{"pageNumber":"2190","pageRowStart":"54725","pageSize":"25","recordCount":68892,"records":[{"id":23153,"text":"ofr80642 - 1980 - Leasable mineral and waterpower land classification map of the Weed 1° x 2° quadrangle, California and Oregon","interactions":[],"lastModifiedDate":"2021-09-20T19:03:57.878283","indexId":"ofr80642","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","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":"80-642","title":"Leasable mineral and waterpower land classification map of the Weed 1° x 2° quadrangle, California and Oregon","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr80642","issn":"0094-9140","usgsCitation":"Throckmorton, M.L., Villalobos, H.A., and Yamamoto, G.S., 1980, Leasable mineral and waterpower land classification map of the Weed 1° x 2° quadrangle, California and Oregon: U.S. Geological Survey Open-File Report 80-642, 1 Plate: \t36.86 × 23.01 inches, https://doi.org/10.3133/ofr80642.","productDescription":"1 Plate: \t36.86 × 23.01 inches","costCenters":[],"links":[{"id":155997,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":389493,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_11722.htm"},{"id":52498,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/0642/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"California, Oregon","otherGeospatial":"Weed 1° x 2° quadrangle","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -124.0,\n              41.0\n            ],\n            [\n              -122,\n              41.0\n            ],\n            [\n              -122,\n              42.0\n            ],\n            [\n              -124.0,\n              42.0\n            ],\n            [\n              -124.0,\n              41.0\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1ae4b07f02db6a805d","contributors":{"authors":[{"text":"Throckmorton, Michael L.","contributorId":102492,"corporation":false,"usgs":true,"family":"Throckmorton","given":"Michael","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":189534,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Villalobos, H. A.","contributorId":8133,"corporation":false,"usgs":true,"family":"Villalobos","given":"H.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":189532,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Yamamoto, George S.","contributorId":82735,"corporation":false,"usgs":true,"family":"Yamamoto","given":"George","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":189533,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":24724,"text":"ofr801051 - 1980 - Geochemical results from a natural waters study in the Mount Belknap Caldera and vicinity, Utah","interactions":[],"lastModifiedDate":"2012-02-02T00:08:22","indexId":"ofr801051","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","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":"80-1051","title":"Geochemical results from a natural waters study in the Mount Belknap Caldera and vicinity, Utah","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr801051","issn":"0094-9140","usgsCitation":"Tucker, R.E., Miller, W.R., and McHugh, J., 1980, Geochemical results from a natural waters study in the Mount Belknap Caldera and vicinity, Utah: U.S. Geological Survey Open-File Report 80-1051, iii, 57 p. ill., maps ;28 cm., https://doi.org/10.3133/ofr801051.","productDescription":"iii, 57 p. ill., maps ;28 cm.","costCenters":[],"links":[{"id":157767,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1980/1051/report-thumb.jpg"},{"id":53750,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1980/1051/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b23e4b07f02db6ade60","contributors":{"authors":[{"text":"Tucker, Robert E.","contributorId":39360,"corporation":false,"usgs":true,"family":"Tucker","given":"Robert","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":192441,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Miller, William R.","contributorId":53838,"corporation":false,"usgs":true,"family":"Miller","given":"William","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":192442,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"McHugh, John B.","contributorId":64651,"corporation":false,"usgs":true,"family":"McHugh","given":"John B.","affiliations":[],"preferred":false,"id":192443,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":56851,"text":"wdrMS781 - 1980 - Water resources data for Mississippi, water year 1978","interactions":[],"lastModifiedDate":"2025-08-28T14:19:52.243104","indexId":"wdrMS781","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","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":"MS-78-1","title":"Water resources data for Mississippi, water year 1978","docAbstract":"<p> Water resources data for the 1978 water year for Mississippi consist of record of stage and discharge, and water quality of streams; stage, contents, and water quality of lakes and reservoirs; and water levels of wells. This report contains discharge records for 82 gaging stations; stage records for 15 of these gaging stations; stage only for 3 gaging stations; contents for 4 lakes; water quality for 25 gaging stations, and 164 wells; and water levels for 175 observation wells. Also included are data for 92 crest-stage 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 Mississippi. </p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wdrMS781","collaboration":"Prepared in cooperation with the Mississippi Board of Water Commissioners and with other State, county, municipal, and Federal agencies","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1980, Water resources data for Mississippi, water year 1978: U.S. Geological Survey Water Data Report MS-78-1, vii, 507 p., https://doi.org/10.3133/wdrMS781.","productDescription":"vii, 507 p.","costCenters":[],"links":[{"id":494994,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/1978/ms-78-1/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":181744,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wdr/1978/ms-78-1/report-thumb.jpg"}],"country":"United 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,{"id":3440,"text":"cir850A - 1980 - Mount St. Helens volcanic-ash fall in the Bull Run watershed, Oregon, March-June 1980","interactions":[{"subject":{"id":15971,"text":"ofr80593 - 1980 - Mount St. Helens ash fall in the Bull Run watershed, Oregon, May-June 1980","indexId":"ofr80593","publicationYear":"1980","noYear":false,"title":"Mount St. Helens ash fall in the Bull Run watershed, Oregon, May-June 1980"},"predicate":"SUPERSEDED_BY","object":{"id":3440,"text":"cir850A - 1980 - Mount St. Helens volcanic-ash fall in the Bull Run watershed, Oregon, March-June 1980","indexId":"cir850A","publicationYear":"1980","noYear":false,"chapter":"A","title":"Mount St. Helens volcanic-ash fall in the Bull Run watershed, Oregon, March-June 1980"},"id":1},{"subject":{"id":48517,"text":"ofr80740 - 1980 - Mount St. Helens ash fall in the Bull Run watershed, Oregon, March-April 1980","indexId":"ofr80740","publicationYear":"1980","noYear":false,"title":"Mount St. Helens ash fall in the Bull Run watershed, Oregon, March-April 1980"},"predicate":"SUPERSEDED_BY","object":{"id":3440,"text":"cir850A - 1980 - Mount St. Helens volcanic-ash fall in the Bull Run watershed, Oregon, March-June 1980","indexId":"cir850A","publicationYear":"1980","noYear":false,"chapter":"A","title":"Mount St. Helens volcanic-ash fall in the Bull Run watershed, Oregon, March-June 1980"},"id":2}],"lastModifiedDate":"2024-06-12T22:08:15.284657","indexId":"cir850A","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","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":"850","chapter":"A","title":"Mount St. Helens volcanic-ash fall in the Bull Run watershed, Oregon, March-June 1980","docAbstract":"During several periods of volcanic-ash eruption at Mount St. Helens, Wash., (March 30, May 25-26, May 30-June 2, and June 12-13, 1980) strong winds from the north occurred at high altitudes. As a result, the volcanic ash fell some 50 miles to the south in the Bull Run watershed, the principal water-supply source for the metropolitan area of Portland, Oreg. Water samples collected from three stream sites within the watershed were compared with samples collected during the same season in previous years. No detectable changes were noted in chemical characteristics. Precipitation samples collected immediately after the June 12-13 ash fall ranged in specific conductance from 20 to 41 micromhos per centimeter at 25C and in pH from 4.0 to 4.3 pH units. Stream samples collected during the May-June period ranged in specific conductance from 18 to 28 micromhos per centimeter at 25C and in pH from 6.7 to 7.5 pH units. Volcanic-ash samples were collected and analyzed for particle size, chemical composition, and weight. Significant differences in particle size of ash were found in samples from two separate eruptions. 