{"pageNumber":"1482","pageRowStart":"37025","pageSize":"25","recordCount":46689,"records":[{"id":44006,"text":"ofr88343 - 1988 - Water use in New Mexico, 1985","interactions":[],"lastModifiedDate":"2022-04-20T16:48:38.723392","indexId":"ofr88343","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","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":"88-343","title":"Water use in New Mexico, 1985","docAbstract":"<p>Water-use data are essential for managing the State's limited water resources. The New Mexico State Engineer Office (NMSEO) and the U.S. Geological Survey collect and publish data on water use at 5-year intervals. These data are used by Federal and State agencies, city and county planners, private industry, and irrigation districts. </p><p>This report graphically summarizes water-use data by county in New Mexico in 1985. The primary source of data was the NMSEO Technical Report 46 (Wilson, 1986), which contains detailed water-use information. The data presented here are in the same format (categories of use and units) as the technical report. The Survey' s national data-collection format differs from the NMSEO format in some category definitions, quantity of data reported, and units. T</p><p>The State Engineer Office defines a withdrawal as the amount of water removed from a surface- or ground-water source. A depletion is that part of a withdrawal consumed by man or livestock, included in crops or products, evaporated or transpired, or otherwise removed. In the figures and text referring to specific data, water use is synonymous with \"withdrawals,\" not consumptive use.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr88343","collaboration":"Prepared in cooperation with the New Mexico State Engineer Office","usgsCitation":"Garrabrant, L.A., 1988, Water use in New Mexico, 1985: U.S. Geological Survey Open-File Report 88-343, 1 Plate: 26.20 x 17.08 inches, https://doi.org/10.3133/ofr88343.","productDescription":"1 Plate: 26.20 x 17.08 inches","costCenters":[],"links":[{"id":399170,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1988/0343/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":169207,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1988/0343/report-thumb.jpg"}],"country":"United States","state":"New 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Mexico\",\"nation\":\"USA  \"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49aee4b07f02db5c7dc7","contributors":{"authors":[{"text":"Garrabrant, Lynn A.","contributorId":44212,"corporation":false,"usgs":true,"family":"Garrabrant","given":"Lynn","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":228975,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":1684,"text":"wsp2322 - 1988 - Leachate migration from an in-situ oil-shale retort near Rock Springs, Wyoming","interactions":[{"subject":{"id":13826,"text":"ofr85575 - 1986 - Leachate migration from an in situ oil-shale retort near Rock Springs, Wyoming","indexId":"ofr85575","publicationYear":"1986","noYear":false,"title":"Leachate migration from an in situ oil-shale retort near Rock Springs, Wyoming"},"predicate":"SUPERSEDED_BY","object":{"id":1684,"text":"wsp2322 - 1988 - Leachate migration from an in-situ oil-shale retort near Rock Springs, Wyoming","indexId":"wsp2322","publicationYear":"1988","noYear":false,"title":"Leachate migration from an in-situ oil-shale retort near Rock Springs, Wyoming"},"id":1}],"lastModifiedDate":"2012-02-02T00:05:24","indexId":"wsp2322","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2322","title":"Leachate migration from an in-situ oil-shale retort near Rock Springs, Wyoming","docAbstract":"Hydrogeologic factors influencing leachate movement from an in-situ oil-shale retort near Rock Springs, Wyoming, were investigated through models of ground-water flow and solute transport. Leachate, indicated by the conservative ion thiocyanate, has been observed ? mile downgradient from the retort. The contaminated aquifer is part of the Green River Formation and consists of thin, permeable layers of tuff and sandstone interbedded with oil shale. Most solute migration has occurred in an 8-foot sandstone at the top of the aquifer. Ground-water flow in the study area is complexly three dimensional and is characterized by large vertical variations in hydraulic head. The solute-transport model was used to predict the concentration of thiocyanate at a point where ground water discharges to the land surface. Leachate with peak concentrations of thiocyanate--45 milligrams per liter or approximately one-half the initial concentration of retort water--was estimated to reach the discharge area during January 1985. \r\n\r\nThis report describes many of th3 advantages, as well as the problems, of site-specific studies. Data such as the distribution of thin, permeable beds or fractures might introduce an unmanageable degree of complexity to basin-wide studies but can be incorporated readily into site-specific models. Solute migration in the study area occurs primarily in thin, permeable beds rather than in oil-shale strata. Because of this behavior, leachate traveled far greater distances than might otherwise have been expected. The detail possible in site-specific models permits more accurate prediction of solute transport than is possible with basin-wide models. A major problem in site-specific studies is identifying model boundaries that permit the accurate estimation of aquifer properties. If the quantity of water flowing through a study area cannot be determined prior to modeling, the hydraulic conductivity and ground-water velocity will be poorly estimated.","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/wsp2322","usgsCitation":"Glover, K.C., 1988, Leachate migration from an in-situ oil-shale retort near Rock Springs, Wyoming: U.S. Geological Survey Water Supply Paper 2322, iv, 26 p. ;28 cm., https://doi.org/10.3133/wsp2322.","productDescription":"iv, 26 p. ;28 cm.","costCenters":[],"links":[{"id":138106,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/2322/report-thumb.jpg"},{"id":26765,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/2322/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1be4b07f02db6a89cd","contributors":{"authors":[{"text":"Glover, Kent C.","contributorId":53766,"corporation":false,"usgs":true,"family":"Glover","given":"Kent","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":143968,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":15779,"text":"ofr88565 - 1988 - Strong motion data from the Hollister earthquake of February 20, 1988","interactions":[],"lastModifiedDate":"2012-02-02T00:07:13","indexId":"ofr88565","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","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":"88-565","title":"Strong motion data from the Hollister earthquake of February 20, 1988","language":"ENGLISH","publisher":"Dept. of the Interior, U.S. Geological Survey,","doi":"10.3133/ofr88565","usgsCitation":"Salsman, M., and Forshee, R., 1988, Strong motion data from the Hollister earthquake of February 20, 1988: U.S. Geological Survey Open-File Report 88-565, 12 p. ill., map ;28 cm., https://doi.org/10.3133/ofr88565.","productDescription":"12 p. ill., map ;28 cm.","costCenters":[],"links":[{"id":149195,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1988/0565/report-thumb.jpg"},{"id":44808,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1988/0565/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b15e4b07f02db6a4bf0","contributors":{"authors":[{"text":"Salsman, M.J.","contributorId":19565,"corporation":false,"usgs":true,"family":"Salsman","given":"M.J.","email":"","affiliations":[],"preferred":false,"id":171704,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Forshee, R.D.","contributorId":12494,"corporation":false,"usgs":true,"family":"Forshee","given":"R.D.","email":"","affiliations":[],"preferred":false,"id":171703,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":59059,"text":"mf1999 - 1988 - Mineral resources and resource potential map of the Pyramid Peak Roadless Area, Riverside County, California","interactions":[],"lastModifiedDate":"2025-05-28T16:41:49.055241","indexId":"mf1999","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","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":"1999","title":"Mineral resources and resource potential map of the Pyramid Peak Roadless Area, Riverside County, California","docAbstract":"<p>The Pyramid Peak Roadless Area is underlain by mid-Cretaceous plutonic rocks (granite, granodiorite, and tonalite) that intrude metasedimentary rocks of the Desert Divide Group. The granodiorite grades eastward into strongly deformed mylonitic rocks mapped as part of the Santa Rosa mylonite zone. Metasedimentary rocks, orthogneiss, and anatexites of the Palm Canyon Complex were displaced westward over the Santa Rosa mylonite zone along low-angle thrust faults that are nearly synchronous with the mylonite zone. The Pliocene and (or) Pleistocene Bautista Formation unconformably overlies the mid-Cretaceous plutonic rocks.