{"pageNumber":"1732","pageRowStart":"43275","pageSize":"25","recordCount":68937,"records":[{"id":17244,"text":"ofr9267 - 1992 - Hydrologic data for the Big Spring basin, Clayton County, Iowa, water year 1990","interactions":[],"lastModifiedDate":"2016-03-11T15:56:38","indexId":"ofr9267","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1992","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":"92-67","title":"Hydrologic data for the Big Spring basin, Clayton County, Iowa, water year 1990","docAbstract":"<p>Hydrologic data were collected in the Big Spring basin located in Clayton County, Iowa, during the 1990 water year. The data were collected by the U.S. Geological Survey in cooperation with the Iowa Department of Natural Resources, Geological Survey Bureau, to provide information on variation and movement of agricultural chemicals in the hydrologic cycle in the basin. Precipitation, surface-water, and ground-water data were collected.</p>\n<p>Rainfall recorded during water year 1990 at a monitoring site on Roberts Creek totaled 43.67 inches. The greatest monthly rainfall (14.45 inches) occurred in August. Calcium and sulfate were the predominant ions in the rain, and the median concentrations of nitrate and ammonia as nitrogen were 0.35 and 0.48 milligrams per liter, respectively.</p>\n<p>Stream discharge, specific conductance, pH, and water temperature were monitored continuously, and monthly water-quality samples were collected at three sites in the basin. The predominant ions in samples from Roberts Creek at the point where it leaves the basin were calcium, magnesium, and bicarbonate. Nitrite plus nitrate as nitrogen concentrations in 42 samples ranged from less than 0.10 to 18 milligrams per liter. Pesticide concentrations in 34 samples ranged from less than 0.10 to 12 micrograms per liter. Alachlor was detected in 56 percent of the samples; atrazine in 100 percent; cyanazine in 68 percent; and metolachlor in 47 percent.</p>\n<p>At Big Spring, the ground-water discharge point, the daily mean specific conductance ranged from 378 to 796 microsiemens per centimeter at 25 degrees Celsius, the daily median pH ranged from 6.5 to 7.2, and the daily mean water temperature ranged from 5.5 to 11.5 degrees Celsius. Calcium, magnesium, and bicarbonate generally were the predominant ions in solution. Concentrations of nitrite plus nitrate as nitrogen in 32 samples ranged from 3.4 to 16 milligrams per liter. Alachlor was detected in 22 percent of the samples; atrazine in 100 percent; cyanazine in 44 percent, and metplachlor in 6 percent. The maximum atrazine concentration was 4.5 micrograms per liter.</p>\n<p>During a low-flow seepage study, May 29 and 30,1990, the measured discharge lost by streams in the basin was 8.56 cubic feet per second, the measured dissolved nitrogen load lost was 0.29 ton per day, and the measured atrazine load lost was 0.028 pound per day. The total measured discharge and total dissolved nitrogen load leaving the basin in streams were 3.63 cubic feet per second and about 0.04 ton per day, respectively.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr9267","collaboration":"Prepared in cooperation with the Iowa Department of Natural Resources (Geological Survey Bureau)","usgsCitation":"Kalkhoff, S.J., Kuzniar, R., Kolpin, D., and Harvey, C., 1992, Hydrologic data for the Big Spring basin, Clayton County, Iowa, water year 1990: U.S. Geological Survey Open-File Report 92-67, vii, 80 p. ill.; 28 cm., https://doi.org/10.3133/ofr9267.","productDescription":"vii, 80 p. ill.; 28 cm.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":351,"text":"Iowa Water Science 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Stephen J. 0000-0003-4110-1716 sjkalkho@usgs.gov","orcid":"https://orcid.org/0000-0003-4110-1716","contributorId":1731,"corporation":false,"usgs":true,"family":"Kalkhoff","given":"Stephen","email":"sjkalkho@usgs.gov","middleInitial":"J.","affiliations":[{"id":36532,"text":"Central Midwest Water Science Center","active":true,"usgs":true},{"id":35680,"text":"Illinois-Iowa-Missouri Water Science Center","active":true,"usgs":true},{"id":351,"text":"Iowa Water Science Center","active":true,"usgs":true}],"preferred":true,"id":175575,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kuzniar, R.L.","contributorId":44558,"corporation":false,"usgs":true,"family":"Kuzniar","given":"R.L.","email":"","affiliations":[],"preferred":false,"id":175576,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Kolpin, D.","contributorId":18128,"corporation":false,"usgs":true,"family":"Kolpin","given":"D.","email":"","affiliations":[],"preferred":false,"id":175578,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Harvey, C.A.","contributorId":84333,"corporation":false,"usgs":true,"family":"Harvey","given":"C.A.","email":"","affiliations":[],"preferred":false,"id":175577,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":28386,"text":"wri914067 - 1992 - Shallow ground water in the Powder River basin, northeastern Wyoming– Description of selected publications, 1950-91, and indications for further study","interactions":[],"lastModifiedDate":"2021-12-09T21:38:15.018146","indexId":"wri914067","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1992","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":"91-4067","title":"Shallow ground water in the Powder River basin, northeastern Wyoming– Description of selected publications, 1950-91, and indications for further study","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri914067","usgsCitation":"Lindner-Lunsford, J.B., and Wilson, J.F., 1992, Shallow ground water in the Powder River basin, northeastern Wyoming– Description of selected publications, 1950-91, and indications for further study: U.S. Geological Survey Water-Resources Investigations Report 91-4067, iv, 71 p., https://doi.org/10.3133/wri914067.","productDescription":"iv, 71 p.","costCenters":[],"links":[{"id":57188,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1991/4067/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":159651,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1991/4067/report-thumb.jpg"},{"id":392701,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_47489.htm"}],"country":"United States","state":"Wyoming","otherGeospatial":"Powder River basin","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -107.25,\n              42.667\n            ],\n            [\n              -104.1667,\n              42.667\n            ],\n            [\n              -104.1667,\n              45\n            ],\n            [\n              -107.25,\n              45\n            ],\n            [\n              -107.25,\n              42.667\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49fae4b07f02db5f426e","contributors":{"authors":[{"text":"Lindner-Lunsford, J. B.","contributorId":81938,"corporation":false,"usgs":true,"family":"Lindner-Lunsford","given":"J.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":199709,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wilson, J. F. Jr.","contributorId":99541,"corporation":false,"usgs":true,"family":"Wilson","given":"J.","suffix":"Jr.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":199710,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":38434,"text":"pp1404A - 1992 - The regional aquifer system underlying the northern Atlantic Coastal Plain in parts of North Carolina, Virginia, Maryland, Delaware, New Jersey, and New York— Summary","interactions":[],"lastModifiedDate":"2025-04-17T18:56:59.91482","indexId":"pp1404A","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1992","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":"1404","chapter":"A","title":"The regional aquifer system underlying the northern Atlantic Coastal Plain in parts of North Carolina, Virginia, Maryland, Delaware, New Jersey, and New York— Summary","docAbstract":"<p>No abstract available.