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,{"id":4927,"text":"pp1129AI - 1980 - Shorter contributions to geochemistry 1979","interactions":[],"lastModifiedDate":"2022-07-08T20:10:04.694013","indexId":"pp1129AI","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","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":"1129","chapter":"A-I","title":"Shorter contributions to geochemistry 1979","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/pp1129AI","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1980, Shorter contributions to geochemistry 1979: U.S. Geological Survey Professional Paper 1129, 110 p., https://doi.org/10.3133/pp1129AI.","productDescription":"110 p.","costCenters":[],"links":[{"id":31786,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/1129a-i/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":403303,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_4729.htm","linkFileType":{"id":5,"text":"html"}},{"id":117061,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/1129a-i/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49fae4b07f02db5f3e88","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":528394,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":4385,"text":"cir818A - 1980 - Seismic engineering program report, January-April 1979","interactions":[],"lastModifiedDate":"2012-02-02T00:05:27","indexId":"cir818A","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","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":"818","chapter":"A","title":"Seismic engineering program report, January-April 1979","language":"ENGLISH","publisher":"U.S. Dept. of the Interior, Geological Survey ;\r\navailable through the Branch of Distribution, U.S. Geological Survey,","doi":"10.3133/cir818A","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1980, Seismic engineering program report, January-April 1979: U.S. Geological Survey Circular 818, v, 20 p. :ill., maps ;26 cm., https://doi.org/10.3133/cir818A.","productDescription":"v, 20 p. :ill., maps ;26 cm.","costCenters":[],"links":[{"id":117341,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1980/0818a/report-thumb.jpg"},{"id":31494,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1980/0818a/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ae4b07f02db5fb8ce","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":528203,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":4929,"text":"pp1124AF - 1980 - Shorter contributions to mineralogy and petrology, 1979","interactions":[{"subject":{"id":70230761,"text":"pp1124E - 1980 - Drake Peak — A structurally complex rhyolite center in southeastern Oregon","indexId":"pp1124E","publicationYear":"1980","noYear":false,"chapter":"E","title":"Drake Peak — A structurally complex rhyolite center in southeastern Oregon"},"predicate":"IS_PART_OF","object":{"id":4929,"text":"pp1124AF - 1980 - Shorter contributions to mineralogy and petrology, 1979","indexId":"pp1124AF","publicationYear":"1980","noYear":false,"chapter":"A-F","title":"Shorter contributions to mineralogy and petrology, 1979"},"id":1},{"subject":{"id":70230762,"text":"pp1124A - 1980 - The Vermilion Granitic Complex — A new name for old rocks in northern Minnesota","indexId":"pp1124A","publicationYear":"1980","noYear":false,"chapter":"A","title":"The Vermilion Granitic Complex — A new name for old rocks in northern Minnesota"},"predicate":"IS_PART_OF","object":{"id":4929,"text":"pp1124AF - 1980 - Shorter contributions to mineralogy and petrology, 1979","indexId":"pp1124AF","publicationYear":"1980","noYear":false,"chapter":"A-F","title":"Shorter contributions to mineralogy and petrology, 1979"},"id":2},{"subject":{"id":70230763,"text":"pp1124B - 1980 - Potassium-argon ages from the Mount Taylor Volcanic Field, New Mexico","indexId":"pp1124B","publicationYear":"1980","noYear":false,"chapter":"B","title":"Potassium-argon ages from the Mount Taylor Volcanic Field, New Mexico"},"predicate":"IS_PART_OF","object":{"id":4929,"text":"pp1124AF - 1980 - Shorter contributions to mineralogy and petrology, 1979","indexId":"pp1124AF","publicationYear":"1980","noYear":false,"chapter":"A-F","title":"Shorter contributions to mineralogy and petrology, 1979"},"id":3},{"subject":{"id":70230767,"text":"pp1124D - 1980 - Zeolitization of Tertiary tuffs in lacustrine and alluvial deposits in the Ray-San Manuel area, Final and Gila Counties, Arizona","indexId":"pp1124D","publicationYear":"1980","noYear":false,"chapter":"D","title":"Zeolitization of Tertiary tuffs in lacustrine and alluvial deposits in the Ray-San Manuel area, Final and Gila Counties, Arizona"},"predicate":"IS_PART_OF","object":{"id":4929,"text":"pp1124AF - 1980 - Shorter contributions to mineralogy and petrology, 1979","indexId":"pp1124AF","publicationYear":"1980","noYear":false,"chapter":"A-F","title":"Shorter contributions to mineralogy and petrology, 1979"},"id":4}],"lastModifiedDate":"2024-11-15T16:27:39.201498","indexId":"pp1124AF","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","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":"1124","chapter":"A-F","title":"Shorter contributions to mineralogy and petrology, 1979","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Washington, D.C.","doi":"10.3133/pp1124AF","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1980, Shorter contributions to mineralogy and petrology, 1979: U.S. Geological Survey Professional Paper 1124, 89 p., https://doi.org/10.3133/pp1124AF.","productDescription":"89 p.","costCenters":[],"links":[{"id":117063,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/1124a-f/report-thumb.jpg"},{"id":31788,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/1124a-f/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":464189,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_4726.htm","text":"Potassium-argon ages from the Mount Taylor volcanic field, New Mexico","linkFileType":{"id":5,"text":"html"}},{"id":464190,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_4727.htm","text":"Drake Peak - a structurally complex rhyolite center in southeastern Oregon","linkFileType":{"id":5,"text":"html"}},{"id":464191,"rank":5,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_93005.htm","text":"Zeolitization of Tertiary tuffs in lacustrine and alluvial deposits in the Ray-San Manuel area, Pinal and Gila Counties, Arizona","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac8e4b07f02db67bfe2","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":528395,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":7459,"text":"ofr80157 - 1980 - Procedures for quality assurance of polyethylene bottles and nitric acid ampoules for trace metal analyses of water quality samples","interactions":[],"lastModifiedDate":"2012-02-02T00:06:13","indexId":"ofr80157","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","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":"80-157","title":"Procedures for quality assurance of polyethylene bottles and nitric acid ampoules for trace metal analyses of water quality samples","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr80157","usgsCitation":"Friedman, L., King, F.E., Miller, H.J., and Schroder, L., 1980, Procedures for quality assurance of polyethylene bottles and nitric acid ampoules for trace metal analyses of water quality samples: U.S. Geological Survey Open-File Report 80-157, iii, 22 p. ill. ;28 cm., https://doi.org/10.3133/ofr80157.","productDescription":"iii, 22 p. ill. ;28 cm.","costCenters":[],"links":[{"id":142094,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1980/0157/report-thumb.jpg"},{"id":34878,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1980/0157/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9ee4b07f02db66098e","contributors":{"authors":[{"text":"Friedman, Linda C.","contributorId":98702,"corporation":false,"usgs":true,"family":"Friedman","given":"Linda C.","affiliations":[],"preferred":false,"id":155713,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"King, Fred E.","contributorId":32168,"corporation":false,"usgs":true,"family":"King","given":"Fred","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":155711,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Miller, Hanford J.","contributorId":67887,"corporation":false,"usgs":true,"family":"Miller","given":"Hanford","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":155712,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Schroder, LeRoy J.","contributorId":8454,"corporation":false,"usgs":true,"family":"Schroder","given":"LeRoy J.","affiliations":[],"preferred":false,"id":155710,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":6101,"text":"pp1085 - 1980 - Leachate plumes in ground water from Babylon and Islip landfills, Long Island, New York","interactions":[{"subject":{"id":9807,"text":"ofr77583 - 1977 - Leachate plumes in ground water from Babylon and Islip landfills, Long Island, New York","indexId":"ofr77583","publicationYear":"1977","noYear":false,"title":"Leachate plumes in ground water from Babylon and Islip landfills, Long Island, New York"},"predicate":"SUPERSEDED_BY","object":{"id":6101,"text":"pp1085 - 1980 - Leachate plumes in ground water from Babylon and Islip landfills, Long Island, New York","indexId":"pp1085","publicationYear":"1980","noYear":false,"title":"Leachate plumes in ground water from Babylon and Islip landfills, Long Island, New York"},"id":1}],"lastModifiedDate":"2012-02-02T00:06:01","indexId":"pp1085","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","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":"1085","title":"Leachate plumes in ground water from Babylon and Islip landfills, Long Island, New York","docAbstract":"Landfills operated by the towns of Babylon and Islip in southwest and central Suffolk County, N.Y., contain urban refuse incinerated garbage, and scavenger (cesspool) waste; some industrial refuse is deposited at the Babylon site. The Islip landfill was started in 1933, the Babylon landfill in 1947. The landfills are in contact with and discharge leachate into the highly permeable upper glacial aquifer (hydraulic conductivity 190 and 500 ft/d). The aquifer is 74 feet thick at the Babylon landfill and 170 feet thick at the Islip landfill. The leachate-enriched water occupies the boundaries retard downward migration of the plumes to deeper aquifers. The Babylon plume is 1,900 feet wide at the landfill and narrows to about 700 feet near its terminus 10,000 feet from the landfill. The Islip plume is 5,000 feet from the landfill. Hydrochemical