Pumpage data from about 2,100 wells used for public and nonpublic water-supply in Nassau County from 1920-77 have been collected and are available for public inspection at the U.S. Geological Survey office in Syosset, Nassau County. Except for wells in use before 1920, these data constitute the entire record available through 1977. The data are divided into two categories--pumpage from wells used for public supply, and pumpage from wells used mainly for industrial and commercial uses, designated as nonpublic water supply. Pumpage is tabulated by well or well field and is given by month or year with an annual total. The report serves as an introduction and user 's manual to the data, which are available for inspection but are not included in the report because they fill several hundred pages. The report describes the method of reporting pumpage on Long Island and how pumpage values were derived from the records. It also includes well-completion data and two maps showing the location of all wells.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr81499","usgsCitation":"Kilburn, C., 1982, Ground-water pumpage in Nassau County, Long Island, New York, 1920-77: Introduction and user's guide to the data compilation: U.S. Geological Survey Open-File Report 81-499, Report: iii, 67 p.; 2 Plates: 27.15 × 38.08 inches and 27.15 × 37.65 inches, https://doi.org/10.3133/ofr81499.","productDescription":"Report: iii, 67 p.; 2 Plates: 27.15 × 38.08 inches and 27.15 × 37.65 inches","costCenters":[],"links":[{"id":410112,"rank":5,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_75499.htm","linkFileType":{"id":5,"text":"html"}},{"id":37576,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/0499/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":37575,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/0499/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":37574,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/0499/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":141786,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/0499/report-thumb.jpg"}],"country":"United States","state":"New York","county":"Nassau County","otherGeospatial":"Long Island","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -73.4167,\n 40.9167\n ],\n [\n -73.7667,\n 40.9167\n ],\n [\n -73.7667,\n 40.5833\n ],\n [\n -73.4167,\n 40.5833\n ],\n [\n -73.4167,\n 40.9167\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa8e4b07f02db6673e5","contributors":{"authors":[{"text":"Kilburn, Chabot","contributorId":83499,"corporation":false,"usgs":true,"family":"Kilburn","given":"Chabot","email":"","affiliations":[],"preferred":false,"id":160321,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":27046,"text":"wri8249 - 1982 - Streamflow losses to Madison Group rocks in the Little Belt and Big Snowy Mountains, Montana","interactions":[],"lastModifiedDate":"2019-08-05T11:31:54","indexId":"wri8249","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"82-49","title":"Streamflow losses to Madison Group rocks in the Little Belt and Big Snowy Mountains, Montana","docAbstract":"Four streams originating in the Little Belt and Big Snowy Mountains in central Montana were measured in 1975 to determine streamflow losses across outcrops of the Madison Group (Mississippian age). Based on streamflow data obtained for 39 months at two streamflow-gaging stations on the Middle Fork Judith River, the average daily loss was 9.1 cubic feet per second or about 6,600 acre-feet per year. Seepage measurements on other stream reaches indicated losses of 7.6 cubic feet per second on the south Fork Judith River, 9.2 cubic feet per second in Yogo Creek, as much as 64 cubic feet per second in Dry Wolf Creek, and about 60 cubic feet per second in Rock Creek. (USGS)","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wri8249","usgsCitation":"Feltis, R., and Shields, R.R., 1982, Streamflow losses to Madison Group rocks in the Little Belt and Big Snowy Mountains, Montana: U.S. Geological Survey Water-Resources Investigations Report 82-49, 16 p. , https://doi.org/10.3133/wri8249.","productDescription":"16 p. ","costCenters":[],"links":[{"id":158971,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1982/0049/report-thumb.jpg"},{"id":366250,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1982/0049/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Montana","otherGeospatial":"Big Snowy Mountains, Little Belt Mountains","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -109.7314453125,\n 46.619261036171515\n ],\n [\n -108.797607421875,\n 46.619261036171515\n ],\n [\n -108.797607421875,\n 46.98774725646568\n ],\n [\n -109.7314453125,\n 46.98774725646568\n ],\n [\n -109.7314453125,\n 46.619261036171515\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b15e4b07f02db6a4d9c","contributors":{"authors":[{"text":"Feltis, R.D.","contributorId":93467,"corporation":false,"usgs":true,"family":"Feltis","given":"R.D.","affiliations":[],"preferred":false,"id":197465,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Shields, Ronald R.","contributorId":64655,"corporation":false,"usgs":true,"family":"Shields","given":"Ronald","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":197464,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":26187,"text":"wri8226 - 1982 - Streamflow and water-quality conditions, Wilsons Creek and James River, Springfield area, Missouri","interactions":[],"lastModifiedDate":"2017-12-06T12:52:13","indexId":"wri8226","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"82-26","title":"Streamflow and water-quality conditions, Wilsons Creek and James River, Springfield area, Missouri","docAbstract":"A network of water-quality-monitoring stations was established upstream and downstream from the Southwest Wastewater-Treatment Plant on