{"pageNumber":"577","pageRowStart":"14400","pageSize":"25","recordCount":16446,"records":[{"id":70168658,"text":"70168658 - 1978 - Jordan aquifer of Iowa","interactions":[],"lastModifiedDate":"2016-02-22T16:22:00","indexId":"70168658","displayToPublicDate":"1978-01-01T17:15:00","publicationYear":"1978","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesNumber":"6","subseriesTitle":"Miscellaneous Map","title":"Jordan aquifer of Iowa","docAbstract":"<p>Water demand for all uses in Iowa is increasing at an accelerated rate. Demand has increased from about 1,800 million gallons per day in 1955 to 3,500 million gallons per day in 1975 (MacKichan, 1957; Murray and Reeves, 1977). By the year 2020, water demand is expected to be eight times that in 1975 (Barnard and Dent, 1976). Historically, about 75 percent of the demand, excluding that required for power generation, has been met by withdrawals from the water-bearing zones (aquifers) in Iowa's ground-water reservoir. Because this percentage is expected to remain about the same, the anticipated future demands will require extensive withdrawals from the ground-water reservoir. The increasing stress on the ground-water system, which already is severely stressed in several places in the state, will create development and management problems that will require hydrologic information to solve. In order to provide this information, the lowa Geological Survey in cooperation with the U.S. Geological Survey has instituted a series of investigations to define, describe, and evaluate the major aquifers in Iowa's groundwater reservoir. Information from each investigation will be presented in atlas format.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","usgsCitation":"Horick, P.J., and Steinhilber, W.L., 1978, Jordan aquifer of Iowa.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":351,"text":"Iowa Water Science Center","active":true,"usgs":true}],"links":[{"id":318305,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":318304,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://s-iihr34.iihr.uiowa.edu/publications/uploads/mms-06.pdf"}],"country":"United 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,{"id":70012714,"text":"70012714 - 1978 - Uranium-isotope variations in groundwaters of the Floridan aquifer and Boulder Zone of south Florida","interactions":[],"lastModifiedDate":"2025-04-10T16:12:58.703516","indexId":"70012714","displayToPublicDate":"1978-01-01T00:00:00","publicationYear":"1978","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2342,"text":"Journal of Hydrology","active":true,"publicationSubtype":{"id":10}},"title":"Uranium-isotope variations in groundwaters of the Floridan aquifer and Boulder Zone of south Florida","docAbstract":"<p>Water samples from four wells from the main Floridan aquifer (300-400 m below mean sea level) in southeast Florida exhibit <sup>234</sup>U <sup>233</sup>U activity ratios that are significantly lower than the secular equilibrium value of 1.00. Such anomalous values have been observed previously only in waters from sedimentary aquifers in the near-surface oxidizing environments. These four wells differ from six others, all producing from the same general horizon, in being located in cavernous highly transmissive zones. We hypothesize that the low activity ratios are indicative of a relic circulation pattern whereby water from the surface aquifer was channelled to lower levels when sea level was much lower. At a deeper cavernous level, known as the Boulder Zone (800-1,000 m below mean sea level), the U isotopes, along with other chemical constituents, show progressive changes with increasing distance from an inferred flow source in the Straits of Florida. This tends to support the hypothesized landward flow (though with a more northerly component) of cold seawater in the extensively transmissive Boulder Zone.&nbsp;</p>","language":"English","publisher":"Elsevier","doi":"10.1016/0022-1694(78)90045-8","issn":"00221694","usgsCitation":"Cowart, J., Kaufman, M.I., and Osmond, J., 1978, Uranium-isotope variations in groundwaters of the Floridan aquifer and Boulder Zone of south Florida: Journal of Hydrology, v. 36, no. 1-2, p. 161-172, https://doi.org/10.1016/0022-1694(78)90045-8.","productDescription":"12 p.","startPage":"161","endPage":"172","costCenters":[],"links":[{"id":222034,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Florida","otherGeospatial":"south Florida","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -82.71978389951833,\n              27.620722131238608\n            ],\n            [\n              -82.71978389951833,\n              25.050310152154353\n            ],\n            [\n              -79.68009174787615,\n              25.050310152154353\n            ],\n            [\n              -79.68009174787615,\n              27.620722131238608\n            ],\n            [\n              -82.71978389951833,\n              27.620722131238608\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","volume":"36","issue":"1-2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bbdebe4b08c986b3292e5","contributors":{"authors":[{"text":"Cowart, J.B.","contributorId":59948,"corporation":false,"usgs":true,"family":"Cowart","given":"J.B.","email":"","affiliations":[],"preferred":false,"id":364319,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kaufman, M. I.","contributorId":66847,"corporation":false,"usgs":true,"family":"Kaufman","given":"M.","email":"","middleInitial":"I.","affiliations":[],"preferred":false,"id":364320,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Osmond, J.K.","contributorId":78467,"corporation":false,"usgs":true,"family":"Osmond","given":"J.K.","email":"","affiliations":[],"preferred":false,"id":364321,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":69546,"text":"hu41 - 1978 - Hydrologic Unit Map-1978, state of South Dakota","interactions":[],"lastModifiedDate":"2023-08-29T21:05:25.336195","indexId":"hu41","displayToPublicDate":"1978-01-01T00:00:00","publicationYear":"1978","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":319,"text":"Hydrologic Unit","code":"HU","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"41","subseriesTitle":"South Dakota 1978","title":"Hydrologic Unit Map-1978, state of South Dakota","docAbstract":"<p>This map and accompanying table show Hydrologic Unites that are basically hydrographic in nature. The Cataloging Unites shown supplant the Cataloging Units previously depicted n the 1974 State Hydrologic Unit Map. The boundaries as shown have been adapted from the 1974 State Hydrologic Unit Map, \"The Catalog of Information on Water Data\" (1972), \"Water Resources Regions and Subregions for the National Assessment of Water and Related Land Resources\" by the U.S. Water Resources Council (1970), \"River Basin of the United States\" by the U.S. Soil Conservation Service (1963, 1970), \"River Basin Maps Showing Hydrologic Stations\" by the Inter-Agency Committee on Water Resources, Subcommittee on Hydrology (1961), and State planning maps.</p>\n<br>\n<p>The Political Subdivision has been adopted from \"Counties and County Equivalents of the States if the United States\" presented in Federal Information Processing Standards Publication 6-2, issued by the National Bureau of Standards (1973) in which each county or county equivalent is identified by a 2-character State code and a 3-character county code.</p>\n<br>\n<p>The Regions, Subregions and Accounting Units are aggregates of the Cataloging Unites. The Regions and Sub regions are currently (1978) used by the U.S> Water Resources Council for comprehensive planning, including the National Assessment, and as a standard geographical framework for more detailed water and related land-resources planning. The Accounting Units are those currently (1978) in use by the U.S. Geological Survey for managing the National Water Data Network.</p>\n<br>\n<p>This map was revised to include a boundary realinement between Cataloging Units 10140103 and 10160009.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/hu41","collaboration":"Prepared in cooperation with the U.S. Water Resources Council","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1978, Hydrologic Unit Map-1978, state of South Dakota: U.S. Geological Survey Hydrologic Unit 41, Report: 1 p.; 1 Plate: 52.51 x 38.30 inches, https://doi.org/10.3133/hu41.","productDescription":"Report: 1 p.; 1 Plate: 52.51 x 38.30 inches","costCenters":[],"links":[{"id":252493,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/hu/41/report-thumb.jpg"},{"id":251580,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/hu/41/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":251581,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/hu/41/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":420277,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_16250.htm","linkFileType":{"id":5,"text":"html"}}],"scale":"500000","projection":"Lambert conformal conic projection","country":"United States","state":"South Dakota","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -104.05,42.5 ], [ -104.05,45.866667 ], [ -96.5,45.866667 ], [ -96.5,42.5 ], [ -104.05,42.5 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a2de4b07f02db61423e","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":534636,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70190919,"text":"70190919 - 1978 - Selected ground-water data, Bonneville Salt Flats and Pilot Valley, western Utah","interactions":[],"lastModifiedDate":"2017-09-17T17:00:56","indexId":"70190919","displayToPublicDate":"1978-01-01T00:00:00","publicationYear":"1978","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":5498,"text":"Utah Basic-Data Release","active":true,"publicationSubtype":{"id":2}},"seriesNumber":"30","title":"Selected ground-water data, Bonneville Salt Flats and Pilot Valley, western Utah","docAbstract":"<p>This report contains ground-water data collected at wells and springs on the Bonneville Salt Flats and in Pilot Valley, western Utah. Most of the data were collected during a study of the hydrology and surface morphology of these two salt-crust areas during the period July 1975 - June 1977. The study was carried out in cooperation with the U.S. Bureau of Land Management. This report is intended to make the basic data conveniently available and to supplement an interpretive report that will be published separately. Some earlier data that were collected by the Geological Survey and other organizations are also included.