maps and sections show the distribution of the major chemical constituents of the plumes. The most highly leachate-enriched ground water obtained was from the Babylon site; it contained 860 mg/L sodium, 110 mg/L potassium, 565 mg/L calcium, 100 mg/L magnesium, 2,7000 mg/L bicarbonate, and 1,300 mg/L chloride. Simulation of the movement and dispersion of the Babylon plume with a mathematical dispersion model indicated the coefficient of the longitudinal dispersion to be about 60 feet squared per day and the ground-water velocity to be 1 ft/d. However, the velocity determined from the hydraulic gradient and public-supply wells in the area was 4 ft/d, which would cause a plume four times as long as that predicted by the model. (Kosco-USGS)","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/pp1085","usgsCitation":"Kimmel, G.E., and Braids, O.C., 1980, Leachate plumes in ground water from Babylon and Islip landfills, Long Island, New York: U.S. Geological Survey Professional Paper 1085, 38 p.;  3 plates in pocket, https://doi.org/10.3133/pp1085.","productDescription":"38 p.;  3 plates in pocket","costCenters":[],"links":[{"id":125039,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/1085/report-thumb.jpg"},{"id":33145,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1085/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":33146,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1085/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":33147,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1085/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":33148,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/1085/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b32e4b07f02db6b4921","contributors":{"authors":[{"text":"Kimmel, Grant E.","contributorId":20741,"corporation":false,"usgs":true,"family":"Kimmel","given":"Grant","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":152113,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Braids, Olin C.","contributorId":84368,"corporation":false,"usgs":true,"family":"Braids","given":"Olin","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":152114,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":7057,"text":"ofr80267 - 1980 - Coal drilling during 1978 in Big Horn, Daniels, Dawson, Musselshell, Richland, Roosevelt, Rosebud, Valley, and Yellowstone counties, Montana","interactions":[],"lastModifiedDate":"2012-02-02T00:06:05","indexId":"ofr80267","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","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":"80-267","title":"Coal drilling during 1978 in Big Horn, Daniels, Dawson, Musselshell, Richland, Roosevelt, Rosebud, Valley, and Yellowstone counties, Montana","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr80267","usgsCitation":"Montana Bureau of Mines and Geology, and Water Resources Division, U.S. Geological Survey, 1980, Coal drilling during 1978 in Big Horn, Daniels, Dawson, Musselshell, Richland, Roosevelt, Rosebud, Valley, and Yellowstone counties, Montana: U.S. Geological Survey Open-File Report 80-267, 273 p.  :maps ;28 cm., https://doi.org/10.3133/ofr80267.","productDescription":"273 p.  :maps ;28 cm.","costCenters":[],"links":[{"id":140588,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1980/0267/report-thumb.jpg"},{"id":34353,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1980/0267/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49d6e4b07f02db5ddfad","contributors":{"authors":[{"text":"Montana Bureau of Mines and Geology","contributorId":128110,"corporation":true,"usgs":false,"organization":"Montana Bureau of Mines and Geology","id":528811,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":528810,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":4394,"text":"cir818C - 1980 - Seismic engineering program report, September-December 1979","interactions":[],"lastModifiedDate":"2012-02-02T00:05:27","indexId":"cir818C","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","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":"818","chapter":"C","title":"Seismic engineering program report, September-December 1979","language":"ENGLISH","publisher":"U.S. Dept. of the Interior, Geological Survey ;\r\n[available from] Branch of Distribution, U.S. Geological Survey,","doi":"10.3133/cir818C","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1980, Seismic engineering program report, September-December 1979: U.S. Geological Survey Circular 818, v, 60 p. :ill., map ;26 cm., https://doi.org/10.3133/cir818C.","productDescription":"v, 60 p. :ill., map ;26 cm.","costCenters":[],"links":[{"id":117399,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1980/0818c/report-thumb.jpg"},{"id":31503,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1980/0818c/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ae4b07f02db5fb7e8","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":528212,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":6397,"text":"pp1044G - 1980 - Hydrogeologic appraisal of the Klamath Falls geothermal area, Oregon","interactions":[],"lastModifiedDate":"2025-04-17T16:56:14.803702","indexId":"pp1044G","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","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":"1044","chapter":"G","title":"Hydrogeologic appraisal of the Klamath Falls geothermal area, Oregon","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/pp1044G","usgsCitation":"Sammel, E.A., 1980, Hydrogeologic appraisal of the Klamath Falls geothermal area, Oregon: U.S. Geological Survey Professional Paper 1044, Report: 45 p.; 4 Plates: 16.00 x 22.00 inches, https://doi.org/10.3133/pp1044G.","productDescription":"Report: 45 p.; 4 Plates: 16.00 x 22.00 inches","costCenters":[{"id":518,"text":"Oregon Water Science Center","active":true,"usgs":true}],"links":[{"id":484684,"rank":7,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_4697.htm","linkFileType":{"id":5,"text":"html"}},{"id":33771,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1044g/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":33774,"rank":6,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1044g/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":33773,"rank":5,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1044g/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":33772,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1044g/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":33775,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/1044g/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":117734,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/1044g/report-thumb.jpg"}],"country":"United States","state":"Oregon","otherGeospatial":"Klamath Falls geothermal area","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -122,\n              42.5\n            ],\n            [\n              -122,\n              42\n            ],\n            [\n              -121,\n              42\n            ],\n            [\n              -121,\n              42.5\n            ],\n            [\n              -122,\n              42.5\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a61e4b07f02db635b5e","contributors":{"authors":[{"text":"Sammel, Edward A.","contributorId":78320,"corporation":false,"usgs":true,"family":"Sammel","given":"Edward","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":152648,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":4408,"text":"cir811 - 1980 - Summary of the river-quality assessment of the upper Chattahoochee River basin, Georgia","interactions":[],"lastModifiedDate":"2016-12-02T11:17:09","indexId":"cir811","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","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":"811","title":"Summary of the river-quality assessment of the upper Chattahoochee River basin, Georgia","docAbstract":"The river-quality assessment of the Upper Chattahoochee River Basin included studies of (1) the impact of heat loads on river quality, (2) sediment transport and deposition, (3) magnitude and nature of point and nonpoint discharges, and (4) phytoplankton growth in the river and reservoirs. The combined thermal effects of flow regulation and powerplants effluents resulted in mean daily river temperature downstream of the powerplants about equal to or less than computed natural temperatures. The average annual river temperature in 1976 was 14.0 ? Celsius just upstream of the Atkinson-McDonough thermoelectric powerplants and 16.0 ? Celsius just downstream from the powerplants. During a low-flow period in June 1977 the heat load from the two powerplants caused an increase in river temperatures of about 7 ? Celsius and a subsequent decrease in the dissolved-oxygen concentration of about 0.2 milligrams per liter. During the June low-flow period, point sources contributed 63 percent of the ultimate biochemical oxygen demand and 97 percent of ammonium as nitrogen at the Franklin station. Oxidation of ultimate biochemical demand and ammonium caused dissolved-oxygen concentrations to decrease from about 8.0 milligrams per liter at river mile 299 to about 4.5 milligrams per liter at river mile 271. Dissolved orthophosphate is the nutrient presently limiting phytoplankton growth in the West Point Lake when water temperatures are greater than about 26 ? Celsius.","language":"ENGLISH","publisher":"U.S. Dept. of the Interior, Geological Survey,","doi":"10.3133/cir811","usgsCitation":"Cherry, R., Faye, R., Stamer, J., and Kleckner, R., 1980, Summary of the river-quality assessment of the upper Chattahoochee River basin, Georgia: U.S. Geological Survey Circular 811, v, 47 p. :ill. ;26 cm., https://doi.org/10.3133/cir811.","productDescription":"v, 