</p>","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Regional aquifer-system analysis - 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,{"id":18103,"text":"ofr91535 - 1992 - Numerical simulation of ground-water flow in the central part of the western San Joaquin Valley, California","interactions":[{"subject":{"id":18103,"text":"ofr91535 - 1992 - Numerical simulation of ground-water flow in the central part of the western San Joaquin Valley, California","indexId":"ofr91535","publicationYear":"1992","noYear":false,"title":"Numerical simulation of ground-water flow in the central part of the western San Joaquin Valley, California"},"predicate":"SUPERSEDED_BY","object":{"id":1008,"text":"wsp2396 - 1993 - Numerical simulation of ground-water flow in the central part of the western San Joaquin Valley, California","indexId":"wsp2396","publicationYear":"1993","noYear":false,"title":"Numerical simulation of ground-water flow in the central part of the western San Joaquin Valley, California"},"id":1}],"supersededBy":{"id":1008,"text":"wsp2396 - 1993 - Numerical simulation of ground-water flow in the central part of the western San Joaquin Valley, California","indexId":"wsp2396","publicationYear":"1993","noYear":false,"title":"Numerical simulation of ground-water flow in the central part of the western San Joaquin Valley, California"},"lastModifiedDate":"2024-03-27T19:31:27.148756","indexId":"ofr91535","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1992","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":"91-535","title":"Numerical simulation of ground-water flow in the central part of the western San Joaquin Valley, California","docAbstract":"<p>The occurrence of selenium in agricultural drain-water in the central part of the western San Joaquin Valley, California, has focused concern on strategies for managing shallow, saline ground water. In order to assess alternatives to agricultural drains, a three-dimensional, finite-difference numerical model of the regional ground-water flow system was developed. This report documents the mathematical approach used to model the flow system, the data base on which the model is based, and the methods used to calibrate the model.</p><p>The 550-square-mile study area includes the Panoche Creek alluvial fan and parts of the Little Panoche Creek and Cantua Creek alluvial fans. The model simulates transient flow in the semiconfined and confined zones above and below the Corcoran Clay Member of the Tulare Formation of Pleistocene age. The model incorporates areally distributed groundwater recharge, areally and vertically distributed pumping, regional-collector drains in the Westlands Water District (operative from 1980 to 1985), on-farm drains in parts of the Panoche, Broadview, and Firebaugh Water Districts, and bare-soil evaporation (which occurs if the water table is within 7 feet of land surface). The model also incorporates textural based estimates of hydraulic conductivity, with texture defined as the fraction of coarse-grained deposits present in a given subsurface interval.</p><p>The numerical model was developed using hydro-logic data from 1972 to 1988. Most of the parameters incorporated into the model were evaluated independent of the model including system geometry, the distribution of texture, the altitudes of the water table and potentiometric surface of the confined zone in 1972 (initial condition), the hydraulic conductivity of coarse-grained deposits derived from the Coast Ranges, the hydraulic conductivity of coarse-grained deposits derived from the Sierra Nevada, specific storage, recharge, pumping, and parameters needed to incorporate drains and bare-soil evaporation. Four parameters were calibration variables: the hydraulic conductivity of fine-grained deposits in the semiconfined zone, the hydraulic conductivity of the Corcoran Clay Member, specific yield, and the transmissivity of the confined zone.</p><p>The model was calibrated in two phases. In the first phase, a steady-state model of the ground-water flow system in 1984 was used to constrain the relation between the hydraulic conductivity of fine-grained deposits in the semiconfined zone and the hydraulic conductivity of the Corcoran Clay Member, thus reducing the number of independent variables from four to three. In the second phase of calibration, the change in altitude of the water table from 1972 to 1984, the change in altitude of the potentiometric surface of the confined zone from 1972 to 1984, and the number of model cells subject to bare-soil evaporation from 1972 to 1988 were used to evaluate the remaining three variables.</p><p>The calibrated model reproduces the average change in water-table altitude (1972-84) to within 0.4 foot (average measured change 11.5 feet) and the average change in confined zone head (1972-84) to within 19 feet (average measured change 120 feet). The simulated time-series record of the total number of model cells subject to bare-soil evaporation (each cell is 1 mile square) is within the range of the measured data. The measured values are at a minimum in October and a maximum in July. The October values ranged from 103 in 1972 to 132 in 1984 (the drains were closed in 1985) to 151 in 1988. The July values ranged from 144 in 1973 to 198 in 1984, to 204 in 1988. The simulated values ranged from 103 in 1972 to 161 in 1984, to 208 in 1988.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr91535","collaboration":"Prepared in cooperation with the San Joaquin Valley Drainage Program","usgsCitation":"Belitz, K., Phillips, S., and Gronberg, J., 1992, Numerical simulation of ground-water flow in the central part of the western San Joaquin Valley, California: U.S. Geological Survey Open-File Report 91-535, v, 71 p., https://doi.org/10.3133/ofr91535.","productDescription":"v, 71 p.","costCenters":[],"links":[{"id":427175,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1991/0535/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":149259,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1991/0535/report-thumb.jpg"}],"country":"United States","state":"California","otherGeospatial":"western San Joaquin Valley","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -120.42243521112113,\n              37.061054807037024\n            ],\n            [\n              -120.42243521112113,\n              36.3292127924184\n            ],\n            [\n              -119.63965595618922,\n              36.3292127924184\n            ],\n            [\n              -119.63965595618922,\n              37.061054807037024\n            ],\n            [\n              -120.42243521112113,\n              37.061054807037024\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b19e4b07f02db6a7f97","contributors":{"authors":[{"text":"Belitz, Kenneth 0000-0003-4481-2345","orcid":"https://orcid.org/0000-0003-4481-2345","contributorId":175082,"corporation":false,"usgs":true,"family":"Belitz","given":"Kenneth","affiliations":[],"preferred":false,"id":178551,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Phillips, S.P.","contributorId":38172,"corporation":false,"usgs":true,"family":"Phillips","given":"S.P.","email":"","affiliations":[],"preferred":false,"id":178550,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Gronberg, J.M.","contributorId":61839,"corporation":false,"usgs":true,"family":"Gronberg","given":"J.M.","email":"","affiliations":[],"preferred":false,"id":178552,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":54417,"text":"wdrCA911 - 1992 - Water Resources Data, California, Water Year 1991. Volume 1. Southern Great Basin from Mexican Border to Mono Lake Basin; and Pacific Slope Basins from Tijuana River to Santa Maria River","interactions":[],"lastModifiedDate":"2012-09-01T01:01:51","indexId":"wdrCA911","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1992","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":"CA-91-1","title":"Water Resources Data, California, Water Year 1991. Volume 1. Southern Great Basin from Mexican Border to Mono Lake Basin; and Pacific Slope Basins from Tijuana River to Santa Maria River","docAbstract":"Water resources data for the 1991 water year for California consist of records of stage, discharge, and water quality of streams; stage and contents in lakes and reservoirs; and water levels and water quality in wells. Volume 1 contains dischrage records for 171 streamflow-gaging stations, 16 crest-stage partial-record streamflow stations, and 3 miscellaneous measurement stations; stage and contents records for 24 lakes and reservoirs; water-quality records for 23 streamflow-gaging stations, 4 partial-record stations; and precipitation records for 16 stations. 