{"pageNumber":"2053","pageRowStart":"51300","pageSize":"25","recordCount":68919,"records":[{"id":11653,"text":"ofr84449 - 1984 - Geohydrologic and drill-hole data for test well USW H-4, Yucca Mountain, Nye County, Nevada","interactions":[],"lastModifiedDate":"2012-02-02T00:06:33","indexId":"ofr84449","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":"84-449","title":"Geohydrologic and drill-hole data for test well USW H-4, Yucca Mountain, Nye County, Nevada","docAbstract":"Data are presented on drilling operations, lithology, geophysical well logs, sidewall-core samples, water-level monitoring, pumping tests, injection tests, radioactive-tracer borehole flow survey, and water chemistry for test well USW H-4. The well is one of a series of test wells drilled in the southwestern part of the Nevada Test Site, Nye County, Nevada, in cooperation with the U.S. Department of Energy. These test wells are part of the Nevada Nuclear Waste Storage Investigations to identify sites for storage of high-level radioactive wastes. Test well USW H-4 was drilled in ash-flow tuff to a total depth of 1,219 meters. Depth to water below land surface was 519 meters or at an altitude of 730 meters above sea level. After test pumping at a rate of 17.4 liters per second for approximately 9 days, the drawdown was 4.85 meters. A radioactive borehole-flow survey indicated that the Bullfrog Member was the most productive geologic unit, producing 36.5 percent of the water in the well. The second most productive geologic unit was the Tram Member, which produced 32 percent of the water. The water in test well USW H-4 is predominantly a soft, sodium bicarbonate type of water typical of water produced in tuffaceous rocks in southern Nevada. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr84449","usgsCitation":"Whitfield, M., Thordarson, W., and Eshom, E., 1984, Geohydrologic and drill-hole data for test well USW H-4, Yucca Mountain, Nye County, Nevada: U.S. Geological Survey Open-File Report 84-449, iv, 69 p. :ill., map ;28 cm., https://doi.org/10.3133/ofr84449.","productDescription":"iv, 69 p. :ill., map ;28 cm.","costCenters":[],"links":[{"id":143710,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1984/0449/report-thumb.jpg"},{"id":39510,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1984/0449/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1be4b07f02db6a8f68","contributors":{"authors":[{"text":"Whitfield, M.S.","contributorId":69547,"corporation":false,"usgs":true,"family":"Whitfield","given":"M.S.","email":"","affiliations":[],"preferred":false,"id":163512,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Thordarson, William","contributorId":23539,"corporation":false,"usgs":true,"family":"Thordarson","given":"William","email":"","affiliations":[],"preferred":false,"id":163511,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Eshom, E.P.","contributorId":83127,"corporation":false,"usgs":true,"family":"Eshom","given":"E.P.","email":"","affiliations":[],"preferred":false,"id":163513,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":55178,"text":"wdrHI831 - 1984 - Water resources data for Hawaii and other Pacific areas, water year 1983: Volume 1. Hawaii","interactions":[],"lastModifiedDate":"2025-12-02T16:24:08.295975","indexId":"wdrHI831","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"HI-83-1","title":"Water resources data for Hawaii and other Pacific areas, water year 1983: Volume 1. Hawaii","docAbstract":"<p>Water resources data for the 1983 water year for Hawaii and other Pacific Areas consist of records of stage, discharge, and water quality of streams and springs; and water levels and water quality in wells. This report, volume 1, contains discharge records for 97 gaging stations; water quality for 13 gaging stations, 92 partial-record flow stations, and 159 wells; and water levels for 24 observation wells. Also included are 108 crest-stage partial-record stations and 24 low-flow partial-record stations. Additional water data were collected at various sites, not part of the systematic data collection program, 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, Federal, and other agencies in Hawaii.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wdrHI831","collaboration":"Prepared in cooperation with the State of Hawaii Department of Land and Natural Resources, Division of Water and Land Development and with other agencies","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1984, Water resources data for Hawaii and other Pacific areas, water year 1983: Volume 1. Hawaii: U.S. Geological Survey Water Data Report HI-83-1, x, 243 p., https://doi.org/10.3133/wdrHI831.","productDescription":"x, 243 p.","costCenters":[],"links":[{"id":496988,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/1983/hi-83-1/report.pdf"},{"id":174380,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wdr/1983/hi-83-1/report-thumb.jpg"}],"country":"United 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 \"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a75e4b07f02db644a3f","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":532281,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":55530,"text":"wdrLA841 - 1984 - Water resources data, Louisiana, water year 1984","interactions":[],"lastModifiedDate":"2025-12-02T16:51:26.348549","indexId":"wdrLA841","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"LA-84-1","title":"Water resources data, Louisiana, water year 1984","docAbstract":"<p>Water resources data for the 1984 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 one volume, contains records for water discharge at 72 gaging stations (including stage for 71 of these stations); stage only for 40 gaging stations and 11 lakes; water quality for 80 surface-water stations (including 26 gaging stations), 17 miscellaneous sites, 10 lakes, and 145 wells; and water levels for 423 observation wells. Also included are data for 141 crest-stage and flood-profile partial-record stations. Additional water data were collected at various sites not involved in the systematic data-collection program, and are published as miscellaneous measurements. 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.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wdrLA841","collaboration":"Prepared in cooperation with the Louisiana Department of Transportation and Development and with other State and Federal agencies","usgsCitation":"Carlson, D., Stallworth, G., Dantin, L., and Stuart, C., 1984, Water resources data, Louisiana, water year 1984: U.S. Geological Survey Water Data Report LA-84-1, xi, 608 p., https://doi.org/10.3133/wdrLA841.","productDescription":"xi, 608 p.","costCenters":[],"links":[{"id":496994,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/1984/la-84-1/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":181503,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wdr/1984/la-84-1/report-thumb.jpg"}],"country":"United 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 \"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f6e4b07f02db5f12c8","contributors":{"authors":[{"text":"Carlson, D.D.","contributorId":10816,"corporation":false,"usgs":true,"family":"Carlson","given":"D.D.","email":"","affiliations":[],"preferred":false,"id":253651,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Stallworth, G.R.","contributorId":107732,"corporation":false,"usgs":true,"family":"Stallworth","given":"G.R.","affiliations":[],"preferred":false,"id":253654,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Dantin, L.J.","contributorId":61891,"corporation":false,"usgs":true,"family":"Dantin","given":"L.J.","email":"","affiliations":[],"preferred":false,"id":253653,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Stuart, C.G.","contributorId":58644,"corporation":false,"usgs":true,"family":"Stuart","given":"C.G.","email":"","affiliations":[],"preferred":false,"id":253652,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":27191,"text":"wri834277 - 1984 - Methods for estimating ground-water pumpage for irrigation","interactions":[],"lastModifiedDate":"2012-02-02T00:08:27","indexId":"wri834277","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":"83-4277","title":"Methods for estimating ground-water pumpage for irrigation","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri834277","usgsCitation":"Frenzel, S., 1984, Methods for estimating ground-water pumpage for irrigation: U.S. Geological Survey Water-Resources Investigations Report 83-4277, ii, 15 p. ;28 