47 p. :ill. ;26 cm.","costCenters":[{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true}],"links":[{"id":31515,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1980/0811/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":124362,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1980/0811/report-thumb.jpg"}],"country":"United States","state":"Alabama, Georgia","otherGeospatial":" Chattahoochee River basin","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      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34.649025753526985\n            ],\n            [\n              -83.59634399414061,\n              34.65213247511267\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4affe4b07f02db697bf9","contributors":{"authors":[{"text":"Cherry, R.N.","contributorId":20728,"corporation":false,"usgs":true,"family":"Cherry","given":"R.N.","email":"","affiliations":[],"preferred":false,"id":149054,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Faye, R.E.","contributorId":106863,"corporation":false,"usgs":true,"family":"Faye","given":"R.E.","email":"","affiliations":[],"preferred":false,"id":149057,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Stamer, J. K.","contributorId":47753,"corporation":false,"usgs":true,"family":"Stamer","given":"J. K.","affiliations":[],"preferred":false,"id":149055,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Kleckner, R.L.","contributorId":70744,"corporation":false,"usgs":true,"family":"Kleckner","given":"R.L.","email":"","affiliations":[],"preferred":false,"id":149056,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":4424,"text":"cir823A - 1980 - The U.S. Geological Survey in Alaska 1980 programs","interactions":[],"lastModifiedDate":"2017-01-29T13:12:29","indexId":"cir823A","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","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":"823","chapter":"A","title":"The U.S. Geological Survey in Alaska 1980 programs","docAbstract":"This circular describes the 1980 programs of the U.S. Geological Survey in Alaska. A brief description of the Alaskan operations of each major division of the Survey is followed by project descriptions arranged by geographic regions in which the work takes place. The mission of the Geological Survey is to identify the Nation 's land, water, energy, and mineral resources; to classify federally-owned mineral lands and waterpower sites; to resolve the exploration and development of energy and natural resources on Federal and Indian lands; and to explore and appraise the petroleum potential of the National Petroleum Reserve in Alaska. Alaska is at once the largest, the least populated, the least explored, and the least developed State in the Nation. More than half of the Nation 's 600 million acres of Outer Continental Shelf lies off Alaska 's coast. The land area of Alaska contains 375 million acres, 16 percent of the onshore land of the Nation. Its resources of all kinds present an opportunity to demonstrate how the needs of both conservation and development can be met for the benefit of the American people. (USGS)","language":"English","publisher":"Branch of Distribution, U.S. Geological Survey,","doi":"10.3133/cir823A","usgsCitation":"1980, The U.S. Geological Survey in Alaska 1980 programs: U.S. Geological Survey Circular 823, vii, 112 p. :ill., maps ;28 cm., https://doi.org/10.3133/cir823A.","productDescription":"vii, 112 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":122603,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1980/0823a/report-thumb.jpg"},{"id":31528,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1980/0823a/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4abce4b07f02db673194","contributors":{"editors":[{"text":"Reed, Katherine M.","contributorId":20327,"corporation":false,"usgs":true,"family":"Reed","given":"Katherine","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":661509,"contributorType":{"id":2,"text":"Editors"},"rank":1}]}}
,{"id":7911,"text":"ofr80384 - 1980 - Schlumberger soundings in the Fish Springs Flat area, Juab County, Utah","interactions":[],"lastModifiedDate":"2022-10-25T19:42:02.707209","indexId":"ofr80384","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","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":"80-384","title":"Schlumberger soundings in the Fish Springs Flat area, Juab County, Utah","docAbstract":"<p>In 1978 the U. S. Geological Survey made 43 Schlumberger soundings in the Fish Springs Flat area, Juab County, Utah. The purpose of this survey was to delineate water quality and obtain structural information. Fish Springs Flat consists mainly of Quaternery deposits of sand, gravel, clay, and silt. On the west Fish Springs Flat is bordered by the Fish Springs Range which is composed primarily of Paleozoic limestone. With the exception of a short section of metal fence and concrete culverts, disruptive cultural features did not appear to be present.</p><p>The purpose of this report is to release the field data obtained in this survey. In addition the automatic inversion of the sounding curves, computer-generated geoelectric cross sections, and interpreted resistivity maps are also given and briefly described.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr80384","usgsCitation":"Bisdorf, R.J., and Zohdy, A.A., 1980, Schlumberger soundings in the Fish Springs Flat area, Juab County, Utah: U.S. Geological Survey Open-File Report 80-384, 73 p., https://doi.org/10.3133/ofr80384.","productDescription":"73 p.","costCenters":[],"links":[{"id":408712,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1980/0384/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":140689,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1980/0384/report-thumb.jpg"}],"country":"United States","state":"Utah","county":"Juab County","otherGeospatial":"Fish Springs Flat area","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -114.0478,39.3132 ], [ -114.0478,40.0112 ], [ -111.583,40.0112 ], [ -111.583,39.3132 ], [ -114.0478,39.3132 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0de4b07f02db5fd44a","contributors":{"authors":[{"text":"Bisdorf, Robert J.","contributorId":107277,"corporation":false,"usgs":true,"family":"Bisdorf","given":"Robert","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":156821,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Zohdy, Adel A. R.","contributorId":61799,"corporation":false,"usgs":true,"family":"Zohdy","given":"Adel","email":"","middleInitial":"A. R.","affiliations":[],"preferred":false,"id":156820,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":7837,"text":"ofr80349 - 1980 - Preliminary data describing the distribution of fluoride and silica in the water in the Ogallala aquifer on the High Plains of Texas","interactions":[],"lastModifiedDate":"2022-07-25T17:47:02.900491","indexId":"ofr80349","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","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":"80-349","title":"Preliminary data describing the distribution of fluoride and silica in the water in the Ogallala aquifer on the High Plains of Texas","docAbstract":"<p>The Ogallala aquifer of Texas historically has been known for elevated fluoride concentration, with many areas in excess of 4 milligrams per liter. In addition, on a regional scale, silica concentrations are also somewhat elevated, with concentrations averaging in the 40 to 50 milligrams per liter range. This aquifer provides a unique geochemical and epidemiological study area because it is completely contained within the High Plains physiographic province.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr80349","usgsCitation":"Bassett, R., Perkins, S., and Waddell, R.K., 1980, Preliminary data describing the distribution of fluoride and silica in the water in the Ogallala aquifer on the High Plains of Texas: U.S. Geological Survey Open-File Report 80-349, iv, 109 p., https://doi.org/10.3133/ofr80349.","productDescription":"iv, 109 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":404427,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1980/0349/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":140549,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1980/0349/report-thumb.jpg"}],"country":"United States","state":"Texas","otherGeospatial":"Ogallala Aquifer, High Plains","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -103.095703125,\n              31.784216884487385\n            ],\n            [\n              -99.931640625,\n              31.784216884487385\n            ],\n            [\n              -99.931640625,\n              36.50963615733049\n            ],\n            [\n              -103.095703125,\n              36.50963615733049\n            ],\n            [\n              -103.095703125,\n              31.784216884487385\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67c596","contributors":{"authors":[{"text":"Bassett, R.L.","contributorId":13233,"corporation":false,"usgs":true,"family":"Bassett","given":"R.L.","email":"","affiliations":[],"preferred":false,"id":156701,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Perkins, S.G.","contributorId":93483,"corporation":false,"usgs":true,"family":"Perkins","given":"S.G.","email":"","affiliations":[],"preferred":false,"id":156703,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Waddell, R. K.","contributorId":25560,"corporation":false,"usgs":true,"family":"Waddell","given":"R.","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":156702,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":3946,"text":"cir832 - 1980 - Estimating the costs of landslide damage in the United