<br></p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Salt Lake City, UT","collaboration":"Prepared in cooperation with the U.S. Bureau of Land Management","usgsCitation":"Lines, G.C., 1978, Selected ground-water data, Bonneville Salt Flats and Pilot Valley, western Utah: Utah Basic-Data Release 30, iv, 14 p.","productDescription":"iv, 14 p.","numberOfPages":"20","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":345851,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":345850,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://www.waterrights.utah.gov/cgi-bin/docview.exe?Folder=TP21-1-600&Title=Basic+Data+Report+30"}],"country":"United States","state":"Utah","otherGeospatial":"Bonneville Salt Flats, Pilot Valley","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"59bf8999e4b091459a5e087b","contributors":{"authors":[{"text":"Lines, Gregory C.","contributorId":50502,"corporation":false,"usgs":true,"family":"Lines","given":"Gregory","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":710692,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":26397,"text":"wri7894 - 1978 - Hydrologic appraisal of the water resources of the Homer-Preble Valley, New York","interactions":[],"lastModifiedDate":"2023-03-14T19:44:50.633293","indexId":"wri7894","displayToPublicDate":"1978-01-01T00:00:00","publicationYear":"1978","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":"78-94","title":"Hydrologic appraisal of the water resources of the Homer-Preble Valley, New York","docAbstract":"<p>Water resources of Homer-Preble Valley, 1 to 2 miles wide and 9 miles long, in central New York, were appraised because the area is expected to undergo considerable residential development in the near future. The main source of water supply to the residents of the area is the glacial-outwash aquifer. Data indicate that additional pumpage of 5 million to 10 million gallons per day from the aquifer would not seriously reduce the quantity and quality of the water supply. Water-quality analyses indicate that ground water and surface water in the valley are suitable for most uses and generally meet State standards for source waters for drinking.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri7894","usgsCitation":"Buller, W., 1978, Hydrologic appraisal of the water resources of the Homer-Preble Valley, New York: U.S. Geological Survey Water-Resources Investigations Report 78-94, v, 31 p., https://doi.org/10.3133/wri7894.","productDescription":"v, 31 p.","costCenters":[],"links":[{"id":157876,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":266236,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1978/0094/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":414121,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_35281.htm","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"New York","otherGeospatial":"Homer-Preble Valley","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -76.208,\n              42.767\n            ],\n            [\n              -76.208,\n              42.642\n            ],\n            [\n              -76.117,\n              42.642\n            ],\n            [\n              -76.117,\n              42.767\n            ],\n            [\n              -76.208,\n              42.767\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a29e4b07f02db6116c2","contributors":{"authors":[{"text":"Buller, William","contributorId":16449,"corporation":false,"usgs":true,"family":"Buller","given":"William","email":"","affiliations":[],"preferred":false,"id":196317,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":25611,"text":"wri786 - 1978 - Impact of potential phosphate mining on the hydrology of Osceola National Forest, Florida","interactions":[],"lastModifiedDate":"2023-03-20T21:58:44.791427","indexId":"wri786","displayToPublicDate":"1978-01-01T00:00:00","publicationYear":"1978","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":"78-6","title":"Impact of potential phosphate mining on the hydrology of Osceola National Forest, Florida","docAbstract":"<p>Potentially exploitable phosphate deposits underlie part of Osceola National Forest, Fla. Hydrologic conditions in the forest are comparable with those in nearby Hamilton County, where phosphate mining and processing have been ongoing since 1965. Given similarity of operations, hydroloigc effects of mining in the forest are predicted. Flow of stream receiving phosphate industry effluent would increase somewhat during mining, but stream quality would not be greatly affected. Local changes in the configuration of the water table and the quality of water in the surficial aquifer will occur. Lowering of the potentiometric surface of the Floridan aquifer because of proposed pumpage would be less than five feet at nearby communities. Flordian aquifer water quality would be appreciably changed only if industrial effluent were discharged into streams which recharge the Flordian through sinkholes. The most significant hydrologic effects would occur at the time of active mining: long-term effects would be less significant.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri786","usgsCitation":"Miller, J.A., Hughes, G., Hull, R.W., Vecchioli, J., and Seaber, P., 1978, Impact of potential phosphate mining on the hydrology of Osceola National Forest, Florida: U.S. Geological Survey Water-Resources Investigations Report 78-6, ix, 159 p., https://doi.org/10.3133/wri786.","productDescription":"ix, 159 p.","costCenters":[],"links":[{"id":414397,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_35259.htm","linkFileType":{"id":5,"text":"html"}},{"id":54360,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1978/0006/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":123360,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1978/0006/report-thumb.jpg"}],"country":"United States","state":"Florida","otherGeospatial":"Osceola National Forest","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -82.667,\n              30.5\n            ],\n            [\n              -82.667,\n              30.15\n            ],\n            [\n              -82.167,\n              30.15\n            ],\n            [\n              -82.167,\n              30.5\n            ],\n            [\n              -82.667,\n              30.5\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a06e4b07f02db5f8c1d","contributors":{"authors":[{"text":"Miller, James A.","contributorId":49772,"corporation":false,"usgs":true,"family":"Miller","given":"James","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":194402,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hughes, G.H.","contributorId":73975,"corporation":false,"usgs":true,"family":"Hughes","given":"G.H.","email":"","affiliations":[],"preferred":false,"id":194405,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hull, R. W.","contributorId":66258,"corporation":false,"usgs":true,"family":"Hull","given":"R.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":194404,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Vecchioli, John","contributorId":36113,"corporation":false,"usgs":true,"family":"Vecchioli","given":"John","email":"","affiliations":[],"preferred":false,"id":194401,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Seaber, P. R.","contributorId":53802,"corporation":false,"usgs":true,"family":"Seaber","given":"P. R.","affiliations":[],"preferred":false,"id":194403,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70259198,"text":"70259198 - 1978 - Water-resources investigations in Florida, 1977: Hydrologic-data stations and hydrologic investigations in Florida, as of June 1977","interactions":[],"lastModifiedDate":"2024-11-19T18:51:49.96011","indexId":"70259198","displayToPublicDate":"1977-01-01T12:21:46","publicationYear":"1978","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"title":"Water-resources investigations in Florida, 1977: Hydrologic-data stations and hydrologic investigations in Florida, as of June 1977","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/70259198","collaboration":"In cooperation with the State of Florida and other State, County, Municipal, and Federal Agencies","usgsCitation":"U.S. Geological Survey, 1978, Water-resources investigations in Florida, 1977: Hydrologic-data stations and hydrologic investigations in Florida, 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,{"id":70043281,"text":"70043281 - 1977 - Hydrologic reconnaissance of the Tule Valley drainage basin, Juab and Millard Counties, Utah","interactions":[{"subject":{"id":11326,"text":"ofr76709 - 1976 - Hydrologic reconnaissance of the Tule Valley drainage basin, Juab and Millard counties, Utah","indexId":"ofr76709","publicationYear":"1976","noYear":false,"title":"Hydrologic reconnaissance of the Tule Valley drainage basin, Juab and Millard counties, Utah"},"predicate":"SUPERSEDED_BY","object":{"id":70043281,"text":"70043281 - 1977 - Hydrologic reconnaissance