{"pageNumber":"5314","pageRowStart":"132825","pageSize":"25","recordCount":184752,"records":[{"id":8606,"text":"ofr82501 - 1982 - Ground water and geology of Marquette County, Michigan","interactions":[],"lastModifiedDate":"2016-09-22T14:26:12","indexId":"ofr82501","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":"82-501","title":"Ground water and geology of Marquette County, Michigan","docAbstract":"<p>Ground-water resources of Marquette County are about evenly divided between bedrock aquifers and aquifers in glacial deposits. In the northern and the extreme southern parts of the county, most wells are completed in bedrock at depths less than 100 feet. In the central part, most wells are completed in glacial deposits; some of these wells are as deep as 200 feet. Yields, in some places as high as 300 gallons per minute, are generally greatest from wells completed in glacial deposits. Most well water is hard and has iron concentrations ranging from &lt;0.1 mg/L to about 5.0 mg/L. Both ground water and surface water sources are used in municipal water systems.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Lansing, MI","doi":"10.3133/ofr82501","collaboration":"Prepared in cooperation with the Michigan Department of Natural Resources","usgsCitation":"Doonan, C.J., and Van Alstine, J.L., 1982, Ground water and geology of Marquette County, Michigan: U.S. Geological Survey Open-File Report 82-501, Document: vi, 46 p.; Plate: 27.03 x 34.96 inches, https://doi.org/10.3133/ofr82501.","productDescription":"Document: vi, 46 p.; Plate: 27.03 x 34.96 inches","costCenters":[{"id":382,"text":"Michigan Water Science Center","active":true,"usgs":true}],"links":[{"id":141059,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0501/report-thumb.jpg"},{"id":36203,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0501/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":36204,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0501/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Michigan","county":"Marquette 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sgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ab0e4b07f02db66dc6a","contributors":{"authors":[{"text":"Doonan, C. J.","contributorId":62592,"corporation":false,"usgs":true,"family":"Doonan","given":"C.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":158023,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Van Alstine, J. L.","contributorId":85962,"corporation":false,"usgs":true,"family":"Van Alstine","given":"J.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":158024,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":42378,"text":"ofr82610 - 1982 - Reconnaissance geology of the Jabal Shaqran Quadrangle, sheet 17/44 B, Kingdom of Saudi Arabia","interactions":[],"lastModifiedDate":"2012-02-02T00:05:05","indexId":"ofr82610","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":"82-610","title":"Reconnaissance geology of the Jabal Shaqran Quadrangle, sheet 17/44 B, Kingdom of Saudi Arabia","docAbstract":"The Jabal Shaqran quadrangle lies in the southeastern Asir province, mostly within the westernmost part of the Rub al Khali desert, and is largely covered by Quaternary deposits. Proterozoic crystalline rocks are exposed as inselbergs or rock pediment surfaces along the western border of the quadrangle. The crystalline basement is metavolcanic rock intruded by plutonic to hypabyssal rocks consisting of diorite and gabbro, biotite tonalite gneiss, biotite-hornblende monzogranite, biotite-sodic amphibole granite, and syenogranite to quartz syenite, listed in the inferred order of emplacement. Rhyolite-dacite fels, associated with andesitic to basaltic metavolcanic flow rocks and minor amphibolite, is interpreted to have resulted from metasomatic alteration of the flow rocks during emplacement of granitic plutons. \r\n\r\nThe Wajid Sandstone, of Cambrian to Ordovician age, is largely a coarse-grained quartz arenite with pebbly phases; common crossbedds indicate north-northwest to north-northeast directions of sand transport. Beds are cemented by iron oxide, carbonate, and minor quartz. The Wajid Sandstone is exposed only in the northwestern and northern parts of the quadrangle. \r\n\r\nQuaternary deposits record a climate that became increasingly more arid. They include Holocene and Pleistocene(?) alluvial and fluvial deposits of sand, gravel, and silt, minor carbonate crusts, and eolian sand and silt. Gravel terraces and gravel plains less than 10 m above the present major wadi channels are widespread and commonly are overlain by marly silt along the wadis. Between major wadis, which discharge into the Rub al Khali basin, gravel-topped surfaces are partly covered by a complex of low, sinuous, discontinuous, generally northwest trending transverse sand dunes. Normal to this trend, higher and more extensive linear dunes and dune complexes, including seif (irq) dunes as high as 50 m, have encroached southwestward. The transverse and linear dunes may represent two stages of advance separated by a pluvial cycle. Studies of aerial photographs indicate that the dunes have not changed appreciably in shape or size between 1951 and 1959, although some seif dunes have advanced their leading edges 15 to 25 m. \r\n\r\nNo potentially economic mineral resources other than sand and gravel were found.","language":"ENGLISH","doi":"10.3133/ofr82610","usgsCitation":"Sable, E.G., 1982, Reconnaissance geology of the Jabal Shaqran Quadrangle, sheet 17/44 B, Kingdom of Saudi Arabia: U.S. Geological Survey Open-File Report 82-610, 1 map :photocopy ;56 x 53 cm., on sheet 70 x 78 cm. +1 text (iii, 19 p. ill. ; 28 cm.), https://doi.org/10.3133/ofr82610.","productDescription":"1 map :photocopy ;56 x 53 cm., on sheet 70 x 78 cm. +1 text (iii, 19 p. ill. ; 28 cm.)","costCenters":[],"links":[{"id":136880,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0610/report-thumb.jpg"},{"id":80142,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0610/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":80143,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0610/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a6fe4b07f02db640949","contributors":{"authors":[{"text":"Sable, Edward G.","contributorId":51273,"corporation":false,"usgs":true,"family":"Sable","given":"Edward","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":226368,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":7274,"text":"ofr8214 - 1982 - Landsat monitoring of albedo changes in northwestern Arizona, 1977-1980","interactions":[],"lastModifiedDate":"2017-03-28T14:21:40","indexId":"ofr8214","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":"82-14","title":"Landsat monitoring of albedo changes in northwestern Arizona, 1977-1980","docAbstract":"As part of a cooperative project between the U.S. Geological Survey and the Bureau of Land Management, changes in albedo (percentage of light reflected from the ground) were calculated and mapped from Landsat images for an area in northwestern Arizona for three periods: August 26, 1977, to September 3, 1979; September 3, 1979, to August 28, 1980; and August 26, 1977, to August 28, 1980. The mapped albedo changes were field checked in April 1981. Decreases in albedo were associated with increases in vegetation, primarily the flush of annual vegetation and the regrowth of vegetation in chained areas and sites of past fires. Increases in albedo were due to recent fires. \r\n\r\nContinuous monitoring of changes in albedo using current, rather than historical, Landsat images can provide the Bureau of Land Management with a means of monitoring vegetation growth, determining areas of high fire potential, and more efficiently deploying of field personnel to sites where severe changes are occuring in the quality of the land and vegetation resources. For example, an albedo change could be an indication of encroachment by an invader species. Similarly, it could indicate where rangeland is being lost to desertification.