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Ground water is present in San Juan County in several bedrock formations and in the alluvium of the river valleys. This report describes the hydrologic data that have been collected in San Juan County, presents examples of the data, shows the locations of the data-collection sites, and indicates where more complete records may be obtained. This data base should be helpful in assessing the quantity, quality, and availability of the county 's water resources. Information collected at 1,877 water wells, 39 streamflow-gaging stations, and 172 springs is presented. The collection sites and geology are shown on a base map with a scale of 1 inch = 2 miles. 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This Circular is intended to serve as a guide to a folio of 13 separate Open-File Reports covering various aspects of these investigations, including geology, bedrock and stream-sediment geochemistry, potassium-argon dating, Landsat imagery, mineral occurrences, aeromagnetic interpretation, and mineral-resource assessment. 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The U.S. Geological Survey (USGS) made a reconnaissance geochemical survey of the Cornplanter Roadless Area (fig. 1) to test for indistinct or unexposed mineral deposits that might be recognized by their geochemical halos or patterns formed by the distribution of trace elements. Lesure, assisted by Andrew E. Grosz, collected 22 stream-sediment, 63 soil, and 23 rock samples from within and dear the study area during October 1980. All samples were analyzed for 31 elements using semi-quantitative spectrographic methods by Day in USGS laboratories, Denver, Colo. (table 1). In addition, the samples were also analyzed for zinc by means of an atomic absorption method by B.F. Arbogast and W.C. Martin, USGS laboratories, Denver Colo. J.T. Hanley and P.G. Schruben formatted the analytical data by computer methods for table 1. 

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Water-level data for 1977-81 show that there has been no significant change in water levels, indicating that during this period, recharge in the Merced area balance natural discharge and withdrawals by pumping. Lithologic logs of shallow test wells drilled around Merced indicate shallow fine-grained material in the aquifer that could interfere with surface artificial recharge to the aquifer system. Short-term and seasonal fluctuations of water levels in wells perforated at different depths and in different aquifers show dissimilar patterns in some areas. The expansion and refinement of the observation-well network will provide a data base for water-management decisions and for assessments of ground-water conditions in the future. 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L. 0000-0001-5753-6189","orcid":"https://orcid.org/0000-0001-5753-6189","contributorId":34921,"corporation":false,"usgs":true,"family":"Rowan","given":"E. L.","affiliations":[],"preferred":false,"id":162221,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hofstra, A. H. 0000-0002-2450-1593","orcid":"https://orcid.org/0000-0002-2450-1593","contributorId":41426,"corporation":false,"usgs":true,"family":"Hofstra","given":"A. H.","affiliations":[],"preferred":false,"id":162222,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Day, G.W.","contributorId":63363,"corporation":false,"usgs":true,"family":"Day","given":"G.W.","email":"","affiliations":[],"preferred":false,"id":162223,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":59142,"text":"mf1354F - 1984 - Maps showing mineral occurrence data for the Wallace 1° by 2° Quadrangle, Montana and Idaho","interactions":[],"lastModifiedDate":"2016-08-22T10:05:44","indexId":"mf1354F","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":325,"text":"Miscellaneous Field Studies Map","code":"MF","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1354","chapter":"F","title":"Maps showing mineral occurrence data for the Wallace 1° by 2° Quadrangle, Montana and Idaho","docAbstract":"

This map is part of a folio of maps of the Wallce 1° x 2°quadrangle, Montana-Idaho, prepared under the Conterminous United States Mineral Resource Assessment Program (CUSMAP).