States","interactions":[],"lastModifiedDate":"2017-07-05T11:26:48","indexId":"cir832","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","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":"832","title":"Estimating the costs of landslide damage in the United States","docAbstract":"Landslide damages are one of the most costly natural disasters in the United States. A recent estimate of the total annual cost of landslide damage is in excess of $1 billion {Schuster, 1978}. The damages can be significantly reduced, however, through the combined action of technical experts, government, and the public. \r\n\r\nBefore they can be expected to take action, local governments need to have an appreciation of costs of damage in their areas of responsibility and of the reductions in losses that can be achieved. Where studies of cost of landslide damages have been conducted, it is apparent that {1} costs to the public and private sectors of our economy due to landslide damage are much larger than anticipated; {2} taxpayers and public officials generally are unaware of the magnitude of the cost, owing perhaps to the lack of any centralization of data; and {3} incomplete records and unavailability of records result in lower reported costs than actually were incurred. \r\n\r\nThe U.S. Geological Survey has developed a method to estimate the cost of landslide damages in regional and local areas and has applied the method in three urban areas and one rural area. Costs are for different periods and are unadjusted for inflation; therefore, strict comparisons of data from different years should be avoided. Estimates of the average annual cost of landslide damage for the urban areas studied are $5,900,000 in the San Francisco Bay area; $4,000,000 in Allegheny County, Pa.; and $5,170,000 in Hamilton County, Ohio. Adjusting these figures for the population of each area, the annual cost of damages per capita are $1.30 in the nine-county San Francisco Bay region; $2.50 in Allegheny County, Pa.; and $5.80 in Hamilton County, Ohio. On the basis of data from other sources, the estimated annual damages on a per capita basis for the City of Los Angeles, Calif., are about $1.60. If the costs were available for the damages from landslides in Los Angeles in 1977-78 and 1979-80, the annual per capita costs probably would be much larger. \r\n\r\nThe landslide near the rural community of Manti, Utah, caused an expenditure of about $1,800,000 or about $1,000 per person during the period 1974-76. Because a recurrence for such a landslide cannot be established, it is not possible to develop a meaningful estimate of annual per capita damages. \r\n\r\nCommunities are urged to examine their costs of landslide damage and to evaluate the feasibility of several alternative programs that, for a modest investment, could significantly reduce these losses.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/cir832","usgsCitation":"Fleming, R.W., and Taylor, F.A., 1980, Estimating the costs of landslide damage in the United States: U.S. Geological Survey Circular 832, iii, 21 p. :ill., map ;27 cm., https://doi.org/10.3133/cir832.","productDescription":"iii, 21 p. :ill., map ;27 cm.","costCenters":[{"id":532,"text":"Pennsylvania Water Science Center","active":true,"usgs":true}],"links":[{"id":31031,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1980/0832/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":124694,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1980/0832/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ce4b07f02db5fc80a","contributors":{"authors":[{"text":"Fleming, Robert W.","contributorId":102062,"corporation":false,"usgs":true,"family":"Fleming","given":"Robert","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":147875,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Taylor, Fred A.","contributorId":38142,"corporation":false,"usgs":true,"family":"Taylor","given":"Fred","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":147874,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":5919,"text":"pp1126AJ - 1980 - Shorter contributions to stratigraphy and structural geology, 1979","interactions":[],"lastModifiedDate":"2024-11-18T19:41:27.730858","indexId":"pp1126AJ","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","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":"1126","chapter":"A-J","title":"Shorter contributions to stratigraphy and structural geology, 1979","docAbstract":"PART A: A system of anticlines lies along the trend of the sinuous course of the Colorado River for a distance of 97 km in the central Grand Canyon. Similar anticlines occur in some perennially wet side canyons. The anticlines are most abundant and well developed along northeast-trending reaches of the main canyon where it is floored by the Cambrian Muav Limestone. Dips of the folded strata are as great as 60?, and the folding locally extends more than 250 m from the river. Low-angle thrust faults in the limbs of the anticlines parallel the river and have formed in response to folding of the comparatively brittle carbonate strata. High-angle reverse kink bands, along which rocks are displaced up toward the river, also parallel the anticlines and have develop2d in response to the upward bulging of the canyon floor. \r\n\r\nThe river anticlines are an unloading phenomenon. They result from lateral squeezing toward the river of saturated shaly parts of the Muav Limestone and underlying Bright Angel Shale. The driving mechanism for the deformation is a stress gradient that results from a difference in lithostatic load between the heavily loaded rocks under the 650-m-high canyon walls and the unloaded canyon floor. Saturation appears to weaken the shaly rocks sufficiently to allow deformation to take place. River anticlines are not present in the eastern Grand Canyon, where the Cambrian rocks also occur at river level. Their absence is explained by a lack of shaly rocks that could flow when saturated. \r\n\r\nPART B:  The current interest in contemporary tectonic processes in the Eastern United States is turning up abundant evidence of crustal movements in late geologic time. Topographic analysis of the highland areas from the southern Blue Ridge to the Adirondack Mountains indicates that most of the landforms owe their origin to erosion of rocks of different resistance rather than to tectonic processes. Most areas of high relief and high altitude have been formed on resistant rocks. The Cambrian and Ordovician belt, containing mostly shale and carbonate rock, on the other hand, forms an extensive lowland from Alabama to the Canadian border and girdles the Adirondack Mountains. Differences in altitude can be explained by the presence of resistant rocks outside the belt; these resistant rocks form local base levels on the streams that drain the belt. A few areas may have undergone local uplift at a higher rate than areas nearby--for example, the Piedmont region northwest of Chesapeake Bay. Most estimates of erosion rates, based on the load transported by streams and of uplift rates, based on removal during a known period of time, are of the same order of magnitude, averaging almost 4x 10^-2 millimeters per year. Rates of uplift, based on study of tilted Pleistocene beaches and repeated geodetic traverses, are at least an order of magnitude higher for comparable areas. Tectonic uplift of the highlands has been slow and involves mostly warping or tilting on a large scale. Erosion rates keep up with or exceed the rate of uplift and have been sufficient to mask evidence of faulting or other differential movements. The high rates of uplift that are inferred on tilted water planes in the glaciated regions or that are measured by differences in repeated geodetic traverses cannot have been sustained for long periods of time.\r\n\r\nPART C: The Hanson Creek Formation southwest of Eureka, Nev., in the Bellevue Peak Quadrangle is composed of three lithostratigraphic members: (1) a basal dark-gray dolomite, (2) a middle silty thin- to thick-bedded, locally nodular, dark-gray, light-yellow-mottled limestone topped by light-gray dolomite, and (3) an upper dark-gray dolomite, which is herein named the Combs Canyon Dolomite Member. Detailed geologic mapping and accompanying fossil collecting prove that the same lithostratigraphic and biostratigraphic sequence is present in the Mountain Boy Range and 11 km to the south near Wood Cone Peak. Minor differences in","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/pp1126AJ","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1980, Shorter contributions to stratigraphy and structural geology, 1979: U.S. Geological Survey Professional Paper 1126, 114 p., https://doi.org/10.3133/pp1126AJ.","productDescription":"114 p.","costCenters":[],"links":[{"id":32802,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/1126a-j/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":117533,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/1126a-j/report-thumb.jpg"},{"id":402717,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_74379.htm","text":"The Upper Ordovician and Silurian Hanson Creek Formation of central Nevada","linkFileType":{"id":5,"text":"html"}},{"id":464253,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_74380.htm","text":"The Marble Hill Bed: an offshore bar-tidal channel complex in the Upper Ordovician Drakes Formation of Kentucky","linkFileType":{"id":5,"text":"html"}},{"id":464254,"rank":5,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_74381.htm","text":"Paleogene sedimentary and volcanogenic rocks from Adak Island, central Aleutian Islands, Alaska","linkFileType":{"id":5,"text":"html"}},{"id":464255,"rank":6,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_74382.htm","text":"The