U.S. Geological Survey and cooperating State and Federal agencies.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wdrME761","collaboration":"Prepared in cooperation with the State of Maine and with other agencies","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1977, Water resources data for Maine, water year 1976: U.S. Geological Survey Water Data Report ME-76-1, vii, 216 p., https://doi.org/10.3133/wdrME761.","productDescription":"vii, 216 p.","costCenters":[],"links":[{"id":493097,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/1976/me-76-1/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":184917,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wdr/1976/me-76-1/report-thumb.jpg"}],"country":"United 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,{"id":43126,"text":"ofr77450 - 1977 - Land use and land cover and associated maps for Port Orford, Oregon","interactions":[],"lastModifiedDate":"2012-02-02T00:05:01","indexId":"ofr77450","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1977","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":"77-450","title":"Land use and land cover and associated maps for Port Orford, Oregon","language":"ENGLISH","doi":"10.3133/ofr77450","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1977, Land use and land cover and associated maps for Port Orford, Oregon: U.S. Geological Survey Open-File Report 77-450, 5 maps ;87 x 102 cm., https://doi.org/10.3133/ofr77450.","productDescription":"5 maps ;87 x 102 cm.","costCenters":[],"links":[{"id":135567,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b26e4b07f02db6af997","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":530976,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":27262,"text":"wri7727 - 1977 - Low-flow characteristics at gaging stations on the Wisconsin, Fox, and Wolf rivers, Wisconsin","interactions":[],"lastModifiedDate":"2015-10-21T10:32:44","indexId":"wri7727","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1977","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":"77-27","title":"Low-flow characteristics at gaging stations on the Wisconsin, Fox, and Wolf rivers, Wisconsin","docAbstract":"<p>Low-flow characteristics are presented at eleven gaging stations on the main stem of the Wisconsin, Fox, and Wolf Rivers in this report. The low-flow characteristics presented are the annual minimum 7-day mean flow below which the flow will fall on the average of once in 2 years (Q7, 2) and the annual minimum 7-day mean flow below which the flow will fall on the average of once in 10 years (Q7, I0).</p>\n<p>To provide accurate and consistent low-flow characteristics for uniform evaluation of waste effluent, a long-term period of streamflow record was used for the analyses. The record selected for the study was 1915-75. This was found to be the most representative that included longterm streamflow conditions and various degrees of regulation by storage reservoirs.</p>\n<p>The Q7, 10 discharge on the Wisconsin River ranged from lUO cubic feet per second at the Wisconsin River at Rainbow Lake near Lake Tomahawk gaging station to 2,790 cubic feet per second at the Wisconsin River at Muscoda gaging station. On the Fox-Wolf Rivers, the Q7, 10 ranged from 360 cubic feet per second at Fox River at Berlin to 950 cubic feet per second at Fox River at Rapide Croche dam near Wrightstown.</p>\n<p>Low-flow characteristics that reflect unregulated and regulated conditions on the upper Wisconsin River were compared. This analysis showed no apparent difference in Q7, 10 discharge values due to regulation at the Wisconsin River at Merrill gaging station, although a more detailed study is warranted to fully evaluate the effect of storage.</p>\n<p>The magnitude of the low-flow characteristics are in some instances affected by the period of record. These characteristics can vary as much as &plusmn;30 percent at some gaging stations depending on whether or not the severe drought of the 1930's was included in the analysis.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri7727","collaboration":"Prepared in cooperation with the Wisconsin Department of Natural Resources","usgsCitation":"Gebert, W., and Holmstrom, B.K., 1977, Low-flow characteristics at gaging stations on the Wisconsin, Fox, and Wolf rivers, Wisconsin: U.S. Geological Survey Water-Resources Investigations Report 77-27, iii, 20 p., https://doi.org/10.3133/wri7727.","productDescription":"iii, 20 p.","numberOfPages":"26","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":677,"text":"Wisconsin Water Science 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,{"id":9509,"text":"ofr77811 - 1977 - Assessment of the current Occoquan water-supply situation, Fairfax County, Virginia","interactions":[],"lastModifiedDate":"2012-02-02T00:06:11","indexId":"ofr77811","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1977","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":"77-811","title":"Assessment of the current Occoquan water-supply situation, Fairfax County, Virginia","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr77811","usgsCitation":"Hirsch, R.M., Schaake, J.C., and Sheer, D.P., 1977, Assessment of the current Occoquan water-supply situation, Fairfax County, Virginia: U.S. Geological Survey Open-File Report 77-811, 3 leaves ;27 cm., https://doi.org/10.3133/ofr77811.","productDescription":"3 leaves ;27 cm.","costCenters":[],"links":[{"id":140997,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4abae4b07f02db671db9","contributors":{"authors":[{"text":"Hirsch, Robert M. 0000-0002-4534-075X rhirsch@usgs.gov","orcid":"https://orcid.org/0000-0002-4534-075X","contributorId":2005,"corporation":false,"usgs":true,"family":"Hirsch","given":"Robert","email":"rhirsch@usgs.gov","middleInitial":"M.","affiliations":[{"id":37778,"text":"WMA - Integrated Modeling and Prediction Division","active":true,"usgs":true},{"id":37316,"text":"WMA - Integrated Information Dissemination Division","active":true,"usgs":true},{"id":502,"text":"Office of Surface Water","active":true,"usgs":true},{"id":436,"text":"National Research Program - Eastern Branch","active":true,"usgs":true}],"preferred":true,"id":159808,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Schaake, John C.","contributorId":58268,"corporation":false,"usgs":true,"family":"Schaake","given":"John","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":159809,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Sheer, Daniel