of the Tule Valley drainage basin, Juab and Millard Counties, Utah","indexId":"70043281","publicationYear":"1977","noYear":false,"title":"Hydrologic reconnaissance of the Tule Valley drainage basin, Juab and Millard Counties, Utah"},"id":1}],"lastModifiedDate":"2016-12-12T14:00:31","indexId":"70043281","displayToPublicDate":"2013-01-01T00:00:00","publicationYear":"1977","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":4,"text":"Other Government Series"},"seriesTitle":{"id":294,"text":"Technical Publication","active":false,"publicationSubtype":{"id":4}},"seriesNumber":"56","title":"Hydrologic reconnaissance of the Tule Valley drainage basin, Juab and Millard Counties, Utah","docAbstract":"The Tule Valley drainage basin is an area of about 940 square miles in Juab and Millard Counties in west-central Utah. Precipitation in the basin averages about 8 inches annually. There is no surface outflow and all streams are ephemeral. Annual runoff averages about 0.09 inch. Because there is no sustained runoff, and flow is local and infrequent, reservoirs do not provide dependable water supplies. Ground-water recharge from precipitation in the basin is estimated to average 7,600 acre-feet annually. Discharge, principally by evapotranspiration, averages about 40,000 acre-feet annually. Subsurface inflow from adjacent areas is estimated to average about 32,000 acre-feet annually.","language":"English","publisher":"Utah Department of Natural Resources, Division of Water Rights","publisherLocation":"Salt Lake City, UT","collaboration":"Prepared by the U.S. Geological Survey in cooperation with the Utah Department of Natural Resources, Division of Water Rights","usgsCitation":"Stephens, J., 1977, Hydrologic reconnaissance of the Tule Valley drainage basin, Juab and Millard Counties, Utah: Technical Publication 56, iv., 37 p.","productDescription":"iv., 37 p.","numberOfPages":"43","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":267167,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":331950,"rank":3,"type":{"id":11,"text":"Document"},"url":"https://waterrights.utah.gov/docSys/v920/w920/w920009i.pdf"},{"id":331949,"rank":2,"type":{"id":15,"text":"Index Page"},"url":"https://www.waterrights.utah.gov/cgi-bin/libview.exe?Modinfo=Viewpub&LIBNUM=20-5-390"}],"country":"United States","state":"Utah","county":"Juab County, Millard County","otherGeospatial":"Tule Valley Basin","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -113.78265380859374,\n              38.805470223177466\n            ],\n            [\n              -113.78265380859374,\n              39.69239407904182\n            ],\n            [\n              -113.32122802734375,\n              39.69239407904182\n            ],\n            [\n              -113.32122802734375,\n              38.805470223177466\n            ],\n            [\n              -113.78265380859374,\n              38.805470223177466\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"51177e02e4b0893acf3fffbf","contributors":{"authors":[{"text":"Stephens, J.C.","contributorId":74010,"corporation":false,"usgs":true,"family":"Stephens","given":"J.C.","email":"","affiliations":[],"preferred":false,"id":473279,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70043932,"text":"70043932 - 1977 - Hydrologic evaluation of the upper Duchesne River Valley, northern Uinta Basin area, Utah","interactions":[{"subject":{"id":9559,"text":"ofr76771 - 1976 - Hydrologic evaluation of the Upper Duchesne River Valley, Northern Uinta Basin area, Utah","indexId":"ofr76771","publicationYear":"1976","noYear":false,"title":"Hydrologic evaluation of the Upper Duchesne River Valley, Northern Uinta Basin area, Utah"},"predicate":"SUPERSEDED_BY","object":{"id":70043932,"text":"70043932 - 1977 - Hydrologic evaluation of the upper Duchesne River Valley, northern Uinta Basin area, Utah","indexId":"70043932","publicationYear":"1977","noYear":false,"title":"Hydrologic evaluation of the upper Duchesne River Valley, northern Uinta Basin area, Utah"},"id":1}],"lastModifiedDate":"2016-12-12T14:04:30","indexId":"70043932","displayToPublicDate":"2013-01-01T00:00:00","publicationYear":"1977","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":4,"text":"Other Government Series"},"seriesTitle":{"id":294,"text":"Technical Publication","active":false,"publicationSubtype":{"id":4}},"seriesNumber":"57","title":"Hydrologic evaluation of the upper Duchesne River Valley, northern Uinta Basin area, Utah","docAbstract":"The upper Duchesne River valley was studied during 1971-74 as part of an investigation of the northern Uinta Basin area, Utah and Colorado. The purpose of the study was to determine the relation of ground water to surface water, to estimate the quantity of ground water that moves to the Duchesne River, and to assess the probable effect of increased ground-water withdrawal on streamflow.","language":"English","publisher":"Utah Department of Natural Resources, Division of Water Rights","publisherLocation":"Salt Lake City, UT","collaboration":"Prepared by the United State Geological Survey in cooperation with the Utah Department of Natural Resources Division of Water Rights","usgsCitation":"Hood, J.W., 1977, Hydrologic evaluation of the upper Duchesne River Valley, northern Uinta Basin area, Utah: Technical Publication 57, iv, 34 p.","productDescription":"iv, 34 p.","numberOfPages":"42","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":268026,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":268025,"type":{"id":11,"text":"Document"},"url":"https://waterrights.utah.gov/docSys/v920/w920/w920009j.pdf"},{"id":331952,"rank":3,"type":{"id":15,"text":"Index Page"},"url":"https://www.waterrights.utah.gov/cgi-bin/libview.exe?Modinfo=Viewpub&LIBNUM=20-5-410"}],"country":"United States","state":"Utah","otherGeospatial":"Duchesne River, Uinta Basin","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -111.86279296875,\n              39.232253141714885\n            ],\n            [\n              -111.86279296875,\n              40.94671366508002\n            ],\n            [\n              -108.56689453125,\n              40.94671366508002\n            ],\n            [\n              -108.56689453125,\n              39.232253141714885\n            ],\n            [\n              -111.86279296875,\n              39.232253141714885\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5129f32ae4b04edf7e93f8de","contributors":{"authors":[{"text":"Hood, James W.","contributorId":66115,"corporation":false,"usgs":true,"family":"Hood","given":"James","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":474509,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70043723,"text":"70043723 - 1977 - Hydrologic evaluation of Ashley Valley, northern Uinta basin area, Utah","interactions":[{"subject":{"id":19438,"text":"ofr76496 - 1976 - Hydrologic evaluation of Ashley Valley, northern Uinta Basin area, Utah","indexId":"ofr76496","publicationYear":"1976","noYear":false,"title":"Hydrologic evaluation of Ashley Valley, northern Uinta Basin area, Utah"},"predicate":"SUPERSEDED_BY","object":{"id":70043723,"text":"70043723 - 1977 - Hydrologic evaluation of Ashley Valley, northern Uinta basin area, Utah","indexId":"70043723","publicationYear":"1977","noYear":false,"title":"Hydrologic evaluation of Ashley Valley, northern Uinta basin area, Utah"},"id":1},{"subject":{"id":52966,"text":"ofr5086 - 1950 - Progress report on ground-water investigation in Ashley Valley, Uintah County, Utah","indexId":"ofr5086","publicationYear":"1950","noYear":false,"title":"Progress report on ground-water investigation in Ashley Valley, Uintah County, Utah"},"predicate":"SUPERSEDED_BY","object":{"id":70043723,"text":"70043723 - 1977 - Hydrologic evaluation of Ashley Valley, northern Uinta basin area, Utah","indexId":"70043723","publicationYear":"1977","noYear":false,"title":"Hydrologic evaluation of Ashley Valley, northern Uinta basin area, Utah"},"id":2}],"lastModifiedDate":"2017-01-05T17:07:01","indexId":"70043723","displayToPublicDate":"2013-01-01T00:00:00","publicationYear":"1977","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":4,"text":"Other Government Series"},"seriesTitle":{"id":294,"text":"Technical Publication","active":false,"publicationSubtype":{"id":4}},"seriesNumber":"54","title":"Hydrologic evaluation of Ashley Valley, northern Uinta basin area, Utah","docAbstract":"<p>The water resources of the northern Uinta Basin, Utah and Colorado, were studied during 1971-74. Ashley Valley was evaluated in slightly greater detail than the general area, in order to assess the general relation of ground- and surface-water supplies.</p>\n<br>\n<p>In Ashley Valley , the principal source of both irrigation supply\nand ground-water recharge is the flow from Ashley Creek canyon .\nGround-water recharge to the valley fill, however, is mainly from canal\nand field losses along the west side of the valley. The permeability of\nthe fill in most places is high, and water-level records indicate rapid\nchanges in storage in response to the annual applications of irrigation\nwater.</p>\n<br>\n<p>Prior to the distribution of water from Steinaker Reservoir, the\nshort runoff season led to a brief, intense irrigation period that was\nfollowed by a long period of post-irrigation drainage. After the\nreservoir began operation, smaller applications of water were made\nduring a longer season, and ground-water levels rose in parts of the\nvalley , mainly the lower areas. Despite local water-level rises, no\nperennially gaining reaches of the canals were observed.