Livengood Dome Chert, a new Ordovician Formation in central Alaska, and its relevance to displacement on the Tintina fault","linkFileType":{"id":5,"text":"html"}},{"id":464256,"rank":7,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_74383.htm","text":"New evidence supporting Nebraskan age for origin of Ohio River in north-central Kentucky","linkFileType":{"id":5,"text":"html"}},{"id":464257,"rank":8,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_74384.htm","text":"Intertonguing between the Star Point Sandstone and the coal-bearing Blackhawk Formation requires revision of some coal-bed correlations in the southern Wasatch Plateau, Utah","linkFileType":{"id":5,"text":"html"}},{"id":464258,"rank":9,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_74385.htm","text":"Constraints on the latest movements on the Melones fault zone, Sierra Nevada foothills, California","linkFileType":{"id":5,"text":"html"}},{"id":464259,"rank":10,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_74386.htm","text":"Origin of the river anticlines, central Grand Canyon, Arizona","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49fae4b07f02db5f3e20","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":528707,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":3827,"text":"cir827 - 1980 - The handling, hazards, and maintenance of heavy liquids in the geologic laboratory","interactions":[],"lastModifiedDate":"2012-02-02T00:05:44","indexId":"cir827","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","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":"827","title":"The handling, hazards, and maintenance of heavy liquids in the geologic laboratory","docAbstract":"In geologic laboratories the organic heavy liquids bromoform, methylene iodide, tetrabromoethane, and clerici compounds have been used for years in mineral separation processes. Because the volume of use of these compounds is low, insufficient data is available on their toxic properties. This report is an attempt to summarize the known data from published and industry sources. The physical properties, hazards of handling,proper storage facilities, and adequate protective Clothing are discussed for each compound as well as for their common and less-common solvents. Toxicity data for these materials is listed along with exposure symptoms and suggested first aid treatments. Safety for the worker is emphasized. Three reclamation methods which recover the solvent used as a dilutant and purify the heavy liquid are discussed and illustrated. These include: the water cascade, re fluxing-distillation-condensation, and flash evaporation methods. Various techniques for restoration and stabilization of these heavy liquids are also included.","language":"ENGLISH","publisher":"U.S. Dept. of the Interior, Geological Survey ;\r\nFree on application to Branch of Distribution, U.S. Geological Survey,","doi":"10.3133/cir827","usgsCitation":"Hauff, P.L., and Airey, J., 1980, The handling, hazards, and maintenance of heavy liquids in the geologic laboratory: U.S. Geological Survey Circular 827, iv, 24 p. :10 ill. ;26 cm., https://doi.org/10.3133/cir827.","productDescription":"iv, 24 p. :10 ill. ;26 cm.","costCenters":[],"links":[{"id":118130,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1980/0827/report-thumb.jpg"},{"id":30896,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1980/0827/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a90e4b07f02db655f41","contributors":{"authors":[{"text":"Hauff, Phoebe L.","contributorId":10402,"corporation":false,"usgs":true,"family":"Hauff","given":"Phoebe","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":147684,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Airey, Joseph","contributorId":92105,"corporation":false,"usgs":true,"family":"Airey","given":"Joseph","email":"","affiliations":[],"preferred":false,"id":147685,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":4804,"text":"pp1162B - 1980 - Makah Formation — A deep-marginal-basin sequence of late Eocene and Oligocene age in the northwestern Olympic Peninsula, Washington","interactions":[{"subject":{"id":7300,"text":"ofr79581 - 1979 - Makah Formation--a deep marginal basin sedimentary sequence of Late Eocene and Oligocene age in the northwestern Olympic Peninsula, Washington","indexId":"ofr79581","publicationYear":"1979","noYear":false,"title":"Makah Formation--a deep marginal basin sedimentary sequence of Late Eocene and Oligocene age in the northwestern Olympic Peninsula, Washington"},"predicate":"SUPERSEDED_BY","object":{"id":4804,"text":"pp1162B - 1980 - Makah Formation — A deep-marginal-basin sequence of late Eocene and Oligocene age in the northwestern Olympic Peninsula, Washington","indexId":"pp1162B","publicationYear":"1980","noYear":false,"chapter":"B","title":"Makah Formation — A deep-marginal-basin sequence of late Eocene and Oligocene age in the northwestern Olympic Peninsula, Washington"},"id":1}],"lastModifiedDate":"2022-10-26T21:04:42.123337","indexId":"pp1162B","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","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":"1162","chapter":"B","title":"Makah Formation — A deep-marginal-basin sequence of late Eocene and Oligocene age in the northwestern Olympic Peninsula, Washington","docAbstract":"The Makah Formation of the Twin River Group crops out in a northwest-trending linear belt in the northwesternmost part of the Olympic Peninsula, Wash. This marine sequence consists of 2800 meters of predominantly thin-bedded siltstone and sandstone that encloses six distinctive newly named members--four thick-bedded amalgamated turbidite sandstone members, an olistostromal shallow-water marine sandstone and conglomerate member, and a thin-bedded water-laid tuff member. A local unconformity of submarine origin occurs within the lower part of the Makah Formation except in the central part of the study area, where it forms the contact between the older Hoko River Formation and the Makah. Foraminiferal faunas indicate that the Makah Formation ranges in age from late Eocene (late Narizian) to late Oligocene (Zemorrian) and was deposited in a predominantly lower to middle bathyal environment. \r\n\r\nThe Makah Formation is part of a deep-marginalbasin facies that crops out in the western part of the Olympic Peninsula, in southwesternmost Washington and coastal embayments in northwestern Oregon, and along the central part of the coast of western Vancouver Island. On the basis of limited subsurface data from exploratory wells, correlative deep-marginal-basin deposits underlie the inner continental shelf of Oregon and the continental shelf (Tofino basin) along the southwestern side of Vancouver Island. \r\n\r\nDirectional structures in the Makah Formation indicate that the predominantly lithic arkosic sandstone that forms the turbidite packets was derived from the northwest. A possible source of the clastic material is the dioritic, granitic, and volcanic terranes in the vicinity of the Hesquiat Peninsula and Barkley Sound on the west coast of Vancouver Island. Vertical and lateral variations of turbidite facies suggest that the four packets of sandstone were formed as depositional lobes on an outer submarine fan. The thin-bedded strata between the turbidite packets have characteristics of basin-plain and outer-fan fringe deposits.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/pp1162B","usgsCitation":"Snavely, P.D., Niem, A.R., MacLeod, N.S., Pearl, J.E., and Rau, W.W., 1980, Makah Formation — A deep-marginal-basin sequence of late Eocene and Oligocene age in the northwestern Olympic Peninsula, Washington: U.S. Geological Survey Professional Paper 1162, iii, 28 p., https://doi.org/10.3133/pp1162B.","productDescription":"iii, 28 p.","costCenters":[],"links":[{"id":31765,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/1162b/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":124890,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/1162b/report-thumb.jpg"},{"id":408779,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_74397.htm","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Washington","otherGeospatial":"Olympic Peninsula","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -124.75,\n              48.4083\n            ],\n            [\n              -124.75,\n              48.1903\n            ],\n            [\n              -124.25,\n              48.1903\n            ],\n            [\n              -124.25,\n              48.4083\n            ],\n            [\n              -124.75,\n              48.4083\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a81e4b07f02db649e1b","contributors":{"authors":[{"text":"Snavely, P. D.","contributorId":13971,"corporation":false,"usgs":true,"family":"Snavely","given":"P.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":149795,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Niem, A. R.","contributorId":54984,"corporation":false,"usgs":true,"family":"Niem","given":"A.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":149796,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"MacLeod, N. S.","contributorId":55816,"corporation":false,"usgs":true,"family":"MacLeod","given":"N.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":149797,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Pearl, J. E.","contributorId":89883,"corporation":false,"usgs":true,"family":"Pearl","given":"J.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":149799,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Rau, W. W.","contributorId":71963,"corporation":false,"usgs":true,"family":"Rau","given":"W.