P.","contributorId":93908,"corporation":false,"usgs":true,"family":"Sheer","given":"Daniel","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":159810,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":64706,"text":"i1015 - 1977 - Leasable mineral and waterpower land classification map of the Havre 1° x 2° quadrangle, Montana","interactions":[{"subject":{"id":46422,"text":"ofr74265 - 1974 - Leasable mineral and waterpower land classification map, Havre Quadrangle, Montana, showing lands withdrawn, classified, and valuable prospectively for leasable minerals and occurrences of other selected minerals, lands withdrawn or classified for waterpower and reservoir sites","indexId":"ofr74265","publicationYear":"1974","noYear":false,"title":"Leasable mineral and waterpower land classification map, Havre Quadrangle, Montana, showing lands withdrawn, classified, and valuable prospectively for leasable minerals and occurrences of other selected minerals, lands withdrawn or classified for waterpower and reservoir sites"},"predicate":"SUPERSEDED_BY","object":{"id":64706,"text":"i1015 - 1977 - Leasable mineral and waterpower land classification map of the Havre 1° x 2° quadrangle, Montana","indexId":"i1015","publicationYear":"1977","noYear":false,"title":"Leasable mineral and waterpower land classification map of the Havre 1° x 2° quadrangle, Montana"},"id":1}],"lastModifiedDate":"2021-11-01T21:21:32.312264","indexId":"i1015","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1977","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":"1015","title":"Leasable mineral and waterpower land classification map of the Havre 1° x 2° quadrangle, Montana","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/i1015","usgsCitation":"Bateman, A.F., Allen, E.G., and Hettinger, R.D., 1977, Leasable mineral and waterpower land classification map of the Havre 1° x 2° quadrangle, Montana: U.S. Geological Survey IMAP 1015, 1 Plate: 31.82 × 22.94 inches, https://doi.org/10.3133/i1015.","productDescription":"1 Plate: 31.82 × 22.94 inches","costCenters":[],"links":[{"id":391240,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_8887.htm"},{"id":255128,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/imap/1015/report-thumb.jpg"},{"id":255127,"rank":299,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/imap/1015/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":255126,"rank":399,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/1015/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"250000","country":"United States","state":"Montana","otherGeospatial":"Havre 1° x 2° quadrangle","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -110,48 ], [ -110,49 ], [ -108,49 ], [ -108,48 ], [ -110,48 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1ae4b07f02db6a8187","contributors":{"authors":[{"text":"Bateman, A. F. Jr.","contributorId":16489,"corporation":false,"usgs":true,"family":"Bateman","given":"A.","suffix":"Jr.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":272009,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Allen, E. G.","contributorId":78379,"corporation":false,"usgs":true,"family":"Allen","given":"E.","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":272010,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hettinger, R. D.","contributorId":92283,"corporation":false,"usgs":true,"family":"Hettinger","given":"R.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":272011,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":56380,"text":"wdrPA763 - 1977 - Water resources data for Pennsylvania; Volume 3, Ohio River and St. Lawrence River basins, water year 1976","interactions":[],"lastModifiedDate":"2012-02-02T00:12:19","indexId":"wdrPA763","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1977","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":"PA-76-3","title":"Water resources data for Pennsylvania; Volume 3, Ohio River and St. Lawrence River basins, water year 1976","language":"ENGLISH","doi":"10.3133/wdrPA763","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1977, Water resources data for Pennsylvania; Volume 3, Ohio River and St. Lawrence River basins, water year 1976: U.S. Geological Survey Water Data Report PA-76-3, 270 p., https://doi.org/10.3133/wdrPA763.","productDescription":"270 p.","costCenters":[],"links":[{"id":185019,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f7e4b07f02db5f1e76","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":532561,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":27018,"text":"wri7732 - 1977 - Saline-water intrusion in the Floridan Aquifer in the Fernandina Beach area, Nassau County, Florida","interactions":[],"lastModifiedDate":"2017-05-09T15:38:37","indexId":"wri7732","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1977","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":"77-32","title":"Saline-water intrusion in the Floridan Aquifer in the Fernandina Beach area, Nassau County, Florida","docAbstract":"The Floridan aquifer is the major source of water for municipal and industrial use in northeastern Nassau County, Florida. Pumpage from the aquifer at Fernandina Beach has created a cone of depression in the potentiometric surface which is at or below sea level in a 35-square mile area. Since 1880 water levels have declined more than 120 feet near the center of pumping, and chloride concentrations have increased from about 20 to a maximum of 800 milligrams per liter in some deep wells. The saline water probably is connate water which comes from zones below 1,250 and 2,000 feet. Several alternate methods to control the migration of saline water are discussed. 