</p>\n<br>\n<p>The amount of ground water available from storage in Ashley\nValley is estimated to be 50,000-75,000 acre-feet (62-92 cubic\nhectometres), or enough water to supply irrigation in the valley for a\nmaximum of 2 years. The ground-water storage varies annually about 10\npercent and has not changed significantly. Ground water is discharged\nfrom Ashley Valley both by seepage back to Ashley Creek and by\nevapotranspiration .</p>\n<br>\n<p>Evapotranspiration of surface and ground water has increased by an estimate 20 percent above the 48,000 acre-feet (59 cubic hectometers) determined for pre-reservoir conditions. As a result, the water that flows from Ashley Valley has been degraded in chemical quality.</p>\n<br>\n<p>The water from Ashley Creek canyon is fresh . Mixing of snowmelt\nand base flow in Steinaker Reservoir yields a water of more uniform\nquality; but despite some concentration by evaporation from the\nreservoir, the outflow from the reservoir is fresh. Ground water in\nmost of the valley is fresh , but the water increases in dissolved-solids\nconcentration toward the south and east as a result of both\nevapotranspiration and solution of minerals from the valley fill and\nsoils .</p>","language":"English","publisher":"Utah Department of Natural Resources, Division of Water Rights","publisherLocation":"Salt Lake City, UT","collaboration":"Prepared by the United States Geological Survey in cooperation with the Utah Department of Natural Resources Division of Water Rights","usgsCitation":"Hood, J.W., 1977, Hydrologic evaluation of Ashley Valley, northern Uinta basin area, Utah: Technical Publication 54, Report: iv, 25 p.; 1 Plate: 25.51 x 26.76 inches.","productDescription":"Report: iv, 25 p.; 1 Plate: 25.51 x 26.76 inches","numberOfPages":"31","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":267700,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/70043723.jpg"},{"id":286044,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/unnumbered/70043723/plate-1.pdf","text":"Plate 1"},{"id":331880,"rank":4,"type":{"id":15,"text":"Index Page"},"url":"https://www.waterrights.utah.gov/cgi-bin/libview.exe?Modinfo=Viewpub&LIBNUM=20-5-350"},{"id":286045,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/unnumbered/70043723/report.pdf"}],"country":"United States","state":"Utah","otherGeospatial":"Ashley Valley","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -114.0,37.0 ], [ -114.0,42.0 ], [ -109.0,42.0 ], [ -109.0,37.0 ], [ -114.0,37.0 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5124ad43e4b0b6328103b447","contributors":{"authors":[{"text":"Hood, James W.","contributorId":66115,"corporation":false,"usgs":true,"family":"Hood","given":"James","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":474171,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70040772,"text":"70040772 - 1977 - Analog-model prediction of the hydrologic effects of sanitary sewerage in southeast Nassau and southwest Suffolk Counties, New York","interactions":[],"lastModifiedDate":"2012-11-16T11:11:30","indexId":"70040772","displayToPublicDate":"2012-01-01T00:00:00","publicationYear":"1977","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":4,"text":"Other Government Series"},"seriesTitle":{"id":263,"text":"Long Island Water Resources Bulletin","active":false,"publicationSubtype":{"id":4}},"seriesNumber":"LIWR-6","title":"Analog-model prediction of the hydrologic effects of sanitary sewerage in southeast Nassau and southwest Suffolk Counties, New York","language":"English","publisher":"Nassau County Department of Public Works","publisherLocation":"Mineola, NY","usgsCitation":"Kimmel, G., Ku, H., Harbaugh, A., Sulam, D., and Getzen, R., 1977, Analog-model prediction of the hydrologic effects of sanitary sewerage in southeast Nassau and southwest Suffolk Counties, New York: Long Island Water Resources Bulletin LIWR-6, 25 p.","productDescription":"25 p.","costCenters":[{"id":474,"text":"New York Water Science Center","active":true,"usgs":true}],"links":[{"id":263231,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"New York","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -79.76,40.48 ], [ -79.76,45.02 ], [ -71.86,45.02 ], [ -71.86,40.48 ], [ -79.76,40.48 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"50a76e7be4b0e93eb366ee60","contributors":{"authors":[{"text":"Kimmel, G.E.","contributorId":23976,"corporation":false,"usgs":true,"family":"Kimmel","given":"G.E.","email":"","affiliations":[],"preferred":false,"id":468997,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ku, H.F.H.","contributorId":53012,"corporation":false,"usgs":true,"family":"Ku","given":"H.F.H.","email":"","affiliations":[],"preferred":false,"id":468998,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Harbaugh, A.W.","contributorId":15208,"corporation":false,"usgs":true,"family":"Harbaugh","given":"A.W.","email":"","affiliations":[],"preferred":false,"id":468995,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Sulam, D.J.","contributorId":99610,"corporation":false,"usgs":true,"family":"Sulam","given":"D.J.","affiliations":[],"preferred":false,"id":468999,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Getzen, R.T.","contributorId":21281,"corporation":false,"usgs":true,"family":"Getzen","given":"R.T.","affiliations":[],"preferred":false,"id":468996,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70162809,"text":"70162809 - 1977 - Simulation of flow from an aquifer to a partially penetrating trench","interactions":[],"lastModifiedDate":"2016-01-29T14:32:14","indexId":"70162809","displayToPublicDate":"2008-12-28T04:00:00","publicationYear":"1977","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2446,"text":"Journal of Research of the U.S. Geological Survey","active":true,"publicationSubtype":{"id":10}},"title":"Simulation of flow from an aquifer to a partially penetrating trench","docAbstract":"<p>Construction of the Tennessee-Tombigbee Waterway in northeast Mississippi will involve dewatering as much as 46 m of an unconfined aquifer near the Tennessee Valley divide. Dewatering by trenching is one of the proposed methods. Methods of calculating effects of dewatering by trenching have been heretofore limited to situations where ideal conditions such as isotropic aquifers and fully penetrating trenches occur. In order to study the effects of trenching on the water table in the more complicated hydrologic system in northeast Mississippi, a two-dimensional cross-sectional digital model was developed from an existing two-dimensional digital model. To make the solutions obtained from the model applicable to any aquifer thickness or other hydrologic condition, a technique for nondimensional simulation was developed. With these techniques, nondimensional water-surface profiles were generated for given stages of trench penetration of the aquifer and for different ratios of anisotropy.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","collaboration":"Prepared in cooperation with the U.S. Army Corps of Engineers, Nashville District","usgsCitation":"Leake, S.A., 1977, Simulation of flow from an aquifer to a partially penetrating trench: Journal of Research of the U.S. Geological Survey, v. 5, no. 5, p. 535-540.","productDescription":"6 p.","startPage":"535","endPage":"540","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":315173,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":315143,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/journal/1977/vol5issue5/report.pdf","text":"Report","size":"17.16 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Report"}],"country":"United States","state":"Mississippi","otherGeospatial":"Gulf of Mexico, Tennessee River valley, Tennessee-Tombigbee Waterway","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -89,\n              35\n            ],\n            [\n              -89.0057373046875,\n              33\n            ],\n            [\n              -88.3355712890625,\n              33\n            ],\n            [\n              -88.11035156249999,\n              35\n            ],\n            [\n              -88.143310546875,\n              35\n            ],\n            [\n              -88.187255859375,\n              35\n            ],\n            [\n              -89,\n              35\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"5","issue":"5","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"56ac9b7be4b0403299f53b23","contributors":{"authors":[{"text":"Leake, Stanley A. 0000-0003-3568-2542 saleake@usgs.gov","orcid":"https://orcid.org/0000-0003-3568-2542","contributorId":1846,"corporation":false,"usgs":true,"family":"Leake","given":"Stanley","email":"saleake@usgs.gov","middleInitial":"A.","affiliations":[{"id":128,"text":"Arizona Water Science Center","active":true,"usgs":true}],"preferred":true,"id":590618,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":27906,"text":"wri7782 - 1977 - Ground-water hydrology of the Lower Milliken-Sarco-Tulucay Creeks area, Napa County, California","interactions":[],"lastModifiedDate":"2016-05-20T11:29:09","indexId":"wri7782","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1977","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"77-82","title":"Ground-water hydrology of the Lower Milliken-Sarco-Tulucay Creeks area, Napa County, California","docAbstract":"<p>The Sonoma Volcanics are the principal water-bearing materials in the lower Milliken-Sarco-Tulucay Creeks area, which occupies about 15 square miles (39 square kilometers) in and east of Napa, Calif. The distribution and composition of these volcanic units are highly variable and complex. Within the Sonoma Volcanics the tuffs constitute the best ground-water reservoir. They are principally pumicitic ash-flow tuffs, partly welded and moderately permeable. These tuffs extend to a depth exceeding 500 feet (150 meters), and are irregularly interbedded with clay, igneous flows, and other volcanically derived material of very low permeability which locally confine the tuffs. Recharge and movement of ground water within these tuffs are affected by the highly variable character of this rock sequence, by adjacent formations, and by tectonic features such as the Cup and Saucer ridge and the Soda Creek fault. The lithology of the area limits specific yields to about 4 percent (unconfined conditions). Specific capacities of wells average less than 3 gallons per minute per foot of drawdown (0.6 liter per second per meter) except in the most permeable areas.