</p>\n<p>Geologic and geochemical data indicate that the study area has high resource potential for marble, and moderate resource potential for epithermal gold deposits and tungsten skarns. The Desert Divide Group and the Palm Canyon Complex contain large resources of marble quarried for Portland cement and for construction applications. Gold occurs in quartz veins and pegmatites in the Desert Divide Group and the Penrod Quartz Monzonite. Skarns in the Desert Divide Group contain scheelite and anomalous concentrations of arsenic and beryllium. Thin layers of tremolite asbestos along low-angle thrust faults occur outside of the study area.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/mf1999","usgsCitation":"Calzia, J., 1988, Mineral resources and resource potential map of the Pyramid Peak Roadless Area, Riverside County, California: U.S. Geological Survey Miscellaneous Field Studies Map 1999, 1 Plate: 28.18 x 25.27 inches, https://doi.org/10.3133/mf1999.","productDescription":"1 Plate: 28.18 x 25.27 inches","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":486650,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_5592.htm","linkFileType":{"id":5,"text":"html"}},{"id":327173,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/1999/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":182642,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/mf1999.PNG"}],"country":"United States","state":"California","county":"Riverside County","otherGeospatial":"Pyramid Peak Roadless Area","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -116.61666666666666,33.55 ], [ -116.61666666666666,33.71666666666667 ], [ -116.41666666666667,33.71666666666667 ], [ -116.41666666666667,33.55 ], [ -116.61666666666666,33.55 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b08e4b07f02db69b9ab","contributors":{"authors":[{"text":"Calzia, J.P.","contributorId":58614,"corporation":false,"usgs":true,"family":"Calzia","given":"J.P.","affiliations":[],"preferred":false,"id":261344,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":27177,"text":"wri884040 - 1988 - Geohydrology of the Navajo sandstone in western Kane, southwestern Garfield, and southeastern Iron counties, Utah","interactions":[],"lastModifiedDate":"2012-02-02T00:08:26","indexId":"wri884040","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","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":"88-4040","title":"Geohydrology of the Navajo sandstone in western Kane, southwestern Garfield, and southeastern Iron counties, Utah","docAbstract":"The upper Navajo and Lamb Point aquifers in the Navajo Sandstone are the principal source of water for the city of Kanab, irrigation, stock, and for rural homes in the study area. Well logs and outcrop descriptions indicate the Navajo Sandstone consists of the Lamb Point Tongue and an unnamed upper member that are separated by the Tenney Canyon Tongue of the Kayenta Formation. The main Kayenta Formation underlies the Lamb Point Tongue. The Lamb Point Tongue and the upper member of the Navajo Sandstone are saturated and hydraulically connected through the Tenney Canyon Tongue. Available data indicate that precipitation percolates to the groundwater reservoir where the Navajo Sandstone crops out. Estimates of the rate of recharge at the outcrop range from 0.1 to as much as 2.8 in/yr. Water level data indicate that water moves from the upper member of the Navajo Sandstone, through the Tenney Canyon Tongue, and into the Lamb Point Tongue. Lateral flow is generally from the outcrop areas toward the incised canyons formed by tributaries of Kanab Creek and Johnson Wash. Direction and rate of groundwater movement and the location and character of the natural hydrologic boundaries in the northern part of the area where the Navajo Sandstone is buried cannot be determined conclusively without additional water level data. (Author 's abstract)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri884040","usgsCitation":"Freethey, G., 1988, Geohydrology of the Navajo sandstone in western Kane, southwestern Garfield, and southeastern Iron counties, Utah: U.S. Geological Survey Water-Resources Investigations Report 88-4040, v, 43 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri884040.","productDescription":"v, 43 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":118738,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1988/4040/report-thumb.jpg"},{"id":56053,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1988/4040/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":56054,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1988/4040/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":56052,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1988/4040/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1be4b07f02db6a8932","contributors":{"authors":[{"text":"Freethey, G. W.","contributorId":105714,"corporation":false,"usgs":true,"family":"Freethey","given":"G. W.","affiliations":[],"preferred":false,"id":197695,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":57519,"text":"wdrAK871 - 1988 - Water Resources Data for Alaska, Water Year 1987","interactions":[],"lastModifiedDate":"2012-02-02T00:12:10","indexId":"wdrAK871","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"AK-87-1","title":"Water Resources Data for Alaska, Water Year 1987","language":"ENGLISH","doi":"10.3133/wdrAK871","usgsCitation":"Vaill, J.E., Still, P., Lamke, R., Bigelow, B.B., and VanMaanen, J., 1988, Water Resources Data for Alaska, Water Year 1987: U.S. Geological Survey Water Data Report AK-87-1, 284 p., https://doi.org/10.3133/wdrAK871.","productDescription":"284 p.","costCenters":[],"links":[{"id":185377,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac7e4b07f02db67b0cf","contributors":{"authors":[{"text":"Vaill, J. E.","contributorId":86362,"corporation":false,"usgs":true,"family":"Vaill","given":"J.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":257248,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Still, P.J.","contributorId":83152,"corporation":false,"usgs":true,"family":"Still","given":"P.J.","email":"","affiliations":[],"preferred":false,"id":257247,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Lamke, R. D.","contributorId":32539,"corporation":false,"usgs":true,"family":"Lamke","given":"R. D.","affiliations":[],"preferred":false,"id":257245,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Bigelow, B. B.","contributorId":76317,"corporation":false,"usgs":true,"family":"Bigelow","given":"B.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":257246,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"VanMaanen, J.L.","contributorId":100072,"corporation":false,"usgs":true,"family":"VanMaanen","given":"J.L.","email":"","affiliations":[],"preferred":false,"id":257249,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":57513,"text":"wdrAL871 - 1988 - Water resources data for Alabama, water year 1987","interactions":[],"lastModifiedDate":"2022-11-23T19:50:37.71252","indexId":"wdrAL871","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"AL-87-1","title":"Water resources data for Alabama, water year 1987","docAbstract":"<p>The Water Resources Division of the U.S. Geological Survey, in cooperation with State and Federal agencies, obtains a large amount of data pertaining to the water resources of Alabama each water year. These data, accumulated during many water years, constitute a valuable data base for developing an improved understanding of the water resources of the State. To make these data readily available to interested parties outside the Geological Survey, the data are published annually in this report series entitled \"Water Resources Data - Alabama.