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,{"id":57420,"text":"wdrOH761 - 1977 - Water Resources Data for Ohio, Water Year 1976--Volume 1. Ohio River Basin","interactions":[],"lastModifiedDate":"2012-02-02T00:12:07","indexId":"wdrOH761","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1977","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":"OH-76-1","title":"Water Resources Data for Ohio, Water Year 1976--Volume 1. Ohio River Basin","language":"ENGLISH","doi":"10.3133/wdrOH761","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1977, Water Resources Data for Ohio, Water Year 1976--Volume 1. Ohio River Basin: U.S. Geological Survey Water Data Report OH-76-1, 611 p., 2 fig., https://doi.org/10.3133/wdrOH761.","productDescription":"611 p., 2 fig.","costCenters":[],"links":[{"id":182097,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ce4b07f02db5fca9d","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":533089,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":4386,"text":"cir736C - 1977 - Seismic engineering program report, July-September 1976","interactions":[],"lastModifiedDate":"2012-02-02T00:05:27","indexId":"cir736C","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1977","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":307,"text":"Circular","code":"CIR","onlineIssn":"2330-5703","printIssn":"1067-084X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"736","chapter":"C","title":"Seismic engineering program report, July-September 1976","language":"ENGLISH","publisher":"U.S. Dept. of the Interior, Geological Survey ;\r\nFree on application to Branch of Distribution, U.S. Geological Survey,","doi":"10.3133/cir736C","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1977, Seismic engineering program report, July-September 1976: U.S. Geological Survey Circular 736, v, 14 p. :map ;26 cm., https://doi.org/10.3133/cir736C.","productDescription":"v, 14 p. :map ;26 cm.","costCenters":[],"links":[{"id":117394,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1977/0736c/report-thumb.jpg"},{"id":31495,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1977/0736c/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ae4b07f02db5fb889","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":528204,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":27035,"text":"wri76113 - 1977 - Ground-water resources of the Lexington, Kentucky, area","interactions":[],"lastModifiedDate":"2019-08-05T11:08:25","indexId":"wri76113","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1977","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":"76-113","title":"Ground-water resources of the Lexington, Kentucky, area","docAbstract":"Ground water in the Lexington, Kentucky, area occurs in Ordovician Limestones in which cavity development is generally limited to about 100 feet below land surface. Some wells produce about 300 gallons per minute in some of the large stream valleys , about 50 gallons per minute in the rolling upland and small stream valleys, and about 5 gallons per minute on hilltops and steep slopes. Many wells throughout the area do not furnish adequate water for domestic supplies because no significant water-bearing openings are penetrated during drilling. Ground-water use is limited mostly to domestic and stock supplies and a few small public supplies. Ground water is generally a calcium bicarbonate type and in places contains sodium chloride and (or) hydrogen sulfide. Bacterial pollution of ground water is widespread because of direct recharge of polluted runoff and streamflow to cavernous limestones. (Woodard-USGS)","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wri76113","usgsCitation":"Faust, R., 1977, Ground-water resources of the Lexington, Kentucky, area: U.S. Geological Survey Water-Resources Investigations Report 76-113, Report: v, 24 p.; 4 Plates: 13.94 x 16.79 inches or smaller , https://doi.org/10.3133/wri76113.","productDescription":"Report: v, 24 p.; 4 Plates: 13.94 x 16.79 inches or smaller ","costCenters":[],"links":[{"id":366227,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1976/0113/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":366228,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1976/0113/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":366229,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1976/0113/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":366230,"rank":5,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1976/0113/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":366231,"rank":6,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1976/0113/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":158624,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1976/0113/report-thumb.jpg"}],"country":"United States","state":"Kentucky","city":"Lexington","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -84.605712890625,\n              37.965854128749434\n            ],\n            [\n              -84.3804931640625,\n              37.965854128749434\n            ],\n            [\n              -84.3804931640625,\n              38.09998264736481\n            ],\n            [\n              -84.605712890625,\n              38.09998264736481\n            ],\n            [\n              -84.605712890625,\n              37.965854128749434\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a92e4b07f02db657904","contributors":{"authors":[{"text":"Faust, R.J.","contributorId":80700,"corporation":false,"usgs":true,"family":"Faust","given":"R.J.","email":"","affiliations":[],"preferred":false,"id":197446,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":43553,"text":"ofr7711 - 1977 - Land use and land cover and associated maps for Harrison, Arkansas; Missouri (Missouri portion only)","interactions":[],"lastModifiedDate":"2012-02-02T00:10:28","indexId":"ofr7711","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1977","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":"77-11","title":"Land use and land cover and associated maps for Harrison, Arkansas; Missouri (Missouri portion only)","language":"ENGLISH","doi":"10.3133/ofr7711","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1977, Land use and land cover and associated maps for Harrison, Arkansas; Missouri (Missouri portion only): U.S. Geological Survey Open-File Report 77-11, 7 maps ;45 x 73 cm. --, https://doi.org/10.3133/ofr7711.","productDescription":"7 maps ;45 x 73 cm. --","costCenters":[],"links":[{"id":172337,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b28e4b07f02db6b10ef","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":531237,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":10478,"text":"ofr77592 - 1977 - Geology of the Midnite uranium mine area, Washington — Maps, description, and interpretation","interactions":[],"lastModifiedDate":"2021-12-08T22:09:56.728257","indexId":"ofr77592","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1977","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":"77-592","title":"Geology of the Midnite uranium mine area, Washington — Maps, description, and interpretation","docAbstract":"<p>Bedrock geology of about 12 km<sup>2</sup> near the Midnite mine has been mapped at the surface, in mine exposures, and from drilling, at scales from 1:600 to 1:12,000 and is presented here at 1:12,000 to provide description of the setting of uranium deposits. Oldest rocks in the area are metapelitic and metacarbonate rocks of the Precambrian (Y) Togo Formation. The chief host for uranium deposits is graphitic and pyritic mica phyllite and muscovite schist. Ore also occurs in calc-silicate hornfels and marble at the western edge of a calcareous section about 1,150 m thick. Calcareous rocks of the Togo are probably older than the pelitic as they are interpreted to be near the axis of a broad anticline. The composition and structural position of the calcareous unit suggests correlation with less metamorphosed carbonate-bearing rocks of the Lower Wallace Formation, Belt Supergroup, about 200 km to the east. Basic sills intrusive into the Togo have been metamorphosed to amphibolite.