</p>\n<p>Annual pumpage of 3,000 acre-feet (3.7 cubic hectometers), mostly from the Sonoma tuffs, represents a significant portion of the ground-water discharge. The seasonal change in ground-water storage was about 6,600 acre-feet (8.1 cubic hectometers) in 1975. Water-level data from the area reflect the seasonal change in ground-water storage, with fluctuations of 3 to 60 feet (1 to 18 meters). The storage capacity to a depth of 500 feet (150 meters) may be as much as 196,000 acre-feet (242 cubic hectometers) in the study area, but physical and economic factors may restrict the usable capacity to about 20,000 acre-feet (25 cubic hectometers).</p>\n<p>Recharge within the area is generally inadequate to marginal under 1975 demand. There is insufficient recharge in the Milliken and Sarco Creeks area to support 1975 pumpage. Long-term changes in the seasonal peak water levels indicate an average decline of 1.5 feet per year (0.5 meter per year). By 1975 annual pumpage was not exceeding recharge in the Tulucay Creek area. Although a downward trend in water levels was noted in the western part of this basin in the late 1940's, the pumping distribution and its stress on the ground-water system have since changed, and no overall downward trend was evident in the Tulucay Creek area in 1975.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Menlo Park, CA","doi":"10.3133/wri7782","usgsCitation":"Johnson, M.J., 1977, Ground-water hydrology of the Lower Milliken-Sarco-Tulucay Creeks area, Napa County, California: U.S. Geological Survey Water-Resources Investigations Report 77-82, Report: v, 40 p.; Plate: 41.82 x 25.99 inches, https://doi.org/10.3133/wri7782.","productDescription":"Report: v, 40 p.; Plate: 41.82 x 25.99 inches","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":158646,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/wri7782.jpg"},{"id":321077,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1977/0082/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":321078,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1977/0082/plate-1.pdf","text":"Figure 3","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"California","county":"Napa 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Michael J. johnsonm@usgs.gov","contributorId":2282,"corporation":false,"usgs":true,"family":"Johnson","given":"Michael","email":"johnsonm@usgs.gov","middleInitial":"J.","affiliations":[{"id":17705,"text":"Wetland and Aquatic Research Center","active":true,"usgs":true}],"preferred":true,"id":198878,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":28330,"text":"wri7741 - 1977 - Maps showing ground-water conditions in the southern part of the Black Mesa area, Navajo, Apache, and Coconino Counties, Arizona, 1976","interactions":[],"lastModifiedDate":"2018-01-29T11:32:16","indexId":"wri7741","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1977","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"77-41","title":"Maps showing ground-water conditions in the southern part of the Black Mesa area, Navajo, Apache, and Coconino Counties, Arizona, 1976","docAbstract":"<p>The southern part of the Black Mesa area includes about 2,500 mi<sup>2</sup> in northeastern Arizona and is entirely in the Navajo and Hopi Indian Reservations. The main source of water is the ground water in the several aquifers that are made up of one or more formations. The aquifers are stacked one on the other and generally are not hydraulically connected; the composite stratigraphic column indicates the relative position of the formations. The main waterbearing units are the N and D aquifers, the Toreva and Wepo Formations, and the alluvium. The geologic structure and topographic relief preclude a uniform depth to water in the area; therefore, recommended drilling depths should be determined on an individual site basis. Ground-water development has been mainly for public, domestic, and livestock supplies, In 1975 about 500 acre-ft of ground water was withdrawn from the aquifers in the southern part of the black Mesa area; mo st of the water was from the N aquifer. In 1951-76-the period for which data were used to compile these maps-withdrawals from the N aquifer resulted in water-level declines in parts of the area . Measurable changes in water levels have not occurred in the other aquifers in the 25-year period.</p><p>The hydrologic data on which these maps are based are available, for the most part, in computer-printout form for consultation at the Arizona Water Commission, 222 North Central Avenue, Suite 800, Phoenix, and at U.S. Geological Survey offices in: Federal Building, 301 West Congress Street, Tucson; Valley Center, Suite 1880, Phoenix; and 2255 North Gemini Drive, Building 3, Flagstaff. Material from which copies can be made at private expense is available at the Tucson, Phoenix, and Flagstaff offices of the U.S. Geological Survey. </p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri7741","collaboration":"Prepared in cooperation with the Arizona Water Commission","usgsCitation":"Levings, G., and Farrar, C.D., 1977, Maps showing ground-water conditions in the southern part of the Black Mesa area, Navajo, Apache, and Coconino Counties, Arizona, 1976: U.S. Geological Survey Water-Resources Investigations Report 77-41, 3 Plates: 44.26 x 30.87 inches or smaller, https://doi.org/10.3133/wri7741.","productDescription":"3 Plates: 44.26 x 30.87 inches or smaller","costCenters":[],"links":[{"id":158950,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1977/0041/report-thumb.jpg"},{"id":350740,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1977/0041/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":350741,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1977/0041/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":350742,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1977/0041/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Arizona","county":"Apache County, Coconino County, Navajo County","otherGeospatial":"Black Mesa Area","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -111.3,\n              35.5\n            ],\n            [\n              -109.9,\n              35.5\n            ],\n            [\n              -109.9,\n              36.25\n            ],\n            [\n              -111.3,\n              36.25\n            ],\n            [\n              -111.3,\n              35.5\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a19e4b07f02db605a2d","contributors":{"authors":[{"text":"Levings, Gary W.","contributorId":106889,"corporation":false,"usgs":true,"family":"Levings","given":"Gary W.","affiliations":[],"preferred":false,"id":199605,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Farrar, C. D.","contributorId":71978,"corporation":false,"usgs":true,"family":"Farrar","given":"C.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":199606,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":30552,"text":"wri7726 - 1977 - Hydrology of the Creeping Swamp Watershed, North Carolina with reference to potential effects of stream channelization","interactions":[],"lastModifiedDate":"2019-07-22T12:15:02","indexId":"wri7726","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1977","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"77-26","title":"Hydrology of the Creeping Swamp Watershed, North Carolina with reference to potential effects of stream channelization","docAbstract":"Hydrologic data were collected for four years at six sites in the Creeping Swamp watershed in eastern North Carolina in a preliminary effort to study the effects of stream channelization on the hydrology of a small watershed. A water-budget evaluation for pre-channelized conditions showed that runoff accounts for about 17 percent of the total rainfall, base runoff about 20 percent, ground-water outflow about 2 percent, and evapotranspiration about 61 percent. Channelization would have caused the greatest decline in ground-water levels nearest the stream, with the decline diminishing with increased distance from the stream. Channelization would also have resulted in a decrease in overland runoff and an increase in the amount of water reaching Creeping Swamp through the ground-water system, although the total volume of runoff would not change significantly. The water-quality characteristics of Creeping Swamp indicate that the stream is relatively free of pollution, although it is likely that channelization would increase (1) suspended-sediment loads, (2) stream temperatures, and (3) concentrations of dissolved solids, especially during low flows.