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 California.","language":"English","publisher":"U.S. Geological Survey, Water Resources Division","publisherLocation":"Sacramento, CA","doi":"10.3133/wdrCA911","collaboration":"Prepared in cooperation with the California Department of Water Resources and with other agencies","usgsCitation":"Jensen, R., Hoffman, E., Bowers, J.C., and Mullen, J., 1992, Water Resources Data, California, Water Year 1991. Volume 1. Southern Great Basin from Mexican Border to Mono Lake Basin; and Pacific Slope Basins from Tijuana River to Santa Maria River (Legacy Report): U.S. Geological Survey Water Data Report CA-91-1, v, 330 p., https://doi.org/10.3133/wdrCA911.","productDescription":"v, 330 p.","costCenters":[],"links":[{"id":175126,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/wdr_ca_91_1.jpg"},{"id":260094,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/1991/ca-91/WDR-1991-vol1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"California","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -120.75,32.5 ], [ -120.75,38.166666666666664 ], [ -114.13333333333334,38.166666666666664 ], [ -114.13333333333334,32.5 ], [ -120.75,32.5 ] ] ] } } ] }","edition":"Legacy Report","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ce4b07f02db5fc2ed","contributors":{"authors":[{"text":"Jensen, R.M.","contributorId":39053,"corporation":false,"usgs":true,"family":"Jensen","given":"R.M.","email":"","affiliations":[],"preferred":false,"id":250292,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hoffman, E.B.","contributorId":47379,"corporation":false,"usgs":true,"family":"Hoffman","given":"E.B.","email":"","affiliations":[],"preferred":false,"id":250293,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Bowers, J. C.","contributorId":57106,"corporation":false,"usgs":true,"family":"Bowers","given":"J.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":250294,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Mullen, J.R.","contributorId":92683,"corporation":false,"usgs":true,"family":"Mullen","given":"J.R.","email":"","affiliations":[],"preferred":false,"id":250295,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":17248,"text":"ofr92107 - 1992 - Hydrologic research at the Princeton, Minnesota management systems evaluation area","interactions":[],"lastModifiedDate":"2019-12-28T09:53:08","indexId":"ofr92107","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1992","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":"92-107","title":"Hydrologic research at the Princeton, Minnesota management systems evaluation area","docAbstract":"<p>The Management Systems Evaluation Area (MSEA) program is part of a multi-scale, inter-agency initiative to evaluate the effects of agricultural management systems on water quality. The program resulted from the integration of the U.S. Department of Agriculture (USDA) Research Plan for Water Quality and the U.S Geological Survey (USGS) Mid-Continent Herbicide Initiative and is part of the President's Water Quality Initiative. The mid-continental corn belt was selected for study because it is an area where about 60% of the Nation's pesticides and nitrogen fertilizers are used.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Mounds View, MN","doi":"10.3133/ofr92107","usgsCitation":"Delin, G., Landon, M., Anderson, J.L., and Dowdy, R., 1992, Hydrologic research at the Princeton, Minnesota management systems evaluation area: U.S. Geological Survey Open-File Report 92-107, 2 p., https://doi.org/10.3133/ofr92107.","productDescription":"2 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":392,"text":"Minnesota Water Science Center","active":true,"usgs":true},{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":46398,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1992/0107/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":149341,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1992/0107/report-thumb.jpg"}],"country":"United States","state":"Minnesota","city":"Princeton","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -93.64797592163086,\n              45.509474756808736\n            ],\n            [\n              -93.64797592163086,\n              45.58304947361755\n            ],\n            [\n              -93.55991363525389,\n              45.58304947361755\n            ],\n            [\n              -93.55991363525389,\n              45.509474756808736\n            ],\n            [\n              -93.64797592163086,\n              45.509474756808736\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a18e4b07f02db6053c6","contributors":{"authors":[{"text":"Delin, G. N.","contributorId":12834,"corporation":false,"usgs":true,"family":"Delin","given":"G. N.","affiliations":[],"preferred":false,"id":175598,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Landon, M.K. 0000-0002-5766-0494","orcid":"https://orcid.org/0000-0002-5766-0494","contributorId":69572,"corporation":false,"usgs":true,"family":"Landon","given":"M.K.","affiliations":[],"preferred":false,"id":175599,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Anderson, J. L.","contributorId":103240,"corporation":false,"usgs":true,"family":"Anderson","given":"J.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":175601,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Dowdy, R.H.","contributorId":92275,"corporation":false,"usgs":true,"family":"Dowdy","given":"R.H.","email":"","affiliations":[],"preferred":false,"id":175600,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":38440,"text":"pp1404G - 1992 - Hydrogeologic framework of the northern Atlantic Coastal Plain in parts of North Carolina, Virginia, Maryland, Delaware, New Jersey, and New York","interactions":[],"lastModifiedDate":"2025-04-17T19:35:52.493914","indexId":"pp1404G","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1992","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":"1404","chapter":"G","title":"Hydrogeologic framework of the northern Atlantic Coastal Plain in parts of North Carolina, Virginia, Maryland, Delaware, New Jersey, and New York","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/pp1404G","usgsCitation":"Trapp, H., 1992, Hydrogeologic framework of the 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,{"id":54769,"text":"wdrND911 - 1992 - Water resources data, North Dakota, water year 1991","interactions":[],"lastModifiedDate":"2020-12-07T19:26:38.900992","indexId":"wdrND911","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1992","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":"ND-91-1","title":"Water resources data, North Dakota, water year 1991","docAbstract":"<p>No abstract available.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wdrND911","usgsCitation":"Harkness, R., Haffield, N., Berkas, W., and Norbeck, S., 1992, Water resources data, North Dakota, water year 1991: U.S. Geological Survey Water Data Report ND-91-1, xv, 350 p., https://doi.org/10.3133/wdrND911.","productDescription":"xv, 350 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,{"id":49603,"text":"ofr92600C - 1992 - Preliminary determination of epicenters; monthly listing July-September 1992","interactions":[],"lastModifiedDate":"2012-02-02T00:11:16","indexId":"ofr92600C","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1992","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":"92-600","chapter":"C","title":"Preliminary determination of epicenters; monthly listing July-September 1992","language":"ENGLISH","doi":"10.3133/ofr92600C","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1992, Preliminary determination of epicenters; monthly listing July-September 1992: U.S. Geological Survey Open-File Report 92-600, p. 116, https://doi.org/10.3133/ofr92600C.","productDescription":"p. 116","costCenters":[],"links":[{"id":175930,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1992/0600c/report-thumb.jpg"},{"id":86215,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1992/0600c/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67c576","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":531992,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":19098,"text":"ofr9272 - 1992 - Summary of data indicating gain or loss of streamflow across outcrops of Paleozoic formations in northeastern Wyoming, 1974-91","interactions":[],"lastModifiedDate":"2017-09-20T16:54:30","indexId":"ofr9272","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1992","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":"92-72","title":"Summary of data indicating gain or loss of streamflow across outcrops of Paleozoic formations in northeastern Wyoming, 1974-91","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nOpen-File Reports-ESIC [distributor], 1992","doi":"10.3133/ofr9272","usgsCitation":"Glass, W.R., and Sultz, L.G., 1992, Summary of data indicating gain or loss of streamflow across outcrops of Paleozoic formations in northeastern Wyoming, 1974-91: U.S. Geological Survey Open-File Report 92-72, v, 136 p. ill., map ;28 cm., https://doi.org/10.3133/ofr9272.","productDescription":"v, 136 p. ill., map ;28 cm.","costCenters":[{"id":5050,"text":"WY-MT Water Science Center","active":true,"usgs":true}],"links":[{"id":151075,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1992/0072/report-thumb.jpg"},{"id":48536,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1992/0072/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b04e4b07f02db6994aa","contributors":{"authors":[{"text":"Glass, William R.","contributorId":107304,"corporation":false,"usgs":true,"family":"Glass","given":"William","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":180304,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Sultz, LaVerne G.","contributorId":82336,"corporation":false,"usgs":true,"family":"Sultz","given":"LaVerne","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":180303,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":42006,"text":"ofr92100 - 1992 - Altitude of the water table in the surficial aquifer system, shallow zone, in eastern Palm Beach County, Florida, October 24-26, 1988","interactions":[],"lastModifiedDate":"2012-02-02T00:10:26","indexId":"ofr92100","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1992","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":"92-100","title":"Altitude of the water table in the surficial aquifer system, shallow zone, in eastern Palm Beach County, Florida, October 24-26, 1988","language":"ENGLISH","doi":"10.3133/ofr92100","usgsCitation":"Kane, R.L., 1992, Altitude of the water table in the surficial aquifer system, shallow zone, in eastern Palm Beach County, Florida, October 24-26, 1988: U.S. Geological Survey Open-File Report 92-100, 1 map :photocopy ;60 x 40 cm., https://doi.org/10.3133/ofr92100.","productDescription":"1 map :photocopy ;60 x 40 cm.","costCenters":[],"links":[{"id":169654,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":79761,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1992/0100/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adce4b07f02db686a02","contributors":{"authors":[{"text":"Kane, Richard L. rkane@usgs.gov","contributorId":2034,"corporation":false,"usgs":true,"family":"Kane","given":"Richard","email":"rkane@usgs.gov","middleInitial":"L.","affiliations":[],"preferred":true,"id":225831,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":39786,"text":"pp1406B - 1992 - Geohydrology and water resources of alluvial basins in south-central Arizona and parts of adjacent states","interactions":[{"subject":{"id":17969,"text":"ofr89378 - 1989 - Geohydrology and water resources of alluvial basins in south-central Arizona and parts of adjacent states","indexId":"ofr89378","publicationYear":"1989","noYear":false,"title":"Geohydrology and water resources of alluvial basins in south-central Arizona and parts of adjacent states"},"predicate":"SUPERSEDED_BY","object":{"id":39786,"text":"pp1406B - 1992 - Geohydrology and water resources of alluvial basins in south-central Arizona and parts of adjacent states","indexId":"pp1406B","publicationYear":"1992","noYear":false,"chapter":"B","title":"Geohydrology and water resources of alluvial basins in south-central Arizona and parts of adjacent states"},"id":1}],"lastModifiedDate":"2012-02-02T00:10:35","indexId":"pp1406B","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1992","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":"1406","chapter":"B","title":"Geohydrology and water resources of alluvial basins in south-central Arizona and parts of adjacent states","docAbstract":"The alluvial basins described in this report include about 82,000 square miles in south-central Arizona and parts of adjacent States. The area is composed of 72 basins that are virtually independent hydrologic systems. ","language":"ENGLISH","doi":"10.3133/pp1406B","usgsCitation":"Anderson, T.W., Freethey, G.W., and Tucci, P., 1992, Geohydrology and water resources of alluvial basins in south-central Arizona and parts of adjacent states: U.S. Geological Survey Professional Paper 1406, p. B1-B67, 3 plates in pocket, https://doi.org/10.3133/pp1406B.","productDescription":"p. B1-B67, 3 plates in pocket","costCenters":[],"links":[{"id":122292,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/1406b/report-thumb.jpg"},{"id":67658,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1406b/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":67659,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1406b/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":67660,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1406b/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":67661,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/1406b/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1be4b07f02db6a8b22","contributors":{"authors":[{"text":"Anderson, T. W.","contributorId":105686,"corporation":false,"usgs":true,"family":"Anderson","given":"T.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":222161,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Freethey, Geoffrey W.","contributorId":25570,"corporation":false,"usgs":true,"family":"Freethey","given":"Geoffrey","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":222160,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Tucci, Patrick ptucci@usgs.gov","contributorId":926,"corporation":false,"usgs":true,"family":"Tucci","given":"Patrick","email":"ptucci@usgs.gov","affiliations":[],"preferred":true,"id":222159,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":49618,"text":"ofr92608A - 1992 - Earthquake data report, August 1992","interactions":[],"lastModifiedDate":"2012-02-02T00:11:12","indexId":"ofr92608A","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1992","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":"92-608","chapter":"A","title":"Earthquake data report, August 1992","language":"ENGLISH","doi":"10.3133/ofr92608A","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1992, Earthquake data report, August 1992: U.S. Geological Survey Open-File Report 92-608, 458 p., https://doi.org/10.3133/ofr92608A.","productDescription":"458 p.","costCenters":[],"links":[{"id":176814,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1992/0608a/report-thumb.jpg"},{"id":86223,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1992/0608a/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a52e4b07f02db62ab04","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":532007,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":18050,"text":"ofr9279 - 1992 - Bibliography, index, and data sources for ground-water hydrology and geology of Colorado west of the continental divide","interactions":[],"lastModifiedDate":"2012-02-02T00:07:20","indexId":"ofr9279","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1992","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":"92-79","title":"Bibliography, index, and data sources for ground-water hydrology and geology of Colorado west of the continental divide","language":"ENGLISH","publisher":"U.S. Geological Survey :\r\nBooks and Open-File Reports Section [distributor],","doi":"10.3133/ofr9279","usgsCitation":"Banta, E., and Lane, T.J., 1992, Bibliography, index, and data sources for ground-water hydrology and geology of Colorado west of the continental divide: U.S. Geological Survey Open-File Report 92-79, iii, 214 p. ;28 cm., https://doi.org/10.3133/ofr9279.","productDescription":"iii, 214 p. ;28 