Wilsons Creek to monitor the effects of sewage effluent on water quality. Data indicate that 82 percent of the time the flow in Wilsons Creek upstream from the wastewater-treatment plant is less than the effluent discharged from the plant. On October 15, 1977, an advanced wastewater-treatment facility was put into operation. Of the four water-quality indicators measured at the monitoring stations (specific conductance, dissolved oxygen, pH, and water temperature), only dissolved oxygen showed improvement downstream from the plant. During urban runoff, the specific conductance momentarily increased and dissolved-oxygen concentration momentarily decreased in Wilsons Creek upstream from the plant. Urban runoff was found to have no long-term effects on specific conductance and dissolved oxygen downstream from the plant before or after the addition of the advanced wastewater-treatment facility. Data collected monthly from the James River showed that the dissolved-oxygen concentrations and the total nitrite plus nitrate nitrogen concentrations increased, whereas the dissolved-manganese concentrations decreased after the advanced wastewater-treatment facility became operational.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri8226","usgsCitation":"Berkas, W.R., 1982, Streamflow and water-quality conditions, Wilsons Creek and James River, Springfield area, Missouri: U.S. Geological Survey Water-Resources Investigations Report 82-26, v, 38 p., https://doi.org/10.3133/wri8226.","productDescription":"v, 38 p.","numberOfPages":"49","costCenters":[],"links":[{"id":157616,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1982/0026/report-thumb.jpg"},{"id":349774,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1982/0026/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Missouri","city":"Springfield","otherGeospatial":"James River, Wilsons Creek","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -93.49983215332031,\n 36.99322996239362\n ],\n [\n -93.27529907226562,\n 36.99322996239362\n ],\n [\n -93.27529907226562,\n 37.20462845803212\n ],\n [\n -93.49983215332031,\n 37.20462845803212\n ],\n [\n -93.49983215332031,\n 36.99322996239362\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b15e4b07f02db6a4e9b","contributors":{"authors":[{"text":"Berkas, Wayne R. wrberkas@usgs.gov","contributorId":425,"corporation":false,"usgs":true,"family":"Berkas","given":"Wayne","email":"wrberkas@usgs.gov","middleInitial":"R.","affiliations":[{"id":5050,"text":"WY-MT Water Science Center","active":true,"usgs":true}],"preferred":true,"id":195957,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":8445,"text":"ofr8235 - 1982 - Environmental geology of Harrison Bay, northern Alaska","interactions":[],"lastModifiedDate":"2012-02-02T00:06:05","indexId":"ofr8235","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"82-35","title":"Environmental geology of Harrison Bay, northern Alaska","docAbstract":"The surficial and shallow subsurface geology of Harrison Bay on the Beaufort Sea coast was mapped as part of the U.S. Geological Survey's prelease evaluation for Outer Continental Shelf (OCS) Oil and Gas Lease Sale 71. During the 1980 summer season, approximately 1600 km of multisensored, high-resolution geophysical profile data were collected along a rectangular grid with 4.8 km line spacing. Interpretation of these data is presented on five maps showing bathymetry, sea-floor microrelief, ice-gouge characteristics, Holocene sediment thickness, and geologic structure to depths of approximately 1000 m. \r\n\r\nOn a broad scale, the seafloor is shallow and almost flat, although microrelief features produced by sediment transport and ice-gouge processes typically vary up to several meters in amplitude. Microrelief bedforms related to hydraulic processes are predominant in water depths less than 12 m. Microrelief caused by ice gouging generally increases with water depth, reaching a maximum of 2 m or more in water depths beyond the 20 m isobath. This intensely gouged area lies beneath the shear zone between the seasonal landfast ice and the mobile polar ice pack. \r\n\r\nThe thickness of recent (Holocene) sediment increases offshore, from 2 m near the Colville River delta to 30 m or more on the outer shelf. The thin Holocene layer is underlain by a complex horizon interpreted to be the upper surface of a Pleistocene deposit similar in composition to the present Arctic Coastal Plain. The base of the inferred Pleistocene section is interpreted to be a low-angle unconformity 100 m below sea level. Beneath this Tertiary-Quaternary unconformity, strata are interpreted to be alluvial fan-delta plain deposits corresponding to the Colville Group and younger formations of Late Cretaceous to Tertiary age. Numerous high-angle faults downthrown to the north trend across the survey area. With few exceptions, these faults terminate at or below the 100 m unconformity, suggesting that most tectonism occurred before Quaternary time. Acoustic anomalies suggesting gas accumulation are rare, and where identified typically occur adjacent to faults. A laterally continuous zone of poor seismic data occurs in the nearshore area and is interpreted to be caused by subsea permafrost. This report describes these geologic conditions in Harrison Bay and discusses potential hazards that they may pose for future oil and gas operations in Sale 71 and adjacent Beaufort Sea shelf areas.