\"</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wdrAL871","collaboration":"Prepared in cooperation with the Alabama Department of Environmental Management, the Alabama Highway Department, the Geological Survey of Alabama, and with other State, municipal, and Federal agencies","usgsCitation":"Rollins, H., Sedberry, F., Pearman, J., and Duvall, T., 1988, Water resources data for Alabama, water year 1987: U.S. Geological Survey Water Data Report AL-87-1, viii, 337 p., https://doi.org/10.3133/wdrAL871.","productDescription":"viii, 337 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,{"id":12002,"text":"ofr88271 - 1988 - Data on the geochemistry and thermal maturation of sedimentary-rock hosted, disseminated gold deposits and associated rocks, southwestern Guizhou Province, People's Republic of China","interactions":[],"lastModifiedDate":"2012-02-02T00:06:39","indexId":"ofr88271","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","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":"88-271","title":"Data on the geochemistry and thermal maturation of sedimentary-rock hosted, disseminated gold deposits and associated rocks, southwestern Guizhou Province, People's Republic of China","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr88271","usgsCitation":"Dean, W., Bostick, N.H., Bartel, A., Brandt, E.L., Daws, T., Doughten, M., Gent, C.A., Jaunarajs, S., Libby, B., Malcolm, M., Robb, E., Taggart, J.E., Threlkeld, C.N., Vuletich, A., Cunningham, C.G., Ashley, R.P., and Chou, I., 1988, Data on the geochemistry and thermal maturation of sedimentary-rock hosted, disseminated gold deposits and associated rocks, southwestern Guizhou Province, People's Republic of China: U.S. Geological Survey Open-File Report 88-271, 22 p. :ill., map ;28 cm., https://doi.org/10.3133/ofr88271.","productDescription":"22 p. :ill., map ;28 cm.","costCenters":[],"links":[{"id":145643,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1988/0271/report-thumb.jpg"},{"id":39995,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1988/0271/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e47a3e4b07f02db4965a1","contributors":{"authors":[{"text":"Dean, W.E.","contributorId":97099,"corporation":false,"usgs":true,"family":"Dean","given":"W.E.","email":"","affiliations":[],"preferred":false,"id":164626,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bostick, N. 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L.","contributorId":40997,"corporation":false,"usgs":true,"family":"Brandt","given":"E.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":164617,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Daws, T.A.","contributorId":56651,"corporation":false,"usgs":true,"family":"Daws","given":"T.A.","email":"","affiliations":[],"preferred":false,"id":164620,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Doughten, M.","contributorId":61830,"corporation":false,"usgs":true,"family":"Doughten","given":"M.","affiliations":[],"preferred":false,"id":164621,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Gent, C. A.","contributorId":17955,"corporation":false,"usgs":true,"family":"Gent","given":"C.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":164613,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Jaunarajs, S.R.","contributorId":25160,"corporation":false,"usgs":true,"family":"Jaunarajs","given":"S.R.","email":"","affiliations":[],"preferred":false,"id":164615,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Libby, B.","contributorId":16421,"corporation":false,"usgs":true,"family":"Libby","given":"B.","email":"","affiliations":[],"preferred":false,"id":164612,"contributorType":{"id":1,"text":"Authors"},"rank":9},{"text":"Malcolm, M.J.","contributorId":95064,"corporation":false,"usgs":true,"family":"Malcolm","given":"M.J.","email":"","affiliations":[],"preferred":false,"id":164625,"contributorType":{"id":1,"text":"Authors"},"rank":10},{"text":"Robb, E.C.","contributorId":23549,"corporation":false,"usgs":true,"family":"Robb","given":"E.C.","email":"","affiliations":[],"preferred":false,"id":164614,"contributorType":{"id":1,"text":"Authors"},"rank":11},{"text":"Taggart, J. E.","contributorId":14829,"corporation":false,"usgs":true,"family":"Taggart","given":"J.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":164611,"contributorType":{"id":1,"text":"Authors"},"rank":12},{"text":"Threlkeld, C. N.","contributorId":80271,"corporation":false,"usgs":true,"family":"Threlkeld","given":"C.","email":"","middleInitial":"N.","affiliations":[],"preferred":false,"id":164624,"contributorType":{"id":1,"text":"Authors"},"rank":13},{"text":"Vuletich, A.K.","contributorId":43784,"corporation":false,"usgs":true,"family":"Vuletich","given":"A.K.","affiliations":[],"preferred":false,"id":164618,"contributorType":{"id":1,"text":"Authors"},"rank":14},{"text":"Cunningham, C. G.","contributorId":76741,"corporation":false,"usgs":true,"family":"Cunningham","given":"C.","middleInitial":"G.","affiliations":[],"preferred":false,"id":164623,"contributorType":{"id":1,"text":"Authors"},"rank":15},{"text":"Ashley, R. P.","contributorId":50513,"corporation":false,"usgs":true,"family":"Ashley","given":"R.","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":164619,"contributorType":{"id":1,"text":"Authors"},"rank":16},{"text":"Chou, I-Ming 0000-0001-5233-6479 imchou@usgs.gov","orcid":"https://orcid.org/0000-0001-5233-6479","contributorId":882,"corporation":false,"usgs":true,"family":"Chou","given":"I-Ming","email":"imchou@usgs.gov","affiliations":[{"id":245,"text":"Eastern Mineral and Environmental Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":164610,"contributorType":{"id":1,"text":"Authors"},"rank":17}]}}
,{"id":36222,"text":"b1827 - 1988 - Segmentation of the Wasatch fault zone, Utah — Summaries, analyses, and interpretations of geological and geophysical data","interactions":[],"lastModifiedDate":"2021-12-21T21:13:05.684876","indexId":"b1827","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":306,"text":"Bulletin","code":"B","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1827","title":"Segmentation of the Wasatch fault zone, Utah — Summaries, analyses, and interpretations of geological and geophysical data","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/b1827","usgsCitation":"Wheeler, R.L., and Krystinik, K.B., 1988, Segmentation of the Wasatch fault zone, Utah — Summaries, analyses, and interpretations of geological and geophysical data: U.S. Geological Survey Bulletin 1827, iv, 47 p., https://doi.org/10.3133/b1827.","productDescription":"iv, 47 p.","costCenters":[],"links":[{"id":64170,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/1827/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":166592,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/1827/report-thumb.jpg"},{"id":393259,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_21963.htm"}],"country":"United States","state":"Utah","otherGeospatial":"Wasatch fault zone","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -112.5,\n              39\n            ],\n            [\n              -111.5,\n              39\n            ],\n            [\n              -111.5,\n              42\n            ],\n            [\n              -112.5,\n              42\n            ],\n            [\n              -112.5,\n              39\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ae4b07f02db5fb9d4","contributors":{"authors":[{"text":"Wheeler, Russell L. wheeler@usgs.gov","contributorId":858,"corporation":false,"usgs":true,"family":"Wheeler","given":"Russell","email":"wheeler@usgs.gov","middleInitial":"L.","affiliations":[],"preferred":false,"id":215971,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Krystinik, Katherine B.","contributorId":77989,"corporation":false,"usgs":true,"family":"Krystinik","given":"Katherine","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":215972,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":12611,"text":"ofr8878 - 1988 - Data for ground-water test holes in Fresno County, western San Joaquin Valley, California, June to August 1985","interactions":[],"lastModifiedDate":"2012-02-02T00:06:41","indexId":"ofr8878","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","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":"88-78","title":"Data for ground-water test holes in Fresno County, western San Joaquin Valley, California, June to August 1985","docAbstract":"Twenty-four test holes were drilled from June 3 to August 29, 1985, in the western San Joaquin Valley, California, to provide information about groundwater hydraulics and geochemistry. The study area is in western Fresno County, west of the San Joaquin River, and east of the Coast Range. Lithologic, hydrologic, and geophysical data were collected from test holes drilled at two cluster sites and at 13 additional sites. Both cluster sites have five cased test holes. A sixth test hole was drilled