","language":"English","publisher":"U. S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/mf1354F","usgsCitation":"Chesson, S., Wallace, R.R., and Griffith, T., 1984, Maps showing mineral occurrence data for the Wallace 1° by 2° Quadrangle, Montana and Idaho: U.S. Geological Survey Miscellaneous Field Studies Map 1354, 33.35 x 55.25 inches, https://doi.org/10.3133/mf1354F.","productDescription":"33.35 x 55.25 inches","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":179771,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/mf1354F.PNG"},{"id":327186,"rank":1,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/1354-F/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"250000","country":"United States","state":"Idaho, Montana","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -116,47 ], [ -116,48 ], [ -114,48 ], [ -114,47 ], [ -116,47 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a19e4b07f02db605c73","contributors":{"authors":[{"text":"Chesson, Sharon","contributorId":14404,"corporation":false,"usgs":true,"family":"Chesson","given":"Sharon","email":"","affiliations":[],"preferred":false,"id":261503,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wallace, Raymond R.","contributorId":173165,"corporation":false,"usgs":false,"family":"Wallace","given":"Raymond","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":261501,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Griffith, Thomas","contributorId":59876,"corporation":false,"usgs":true,"family":"Griffith","given":"Thomas","email":"","affiliations":[],"preferred":false,"id":261502,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":10626,"text":"ofr83149 - 1984 - Hydrologic data for aquifers in Philadelphia, Pennsylvania","interactions":[],"lastModifiedDate":"2017-06-20T09:53:01","indexId":"ofr83149","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"83-149","title":"Hydrologic data for aquifers in Philadelphia, Pennsylvania","docAbstract":"Selected data on the ground-water resources of Philadelphia, Pennsylvania, are presented in this report. Information including water levels and data on aquifers is tabulated for 828 wells and 3 sumps. Chemical analyses are given for 1,467 water samples obtained from 205 sites and include 103 analyses for trace elements and 68 analyses for volatile organic compounds. An index of geophysical logs including gamma ray, neutron, caliper, fluid conductivity, fluid velocity, single-point resistance, spontaneous potential, and temperature determinations made in 51 wells is also presented. Data-collection sites are shown on a 1:50,000 scale location map.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr83149","usgsCitation":"Paulachok, G., Wood, C.R., and Norton, L., 1984, Hydrologic data for aquifers in Philadelphia, Pennsylvania: U.S. Geological Survey Open-File Report 83-149, v, 86 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr83149.","productDescription":"v, 86 p. :ill., maps ;28 cm.","costCenters":[{"id":532,"text":"Pennsylvania Water Science Center","active":true,"usgs":true}],"links":[{"id":142514,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0149/report-thumb.jpg"},{"id":38456,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0149/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":38457,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0149/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a25e4b07f02db60ebab","contributors":{"authors":[{"text":"Paulachok, G. N.","contributorId":15205,"corporation":false,"usgs":true,"family":"Paulachok","given":"G. N.","affiliations":[],"preferred":false,"id":161701,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wood, C. R.","contributorId":100386,"corporation":false,"usgs":true,"family":"Wood","given":"C.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":161702,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Norton, L.J.","contributorId":106497,"corporation":false,"usgs":true,"family":"Norton","given":"L.J.","email":"","affiliations":[],"preferred":false,"id":161703,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":26759,"text":"wri844173 - 1984 - Assessment of selected ground-water-quality data in Montana","interactions":[],"lastModifiedDate":"2012-02-02T00:08:34","indexId":"wri844173","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"84-4173","title":"Assessment of selected ground-water-quality data in Montana","docAbstract":"Ground-water-quality data for Montana in the U.S. Geological Survey 's computer data file WATSTORE were evaluated for nine geohydrologic units in part of the State east of the Rocky Mountains and for two geohydrologic units in the western mountainous part of the stated region. The availability of data for inorganic, trace, and organic constituents for each grouping of units was assessed. Median dissolved-solids concentrations for the groupings of units range from about 100 to 5,000 milligrams per liter. However, the number and distribution of data sites for some groupings of units wee inadequate to be representative of the aquifer as a whole. Concentrations of most trace constituents do not exceed Federal primary drinking-water standards, although exceptions occur. Few data were available for organic constituents. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri844173","usgsCitation":"Davis, R.E., and Rogers, G., 1984, Assessment of selected ground-water-quality data in Montana: U.S. Geological Survey Water-Resources Investigations Report 84-4173, x, 177 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri844173.","productDescription":"x, 177 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":122847,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1984/4173/report-thumb.jpg"},{"id":55648,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1984/4173/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":55649,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1984/4173/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae4e4b07f02db68a0cf","contributors":{"authors":[{"text":"Davis, R. E.","contributorId":77153,"corporation":false,"usgs":true,"family":"Davis","given":"R.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":196952,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Rogers, G.D.","contributorId":21586,"corporation":false,"usgs":true,"family":"Rogers","given":"G.D.","email":"","affiliations":[],"preferred":false,"id":196951,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":26915,"text":"wri844024 - 1984 - Water use in Ohio, 1980","interactions":[],"lastModifiedDate":"2012-02-02T00:08:23","indexId":"wri844024","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"84-4024","title":"Water use in Ohio, 1980","docAbstract":"An estimated 13,389 million gallons of water per day were used in Ohio in 1980, in four major categories of water use. Of this total, 12,645 Mgal/d (million gallons per day) were taken from surface-water sources whereas 744 Mgal/d was ground water. Totals for each category (in Mgal/d) were: thermoelectric power generation, 10,417; self-supplied manufacturing, 1,399; public water supplies, 1,432; and rural domestic and livestock, 141. Additional miscellaneous uses (irrigation, rural commercial, and non-manufacturing industrial) probably totaled about 300 Mgal/d. The five counties that led the state in total water use were: Jefferson, 2,620 Mgal/d; Lucas, 1,150 Mgal/d; Gallia, 1.086 Mgal/d; Cuyahoga, 1,085 Mgal/d; and Lorain, 991 Mgal/d. These counties, in the same order, were the top five surface-water users. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri844024","usgsCitation":"Eberle, M., and McClure, J., 1984, Water use in Ohio, 1980: U.S. Geological Survey Water-Resources Investigations Report 84-4024, iv, 34 p. :maps ;28 cm., https://doi.org/10.3133/wri844024.","productDescription":"iv, 34 p. :maps ;28 cm.","costCenters":[],"links":[{"id":118789,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1984/4024/report-thumb.jpg"},{"id":55797,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1984/4024/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a08e4b07f02db5f9cad","contributors":{"authors":[{"text":"Eberle, Michael","contributorId":39770,"corporation":false,"usgs":true,"family":"Eberle","given":"Michael","email":"","affiliations":[],"preferred":false,"id":197238,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"McClure, J.A.","contributorId":86347,"corporation":false,"usgs":true,"family":"McClure","given":"J.A.","email":"","affiliations":[],"preferred":false,"id":197239,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":10540,"text":"ofr84515 - 1984 - Liquefaction potential in the central Mississippi Valley","interactions":[{"subject":{"id":10540,"text":"ofr84515 - 1984 - Liquefaction potential in the central Mississippi Valley","indexId":"ofr84515","publicationYear":"1984","noYear":false,"title":"Liquefaction potential in the central Mississippi Valley"},"predicate":"SUPERSEDED_BY","object":{"id":35391,"text":"b1832 - 1988 - Liquefaction potential in the central Mississippi Valley","indexId":"b1832","publicationYear":"1988","noYear":false,"title":"Liquefaction potential in the central Mississippi Valley"},"id":1}],"supersededBy":{"id":35391,"text":"b1832 - 1988 - Liquefaction potential in the central Mississippi Valley","indexId":"b1832","publicationYear":"1988","noYear":false,"title":"Liquefaction potential in the central Mississippi Valley"},"lastModifiedDate":"2020-03-02T14:48:00","indexId":"ofr84515","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"84-515","title":"Liquefaction potential in the central Mississippi Valley","docAbstract":"