cm.","costCenters":[],"links":[{"id":149920,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1992/0079/report-thumb.jpg"},{"id":47294,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1992/0079/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4ce4b07f02db6261e3","contributors":{"authors":[{"text":"Banta, Edward R.","contributorId":49820,"corporation":false,"usgs":true,"family":"Banta","given":"Edward R.","affiliations":[],"preferred":false,"id":178443,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lane, Theresa Jo","contributorId":53648,"corporation":false,"usgs":true,"family":"Lane","given":"Theresa","email":"","middleInitial":"Jo","affiliations":[],"preferred":false,"id":178444,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":19027,"text":"ofr92110 - 1992 - Water-quality data from continuously monitored sites in the Pamlico and Neuse River estuaries, North Carolina, 1990-91","interactions":[],"lastModifiedDate":"2016-12-16T11:19:23","indexId":"ofr92110","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1992","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":"92-110","title":"Water-quality data from continuously monitored sites in the Pamlico and Neuse River estuaries, North Carolina, 1990-91","docAbstract":"Water quality measurements were made at six sites in or near North Carolina's Pamlico River estuary and at five sites in or near the Neuse River estuary. Measurements taken at 15-minute intervals included near-surface and near-bottom specific conductance; near-surface water temperature; and near-surface, mid-depth, and near-bottom dissolved-oxygen concentrations. In the Pamlico River estuary, salinities generally ranged from near zero to about 20 parts per thousand during the period April 1989 through September 1991; however, unnaturally high salinities (up to about 51 parts per thousand) were observed at one site on July 11, 1990. Recorded water temperatures in the Pamlico River were between 0 and 33 degrees Celsius during the measurement period. Dissolved-oxygen concentrations ranged from less than 1 to 20 milligrams per liter. In the Neuse River estuary, salinities ranged from less than 0.1 to nearly 33 parts per thousand between May 1989 and September 1991. During the same period, recorded water temperatures in this estuary were between 0 and 33 degrees Celsius. Dissolved-oxygen concentrations ranged from less than 1 to 21 milligrams per liter. Instantaneous values for selected periods are summarized in a series of box plots. Daily mean values of salinity, water temperature, dissolved-oxygen concentrations, and dissolved oxygen, percent saturation, are presented in tables and graphs, as are 5-day mean values for day and night conditions. This is the second in a series of reports summarizing water quality data obtained from these continuously monitored sites.","language":"ENGLISH","publisher":"U.S. Dept. of the Interior, U.S. Geological Survey ;\r\nBooks and Open-File Reports--ESIC [distributor],","doi":"10.3133/ofr92110","usgsCitation":"Garrett, R.G., 1992, Water-quality data from continuously monitored sites in the Pamlico and Neuse River estuaries, North Carolina, 1990-91: U.S. Geological Survey Open-File Report 92-110, ix, 196 p. ill. ;28 cm., https://doi.org/10.3133/ofr92110.","productDescription":"ix, 196 p. ill. ;28 cm.","costCenters":[{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true}],"links":[{"id":48437,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1992/0110/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":151463,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1992/0110/report-thumb.jpg"}],"country":"United States","state":"North Carolina","otherGeospatial":"Neuse River estuary, Pamlico River estuary","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -79.969482421875,\n              33.63291573870479\n            ],\n            [\n              -79.969482421875,\n              36.756490329505176\n            ],\n            [\n              -74.86083984375,\n              36.756490329505176\n            ],\n            [\n              -74.86083984375,\n              33.63291573870479\n            ],\n            [\n              -79.969482421875,\n              33.63291573870479\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae0e4b07f02db687f16","contributors":{"authors":[{"text":"Garrett, Ronald G.","contributorId":34947,"corporation":false,"usgs":true,"family":"Garrett","given":"Ronald","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":180175,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":30501,"text":"wri924020 - 1992 - Techniques for estimating peak-flow frequency relations for North Dakota streams","interactions":[],"lastModifiedDate":"2018-03-13T13:44:07","indexId":"wri924020","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1992","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":"92-4020","title":"Techniques for estimating peak-flow frequency relations for North Dakota streams","docAbstract":"<p>This report presents techniques for estimating peak-flow frequency relations for North Dakota streams.&nbsp; In addition, a generalized skew coefficient analysis was completed for North Dakota to test the validity of using the generalized skew coefficient map in Bulletin 17B of the Hydrology Subcommittee of the Interagency Advisory Committee on Water Data, 1982, \"Guidelines for Determining Flood Flow Frequency.\"&nbsp; The analysis indicates that the generalized skew coefficient map in Bulletin 17B provides accurate estimates of generalized skew coefficient values for natural-flow streams in North Dakota.</p><p>&nbsp;Peak-flow records through 1988 for 192 continuous- and partial-record streamflow gaging stations that had 10 or more years of record were used in a generalized least-squares regression analysis that relates peak flows for selected recurrence intervals to selected basin characteristics.&nbsp; Peak-flow equations were developed for recurrence intervals of 2, 10, 15, 25, 50, 100, and 500 years for three hydrologic regions in North Dakota.&nbsp; The peak-flow equations are applicable to natural-flow streams that have drainage areas of less than or equal to 1,000 square miles.&nbsp; The standard error of estimate for the three hydrologic regions ranges from 60 to 70 percent for the 100-year peak-flow equations.</p><p>&nbsp;Methods are presented for transferring peak-flow data from gaging stations to ungaged sites on the same stream and for determining peak flows for ungaged sites on ungaged streams.&nbsp; Peak-flow relations, weighted estimates of peak flow, and selected basin characteristics are tabulated for the 192 gaging stations used in the generalized skew coefficient and regression analyses.&nbsp; Peak-flow relations also are provided for 63 additional gaging stations that were not used in the generalized skew coefficient and regression analyses.&nbsp; These 63 gaging stations generally represent streams that are significantly controlled by regulation and those that have drainage areas greater than 1,000 square miles.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri924020","usgsCitation":"Williams-Sether, T., 1992, Techniques for estimating peak-flow frequency relations for North Dakota streams: U.S. Geological Survey Water-Resources Investigations Report 92-4020, iv, 57 p., https://doi.org/10.3133/wri924020.","productDescription":"iv, 57 p.","costCenters":[{"id":478,"text":"North Dakota Water Science Center","active":true,"usgs":true},{"id":34685,"text":"Dakota Water Science Center","active":true,"usgs":true}],"links":[{"id":159529,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1992/4020/report-thumb.jpg"},{"id":59276,"rank":299,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1992/4020/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"North 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,{"id":29283,"text":"wri924117 - 1992 - Evaluation of the use of remote-sensing data to identify crop types and estimate irrigated acreage, Uvalde and Medina counties, Texas, 1989","interactions":[],"lastModifiedDate":"2016-08-16T10:42:33","indexId":"wri924117","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1992","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":"92-4117","title":"Evaluation of the use of remote-sensing data to identify crop types and estimate irrigated acreage, Uvalde and Medina counties, Texas, 1989","docAbstract":"<p>Remote-sensing data were used to estimate that 190,000 acre-feet of water was pumped from the Edwards aquifer in 1989 to irrigate crops in Uvalde and Medina Counties. Landsat digital satellite images for March and July 1989 were combined and classified to identify the areas of crops irrigated with water from the Edwards aquifer in the two counties. Normalized difference, the difference between the infrared and red reflectance values divided by the total of those values, was used to discriminate vegetative from nonvegetative ground cover. The images subsequently were classified using maximum likelihood, an unsupervised classification procedure. Detailed vegetation distribution maps of two calibration sites in the study area, and boundaries of the areas probably irrigated in 1989, helped to interpret the results and to separate probable irrigated areas from the rest of the image.