at one of the cluster sites but was destroyed. Each of the 10 cased test holes is perforated at a different 10-ft depth interval. Six of the 13 additional test holes were also cased. Lithology logs were constructed from descriptions of cuttings and cores recovered during drilling. Geophysical logs were made of the deepest hole at each cluster site. Initial water level measurements were made at most sites. (Author 's abstract)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr8878","usgsCitation":"Beard, S., and Laudon, J., 1988, Data for ground-water test holes in Fresno County, western San Joaquin Valley, California, June to August 1985: U.S. Geological Survey Open-File Report 88-78, iv, 39 p. :ill., map ;28 cm., https://doi.org/10.3133/ofr8878.","productDescription":"iv, 39 p. :ill., map ;28 cm.","costCenters":[],"links":[{"id":145615,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1988/0078/report-thumb.jpg"},{"id":41017,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1988/0078/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67c922","contributors":{"authors":[{"text":"Beard, Sherrill","contributorId":67098,"corporation":false,"usgs":true,"family":"Beard","given":"Sherrill","email":"","affiliations":[],"preferred":false,"id":166417,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Laudon, Julie","contributorId":68320,"corporation":false,"usgs":true,"family":"Laudon","given":"Julie","email":"","affiliations":[],"preferred":false,"id":166418,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":16682,"text":"ofr88471 - 1988 - Chemical and hydrologic data for selected thermal-water wells and nonthermal springs in the Boise Area, southwesten Idaho","interactions":[],"lastModifiedDate":"2012-02-02T00:07:05","indexId":"ofr88471","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","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":"88-471","title":"Chemical and hydrologic data for selected thermal-water wells and nonthermal springs in the Boise Area, southwesten Idaho","docAbstract":"Data were collected during January to July 1988 from 37 thermal-water wells and 3 nonthermal springs in the Boise area, southwestern Idaho. Included are well and spring locations; well-construction, water-level, and water-use information; hydrographs of water levels in 3 wells; chemical and isotopic analyses of water from 18 thermal-water wells and 3 nonthermal springs; and drillers ' logs from 23 wells. The purpose of the report is to make these data conveniently available to the public. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr88471","usgsCitation":"Young, H., Parliman, D., and Mariner, R.H., 1988, Chemical and hydrologic data for selected thermal-water wells and nonthermal springs in the Boise Area, southwesten Idaho: U.S. Geological Survey Open-File Report 88-471, iv, 35 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr88471.","productDescription":"iv, 35 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":149042,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1988/0471/report-thumb.jpg"},{"id":45754,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1988/0471/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e1e4b07f02db5e4841","contributors":{"authors":[{"text":"Young, H.W.","contributorId":68278,"corporation":false,"usgs":true,"family":"Young","given":"H.W.","email":"","affiliations":[],"preferred":false,"id":173280,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Parliman, D. J.","contributorId":64220,"corporation":false,"usgs":true,"family":"Parliman","given":"D. J.","affiliations":[],"preferred":false,"id":173279,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Mariner, Robert H.","contributorId":81075,"corporation":false,"usgs":true,"family":"Mariner","given":"Robert","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":173281,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":25848,"text":"wri884233 - 1988 - Water quality of Lake Austin and Town Lake, Austin, Texas","interactions":[],"lastModifiedDate":"2016-08-10T15:48:48","indexId":"wri884233","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","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":"88-4233","title":"Water quality of Lake Austin and Town Lake, Austin, Texas","docAbstract":"<p>Lake Austin and Town Lake are located on the Colorado River in Travis County, central Texas, and serve as a source of water for municipal and industrial water supplies, electrical-power generation, and recreation for more than 500,000 people in the Austin metropolitan area. Lake Austin, located immediately downstream of Lake Travis, extends for more than 20 miles into the western edge of the city of Austin. Town Lake extends through the downtown area of the city of Austin for nearly 6 miles where the Colorado River is impounded by Longhorn Dam.</p>\n<p>Many of the detrimental effects of impoundment of water in a lake or reservoir are related to thermal stratification, which generally does not occur in Lake Austin or in Town Lake. The largest detected difference in vertical temperature was 6.5 degrees Celsius in Lake Austin and 3.5 degrees Celsius in Town Lake. The small vertical temperature variations in both lakes can be attributed to shallow depths in the lakes and to the short retention times of water in the lakes during the summer months.</p>\n<p>Large vertical dissolved-oxygen gradients were not detected in Lake Austin and Town Lake. Average dissolved-oxygen concentrations for Lake Austin at site Ac, a deep site (about 50 feet) at the dam, differ by about 2.5 milligrams per liter from surface to bottom during the summer. At site Ac on Town Lake, average dissolved-oxygen concentrations differ by about 1 milligram per liter from surface to bottom. The largest areal variations in dissolved oxygen generally occur in Lake Austin during the summer. Water released to Lake Austin during the summer is from below the thermocline in Lake Travis, and consequently, dissolved-oxygen concentrations generally are small. For example, in August 1984, dissolved-oxygen concentrations in Lake Austin increased from 2.8 milligrams per liter in the headwaters to slightly greater than 7.0 milligrams per liter approximately 14 miles downstream. This increase in dissolved oxygen was caused by reaeration from the atmosphere and from photosynthetic production of oxygen by aquatic plants.</p>\n<p>Dissolved trace-element data collected from Lake Austin and Town Lake indicate that with the exception of iron, manganese, and mercury, none of the dissolved trace elements analyzed for exceeded either the primary maximum contaminant level or secondary maximum contaminant level set by the U.S. Environmental Protection Agency. Average concentrations of dissolved iron and dissolved manganese in water collected near the bottom of Lake Austin did not exceed 40 and 50 micrograms per liter, respectively.</p>\n<p>Little seasonal or areal variation was noted in nitrogen concentrations in Lake Austin or Town Lake. Organic nitrogen is the predominant nitrogen&nbsp;species in both lakes. Stormwater runoff had little effect on nitrogen concentrations in Lake Austin. Nitrogen concentrations in Town Lake were slightly larger following periods of runoff. Total nitrogen concentrations in Town Lake following periods of runoff often exceed 1.0 milligram per liter.</p>\n<p>Total phosphorus concentrations are small in Lake Austin and Town Lake. About 95 percent of the total phosphorus concentrations measured in Lake Austin and about 81 percent of the total phosphorus concentrations measured in Town Lake were less than 0.03 milligram per liter. Total phosphorus concentrations are largest in Town Lake following periods of runoff.</p>\n<p>Dissolved-solids concentrations ranged from 240 to 340 milligrams per liter in Lake Austin and from 170 to 360 milligrams per liter in Town Lake. The smallest concentrations of dissolved solids in Town Lake occurred following periods of runoff. During periods of no runoff, dissolved-solids concentrations in Town Lake ranged from 240 to 360 milligrams per liter, which was very similar to the range in Lake Austin.</p>\n<p>Densities of feca1-coliform bacteria in Lake Austin ranged from less than 1 to 600 colonies per 100 milliliters, and densities of fecal-streptococci bacteria ranged from less than 1 to 340 colonies per 100 milliliters. Densities of fecal-coliform bacteria in Town Lake ranged from 4 to 14,000 colonies per 100 milliliters, and densities of fecal-streptococci bacteria ranged from less than 1 to 15,000 colonies per 100 milliliters. The largest densities of both bacteria in Town Lake occurred following runoff.