cm., https://doi.org/10.3133/wri834277.","productDescription":"ii, 15 p. ;28 cm.","costCenters":[],"links":[{"id":123251,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1983/4277/report-thumb.jpg"},{"id":56066,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1983/4277/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a51e4b07f02db62a1ee","contributors":{"authors":[{"text":"Frenzel, S.A.","contributorId":9246,"corporation":false,"usgs":true,"family":"Frenzel","given":"S.A.","email":"","affiliations":[],"preferred":false,"id":197713,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":9769,"text":"ofr84690 - 1984 - Fortran programs for properties of water and steam, and solubilities of solid silica phases","interactions":[],"lastModifiedDate":"2012-02-02T00:06:14","indexId":"ofr84690","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":"84-690","title":"Fortran programs for properties of water and steam, and solubilities of solid silica phases","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr84690","usgsCitation":"Keith, L., and Delaney, P., 1984, Fortran programs for properties of water and steam, and solubilities of solid silica phases: U.S. Geological Survey Open-File Report 84-690, iii, 62 p. ;28 cm., https://doi.org/10.3133/ofr84690.","productDescription":"iii, 62 p. ;28 cm.","costCenters":[],"links":[{"id":142200,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1984/0690/report-thumb.jpg"},{"id":37528,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1984/0690/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b23e4b07f02db6ae38a","contributors":{"authors":[{"text":"Keith, L.A.","contributorId":82309,"corporation":false,"usgs":true,"family":"Keith","given":"L.A.","email":"","affiliations":[],"preferred":false,"id":160265,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Delaney, P.T.","contributorId":69980,"corporation":false,"usgs":true,"family":"Delaney","given":"P.T.","email":"","affiliations":[],"preferred":false,"id":160264,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":2125,"text":"wsp2224 - 1984 - Quantity and quality of streamflow in the southeastern Uinta Basin, Utah and Colorado","interactions":[{"subject":{"id":10045,"text":"ofr82688 - 1982 - Quantity of quality of streamflow in the southeastern Uinta Basin, Utah and Colorado","indexId":"ofr82688","publicationYear":"1982","noYear":false,"title":"Quantity of quality of streamflow in the southeastern Uinta Basin, Utah and Colorado"},"predicate":"SUPERSEDED_BY","object":{"id":2125,"text":"wsp2224 - 1984 - Quantity and quality of streamflow in the southeastern Uinta Basin, Utah and Colorado","indexId":"wsp2224","publicationYear":"1984","noYear":false,"title":"Quantity and quality of streamflow in the southeastern Uinta Basin, Utah and Colorado"},"id":1}],"lastModifiedDate":"2017-08-31T17:24:19","indexId":"wsp2224","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2224","title":"Quantity and quality of streamflow in the southeastern Uinta Basin, Utah and Colorado","docAbstract":"<p>The southeastern Uinta Basin of Utah and Colorado includes an area of 3,000 square miles containing large oilshale deposits. Future mining and retorting of the oil shale in northeastern Utah is expected to impact the area's water resources. In order to determine premining conditions, streamflow and water-quality data were collected during 1974-79. These data plus all other available information were used to define baseline conditions for streamflow and water-quality characteristics. The data and interpretations will provide a basis for evaluating impacts of future mining.</p><p>Areal and time variances in streamflow and waterquality characteristics were determined for the major rivers (Green and White) and the intra-area streams (streams that originate within the study area). The streamflow characteristics defined are average streamflow and low- and highflow extremes. Graphs of frequency curves, duration curves, and draft-storage relations are presented for selected gaging stations. Areal variances in average and peak flows are illustrated. Water-quality characteristics are summarized according to the following categories: general waterquality characteristics, major dissolved constituents, trace elements, nutrients, pesticides, and sediment, biological, organic, and radiochemical characteristics. The means and ranges in values are discussed for the major rivers and the intra-area streams. The water-quality constituents are compared to water-quality criteria of the Environmental Protection Agency.</p><p>The major rivers flowing into the area convey an average of 5,900 cubic feet per second from a total drainage area of about 34,000 square miles. This is more than 100 times as much runoff as originates within the study area. The average flow for the major rivers is 0.17 cubic foot per second per square mile and does not vary significantly from one location to another within the study area. The flows of the intra-area streams vary from less than 0.001 to more than 0.10 cubic foot per second per square mile. Evapotranspiration losses can exceed inflow; thus average flows of some intra-area streams decrease in a downstream direction.</p><p>The quality of streamflow varies considerably between the major rivers and the intra-area streams. In the major rivers, the concentrations vary seasonally but do not vary&nbsp;significantly from one location to another. In the intra-area streams, concentrations vary both seasonally and from one location to another. The water quality in the major rivers generally is better than that in the intra-area streams. Dissolved-solids concentrations average 572 milligrams per liter for the Green River and 500 milligrams per liter for the White River, whereas mean concentrations for the intraarea streams range from 549 milligrams per liter in ephemeral streams to 5,320 milligrams per liter in Bitter Creek. Concentrations of major constituents generally do not exceed water-quality criteria of the Environmental Protection Agency except for hardness and sulfate. Several trace elements exceed water-quality criteria in intra-area streams. Dissolved-solids concentrations in base flow in short reaches of Bitter Creek can exceed 10,000 milligrams per liter. </p>","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/wsp2224","usgsCitation":"Lindskov, K., and Kimball, B.A., 1984, Quantity and quality of streamflow in the southeastern Uinta Basin, Utah and Colorado: U.S. Geological Survey Water Supply Paper 2224, vii, 72 p., https://doi.org/10.3133/wsp2224.","productDescription":"vii, 72 p.","numberOfPages":"80","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":138267,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/2224/report-thumb.jpg"},{"id":27725,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/2224/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Colorado, utah","otherGeospatial":"Uinta Basin","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a61e4b07f02db635a35","contributors":{"authors":[{"text":"Lindskov, K.L.","contributorId":91077,"corporation":false,"usgs":true,"family":"Lindskov","given":"K.L.","affiliations":[],"preferred":false,"id":144707,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kimball, Briant A. bkimball@usgs.gov","contributorId":533,"corporation":false,"usgs":true,"family":"Kimball","given":"Briant","email":"bkimball@usgs.gov","middleInitial":"A.","affiliations":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"preferred":true,"id":144706,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":27041,"text":"wri844000 - 1984 - Simulation of dynamic floodflows at gaged stations in the southeastern United States","interactions":[],"lastModifiedDate":"2012-02-02T00:08:42","indexId":"wri844000","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":"84-4000","title":"Simulation of dynamic floodflows at gaged stations in the southeastern United States","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri844000","usgsCitation":"Faye, R., and Blalock, M., 1984, Simulation of dynamic floodflows at gaged stations in the southeastern United States: U.S. Geological Survey Water-Resources Investigations Report 84-4000, vi, 114 p. :ill. ;28 cm., https://doi.org/10.3133/wri844000.","productDescription":"vi, 114 p. :ill. ;28 