</p>\n<p>Results were verified using crop acreages reported by the U.S. Department of Agriculture, Agricultural Stabilization and Conservation Service (ASCS). The total areas for all irrigated crops estimated using remote-sensing data were about 8 percent higher for Uvalde County and about 4 percent higher for Medina County than the areas reported by the ASCS. Irrigated-crop areas subsequently were multiplied by the respective duties of water to calculate the total quantity of water pumped from the aquifer for irrigation. Pumpage did not differ for the two estimates of crop areas for Uvalde County and differed by about 3 percent for Medina County.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Austin, TX","doi":"10.3133/wri924117","collaboration":"Prepared in cooperation with the Edwards Underground Water District","usgsCitation":"Raymond, L., Nalley, G., and Rettman, P., 1992, Evaluation of the use of remote-sensing data to identify crop types and estimate irrigated acreage, Uvalde and Medina counties, Texas, 1989: U.S. Geological Survey Water-Resources Investigations Report 92-4117, iv, 21 p., https://doi.org/10.3133/wri924117.","productDescription":"iv, 21 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":118807,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1992/4117/report-thumb.jpg"},{"id":58128,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1992/4117/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Texas","county":"Medina County, Uvalde County","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-98.8056,29.6968],[-98.8042,29.2513],[-98.8039,29.0884],[-99.4107,29.087],[-99.6813,29.0872],[-100.1119,29.0844],[-100.1112,29.3486],[-100.111,29.6236],[-100.0145,29.6237],[-99.6173,29.6257],[-99.6033,29.6257],[-99.4132,29.6253],[-99.0103,29.6187],[-98.9909,29.6185],[-98.982,29.6148],[-98.9794,29.6129],[-98.9789,29.6102],[-98.9779,29.606],[-98.9801,29.5983],[-98.9818,29.5909],[-98.9819,29.5804],[-98.9836,29.5717],[-98.9837,29.5671],[-98.9832,29.5625],[-98.9811,29.5589],[-98.978,29.5556],[-98.9765,29.5547],[-98.9712,29.5533],[-98.9676,29.5546],[-98.9633,29.5578],[-98.9607,29.5578],[-98.9513,29.5581],[-98.9429,29.5585],[-98.9318,29.5588],[-98.9282,29.5593],[-98.9245,29.562],[-98.9213,29.5665],[-98.8056,29.6968]]]},\"properties\":{\"name\":\"Medina\",\"state\":\"TX\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a29e4b07f02db611a91","contributors":{"authors":[{"text":"Raymond, L.H.","contributorId":23151,"corporation":false,"usgs":true,"family":"Raymond","given":"L.H.","email":"","affiliations":[],"preferred":false,"id":201276,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Nalley, G.M.","contributorId":23535,"corporation":false,"usgs":true,"family":"Nalley","given":"G.M.","email":"","affiliations":[],"preferred":false,"id":201277,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Rettman, P.L.","contributorId":60663,"corporation":false,"usgs":true,"family":"Rettman","given":"P.L.","affiliations":[],"preferred":false,"id":201278,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":19031,"text":"ofr92629 - 1992 - Water-supply potential of major streams and the upper Floridan Aquifer in the vicinity of Savannah, Georgia","interactions":[{"subject":{"id":19031,"text":"ofr92629 - 1992 - Water-supply potential of major streams and the upper Floridan Aquifer in the vicinity of Savannah, Georgia","indexId":"ofr92629","publicationYear":"1992","noYear":false,"title":"Water-supply potential of major streams and the upper Floridan Aquifer in the vicinity of Savannah, Georgia"},"predicate":"SUPERSEDED_BY","object":{"id":1414,"text":"wsp2411 - 1997 - Water-supply potential of major streams and the Upper Floridan Aquifer in the vicinity of Savannah, Georgia","indexId":"wsp2411","publicationYear":"1997","noYear":false,"title":"Water-supply potential of major streams and the Upper Floridan Aquifer in the vicinity of Savannah, Georgia"},"id":1}],"supersededBy":{"id":1414,"text":"wsp2411 - 1997 - Water-supply potential of major streams and the Upper Floridan Aquifer in the vicinity of Savannah, Georgia","indexId":"wsp2411","publicationYear":"1997","noYear":false,"title":"Water-supply potential of major streams and the Upper Floridan Aquifer in the vicinity of Savannah, Georgia"},"lastModifiedDate":"2021-03-04T21:16:43.635017","indexId":"ofr92629","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1992","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":"92-629","title":"Water-supply potential of major streams and the upper Floridan Aquifer in the vicinity of Savannah, Georgia","docAbstract":"<p><span>Long-term pumping from the Upper Floridan aquifer in the Savannah, Georgia, area has lowered </span><span>ground-water levels, resulting in increased salinity of ground water by seawater encroachment at Hilton Head </span><span>Island, S.C., and by saltwater intrusion at Brunswick, Ga. Increased pumpage could cause further salinization </span><span>of the ground-water resources. </span></p><p><span>The Savannah and Ogeechee Rivers can be considered potential water-supply sources for the Savannah, Ga., area, on the basis of historic stream flow records and water-quality constituents and properties examined. Analyses of stream-discharge data indicate that the minimum average discharges for 7 consecutive days for a 10-year recurrence interval (7010), was 5,460 cubic feet per second (ft3/s) at Savannah River near Clyo, Ga., and 192 ft3/s at Ogeechee River near Eden, Ga. For example, 90 percent of the time, flows in excess of the 7010 discharges are about 900 and 200 ft3/s, respectively. However, Georgia Department of Natural Resources, Environmental Protection Division, imposes a non-depletable flow criterion; thus, the actual quantity of water available for withdrawal probably would be less than flows in excess of minimum flow criteria, such as the 7Q10.</span></p><div class=\"page\" data-page-number=\"11\" data-loaded=\"true\"><div class=\"textLayer\"><span>A ground-water flow model was developed and used in conjunction with other previously calibrated </span><span>models in the coastal area to simulate the effects of additional pumping on water levels near sites of seawater </span><span>encroachment at Hilton Head Island and saltwater intrusion at Brunswick. Based on model simulations and the </span><span>constraint of preventing water-level declines at locations of encroachment and intrusion, the potential of the </span><span>Upper Floridan aquifer to supply additional water in the Savannah area is limited under present (1985) </span><span>hydrologic conditions. The water-supply potential ranges from less than 1 million gallons per day (Mgal/d) in </span><span>Liberty, McIntosh, most of Bryan, and southern Chatham Counties, Ga., and in southern Beaufort County, S.C., </span><span>to more than 5 Mgal/d in northern Jasper and northern Beaufort Counties, S.C. Because of the limited water-</span><span>supply potential, hypothetical alternatives involving redistributions, redistributions and small increases, and </span><span>decreases in pumpage were simulated to determine the effects on water levels. These simulations indicate that </span><span>reductions and redistributions of pumping would not adversely affect water levels at locations of encroachment </span><span>and intrusion. Increased pumping would cause water-level declines, which might increase salinization of the </span><span>fresh-water aquifer.