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr8214","usgsCitation":"Robinove, C.J., 1982, Landsat monitoring of albedo changes in northwestern Arizona, 1977-1980: U.S. Geological Survey Open-File Report 82-14, 14 p., https://doi.org/10.3133/ofr8214.","productDescription":"14 p.","costCenters":[{"id":222,"text":"Earth Resources Observation and Science (EROS) Center","active":true,"usgs":true}],"links":[{"id":34652,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0014/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":140323,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0014/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b20e4b07f02db6abb65","contributors":{"authors":[{"text":"Robinove, Charles Joseph","contributorId":71153,"corporation":false,"usgs":true,"family":"Robinove","given":"Charles","email":"","middleInitial":"Joseph","affiliations":[],"preferred":false,"id":154995,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":8301,"text":"ofr821029 - 1982 - Occurrences of copper minerals in Alaska","interactions":[{"subject":{"id":8301,"text":"ofr821029 - 1982 - Occurrences of copper minerals in Alaska","indexId":"ofr821029","publicationYear":"1982","noYear":false,"title":"Occurrences of copper minerals in Alaska"},"predicate":"SUPERSEDED_BY","object":{"id":69289,"text":"mr90 - 1984 - Map showing occurrences of copper minerals in Alaska","indexId":"mr90","publicationYear":"1984","noYear":false,"title":"Map showing occurrences of copper minerals in Alaska"},"id":1}],"supersededBy":{"id":69289,"text":"mr90 - 1984 - Map showing occurrences of copper minerals in Alaska","indexId":"mr90","publicationYear":"1984","noYear":false,"title":"Map showing occurrences of copper minerals in Alaska"},"lastModifiedDate":"2023-11-21T22:47:38.310187","indexId":"ofr821029","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":"82-1029","title":"Occurrences of copper minerals in Alaska","docAbstract":"<p>The following references give data, as of June 1, 1982, on localities where copper minerals have been found in Alaska. References are keyed by number to locations shown on the accompanying map. An asterisk (*) preceding a locality name indicates recorded production.</p><p>In most instances the report(s) cited for each occurrence is a summary of data in older reports and was compiled since 1975. Most of the summary reports contain lists of the reports used in their compilation. Citations are in standard bibliographic format with the exception that each includes, in parentheses, an abbreviation for the report or map series and the number of the report or map. Abbreviations used are: AOF, State of Alaska Division of Geological and Geophysical Surveys Open-File Report; B, U.S. Geological Survey Bulletin; BMOF, U.S. Bureau of Mines Open-File Report; C, U.S. Geological Survey Circular; MF, U.S. Geological Survey Miscellaneous Field Studies Map; OF, U.S. Geological Survey Open-File Report; P, U.S. Geological Survey Professional Paper.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr821029","usgsCitation":"1982, Occurrences of copper minerals in Alaska: U.S. Geological Survey Open-File Report 82-1029, Report: 32 p.; 1 Plate: 47.99 x 35.97 inches, https://doi.org/10.3133/ofr821029.","productDescription":"Report: 32 p.; 1 Plate: 47.99 x 35.97 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,{"id":29786,"text":"wri8173 - 1982 - A stormwater management model for the West Branch Brandywine Creek, Chester County, Pennsylvania","interactions":[],"lastModifiedDate":"2017-06-09T11:25:16","indexId":"wri8173","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":"81-73","title":"A stormwater management model for the West Branch Brandywine Creek, Chester County, Pennsylvania","docAbstract":"<p>Three subbasins in the West Branch Brandywine Creek watershed were modeled by the Dawby, Schaake, and Alley distributed routing rainfall- runoff model. The Honeybrook subbasin could not be calibrated because of nonrepresentative rainfall data. The Coatesville subbasin was calibrated, but not verified; the average standard error of estimate is 34 percent for peak discharge. The Modena subbasin was calibrated and verified. Average error for peak discharge is 38 percent for calibration and 24 percent for verification.</p>\n<p>Predictive simulations using selected storms were made to determine the effects of projected population and four proposed flood-control structures in the Coatesville and Modena subbasins. Simulation of projected population growth in both subbasins showed that runoff volumes would generally have a greater percentage increase for low-magnitude floods than for high-magnitude floods. Proposed flood-control structure PA-436D had the greatest reduction in peak discharge at West Branch Brandywine Creek at Coatesville when a large quantity of runoff entered the Coatesville subbasin from upstream. WA-2 had the greatest reduction in peak discharge when most of the runoff came from within the Coatesville subbasin. Although WA-2 and PA-430 will control about the same drainage area, WA-2 causes a greater reduction in peak discharge at Coatesville because PA-430 is to be located upstream from Rock Run Reservoir, which provides some flood- water storage. In the Modena subbasin, the simulated effect of proposed flood-control structure PA-428 showed that it would lower the peak discharge of Sucker Run at State Route 82 and either raise or have no effect on peak discharges at West Branch Brandywine Creek at Modena. Most simulations of the effects of proposed flood-control structures in the Coatesville subbasin on peak discharge at Modena showed a reduction in peak discharge.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri8173","usgsCitation":"Sloto, R.A., 1982, A stormwater management model for the West Branch Brandywine Creek, Chester County, Pennsylvania: U.S. Geological Survey Water-Resources Investigations Report 81-73, v, 34 p., https://doi.org/10.3133/wri8173.","productDescription":"v, 34 p.","numberOfPages":"43","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":532,"text":"Pennsylvania Water Science Center","active":true,"usgs":true}],"links":[{"id":159723,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/wri8173.jpg"},{"id":310282,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1981/0073/report.pdf","text":"Report","linkFileType":{"id":1,"text":"pdf"}}],"country":"United 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,{"id":7145,"text":"ofr82948 - 1982 - Geochemical analyses for platinum group elements in rock samples from the Kalmiopsis Wilderness, southwestern Oregon","interactions":[],"lastModifiedDate":"2012-02-02T00:06:03","indexId":"ofr82948","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":"82-948","title":"Geochemical analyses for platinum group elements in rock samples from the Kalmiopsis Wilderness, southwestern Oregon","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82948","usgsCitation":"Carlson, R.R., Carlson, C., Grimes, D.J., Leinz, R.W., and Page, N., 1982, Geochemical analyses for platinum group elements in rock samples from the Kalmiopsis Wilderness, southwestern Oregon: U.S. Geological Survey Open-File Report 82-948, 68 p., maps ;28 cm., https://doi.org/10.3133/ofr82948.","productDescription":"68 p., maps ;28 cm.","costCenters":[],"links":[{"id":140512,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0948/report-thumb.jpg"},{"id":34454,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0948/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b24e4b07f02db6ae932","contributors":{"authors":[{"text":"Carlson, R. R.","contributorId":75918,"corporation":false,"usgs":true,"family":"Carlson","given":"R.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":154472,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Carlson, C.A.","contributorId":85178,"corporation":false,"usgs":true,"family":"Carlson","given":"C.A.","email":"","affiliations":[],"preferred":false,"id":154473,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Grimes, D. J.","contributorId":73575,"corporation":false,"usgs":true,"family":"Grimes","given":"D.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":154471,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Leinz, R. W.","contributorId":89885,"corporation":false,"usgs":true,"family":"Leinz","given":"R.