The Minnesota State Legislature passed laws as early as 1937 to regulate use of Minnesota's ground water and surface water through a permit system. Several unsuccessful attempts were made to computerize water-use data reported to the State. The U.S. Geological Survey, through the National Water-Use Information Program, assisted the Minnesota Department of Natural Resources and the Minnesota State Planning Agency, Land Management Information Center, in developing MWUDS (Minnesota Water-Use Data System).
\nThe Minnesota Water-Use Data System stores data on the quantity of individual annual water withdrawals and discharges in relation to the water resources affected, provides descriptors for aggregation of data and trend analysis, and enables access to additional data contained in other data bases. MWUDS is stored on a computer at the Land Management Information Center, an agency associated with the State Planning Agency. Interactive menu-driven programs simplify data entry, update, and retrieval and are easy to use. Estimates of unreported water use supplement reported water use to completely describe the stress on the hydrologic system. Links or common elements developed in the MWUDS enable access to data available in other State waterrelated data bases, forming a water-resource information system. Water-use information can be improved by developing methods for increasing accuracy of reported water use and refining methods for estimating unreported water use.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"St. Paul, MN","doi":"10.3133/wri854306","collaboration":"Prepared in cooperation with the Minnesota Department of Natural Resources and the Minnesota State Planning Agency","usgsCitation":"Horn, M., 1986, Development of a water-use data system in Minnesota: U.S. Geological Survey Water-Resources Investigations Report 85-4306, iv, 59 p., https://doi.org/10.3133/wri854306.","productDescription":"iv, 59 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":392,"text":"Minnesota Water Science Center","active":true,"usgs":true}],"links":[{"id":56608,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1985/4306/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":122851,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1985/4306/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9be4b07f02db65dff0","contributors":{"authors":[{"text":"Horn, M.A.","contributorId":92223,"corporation":false,"usgs":true,"family":"Horn","given":"M.A.","email":"","affiliations":[],"preferred":false,"id":198651,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":27528,"text":"wri844209 - 1986 - Water resources of Lake and Moody counties, South Dakota","interactions":[],"lastModifiedDate":"2012-02-02T00:08:40","indexId":"wri844209","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1986","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":"84-4209","title":"Water resources of Lake and Moody counties, South Dakota","docAbstract":"The primary sources of surface water in Lake and Moody Counties are the Big Sioux River and its intermittent tributaries, and Lakes Herman, Madison, and Brant. Seasonal variations in streamflow and lake levels are directly related to seasonal variations in precipitation. Dissolved-solids concentration in water from streams and lakes increases as streamflow decreases and lake levels decline. Eight glacial aquifers and four bedrock aquifers were delineated in Lake and Moody Counties. The Big Sioux, North Skunk Creek, Pipestone Creek, Battle Creek, and East Fork Vermillion aquifers are composed of glacial outwash. These aquifers are less than 60 feet below land surface, and are in hydraulic connection with the river or creek of the same name. The Rutland, Ramona, and Howard aquifers are composed of glacial outwash and are overlain by 50 to 470 feet of till. The four bedrock aquifers are the Niobrara, Codell, Dakota, and Quartzite wash. The average thickness of the Big Sioux, Pipestone Creek, North Skunk Creek, Battle Creek, and East Fork Vermillion aquifers ranges from 14 feet for the Battle Creek aquifer to 39 feet for the North Skunk Creek aquifer. The average thickness of the Rutland, Ramona, and Howard aquifers ranges from 18 feet for the Ramona aquifer to 40 feet for the Howard aquifer. Predominant chemical constituents in water from the Big Sioux, North Skunk Creek, and Pipestone Creek aquifers are calcium and bicarbonate. Predominant chemical constituents in the Battle Creek and East Fork Vermillion aquifers are calcium and sulfate. Predominant chemical constituents in water from the Rutland, Ramona, and Howard aquifers are calcium, sulfate and biocarbonate. The average thickness of the four bedrock aquifers ranges from 60 to 400 feet. The aquifers are under artesian conditions. Predominant chemical constituents in water from the Niobrara aquifer are calcium, sodium, and sulfate; from the Codell and Dakota aquifers are sodium and sulfate; and from the Quartzite wash aquifer are calcium, sulfate, and bicarbonate. Water use in 1980 in Lake and Moody Counties was about 2.6 billion gallons. Ninety percent of the water used in the counties was withdrawn from the glacial aquifers and 10 percent was withdrawn from the bedrock aquifers. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri844209","usgsCitation":"Hansen, D.S., 1986, Water resources of Lake and Moody counties, South Dakota: U.S. Geological Survey Water-Resources Investigations Report 84-4209, vi, 51 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri844209.","productDescription":"vi, 51 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":124033,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1984/4209/report-thumb.jpg"},{"id":56388,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1984/4209/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f4e4b07f02db5f082b","contributors":{"authors":[{"text":"Hansen, D. S.","contributorId":70003,"corporation":false,"usgs":true,"family":"Hansen","given":"D.