</span>.&nbsp;<br></div></div>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr92629","usgsCitation":"Garza, R., and Krause, R., 1992, Water-supply potential of major streams and the upper Floridan Aquifer in the vicinity of Savannah, Georgia: U.S. Geological Survey Open-File Report 92-629, Report: viii, 49 p.; 19 Plates: 17.34 x 19.64 inches or smaller, https://doi.org/10.3133/ofr92629.","productDescription":"Report: viii, 49 p.; 19 Plates: 17.34 x 19.64 inches or smaller","costCenters":[{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true}],"links":[{"id":383864,"rank":14,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1992/0629/plate-16.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":383863,"rank":13,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1992/0629/plate-17.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":383862,"rank":12,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1992/0629/plate-18.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":383861,"rank":11,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1992/0629/plate-19.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":383860,"rank":10,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1992/0629/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":383859,"rank":9,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1992/0629/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":383858,"rank":8,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1992/0629/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":383857,"rank":7,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1992/0629/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":383856,"rank":6,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1992/0629/plate-6.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":383855,"rank":5,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1992/0629/plate-7.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":151485,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1992/0629/report-thumb.jpg"},{"id":383867,"rank":17,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1992/0629/plate-13.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":383866,"rank":16,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1992/0629/plate-14.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":383865,"rank":15,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1992/0629/plate-15.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":383854,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1992/0629/plate-8.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":383853,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1992/0629/plate-9.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":383852,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1992/0629/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":383871,"rank":21,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1992/0629/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":383870,"rank":20,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1992/0629/plate-10.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":383869,"rank":19,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1992/0629/plate-11.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":383868,"rank":18,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1992/0629/plate-12.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Georgia","city":"Savannah","otherGeospatial":"Floridan Aquifer","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -81.221923828125,\n              32.008075959291055\n            ],\n            [\n              -80.892333984375,\n              32.008075959291055\n            ],\n            [\n              -80.892333984375,\n              32.16631295696736\n            ],\n            [\n              -81.221923828125,\n              32.16631295696736\n            ],\n            [\n              -81.221923828125,\n              32.008075959291055\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e2e4b07f02db5e4d78","contributors":{"authors":[{"text":"Garza, Reggina","contributorId":102051,"corporation":false,"usgs":true,"family":"Garza","given":"Reggina","email":"","affiliations":[],"preferred":false,"id":180182,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Krause, R.E.","contributorId":73210,"corporation":false,"usgs":true,"family":"Krause","given":"R.E.","email":"","affiliations":[],"preferred":false,"id":180181,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":65564,"text":"i2261 - 1992 - Controlled photomosaic of the MTM 25182 Quadrangle, Ma'Adim Vallis region of Mars","interactions":[],"lastModifiedDate":"2019-12-23T11:42:58","indexId":"i2261","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1992","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":"2261","title":"Controlled photomosaic of the MTM 25182 Quadrangle, Ma'Adim Vallis region of Mars","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/i2261","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1992, Controlled photomosaic of the MTM 25182 Quadrangle, Ma'Adim Vallis region of Mars: U.S. Geological Survey IMAP 2261, Plate: 26 x 37 inches, https://doi.org/10.3133/i2261.","productDescription":"Plate: 26 x 37 inches","costCenters":[],"links":[{"id":190123,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":101016,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/2261/plate-1.pdf","size":"11960","linkFileType":{"id":1,"text":"pdf"}}],"scale":"502000","otherGeospatial":"Mars","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae0e4b07f02db688364","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":533951,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":65752,"text":"i2154 - 1992 - Pictorial map of Triton","interactions":[],"lastModifiedDate":"2012-02-10T00:11:02","indexId":"i2154","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1992","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":"2154","subseriesTitle":"NONE","title":"Pictorial map of Triton","language":"ENGLISH","doi":"10.3133/i2154","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1992, Pictorial map of Triton: U.S. Geological Survey IMAP 2154, 2 remote-sensing images ;22 x 57 cm. and 19 cm. diam., on sheet 67 x 64 cm., folded in envelope 30 x 24 cm., https://doi.org/10.3133/i2154.","productDescription":"2 remote-sensing images ;22 x 57 cm. and 19 cm. diam., on sheet 67 x 64 cm., folded in envelope 30 x 24 cm.","costCenters":[],"links":[{"id":190333,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":101117,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/2154/plate-1.pdf","size":"4293","linkFileType":{"id":1,"text":"pdf"}}],"scale":"5000000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ 180,-57 ], [ 180,57 ], [ 180,57 ], [ 180,-57 ], [ 180,-57 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adae4b07f02db6858db","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":534114,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":30398,"text":"wri914046 - 1992 - Evaluation of proposed water-management alternatives to lower the high water table in the Arkansas River Valley near La Junta, Colorado","interactions":[],"lastModifiedDate":"2022-01-04T20:24:43.74158","indexId":"wri914046","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1992","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":"91-4046","title":"Evaluation of proposed water-management alternatives to lower the high water table in the Arkansas River Valley near La Junta, Colorado","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri914046","usgsCitation":"Watts, K.R., and Lindner-Lunsford, J.B., 1992, Evaluation of proposed water-management alternatives to lower the high water table in the Arkansas River Valley near La Junta, Colorado: U.S. Geological Survey Water-Resources Investigations Report 91-4046, vi, 59 p., https://doi.org/10.3133/wri914046.","productDescription":"vi, 59 