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr8235","usgsCitation":"Craig, J., and Thrasher, G.P., 1982, Environmental geology of Harrison Bay, northern Alaska: U.S. Geological Survey Open-File Report 82-35, iii, 28 p., 6 over-size sheets, ill., maps ;28 cm., https://doi.org/10.3133/ofr8235.","productDescription":"iii, 28 p., 6 over-size sheets, ill., maps ;28 cm.","costCenters":[],"links":[{"id":140504,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0035/report-thumb.jpg"},{"id":36009,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0035/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":36010,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0035/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":36011,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0035/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":36012,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0035/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":36013,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0035/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":36014,"rank":405,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0035/plate-6.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":36015,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0035/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4abbe4b07f02db6723d7","contributors":{"authors":[{"text":"Craig, J.D.","contributorId":14405,"corporation":false,"usgs":true,"family":"Craig","given":"J.D.","email":"","affiliations":[],"preferred":false,"id":157726,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Thrasher, G. P.","contributorId":42939,"corporation":false,"usgs":true,"family":"Thrasher","given":"G.","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":157727,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":7213,"text":"ofr82291 - 1982 - Guide to the use of PACER, the data retrieval and update system for the National Coal Resources Data System (NCRDS)","interactions":[],"lastModifiedDate":"2012-02-02T00:06:00","indexId":"ofr82291","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"82-291","title":"Guide to the use of PACER, the data retrieval and update system for the National Coal Resources Data System (NCRDS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82291","usgsCitation":"Krohn, K., Carey, M., Carter, M., and Medlin, A., 1982, Guide to the use of PACER, the data retrieval and update system for the National Coal Resources Data System (NCRDS): U.S. Geological Survey Open-File Report 82-291, 101 p., 28 cm., https://doi.org/10.3133/ofr82291.","productDescription":"101 p., 28 cm.","costCenters":[],"links":[{"id":140825,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0291/report-thumb.jpg"},{"id":34613,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0291/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a82e4b07f02db64b081","contributors":{"authors":[{"text":"Krohn, K.K.","contributorId":102465,"corporation":false,"usgs":true,"family":"Krohn","given":"K.K.","email":"","affiliations":[],"preferred":false,"id":154781,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Carey, M.A.","contributorId":62581,"corporation":false,"usgs":true,"family":"Carey","given":"M.A.","email":"","affiliations":[],"preferred":false,"id":154780,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Carter, M.D.","contributorId":31382,"corporation":false,"usgs":true,"family":"Carter","given":"M.D.","email":"","affiliations":[],"preferred":false,"id":154779,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Medlin, A.L.","contributorId":28226,"corporation":false,"usgs":true,"family":"Medlin","given":"A.L.","email":"","affiliations":[],"preferred":false,"id":154778,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":57263,"text":"wdrID811 - 1982 - Water Resources Data, Idaho, Water Year 1981--Volume 1. Great Basin and Snake River Basin above King Hill","interactions":[],"lastModifiedDate":"2012-02-02T00:12:22","indexId":"wdrID811","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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-81-1","title":"Water Resources Data, Idaho, Water Year 1981--Volume 1. Great Basin and Snake River Basin above King Hill","language":"ENGLISH","doi":"10.3133/wdrID811","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1982, Water Resources Data, Idaho, Water Year 1981--Volume 1. Great Basin and Snake River Basin above King Hill: U.S. Geological Survey Water Data Report ID-81-1, 447 p., 12 Fig., https://doi.org/10.3133/wdrID811.","productDescription":"447 p., 12 Fig.","costCenters":[],"links":[{"id":183482,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ae4b07f02db5fba0e","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":533050,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":57287,"text":"wdrPA821 - 1982 - Water resources data, Pennsylvania water year 1982. Volume 1: Delaware River basin","interactions":[],"lastModifiedDate":"2024-07-26T22:42:15.033828","indexId":"wdrPA821","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"PA-82-1","title":"Water resources data, Pennsylvania water year 1982. Volume 1: Delaware River basin","docAbstract":"Water resources data for the 1982 water year for Pennsylvania consist of records of discharge and water quality of streams; elevation and contents of lakes and reservoirs; and elevation of tides; and water levels of ground-water wells. This volume contains records for water discharge at 66 gaging stations; elevation and contents at 11 lakes and reservoirs; elevation of tides at 1 gaging station; water quality at 33 gaging stations; and water levels at 16 observation wells. Also included are data for 34 crest-stage, 80 low-flow, and 43 water-quality partial-record stations. Locations of these sites are shown on figures 6 through 9. Additional water data were collected at various sites not involved in the systematic data-collection program and are published as miscellaneous measurements and analyses. These data together with the data in Volume 2 and 3 represent that part of the National Water Data System operated by the
U.S. Geological Survey and cooperating State, local and Federal agencies in Pennsylvania.