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":198263,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":26570,"text":"wri854297 - 1986 - Manual for estimating selected streamflow characteristics of natural-flow streams in the Colorado River basin in Utah","interactions":[],"lastModifiedDate":"2012-02-02T00:08:28","indexId":"wri854297","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1986","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":"85-4297","title":"Manual for estimating selected streamflow characteristics of natural-flow streams in the Colorado River basin in Utah","docAbstract":"Methods are presented for estimating 10 streamflow characteristics at three types of sites on natural flow streams in the Colorado River Basin in Utah. The streamflow characteristics include average discharge and annual maximum 1-, 7-, and 15-day mean discharges for recurrence intervals of 10, 50 and 100 years. At or near gaged sites, two methods weight gaging station data with regression equation values to estimate streamflow characteristics. At sites on ungaged streams, a method estimates streamflow characteristics using regression equations. The regression equations relate the streamflow characteristics to the following basin and climatic characteristics: contributing drainage area, mean basin elevation, mean annual precipitation, main channel slope, and forested area. Separate regression equations were developed for four hydrologically distinct regions in the study area. The standard error of estimate for the 10 streamflow characteristics ranges from 13% to 87%. Basin, climatic, and streamflow characteristics, available as of September 30, 1981, are presented for 135 gaging stations in Utah, Arizona, Colorado, and Wyoming. In addition, weighted estimates of the streamflow characteristics based on station data and the regression equation estimates are provided for most gaging stations. (Author 's abstract)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri854297","usgsCitation":"Christensen, R., Johnson, E., and Plantz, G., 1986, Manual for estimating selected streamflow characteristics of natural-flow streams in the Colorado River basin in Utah: U.S. Geological Survey Water-Resources Investigations Report 85-4297, vi, 38 p. :map ;28 cm., https://doi.org/10.3133/wri854297.","productDescription":"vi, 38 p. :map ;28 cm.","costCenters":[],"links":[{"id":118865,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1985/4297/report-thumb.jpg"},{"id":55434,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1985/4297/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":55435,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1985/4297/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a82e4b07f02db64aec8","contributors":{"authors":[{"text":"Christensen, R.C.","contributorId":56670,"corporation":false,"usgs":true,"family":"Christensen","given":"R.C.","email":"","affiliations":[],"preferred":false,"id":196634,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Johnson, E.B.","contributorId":77953,"corporation":false,"usgs":true,"family":"Johnson","given":"E.B.","affiliations":[],"preferred":false,"id":196635,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Plantz, G.G.","contributorId":79103,"corporation":false,"usgs":true,"family":"Plantz","given":"G.G.","affiliations":[],"preferred":false,"id":196636,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":63101,"text":"gq1601 - 1986 - Geologic map of the Annandale quadrangle, Fairfax and Arlington Counties, and Alexandria City, Virginia","interactions":[],"lastModifiedDate":"2022-04-11T19:18:50.192251","indexId":"gq1601","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1986","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":316,"text":"Geologic Quadrangle","code":"GQ","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1601","title":"Geologic map of the Annandale quadrangle, Fairfax and Arlington Counties, and Alexandria City, Virginia","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/gq1601","usgsCitation":"Drake, A., and Froelich, A., 1986, Geologic map of the Annandale quadrangle, Fairfax and Arlington Counties, and Alexandria City, Virginia: U.S. Geological Survey Geologic Quadrangle 1601, Report: 2 p.; 1 Plate: 43.83 × 33.35 inches, https://doi.org/10.3133/gq1601.","productDescription":"Report: 2 p.; 1 Plate: 43.83 × 33.35 inches","costCenters":[],"links":[{"id":252392,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gq/1601/report-thumb.jpg"},{"id":249228,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/gq/1601/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":249227,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gq/1601/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":398501,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_92836.htm"}],"scale":"24000","country":"United States","state":"Virginia","county":"Arlington County, Fairfax County","otherGeospatial":"Annandale quadrangle","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -77.25,\n 38.75\n ],\n [\n -77.125,\n 38.75\n ],\n [\n -77.125,\n 38.875\n ],\n [\n -77.25,\n 38.875\n ],\n [\n -77.25,\n 38.75\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b11e4b07f02db6a2475","contributors":{"authors":[{"text":"Drake, Avery Ala","contributorId":65460,"corporation":false,"usgs":true,"family":"Drake","given":"Avery