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":154474,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Page, N.J.","contributorId":38125,"corporation":false,"usgs":true,"family":"Page","given":"N.J.","affiliations":[],"preferred":false,"id":154470,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":7127,"text":"ofr811115 - 1982 - An evaluation of water-quality monitoring in the Brandywine Creek basin, Pennsylvania, 1973-78","interactions":[],"lastModifiedDate":"2017-06-20T10:02:13","indexId":"ofr811115","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":"81-1115","title":"An evaluation of water-quality monitoring in the Brandywine Creek basin, Pennsylvania, 1973-78","docAbstract":"Data recorded from 1973 through 1978 by monitors on West Branch Brandywine Creek at Modena, East Branch Brandywine Creek below Downingtown, and Brandywine Creek at Chadds Ford were analyzed to evaluate the effectiveness of the monitors in describing water-quality conditions. The data show that the stream at Modena and below Downingtown had periods of low dissolved oxygen, and that the stream below Downingtown had a particularly severe dissolved-oxygen deficiency from May through September 1974. The pH at all three sites exceeded 9.0 at times and the pH below Downingtown occasionally dropped below 6.0. The most critical period in the basin was from March to November when pH was most likely to exceed water-quality standards and dissolved oxygen was most likely to fall below the standards. Without the monitors, the extent and magnitude of these problems would not have been detected.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Harrisburg, PA","doi":"10.3133/ofr811115","usgsCitation":"Murphy, J., Ritter, J., Brown, A., and Chiarella, J., 1982, An evaluation of water-quality monitoring in the Brandywine Creek basin, Pennsylvania, 1973-78: U.S. Geological Survey Open-File Report 81-1115, iv, 28 p., https://doi.org/10.3133/ofr811115.","productDescription":"iv, 28 p.","additionalOnlineFiles":"N","costCenters":[{"id":532,"text":"Pennsylvania Water Science Center","active":true,"usgs":true}],"links":[{"id":141561,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/1115/report-thumb.jpg"},{"id":277911,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/1115/report.pdf"}],"country":"United States","state":"Pennsylvania","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -76.0000,39.7283 ], [ -76.0000,40.1250 ], [ -75.2563,40.1250 ], [ -75.2563,39.7283 ], [ -76.0000,39.7283 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad8e4b07f02db68484c","contributors":{"authors":[{"text":"Murphy, J.J.","contributorId":69144,"corporation":false,"usgs":true,"family":"Murphy","given":"J.J.","email":"","affiliations":[],"preferred":false,"id":154391,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ritter, J.R.","contributorId":22350,"corporation":false,"usgs":true,"family":"Ritter","given":"J.R.","email":"","affiliations":[],"preferred":false,"id":154389,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Brown, A.E.","contributorId":48557,"corporation":false,"usgs":true,"family":"Brown","given":"A.E.","email":"","affiliations":[],"preferred":false,"id":154390,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Chiarella, J.P.","contributorId":17603,"corporation":false,"usgs":true,"family":"Chiarella","given":"J.P.","email":"","affiliations":[],"preferred":false,"id":154388,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":65011,"text":"i1251D - 1982 - Aeroradioactivity map of the Charlotte 1 degree by 2 degrees Quadrangle, North Carolina and South Carolina","interactions":[],"lastModifiedDate":"2012-02-10T00:11:09","indexId":"i1251D","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":320,"text":"IMAP","code":"I","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1251","subseriesTitle":"NONE","chapter":"D","title":"Aeroradioactivity map of the Charlotte 1 degree by 2 degrees Quadrangle, North Carolina and South Carolina","language":"ENGLISH","doi":"10.3133/i1251D","usgsCitation":"Daniels, D.L., and Zietz, I., 1982, Aeroradioactivity map of the Charlotte 1 degree by 2 degrees Quadrangle, North Carolina and South Carolina: U.S. Geological Survey IMAP 1251, 1 map :col. ;44 x 73 cm. folded in envelope 30 x 24 cm., https://doi.org/10.3133/i1251D.","productDescription":"1 map :col. ;44 x 73 cm. folded in envelope 30 x 24 cm.","costCenters":[],"links":[{"id":189254,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":106664,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_9067.htm","linkFileType":{"id":5,"text":"html"},"description":"9067"}],"scale":"250000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -82,35 ], [ -82,36 ], [ -80,36 ], [ -80,35 ], [ -82,35 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae4e4b07f02db689abe","contributors":{"authors":[{"text":"Daniels, D. L.","contributorId":69114,"corporation":false,"usgs":true,"family":"Daniels","given":"D.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":272506,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Zietz, Isidore","contributorId":76708,"corporation":false,"usgs":true,"family":"Zietz","given":"Isidore","affiliations":[],"preferred":false,"id":272507,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":7130,"text":"ofr82612 - 1982 - Reconnaissance geologic map of south-central Misheguk Mountain Quadrangle, Alaska","interactions":[{"subject":{"id":7130,"text":"ofr82612 - 1982 - Reconnaissance geologic map of south-central Misheguk Mountain Quadrangle, Alaska","indexId":"ofr82612","publicationYear":"1982","noYear":false,"title":"Reconnaissance geologic map of south-central Misheguk Mountain Quadrangle, Alaska"},"predicate":"SUPERSEDED_BY","object":{"id":64589,"text":"i1504 - 1984 - Reconnaissance geologic map of south-central Misheguk Mountain Quadrangle, Alaska","indexId":"i1504","publicationYear":"1984","noYear":false,"title":"Reconnaissance geologic map of south-central Misheguk Mountain Quadrangle, Alaska"},"id":1}],"supersededBy":{"id":64589,"text":"i1504 - 1984 - Reconnaissance geologic map of south-central Misheguk Mountain Quadrangle, Alaska","indexId":"i1504","publicationYear":"1984","noYear":false,"title":"Reconnaissance geologic map of south-central Misheguk Mountain Quadrangle, Alaska"},"lastModifiedDate":"2023-12-29T23:39:00.674933","indexId":"ofr82612","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":"82-612","title":"Reconnaissance geologic map of south-central Misheguk Mountain Quadrangle, Alaska","docAbstract":"<p>This map is one of a series of three reconnaissance geologic maps of the southern Misheguk Mountain quadrangle (fig. 1). Because the geology in all three map areas is similar, a composite map explanation has been designed to facilitate their combined use and provide the reader with a better perspective of the regional geology. There are some rock units and allochthons which do not occur on all three maps. For this reason, the explanation contains more rock units than occur on any one map. Rock units which appear on the accompanying map are indicated by an asterisk beside the map symbol in the explanation.</p><p><br data-mce-bogus=\"1\"></p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr82612","usgsCitation":"Ellersieck, I., Curtis, S., Mayfield, C., and Tailleur, I., 1982, Reconnaissance geologic map of south-central Misheguk Mountain Quadrangle, Alaska: U.S. Geological Survey Open-File Report 82-612, Report: 37 p.; 2 Plates: 29.63 x 53.51 inches and 52.87 x 24.75 inches, https://doi.org/10.3133/ofr82612.","productDescription":"Report: 37 p.; 2 Plates: 29.63 x 53.51 inches and 52.87 x 24.75 inches","costCenters":[],"links":[{"id":424047,"rank":5,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0612/plate-1-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":424046,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0612/plate-1-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":424045,"rank":3,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0612/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":140004,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0612/report-thumb.jpg"},{"id":388850,"rank":2,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_13779.htm"}],"country":"United States","state":"Alaska","otherGeospatial":"Misheguk Mountain Quadrangle","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -160,\n              68.0\n            ],\n            [\n              -161,\n              68.0\n            ],\n            [\n              -161,\n              68.6\n            ],\n            [\n              -160,\n              68.6\n            ],\n            [\n              -160,\n              