cm.","costCenters":[],"links":[{"id":159014,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1984/4000/report-thumb.jpg"},{"id":55922,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1984/4000/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f8e4b07f02db5f2e57","contributors":{"authors":[{"text":"Faye, R.E.","contributorId":106863,"corporation":false,"usgs":true,"family":"Faye","given":"R.E.","email":"","affiliations":[],"preferred":false,"id":197455,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Blalock, M.E.","contributorId":54254,"corporation":false,"usgs":true,"family":"Blalock","given":"M.E.","email":"","affiliations":[],"preferred":false,"id":197454,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":29841,"text":"wri844251 - 1984 - Aldicarb-pesticide contamination of ground water in eastern Suffolk County, Long Island, New York","interactions":[],"lastModifiedDate":"2012-02-02T00:09:01","indexId":"wri844251","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":"84-4251","title":"Aldicarb-pesticide contamination of ground water in eastern Suffolk County, Long Island, New York","docAbstract":"Aldicarb, a toxic oxime-carbamate pesticide that was believed incapable of reaching ground water, was used in potato-farming areas of eastern Suffolk County, New York during 1975-80. In 1979, aldicarb was found in substantial concentrations in ground water throughout the area. The New York State Department of Health set a limit of 7 micrograms per liter for aldicarb in drinking water. Extensive ground-water sampling into 1980 showed widespread contamination ranging from small amounts to as much as 515 micrograms per liter. In 1980, the U.S. Environmental Protection Agency banned the use of aldicarb on Long Island at the manufacturer 's request. A 1982 sampling study found aldicarb to have penetrated to about 40 feet below the water table in concentrations ranging from below detection limit to 239 micrograms per liter. Despite reputed toxicity, no instance of aldicarb poisoning on Long Island has been documented. The excessive aldicarb concentrations in the ground water of eastern Long Island may persist for decades; the duration has not been precisely determined and remains under investigation. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri844251","usgsCitation":"Soren, J., and Stelz, W., 1984, Aldicarb-pesticide contamination of ground water in eastern Suffolk County, Long Island, New York: U.S. Geological Survey Water-Resources Investigations Report 84-4251, vi, 40 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri844251.","productDescription":"vi, 40 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":123646,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1984/4251/report-thumb.jpg"},{"id":58648,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1984/4251/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":58649,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1984/4251/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae0e4b07f02db688006","contributors":{"authors":[{"text":"Soren, Julian","contributorId":54184,"corporation":false,"usgs":true,"family":"Soren","given":"Julian","email":"","affiliations":[],"preferred":false,"id":202224,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Stelz, W. G.","contributorId":72837,"corporation":false,"usgs":true,"family":"Stelz","given":"W. G.","affiliations":[],"preferred":false,"id":202225,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":8696,"text":"ofr84711 - 1984 - Ground-water levels in Arkansas, spring 1984","interactions":[],"lastModifiedDate":"2012-02-02T00:06:16","indexId":"ofr84711","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":"84-711","title":"Ground-water levels in Arkansas, spring 1984","docAbstract":"This report contains about 680 ground-water level measurements made in observation wells in Arkansas in the spring of 1984. In addition, the report contains well hydrographs relating to the alluvial aquifer and the Sparta Sand and Memphis Sand aquifers, the most important aquifers with respect to ground-water availability and use in Arkansas. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr84711","usgsCitation":"Edds, J., 1984, Ground-water levels in Arkansas, spring 1984: U.S. Geological Survey Open-File Report 84-711, v, 58 p. :ill. ;28 cm., https://doi.org/10.3133/ofr84711.","productDescription":"v, 58 p. :ill. ;28 cm.","costCenters":[],"links":[{"id":141775,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1984/0711/report-thumb.jpg"},{"id":36282,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1984/0711/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a6fe4b07f02db640eea","contributors":{"authors":[{"text":"Edds, Joe","contributorId":48532,"corporation":false,"usgs":true,"family":"Edds","given":"Joe","email":"","affiliations":[],"preferred":false,"id":158171,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":55249,"text":"wdrKS831 - 1984 - Water resources data, Kansas, water year 1983","interactions":[],"lastModifiedDate":"2012-02-02T00:11:51","indexId":"wdrKS831","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"KS-83-1","title":"Water resources data, Kansas, water year 1983","language":"ENGLISH","doi":"10.3133/wdrKS831","usgsCitation":"Geiger, C., Lacock, D., Shelton, L., Penny, M., and Merry, C., 1984, Water resources data, Kansas, water year 1983: U.S. Geological Survey Water Data Report KS-83-1, 483 p., https://doi.org/10.3133/wdrKS831.","productDescription":"483 p.","costCenters":[],"links":[{"id":174567,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":94541,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://hdl.handle.net/2027/mdp.39015040390570?urlappend=%3Bseq=6"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a6fe4b07f02db640d86","contributors":{"authors":[{"text":"Geiger, C.O.","contributorId":18415,"corporation":false,"usgs":true,"family":"Geiger","given":"C.O.","email":"","affiliations":[],"preferred":false,"id":253007,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lacock, D.L.","contributorId":20003,"corporation":false,"usgs":true,"family":"Lacock","given":"D.L.","email":"","affiliations":[],"preferred":false,"id":253008,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Shelton, L.R.","contributorId":12503,"corporation":false,"usgs":true,"family":"Shelton","given":"L.R.","email":"","affiliations":[],"preferred":false,"id":253006,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Penny, M.L.","contributorId":69637,"corporation":false,"usgs":true,"family":"Penny","given":"M.L.","email":"","affiliations":[],"preferred":false,"id":253010,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Merry, C.E.","contributorId":61497,"corporation":false,"usgs":true,"family":"Merry","given":"C.E.","email":"","affiliations":[],"preferred":false,"id":253009,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":11519,"text":"ofr84150 - 1984 - Drainage areas in New Jersey; Atlantic coastal basins, South Amboy to Cape May","interactions":[],"lastModifiedDate":"2012-02-02T00:06:49","indexId":"ofr84150","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":"84-150","title":"Drainage areas in New Jersey; Atlantic coastal basins, South Amboy to Cape May","docAbstract":"Drainage areas of New Jersey streams in the coastal basin from South Amboy to Cape May are listed for more than 700 sites. Tables list the descriptive location of each site, the latitude and longitude, county, and National Topographic map name. For gaged sites established through 1982, the U.S. Geological Survey station name and site number are also shown. The data are presented alphabetically by stream name and in downstream order. Drainage areas were tabulated for named streams and unnamed streams with a drainage area greater than 5 square miles. The methods used to delineate the drainage divides, measure areas, and determine mouths of streams follow the guidelines developed by the U.S. Water Resources Council. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr84150","usgsCitation":"Velnich, A., 1984, Drainage areas in New Jersey; Atlantic coastal basins, South Amboy to Cape May: U.S. Geological Survey Open-File Report 84-150, iv, 37 p. :map ;28 cm., https://doi.org/10.3133/ofr84150.","productDescription":"iv, 37 p. :map ;28 cm.","costCenters":[],"links":[{"id":146073,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1984/0150/report-thumb.jpg"},{"id":39384,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1984/0150/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a61e4b07f02db635fad","contributors":{"authors":[{"text":"Velnich, A. J.","contributorId":25149,"corporation":false,"usgs":true,"family":"Velnich","given":"A. J.","affiliations":[],"preferred":false,"id":163290,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":19494,"text":"ofr84375 - 1984 - Signature tests on 400-in3 water gun and 540-in3 air gun","interactions":[],"lastModifiedDate":"2012-02-02T00:07:29","indexId":"ofr84375","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":"84-375","title":"Signature tests on 400-in3 water gun and 540-in3 air gun","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr84375","usgsCitation":"Hutchinson, D.R., 1984, Signature tests on 400-in3 water gun and 540-in3 air gun: U.S. Geological Survey Open-File Report 84-375, 9 p. :ill. ;28 cm., https://doi.org/10.3133/ofr84375.","productDescription":"9 p. :ill. ;28 cm.","costCenters":[],"links":[{"id":151788,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1984/0375/report-thumb.jpg"},{"id":48957,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1984/0375/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49fae4b07f02db5f3d0f","contributors":{"authors":[{"text":"Hutchinson, D. R.","contributorId":31770,"corporation":false,"usgs":true,"family":"Hutchinson","given":"D.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":181006,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":25622,"text":"wri844073 - 1984 - Leaching study of oil shale in Kentucky: With a section on hydrologic reconnaissance of the oil shale outcrop in Kentucky","interactions":[],"lastModifiedDate":"2021-01-27T19:54:28.722464","indexId":"wri844073","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":"84-4073","title":"Leaching study of oil shale in Kentucky: With a section on hydrologic reconnaissance of the oil shale outcrop in Kentucky","docAbstract":"Oil shales in Kentucky are rocks of predominantly Devonian age. The most prominant are the Ohio, Chattanooga, and New Albany Shales. A leaching study was done on six fresh oil shale samples and one retorted oil shale sample. Leaching reagents were distilled water, 0.0005 N sulfuric acid, and 0.05 N sulfuric acid. The concentration of constituents in the leachates were highly variable. The concentration of sodium, manganese, and zinc in the retorted shale leachate was several orders of magnitude higher than those of the leachates of fresh shale samples. The major oil shale outcrop covers approximately 1,000 square miles in a horseshoe pattern from Vanceburg, Lewis County , in the east, to Louisville, Jefferson County, in the west. The Kentucky, Red, and Licking Rivers cross the outcrop belt, the Rolling Fork River flows along the strike of the shale in the southwest part of the outcrop, and the Ohio River flows past the outcrop at the ends of the horseshoe. Oil shale does not appear to significantly alter the water quality of these streams. Oil shale is not an aquifer, but seeps and springs found in the shale indicate that water moves through it. Ground water quality is highly variable. (USGS)","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wri844073","usgsCitation":"Leung, S.S., Leist, D., Davis, R.W., and Cordiviola, S., 1984, Leaching study of oil shale in Kentucky: With a section on hydrologic reconnaissance of the oil shale outcrop in Kentucky: U.S. Geological Survey Water-Resources Investigations Report 84-4073, Report: viii, 68 p.; 1 Plate: 26.54 x 26.30 inches, https://doi.org/10.3133/wri844073.","productDescription":"Report: viii, 68 p.; 1 Plate: 26.54 x 26.30 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,{"id":41515,"text":"ofr84205 - 1984 - Aeromagnetic map of southwest Washington and northwest Oregon","interactions":[],"lastModifiedDate":"2022-08-17T18:50:49.375651","indexId":"ofr84205","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":"84-205","title":"Aeromagnetic map of southwest Washington and northwest Oregon","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr84205","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1984, Aeromagnetic map of southwest Washington and northwest Oregon: U.S. Geological Survey Open-File Report 84-205, 1 Plate: 18.74 × 22.24 inches, https://doi.org/10.3133/ofr84205.","productDescription":"1 Plate: 18.74 × 22.24 inches","costCenters":[],"links":[{"id":170995,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":405268,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_13307.htm","linkFileType":{"id":5,"text":"html"}},{"id":79241,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1984/0205/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Oregon, Washington","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -124.7110,\n              45.808\n            ],\n            [\n              -123.4544,\n              45.808\n            ],\n            [\n              -123.4544,\n              46.5089\n            ],\n            [\n              -124.7110,\n              46.5089\n            ],\n            [\n              -124.7110,\n              45.808\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b00e4b07f02db6980fc","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":530443,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":47190,"text":"ofr8452 - 1984 - Flow characteristics of the Snake River and water budget for the Snake River plain, Idaho and eastern Oregon","interactions":[{"subject":{"id":47190,"text":"ofr8452 - 1984 - Flow characteristics of the Snake River and water budget for the Snake River plain, Idaho and eastern Oregon","indexId":"ofr8452","publicationYear":"1984","noYear":false,"title":"Flow characteristics of the Snake River and water budget for the Snake River plain, Idaho and eastern Oregon"},"predicate":"SUPERSEDED_BY","object":{"id":68263,"text":"ha680 - 1986 - Flow characteristics of the Snake River and water budget for the Snake River Plain, Idaho and eastern Oregon","indexId":"ha680","publicationYear":"1986","noYear":false,"title":"Flow characteristics of the Snake River and water budget for the Snake River Plain, Idaho and eastern Oregon"},"id":1}],"supersededBy":{"id":68263,"text":"ha680 - 1986 - Flow characteristics of the Snake River and water budget for the Snake River Plain, Idaho and eastern Oregon","indexId":"ha680","publicationYear":"1986","noYear":false,"title":"Flow characteristics of the Snake River and water budget for the Snake River Plain, Idaho and eastern Oregon"},"lastModifiedDate":"2022-04-27T18:12:32.179177","indexId":"ofr8452","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":"84-52","title":"Flow characteristics of the Snake River and water budget for the Snake River plain, Idaho and eastern Oregon","docAbstract":"<p>This report is one in a series resulting from the U.S. Geological Survey's Snake River Plain Rasa (Regional Aquifer System Analysis) study that was initiation in October 1979.&nbsp;</p><p>Purposes of the RASA study were to (1) refine knowledge of the regional ground-water flow system, (2) determine effects of conjunctive use of ground water and surface water, and (3) describe water chemistry. This purpose of this report is to describe flow characteristics of the Snake River and tributaries and to develop a water budget for the Snake River Plain. Data and interpretation in this report will be used in development of ground-water flow models.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr8452","usgsCitation":"Kjelstrom, L., 1984, Flow characteristics of the Snake River and water budget for the Snake River plain, Idaho and eastern Oregon: U.S. Geological Survey Open-File Report 84-52, 2 Plates: 50.67 x 38.09 inches and 41.32 x 30.24 inches, https://doi.org/10.3133/ofr8452.","productDescription":"2 Plates: 50.67 x 38.09 inches and 41.32 x 30.24 inches","costCenters":[],"links":[{"id":399778,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1984/0052/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":399777,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1984/0052/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":135235,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1984/0052/report-thumb.jpg"}],"scale":"500000","country":"United States","state":"Idaho, Oregon","otherGeospatial":"Snake River plain","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -117.1142578125,\n              44.5278427984555\n            ],\n            [\n              -117.46582031249999,\n              44.276671273775186\n            ],\n            [\n              -117.57568359374999,\n              43.77109381775651\n            ],\n            [\n              -116.8505859375,\n              43.27720532212024\n            ],\n            [\n              -116.4111328125,\n              42.924251753870685\n            ],\n            [\n              -115.29052734375,\n              42.4234565179383\n            ],\n            [\n              -114.2578125,\n              42.342305278572816\n            ],\n            [\n              -112.8955078125,\n              42.61779143282346\n            ],\n            [\n              -112.4560546875,\n              43.197167282501276\n            ],\n            [\n              -111.7529296875,\n              43.644025847699496\n            ],\n            [\n              -111.4892578125,\n              44.213709909702054\n            ],\n            [\n              -111.4892578125,\n              44.32384807250689\n            ],\n            [\n              -111.884765625,\n              44.74673324024678\n            ],\n            [\n              -112.52197265625,\n              44.62175409623324\n            ],\n            [\n              -112.8515625,\n              44.276671273775186\n            ],\n            [\n              -113.64257812499999,\n              43.51668853502906\n            ],\n            [\n              -114.12597656249999,\n              43.51668853502906\n            ],\n            [\n              -114.9169921875,\n              43.56447158721811\n            ],\n            [\n              -115.3564453125,\n              43.59630591596548\n            ],\n            [\n              -115.90576171874999,\n              43.67581809328341\n            ],\n            [\n              -116.1474609375,\n              44.10336537791152\n            ],\n            [\n              -116.03759765625,\n              44.37098696297173\n            ],\n            [\n              -116.3232421875,\n              44.824708282300236\n            ],\n            [\n              -116.71874999999999,\n              44.74673324024678\n            ],\n            [\n              -117.1142578125,\n              44.5278427984555\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49d8e4b07f02db5defef","contributors":{"authors":[{"text":"Kjelstrom, L.C.","contributorId":89104,"corporation":false,"usgs":true,"family":"Kjelstrom","given":"L.C.","email":"","affiliations":[],"preferred":false,"id":234796,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":15469,"text":"ofr84818 - 1984 - Land subsidence in the Santa Clara Valley, California as of 1980","interactions":[{"subject":{"id":15469,"text":"ofr84818 - 1984 - Land subsidence in the Santa Clara Valley, California as of 1980","indexId":"ofr84818","publicationYear":"1984","noYear":false,"title":"Land subsidence in the Santa Clara Valley, California as of 1980"},"predicate":"SUPERSEDED_BY","object":{"id":38874,"text":"pp497F - 1988 - Land subsidence in the Santa Clara Valley, California, as of 1982","indexId":"pp497F","publicationYear":"1988","noYear":false,"chapter":"F","title":"Land subsidence in the Santa Clara Valley, California, as of 1982"},"id":1}],"supersededBy":{"id":38874,"text":"pp497F - 1988 - Land subsidence in the Santa Clara Valley, California, as of 1982","indexId":"pp497F","publicationYear":"1988","noYear":false,"title":"Land subsidence in the Santa Clara Valley, California, as of 1982"},"lastModifiedDate":"2019-08-29T10:12:02","indexId":"ofr84818","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":"84-818","title":"Land subsidence in the Santa Clara Valley, California as of 1980","docAbstract":"From 1916 to 1966 in the San Jose area of Santa Clara Valley, California, deficient rainfall and runoff was accompanied by a fourfold increase in groundwater withdrawals. In response the artesian head declined 180-240 ft. The land surface subsided 12.7 ft in San Jose, due to compaction of the fine-grained compressible beds. The subsidence resulted in flooding of lands, and the compaction of the sediments caused compressional failure of many well casings. From 1967 to 1975, the artesian head recovered 70 to 100 feet due to a fivefold increase in surface water imports, favorable local water supply, decreased withdrawal, and increased recharge. In 1960, the Geological Survey installed extensometers in core holes 1,000 ft deep in San Jose and Sunnyvale. Measurements of compaction of the confined aquifer system obtained from these extensometers demonstrate the marked decrease in rate of compaction in response to the major head recovery since 1967. In San Jose the rate decreased from about 1 ft/yr in 1961 to 0.1 ft/yr in 1973. The subsidence has been stopped by raising the artesian head in the aquifers until it equaled or exceeded the maximum pore pressures in the fine-grained beds. However, the subsidence will recommence if the artesian head is drawn down appreciably below the levels of 1971-73. (USGS)","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr84818","usgsCitation":"Poland, J.F., and Ireland, R.L., 1984, Land subsidence in the Santa Clara Valley, California as of 1980: U.S. Geological Survey Open-File Report 84-818, vi, 93 p. , https://doi.org/10.3133/ofr84818.","productDescription":"vi, 93 p. ","costCenters":[],"links":[{"id":147961,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1984/0818/report-thumb.jpg"},{"id":367074,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1984/0818/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"California","otherGeospatial":"Santa Clara Valley","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -122.420654296875,\n              36.97183825093165\n            ],\n            [\n              -121.40991210937499,\n              36.97183825093165\n            ],\n            [\n              -121.40991210937499,\n              37.58811876638322\n            ],\n            [\n              -122.420654296875,\n              37.58811876638322\n            ],\n            [\n              -122.420654296875,\n              36.97183825093165\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b24e4b07f02db6ae9aa","contributors":{"authors":[{"text":"Poland, J. F.","contributorId":64223,"corporation":false,"usgs":true,"family":"Poland","given":"J.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":171181,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ireland, R. L.","contributorId":89893,"corporation":false,"usgs":true,"family":"Ireland","given":"R.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":171182,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":46865,"text":"ofr8451 - 1984 - Geohydrologic framework of the Snake River plain, Idaho and eastern Oregon","interactions":[{"subject":{"id":46865,"text":"ofr8451 - 1984 - Geohydrologic framework of the Snake River plain, Idaho and eastern Oregon","indexId":"ofr8451","publicationYear":"1984","noYear":false,"title":"Geohydrologic framework of the Snake River plain, Idaho and eastern Oregon"},"predicate":"SUPERSEDED_BY","object":{"id":67933,"text":"ha681 - 1986 - Geohydrologic framework of the Snake River Plain, Idaho and eastern Oregon","indexId":"ha681","publicationYear":"1986","noYear":false,"title":"Geohydrologic framework of the Snake River Plain, Idaho and eastern Oregon"},"id":1}],"supersededBy":{"id":67933,"text":"ha681 - 1986 - Geohydrologic framework of the Snake River Plain, Idaho and eastern Oregon","indexId":"ha681","publicationYear":"1986","noYear":false,"title":"Geohydrologic framework of the Snake River Plain, Idaho and eastern Oregon"},"lastModifiedDate":"2022-04-21T20:46:02.999936","indexId":"ofr8451","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":"84-51","title":"Geohydrologic framework of the Snake River plain, Idaho and eastern Oregon","docAbstract":"<p>This report is one in a series resulting from the U.S. Geological Survey's Snake River Plain RASA (Regional Aquifer System Analysis) study that was initiated in October 1979.&nbsp;</p><p>As stated by Lindholm (1981), the purpose of the study was to (1) refine knowledge of the regional ground-water flow system, (2) determine effects of conjunctive use of ground and surface water, and (3) describe water chemistry.</p><p>The purpose of this report is to summarize knowledge concerning the geohydrologic framework of the Snake River Plain. Definition of the framework is based on preexisting geologic and hydrologic data and new date collected during this study.