</p>\n<p>Little or no effect of stormwater runoff on temperature, dissolved oxygen, or trace elements was detected in either Lake Austin or Town Lake. Increased concentrations of total nitrogen and phosphorus were detected in Town Lake, but not in Lake Austin following runoff. A decrease in concentrations of dissolved solids and major ions occurred in Town Lake, but not in Lake Austin, following runoff. Densities of fecal-coliform and fecal-streptococci bacteria were larger in Lake Austin and Town Lake following runoff, but significantly larger increases were noted in Town Lake.</p>\n<p>Water-quality data collected from Lake Austin and Town Lake, following runoff, generally were not adequate to fully determine the effects of runoff on the lakes. Data collection should not to be limited to fixed-station sampling following runoff, and both lakes need to be sampled simultaneously as soon as possible following significant precipitation.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Austin, TX","doi":"10.3133/wri884233","usgsCitation":"Andrews, F.L., Wells, F.C., Shelby, W.J., and McPherson, E., 1988, Water quality of Lake Austin and Town Lake, Austin, Texas: U.S. Geological Survey Water-Resources Investigations Report 88-4233, vii, 322 p., https://doi.org/10.3133/wri884233.","productDescription":"vii, 322 p.","numberOfPages":"329","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":158245,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1988/4233/report-thumb.jpg"},{"id":54592,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1988/4233/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b15e4b07f02db6a4dac","contributors":{"authors":[{"text":"Andrews, Freeman L.","contributorId":91486,"corporation":false,"usgs":true,"family":"Andrews","given":"Freeman","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":195328,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wells, Frank C.","contributorId":80664,"corporation":false,"usgs":true,"family":"Wells","given":"Frank","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":645150,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Shelby, Wanda J.","contributorId":173579,"corporation":false,"usgs":false,"family":"Shelby","given":"Wanda","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":645151,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"McPherson, Emma","contributorId":85629,"corporation":false,"usgs":true,"family":"McPherson","given":"Emma","email":"","affiliations":[],"preferred":false,"id":645152,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":12646,"text":"ofr87573 - 1988 - Character and evolution of the ground-water flow system in the central part of the western San Joaquin Valley, California","interactions":[{"subject":{"id":12646,"text":"ofr87573 - 1988 - Character and evolution of the ground-water flow system in the central part of the western San Joaquin Valley, California","indexId":"ofr87573","publicationYear":"1988","noYear":false,"title":"Character and evolution of the ground-water flow system in the central part of the western San Joaquin Valley, California"},"predicate":"SUPERSEDED_BY","object":{"id":1007,"text":"wsp2348 - 1990 - Character and evolution of the ground-water flow system in the central part of the western San Joaquin Valley, California","indexId":"wsp2348","publicationYear":"1990","noYear":false,"title":"Character and evolution of the ground-water flow system in the central part of the western San Joaquin Valley, California"},"id":1}],"supersededBy":{"id":1007,"text":"wsp2348 - 1990 - Character and evolution of the ground-water flow system in the central part of the western San Joaquin Valley, California","indexId":"wsp2348","publicationYear":"1990","noYear":false,"title":"Character and evolution of the ground-water flow system in the central part of the western San Joaquin Valley, California"},"lastModifiedDate":"2019-03-08T12:24:51","indexId":"ofr87573","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","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":"87-573","title":"Character and evolution of the ground-water flow system in the central part of the western San Joaquin Valley, California","docAbstract":"<p>The occurrence of selenium in agricultural drain water derived from the western San Joaquin Valley, California, has focused concern on the ground-water flow system of the western valley. In this investigation, previous work and recently collected texture and water-level data are used to evaluate the character and evolution of the regional ground-water flow system in the central part of the western valley, with particular emphasis on the deposits overlying the Corcoran Clay Member of the Tulare Formation.</p><p>The Corcoran Clay Member, where present, divides the flow system into an upper semiconfined zone and a lower con-fined zone. Above the Corcoran, three hydrogeologic units can be recognized: Coast Range alluvium, Sierran sand, and flood-basin deposits. These units differ in texture, hydrologic properties, and oxidation state.</p><p>The development of irrigated agriculture in the central part of the western valley has significantly altered the flow system. Percolation of irrigation water past crop roots has caused a rise in the altitude of the water table in midfan and distal-fan areas. Pumpage of ground water from wells has caused a lowering of the water table beneath parts of the fanheads and a lowering of the potentiometric surface of the confined zone over much of the western valley. The combination of percolation and pumpage has resulted in development of a large downward hydraulic head gradient in the semi-confined zone and has created a groundwater divide along the western margin of the valley. Surface-water deliveries from the California Aqueduct have allowed a decrease in pumpage and a consequent recovery in hydraulic head throughout the system.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr87573","usgsCitation":"Belitz, K., 1988, Character and evolution of the ground-water flow system in the central part of the western San Joaquin Valley, California: U.S. Geological Survey Open-File Report 87-573, iv, 34 p., https://doi.org/10.3133/ofr87573.","productDescription":"iv, 34 p.","costCenters":[],"links":[{"id":361896,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1987/0573/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":143778,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1987/0573/report-thumb.jpg"}],"country":"United States","state":"California","otherGeospatial":"San Joaquin Valley","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -120.75,\n              36\n            ],\n            [\n              -119.75,\n              36\n            ],\n            [\n              -119.75,\n              37\n            ],\n            [\n              -120.75,\n              37\n            ],\n            [\n              -120.75,\n              36\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e3e4b07f02db5e5546","contributors":{"authors":[{"text":"Belitz, Kenneth 0000-0003-4481-2345 kbelitz@usgs.gov","orcid":"https://orcid.org/0000-0003-4481-2345","contributorId":442,"corporation":false,"usgs":true,"family":"Belitz","given":"Kenneth","email":"kbelitz@usgs.gov","affiliations":[{"id":451,"text":"National Water Quality Assessment Program","active":true,"usgs":true},{"id":466,"text":"New England Water Science Center","active":true,"usgs":true},{"id":376,"text":"Massachusetts Water Science Center","active":true,"usgs":true},{"id":27111,"text":"National Water Quality Program","active":true,"usgs":true},{"id":503,"text":"Office of Water Quality","active":true,"usgs":true}],"preferred":true,"id":166476,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":57414,"text":"wdrOH871 - 1988 - Water resources data for Ohio, 1987. Volume 1: Ohio River Basin","interactions":[],"lastModifiedDate":"2020-11-02T16:34:23.337269","indexId":"wdrOH871","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"OH-87-1","title":"Water resources data for Ohio, 1987. Volume 1: Ohio River Basin","docAbstract":"<p>No abstract available.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wdrOH871","usgsCitation":"Shindel, H., Klingler, J., Mangus, J., and Trimble, L., 1988, Water resources data for Ohio, 1987. 