Data are presented on the phytoplankton species composition and abundance in San Francisco Bay from January 1980 through February 1981. Phytoplankton were identified and enumerated in surface samples collected approximately every two weeks at selected stations in the main channel of the Bay, and at shoal stations in the central portion of South San Francisco Bay, San Pablo Bay, and Suisun Bay. Also reported are separate species lists for microphytoplankton (< 60 micrometers) and macrophytoplankton (> 60 micrometers). (Author 's abstract)
","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82443","issn":"0094-9140","usgsCitation":"Wong, R., and Cloern, J., 1982, Plankton studies in San Francisco Bay; IV, Phytoplankton abundance and species composition, January 1980 - February 1981: U.S. Geological Survey Open-File Report 82-443, 152 p. ill., 1 map ;28 cm., https://doi.org/10.3133/ofr82443.","productDescription":"152 p. ill., 1 map ;28 cm.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":552,"text":"San Francisco Bay-Delta","active":false,"usgs":true},{"id":5079,"text":"Pacific Regional Director's Office","active":true,"usgs":true}],"links":[{"id":53882,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0443/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":157669,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0443/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adae4b07f02db68556e","contributors":{"authors":[{"text":"Wong, R.L.","contributorId":104068,"corporation":false,"usgs":true,"family":"Wong","given":"R.L.","email":"","affiliations":[],"preferred":false,"id":192770,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Cloern, J. E.","contributorId":59453,"corporation":false,"usgs":true,"family":"Cloern","given":"J. E.","affiliations":[],"preferred":false,"id":192769,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":7159,"text":"ofr821026 - 1982 - Geochemical data for the Killik River and Chandler Lake quadrangles, Alaska","interactions":[],"lastModifiedDate":"2012-02-02T00:06:04","indexId":"ofr821026","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"82-1026","title":"Geochemical data for the Killik River and Chandler Lake quadrangles, Alaska","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr821026","usgsCitation":"Barton, H.N., Odland, S., O’Leary, R.M., and Day, G., 1982, Geochemical data for the Killik River and Chandler Lake quadrangles, Alaska: U.S. Geological Survey Open-File Report 82-1026, 53 p., map ;28 cm., https://doi.org/10.3133/ofr821026.","productDescription":"53 p., map ;28 cm.","costCenters":[],"links":[{"id":140520,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/1026/report-thumb.jpg"},{"id":34504,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/1026/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b24e4b07f02db6ae41d","contributors":{"authors":[{"text":"Barton, H. N.","contributorId":99546,"corporation":false,"usgs":true,"family":"Barton","given":"H.","email":"","middleInitial":"N.","affiliations":[],"preferred":false,"id":154548,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Odland, S. K.","contributorId":48933,"corporation":false,"usgs":true,"family":"Odland","given":"S. K.","affiliations":[],"preferred":false,"id":154546,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"O’Leary, R. M.","contributorId":44894,"corporation":false,"usgs":true,"family":"O’Leary","given":"R.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":154545,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Day, G.W.","contributorId":63363,"corporation":false,"usgs":true,"family":"Day","given":"G.W.","email":"","affiliations":[],"preferred":false,"id":154547,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":4682,"text":"twri05A6 - 1982 - Quality assurance practices for the chemical and biological analyses of water and fluvial sediments","interactions":[],"lastModifiedDate":"2013-11-21T11:01:11","indexId":"twri05A6","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":336,"text":"Techniques of Water-Resources Investigations","code":"TWRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"05-A6","title":"Quality assurance practices for the chemical and biological analyses of water and fluvial sediments","docAbstract":"This chapter contains practices used by the U.S. Geological Survey to assure the quality of analytical data for water, fluvial sediment, and aquatic organisms. These practices are directed primarily toward personnel making water quality measurements. Some detail specific quality control techniques, others document quality assurance procedures being used by the Central Laboratories System of the U.S. Geological Survey, and still others describe various statistical techniques and give examples of their use in evaluating and assuring the quality of analytical data. The practices are arranged into eight sections: Analytical Methods Development