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr8451","usgsCitation":"Whitehead, R., 1984, Geohydrologic framework of the Snake River plain, Idaho and eastern Oregon: U.S. Geological Survey Open-File Report 84-51, 3 Plates: 44:45 x 28.07 inches or smaller, https://doi.org/10.3133/ofr8451.","productDescription":"3 Plates: 44:45 x 28.07 inches or smaller","costCenters":[],"links":[{"id":172258,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1984/0051/report-thumb.jpg"},{"id":399460,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1984/0051/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":399459,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1984/0051/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":399458,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1984/0051/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"500000","country":"United States","state":"Idaho, Oregon","otherGeospatial":"Snake River plain","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -117.1142578125,\n              44.5278427984555\n            ],\n            [\n              -117.46582031249999,\n              44.276671273775186\n            ],\n            [\n              -117.57568359374999,\n              43.77109381775651\n            ],\n            [\n              -116.8505859375,\n              43.27720532212024\n            ],\n            [\n              -116.4111328125,\n              42.924251753870685\n            ],\n            [\n              -115.29052734375,\n              42.4234565179383\n            ],\n            [\n              -114.2578125,\n              42.342305278572816\n            ],\n            [\n              -112.8955078125,\n              42.61779143282346\n            ],\n            [\n              -112.4560546875,\n              43.197167282501276\n            ],\n            [\n              -111.7529296875,\n              43.644025847699496\n            ],\n            [\n              -111.4892578125,\n              44.213709909702054\n            ],\n            [\n              -111.4892578125,\n              44.32384807250689\n            ],\n            [\n              -111.884765625,\n              44.74673324024678\n            ],\n            [\n              -112.52197265625,\n              44.62175409623324\n            ],\n            [\n              -112.8515625,\n              44.276671273775186\n            ],\n            [\n              -113.64257812499999,\n              43.51668853502906\n            ],\n            [\n              -114.12597656249999,\n              43.51668853502906\n            ],\n            [\n              -114.9169921875,\n              43.56447158721811\n            ],\n            [\n              -115.3564453125,\n              43.59630591596548\n            ],\n            [\n              -115.90576171874999,\n              43.67581809328341\n            ],\n            [\n              -116.1474609375,\n              44.10336537791152\n            ],\n            [\n              -116.03759765625,\n              44.37098696297173\n            ],\n            [\n              -116.3232421875,\n              44.824708282300236\n            ],\n            [\n              -116.71874999999999,\n              44.74673324024678\n            ],\n            [\n              -117.1142578125,\n              44.5278427984555\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1be4b07f02db6a8e6e","contributors":{"authors":[{"text":"Whitehead, R.L.","contributorId":34891,"corporation":false,"usgs":true,"family":"Whitehead","given":"R.L.","email":"","affiliations":[],"preferred":false,"id":234225,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":16692,"text":"ofr84730 - 1984 - Hydrogeologic framework of the New Jersey coastal plain","interactions":[{"subject":{"id":16692,"text":"ofr84730 - 1984 - Hydrogeologic framework of the New Jersey coastal plain","indexId":"ofr84730","publicationYear":"1984","noYear":false,"title":"Hydrogeologic framework of the New Jersey coastal plain"},"predicate":"SUPERSEDED_BY","object":{"id":38435,"text":"pp1404B - 1989 - Hydrogeologic framework of the New Jersey Coastal Plain","indexId":"pp1404B","publicationYear":"1989","noYear":false,"chapter":"B","title":"Hydrogeologic framework of the New Jersey Coastal Plain"},"id":1}],"supersededBy":{"id":38435,"text":"pp1404B - 1989 - Hydrogeologic framework of the New Jersey Coastal Plain","indexId":"pp1404B","publicationYear":"1989","noYear":false,"title":"Hydrogeologic framework of the New Jersey Coastal Plain"},"lastModifiedDate":"2021-03-04T21:45:15.274818","indexId":"ofr84730","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":"84-730","title":"Hydrogeologic framework of the New Jersey coastal plain","docAbstract":"<p>Results are presented of a water-resources-oriented subsurface mapping program within the Coastal Plain of New Jersey. The occurrence and configuration of 15 regional hydrogeologic units are defined based primarily on the interpretation of borehole geophysical data. The nine aquifers and six confining beds are composed of unconsolidated clay, silt, sand, and gravel and range in age from Cretaceous to Quaternary. </p><p>Electric and gamma-ray logs from more than 1,000 Coastal Plain wells were examined. Of these, interpretive data for 302 sites, selected for log depth, quality, and distribution, were used to prepare structure contour and thickness maps for each aquifer, and a thickness map for each confining bed. These maps, along with 14 hydrogeologic sections, show the geometry, lateral extent, and vertical and horizontal relationships among the 15 hydrogeologic units. </p><p><span>The hydrogeologic maps and sections show that distinct </span><span>lower, middle, and upper aquifers are present within the Potomac-</span><span>Raritan-Magothy aquifer system near the Delaware River from </span><span>Burlington County to Salem County. Although the lower aquifer is </span><span>recognized only in this area, the middle aquifer extends into the </span><span>northeastern Coastal Plain of New Jersey where it is stratigraph</span><span>ically equivalent to the Farrington aquifer. The upper aquifer </span><span>extends throughout most of the New Jersey Coastal Plain and is </span><span>stratigraphically equivalent to the Old Bridge aquifer in the </span><span>northeastern Coastal Plain. The overlying Merchantville-Woodbury </span><span>confining bed is the most regionally extensive confining bed </span><span>within the Coastal Plain of New Jersey. Its thickness ranges from </span><span>less than 100 feet near the outcrop to more than 450 feet along </span><span>the coast. </span><span>The Englishtown aquifer system acts as a single aquifer throughout most of its subsurface extent, but contains two water-bearing sands in parts of Monmouth and Ocean Counties. The overlying Marshalltown-Wenonah confining bed is a thin, leaky unit ranging in thickness from approximately 20 to 80 feet. The Wenonah-Mount Laurel aquifer is identified in the subsurface throughout the New Jersey Coastal Plain southeast of its outcrop area. </span></p><p><span>Sediments that overlie the Wenonah-Mount Laurel aquifer and </span><span>that are subjacent to the major aquifers within the Kirkwood </span><span>Formation and Cohansey Sand are described hydrologically as a </span><span>composite confining bed. </span><span>These include the Navesink Formation, </span><span>Red Bank Sand, Tinton Sand, Hornerstown Sand, Vincentown Forma-</span><span>tion, Manasquan Formation, Shark River Formation, Piney Point </span><span>Formation, and the basal clay of the Kirkwood Formation. </span><span>The </span><span>Vincentown Formation functions as an aquifer within 3 to 10 miles </span><span>downdip of its outcrop area. </span><span>In areas farther downdip the </span><span>Vincentown Formation functions as a confining bed. The Piney </span><span>Point aquifer is laterally persistent from the southern New Jersey </span><span>Coastal Plain northward into parts of Burlington and Ocean </span><span>Counties. The Atlantic City 800-foot sand of the Kirkwood </span><span>Formation can be recognized in the subsurface along coastal areas </span><span>of Cape May, Atlantic, and southern Ocean Counties, but inland </span><span>only as far west as the extent of the overlying confining bed. In </span><span>areas west of the extent of the overlying confining bed, the </span><span>Kirkwood Formation is in hydraulic connection with the overlying </span><span>Cohansey Sand and younger surficial deposits and functions as an </span><span>unconfined aquifer. </span>(USGS)</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr84730","usgsCitation":"Zapecza, O., 1984, Hydrogeologic framework of the New Jersey coastal plain: U.S. Geological Survey Open-File Report 84-730, Report: vi, 61 p.; 24 Plates: 41.22 x 