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L.E.","contributorId":101732,"corporation":false,"usgs":true,"family":"Trimble","given":"L.E.","email":"","affiliations":[],"preferred":false,"id":256959,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":14602,"text":"ofr88694 - 1988 - Data report for the PACE 1987 seismic refraction survey, west-central Arizona","interactions":[],"lastModifiedDate":"2012-02-02T00:06:59","indexId":"ofr88694","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","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":"88-694","title":"Data report for the PACE 1987 seismic refraction survey, west-central Arizona","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr88694","usgsCitation":"Larkin, S.P., McCarthy, J., and Fuis, G.S., 1988, Data report for the PACE 1987 seismic refraction survey, west-central Arizona: U.S. Geological Survey Open-File Report 88-694, 95 p. ill., maps ;28 cm., https://doi.org/10.3133/ofr88694.","productDescription":"95 p. ill., maps ;28 cm.","costCenters":[],"links":[{"id":147851,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1988/0694/report-thumb.jpg"},{"id":43265,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1988/0694/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac5e4b07f02db679cc3","contributors":{"authors":[{"text":"Larkin, Steven P.","contributorId":85204,"corporation":false,"usgs":true,"family":"Larkin","given":"Steven","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":169723,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"McCarthy, Jill jmccarthy@usgs.gov","contributorId":2732,"corporation":false,"usgs":true,"family":"McCarthy","given":"Jill","email":"jmccarthy@usgs.gov","affiliations":[],"preferred":true,"id":169722,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Fuis, Gary S. 0000-0002-3078-1544 fuis@usgs.gov","orcid":"https://orcid.org/0000-0002-3078-1544","contributorId":2639,"corporation":false,"usgs":true,"family":"Fuis","given":"Gary","email":"fuis@usgs.gov","middleInitial":"S.","affiliations":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true}],"preferred":true,"id":169721,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":36013,"text":"b1852 - 1988 - Toward a Federal Land Information System: Experiences and issues","interactions":[],"lastModifiedDate":"2017-03-27T14:52:56","indexId":"b1852","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":306,"text":"Bulletin","code":"B","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1852","title":"Toward a Federal Land Information System: Experiences and issues","docAbstract":"<p>From 1983 to 1987, the U.S. Geological Survey conducted research to develop a national resource data base of Federal lands under the auspices of the Federal Land Information System (FLIS) program. The program's goal was to develop the capability to provide information to national mineral-use policymakers. Prototype spatial data bases containing mineral, land status, and base cartographic data were developed for the Medford, Oreg., area, the State of Alaska, and the Silver City, N. Mex., area. Other accomplishments included (1) the preparation of a digital format for U.S. Geological Survey mineral assessment data and (2) the development of a procedure for integrating parcel-level tabular Alaska land status data into a section-level geographic information system. Overall findings indicated that both vector and raster capabilities are required for a FLIS and that nationwide data availability is a limiting factor in FLIS development. </p><p>As a result of a 1986 interbureau (U.S. Geological Survey, Bureau of Land Management, and Bureau of Mines) review of the FLIS program, activities were redirected to undertake research on large-area geographic information system techniques. Land use and land cover data generalization strategies were tested, and areafiltering software was found to be the optimum type. In addition, a procedure was developed for transferring tabular land status data of surveyed areas in the contiguous 48 States to spatial data for use in geographic information systems. </p><p>The U.S. Geological Survey FLIS program, as an administrative unit, ended in 1987, but FLIS-related research on large-area geographic information systems continues. </p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/b1852","usgsCitation":"Sturdevant, J.A., 1988, Toward a Federal Land Information System: Experiences and issues: U.S. Geological Survey Bulletin 1852, iv, 15 p., https://doi.org/10.3133/b1852.","productDescription":"iv, 15 p.","costCenters":[{"id":222,"text":"Earth Resources Observation and Science (EROS) Center","active":true,"usgs":true}],"links":[{"id":63961,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/1852/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":163620,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/1852/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4ee4b07f02db62813f","contributors":{"authors":[{"text":"Sturdevant, James A.","contributorId":67563,"corporation":false,"usgs":true,"family":"Sturdevant","given":"James","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":215616,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":57411,"text":"wdrSD871 - 1988 - Water resources data, South Dakota, water year 1987","interactions":[],"lastModifiedDate":"2024-08-07T19:21:41.466384","indexId":"wdrSD871","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"SD-87-1","title":"Water resources data, South Dakota, water year 1987","docAbstract":"<p>Water Resources Data for the 1987 water year for South Dakota consists of records of stage, discharge, and water quality of streams; stage, contents, and water quality of lakes and reservoirs; and water levels in wells. This report contains discharge records for 114 streamflow-gaging stations; stage and contents records for 10 lakes and reservoirs, stage for 2 streams and 2 lakes; water-quality records for 25 stream-gaging stations, 3 wells, 6 ungaged streamsites, 3 lakes, 1 sewage lagoon, and 1 precipitation site; water levels for 31 wells; and precipitation records at 9 sites. Additional water data were collected at various sites, not part of the systematic data-collection program, and are published as miscellaneous measurements and analyses. 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 South Dakota.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wdrSD871","collaboration":"Prepared in cooperation with the State of South Dakota  and with other agencies","usgsCitation":"Hoffman, E., Benson, R., and Lawrence, S., 1988, Water resources data, South Dakota, water year 1987: U.S. Geological Survey Water Data Report SD-87-1, ix, 307 p., https://doi.org/10.3133/wdrSD871.","productDescription":"ix, 307 p.","costCenters":[],"links":[{"id":414281,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wdr/1987/sd-87-1/report-thumb.jpg"},{"id":432379,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/1987/sd-87-1/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"South 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,{"id":57406,"text":"wdrSC871 - 1988 - Water resources data for South Carolina, water year 1987","interactions":[],"lastModifiedDate":"2020-10-23T18:54:24.954626","indexId":"wdrSC871","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"SC-87-1","title":"Water resources data for South Carolina, water year 1987","docAbstract":"<p>No abstract available.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wdrSC871","usgsCitation":"Bennett, C., Hayes, R., Jones, K., and Cooney, T., 1988, Water resources data for South Carolina, water year 1987: U.S. Geological Survey Water Data Report SC-87-1, viii, 486 p., https://doi.org/10.3133/wdrSC871.","productDescription":"viii, 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,{"id":12373,"text":"ofr88100 - 1988 - Water-resources activities of the U.S. Geological Survey in Texas– Fiscal year 1987","interactions":[],"lastModifiedDate":"2021-12-03T21:01:27.335323","indexId":"ofr88100","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","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":"88-100","title":"Water-resources activities of the U.S. Geological Survey in Texas– Fiscal year 1987","docAbstract":"<p>The U.S. Geological Survey (USGS) was established by an act of Congress on March 3, 1879, to provide a permanent Federal agency to conduct the systematic and scientific classification of the public lands and to examine the geological structure, mineral resources, and products of national domain. An integral part of that original mission includes publishing and disseminating the earth science information needed to understand, to plan the use of, and to manage the Nation's energy, land, mineral, and water resources.