Ala","affiliations":[],"preferred":false,"id":268332,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Froelich, A.J.","contributorId":13593,"corporation":false,"usgs":true,"family":"Froelich","given":"A.J.","email":"","affiliations":[],"preferred":false,"id":268331,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":27749,"text":"wri864165 - 1986 - Reconnaissance of surficial geology, regolith thickness, and configuration of the bedrock surface in Bear Creek and Union Valleys, near Oak Ridge, Tennessee","interactions":[],"lastModifiedDate":"2012-02-02T00:08:26","indexId":"wri864165","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1986","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":"86-4165","title":"Reconnaissance of surficial geology, regolith thickness, and configuration of the bedrock surface in Bear Creek and Union Valleys, near Oak Ridge, Tennessee","docAbstract":"A preliminary interpretation of the lithology, thickness of regolith, and configuration of the bedrock surface underlying Bear Creek and Union Valleys near Oak Ridge, Tennessee, was made based on geologic and geophysical data from boreholes and cores in Bear Creek Valley and on related work of other investigators. Analysis of drillers ' logs and lithologic logs and comparison of these data with a topographic map indicated that topography and depth of weathering are interdependent and are ultimately controlled by lithology. Topographic patterns were, therefore, used to extend localized geologic data to a larger scale. Maps of the surficial geology, thickness of regolith, and configuration of the bedrock surface are presented. (Author 's abstract)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri864165","usgsCitation":"Hoos, A., and Bailey, Z., 1986, Reconnaissance of surficial geology, regolith thickness, and configuration of the bedrock surface in Bear Creek and Union Valleys, near Oak Ridge, Tennessee: U.S. Geological Survey Water-Resources Investigations Report 86-4165, iii, 9 p. :ill., map ;28 cm., https://doi.org/10.3133/wri864165.","productDescription":"iii, 9 p. :ill., map ;28 cm.","costCenters":[],"links":[{"id":157952,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1986/4165/report-thumb.jpg"},{"id":56592,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1986/4165/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":56593,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1986/4165/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67c5bd","contributors":{"authors":[{"text":"Hoos, A.B.","contributorId":23572,"corporation":false,"usgs":true,"family":"Hoos","given":"A.B.","affiliations":[],"preferred":false,"id":198636,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bailey, Z. C.","contributorId":54587,"corporation":false,"usgs":true,"family":"Bailey","given":"Z. C.","affiliations":[],"preferred":false,"id":198637,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":15157,"text":"ofr86551C - 1986 - Earthquake data report; March 1985","interactions":[],"lastModifiedDate":"2012-02-02T00:07:05","indexId":"ofr86551C","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1986","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":"86-551","chapter":"C","title":"Earthquake data report; March 1985","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr86551C","usgsCitation":"National Earthquake Information Center, 1986, Earthquake data report; March 1985: U.S. Geological Survey Open-File Report 86-551, 278 p. ;28 cm., https://doi.org/10.3133/ofr86551C.","productDescription":"278 p. ;28 cm.","costCenters":[],"links":[{"id":148757,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1986/0551c/report-thumb.jpg"},{"id":44076,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1986/0551c/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a51e4b07f02db629868","contributors":{"authors":[{"text":"National Earthquake Information Center","contributorId":128066,"corporation":true,"usgs":false,"organization":"National Earthquake Information Center","id":528981,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":15233,"text":"ofr85134 - 1986 - Description of drill-hole GN042V core from the Jabiluka unconformity-type uranium deposit, Northern Territory, Australia","interactions":[],"lastModifiedDate":"2012-02-02T00:06:55","indexId":"ofr85134","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1986","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":"85-134","title":"Description of drill-hole GN042V core from the Jabiluka unconformity-type uranium deposit, Northern Territory, Australia","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr85134","usgsCitation":"Nutt, C., 1986, Description of drill-hole GN042V core from the Jabiluka unconformity-type uranium deposit, Northern Territory, Australia: U.S. Geological Survey Open-File Report 85-134, i, 15 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr85134.","productDescription":"i, 15 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":146702,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1985/0134/report-thumb.jpg"},{"id":44181,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1985/0134/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ab0e4b07f02db66dd34","contributors":{"authors":[{"text":"Nutt, C.J.","contributorId":52577,"corporation":false,"usgs":true,"family":"Nutt","given":"C.J.","email":"","affiliations":[],"preferred":false,"id":170786,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":15087,"text":"ofr86345 - 1986 - Analytical results, geochemical signatures, and sample locality map of lode gold, placer gold, and heavy-mineral concentrates from the Koyukuk- Chandalar mining district, Alaska","interactions":[],"lastModifiedDate":"2022-09-20T19:31:11.852711","indexId":"ofr86345","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1986","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":"86-345","title":"Analytical