Procedures, Standard Quantitative Analysis Techniques, Instrumental Techniques, Reference Material, Laboratory Quality Control; Quality Assurance Monitoring; Documentation, Summary, and Evaluation of Data, Materials Evaluation. Each section is preceded by a brief description of the material covered. Similarly within each section, each practice is preceded by a description of its application or scope.","language":"English","publisher":"U.S. Government Printing Office","doi":"10.3133/twri05A6","usgsCitation":"Friedman, L., and Erdmann, D.E., 1982, Quality assurance practices for the chemical and biological analyses of water and fluvial sediments: U.S. Geological Survey Techniques of Water-Resources Investigations 05-A6, ix, 181 p., https://doi.org/10.3133/twri05A6.","productDescription":"ix, 181 p.","numberOfPages":"164","costCenters":[{"id":343,"text":"Idaho Water Science Center","active":true,"usgs":true}],"links":[{"id":243,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/twri/twri5a6/","linkFileType":{"id":5,"text":"html"}},{"id":139154,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/twri/05a06/report-thumb.jpg"},{"id":31714,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/twri/05a06/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a8fe4b07f02db655218","contributors":{"authors":[{"text":"Friedman, Linda C.","contributorId":98702,"corporation":false,"usgs":true,"family":"Friedman","given":"Linda C.","affiliations":[],"preferred":false,"id":149617,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Erdmann, David E.","contributorId":62991,"corporation":false,"usgs":true,"family":"Erdmann","given":"David","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":149616,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":7462,"text":"ofr82782 - 1982 - Progress report on lithium-related geologic investigations in Bolivia","interactions":[],"lastModifiedDate":"2012-02-02T00:06:03","indexId":"ofr82782","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"82-782","title":"Progress report on lithium-related geologic investigations in Bolivia","docAbstract":"The September 1, 1981, Samoa Islands Region earthquake occurred at the extreme northern end of the Tonga arc in a region where the Pacific plate may be disjointed along a hinge fault. In the last 50 years, magnitude 7 or greater earthquakes have occurred in this region on the average of once every six years, but four 7+ events have now occurred within the last six years. The mainshock was preceded about two hours earlier by a foreshock that was used as a calibration event for the Joint Epicenter Determination relocation of the mainshock and nearby seismicity occurring within a period seven months prior to and one week after the mainshock. The foreshock, better-located events of the prior seismicity, and most aftershocks are concentrated in a group near the mainshock epicenter, but several more distant aftershocks suggest that the aftershock zone may have been as large as 125 km in length and trended about S35?E. Identification of depth phases from a full suite of broadband records gives source depths of 25-3km for the mainshock and 29.5?3 km for the foreshock using a JB earth model. \r\n\r\nSource parameters were determined for the mainshock utilizing WWSSN analog and GDSN digital data. The preferred fault plane solution based on P-wave first motion data is a south by southwesterly steeply dipping normal fault, remarkably similar to the mechanism reported by Johnson and Molnar (1972) for the nearby earthquake of April 20, 196B. A waveform inversion technique described by Sipkin (1982), when applied to long-period P waveforms, gives an 'average' point source solution for a purely deviatoric moment rate tensor at a preferred source depth of 22 km. Very similar results were obtained from long-period GDSN body-wave and mantle-wave data using a centroid-moment tensor inversion technique described in Dziewonski, and others (1981). Both techniques provide solutions very close to a double couple source with a south by southwesterly shallow-dipping normal fault mechanism. \r\n\r\nTo obtain the scalar mantle wave moment, GDSN vertical and transverse records 20,000 see in length were processed as described by Buland and Taggart (1981). Averaging all the data from Rayleigh and Love waves yields an estimate of 3.8 x 10^27 dyne-cm (as compared to about 1.9 x 10^27 from body-wave moment tensor inversions) or a moment magnitude (Mr) of 7.6. \r\n\r\nFor the portion of the waveform analysed (50-5B sec), the body-wave inversion performed by Sipkin gives a source time function of duration approximately 28 sec with two peaks in activity. Simultaneous analysis of short-period records, and broadband ground displacements and velocities, a method described by Harvey and Choy (1982) and Choy and Boatwright (1981) revealed a complex rupture consisting of two subevents, of about the same moment, separated in time by about 25 sec, and with durations of about 25 sec each. The two peaks in activity resolved by the body-wave moment tensor inversion correspond to the first of these subevents.