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":149798,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":5913,"text":"pp1164 - 1980 - Effects of coal mine subsidence in the Sheridan, Wyoming, area","interactions":[{"subject":{"id":8650,"text":"ofr78473 - 1978 - Effects of coal mine subsidence in the western Powder River basin, Wyoming","indexId":"ofr78473","publicationYear":"1978","noYear":false,"title":"Effects of coal mine subsidence in the western Powder River basin, Wyoming"},"predicate":"SUPERSEDED_BY","object":{"id":5913,"text":"pp1164 - 1980 - Effects of coal mine subsidence in the Sheridan, Wyoming, area","indexId":"pp1164","publicationYear":"1980","noYear":false,"title":"Effects of coal mine subsidence in the Sheridan, Wyoming, area"},"id":1}],"lastModifiedDate":"2012-02-02T00:05:41","indexId":"pp1164","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","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":"1164","title":"Effects of coal mine subsidence in the Sheridan, Wyoming, area","docAbstract":"Analyses of the surface effects of past underground coal mining in the Sheridan, Wyoming, area suggest that underground mining of strippable coal deposits may damage the environment more over long periods of time than would modern surface mining, provided proper restoration procedures are followed after surface mining. Subsidence depressions and pits are a continuing hazard to the environment and to man's activities in the Sheridan, Wyo., area above abandoned underground mines in weak overburden less than about 60 m thick and where the overburden is less than about 10-15 times the thickness of coal mined. In addition, fires commonly start by spontaneous ignition when water and air enter the abandoned mine workings via subsidence cracks and pits. The fires can then spread to unmined coal as they create more cavities, more subsidence, and more cracks and pits through which air can circulate. \r\n\r\nIn modern surface mining operations the total land surface underlain by minable coal is removed to expose the coal. The coal is removed, the overburden and topsoil are replaced, and the land is regraded and revegetated. The land, although disturbed, can be more easily restored and put back into use than can land underlain by abandoned underground mine workings in areas where the overburden is less than about 60 m thick or less than about 10-15 times the thickness of coal mined. The resource recovery of modern surface mining commonly is much greater than that of underground mining procedures. Although present-day underground mining technology is advanced as compared to that of 25-80 years ago, subsidence resulting from underground mining of thick coal beds beneath overburden less than about 60 m thick can still cause greater damage to surface drainage, ground water, and vegetation than can properly designed surface mining operations. \r\n\r\nThis report discusses (11 the geology and surface and underground effects of former large-scale underground coal mining in a 50-km 2 area 5-20 km north of Sheridan, Wyo., (2) a ground and aerial reconnaissance study of a 5-km^2 coal mining area 8-10 km west of Sheridan, and (31 some environmental consequences and problems caused by coal mining.","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/pp1164","usgsCitation":"Dunrud, C., and Osterwald, F.W., 1980, Effects of coal mine subsidence in the Sheridan, Wyoming, area: U.S. Geological Survey Professional Paper 1164, 49 p., https://doi.org/10.3133/pp1164.","productDescription":"49 p.","costCenters":[],"links":[{"id":124834,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/1164/report-thumb.jpg"},{"id":32798,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/1164/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a2fe4b07f02db615ca8","contributors":{"authors":[{"text":"Dunrud, C. Richard","contributorId":48964,"corporation":false,"usgs":true,"family":"Dunrud","given":"C. Richard","affiliations":[],"preferred":false,"id":151800,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Osterwald, Frank W.","contributorId":98301,"corporation":false,"usgs":true,"family":"Osterwald","given":"Frank","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":151801,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":7974,"text":"ofr801300 - 1980 - Digital model simulation of the hydrologic flow system, with emphasis on ground water in Spokane Valley, Washington and Idaho","interactions":[],"lastModifiedDate":"2019-05-10T13:27:52","indexId":"ofr801300","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","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":"80-1300","title":"Digital model simulation of the hydrologic flow system, with emphasis on ground water in Spokane Valley, Washington and Idaho","docAbstract":"<p>A digital-computer model of the hydrologic flow system, with emphasis on ground water, was developed for Spokane Valley, Washington and Idaho. The current rate of ground-water pumping in Spokane Valley has little effect on water levels in the Spokane aquifer, although short-term water-level declines occur locally. The model was used to show the effects of increased ground-water pumpage on aquifer heads and streamflow. A simulated pumping rate twice that of actual 1977 pumping rates of 227 cubic feet per second lowered water levels in the Spokane aquifer less than 3 feet during a 1-year simulation period. This doubling of the ground water pumpage caused a decrease in discharge of the Spokane River, as measured at Spokane, of about 150 cubic feet per second during the summer months and about 50 cubic feet per second during the rest of the year. Leakage from the aquifer to the Little Spokane River was decreased by less than 10 cubic feet per second. </p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr801300","collaboration":"Prepared in cooperation with State of Washington Department of Ecology and Spokane Engineers Office","usgsCitation":"Bolke, E., and Washington, J., 1980, Digital model simulation of the hydrologic flow system, with emphasis on ground water in Spokane Valley, Washington and Idaho (WRI/OFR): U.S. Geological Survey Open-File Report 80-1300, v, 43 p., https://doi.org/10.3133/ofr801300.","productDescription":"v, 43 p.","costCenters":[],"links":[{"id":363671,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1980/1300/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":140319,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1980/1300/report-thumb.jpg"}],"country":"United States","state":"Idaho, Washington","otherGeospatial":"Spokane Valley","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -117.71301269531249,\n              47.544090665057986\n            ],\n            [\n              -116.89590454101562,\n              47.544090665057986\n            ],\n            [\n              -116.89590454101562,\n              47.91173983456231\n            ],\n            [\n              -117.71301269531249,\n              47.91173983456231\n            ],\n            [\n              -117.71301269531249,\n              47.544090665057986\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","edition":"WRI/OFR","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a96e4b07f02db65ab28","contributors":{"authors":[{"text":"Bolke, E.L.","contributorId":52151,"corporation":false,"usgs":true,"family":"Bolke","given":"E.L.","affiliations":[],"preferred":false,"id":156917,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Washington, J.J.","contributorId":93044,"corporation":false,"usgs":true,"family":"Washington","given":"J.J.","email":"","affiliations":[],"preferred":false,"id":156918,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":6240,"text":"pp1109 - 1980 - Geology of the Round Bay quadrangle, Anne Arundel County, Maryland","interactions":[],"lastModifiedDate":"2021-10-13T19:03:45.399259","indexId":"pp1109","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","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":"1109","title":"Geology of the Round Bay quadrangle, Anne Arundel County, Maryland","docAbstract":"Six Coastal Plain formations and one group crop out in the Round Bay quadrangle near the inner edge of the Atlantic Coastal Plain physiographic province. The quadrangle lies astride the Severn River, in Anne Arundel County, near Annapolis, Md. The seven stratigraphic units aggregate as much as 128 m in outcrop. In ascending order, the units are: the upper part of the Potomac Group and the Magothy, Matawan, and Severn Formations, all of Cretaceous age; the Brightseat and Aquia Formations of Paleocene age and the Calvert Formation of Miocene age. \r\n\r\nQuaternary deposits are thin and cover only small areas; they are all mapped under one unit. Several small, thin deposits of Tertiary alluvium are mapped separately. \r\n\r\nThe largely unconsolidated Cretaceous and Tertiary formations consist chiefly of quartz, glauconite, clays, muscovite, chlorite, lignite, feldspar, and pyrite. Quaternary sediments are mostly locally derived sands, silts, and clays with some gravel and, in the finer sediments, considerable amounts of organic matter. \r\n\r\nThe Cretaceous and Tertiary units strike generally northeast; the younger the formation, the more easterly it strikes. Dips are gentle, 3.6 to 15 m per kilometer toward the southeast, and decrease upward through the section. \r\n\r\nThe Round Bay quadrangle is near the southern limit of several formations that thin progressively toward the southwest from New Jersey. Some pinch out between Betterton, on the eastern shore of Chesapeake Bay, and Round Bay, on the western shore, whereas others are present only as thin remnants 1-2 m thick. Resources of the quadrangle include abundant ground water, sand, and high land values near water.