results, geochemical signatures, and sample locality map of lode gold, placer gold, and heavy-mineral concentrates from the Koyukuk- Chandalar mining district, Alaska","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr86345","usgsCitation":"Mosier, E.L., and Lewis, J.S., 1986, Analytical results, geochemical signatures, and sample locality map of lode gold, placer gold, and heavy-mineral concentrates from the Koyukuk- Chandalar mining district, Alaska: U.S. Geological Survey Open-File Report 86-345, Report: 172 p.; 1 Plate: 45.43 × 27.76 inches, https://doi.org/10.3133/ofr86345.","productDescription":"Report: 172 p.; 1 Plate: 45.43 × 27.76 inches","costCenters":[],"links":[{"id":44003,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1986/0345/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":44004,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1986/0345/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":407083,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_19011.htm","linkFileType":{"id":5,"text":"html"}},{"id":148054,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1986/0345/report-thumb.jpg"}],"country":"United States","state":"Alaska","otherGeospatial":"Koyukuk-Chandalar mining district","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -153,\n 66.636\n ],\n [\n -147,\n 66.636\n ],\n [\n -147,\n 68\n ],\n [\n -153,\n 68\n ],\n [\n -153,\n 66.636\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67c4ab","contributors":{"authors":[{"text":"Mosier, E. L.","contributorId":71537,"corporation":false,"usgs":true,"family":"Mosier","given":"E.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":170542,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lewis, J. S.","contributorId":99988,"corporation":false,"usgs":true,"family":"Lewis","given":"J.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":170543,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":12236,"text":"ofr86544 - 1986 - Preliminary report on geophysical well-logging activity on the Salton Sea Scientific Drilling Project, Imperial Valley, California","interactions":[],"lastModifiedDate":"2012-02-02T00:06:49","indexId":"ofr86544","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1986","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":"86-544","title":"Preliminary report on geophysical well-logging activity on the Salton Sea Scientific Drilling Project, Imperial Valley, California","docAbstract":"The Salton Sea Scientific Drilling Project has culminated in a 10,564-ft deep test well, State 2-14 well, in the Imperial Valley of southern California. A comprehensive scientific program of drilling, coring, and downhole measurements, which was conducted for about 5 months, has obtained much scientific information concerning the physical and chemical processes associated with an active hydrothermal system. This report primarily focuses on the geophysical logging activities at the State 2-14 well and provides early dissemination of geophysical data to other investigators working on complementary studies. Geophysical-log data were obtained by a commercial logging company and by the U.S. Geological Survey (USGS). Most of the commercial logs were obtained during three visits to the site; only one commercial log was obtained below a depth of 6,000 ft. The commercial logs obtained were dual induction, natural gamma, compensated neutron formation density, caliper and sonic. The USGS logging effort consisted of four primary periods, with many logs extending below a depth of 6,000 ft. The USGS logs obtained were temperature, caliper, natural gamma, gamma spectral, epithermal neutron, acoustic velocity, full-waveform, and acoustic televiewer. Various problems occurred throughout the drilling phase of the Salton Sea Scientific Drilling Project that made successful logging difficult: (1) borehole constrictions, possibly resulting from mud coagulation, (2) maximum temperatures of about 300 C, and (3) borehole conditions unfavorable for logging because of numerous zones of fluid loss, cement plugs, and damage caused by repeated trips in and out of the hole. These factors hampered and compromised logging quality at several open-hole intervals. The quality of the logs was dependent on the degree of probe sophistication and sensitivity to borehole-wall conditions. Digitized logs presented were processed on site and are presented in increments of 1,000 ft. A summary of the numerous factors that may be relevant to this interpretation also is presented. 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H.","contributorId":31794,"corporation":false,"usgs":true,"family":"Morin","given":"R.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":165582,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hodges, H.E.","contributorId":22624,"corporation":false,"usgs":true,"family":"Hodges","given":"H.E.","email":"","affiliations":[],"preferred":false,"id":165581,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":15182,"text":"ofr8673 - 1986 - Dissolved-selenium data for wells in the western San Joaquin Valley, California, February to July 1985","interactions":[],"lastModifiedDate":"2012-02-02T00:07:00","indexId":"ofr8673","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1986","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":"86-73","title":"Dissolved-selenium data for wells in the western San Joaquin Valley, California, February to July 1985","docAbstract":"Water samples were collected for selenium analysis from 63 wells in western San Joaquin Valley, California, during February to July 1985. 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