Water resources data for the 1990 water year for Wyoming consists of records of stage, discharge and water quality of streams; stage and contents of lakes and reservoirs; and water levels and water quality of ground water. This report contains discharge records for 198 gaging stations; stage 'and contents for 16 lakes and reservoirs; water quality for 62 gaging stations, and 55 ungaged stations; and water levels for 5 observation wells. Additional water data were collected at various sites, not part of the systematic data collection program, and are published as miscellaneous measurements. These data represent that part of the National Water Data System operated by the U.S. Geological Survey and cooperating State and Federal agencies in Wyoming.
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The importance and limited nature of these sources caused the island of Oahu to be selected, along with 27 other aquifer systems in the United States, as part of the U.S. Geological Survey's Regional Aquifer System Analysis (RASA) program. The primary purpose of this program is to investigate the effects of that ground-water development has had or could have on the ground-water levels and the distribution of ground-water flow on a regional scale.
An important factor in the study of an aquifer system is the quantity of water recharging and flowing through the system. Ground-water recharge can be estimated from water-balance calculations, which subtract runoff and evapotranspiration from rainfall and irrigation. The quantification and distribution of recharge are necessary for ground-water flow simulation, an important element of the RASA project.
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","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/b1913","issn":"00831093","usgsCitation":"Englund, K.J., and Thomas, R.E., 1991, Coal resources of Tazewell County, Virginia, 1980: U.S. Geological Survey Bulletin 1913, Report: iv, 17 p; 5 Plates: 46.0 x 41.96 inches or smaller, https://doi.org/10.3133/b1913.","productDescription":"Report: iv, 17 p; 5 Plates: 46.0 x 41.96 inches or 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E.","contributorId":49363,"corporation":false,"usgs":true,"family":"Gray","given":"J.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":175341,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hageman, P. L. 0000-0002-3440-2150","orcid":"https://orcid.org/0000-0002-3440-2150","contributorId":27459,"corporation":false,"usgs":true,"family":"Hageman","given":"P. L.","affiliations":[],"preferred":false,"id":175339,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"McDougal, C. M.","contributorId":21129,"corporation":false,"usgs":true,"family":"McDougal","given":"C.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":175338,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Slaughter, K. 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W.","contributorId":39768,"corporation":false,"usgs":true,"family":"Thomsen","given":"B.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":202753,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Porcello, J.J.","contributorId":11661,"corporation":false,"usgs":true,"family":"Porcello","given":"J.J.","email":"","affiliations":[],"preferred":false,"id":202752,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":29708,"text":"wri914105 - 1991 - Evaluation of the drought susceptibility of water supplies used in the Kentucky River Basin in 1988","interactions":[],"lastModifiedDate":"2012-02-02T00:08:56","indexId":"wri914105","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1991","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":"91-4105","title":"Evaluation of the drought susceptibility of water supplies used in the Kentucky River Basin in 1988","language":"ENGLISH","publisher":"U.S. Dept. of the Interior, U.S. Geological Survey ;\r\nBooks and Open-File Reports Section [distributor],","doi":"10.3133/wri914105","usgsCitation":"Sholar, C., and Wood, P., 1991, Evaluation of the drought susceptibility of water supplies used in the Kentucky River Basin in 1988: U.S. Geological Survey Water-Resources Investigations Report 91-4105, v, 34 p. :ill. ;28 cm., https://doi.org/10.3133/wri914105.","productDescription":"v, 34 p. :ill. ;28 cm.","costCenters":[],"links":[{"id":119481,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1991/4105/report-thumb.jpg"},{"id":58526,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1991/4105/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afde4b07f02db696eed","contributors":{"authors":[{"text":"Sholar, C.J.","contributorId":44186,"corporation":false,"usgs":true,"family":"Sholar","given":"C.J.","affiliations":[],"preferred":false,"id":201984,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wood, P.A.","contributorId":106540,"corporation":false,"usgs":true,"family":"Wood","given":"P.A.","email":"","affiliations":[],"preferred":false,"id":201985,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":68285,"text":"ha711K - 1991 - Water type and concentration of dissolved solids, chloride, and sulfate in water from the Ozark aquifer in Missouri, Arkansas, Kansas, and Oklahoma","interactions":[],"lastModifiedDate":"2015-10-28T11:59:54","indexId":"ha711K","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1991","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":318,"text":"Hydrologic Atlas","code":"HA","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"711","chapter":"K","title":"Water type and concentration of dissolved solids, chloride, and sulfate in water from the Ozark aquifer in Missouri, Arkansas, Kansas, and Oklahoma","docAbstract":"The Ozark aquifer is a thick sequence of water-bearing dolostone, limestone, and sandstone of latest Cambrian through Middle Devonian age that is widely used as a source of water throughout the Ozark Plateaus province (index map). The Ozark aquifer is the largest of three aquifers that form part of the Ozark Plateaus aquifer system. The aquifer was studied as part of the Central Midwest Regional Aquifer-System Analysis (CMRASA; Jorgensen and Signor, 1981), a study of regional aquifer systems in the midcontinent United States that includes parts of 10States. Because of its significance as a source of freshwater in parts of Missouri, Arkansas, Kansas, and Oklahoma, a subregional project was established to investigate the Ozark Plateaus aquifer system in more detail than the regional study could provide.
The geologic and hydrologic relation between the Ozark Plateaus aquifer system and other regional aquifer systems of the Midwest is presented in Jorgensen and others (in press). The relation of the Ozark aquifer to the Ozark Plateaus aquifer system is explained in Imes [in press (a)]. A companion publication, Imes [1990 (b)], contains contour maps of the altitude of the top, thickness, and potentiometric surface of the Ozark aquifer. This report contains maps that show water type and concentrations of dissolved solids, chloride, and sulfate in water from the Ozark aquifer. Most of the data from which these maps are compiled is stored in the CMRASA hydrochemical data base (R.B. Leonard, U.S. Geological Survey, written commun., 1986). Data for Oklahoma were also taken from data published by Havens (1978). The maps in this report on the Ozark subregion may contain small differences from maps in other CMRASA publications because the criteria for data selection may be different and the subregional maps may contain additional data. However, regional trends in these maps are consistent with other maps published as part of the regional project.