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82782","usgsCitation":"Davis, J., Howard, K.A., Rettig, S., Smith, R.L., Ericksen, G.E., Risacher, F., Alarcon, H., and Morales, R., 1982, Progress report on lithium-related geologic investigations in Bolivia: U.S. Geological Survey Open-File Report 82-782, 18 p., maps ;28 cm., https://doi.org/10.3133/ofr82782.","productDescription":"18 p., maps ;28 cm.","costCenters":[],"links":[{"id":140516,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0782/report-thumb.jpg"},{"id":34882,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0782/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae1e4b07f02db688582","contributors":{"authors":[{"text":"Davis, J.R.","contributorId":83907,"corporation":false,"usgs":true,"family":"Davis","given":"J.R.","email":"","affiliations":[],"preferred":false,"id":155724,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Howard, K. A.","contributorId":48938,"corporation":false,"usgs":false,"family":"Howard","given":"K.","middleInitial":"A.","affiliations":[],"preferred":false,"id":155722,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Rettig, S.L.","contributorId":42592,"corporation":false,"usgs":true,"family":"Rettig","given":"S.L.","email":"","affiliations":[],"preferred":false,"id":155720,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Smith, R. L.","contributorId":93904,"corporation":false,"usgs":true,"family":"Smith","given":"R.","email":"","middleInitial":"L.","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":155725,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Ericksen, G. E.","contributorId":44538,"corporation":false,"usgs":true,"family":"Ericksen","given":"G.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":155721,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Risacher, Francois","contributorId":74748,"corporation":false,"usgs":true,"family":"Risacher","given":"Francois","email":"","affiliations":[],"preferred":false,"id":155723,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Alarcon, Hugo","contributorId":96678,"corporation":false,"usgs":true,"family":"Alarcon","given":"Hugo","email":"","affiliations":[],"preferred":false,"id":155726,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Morales, Ricardo","contributorId":10796,"corporation":false,"usgs":true,"family":"Morales","given":"Ricardo","email":"","affiliations":[],"preferred":false,"id":155719,"contributorType":{"id":1,"text":"Authors"},"rank":8}]}} ,{"id":7777,"text":"ofr82718 - 1982 - High-resolution seismic-reflection profiles collected aboard R/V James M. Gilliss Cruise GS-7903-3, over the Atlantic Continental Slope and Rise off New England","interactions":[],"lastModifiedDate":"2018-06-18T10:55:19","indexId":"ofr82718","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"82-718","title":"High-resolution seismic-reflection profiles collected aboard R/V James M. Gilliss Cruise GS-7903-3, over the Atlantic Continental Slope and Rise off New England","docAbstract":"During June 1979, the U.S. Geological Survey (USGS) collected 4,032 km of single-channel seismic-reflection data from the Atlantic Continental Slope and Rise off New England. The work was conducted aboard R/V JAMES M. GILLISS (cruise GS-7903-3). The purpose of the cruise was to determine the characteristics of mass sediment movement on the Continental Slope, and to study and correlate the stratigraphy of the Jurassic and Cretaceous strata lying north and south of the New England seamount chain.
Seismic instrumentation included 40-in3, 160-in3, and 500-in3 airguns; a Teledyne 800-joule minisparker system; a 3-5-kHz to 7-kHz, hull-mounted tunable transducer; and a 7-channel analog tape recorder.
Navigation control during the cruise was provided by a Western Integrated Navigation System capable of integrating satellite, rho-rho Loran-C, hyperbolic Loran-C, gyro compass, and doppler speed-log position data. The prime navigation sensor was the rho-rho Loran-C automatically recorded at 20-second intervals and manually plotted every 15 minutes, backed up by hyperbolic Loran-C fixes automatically recorded every 5 minutes.
Of the 4,032 km of data collected, 3,257 km of 3-5-kHz, minisparker and 40-in3 airgun were for the sediment-slump studand the other 775 km of 3-5-kHz, minis parker, 160-in3 air gun and 500-in3 airgun were for the deep stratigraphy study. Overall, the quality of the data is excellent with good resolution and penetration.
The original data may be examined at the U.S. Geological Survey, Woods Hole, MA 02543. Copies of the data can be purchased only from the National Geophysical and Solar-Terrestrial Data Center, NOAA/EDIS/NGSDC, Code D621, 325 Broadway, Boulder, CO 80303 (303-497-6338).