</p>\n<p>Since 1879, the research and fact-finding role of the USGS has grown and been modified to meet the changing needs of the Nation it serves. As part of that evolution, the USGS has become the Federal Government's largest earthscience research agency, the Nation's largest civilian mapmaking agency, the primary source of data on the Nation's surface- and ground-water resources, and the employer of the largest number of professional earth scientists. Today's programs serve a diversity of needs and users. Programs include:</p>\n<ul>\n<li>Conducting detailed assessments of the energy and mineral potential of the Nation's land and offshore areas.</li>\n<li>Investigating and issuing warnings of earthquakes, volcanic eruptions, landslides, and other geologic and hydrologic hazards.</li>\n<li>Conducting research on the geologic structure of the Nation.</li>\n<li>Studying the geologic features, structure, processes, and history of the other planets of our solar system.</li>\n<li>Conducting topographic surveys of the Nation and preparing topographic and thematic maps and related cartographic products.</li>\n<li>Developing and producing digital cartographic data bases and products.</li>\n<li>Collecting data on a routine basis to determine the quantity, quality, and use of surface and ground water.</li>\n<li>Conducting water-resources appraisals in order to describe the consequences of alternative plans for developing land and water resources.</li>\n<li>Conducting research in hydraulics and 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,{"id":16301,"text":"ofr8740 - 1988 - Aggregation of Minnesota water-use data and transfer of data to the National Water-Use Data System; Procedures and programs","interactions":[],"lastModifiedDate":"2018-04-02T11:46:34","indexId":"ofr8740","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","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":"87-40","title":"Aggregation of Minnesota water-use data and transfer of data to the National Water-Use Data System; Procedures and programs","docAbstract":"<p>The Minnesota Water-Use Data System stores data on the quantity of withdrawals and discharge in Minnesota. To transfer these data into the U.S. Geological Survey 's National Water-Use Data System properly, certain procedures must be followed. Uniform data categorization and entry allows comparison of water use from State to State. The data in the National Water-Use Data System are aggregated by county and by watershed (hydrologic unit). This report documents the data aggregation and transfer process as developed by the Minnesota Department of Natural Resources, the Minnesota State Planning Agency/Planning Information Center, and the U.S. Geological Survey as part of the National Water-Use Information Program.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"St. Paul, MN","doi":"10.3133/ofr8740","collaboration":"Prepared in cooperation with the Minnesota Department of Natural Resources and the Minnesota State Planning Agency","usgsCitation":"Trotta, L.C., 1988, Aggregation of Minnesota water-use data and transfer of data to the National Water-Use Data System; Procedures and programs: U.S. Geological Survey Open-File Report 87-40, iv, 71 p., https://doi.org/10.3133/ofr8740.","productDescription":"iv, 71 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":392,"text":"Minnesota Water Science 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 \"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae3e4b07f02db689125","contributors":{"authors":[{"text":"Trotta, L. C.","contributorId":63410,"corporation":false,"usgs":true,"family":"Trotta","given":"L.","email":"","middleInitial":"C.","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":172574,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":16302,"text":"ofr88466 - 1988 - Inventory of interbasin water transfers in Minnesota","interactions":[],"lastModifiedDate":"2018-04-02T11:47:01","indexId":"ofr88466","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","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":"88-466","title":"Inventory of interbasin water transfers in Minnesota","docAbstract":"<p>Water transfer data were collected by the U.S. Geological Survey , in cooperation with the Minnesota Department of Natural Resources, from the 13 hydrologic subregions in Minnesota. About 30,000 acre-ft of water is exported annually from eight of these subregions. Interbasin transfer of water is classified according to type of water conveyance in Minnesota. This information is needed by water-system managers and planners to develop water budgets for major river basins, to examine the extent of existing interbasin transfers, and to evaluate the feasibility of transferring water to meet regional water demands.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"St. Paul, MN","doi":"10.3133/ofr88466","collaboration":"Prepared in cooperation with the Minnesota Department of Natural Resources","usgsCitation":"Trotta, L.C., 1988, Inventory of interbasin water transfers in Minnesota: U.S. Geological Survey Open-File Report 88-466, iii, 15 p., https://doi.org/10.3133/ofr88466.","productDescription":"iii, 15 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":392,"text":"Minnesota Water Science 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,{"id":12667,"text":"ofr87679 - 1988 - Geophysical logs and hydrologic data for eight wells in the Coyote Spring Valley area, Clark and Lincoln counties, Nevada","interactions":[],"lastModifiedDate":"2012-02-02T00:06:32","indexId":"ofr87679","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","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":"87-679","title":"Geophysical logs and hydrologic data for eight wells in the Coyote Spring Valley area, Clark and Lincoln counties, Nevada","docAbstract":"Geophysical logs, drilling operations, pump-test data, and water quality determinations are presented for eight wells in the Coyote Spring Valley area of southeastern Nevada. The wells are in an area where thick units of Paleozoic carbonate rock are overlain by Tertiary semiconsolidated basin-fill deposits and Quaternary alluvial deposits. Data collected by the U.S. Geological Survey were augmented with data from previous investigations; however, complete sets of logs and other data are not available for all eight wells. Geophysical data presented included natural-gamma, neutron, gamma-gamma density, caliper, temperature, acoustic, single-point resistance, long- and short-natural resistivity, and spontaneous-potential logs. Drilling penetration rates, lithologic columns, and well construction are also summarized and presented. Measurements of drawdown and recovery during and after constant-discharge pumping periods are also included. Also presented are results of chemical and physical analyses for major-ion chemistry, trace constituents, stable and radioactive isotopes, temperature, pH, specific conductance, and dissolved oxygen. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr87679","usgsCitation":"Berger, D., Kilroy, K., and Schaefer, D.H., 1988, Geophysical logs and hydrologic data for eight wells in the Coyote Spring Valley area, Clark and Lincoln counties, Nevada: U.S. Geological Survey Open-File Report 87-679, vii, 58 p. :ill., map ;28 cm., https://doi.org/10.3133/ofr87679.","productDescription":"vii, 58 p. :ill., map ;28 cm.","costCenters":[],"links":[{"id":143704,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1987/0679/report-thumb.jpg"},{"id":41075,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1987/0679/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1ae4b07f02db6a8602","contributors":{"authors":[{"text":"Berger, D.L.","contributorId":106904,"corporation":false,"usgs":true,"family":"Berger","given":"D.L.","email":"","affiliations":[],"preferred":false,"id":166514,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kilroy, K. C.","contributorId":49795,"corporation":false,"usgs":true,"family":"Kilroy","given":"K. C.","affiliations":[],"preferred":false,"id":166512,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Schaefer, D. H.","contributorId":84763,"corporation":false,"usgs":true,"family":"Schaefer","given":"D.","middleInitial":"H.","affiliations":[],"preferred":false,"id":166513,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":57647,"text":"wdrID871 - 1988 - Water Resources Data for Idaho, Water Year 1987","interactions":[],"lastModifiedDate":"2012-02-02T00:12:13","indexId":"wdrID871","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"ID-87-1","title":"Water