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wri7726","usgsCitation":"Winner, M., and Simmons, C., 1977, Hydrology of the Creeping Swamp Watershed, North Carolina with reference to potential effects of stream channelization: U.S. Geological Survey Water-Resources Investigations Report 77-26, vi, 54 p. , https://doi.org/10.3133/wri7726.","productDescription":"vi, 54 p. ","costCenters":[{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true}],"links":[{"id":365792,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1977/0026/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":160607,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1977/0026/report-thumb.jpg"}],"country":"United States","state":"North Carolina","otherGeospatial":"Creeping Swamp 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Carolina\",\"nation\":\"USA  \"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aeee4b07f02db691232","contributors":{"authors":[{"text":"Winner, M.D.","contributorId":59801,"corporation":false,"usgs":true,"family":"Winner","given":"M.D.","email":"","affiliations":[],"preferred":false,"id":203444,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Simmons, C.E.","contributorId":32572,"corporation":false,"usgs":true,"family":"Simmons","given":"C.E.","email":"","affiliations":[],"preferred":false,"id":203443,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":27885,"text":"wri7714 - 1977 - Simulation studies of flow and sediment transport using a mathematical model, Atchafalaya River Basin, Louisiana","interactions":[],"lastModifiedDate":"2018-11-16T09:58:48","indexId":"wri7714","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1977","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"77-14","title":"Simulation studies of flow and sediment transport using a mathematical model, Atchafalaya River Basin, Louisiana","docAbstract":"<p>Simulation studies were made of flow and sediment transport for the Atchafalaya River basin, Louisiana using a mathematical model calibrated and supplied by the Hydrologic Engineering Center and the New Orleans District, U.S. Army Corps of Engineers. The study results are based on three, 50-year computer simulations for the following alternatives: (1) no-action alternative, (2) channelization with a center-channel flow area of 80,000 sq ft, and (3) channelization with a center-channel flow area of 100,000 sq ft. Analyses of the simulated data base for depth-frequency, inundated-area, floodway cross-section and water-surface profile relationships were made for 10 flow rates. The analyses indicate a general trend of aggradation in the lower part of the floodway with a consequent trend toward increasing the inundated area, especially at higher flood flows.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri7714","usgsCitation":"Jennings, M.E., and Land, L.F., 1977, Simulation studies of flow and sediment transport using a mathematical model, Atchafalaya River Basin, Louisiana: U.S. Geological Survey Water-Resources Investigations Report 77-14, vi, 55 p., https://doi.org/10.3133/wri7714.","productDescription":"vi, 55 p.","costCenters":[],"links":[{"id":359497,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1977/0014/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":158775,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1977/0014/report-thumb.jpg"}],"country":"United States","state":"Louisiana","otherGeospatial":"Atchafalaya River Basin","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -91.91986083984375,\n              29.310351371763023\n            ],\n            [\n              -91.14532470703125,\n              29.310351371763023\n            ],\n            [\n              -91.14532470703125,\n              31.027047769854388\n            ],\n            [\n              -91.91986083984375,\n              31.027047769854388\n            ],\n            [\n              -91.91986083984375,\n              29.310351371763023\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae5e4b07f02db68a5f6","contributors":{"authors":[{"text":"Jennings, Marshall E.","contributorId":55813,"corporation":false,"usgs":true,"family":"Jennings","given":"Marshall","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":198848,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Land, Larry F.","contributorId":60612,"corporation":false,"usgs":true,"family":"Land","given":"Larry","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":198847,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":29487,"text":"wri7789 - 1977 - Hydrologic reconnaissance of Tsala Apopka Lake, Citrus County, Florida","interactions":[],"lastModifiedDate":"2019-07-22T10:19:52","indexId":"wri7789","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1977","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"77-89","title":"Hydrologic reconnaissance of Tsala Apopka Lake, Citrus County, Florida","docAbstract":"The swamps, marshes, and open waters of Tsala Apopka Lake, Florida, were mapped and the hydrologic connection between the lake and the Floridan limestone aquifer was studied from October 1975 to September 1976. Tsala Apopka Lake is a series of shallow , interconnected lakes, ponds, and marshes whose water surface slopes northward at 0.5 foot per mile. According to aerial photographs of December 1972, only 6 percent of the 103 square miles of study area is covered by open water. Open water is abundant along the western side of the lake, dense and sparse marshes occupy most of the lake area, and swamps occupy a thick zone around the Withlacoochee River which borders the lake to the east. Only a small fraction of the total surface flow occurs through the lake. The average lake outflow through S-351 canal is 23.6 cfs; while the average river flow at Holder is 714 cfs. Tsala Apopka Lake is hydraulically connected to the Floridan aquifer. At low flow, the major source of water in the river is ground water from the Floridan aquifer. The specific conductance of water in the Floridan aquifer averages 250-350 umho/cm (micromhos per centimeter) at 25C in this area. The specific conductance of water in the Withlacoochee River near Holder averages 268 umho/cm at 25C, while water in Tsala Apopka Lake at Hernando averages 139 umho/cm at 25C. (Woodard-USGS)","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wri7789","usgsCitation":"Rutledge, A.T., 1977, Hydrologic reconnaissance of Tsala Apopka Lake, Citrus County, Florida: U.S. Geological Survey Water-Resources Investigations Report 77-89, 2 Plates: 37.40 x 27.79 inches and 37.92 x 28.06 inches, https://doi.org/10.3133/wri7789.","productDescription":"2 Plates: 37.40 x 27.79 inches and 37.92 x 28.06 inches","costCenters":[],"links":[{"id":365758,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1977/0089/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":159738,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1977/0089/report-thumb.jpg"},{"id":365759,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1977/0089/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Florida","county":"Citrus County","otherGeospatial":"Tsala Apopka Lake","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -81.70806884765625,\n              28.553163550610673\n            ],\n            [\n              -81.54327392578125,\n              28.553163550610673\n            ],\n            [\n              -81.54327392578125,\n              28.697815516328\n            ],\n            [\n              -81.70806884765625,\n              28.697815516328\n            ],\n            [\n              -81.70806884765625,\n              28.553163550610673\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1be4b07f02db6a88d7","contributors":{"authors":[{"text":"Rutledge, A. T.","contributorId":38532,"corporation":false,"usgs":true,"family":"Rutledge","given":"A.","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":201598,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":28658,"text":"wri7767 - 1977 - Ground-water resources of Chester County, Pennsylvania","interactions":[],"lastModifiedDate":"2017-07-06T08:52:46","indexId":"wri7767","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1977","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"77-67","title":"Ground-water resources of Chester County, Pennsylvania","docAbstract":"<p>Fifty gallons per minute (3 liters per second) or more may be obtained from wells in almost all parts of the county, but not at all locations. Adequate exploration to find fracture or solution openings is required. Five hundred gallons per minute (30 liters per second) or more may be obtained from some of the carbonate rocks. Linear features are visible on 1:1,000,000-to 1:24,000-scale aerial imagery. Many linear features, but not all, have geologic or hydrologic significance, and some may indicate fractured rock that might be tapped by wells. Dissolved-solids concentration of most ground water is less than 500 milligrams per liter. Chemical-quality problems are predominantly caused by acidity, iron and manganese, or nitrate. Base (ground-water) runoff during a near-average year, 1968, was about 420 million gallons per day (18 cubic meters per second).</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri7767","usgsCitation":"McGreevy, L., and Sloto, R.A., 1977, Ground-water resources of Chester County, Pennsylvania: U.S. Geological Survey Water-Resources Investigations Report 77-67, Report: vi, 76 p.; 6 Plates: 47.96 x 39.87 inches or less, https://doi.org/10.3133/wri7767.","productDescription":"Report: vi, 76 p.; 6 Plates: 47.96 x 39.87 inches or less","costCenters":[{"id":532,"text":"Pennsylvania Water Science Center","active":true,"usgs":true}],"links":[{"id":158322,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":337193,"rank":8,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1977/0067/plate-6.