No abstract available.

","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr84515","usgsCitation":"Obermeier, S., 1984, Liquefaction potential in the central Mississippi Valley: U.S. Geological Survey Open-File Report 84-515, 86 p., https://doi.org/10.3133/ofr84515.","productDescription":"86 p.","costCenters":[],"links":[{"id":142452,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1984/0515/report-thumb.jpg"},{"id":372801,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1984/0515/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b15e4b07f02db6a4f92","contributors":{"authors":[{"text":"Obermeier, S. F.","contributorId":17602,"corporation":false,"usgs":true,"family":"Obermeier","given":"S. F.","affiliations":[],"preferred":false,"id":161566,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":10760,"text":"ofr84794 - 1984 - Reconnaissance geology of the Zarghat Quadrangle, sheet 26/40 B, Kingdom of Saudi Arabia","interactions":[],"lastModifiedDate":"2015-09-07T14:32:44","indexId":"ofr84794","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"84-794","title":"Reconnaissance geology of the Zarghat Quadrangle, sheet 26/40 B, Kingdom of Saudi Arabia","docAbstract":"

The Zarghat quadrangle is located in the northern Precambrian shield of Saudi Arabia between lat 26°30' and 27°00' N. and long 41°00' and 41°30 ' E. The area is underlain by three Precambrian volcanosedimentary units and a range of Precambrian dioritoid and granitoid plutonic intrusive rocks. Paleozoic(?) sandstone crops out in small areas in the northwestern part of the quadrangle, and a lobe of QuaternaryC?) basalt from Harrat Ithnain penetrates the southwest corner of the quadrangle.

\n

The Banana greenstone, the oldest unit in the quadrangle, is composed of basic to intermediate volcanic and subvolcanic rocks and minor interbedded marble that have been metamorphosed to greenschist-facies assemblages. The volcanic rocks range from basalt to andesite and dacite, and the subvolcanic rocks are diabase and diorite.

\n

Two less-metamorphosed Precambrian units, the Hadn formation and the Zarghat formation, unconformably overlie the Banana greenstone. The Hadn formation is composed of predominantly rhyolitic to dacitic volcanic rock and minor amounts of continental sedimentary rock; it is exposed only in the east half of the quadrangle. The Zarghat formation is also rhyolitic to dacitic volcanic rock but contains much more sedimentary rock that appears to have been deposited in a shallow-marine environment. The relation between these two formations is not clear at this time.

\n

Two groups of intrusive rocks are recognized on the basis of their ages relative to the Hadn and Zarghat formations. An older group is composed of hornblende quartz diorite, granodiorite, tonalite, and lesser amounts of granite. Tnese rocks intrude the Banana greenstone but predate the Hadn and Zarghat formations. Post-Hadn/Zarghat intrusive rocks are voluminous undivided granite, several varieties of alkali-feldspar granite, monzogranite, granophyre, hypabyssal rhyolite, aplite, diabase, and gabbro.

\n

The structural grain within the quadrangle appears to trend north-south. The Precambrian volcanosedimentary rocks and older plutonic rocks define three major north-trending lithologic belts. The Zarghat formation makes up the westernmost belt, and the Hadn formation comprises the easternmost belt. The central belt consists of Banana greenstone and older plutonic rocks. The north-south structural grain is crosscut by large plutons that postdate the Hadn and Zarghat formations. The dominant faults in the area belong to a northeast-trending system of shears; less common fault orientations are northwesterly, northerly, and east-westerly.

\n

Outcrops of magnesite in the southwest corner of the quadrangle constitute the only known economic potential in the area.