p.","costCenters":[],"links":[{"id":393876,"rank":2,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_47474.htm"},{"id":59168,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1991/4046/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":123147,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1991/4046/report-thumb.jpg"}],"country":"United States","state":"Colorado","city":"La Junta","otherGeospatial":"Arkansas River Valley","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -103.66493225097656,\n              37.96098194415897\n            ],\n            [\n              -103.40194702148438,\n              37.96098194415897\n            ],\n            [\n              -103.40194702148438,\n              38.025\n            ],\n            [\n              -103.66493225097656,\n              38.025\n            ],\n            [\n              -103.66493225097656,\n              37.96098194415897\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a09e4b07f02db5fac1d","contributors":{"authors":[{"text":"Watts, Kenneth R.","contributorId":43783,"corporation":false,"usgs":true,"family":"Watts","given":"Kenneth","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":203185,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lindner-Lunsford, J. B.","contributorId":81938,"corporation":false,"usgs":true,"family":"Lindner-Lunsford","given":"J.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":203186,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":65545,"text":"i2246 - 1992 - Controlled photomosaic of the MTM 10052 Quadrangle, Ganges Chasma region of Mars","interactions":[],"lastModifiedDate":"2012-02-10T00:11:05","indexId":"i2246","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1992","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":"2246","subseriesTitle":"NONE","title":"Controlled photomosaic of the MTM 10052 Quadrangle, Ganges Chasma region of Mars","language":"ENGLISH","doi":"10.3133/i2246","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1992, Controlled photomosaic of the MTM 10052 Quadrangle, Ganges Chasma region of Mars: U.S. Geological Survey IMAP 2246, 1 remote-sensing image ;61 x 59 cm., on sheet 94 x 66 cm., folded in envelope 30 x 24 cm., https://doi.org/10.3133/i2246.","productDescription":"1 remote-sensing image ;61 x 59 cm., on sheet 94 x 66 cm., folded in envelope 30 x 24 cm.","costCenters":[],"links":[{"id":190035,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":100998,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/2246/plate-1.pdf","size":"11368","linkFileType":{"id":1,"text":"pdf"}}],"scale":"502000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ 45,-12.5 ], [ 45,-7.5 ], [ 50,-7.5 ], [ 50,-12.5 ], [ 45,-12.5 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae2e4b07f02db688b21","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":533932,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":30225,"text":"wri904041 - 1992 - Potential effects of dredging the South Fork Obion River on ground-water levels near Sidonia, Weakley County, Tennessee","interactions":[],"lastModifiedDate":"2012-02-02T00:08:54","indexId":"wri904041","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1992","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":"90-4041","title":"Potential effects of dredging the South Fork Obion River on ground-water levels near Sidonia, Weakley County, Tennessee","docAbstract":"The U.S. Army Corps of Engineers has proposed dredging an approximate 7-mile reach of the South Fork Obion River near Sidonia, Tennessee. This dredging will have an effect on ground-water levels in a wetland area near the river. The river cuts into a sandy aquifer that is confined by an overlying clay layer. Ground water in the confined aquifer flows from a ridge on the north side of the study area toward the river, Estimates of aquifer transmissivity range from 3,300 to 18,800 feet squared per day.\r\n\r\nAssuming a 3-foot decline in stream stage due to dredging, the maximum decline in ground-water levels would be about 2.4 feet at low flow. Ground-water levels in the aquifer would decline by at least 2 feet at a distance of 0.5 mile from the river within 60 days after the change in stream stage, regardless of the assumed transmissivity value. Water-level declines in the upper clay layer probably would be much smaller. The time required for a specified change in ground-water level is dependent on the aquifer properties and distance from the river.","language":"ENGLISH","publisher":"U.S. Dept. of the Interior, U.S. Geological Survey ;\r\nBooks and Open-File Reports Section [distributor],","doi":"10.3133/wri904041","usgsCitation":"Tucci, P., and Hileman, G.E., 1992, Potential effects of dredging the South Fork Obion River on ground-water levels near Sidonia, Weakley County, Tennessee: U.S. Geological Survey Water-Resources Investigations Report 90-4041, iii, 12 p. :ill. ;28 cm., https://doi.org/10.3133/wri904041.","productDescription":"iii, 12 p. :ill. ;28 cm.","costCenters":[],"links":[{"id":2416,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/wri904041/","linkFileType":{"id":5,"text":"html"}},{"id":126543,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/wri_90_4041.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67c8d1","contributors":{"authors":[{"text":"Tucci, Patrick ptucci@usgs.gov","contributorId":926,"corporation":false,"usgs":true,"family":"Tucci","given":"Patrick","email":"ptucci@usgs.gov","affiliations":[],"preferred":true,"id":202890,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hileman, G. E.","contributorId":11639,"corporation":false,"usgs":true,"family":"Hileman","given":"G.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":202891,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":30046,"text":"wri914133 - 1992 - Hydrogeology of Huron County, Michigan","interactions":[],"lastModifiedDate":"2012-02-02T00:08:51","indexId":"wri914133","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1992","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":"91-4133","title":"Hydrogeology of Huron County, Michigan","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nBooks and Open-File Reports Section [distributor],","doi":"10.3133/wri914133","usgsCitation":"Sweat, M., 1992, Hydrogeology of Huron County, Michigan: U.S. Geological Survey Water-Resources Investigations Report 91-4133, viii, 76 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri914133.","productDescription":"viii, 76 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":119687,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1991/4133/report-thumb.jpg"},{"id":58845,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1991/4133/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":58846,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1991/4133/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4ae4b07f02db6251b6","contributors":{"authors":[{"text":"Sweat, M.J.","contributorId":90786,"corporation":false,"usgs":true,"family":"Sweat","given":"M.J.","email":"","affiliations":[],"preferred":false,"id":202589,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":65751,"text":"i2153 - 1992 - Pictorial map of the Slidr Linea Quadrangle (Nt-2) of Triton","interactions":[],"lastModifiedDate":"2019-12-23T11:15:02","indexId":"i2153","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1992","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":"2153","title":"Pictorial map of the Slidr Linea Quadrangle (Nt-2) of Triton","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/i2153","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1992, Pictorial map of the Slidr Linea Quadrangle (Nt-2) of Triton: U.S. Geological Survey IMAP 2153, Plate: 28 x 32 inches, https://doi.org/10.3133/i2153.","productDescription":"Plate: 28 x 32 inches","costCenters":[],"links":[{"id":190332,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":101116,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/2153/plate-1.pdf","size":"9851","linkFileType":{"id":1,"text":"pdf"}}],"scale":"5000000","otherGeospatial":"Triton, moon of Neptune","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adae4b07f02db6858ed","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":534113,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
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