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":337192,"rank":7,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1977/0067/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":337187,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1977/0067/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":337189,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1977/0067/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":337188,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1977/0067/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":337190,"rank":5,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1977/0067/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":337191,"rank":6,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1977/0067/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Pennsylvania","county":"Chester County","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9ae4b07f02db65d88e","contributors":{"authors":[{"text":"McGreevy, Laurence J.","contributorId":98706,"corporation":false,"usgs":true,"family":"McGreevy","given":"Laurence J.","affiliations":[],"preferred":false,"id":200186,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Sloto, Ronald A. rasloto@usgs.gov","contributorId":424,"corporation":false,"usgs":true,"family":"Sloto","given":"Ronald","email":"rasloto@usgs.gov","middleInitial":"A.","affiliations":[{"id":532,"text":"Pennsylvania Water Science Center","active":true,"usgs":true}],"preferred":true,"id":200185,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":43874,"text":"ofr77435 - 1977 - Land use and land cover and associated maps for Vancouver, Washington-Oregon","interactions":[],"lastModifiedDate":"2017-01-18T14:31:07","indexId":"ofr77435","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1977","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"77-435","title":"Land use and land cover and associated maps for Vancouver, Washington-Oregon","docAbstract":"<p>This report consists of four plates for Vancouver, Washington-Oregon:<br></p><p><ul><li>Plate 1: Land use and land cover, 1974-1975<br></li><li>Plate 2: Political units, 1970<br></li><li>Plate 3: Hydrologic units, 1974<br></li><li>Plate 4: Census county subdivisions, 1970.<br></li></ul></p><p><br data-mce-bogus=\"1\"></p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr77435","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1977, Land use and land cover and associated maps for Vancouver, Washington-Oregon: U.S. Geological Survey Open-File Report 77-435, 4 Plates: 34.01 x 21.29 inches or smaller, https://doi.org/10.3133/ofr77435.","productDescription":"4 Plates: 34.01 x 21.29 inches or smaller","costCenters":[],"links":[{"id":168234,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr77435.PNG"},{"id":332975,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1977/0435/plate-1.pdf","text":"Plate 1","size":"6.13 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Plate 1"},{"id":332978,"rank":5,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1977/0435/plate-4.pdf","text":"Plate 4","size":"7.28 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Plate 4"},{"id":332976,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1977/0435/plate-2.pdf","text":"Plate 2","size":"6.14 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Plate 2"},{"id":332977,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1977/0435/plate-3.pdf","text":"Plate 3","size":"6.13 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Plate 3"}],"scale":"250000","country":"United States","state":"Oregon, Washington","city":"Vancouver","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -124,\n              45\n            ],\n            [\n              -124,\n              46\n            ],\n            [\n              -122,\n              46\n            ],\n            [\n              -122,\n              45\n            ],\n            [\n              -124,\n              45\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b24e4b07f02db6aebea","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":531422,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":43743,"text":"ofr77793 - 1977 - Winfield Quadrangle, geology, hydrology and mineral resoures","interactions":[{"subject":{"id":43743,"text":"ofr77793 - 1977 - Winfield Quadrangle, geology, hydrology and mineral resoures","indexId":"ofr77793","publicationYear":"1977","noYear":false,"title":"Winfield Quadrangle, geology, hydrology and mineral resoures"},"predicate":"SUPERSEDED_BY","object":{"id":70047502,"text":"70047502 - 1980 - Hydrogeologic atlas, Winfield quadrangle, Carroll County, Maryland","indexId":"70047502","publicationYear":"1980","noYear":false,"title":"Hydrogeologic atlas, Winfield quadrangle, Carroll County, Maryland"},"id":1}],"supersededBy":{"id":70047502,"text":"70047502 - 1980 - Hydrogeologic atlas, Winfield quadrangle, Carroll County, Maryland","indexId":"70047502","publicationYear":"1980","noYear":false,"title":"Hydrogeologic atlas, Winfield quadrangle, Carroll County, Maryland"},"lastModifiedDate":"2013-08-08T09:28:10","indexId":"ofr77793","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1977","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"77-793","title":"Winfield Quadrangle, geology, hydrology and mineral resoures","language":"ENGLISH","doi":"10.3133/ofr77793","usgsCitation":"Otton, E., 1977, Winfield Quadrangle, geology, hydrology and mineral resoures: U.S. Geological Survey Open-File Report 77-793, 5 maps : col. ;58 x 45 cm.; 4 p., https://doi.org/10.3133/ofr77793.","productDescription":"5 maps : col. ;58 x 45 cm.; 4 p.","costCenters":[],"links":[{"id":135202,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49dbe4b07f02db5e0dda","contributors":{"authors":[{"text":"Otton, E. G.","contributorId":22311,"corporation":false,"usgs":true,"family":"Otton","given":"E. G.","affiliations":[],"preferred":false,"id":228628,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":43742,"text":"ofr77790 - 1977 - Westminster Quadrangle, geology, hydrology, and mineral resources","interactions":[{"subject":{"id":43742,"text":"ofr77790 - 1977 - Westminster Quadrangle, geology, hydrology, and mineral resources","indexId":"ofr77790","publicationYear":"1977","noYear":false,"title":"Westminster Quadrangle, geology, hydrology, and mineral resources"},"predicate":"SUPERSEDED_BY","object":{"id":70047510,"text":"70047510 - 1979 - Hydrogeologic atlas, Westminster quadrangle, Carroll County, Maryland","indexId":"70047510","publicationYear":"1979","noYear":false,"title":"Hydrogeologic atlas, Westminster quadrangle, Carroll County, Maryland"},"id":1}],"supersededBy":{"id":70047510,"text":"70047510 - 1979 - Hydrogeologic atlas, Westminster quadrangle, Carroll County, Maryland","indexId":"70047510","publicationYear":"1979","noYear":false,"title":"Hydrogeologic atlas, Westminster quadrangle, Carroll County, Maryland"},"lastModifiedDate":"2013-08-08T10:26:40","indexId":"ofr77790","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1977","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"77-790","title":"Westminster Quadrangle, geology, hydrology, and mineral resources","language":"ENGLISH","doi":"10.3133/ofr77790","usgsCitation":"Otton, E., 1977, Westminster Quadrangle, geology, hydrology, and mineral resources: U.S. Geological Survey Open-File Report 77-790, 5 maps : col. ;59 x 45 cm.; 44 p., https://doi.org/10.3133/ofr77790.","productDescription":"5 maps : col. ;59 x 45 cm.; 44 p.","costCenters":[],"links":[{"id":135201,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e2e4b07f02db5e49c1","contributors":{"authors":[{"text":"Otton, E. G.","contributorId":22311,"corporation":false,"usgs":true,"family":"Otton","given":"E. G.","affiliations":[],"preferred":false,"id":228627,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":25023,"text":"pp715B - 1977 - Combined Ice and Water Balances of Maclure Glacier, California, South Cascade Glacier, Washington, and Wolverine and Gulkana Glaciers, Alaska, 1967 Hydrologic Year","interactions":[],"lastModifiedDate":"2012-02-02T00:08:22","indexId":"pp715B","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1977","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"715","chapter":"B","title":"Combined Ice and Water Balances of Maclure Glacier, California, South Cascade Glacier, Washington, and Wolverine and Gulkana Glaciers, Alaska, 1967 Hydrologic Year","docAbstract":"Combined ice and water balances were measured in the 1967 hydrologic year (October 1-September 30) on four glaciers in western North America ranging in latitude from 37 deg to 63 deg N. This hydrologic year was characterized by heavier than normal winter precipitation in California and Washington and abnormally dry winter conditions in coastal Alaska. In summer the western conterminous states were abnormally dry and central and southern Alaska experienced very wet conditions.\r\n\r\nMaclure Glacier (lat 37 deg 45' N., 3,650-m (metres) mean equilibrium line altitude) had an above normal winter balance of 3.46 m and a positive annual balance of 1.05 m (metres of water equivalent).\r\n\r\nSouth Cascade Glacier (lat 48 deg 22' N., 1900-m mean equilibrium line altitude) had a winter balance of 3.28 m, slightly above average. Above normal summer ablation resulted in a final annual balance of -0.58 m, slightly more negative than has been the case for the past decade.\r\n\r\nWolverine Glacier's (lat 60 deg 24' N., 1,200-m mean equilibrium line altitude) winter balance was 1.17 m, considerably below normal; the annual balance was -2.04 m.