68.0\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a73e4b07f02db643758","contributors":{"authors":[{"text":"Ellersieck, Inyo","contributorId":34914,"corporation":false,"usgs":true,"family":"Ellersieck","given":"Inyo","affiliations":[],"preferred":false,"id":154403,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Curtis, S.M.","contributorId":16823,"corporation":false,"usgs":true,"family":"Curtis","given":"S.M.","email":"","affiliations":[],"preferred":false,"id":154402,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Mayfield, C.F.","contributorId":95467,"corporation":false,"usgs":true,"family":"Mayfield","given":"C.F.","email":"","affiliations":[],"preferred":false,"id":154405,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Tailleur, I.L.","contributorId":59027,"corporation":false,"usgs":true,"family":"Tailleur","given":"I.L.","email":"","affiliations":[],"preferred":false,"id":154404,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":29740,"text":"wri8150 - 1982 - Sinkhole development resulting from ground-water withdrawal in the Tampa area, Florida","interactions":[],"lastModifiedDate":"2012-02-10T00:10:08","indexId":"wri8150","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":"81-50","title":"Sinkhole development resulting from ground-water withdrawal in the Tampa area, Florida","docAbstract":"The area of municipal well fields on the Gulf Coastal Plain north of tampa, Fla., is densely pitted with natural sinkholes and sinkhole lakes that have resulted from collapse of surficial sand and clay into solution cavities in the underlying carbonate rocks of the Floridan aquifer. Although solution of the underlying rocks is the ultimate cause of sinkholes, some have been induced by abrupt changes in ground-water levels caused by pumping. Declines in water levels cause loss of support to the bedrock roofs over cavities and to surficial material overlying openings in the top of bedrock. The volume of calcium, magnesium , and carbonate (the constituents of limestone and dolomite) in solution in the water withdrawn from four well fields near Tampa totaled about 240,000 cubic feet in 1978. Most induced solution takes place at the limestone surface however, and the area of induced recharge is so extensive that the effect of induced limestone solution on sinkhole development is negligible. Alinement of established sinkholes along joint patterns in the bedrock suggests that a well along these lineations might have direct hydraulic connection with a zone of incipient sinkholes. Therefore, pumping of large-capacity wells along such lineations would increase the probability of sinkhole development. Although sinkholes generally form abruptly in the study area, local changes such as vegetative stress, ponding of rainfall, misalinement of structures, and turbidity in well water are all indications that percollapse subsidence may be taking place. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wri8150","collaboration":"Prepared in cooperation with the Southwest Florida Water Management District","usgsCitation":"Sinclair, W.C., 1982, Sinkhole development resulting from ground-water withdrawal in the Tampa area, Florida: U.S. Geological Survey Water-Resources Investigations Report 81-50, iv, 19 p.; ill., maps; 28 cm., https://doi.org/10.3133/wri8150.","productDescription":"iv, 19 p.; ill., maps; 28 cm.","startPage":"i","endPage":"19","numberOfPages":"23","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":116992,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1981/0050/report-thumb.jpg"},{"id":24584,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/wri/1981/0050/","linkFileType":{"id":5,"text":"html"}},{"id":58542,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1981/0050/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Florida","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -82.83333333333333,27.916666666666668 ], [ -82.83333333333333,28.25 ], [ -82.16666666666667,28.25 ], [ -82.16666666666667,27.916666666666668 ], [ -82.83333333333333,27.916666666666668 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f6e4b07f02db5f171a","contributors":{"authors":[{"text":"Sinclair, William C.","contributorId":14798,"corporation":false,"usgs":true,"family":"Sinclair","given":"William","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":202040,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":7296,"text":"ofr82406 - 1982 - Lode gold and silver occurrences in Alaska","interactions":[{"subject":{"id":7296,"text":"ofr82406 - 1982 - Lode gold and silver occurrences in Alaska","indexId":"ofr82406","publicationYear":"1982","noYear":false,"title":"Lode gold and silver occurrences in Alaska"},"predicate":"SUPERSEDED_BY","object":{"id":61994,"text":"mr84 - 1984 - Map showing occurrences of lode gold and silver in Alaska","indexId":"mr84","publicationYear":"1984","noYear":false,"title":"Map showing occurrences of lode gold and silver in Alaska"},"id":1}],"supersededBy":{"id":61994,"text":"mr84 - 1984 - Map showing occurrences of lode gold and silver in Alaska","indexId":"mr84","publicationYear":"1984","noYear":false,"title":"Map showing occurrences of lode gold and silver in Alaska"},"lastModifiedDate":"2023-09-29T20:05:34.765896","indexId":"ofr82406","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":"82-406","title":"Lode gold and silver occurrences in Alaska","docAbstract":"<p>The following references give data, as of September 1, 1981, on localities where lode gold or silver has been found and are keyed to locations shown on the accompanying map. An asterisk (*) preceding a locality name indicates recorded production. In most instances the report(s) cited for each occurrence is a summary of data in older reports and was compiled since 1975. Most of the summary reports contain lists of the reports used in their compilation. Citations are in standard bibliographic format with the exception that each includes, in parentheses, an abbreviation for the report series and the number of the report. Abbreviations are: AOF, State of Alaska Division of Geological and Geophysical Surveys Open-File Report; B, U.S. Geological Survey Bulletin; BMOF, U.S. Bureau of Mines Open-File Report; MF, U.S. Geological Survey Miscellaneous Field Studies Map; OF, U.S. Geological Survey Open-File Report.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr82406","usgsCitation":"Cobb, E., 1982, Lode gold and silver occurrences in Alaska: U.S. Geological Survey Open-File Report 82-406, Report: 31 p.; 1 Plate: 49.90 x 37.51 inches, https://doi.org/10.3133/ofr82406.","productDescription":"Report: 31 p.; 1 Plate: 49.90 x 37.51 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,{"id":7490,"text":"ofr82346 - 1982 - Results of hydraulic tests in U.S. Department of Energy's wells DOE-4, 5, 6, 7, 8, and 9, Salt Valley, Grand County, Utah","interactions":[],"lastModifiedDate":"2017-09-02T09:55:54","indexId":"ofr82346","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":"82-346","title":"Results of hydraulic tests in U.S. Department of Energy's wells DOE-4, 5, 6, 7, 8, and 9, Salt Valley, Grand County, Utah","docAbstract":"<p>Six exploratory wells were drilled into the cap rock underlying Salt Valley, Utah, for geologic, geophysical, and hydrologic data to augment information obtained from three previous test wells. Drilling of three other test holes was abandoned due to caving and loss of drilling tools, Before reaching the zone of saturation; the upper 100 meters of cap rock is unsaturated. Within the saturated part of the cap rock, hydraulic heads generally decrease with depth and to the northwest in this part of the valley.</p><p>Hydraulic conductivity of the cap rock, as determined from pumping tests, ranged from 9.3 X 10<sup>-5</sup> to 2.06 X 10<span id=\"_mce_caret\" data-mce-bogus=\"true\"><sup>-1</sup></span> meters per day; as a result, groundwater flow rates in the cap rock are low. Water ranges from a calcium bicarbonate sulfate type on the western edge of the valley to a calcium magnesium sodium bicarbonate, sulfate, chloride type near the center of the valley. Carbon-14 specific activity for cap-rock water yielded an uncorrected age of about 17,000 to 26,000 years before present near the western edge of the valley and about 41,000 years before present near the center of the valley.