</p><p> Unmetamorphosed rocks in the mine area are Cretaceous(?) and Eocene igneous rocks. Porphyritic quartz monzonite of Cretaceous age, part of the Loon Lake batholith, is exposed over one third of the mine area. It underlies the roof pendant of Precambrian rocks in which the Midnite mine occurs at depths of generally less than 300 m. The pluton is a two-mica granite and exhibits pegmatitic and aplitic textural features indicative of water saturation and pressure quenching. Eocene intrusive and extrusive rocks in the area provide evidence that the Eocene surface was only a short distance above the present uranium deposits. </p><p>Speculative hypotheses are presented for penesyngenetic, hydrothermal, and supergene modes of uranium emplacement. The Precambrian Stratigraphy, similar in age and pre-metamorphic lithology to that of rocks hosting large uranium deposits in Saskatchewan and Northern Territory, Australia, suggests the possibility of uranium accumulation along with diagenetic pyrite in carbonaceous muds in a marine shelf environment. This hypothesis is not favored by the author because there is no evidence for stratabound uranium such as high regional radioactivity in the Togo. A hydrothermal mode of uranium emplacement is supported by the close apparent ages of mineralization and plutonism, and by petrology of the pluton. I speculate that uranium may have become enriched in postmagmatic fluids at the top of the pluton, possibly by hydrothermal leaching of soluble uranium associated with magnetite, and diffused outward into metasedimentary wall rocks to create an aureole about 100 m thick containing about 100 ppm uranium. Chemistry of the hydrothermal process is not understood, but uranium does not appear to have been transported by an oxidizing fluid, and the fluid did not produce veining and alteration comparable to that of base-metal sulfide deposits. Uranium in the low-grade protore is believed to have been redistributed into permeable zones in the Tertiary to create ore grades. Geologic and isotopic ages of uranium mineralization, and the small volume of porphyritic quartz monzonite available for leaching, are not supportive of supergene emplacement of uranium.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr77592","usgsCitation":"Nash, J.T., 1977, Geology of the Midnite uranium mine area, Washington — Maps, description, and interpretation: U.S. Geological Survey Open-File Report 77-592, Report: ii, 39 p.; 2 Plates: 15.00 × 20.00 inches and 16.00 × 17.00 inches, https://doi.org/10.3133/ofr77592.","productDescription":"Report: ii, 39 p.; 2 Plates: 15.00 × 20.00 inches and 16.00 × 17.00 inches","costCenters":[],"links":[{"id":392655,"rank":5,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_14485.htm"},{"id":38343,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1977/0592/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":143959,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1977/0592/report-thumb.jpg"},{"id":94974,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1977/0592/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":94973,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1977/0592/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"12000","country":"United States","state":"Washington","otherGeospatial":"Midnite uranium mine area","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -118.118,\n              47.933\n            ],\n            [\n              -118.0670,\n              47.933\n            ],\n            [\n              -118.0670,\n              47.962\n            ],\n            [\n              -118.118,\n              47.962\n            ],\n            [\n              -118.118,\n              47.933\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4acce4b07f02db67e9da","contributors":{"authors":[{"text":"Nash, J. Thomas","contributorId":26306,"corporation":false,"usgs":true,"family":"Nash","given":"J.","email":"","middleInitial":"Thomas","affiliations":[],"preferred":false,"id":161468,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":8217,"text":"ofr77278 - 1977 - A preliminary appraisal of the Garber-Wellington Aquifer, southern Logan and northern Oklahoma counties, Oklahoma","interactions":[],"lastModifiedDate":"2012-02-02T00:06:08","indexId":"ofr77278","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1977","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":"77-278","title":"A preliminary appraisal of the Garber-Wellington Aquifer, southern Logan and northern Oklahoma counties, Oklahoma","docAbstract":"The Garber-Wellington aquifer, which dips westward at 30 to 40 feet per mile, consists of about 900 feet of interbedded sandstone, shale, and siltstone. Sandstone comprises 35 to 75 percent of the aquifer and averages about 50 percent. Water-table conditions generally exist in the upper 200 feet in the outcrop area of the aquifer; semi-artesian or artesian conditions exist below a depth of 200 feet and beneath rocks of the Hennessey Group (predominantly shale) where the aquifer is fully saturated. Water containing more than 1,000 milligrams per liter dissolved solids occurs at various depths through the area. The altitude of the base of fresh water ranges from 250 feet above sea level in the south-central part of the area to 950 feet in the northwestern part. The thickness of the fresh-water zone ranges from less than 150 feet in the northern part of the area to about 850 feet in the southern part. The total amount of water stored in the fresh-water zone is estimated to be 21 million acre-feet based on specific yield of 0.20.