\r\n\r\nGulkana Glacier (lat 63 deg 15' N., 1,700-m mean equilibrium line altitude) had a winter balance of 1.05 m, approximately normal for this glacier; the final annual balance was -0.30 m.","language":"ENGLISH","publisher":"U.S. Geological Survey","doi":"10.3133/pp715B","collaboration":"A contribution to the International Hydrological Decade","usgsCitation":"Tangborn, W.V., Mayo, L.R., Scully, D.R., and Krimmel, R.M., 1977, Combined Ice and Water Balances of Maclure Glacier, California, South Cascade Glacier, Washington, and Wolverine and Gulkana Glaciers, Alaska, 1967 Hydrologic Year: U.S. Geological Survey Professional Paper 715, 19 p., https://doi.org/10.3133/pp715B.","productDescription":"19 p.","temporalStart":"1966-10-01","temporalEnd":"1967-09-30","costCenters":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"links":[{"id":12505,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://www.nps.gov/history/history/online_books/geology/publications/pp/715-B/index.htm","linkFileType":{"id":5,"text":"html"}},{"id":157686,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0715b/report-thumb.jpg"},{"id":54025,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0715b/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":54026,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0715b/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":54027,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0715b/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":54028,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0715b/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":54029,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0715b/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b24e4b07f02db6ae736","contributors":{"authors":[{"text":"Tangborn, Wendell V.","contributorId":32152,"corporation":false,"usgs":true,"family":"Tangborn","given":"Wendell","email":"","middleInitial":"V.","affiliations":[],"preferred":false,"id":193075,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Mayo, Lawrence R.","contributorId":98344,"corporation":false,"usgs":true,"family":"Mayo","given":"Lawrence","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":193077,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Scully, David R.","contributorId":6857,"corporation":false,"usgs":true,"family":"Scully","given":"David","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":193074,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Krimmel, Robert M.","contributorId":34902,"corporation":false,"usgs":true,"family":"Krimmel","given":"Robert","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":193076,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":28992,"text":"wri7641 - 1977 - Guide for data collection to calibrate a predictive digital ground-water model of the unconfined aquifer in and near the city of Modesto, California","interactions":[],"lastModifiedDate":"2019-07-16T12:04:34","indexId":"wri7641","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1977","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"76-41","title":"Guide for data collection to calibrate a predictive digital ground-water model of the unconfined aquifer in and near the city of Modesto, California","docAbstract":"The city of Modesto encompasses about 12 square miles in the northeastern part of the San Joaquin Valley, Calif. The ground-water model encompasses about 542 square miles. In the Modesto area, ground water occurs in an unconfined aquifer a confined aquifer. both of which are composed of unconsolidated materials, and a consolidated-rock aquifer. Only the unconfined aquifer was modeled, using several simplifying assumptions concerning hydrologic conditions in the ground-water basin. A program is used that computes the net rate of recharge and discharge under steady-state conditions. The model was then modified until reasonable values of recharge and discharge were computed. Testing of the model indicated that simulated water levels were especially sensitive to tansmissivity, storage coefficient, irrigation return, and riverbed hydraulic conductivity; amond the parameters that affected water levels least were the vertical hydraulic conductivity and specific storage of the confining bed, the so-called E-clay. (Woodard-USGS)","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wri7641","usgsCitation":"Page, R.W., 1977, Guide for data collection to calibrate a predictive digital ground-water model of the unconfined aquifer in and near the city of Modesto, California: U.S. Geological Survey Water-Resources Investigations Report 76-41, v, 46 p. , https://doi.org/10.3133/wri7641.","productDescription":"v, 46 p. ","costCenters":[],"links":[{"id":365615,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1976/0041/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":159171,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1976/0041/report-thumb.jpg"}],"country":"United States","state":"California","city":"Modesto","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -121.09954833984374,\n              37.57070524233116\n            ],\n            [\n              -120.8441162109375,\n              37.57070524233116\n            ],\n            [\n              -120.8441162109375,\n              37.690340943717715\n            ],\n            [\n              -121.09954833984374,\n              37.690340943717715\n            ],\n            [\n              -121.09954833984374,\n              37.57070524233116\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a7fe4b07f02db648b3b","contributors":{"authors":[{"text":"Page, R. W.","contributorId":17215,"corporation":false,"usgs":true,"family":"Page","given":"R.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":200749,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":27793,"text":"wri76128 - 1977 - Evaluation of ground-water quality in the Santa Maria Valley, California","interactions":[],"lastModifiedDate":"2019-04-26T11:49:19","indexId":"wri76128","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1977","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"76-128","title":"Evaluation of ground-water quality in the Santa Maria Valley, California","docAbstract":"<p>The quality and quantity of recharge to the Santa Maria Valley groundwater basin from natural sources, point sources, and agriculture were evaluated. The results are expressed in terms of a hydrologic budget, a solute balance, and maps showing the distribution of selected chemical constituents in ground water. Point sources of waste discharge that could cause ground-water degradation were investigated including a sugar-beet refinery, oil refineries and oil-field wastewater, stockyards, golf courses, poultry farms, solid-waste landfills, and municipal and industrial wastewater-treatment facilities.</p><p>Measurements of specific conductance of ground water and water levels in nearly 400 wells and the analyses of about 100 water samples for most major anions and cations plus detergents, dissolved organic carbon, and trace metals permitted preparation of maps showing the potentiometric surface and the distribution of dissolved solids, chloride, sulfate, calcium plus magnesium, and nitrogen in ground water.</p><p>Pumpage of ground water for agricultural, municipal, and industrial uses has exceeded recharge by about 10,000 acre-feet per year (12.3 cubic hectometers per year). Most of the ground water pumped in the Santa Maria Valley is for agriculture. The result of pumping in excess of recharge is a declining potentiometric surface, an accumulation of solutes, and an increase in nitrogen in ground water. At present (1976), the area of confined water is most severely affected by this degradation. Nitrogen concentrations in ground water have reached as much as 50 milligrams per liter in isolated areas, with concentrations in excess of 10 milligrams per liter occurring through most of the area of confined water. Continued pumping in excess of recharge may also lower the potentiometric surface sufficiently to permit intrusion of seawater into the fresh-water zones.</p><p>Discharge of wastewater from municipal and industrial wastewater-treatment facilities is also contributing solutes to the ground-water system. In comparison to the influences of irrigation return water on ground-water quality, the contribution from point sources is less than 10 percent of the total solutes. In some areas of the valley, the concentration of dissolved solids and some chemical constituents in water discharging from municipal and industrial wastewater-treatment facilities is lower than in the receiving ground water. </p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri76128","collaboration":"Prepared in cooperation with the California State Water Resources Control Board and the California Regional Water Quality Control Board, Central Coast Region","usgsCitation":"Hughes, J.L., 1977, Evaluation of ground-water quality in the Santa Maria Valley, California: U.S. Geological Survey Water-Resources Investigations Report 76-128, v, 72 p., https://doi.org/10.3133/wri76128.","productDescription":"v, 72 p.","costCenters":[],"links":[{"id":158599,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1976/0128/report-thumb.jpg"},{"id":363266,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1976/0128/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States ","state":"California","otherGeospatial":"Santa Maria Valley","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -120.673828125,\n              34.80252766591687\n            ],\n            [\n              -120.14511108398436,\n              34.80252766591687\n            ],\n            [\n              -120.14511108398436,\n              35.13675607652669\n            ],\n            [\n              -120.673828125,\n              35.13675607652669\n            ],\n            [\n              -120.673828125,\n              34.80252766591687\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a09e4b07f02db5fad6f","contributors":{"authors":[{"text":"Hughes, Jerry L.","contributorId":19944,"corporation":false,"usgs":true,"family":"Hughes","given":"Jerry","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":198695,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
]}