31.58 inches or smaller, https://doi.org/10.3133/ofr84730.","productDescription":"Report: vi, 61 p.; 24 Plates: 41.22 x 31.58 inches or 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,{"id":26314,"text":"wri834121A - 1984 - Maps showing ground-water units and withdrawal, Basin and Range Province, Texas","interactions":[],"lastModifiedDate":"2016-08-22T11:36:07","indexId":"wri834121A","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":"83-4121","chapter":"A","title":"Maps showing ground-water units and withdrawal, Basin and Range Province, Texas","docAbstract":"<p>This report on ground-water units and withdrawal in the Basin and Range province of Texas (see index map) was prepared as part of a program of the U.S. Geological Survey to identify prospective regions for further study relative to isolation of high-level nuclear waste (Bedinger, Sargent, and Reed, 1984), utilizing program guidelines defined in Sargent and Bedinger (1984). Also included in this report are selected references on pertinent geologic and hydrologic studies of the region. Other map reports in this series contain detailed data on ground-water quality, surface distribution of selected rock types, tectonic conditions, areal geophysics, Pleistocene lakes and marshes, and mineral and energy resources.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri834121A","usgsCitation":"Brady, B.T., Bedinger, M.S., and Mikels, J., 1984, Maps showing ground-water units and withdrawal, Basin and Range Province, Texas: U.S. Geological Survey Water-Resources Investigations Report 83-4121, 6 p., https://doi.org/10.3133/wri834121A.","productDescription":"6 p.","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":55112,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1983/4121a/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":55113,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1983/4121a/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":118754,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1983/4121a/report-thumb.jpg"}],"country":"United States","state":"Texas","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a19e4b07f02db605aa4","contributors":{"authors":[{"text":"Brady, B. T.","contributorId":93047,"corporation":false,"usgs":true,"family":"Brady","given":"B.","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":196159,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bedinger, M. S.","contributorId":65452,"corporation":false,"usgs":true,"family":"Bedinger","given":"M.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":196158,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Mikels, John","contributorId":24817,"corporation":false,"usgs":true,"family":"Mikels","given":"John","email":"","affiliations":[],"preferred":false,"id":196157,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":45824,"text":"ofr84589 - 1984 - Linear features determined from Landsat imagery in the Texas and Oklahoma panhandles","interactions":[],"lastModifiedDate":"2012-02-02T00:04:59","indexId":"ofr84589","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":"84-589","title":"Linear features determined from Landsat imagery in the Texas and Oklahoma panhandles","docAbstract":"A map (scale 1:500,000) shows the linear features determined from Landsat imagery in the Texas and Oklahoma panhandles. The linear features, sometimes called linear trends or lineaments, are not identified as to type or origin. Most probably represent fractures or fracture zones, which may affect the movement of water or other fluids through rocks. The linear features are classified as to length--less than 30 mi/mg and more than 30 mi/mg. (USGS)","language":"ENGLISH","doi":"10.3133/ofr84589","usgsCitation":"Cooley, M.E., 1984, Linear features determined from Landsat imagery in the Texas and Oklahoma panhandles: U.S. Geological Survey Open-File Report 84-589, 1 map :photocopy ;80 x 56 cm., on sheet 98 x 83 cm., https://doi.org/10.3133/ofr84589.","productDescription":"1 map :photocopy ;80 x 56 cm., on sheet 98 x 83 cm.","costCenters":[],"links":[{"id":135881,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":82801,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1984/0589/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b15e4b07f02db6a4bd1","contributors":{"authors":[{"text":"Cooley, M. E.","contributorId":89868,"corporation":false,"usgs":true,"family":"Cooley","given":"M.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":232081,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":45715,"text":"pp1292AB - 1984 - Geology, geochemistry, and age of Archean and Early Proterozoic rocks in the Marenisco-Watersmeet area, northern Michigan; and Geologic interpretation of gravity data, Marenisco-Watersmeet area, northern Michigan","interactions":[],"lastModifiedDate":"2022-06-10T19:47:05.247792","indexId":"pp1292AB","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":"1292","chapter":"A,B","title":"Geology, geochemistry, and age of Archean and Early Proterozoic rocks in the Marenisco-Watersmeet area, northern Michigan; and Geologic interpretation of gravity data, Marenisco-Watersmeet area, northern Michigan","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/pp1292AB","usgsCitation":"Sims, P., Peterman, Z.E., Prinz, W.C., Benedict, F.C., and Klasner, J.S., 1984, Geology, geochemistry, and age of Archean and Early Proterozoic rocks in the Marenisco-Watersmeet area, northern Michigan; and Geologic interpretation of gravity data, Marenisco-Watersmeet area, northern Michigan: U.S. Geological Survey Professional Paper 1292, 68 p., https://doi.org/10.3133/pp1292AB.","productDescription":"68 p.","costCenters":[],"links":[{"id":82299,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/1292a-b/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":135174,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/1292a-b/report-thumb.jpg"},{"id":402068,"rank":2,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_4789.htm","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Michigan","otherGeospatial":"Marenisco-Watersmeet area","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -89.75,\n              46.25\n            ],\n            [\n              -89.0339,\n              46.25\n            ],\n            [\n              -89.0339,\n              46.5\n            ],\n            [\n              -89.75,\n              46.5\n            ],\n            [\n              -89.75,\n              46.25\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67c697","contributors":{"authors":[{"text":"Sims, P.K.","contributorId":30191,"corporation":false,"usgs":true,"family":"Sims","given":"P.K.","email":"","affiliations":[],"preferred":false,"id":231896,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Peterman, Z. E.","contributorId":63781,"corporation":false,"usgs":true,"family":"Peterman","given":"Z.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":231897,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Prinz, W. C.","contributorId":82670,"corporation":false,"usgs":true,"family":"Prinz","given":"W.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":231899,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Benedict, F. C.","contributorId":97068,"corporation":false,"usgs":true,"family":"Benedict","given":"F.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":231900,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Klasner, J. S.","contributorId":66228,"corporation":false,"usgs":true,"family":"Klasner","given":"J.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":231898,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":45713,"text":"pp1273D - 1984 - Apparent water resistivity, porosity, and water temperature of the Madison Limestone and underlying rocks in parts of Montana, Nebraska, North Dakota, South Dakota, and Wyoming","interactions":[{"subject":{"id":41885,"text":"ofr81629 - 1981 - Apparent water resistivity, porosity, and ground-water temperature of the Madison limestone and underlying rocks in parts of Montana, Nebraska, North Dakota, South Dakota, and Wyoming","indexId":"ofr81629","publicationYear":"1981","noYear":false,"title":"Apparent water resistivity, porosity, and ground-water temperature of the Madison limestone and underlying rocks in parts of Montana, Nebraska, North Dakota, South Dakota, and Wyoming"},"predicate":"SUPERSEDED_BY","object":{"id":45713,"text":"pp1273D - 1984 - Apparent water resistivity, porosity, and water temperature of the Madison Limestone and underlying rocks in parts of Montana, Nebraska, North Dakota, South Dakota, and Wyoming","indexId":"pp1273D","publicationYear":"1984","noYear":false,"chapter":"D","title":"Apparent water resistivity, porosity, and water temperature of the Madison Limestone and underlying rocks in parts of Montana, Nebraska, North Dakota, South Dakota, and Wyoming"},"id":1}],"lastModifiedDate":"2012-02-02T00:04:56","indexId":"pp1273D","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":"1273","chapter":"D","title":"Apparent water resistivity, porosity, and water temperature of the Madison Limestone and underlying rocks in parts of Montana, Nebraska, North Dakota, South Dakota, and Wyoming","language":"ENGLISH","doi":"10.3133/pp1273D","usgsCitation":"MacCary, L., 1984, Apparent water resistivity, porosity, and water temperature of the Madison Limestone and underlying rocks in parts of Montana, Nebraska, North Dakota, South Dakota, and Wyoming: U.S. Geological Survey Professional Paper 1273, p. 