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Denver, CO","doi":"10.3133/ofr82346","collaboration":"Prepared in cooperation with the U.S. Department of Energy","usgsCitation":"Wollitz, L.E., Thordarson, W., Whitfield, M.S., and Weir, J.E., 1982, Results of hydraulic tests in U.S. Department of Energy's wells DOE-4, 5, 6, 7, 8, and 9, Salt Valley, Grand County, Utah: U.S. Geological Survey Open-File Report 82-346, vii, 71 p., https://doi.org/10.3133/ofr82346.","productDescription":"vii, 71 p.","numberOfPages":"78","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":140454,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0346/report-thumb.jpg"},{"id":34934,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0346/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Utah","county":"Grand County","otherGeospatial":"Salt Valley","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9be4b07f02db65e092","contributors":{"authors":[{"text":"Wollitz, Leonard E.","contributorId":22340,"corporation":false,"usgs":true,"family":"Wollitz","given":"Leonard","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":155857,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Thordarson, William","contributorId":23539,"corporation":false,"usgs":true,"family":"Thordarson","given":"William","email":"","affiliations":[],"preferred":false,"id":155858,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Whitfield, Merrick S. Jr.","contributorId":67911,"corporation":false,"usgs":true,"family":"Whitfield","given":"Merrick","suffix":"Jr.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":155859,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Weir, James E. Jr.","contributorId":47419,"corporation":false,"usgs":true,"family":"Weir","given":"James","suffix":"Jr.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":155860,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":9732,"text":"ofr82373 - 1982 - Quality of water in Luxapallia Creek at Columbus, Mississippi","interactions":[],"lastModifiedDate":"2022-08-23T20:06:49.956171","indexId":"ofr82373","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":"82-373","title":"Quality of water in Luxapallia Creek at Columbus, Mississippi","docAbstract":"<p>A quality-of-water study was conducted on September 9-12, 1979, on Luxapallila Creek and its tributaries, Magby and McCrary Creeks. The short term study indicated that the water in Luxapallila, Magby, and McCrary Creeks is suitable for many purposes.</p><p>The dissolved-oxygen concentration, temperature, and pH of the water in Luxapallila Creek changed little downstream from site 1 to site 5. The mean specific conductance increased from 25 micromhos per centimeter at site 1 to 46 micromhos per centimeter at site 5. The concentrations of nitrogen and phosphorus species, densities of fecal bacteria and 5-day biochemical-oxygen-demand load in Luxapallila Creek also increased downstream.</p><p>The maximum BOD<sub>5</sub> increased from 0.7 mg/L at the upstream site to 2.6 mg/L at the most downstream site. The maximum total nitrogen concentration increased from 0.71 mg/L to 2.0 mg/L. The maximum ammonia nitrogen concentration increased from 0.08 mg/L to 0.50 mg/L. Maximum nitrate plus nitrite concentrations increased from 0.13 mg/L to 0.15 mg/L and the maximum organic nitrogen concentrations increased from 0.53 mg/L to 1.6 mg/L.</p><p>Maximum total phosphorus concentrations increased from 0.04 mg/L at the upstream site to 0.30 mg/L at the downstream site.</p><p>The fecal coliform to fecal streptococcus ratio of three of five samples collected at site 5 was greater than 4.0 strongly suggesting the presence of human wastes at the downstream sites during the study.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr82373","collaboration":"Prepared in cooperation with the Mississippi Department of Natural Resources Bureau of Pollution Control","usgsCitation":"Kalkhoff, S.J., 1982, Quality of water in Luxapallia Creek at Columbus, Mississippi: U.S. Geological Survey Open-File Report 82-373, v, 38 p., https://doi.org/10.3133/ofr82373.","productDescription":"v, 38 p.","costCenters":[],"links":[{"id":405490,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0373/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":143058,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0373/report-thumb.jpg"}],"country":"United States","state":"Mississippi","city":"Columbus","otherGeospatial":"Luxapallia Creek","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -88.44131469726562,\n              33.47154465603414\n            ],\n            [\n              -88.37127685546875,\n              33.47154465603414\n            ],\n            [\n              -88.37127685546875,\n              33.529947711130646\n            ],\n            [\n              -88.44131469726562,\n              33.529947711130646\n            ],\n            [\n              -88.44131469726562,\n              33.47154465603414\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a8be4b07f02db6516cb","contributors":{"authors":[{"text":"Kalkhoff, Stephen J. 0000-0003-4110-1716 sjkalkho@usgs.gov","orcid":"https://orcid.org/0000-0003-4110-1716","contributorId":1731,"corporation":false,"usgs":true,"family":"Kalkhoff","given":"Stephen","email":"sjkalkho@usgs.gov","middleInitial":"J.","affiliations":[{"id":36532,"text":"Central Midwest Water Science Center","active":true,"usgs":true},{"id":351,"text":"Iowa Water Science Center","active":true,"usgs":true},{"id":35680,"text":"Illinois-Iowa-Missouri Water Science Center","active":true,"usgs":true}],"preferred":true,"id":160202,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":41986,"text":"ofr82540 - 1982 - Aeromagnetic map of Mt. Baker, Washington","interactions":[],"lastModifiedDate":"2012-02-02T00:05:02","indexId":"ofr82540","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":"82-540","title":"Aeromagnetic map of Mt. Baker, Washington","language":"ENGLISH","doi":"10.3133/ofr82540","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1982, Aeromagnetic map of Mt. Baker, Washington: U.S. Geological Survey Open-File Report 82-540, 1 map ;49 x 48 cm., https://doi.org/10.3133/ofr82540.","productDescription":"1 map ;49 x 48 cm.","costCenters":[],"links":[{"id":135427,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":79742,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0540/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b00e4b07f02db698000","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":530753,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":7140,"text":"ofr82589 - 1982 - Field, model, and computer simulation study of some aspects of the origin and distribution of Colorado Plateau-type uranium deposits","interactions":[],"lastModifiedDate":"2012-02-02T00:06:08","indexId":"ofr82589","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":"82-589","title":"Field, model, and computer simulation study of some aspects of the origin and distribution of Colorado Plateau-type uranium deposits","docAbstract":"Numerous hypotheses have been proposed to account for the nature and distribution of tabular uranium and vanadium-uranium deposits of the Colorado Plateau. In one of these hypotheses it is suggested that the deposits resulted from geochemical reactions at the interface between a relatively stagnant groundwater solution and a dynamic, ore-carrying groundwater solution which permeated the host sandstones (Shawe, 1956; Granger, et al., 1961; Granger, 1968, 1976; and Granger and Warren, 1979). The study described here was designed to investigate some aspects of this hypothesis, particularly the nature of fluid flow in sands and sandstones, the nature and distribution of deposits, and the relations between the deposits and the host sandstones. \r\n\r\nThe investigation, which was divided into three phases, involved physical model, field, and computer simulation studies. During the initial phase of the investigation, physical model studies were conducted in porous-media flumes. These studies verified the fact that humic acid precipitates could form at the interface between a humic acid solution and a potassium aluminum sulfate solution and that the nature and distribution of these precipitates were related to flow phenomena and to the nature and distribution of the host porous-media. During the second phase of the investigation field studies of permeability and porosity patterns in Holocene stream deposits were investigated and the data obtained were used to design more realistic porous media models. These model studies, which simulated actual stream deposits, demonstrated that precipitates possess many characteristics, in terms of their nature and relation to host sandstones, that are similar to ore deposits of the