","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr84794","usgsCitation":"Quick, J.E., 1984, Reconnaissance geology of the Zarghat Quadrangle, sheet 26/40 B, Kingdom of Saudi Arabia: U.S. Geological Survey Open-File Report 84-794, ii, 40 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr84794.","productDescription":"ii, 40 p. :ill., maps ;28 cm.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":143384,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1984/0794/report-thumb.jpg"},{"id":38567,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1984/0794/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":38568,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1984/0794/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":38569,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1984/0794/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"Saudi Arabia","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n 40,\n 26\n ],\n [\n 40,\n 27\n ],\n [\n 41,\n 27\n ],\n [\n 41,\n 26\n ],\n [\n 40,\n 26\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a6de4b07f02db63ed9d","contributors":{"authors":[{"text":"Quick, J. E.","contributorId":48563,"corporation":false,"usgs":true,"family":"Quick","given":"J.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":161914,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":10712,"text":"ofr84130 - 1984 - Ground-water conditions in Las Vegas Valley, Clark County, Nevada; Part I, Hydrogeologic framework","interactions":[{"subject":{"id":10712,"text":"ofr84130 - 1984 - Ground-water conditions in Las Vegas Valley, Clark County, Nevada; Part I, Hydrogeologic framework","indexId":"ofr84130","publicationYear":"1984","noYear":false,"title":"Ground-water conditions in Las Vegas Valley, Clark County, Nevada; Part I, Hydrogeologic framework"},"predicate":"SUPERSEDED_BY","object":{"id":3160,"text":"wsp2320A - 1989 - Ground-water conditions in Las Vegas Valley, Clark County, Nevada; part 1 Hydrogeologic Framework","indexId":"wsp2320A","publicationYear":"1989","noYear":false,"chapter":"A","title":"Ground-water conditions in Las Vegas Valley, Clark County, Nevada; part 1 Hydrogeologic Framework"},"id":1}],"supersededBy":{"id":3160,"text":"wsp2320A - 1989 - Ground-water conditions in Las Vegas Valley, Clark County, Nevada; part 1 Hydrogeologic Framework","indexId":"wsp2320A","publicationYear":"1989","noYear":false,"title":"Ground-water conditions in Las Vegas Valley, Clark County, Nevada; part 1 Hydrogeologic Framework"},"lastModifiedDate":"2021-02-04T17:54:33.577471","indexId":"ofr84130","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"84-130","title":"Ground-water conditions in Las Vegas Valley, Clark County, Nevada; Part I, Hydrogeologic framework","docAbstract":"

No abstract available. 

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No abstract available.

","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr8471","usgsCitation":"Plantz, G., 1984, Hydrologic reconnaissance of the Kolob, Alton, and Kaiparowits Plateau coal fields, south-central Utah: U.S. Geological Survey Open-File Report 84-71, Report: 18 p.; 2 Plates: 36.15 x 24.13 inches and 36.65 x 24.30 inches, https://doi.org/10.3133/ofr8471.","productDescription":"Report: 18 p.; 2 Plates: 36.15 x 24.13 inches and 36.65 x 24.30 inches","costCenters":[],"links":[{"id":143259,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1984/0071/report-thumb.jpg"},{"id":383938,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1984/0071/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":383937,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1984/0071/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":383936,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1984/0071/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Utah","otherGeospatial":"Alton coal field, Kaiparowits Plateau coal field, Kolob coal field","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -112.0880126953125,\n 37.21283151445594\n ],\n [\n -111.14868164062499,\n 37.21283151445594\n ],\n [\n -111.14868164062499,\n 37.66208079655377\n ],\n [\n -112.0880126953125,\n 37.66208079655377\n ],\n [\n -112.0880126953125,\n 37.21283151445594\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a18e4b07f02db6054f6","contributors":{"authors":[{"text":"Plantz, G.G.","contributorId":79103,"corporation":false,"usgs":true,"family":"Plantz","given":"G.G.","affiliations":[],"preferred":false,"id":161825,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":29067,"text":"wri844028 - 1984 - Quality of water from bedrock aquifers in the South Carolina Piedmont","interactions":[],"lastModifiedDate":"2017-01-24T09:49:15","indexId":"wri844028","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"84-4028","title":"Quality of water from bedrock aquifers in the South Carolina Piedmont","docAbstract":"The geographic distributions of 12 common water-quality parameters of ground water from bedrock aquifers in the Piedmont physiographic province of South Carolina are presented in a series of maps. 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Presently, 145 continuous surface-water stations are operated in Nebraska on a budget of $908,500. Data uses and funding sources are identified for each of the 145 stations. Data from most stations have multiple uses. All stations have sufficient justification for continuation, but two stations primarily are used in short-term research studies; their continued operation needs to be evaluated when the research studies end. The present measurement frequency produces an average standard error for instantaneous discharges of about 12 percent, including periods when stage data are missing. Altering the travel routes and the measurement frequency will allow a reduction in standard error of about 1 percent with the present budget. Standard error could be reduced to about 8 percent if lost record could be eliminated. A minimum budget of $822,000 is required to operate the present network, but operations at that funding level would result in an increase in standard error to about 16 percent. The maximum budget analyzed was $1,363,000, which would result in an average standard error of 6 percent. 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