\r\nMinimum recharge to the aquifer in 1975 is estimated to be 190 acre-feet per square mile or about 10 percent of the annual precipitation. Total minimum recharge to the aquifer in the study area in 1975 is estimated to be 129,000 acre-feet. Streams in the area are the principal means of ground-water discharge; the amount of discharge is essentially the same as recharge. The amount of groundwater used for municipal and rural water supply in 1975 is estimated to have been 5,000 acre-feet; a similar amount may have been used for industrial purposes. As a result of pumping, the potentiometric surface in 1975 had been lowered about 200 feet in the vicinity of Edmond and about 100 feet in the vicinity of Nichols Hills.\r\n\r\nChemical analyses of water from the aquifer indicates that hardness is greater in the upper part of the aquifer than in the lower part, and that sulfate, chloride, and dissolved solids increase with depth.\r\n\r\nReported yields of wells more than 250 feet deep range from 70 to 475 gallons per minute and average 240 gallons per minute. Potential well yields range from 225 gallons per minute when the fresh-water zone is 350 feet thick to about 550 gallons per minute where the fresh water zone is 850 feet thick. These estimates of potential yield are based on an available drawdown of half the thickness of the fresh-water zone and a specific capacity of 1.3 gallons per minute per foot.\r\n\r\nIntrusion of saline water into the fresh-water zone is a potential threat to water quality in the aquifer if the pressure head in the fresh-water zone is reduced sufficiently to allow upconing of saline water. One way to avoid the problem of upconing is by steady pumping at low rates from widely spaced wells; however, information required to determine pumping rates and well spacing is not available.\r\n\r\nFor proper aquifer management the distribution of wells and rates of withdrawals should be designed to capture maximum recharge to the ground-water system. This may be accomplished by developing regional ground-water gradients that are sufficiently large to move water to pumpage centers but not so steep as to cause upconing of saline water or excessive water-level declines.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr77278","usgsCitation":"Carr, J.E., and Marcher, M.V., 1977, A preliminary appraisal of the Garber-Wellington Aquifer, southern Logan and northern Oklahoma counties, Oklahoma: U.S. Geological Survey Open-File Report 77-278, v, 23 p. :ill., maps (5 fold. in pocket) ;26 cm.; (49 p., 5 sheets - PGS), https://doi.org/10.3133/ofr77278.","productDescription":"v, 23 p. :ill., maps (5 fold. in pocket) ;26 cm.; (49 p., 5 sheets - PGS)","costCenters":[],"links":[{"id":141558,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1977/0278/report-thumb.jpg"},{"id":35843,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1977/0278/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":35844,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1977/0278/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":35845,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1977/0278/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":35846,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1977/0278/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":35847,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1977/0278/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":35848,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1977/0278/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1be4b07f02db6a9072","contributors":{"authors":[{"text":"Carr, Jerry E.","contributorId":47758,"corporation":false,"usgs":true,"family":"Carr","given":"Jerry","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":157360,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Marcher, Melvin V.","contributorId":11590,"corporation":false,"usgs":true,"family":"Marcher","given":"Melvin","email":"","middleInitial":"V.","affiliations":[],"preferred":false,"id":157359,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":42785,"text":"ofr77473 - 1977 - Preliminary simple Bouguer gravity map of northeastern Sonora, northwestern Chihuahua, and southeastern Arizona","interactions":[],"lastModifiedDate":"2021-11-17T21:13:18.959962","indexId":"ofr77473","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1977","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":"77-473","title":"Preliminary simple Bouguer gravity map of northeastern Sonora, northwestern Chihuahua, and southeastern Arizona","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr77473","usgsCitation":"Consejo de Recursos Minerales (Mexico), and Water Resources Division, U.S. Geological Survey, 1977, Preliminary simple Bouguer gravity map of northeastern Sonora, northwestern Chihuahua, and southeastern Arizona: U.S. Geological Survey Open-File Report 77-473, 1 Plate: 33.65 × 38.86 inches, https://doi.org/10.3133/ofr77473.","productDescription":"1 Plate: 33.65 × 38.86 inches","costCenters":[],"links":[{"id":135635,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":391824,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_14455.htm"},{"id":80598,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1977/0473/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"Mexico, United States","state":"Arizona, Chihuahua, Sonora","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -112,\n              29\n            ],\n            [\n              -108,\n              29\n            ],\n            [\n              -108,\n              32\n            ],\n            [\n              -112,\n              32\n            ],\n            [\n              -112,\n              29\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aace4b07f02db66a956","contributors":{"authors":[{"text":"Consejo de Recursos Minerales (Mexico)","contributorId":127909,"corporation":true,"usgs":false,"organization":"Consejo de Recursos Minerales (Mexico)","id":530939,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":530940,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":39611,"text":"pp1022A - 1977 - Assessment of increased thermal activity at Mount Baker, Washington, March 1975-March 1976","interactions":[],"lastModifiedDate":"2012-02-02T00:10:18","indexId":"pp1022A","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1977","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":"1022","chapter":"A","title":"Assessment