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,{"id":57601,"text":"wdrFL831A - 1984 - Water resources data, Florida, water year 1983; Volume 1A. Northeast Florida surface water","interactions":[],"lastModifiedDate":"2023-01-10T20:01:46.306699","indexId":"wdrFL831A","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"FL-83-1A","title":"Water resources data, Florida, water year 1983; Volume 1A. Northeast Florida surface water","docAbstract":"<p>Water resources data for the 1983 water year for northeast Florida consist of records of stage, discharge, and water quality of streams; elevation and water quality of lakes and reservoirs; and discharge and water quality of springs. Records of water levels and water quality of wells are in volume 1B. 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 in Florida.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wdrFL831A","collaboration":"Prepared in cooperation with the State of Florida and with other agencies","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1984, Water resources data, Florida, water year 1983; Volume 1A. 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,{"id":19592,"text":"ofr836 - 1984 - Engineering geology studies in the National Petroleum Reserve, Alaska","interactions":[],"lastModifiedDate":"2012-02-02T00:07:29","indexId":"ofr836","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":"83-6","title":"Engineering geology studies in the National Petroleum Reserve, Alaska","docAbstract":"Engineering geology studies were conducted in direct support of the exploration program in the National Petroleum Reserve, Alaska. The studies included laboratory and field tests and observations to address design and construction problems of airfields, roads, drill pads and foundations, and to evaluate their actual performance. Permafrost containing large amounts of near surface ground ice as wedges, masses, and intergranular ice, required that all construction activity not disturb the thermal regime of the ground surface, which could lead to thaw of permafrost and ground subsidence. Summer activity, therefore was not allowable, yet the winter climate was so harsh that winter work was slow and inefficient. To allow summer operations at well sites planned for all year activity, it was necessary to adapt existing techniques for arctic construction and to devise new ones. \r\n\r\nThe design and construction of facilities at the deep exploration wells at Inigok, Tunalik, and Lisburne posed the greatest challenge. These sites, requiring a year or more to drill, could only be attempted if continuous access to drilling and logistic supplies could be assured throughout the year, including the possibility of bringing in another drill rig, in the event of a blowout. Thus all-seasons airstrips were required at these wells. Sufficient quantities of local gravel were not readily available at the Inigok and Tunalik sites to construct the airstrips with the required 6 feet or more of gravel to prevent the underlying permafrost from thawing. Therefore, insulation was used to maintain the subbase of local sands in a continuously frozen state, which in turn was overlain by 15 inches of gravel or sandy gravel. Tests at the U.S. Army Waterways Experimental Station defined the minimum thickness of gravel required above the insulation to provide the desired bearing capacity for the C-130 type aircraft without crushing the insulation. \r\n\r\nField testing also included the evaluation of another design option, using military landing mat underlain by insulation. Temperature recording devices were installed beneath the landing mat test sections, insulated runways, roads, drill pads, and reserve pits, to monitor the actual conditions and confirm the design assumptions. Investigations of thaw-settlement, erosion, and revegetation of all areas affected by construction were also conducted in anticipation of abandoning the sites, or, upgrading the facilities in the event the design life was extended.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr836","usgsCitation":"Kachadoorian, R., and Crory, F., 1984, Engineering geology studies in the National Petroleum Reserve, Alaska: U.S. Geological Survey Open-File Report 83-6, i, 37 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr836.","productDescription":"i, 37 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":151952,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0006/report-thumb.jpg"},{"id":49061,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0006/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a14e4b07f02db60271a","contributors":{"authors":[{"text":"Kachadoorian, Reuben","contributorId":24336,"corporation":false,"usgs":true,"family":"Kachadoorian","given":"Reuben","email":"","affiliations":[],"preferred":false,"id":181177,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Crory, F.E.","contributorId":45734,"corporation":false,"usgs":true,"family":"Crory","given":"F.E.","email":"","affiliations":[],"preferred":false,"id":181178,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":45980,"text":"ofr84705 - 1984 - Low-Flow Characteristics of Kentucky Streams, 1984","interactions":[],"lastModifiedDate":"2012-02-10T00:10:09","indexId":"ofr84705","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":"84-705","title":"Low-Flow Characteristics of Kentucky Streams, 1984","docAbstract":"INTRODUCTION\r\n\r\nThe U. S. Geologlcal Survey has been gathering low-flow data on streams throughout Kentucky for many years. This report presents low-flow characteristics at gaged and ungaged sites where the flow is not significantly regulated. Data on avai1able streamflow during low-flow periods are used for the design of plants that dispose of waste using di1ution procedures, to estimate avai1able industrial and municipal water supplies, to estimate irrigation supplies, and in the design of recreational faci1ities.\r\n\r\nThis preliminary report presents low-flow data at 84 continuous-record sites and the 7-day 2-year and 7-day 10-year flow only at 203 partial-record sites. The station identifier, 7-day 10-year dlscharge in cubic feet per second (ft3/s), and the drainage area in square mi1es (mi2 ) are shown on the map. Other data are shown in tabular form. Low-flow characteristics previously published by Swisshelm (1974) and Sullavan (1980) have been combined and included in this report for reference purposes.","language":"ENGLISH","publisher":"Geological Survey (U.S.)","doi":"10.3133/ofr84705","collaboration":"Prepared in cooperation with the U.S. Army Corps of Engineers","usgsCitation":"Sullavan, J.N., 1984, Low-Flow Characteristics of Kentucky Streams, 1984: U.S. Geological Survey Open-File Report 84-705, 2 p., 1 Map, https://doi.org/10.3133/ofr84705.","productDescription":"2 p., 1 Map","costCenters":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"links":[{"id":162256,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1984/0705/report-thumb.jpg"},{"id":82958,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1984/0705/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -90,36.5 ], [ -90,39 ], [ -82,39 ], [ -82,36.5 ], [ -90,36.5 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a82e4b07f02db64b026","contributors":{"authors":[{"text":"Sullavan, John N.","contributorId":70448,"corporation":false,"usgs":true,"family":"Sullavan","given":"John","email":"","middleInitial":"N.","affiliations":[],"preferred":false,"id":232396,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
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