","language":"ENGLISH","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr82718","usgsCitation":"Bailey, N.G., and Aaron, J.M., 1982, High-resolution seismic-reflection profiles collected aboard R/V James M. Gilliss Cruise GS-7903-3, over the Atlantic Continental Slope and Rise off New England: U.S. Geological Survey Open-File Report 82-718, 2 p. :map ;28 cm., https://doi.org/10.3133/ofr82718.","productDescription":"2 p. :map ;28 cm.","costCenters":[],"links":[{"id":141234,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":259853,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0718/ofr1982718.pdf","text":"Report","size":"9:40 MB","linkFileType":{"id":1,"text":"pdf"},"description":"OFR 1982-718"}],"contact":"Coastal and Marine Geology Program
U.S. Geological Survey
384 Woods Hole Road
Woods Hole, MA 02543
Surface water arid;ground water from an area underlain by coal- bearing rocks in the vicinity of St. Charles Michigan, were analyzed to determine the quality characteristics of these water resources and to assess the relation between the two. Data for 15 constituents, including boron, phenol, lithium, strontium and manganese, were in such high concentrations that they could be used to differentiate between water from wells drilled into coal-bearing beds and water from streams not directly associated with coal deposits.
Ground water from abandoned mines and undisturbed coal-bearing beds is highly mineralized, and contains higher concentrations of trace metals than surface water. Water from the undistrubed coal- bearing beds and abandoned mines is not suitable for domestic, public supply, or agricultural uses. Large amounts of this highly mineralized ground water reaching local streams would have a deleterious effect on surface-water quality.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Lansing, MI","doi":"10.3133/ofr82511","usgsCitation":"Handy, A., 1982, Water quality of coal deposits and abandoned mines, Saginaw County, Michigan: U.S. Geological Survey Open-File Report 82-511, v, 35 p, https://doi.org/10.3133/ofr82511.","productDescription":"v, 35 p","numberOfPages":"45","costCenters":[{"id":382,"text":"Michigan Water Science Center","active":true,"usgs":true}],"links":[{"id":343704,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0511/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":142369,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0511/report-thumb.jpg"}],"country":"United States","state":"Michigan","county":"Saginaw County","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-84.1702,43.5689],[-84.0521,43.5668],[-84.0524,43.5235],[-83.8188,43.5217],[-83.8186,43.478],[-83.7,43.4787],[-83.7009,43.3941],[-83.6996,43.3317],[-83.6943,43.3252],[-83.694,43.2223],[-83.8154,43.2212],[-83.9318,43.2204],[-83.9294,43.1334],[-84.0519,43.1317],[-84.1687,43.1306],[-84.2874,43.1286],[-84.3684,43.1281],[-84.3698,43.2059],[-84.3701,43.2146],[-84.3717,43.3884],[-84.3718,43.4654],[-84.3713,43.4817],[-84.1719,43.4825],[-84.1702,43.5689]]]},\"properties\":{\"name\":\"Saginaw\",\"state\":\"MI\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a07e4b07f02db5f99be","contributors":{"authors":[{"text":"Handy, A.H.","contributorId":104493,"corporation":false,"usgs":true,"family":"Handy","given":"A.H.","email":"","affiliations":[],"preferred":false,"id":159486,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":56876,"text":"wdrMI811 - 1982 - Water resources data for Michigan, water year 1981","interactions":[],"lastModifiedDate":"2017-08-10T14:56:08","indexId":"wdrMI811","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"MI-81-1","title":"Water resources data for Michigan, water year 1981","docAbstract":"Water resources data for the 1981 water year for Michigan consist of records of stage, discharge, and water quality of streams; stage, contents, and water quality of lakes and reservoirs; and water levels and water temperature of ground water. This report contains discharge records for 178 gaging stations; stage only records for 4 gaging stations; stage and contents for 5 lakes and reservoirs; water quality for 45 continuous-record stations; and water levels for 53 observation wells. Also included are 85 crest-stage partial-record stations and 59 low-flow partial-record stations. Additional water data were collected at various sites, not part of the systematic data-collection program, and are published as miscellaneous measurements. These data represent that part of the National Water Data System operated by the U.S. Geological Survey and cooperating State and Federal agencies in Michigan.