of increased thermal activity at Mount Baker, Washington, March 1975-March 1976","docAbstract":"In March 1975 Mount Baker showed a large increase in thermal emission, which has persisted for more than 1 year. Fumarole ejecta accompanied the thermal activity from March to September, but the ejecta had no constituents that suggest a magmatic source. Estimates of that part of the total heat flux that would account for the observed snow and ice loss show that the heat-flow increase was roughly one order of magnitude, from about 2 megawatts at 10 watts per square meter, averaged over Sherman Crater before 1975, to about 30 megawatts at 180 watts per square meter, during 1975. Almost half of the glacier that occupied the basin of Sherman Crater was melted in 1975. \r\n\r\nThe new activity generated great concern among the public and the government agencies responsible for geological evaluation of potential hazards and for protection of life and property. The past geologic history, current topography, rock alteration, and location of major fumarolic activity indicate that large rock avalanches and mudflows on the east slope in Boulder Creek valley are the potential hazards of most significance related to present conditions. The most probable types of large mass movements would be mudflows, having speeds of as much as 50 kilometers per hour, that would originate from mixtures of snow, ice, and melt water and avalanches of structurally weak clay-rich rocks that make up the rim of Sherman Crater. Similar mudflows from the volcano have traveled at least 12 kilometers 8 times during the past 10,000 years. A possible worst case event, however, might be a larger, air-cushioned avalanche of as much as 20 to 30 million cubic meters that could hit Baker Lake at speeds of more than 300 kilometers per hour and generate a wave of water large enough to overtop Upper Baker Dam. \r\n\r\nAt least 30 million cubic meters of potentially unstable material occurs as hydrothermally altered remnants of the rim of Sherman Crater and could provide the required volume for the estimated worst case event or for smaller avalanches and mudflows. An earthquake, steam explosion, or eruption could provide a suitable trigger to initiate movement. Although such triggering events were possible before 1975, the probability might have been as much as 10 times greater in 1975 because of the increased thermal activity. The threat of avalanches and mudflows on Boulder Creek valley and Baker Lake prompted the closure by management agencies of the Boulder Creek drainage and of Baker Lake and its shoreline in the summer of 1975. Additionally, Baker Lake was kept below full pool at a level calculated to prevent overtopping of Upper Baker Dam by waves which could result from a worst-case avalanche. \r\n\r\nIn 1975 an interdisciplinary program of seismic, tilt, gravity, gas, hydrologic, petrologic, thermal infrared, and photographic studies by Federal and university scientists was initiated to evaluate the impact of the current thermal activity and to monitor changes that might indicate an impending eruption. By March 1976 only one small earth- quake had been identified beneath Mount Baker. Tilt and gravity changes have been observed but cannot be attributed solely to volcanic causes. The data available thus far provide no evidence of an impending eruption, but they cannot be fully interpreted without many additional geophysical and geochemical measurements, as it is not yet possible to clearly distinguish volcanic effects from non- volcanic background effects. \r\n\r\nInasmuch as current activity continues unchanged - without steam explosions, eruptions, or frequent or large earthquakes - the probability of a suitable trigger for large avalanches and mudflows should decrease and should approach that of a more average year. Such an average year would have a hazard probability at least as great as that which existed before 1975, although that level of hazard was not recognized at the time by the public or by administrative agencies. The potential hazard and the uncertainties of future activ","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/pp1022A","usgsCitation":"Frank, D., Meier, M.F., Swanson, D., with contributions by Babcock, J.W., Fretwell, M.O., Malone, S.D., Rosenfeld, C.L., Shreve, R.L., and Wilcox, R.E., 1977, Assessment of increased thermal activity at Mount Baker, Washington, March 1975-March 1976: U.S. Geological Survey Professional Paper 1022, vii, 49 p., https://doi.org/10.3133/pp1022A.","productDescription":"vii, 49 p.","temporalStart":"1975-03-01","temporalEnd":"1976-03-31","costCenters":[],"links":[{"id":120086,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/1022a/report-thumb.jpg"},{"id":67204,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/1022a/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4abae4b07f02db671f54","contributors":{"authors":[{"text":"Frank, David","contributorId":13969,"corporation":false,"usgs":true,"family":"Frank","given":"David","affiliations":[],"preferred":false,"id":221791,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Meier, Mark Frederick","contributorId":30982,"corporation":false,"usgs":true,"family":"Meier","given":"Mark","email":"","middleInitial":"Frederick","affiliations":[],"preferred":false,"id":221793,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Swanson, Donald A. 0000-0002-1680-3591","orcid":"https://orcid.org/0000-0002-1680-3591","contributorId":22303,"corporation":false,"usgs":true,"family":"Swanson","given":"Donald A.","affiliations":[],"preferred":false,"id":221792,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"with contributions by Babcock, James W.","contributorId":105596,"corporation":false,"usgs":true,"family":"with contributions by Babcock","given":"James","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":221799,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Fretwell, Marvin O.","contributorId":98999,"corporation":false,"usgs":true,"family":"Fretwell","given":"Marvin","email":"","middleInitial":"O.","affiliations":[],"preferred":false,"id":221798,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Malone, Stephen D.","contributorId":68135,"corporation":false,"usgs":true,"family":"Malone","given":"Stephen","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":221796,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Rosenfeld, Charles L.","contributorId":70249,"corporation":false,"usgs":true,"family":"Rosenfeld","given":"Charles","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":221797,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Shreve, Ronald L.","contributorId":52341,"corporation":false,"usgs":true,"family":"Shreve","given":"Ronald","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":221794,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Wilcox, Ray E.","contributorId":63074,"corporation":false,"usgs":true,"family":"Wilcox","given":"Ray","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":221795,"contributorType":{"id":1,"text":"Authors"},"rank":9}]}}