Colorado Plateau. \r\n\r\nThe final phase of the investigation involved field studies of actual deposits, additional model studies in a large indoor flume, and computer simulation studies. The field investigations provided an up-to-date interpretation of the depositional environments of the host sandstones in the Slick Rock District and data on the nature and distribution of the ore deposits which are found to be directly related to the architecture of the host sandstones which acted as conduits for the transport of mineralized groundwaters. Large-scale model studies, designed to simulate Grants Mineral Belt deposits, demonstrated that precipitates had characteristics similar to those of actual uranium deposits and data obtained from these studies strongly supported the hypothesis that the ores formed soon after deposition of the host sandstones and that their distribution was largely controlled by permeability and porosity patterns established at the time of deposition of the host sandstones. \r\n\r\nA numerical model was developed during the second and third stages of the investigation that can predict favorable locations for mineralization given sufficient data on porosity, hydraulic conductivity, the distribution and thickness of sandstone hosts, and an estimate of the initial hydrologic conditions. The model was successfully tested using data from the Slick Rock District.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82589","usgsCitation":"Ethridge, F., Sunada, D., Tyler, N., and Andrews, S., 1982, Field, model, and computer simulation study of some aspects of the origin and distribution of Colorado Plateau-type uranium deposits: U.S. Geological Survey Open-File Report 82-589, 56 p., ill., maps ;28 cm., https://doi.org/10.3133/ofr82589.","productDescription":"56 p., ill., maps ;28 cm.","costCenters":[],"links":[{"id":141542,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0589/report-thumb.jpg"},{"id":34446,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0589/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49bde4b07f02db5d0bc1","contributors":{"authors":[{"text":"Ethridge, F.G.","contributorId":42211,"corporation":false,"usgs":true,"family":"Ethridge","given":"F.G.","email":"","affiliations":[],"preferred":false,"id":154448,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Sunada, D.K.","contributorId":87940,"corporation":false,"usgs":true,"family":"Sunada","given":"D.K.","email":"","affiliations":[],"preferred":false,"id":154449,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Tyler, Noel","contributorId":16010,"corporation":false,"usgs":true,"family":"Tyler","given":"Noel","email":"","affiliations":[],"preferred":false,"id":154447,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Andrews, Sarah","contributorId":104059,"corporation":false,"usgs":true,"family":"Andrews","given":"Sarah","email":"","affiliations":[],"preferred":false,"id":154450,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":41988,"text":"ofr82549 - 1982 - Aeromagnetic map of Mt. Jefferson and vicinity, Oregon","interactions":[],"lastModifiedDate":"2012-02-02T00:05:02","indexId":"ofr82549","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":"82-549","title":"Aeromagnetic map of Mt. Jefferson and vicinity, Oregon","language":"ENGLISH","doi":"10.3133/ofr82549","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1982, Aeromagnetic map of Mt. Jefferson and vicinity, Oregon: U.S. Geological Survey Open-File Report 82-549, 2 maps ;92 x 80 cm. and 48 x 52 cm., https://doi.org/10.3133/ofr82549.","productDescription":"2 maps ;92 x 80 cm. and 48 x 52 cm.","costCenters":[],"links":[{"id":135429,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":79744,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0549/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":79745,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0549/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b00e4b07f02db6981b7","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":530755,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":8118,"text":"ofr82460 - 1982 - Gravity and aeromagnetic modelling of a large gabbroic body near the Border Ranges Fault, southern Alaska","interactions":[],"lastModifiedDate":"2012-02-02T00:06:05","indexId":"ofr82460","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":"82-460","title":"Gravity and aeromagnetic modelling of a large gabbroic body near the Border Ranges Fault, southern Alaska","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82460","usgsCitation":"Burns, L., 1982, Gravity and aeromagnetic modelling of a large gabbroic body near the Border Ranges Fault, southern Alaska: U.S. Geological Survey Open-File Report 82-460, v, 72 p., 3 over-size sheets, ill., maps ;28 cm., https://doi.org/10.3133/ofr82460.","productDescription":"v, 72 p., 3 over-size sheets, ill., maps ;28 cm.","costCenters":[],"links":[{"id":140667,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0460/report-thumb.jpg"},{"id":35722,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0460/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":35723,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0460/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":35724,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0460/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":35725,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0460/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b12e4b07f02db6a282f","contributors":{"authors":[{"text":"Burns, L.E.","contributorId":80676,"corporation":false,"usgs":true,"family":"Burns","given":"L.E.","email":"","affiliations":[],"preferred":false,"id":157179,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":41991,"text":"ofr82659 - 1982 - Aeromagnetic map of Mt. St. Helens, Washington: Post May 1980 eruption","interactions":[],"lastModifiedDate":"2022-12-15T19:46:21.499999","indexId":"ofr82659","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":"82-659","title":"Aeromagnetic map of Mt. St. Helens, Washington: Post May 1980 eruption","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr82659","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1982, Aeromagnetic map of Mt. St. Helens, Washington: Post May 1980 eruption: U.S. Geological Survey Open-File Report 82-659, 1 Plate: 22.72 × 21.50 inches, https://doi.org/10.3133/ofr82659.","productDescription":"1 Plate: 22.72 × 21.50 inches","costCenters":[],"links":[{"id":135432,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":410561,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_13792.htm","linkFileType":{"id":5,"text":"html"}},{"id":79748,"rank":1,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0659/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Washington","otherGeospatial":"Mount St. Helens","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -122.29316236532115,\n              46.291342447934596\n            ],\n            [\n              -122.29316236532115,\n              46.12071757509011\n            ],\n            [\n              -122.0997944598669,\n              46.12071757509011\n            ],\n            [\n              -122.0997944598669,\n              46.291342447934596\n            ],\n            [\n              -122.29316236532115,\n              46.291342447934596\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b00e4b07f02db6983f3","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":530757,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":29979,"text":"wri8229 - 1982 - Water type and suitability of Oklahoma surface waters for public supply and irrigation, Part 5: Washita river basin through 1979","interactions":[],"lastModifiedDate":"2020-11-05T22:12:00.292527","indexId":"wri8229","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":"82-29","title":"Water type and suitability of Oklahoma surface waters for public supply and irrigation, Part 5: Washita river basin through 1979","docAbstract":"<p><span>Water-quality data through 1979 in the Washita River basin within </span><span>Oklahoma were examined for water type and suitability for public water </span><span>supply and for irrigation use. Of 82 stations with available data, 32 </span><span>stations or 39 percent were considered to have sufficient data for </span><span>analysis. The classification of water type was based on the relation of </span><span>the major ions: calcium, magnesium, sodium, carbonate, bicarbonate, </span><span>sulfate, and chloride to each other within the range of measured specific </span><span>conductance. The suitability for use as a public supply was based on </span><span>the concentration distribution of selected constituents. The constitu</span><span>ents selected were those with maximum contaminant levels established by </span><span>regulation, or constituents for which recommended maximum limits have </span><span>been established and for which historic data are available. The irriga</span><span>tion classification method of Wilcox </span><span>was </span><span>used to relate sodium, calcium, </span><span>and magnesium concentrations and the salinity distribution to the suita</span><span>bility for use of the water for irrigation. Where data were available, </span><span>the chance of phytotoxic effects by boron was discussed. </span></p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri8229","collaboration":"Prepared in cooperation with the Oklahoma Water Resources Board","usgsCitation":"Stoner, J.D., 1982, Water type and suitability of Oklahoma surface waters for public supply and irrigation, Part 5: Washita river basin through 1979: U.S. Geological Survey Water-Resources Investigations Report 82-29, v, 150 p., https://doi.org/10.3133/wri8229.","productDescription":"v, 150 p.","costCenters":[],"links":[{"id":380233,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1982/0029/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":160035,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1982/0029/report-thumb.jpg"}],"country":"United States","state":"Oklahoma","otherGeospatial":"Washita River basin","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -100,\n              33.669496972795535\n            ],\n            [\n              -96,\n              33.669496972795535\n            ],\n            [\n              -96,\n              36\n            ],\n            [\n              -100,\n              36\n            ],\n            [\n              -100,\n              33.669496972795535\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f4e4b07f02db5f0059","contributors":{"authors":[{"text":"Stoner, Jerry D.","contributorId":38611,"corporation":false,"usgs":true,"family":"Stoner","given":"Jerry","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":202471,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":8143,"text":"ofr82416 - 1982 - Uranium and other element geochemical covariation in a granitic host rock and in the derived sediment, Deep Creek Range, Juab County, Utah","interactions":[],"lastModifiedDate":"2012-02-02T00:06:13","indexId":"ofr82416","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":"82-416","title":"Uranium and other element geochemical covariation in a granitic host rock and in the derived sediment, Deep Creek Range, Juab County, Utah","docAbstract":"Correlation and factor analysis of geochemical data from a Tertiary biotite quartz monzonite, the Ibapah stock, and from derived sediment shows on comparison a major shift in element covariation among uranium and 24 other elements. Samples used were collected for a 1978 study in the central part of the Deep Creek Range, Juab County, Utah. \r\n\r\nComputed correlations among elements in granitic igneous rock samples suggest a high degree of covariation among elements that compose the rock. Uranium, however, shows significant correlation with only 12 elements and almost zero correlation with thorium. Computed correlations among elements in the derived sediment suggest that major decreases have occurred in covariation of the elements in the derived sands. Uranium in the sands, however, shows 15 significant correlations compared to 12 in the igneous rock samples, and shows an extremely high correlation with thorium. Factor analysis shows three geochemical petrogenic factors and the regional Be-U mineralization factor in the igneous rocks, and two mechanical segregation and one chemical precipitation factors in the sediments.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82416","usgsCitation":"Cadigan, R.A., 1982, Uranium and other element geochemical covariation in a granitic host rock and in the derived sediment, Deep Creek Range, Juab County, Utah: U.S. Geological Survey Open-File Report 82-416, 24 p. :ill., map ;28 cm., https://doi.org/10.3133/ofr82416.","productDescription":"24 p. :ill., map ;28 cm.","costCenters":[],"links":[{"id":142293,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0416/report-thumb.jpg"},{"id":35746,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0416/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a19e4b07f02db605d74","contributors":{"authors":[{"text":"Cadigan, R. A.","contributorId":57844,"corporation":false,"usgs":true,"family":"Cadigan","given":"R.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":157221,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":42106,"text":"ofr82449 - 1982 - Altitude and configuration of the water table in the High Plains Aquifer in Kansas, 1965","interactions":[],"lastModifiedDate":"2012-02-02T00:11:11","indexId":"ofr82449","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":"82-449","title":"Altitude and configuration of the water table in the High Plains Aquifer in Kansas, 1965","docAbstract":"The High Plains aquifer in Kansas is a part of a regional system that extends South Dakota to Texas. The aquifer in Kansas underlies an area of 31,000 square miles in the western and south-central part. This aquifer is a hydraulically connected assemblage of unconsolidated water-bearing deposits of Tertiary and Quaternary age. Maps published at a scale of 1:500,000 show the altitude and configuration of the water table in Kansas during 1965. Groundwater moved from higher altitudes in the western part of the High Plains to lower altitudes in the eastern part at a average rate of 10 ft/mi. The upgradient flexure of water table contours along some of the valleys indicates that groundwater was discharged to the streams in those areas. (USGS)","language":"ENGLISH","doi":"10.3133/ofr82449","usgsCitation":"Pabst, M.E., and Stullken, L.E., 1982, Altitude and configuration of the water table in the High Plains Aquifer in Kansas, 1965: U.S. Geological Survey Open-File Report 82-449, 1 map :photocopy ;66 x 87 cm., on sheet 85 x 113 cm., folded in envelope 31 x 23 cm., https://doi.org/10.3133/ofr82449.","productDescription":"1 map :photocopy ;66 x 87 cm., on sheet 85 x 113 cm., folded in envelope 31 x 23 cm.","costCenters":[],"links":[{"id":176702,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":20565,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0449/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adde4b07f02db686aec","contributors":{"authors":[{"text":"Pabst, Marilyn E.","contributorId":25566,"corporation":false,"usgs":true,"family":"Pabst","given":"Marilyn","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":225948,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Stullken, Lloyd E.","contributorId":60609,"corporation":false,"usgs":true,"family":"Stullken","given":"Lloyd","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":225949,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":39114,"text":"pp306F - 1982 - Geology and paleontology of Canal Zone and adjoining parts of Panama : description of Tertiary mollusks (pelecypods: Propeamussiidae to Cuspidariidae; additions to families covered in P 306-E; additions to gastropods; cephalopods)","interactions":[],"lastModifiedDate":"2012-02-02T00:10:18","indexId":"pp306F","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"306","chapter":"F","title":"Geology and paleontology of Canal Zone and adjoining parts of Panama : description of Tertiary mollusks (pelecypods: Propeamussiidae to Cuspidariidae; additions to families covered in P 306-E; additions to gastropods; cephalopods)","language":"ENGLISH","doi":"10.3133/pp306F","usgsCitation":"Woodring, W.P., 1982, Geology and paleontology of Canal Zone and adjoining parts of Panama : description of Tertiary mollusks (pelecypods: Propeamussiidae to Cuspidariidae; additions to families covered in P 306-E; additions to gastropods; cephalopods): U.S. Geological Survey Professional Paper 306, iv, 541-759 p., [42] leaves of plates : ill., col. map ; 30 cm. , https://doi.org/10.3133/pp306F.","productDescription":"iv, 541-759 p., [42] leaves of plates : ill., col. map ; 30 cm. ","costCenters":[],"links":[{"id":122153,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0306f/report-thumb.jpg"},{"id":66573,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0306f/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":66574,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0306f/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad7e4b07f02db68438e","contributors":{"authors":[{"text":"Woodring, Wendell Phillips","contributorId":10672,"corporation":false,"usgs":true,"family":"Woodring","given":"Wendell","email":"","middleInitial":"Phillips","affiliations":[],"preferred":false,"id":220981,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":46904,"text":"ofr8281 - 1982 - Geohydrology of the valley-fill aquifer in the Sprout and Fishkill creeks area, Dutchess County, New York","interactions":[],"lastModifiedDate":"2012-02-02T00:10:41","indexId":"ofr8281","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":"82-81","title":"Geohydrology of the valley-fill aquifer in the Sprout and Fishkill creeks area, Dutchess County, New York","docAbstract":"This report is the fifth in a series of 11 map sets depicting geohydrologic conditions in selected aquifers in upstate New York. Geohydrologic data are compiled on six maps at 1:24,000 scale. Together the maps provide a comprehensive overview of a major valley-fill aquifer in southwestern Dutchess County and a small part of Putnan County. The maps include surficial geology, geologic sections, water-infiltration potential of soil zone, aquifer thickness, water-table elevations and land use. The valley-fill deposits consist of alluvial silt and sand, glacial-outwash (sand and gravel), ice-contact sand and gravel, till, and lacustrine silt and clay. The sand and gravel have relatively high permeabilities whereas the till, silt and clay deposits have relatively low permeabilities. Saturated layers of sand and gravel underlie confining layers of silt and clay, and also underlie confining till. The water-infiltration potential of the soil zone of the valley-fill varies widely. Aquifer thickness data is sparse, especially data on the lower confined aquifer layers. Water-table elevations within the surface aquifer are gently sloping, directing ground-water flow towards streams into which discharge occurs. The use of land overlying the aquifer is predominantly agricultural and residential, with lesser amounts of commercial and industrial uses. (USGS)","language":"ENGLISH","doi":"10.3133/ofr8281","usgsCitation":"Moore, R.B., LaFleur, R., Stelz, W., and Belli, J.L., 1982, Geohydrology of the valley-fill aquifer in the Sprout and Fishkill creeks area, Dutchess County, New York: U.S. Geological Survey Open-File Report 82-81, 5 maps ;120 x 75 cm. on sheets 101 x 77 cm. +4 cross sections on sheet 101 x 77 cm. folded in envelope 31 x 23 cm., https://doi.org/10.3133/ofr8281.","productDescription":"5 maps ;120 x 75 cm. on sheets 101 x 77 cm. +4 cross sections on sheet 101 x 77 cm. folded in envelope 31 x 23 cm.","costCenters":[],"links":[{"id":170932,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":83827,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0081/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":83828,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0081/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":83829,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0081/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":83830,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0081/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":83831,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0081/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":83832,"rank":405,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0081/plate-6.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1ae4b07f02db6a8773","contributors":{"authors":[{"text":"Moore, Richard B. rmoore@usgs.gov","contributorId":1464,"corporation":false,"usgs":true,"family":"Moore","given":"Richard","email":"rmoore@usgs.gov","middleInitial":"B.","affiliations":[{"id":405,"text":"NH/VT office of New England Water Science Center","active":true,"usgs":true}],"preferred":true,"id":234302,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"LaFleur, R.G.","contributorId":29869,"corporation":false,"usgs":true,"family":"LaFleur","given":"R.G.","email":"","affiliations":[],"preferred":false,"id":234303,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Stelz, W. G.","contributorId":72837,"corporation":false,"usgs":true,"family":"Stelz","given":"W. G.","affiliations":[],"preferred":false,"id":234304,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Belli, J. L.","contributorId":83561,"corporation":false,"usgs":true,"family":"Belli","given":"J.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":234305,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":4156,"text":"cir855 - 1982 - The Alaska Mineral Resource Assessment Program: Guide to information about the geology and mineral resources of the Ketchikan and Prince Rupert quadrangles, southeastern Alaska","interactions":[],"lastModifiedDate":"2021-11-18T20:54:59.200928","indexId":"cir855","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":307,"text":"Circular","code":"CIR","onlineIssn":"2330-5703","printIssn":"1067-084X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"855","title":"The Alaska Mineral Resource Assessment Program: Guide to information about the geology and mineral resources of the Ketchikan and Prince Rupert quadrangles, southeastern Alaska","docAbstract":"The Ketchikan and Prince Rupert 1-degree by 2-degree quadrangles, which encompass about 16,000 km2 at the south tip of southeastern Alaska, have been investigated by integrated field and laboratory studies in the disciplines of geology, geochemistry, geophysics, and Landsat data interpretation to determine their mineral-resource potential. Mineral deposits in the study area have been mined or prospected intermittently since about 1900, and production of small tonnages of ores containing gold, silver, copper, lead, zinc, and tungsten has been recorded. Extensive exploration and development currently (1981) is underway at a molybdenum prospect about 65 km east of Ketchikan. Our mineral-resource assessment indicates that the area contains potentially significant amounts of those metallic commodities, as well as of molybdenum, iron, antimony, and barite. The results of these studies have been published in a folio of maps accompanied by descriptive texts, diagrams, tables, and pertinent references. The present report serves as a guide to these investigations, provides relevant background information, and integrates the component maps and reports. It also describes revisions to the geology based on studies completed since the folio was published and includes a list of specific and general references on the geology and mineral deposits of the study area.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/cir855","usgsCitation":"Berg, H., 1982, The Alaska Mineral Resource Assessment Program: Guide to information about the geology and mineral resources of the Ketchikan and Prince Rupert quadrangles, southeastern Alaska: U.S. Geological Survey Circular 855, iii, 24 p., https://doi.org/10.3133/cir855.","productDescription":"iii, 24 p.","costCenters":[],"links":[{"id":391884,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_23951.htm"},{"id":139234,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1982/0855/report-thumb.jpg"},{"id":31265,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1982/0855/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Alaska","otherGeospatial":"Ketchikan and Prince Rupert quadrangles","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -132,\n              54.717\n            ],\n            [\n              -130,\n              54.717\n            ],\n            [\n              -130,\n              56\n            ],\n            [\n              -132,\n              56\n            ],\n            [\n              -132,\n              54.717\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad5e4b07f02db6835c1","contributors":{"authors":[{"text":"Berg, Henry C.","contributorId":73176,"corporation":false,"usgs":true,"family":"Berg","given":"Henry C.","affiliations":[],"preferred":false,"id":148308,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
]}