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\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49fae4b07f02db5f3dd9","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":532963,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":25600,"text":"wri824076 - 1982 - Hydrologic-information needs for oil-shale development, northwestern Colorado","interactions":[],"lastModifiedDate":"2012-02-02T00:08:28","indexId":"wri824076","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"82-4076","title":"Hydrologic-information needs for oil-shale development, northwestern Colorado","docAbstract":"Hydrologic information is not adequate for proper development of the large oil-shale reserves of Piceance basin in northwestern Colorado. Exploratory drilling and aquifer testing are needed to define the hydrologic system, to provide wells for aquifer testing, to design mine-drainage techniques, and to explore for additional water supplies. Sampling networks are needed to supply hydrologic data on the quantity and quality of surface water, ground water, and springs. A detailed sampling network is proposed for the White River basin because of expected impacts related to water supplies and waste disposal. Emissions from oil-shale retorts to the atmosphere need additional study because of possible resulting corrosion problems and the destruction of fisheries. Studies of the leachate materials and the stability of disposed retorted shale piles are needed to insure that these materials will not cause problems. Hazards related to in-situ retorts, and the wastes related to oil-shale development in general also need further investigation. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri824076","usgsCitation":"Taylor, O., 1982, Hydrologic-information needs for oil-shale development, northwestern Colorado: U.S. Geological Survey Water-Resources Investigations Report 82-4076, ix, 101 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri824076.","productDescription":"ix, 101 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":123458,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1982/4076/report-thumb.jpg"},{"id":54344,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1982/4076/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa7e4b07f02db66710d","contributors":{"authors":[{"text":"Taylor, O.J.","contributorId":71584,"corporation":false,"usgs":true,"family":"Taylor","given":"O.J.","email":"","affiliations":[],"preferred":false,"id":194363,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":9768,"text":"ofr82528 - 1982 - Characteristics and description of cores from the USGS core hole CRU-1, Parachute Creek Member, Green River Formation, east-central Uinta Basin, Utah","interactions":[],"lastModifiedDate":"2012-02-02T00:06:14","indexId":"ofr82528","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"82-528","title":"Characteristics and description of cores from the USGS core hole CRU-1, Parachute Creek Member, Green River Formation, east-central Uinta Basin, Utah","docAbstract":"Oil-yield, lithologic, and mineral distribution data were determined for cores taken from a 497.7-foot drill hole in the upper part of the Parachute Creek Member of the Eocene Green River Formation. The drill hole, 1050 feet FEL, 700 feet FNL, sec. 3, T. 12 S., R. 24 E., Uintah County, Utah, started slightly below the contact between the Uinta Formation, also of Eocene age, and the underlying Green River Formation. It ended 32 feet below the base of the Mahogany bed (the richest oil-shale bed between A groove and B groove--which define the upper and lower boundaries, respectively, of the Mahogany zone). Most of the interval studied is kerogen- or carbonate-rich, commonly tuffaceous, and is very fine grained. \r\n\r\nSeveral thin (<3 feet) oil-shale beds which yield as much as 25 gallons of oil per ton occur above the Mahogany zone, but are probably not of economic interest. The cored sequence contains several tuff beds. The thickest of these beds is approximately 2 feet thick; the average thickness is rarely greater than 0.5 feet. Two oil-saturated tuff beds occur approximately 65 feet above the Mahogany oil-shale bed. Although these two tuffs are exposed on nearby surface outcrops, no evidence of oil is seen on outcrop. The Mahogany zone is approximately 69 feet thick at the drill site; the lowermost few feet were not penetrated. At the site cored, the Mahogany zone is overlain by 435 feet of overburden. Fischer assays indicate that 42.3 feet of oil shale within the Mahogany zone could yield at least 25 gallons of oil per ton from beds at least 10 feet thick.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82528","usgsCitation":"Keighin, C.W., 1982, Characteristics and description of cores from the USGS core hole CRU-1, Parachute Creek Member, Green River Formation, east-central Uinta Basin, Utah: U.S. Geological Survey Open-File Report 82-528, i, 46 p., ill., map ;28 cm., https://doi.org/10.3133/ofr82528.","productDescription":"i, 46 p., ill., map ;28 cm.","costCenters":[],"links":[{"id":142199,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0528/report-thumb.jpg"},{"id":37527,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0528/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e3e4b07f02db5e5592","contributors":{"authors":[{"text":"Keighin, C. W.","contributorId":79887,"corporation":false,"usgs":true,"family":"Keighin","given":"C.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":160263,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":56877,"text":"wdrSD811 - 1982 - Water resources data for South Dakota, water year 1981","interactions":[],"lastModifiedDate":"2020-10-23T20:40:50.251101","indexId":"wdrSD811","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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-81-1","title":"Water resources data for South Dakota, water year 1981","docAbstract":"No abstract available.
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