,{"id":9528,"text":"ofr77759 - 1977 - Availability of ground water on the Delmarva Peninsula","interactions":[],"lastModifiedDate":"2012-02-02T00:06:17","indexId":"ofr77759","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1977","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":"77-759","title":"Availability of ground water on the Delmarva Peninsula","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr77759","usgsCitation":"Hodges, A., 1977, Availability of ground water on the Delmarva Peninsula: U.S. Geological Survey Open-File Report 77-759, 7 leaves ;27 cm.; (6 p. - PGS), https://doi.org/10.3133/ofr77759.","productDescription":"7 leaves ;27 cm.; (6 p. - PGS)","costCenters":[],"links":[{"id":142686,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9ae4b07f02db65d802","contributors":{"authors":[{"text":"Hodges, Arthur L.","contributorId":43357,"corporation":false,"usgs":true,"family":"Hodges","given":"Arthur L.","affiliations":[],"preferred":false,"id":159838,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":27906,"text":"wri7782 - 1977 - Ground-water hydrology of the Lower Milliken-Sarco-Tulucay Creeks area, Napa County, California","interactions":[],"lastModifiedDate":"2016-05-20T11:29:09","indexId":"wri7782","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1977","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":"77-82","title":"Ground-water hydrology of the Lower Milliken-Sarco-Tulucay Creeks area, Napa County, California","docAbstract":"<p>The Sonoma Volcanics are the principal water-bearing materials in the lower Milliken-Sarco-Tulucay Creeks area, which occupies about 15 square miles (39 square kilometers) in and east of Napa, Calif. The distribution and composition of these volcanic units are highly variable and complex. Within the Sonoma Volcanics the tuffs constitute the best ground-water reservoir. They are principally pumicitic ash-flow tuffs, partly welded and moderately permeable. These tuffs extend to a depth exceeding 500 feet (150 meters), and are irregularly interbedded with clay, igneous flows, and other volcanically derived material of very low permeability which locally confine the tuffs. Recharge and movement of ground water within these tuffs are affected by the highly variable character of this rock sequence, by adjacent formations, and by tectonic features such as the Cup and Saucer ridge and the Soda Creek fault. The lithology of the area limits specific yields to about 4 percent (unconfined conditions). Specific capacities of wells average less than 3 gallons per minute per foot of drawdown (0.6 liter per second per meter) except in the most permeable areas.</p>\n<p>Annual pumpage of 3,000 acre-feet (3.7 cubic hectometers), mostly from the Sonoma tuffs, represents a significant portion of the ground-water discharge. The seasonal change in ground-water storage was about 6,600 acre-feet (8.1 cubic hectometers) in 1975. Water-level data from the area reflect the seasonal change in ground-water storage, with fluctuations of 3 to 60 feet (1 to 18 meters). The storage capacity to a depth of 500 feet (150 meters) may be as much as 196,000 acre-feet (242 cubic hectometers) in the study area, but physical and economic factors may restrict the usable capacity to about 20,000 acre-feet (25 cubic hectometers).</p>\n<p>Recharge within the area is generally inadequate to marginal under 1975 demand. There is insufficient recharge in the Milliken and Sarco Creeks area to support 1975 pumpage. Long-term changes in the seasonal peak water levels indicate an average decline of 1.5 feet per year (0.5 meter per year). By 1975 annual pumpage was not exceeding recharge in the Tulucay Creek area. Although a downward trend in water levels was noted in the western part of this basin in the late 1940's, the pumping distribution and its stress on the ground-water system have since changed, and no overall downward trend was evident in the Tulucay Creek area in 1975.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Menlo Park, CA","doi":"10.3133/wri7782","usgsCitation":"Johnson, M.J., 1977, Ground-water hydrology of the Lower Milliken-Sarco-Tulucay Creeks area, Napa County, California: U.S. Geological Survey Water-Resources Investigations Report 77-82, Report: v, 40 p.; Plate: 41.82 x 25.99 inches, https://doi.org/10.3133/wri7782.","productDescription":"Report: v, 40 p.; Plate: 41.82 x 25.99 inches","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":158646,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/wri7782.jpg"},{"id":321077,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1977/0082/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":321078,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1977/0082/plate-1.pdf","text":"Figure 3","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"California","county":"Napa 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Michael J. johnsonm@usgs.gov","contributorId":2282,"corporation":false,"usgs":true,"family":"Johnson","given":"Michael","email":"johnsonm@usgs.gov","middleInitial":"J.","affiliations":[{"id":17705,"text":"Wetland and Aquatic Research Center","active":true,"usgs":true}],"preferred":true,"id":198878,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":55412,"text":"wdrLA773 - 1977 - Water resources data for Louisiana, water year 1977, volume 3. Coastal Louisiana","interactions":[],"lastModifiedDate":"2025-05-22T18:48:53.636938","indexId":"wdrLA773","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1977","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"LA-77-3","title":"Water resources data for Louisiana, water year 1977, volume 3. Coastal Louisiana","docAbstract":"<p>Water resources data for the 1977 water year for