Resources Data for Idaho, Water Year 1987","language":"ENGLISH","doi":"10.3133/wdrID871","usgsCitation":"Harenberg, W., Jones, M., O'Dell, I., and Cordes, S., 1988, Water Resources Data for Idaho, Water Year 1987: U.S. Geological Survey Water Data Report ID-87-1, 655 p., https://doi.org/10.3133/wdrID871.","productDescription":"655 p.","costCenters":[],"links":[{"id":185305,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b15e4b07f02db6a4ecf","contributors":{"authors":[{"text":"Harenberg, W. A.","contributorId":78743,"corporation":false,"usgs":true,"family":"Harenberg","given":"W. A.","affiliations":[],"preferred":false,"id":257601,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Jones, M.L.","contributorId":88731,"corporation":false,"usgs":true,"family":"Jones","given":"M.L.","email":"","affiliations":[],"preferred":false,"id":257603,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"O'Dell, I.","contributorId":80336,"corporation":false,"usgs":true,"family":"O'Dell","given":"I.","affiliations":[],"preferred":false,"id":257602,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Cordes, S.C.","contributorId":106196,"corporation":false,"usgs":true,"family":"Cordes","given":"S.C.","email":"","affiliations":[],"preferred":false,"id":257604,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":26983,"text":"wri874082 - 1988 - A digital simulation of the glacial-aquifer system in Sanborn and parts of Beadle, Miner, Hanson, Davison, and Jerauld counties, South Dakota","interactions":[],"lastModifiedDate":"2012-02-02T00:08:44","indexId":"wri874082","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","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":"87-4082","title":"A digital simulation of the glacial-aquifer system in Sanborn and parts of Beadle, Miner, Hanson, Davison, and Jerauld counties, South Dakota","docAbstract":"The drought in South Dakota from 1974-76 and the near drought conditions in 1980-81 have resulted in increased demands on the groundwater resources within many of the irrigated areas of the James River basin in eastern South Dakota. These increases in demand for irrigation water from the glacial aquifer system, and continued requests to the State for additional irrigation well permits, have created a need for a systematic water management program to avoid over-development of this system in the James River basin. An equally spaced grid containing 56 rows and 52 columns used to simulate the glacial aquifer system, was calibrated using water level data collected before significant groundwater development (before 1973). The aquifer was also simulated in 11 annual transient stress periods from 1973 through 1983 and in 12 monthly transient stress periods for 1976. The simulated pre-development potentiometric heads were compared to average water levels from 32 observation wells to check the accuracy of the simulate potentiometric surface. The average arithmetic difference between the simulated and observed water levels was 1.68 ft and the average absolute difference was 4.38 ft. The non-pumping steady-state simulated water budget indicates that recharge from precipitation accounts for 97.1% of the water entering the aquifer and evapotranspiration accounts for 98.2% of the water leaving the aquifer. The sensitivity analysis of the steady-state model indicates that the model is most sensitive to reductions in recharge and least to changes in hydraulic conductivity. The maximum annual recharge varied from 0.10 inch in 1976 to 8.14 inches in 1977. The potential annual evapotranspiration varied from 29.9 inches in 1982 to 48.9 inches in 1976. Withdrawals from the glacial aquifer system increased 2.6 times between 1975 and 1976. The average annual arithmetic difference between the simulated and observed water levels ranged from 3.88 ft in 1974 to 2.23 ft in 1982; the average absolute difference ranged from 4.70 ft in 1973 to 11.70 ft in 1982. In the 1976 monthly transient simulation, the maximum annual recharge rate 0.10 inch was distributed over the months of March, April, and September. The potential monthly evapotranspiration rate ranged from 12.50 inches in August to 0.00 inch during the winter when the ground was frozen. (Author 's abstract)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri874082","usgsCitation":"Emmons, P., 1988, A digital simulation of the glacial-aquifer system in Sanborn and parts of Beadle, Miner, Hanson, Davison, and Jerauld counties, South Dakota: U.S. Geological Survey Water-Resources Investigations Report 87-4082, v, 59 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri874082.","productDescription":"v, 59 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":124046,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1987/4082/report-thumb.jpg"},{"id":55870,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1987/4082/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b25e4b07f02db6aed4d","contributors":{"authors":[{"text":"Emmons, P.J.","contributorId":60630,"corporation":false,"usgs":true,"family":"Emmons","given":"P.J.","email":"","affiliations":[],"preferred":false,"id":197359,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":12422,"text":"ofr88604 - 1988 - Zircon morphology and U-Pb geochronology of seven metaluminous and peralkaline post-orogenic granite complexes of the Arabian Shield, Kingdom of Saudi Arabia","interactions":[],"lastModifiedDate":"2015-09-02T19:09:32","indexId":"ofr88604","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","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":"88-604","title":"Zircon morphology and U-Pb geochronology of seven metaluminous and peralkaline post-orogenic granite complexes of the Arabian Shield, Kingdom of Saudi Arabia","docAbstract":"<p>The U-Pb zircon method was used to determine the ages of seven metaluminous-to-peralkaline post-orogenic granites located throughout the Late Proterozoic Arabian Shield of Saudi Arabia. Zircons from the metaluminous rocks are prismatic, with length-to-width ratios of about 2-4:1 and small pyramidal terminations. In contrast, zircons from three of the four peralkaline complexes either lack well developed prismatic faces (are pseudo-octahedral) or are anhedral. Some of the zircons from the peralkaline granites contain inherited radiogenic lead. This complicates interpretation of the isotopic data and. in many cases, may make the U-Pb method unsuitable for determining the age of a peralkaline granite. Zircons in the metaluminous granites do not contain inheritance and thus, best-fit chords calculated through the data have upper concordia intercepts that indicate the age of intrusion, and lower intercepts that indicate simple episodic lead loss. The results show that these granites were emplaced during multiple intrusive episodes from 670 to 510 Ma (Late Proterozoic to Cambrian).</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr88604","usgsCitation":"Aleinikoff, J.N., and Stoeser, D.B., 1988, Zircon morphology and U-Pb geochronology of seven metaluminous and peralkaline post-orogenic granite complexes of the Arabian Shield, Kingdom of Saudi Arabia: U.S. Geological Survey Open-File Report 88-604, ii, 32 p. ill., maps ;28 cm., https://doi.org/10.3133/ofr88604.","productDescription":"ii, 32 p. ill., maps ;28 cm.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":144032,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1988/0604/report-thumb.jpg"},{"id":40662,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1988/0604/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              35,\n              30\n            ],\n            [\n              35,\n              16\n            ],\n            [\n              45,\n              16\n            ],\n            [\n              45,\n              30\n            ],\n            [\n              35,\n              30\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b15e4b07f02db6a4bcb","contributors":{"authors":[{"text":"Aleinikoff, John Nicholas 0000-0003-3494-6841","orcid":"https://orcid.org/0000-0003-3494-6841","contributorId":18223,"corporation":false,"usgs":true,"family":"Aleinikoff","given":"John","email":"","middleInitial":"Nicholas","affiliations":[],"preferred":false,"id":166113,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Stoeser, D. B.","contributorId":18735,"corporation":false,"usgs":true,"family":"Stoeser","given":"D.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":166114,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
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