Louisiana consist of records of stage, discharge, and water quality of streams; stage, contents, and water quality of lakes and reservoirs; and water levels and water quality of ground water. This report, in three volumes, contains discharge records for 72 gaging stations; stage records for 66 of these gaging stations; stage only for 30 gaging stations; contents for 1 reservoir; stage only for 10 lakes; water quality for 148 stations; 27 of these at gaging stations; 215 areal stations, 10 lakes, and 174 wells; and water levels for 696 observation wells. Also included are 199 crest-stage partial-record stations and flood-profile partial-record stations. Additional water data were collected at various sites, not involved in the systematic data-collection program, and are published as miscellaneous measurements. Records for a few pertinent stations in bordering States are also included in this report. These data represent that part of the National Water Data System operated by the U.S. Geological Survey and cooperating State and Federal agencies in Louisiana.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wdrLA773","collaboration":"Prepared in cooperation with the State of Louisiana and with other agencies.","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1977, Water resources data for Louisiana, water year 1977, volume 3. 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,{"id":10754,"text":"ofr77566 - 1977 - Ground-water hydrology and subsurface migration of radioisotopes at a low-level solid radioactive-waste disposal site, West Valley, New York","interactions":[{"subject":{"id":10754,"text":"ofr77566 - 1977 - Ground-water hydrology and subsurface migration of radioisotopes at a low-level solid radioactive-waste disposal site, West Valley, New York","indexId":"ofr77566","publicationYear":"1977","noYear":false,"title":"Ground-water hydrology and subsurface migration of radioisotopes at a low-level solid radioactive-waste disposal site, West Valley, New York"},"predicate":"SUPERSEDED_BY","object":{"id":38538,"text":"pp1325 - 1986 - Ground-water hydrology and subsurface migration of radionuclides at a commercial radioactive-waste burial site, West Valley, Cattaraugus County, New York","indexId":"pp1325","publicationYear":"1986","noYear":false,"title":"Ground-water hydrology and subsurface migration of radionuclides at a commercial radioactive-waste burial site, West Valley, Cattaraugus County, New York"},"id":1}],"supersededBy":{"id":38538,"text":"pp1325 - 1986 - Ground-water hydrology and subsurface migration of radionuclides at a commercial radioactive-waste burial site, West Valley, Cattaraugus County, New York","indexId":"pp1325","publicationYear":"1986","noYear":false,"title":"Ground-water hydrology and subsurface migration of radionuclides at a commercial radioactive-waste burial site, West Valley, Cattaraugus County, New York"},"lastModifiedDate":"2012-02-02T00:06:23","indexId":"ofr77566","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1977","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":"77-566","title":"Ground-water hydrology and subsurface migration of radioisotopes at a low-level solid radioactive-waste disposal site, West Valley, New York","docAbstract":"Burial trenches for disposal of solid radioactive waste at West Valley, N.Y., are excavated in till that has very low hydraulic conductivity (about 5 x 10 to the minus 8th power centimeters per second). Fractures and root tubes with chemically oxidized and (or) reduced soil in their walls extend to 3 to 4.5 meters below natural land surface. Preliminary simulations of pressure heads with a digital model suggest that hydraulic conductivity is an order of magnitude greater in the fractured till near land surface than at greater depth. Hydraulic gradients are predominantly downward, even beneath small valleys. The upper part of a body of underlying lacustrine silt is unsaturated; in the lower, saturated part, slow lateral flow may occur. In the older trenches, water began to build up in 1971, overflowed briefly in 1975, and was pumped out in 1975-76. Water levels rose abruptly during major rainstorms in mid-1975, indicating rapid infiltration through cracks in the cover material. The new trenches have maintained low, stable water levels, perhaps because of thicker, more compact cover and less waste settlement; pressure heads near these trenches are low, locally approaching zero, perhaps because of slight infiltration and limited near-surface storage. Peak tritium concentrations in test-hole cores (generally 0.00001 to 0.001 microcuries per milliliter) were found within 3 meters of land surface and are attributed to surface contamination. Concentrations declined rapidly with depth within the fractured till; secondary peaks found at about 9 meters in three holes are attributed to lateral migration from trenches. Other radioisotopes were detected only near land surface. Samples from the walls of shallow fractures revealed no accumulation of radioisotopes. (Woodard-USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr77566","usgsCitation":"Prudic, D.E., and Randall, A.D., 1977, Ground-water hydrology and subsurface migration of radioisotopes at a low-level solid radioactive-waste disposal site, West Valley, New York: U.S. Geological Survey Open-File Report 77-566, iv, 28 leaves :ill., map ;27 cm., https://doi.org/10.3133/ofr77566.","productDescription":"iv, 28 leaves :ill., map ;27 cm.","costCenters":[],"links":[{"id":143580,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1977/0566/report-thumb.jpg"},{"id":38559,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1977/0566/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aaae4b07f02db668c43","contributors":{"authors":[{"text":"Prudic, David E. deprudic@usgs.gov","contributorId":3430,"corporation":false,"usgs":true,"family":"Prudic","given":"David","email":"deprudic@usgs.gov","middleInitial":"E.","affiliations":[{"id":465,"text":"Nevada Water Science Center","active":true,"usgs":true}],"preferred":true,"id":161905,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Randall, Allan D. arandall@usgs.gov","contributorId":1168,"corporation":false,"usgs":true,"family":"Randall","given":"Allan","email":"arandall@usgs.gov","middleInitial":"D.","affiliations":[{"id":474,"text":"New York Water Science Center","active":true,"usgs":true}],"preferred":true,"id":161904,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
]}