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/pp1109","usgsCitation":"Minard, J.P., May, F.E., and Christopher, R.A., 1980, Geology of the Round Bay quadrangle, Anne Arundel County, Maryland: U.S. Geological Survey Professional Paper 1109, Report: iv, 30 p.; 1 Plate: 25.00 × 28.00 inches, https://doi.org/10.3133/pp1109.","productDescription":"Report: iv, 30 p.; 1 Plate: 25.00 × 28.00 inches","costCenters":[],"links":[{"id":126756,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/1109/report-thumb.jpg"},{"id":104552,"rank":700,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_4721.htm","linkFileType":{"id":5,"text":"html"},"description":"4721"},{"id":33453,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/1109/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":33452,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1109/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Maryland","county":"Anne Arundel County","otherGeospatial":"Round Bay quadrangle","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -76.625,\n              39\n            ],\n            [\n              -76.5,\n              39\n            ],\n            [\n              -76.5,\n              39.125\n            ],\n            [\n              -76.625,\n              39.125\n            ],\n            [\n              -76.625,\n              39\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4acce4b07f02db67e5ba","contributors":{"authors":[{"text":"Minard, James Pierson","contributorId":85169,"corporation":false,"usgs":true,"family":"Minard","given":"James","email":"","middleInitial":"Pierson","affiliations":[],"preferred":false,"id":152369,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"May, Fred E.","contributorId":32157,"corporation":false,"usgs":true,"family":"May","given":"Fred","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":152368,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Christopher, Raymond A.","contributorId":29812,"corporation":false,"usgs":true,"family":"Christopher","given":"Raymond","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":152367,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":7232,"text":"ofr801107 - 1980 - Hydrologic evaluation of a hypothetical coal-mining site near Chrisney, Spencer County, Indiana","interactions":[],"lastModifiedDate":"2014-03-25T08:24:42","indexId":"ofr801107","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","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":"80-1107","title":"Hydrologic evaluation of a hypothetical coal-mining site near Chrisney, Spencer County, Indiana","docAbstract":"<p>Protecting the water resources of the Nation is a major emphasis of the \nSurface Mining Control and Reclamation Act, PL 95-87. Permanent regulations \nestablished for this Act by the Office of Surface Mining (OSM) require the \nissuance of a permit before mining begins. An application for a mining permit \nmust include an assessment of the hydrologic characteristics of the mining \nsite and adjacent area, and a projection of the potential impacts of \nmining activities on surface water and ground water.</p>\n<br/>\n<p>OSM's permanent regulations and guidelines provide little insight on the \n\"how to\" aspect of making the required hydrologic assessment. This investigation\nwas completed to improve the understanding of the kinds of information \nneeded to make such assessments by: (a) reviewing the regulations to determine \nwhat hydrologic information is required; (b) preparing an example hydrologic \nassessment based on the regulations; and (c) using the experience \ngained in (a) and (b) to identify areas lacking or needing additional data to \nmake the required assessment.</p>\n<br/>\n<p>Hydrologic data for the study area were obtained from published and unpublished \nreports, maps, aerial photographs, personal interviews with residents \nin the area of the hypothetical mine site, and discussions with experts in \nthe field. Where data were unavailable, \"synthetic\" data were generated by \nextrapolation from proximate or similar watersheds and (or) by assumptions \nbased on experience or theory. Some field data were collected to corroborate \nand augment information originating from all these sources.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Indianapolis, Indiana","doi":"10.3133/ofr801107","usgsCitation":"Zogorski, J.S., Ramey, D.S., Lambert, P.W., Martin, J.D., and Warner, R., 1980, Hydrologic evaluation of a hypothetical coal-mining site near Chrisney, Spencer County, Indiana: U.S. Geological Survey Open-File Report 80-1107, xix, 133 p., https://doi.org/10.3133/ofr801107.","productDescription":"xix, 133 p.","numberOfPages":"154","costCenters":[],"links":[{"id":139941,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1980/1107/report-thumb.jpg"},{"id":284493,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1980/1107/report.pdf"}],"country":"United States","state":"Indiana","county":"Spencer County","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -87.101594,37.988893 ], [ -87.101594,38.100379 ], [ -86.984701,38.100379 ], [ -86.984701,37.988893 ], [ -87.101594,37.988893 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53cd6184e4b0b290850fd962","contributors":{"authors":[{"text":"Zogorski, John S. jszogors@usgs.gov","contributorId":189,"corporation":false,"usgs":true,"family":"Zogorski","given":"John","email":"jszogors@usgs.gov","middleInitial":"S.","affiliations":[],"preferred":true,"id":154848,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ramey, Daniel S.","contributorId":22761,"corporation":false,"usgs":true,"family":"Ramey","given":"Daniel","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":154850,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Lambert, Paul W.","contributorId":61030,"corporation":false,"usgs":true,"family":"Lambert","given":"Paul","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":154851,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Martin, Jeffrey D. 0000-0003-1994-5285 jdmartin@usgs.gov","orcid":"https://orcid.org/0000-0003-1994-5285","contributorId":1066,"corporation":false,"usgs":true,"family":"Martin","given":"Jeffrey","email":"jdmartin@usgs.gov","middleInitial":"D.","affiliations":[{"id":451,"text":"National Water Quality Assessment Program","active":true,"usgs":true},{"id":27231,"text":"Indiana-Kentucky Water Science Center","active":true,"usgs":true},{"id":346,"text":"Indiana Water Science Center","active":true,"usgs":true}],"preferred":true,"id":154849,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Warner, Robert E.","contributorId":61415,"corporation":false,"usgs":true,"family":"Warner","given":"Robert E.","affiliations":[],"preferred":false,"id":154852,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":7548,"text":"ofr82398 - 1980 - Summary of regional geology, petroleum potential, resource assessment and environmental considerations for oil and gas lease sale area #56","interactions":[],"lastModifiedDate":"2022-09-26T19:10:40.19118","indexId":"ofr82398","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","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":"82-398","title":"Summary of regional geology, petroleum potential, resource assessment and environmental considerations for oil and gas lease sale area #56","docAbstract":"<p>This report summarizes our general knowledge of the petroleum potential, as well as problems and hazards associated with development of petroleum resources in the area proposed for nominations for lease sale number 56. This area includes the U.S. eastern continental margin from the North Carolina-Virginia border south to approximately Cape Canaveral, Florida and from three miles from shore, seaward to include the upper Continental Slope and inner Blake Plateau. The area for possible sales is shown in figure 1; major physiographic features of the region are shown in figure 2.</p><p>No wells have been drilled for petroleum within this proposed lease area and no significant commercial production has been obtained onshore in the Southeast Georgia Embayment. The COST GE-1 stratigraphic test well, drilled on the Continental Shelf off Jacksonville, Fla. (fig- 1), reached basement at 3,300 m. The bottom third of the section consists of dominantly continental rocks that are typically poor sources of petroleum (Scholle, 1979) and the rocks that contain organic carbon adequate for generation of petroleum at the well are seen in seismic profiles always at shallow subbottom depths, so they probably have not reached thermal maturity. However, seismic profiles indicate that the sedimentary deposits thicken markedly in a seaward direction where more of the section was deposited under marine conditions; therefore, commercial accumulations of petroleum offshore are more likely.</p><p>Several potential sources of environmental hazard exist. Among the most important are hurricanes, the Gulf Stream, and earthquakes. The potential danger from high wind, waves, storm surges, and storm-driven currents associated with hurricanes is obvious. Evidence for significant bottom scour by the Gulf Stream is abundant; such scour is a threat to the stability of bottom-mounted structures. The fast-flowing water also will hamper floating drill rigs and control of drill strings. A major earthquake of about magnitude 6.8 struck Charleston in 1886; it may have been associated with a zone of active seismicity that crosses South Carolina. The likelihood of a repetition of the 1886 event is presently not predictable but a seismic hazard must be assumed to exist.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr82398","usgsCitation":"Dillon, W.P., Klitgord, K.D., Paull, C.K., Grow, J.A., Ball, M.M., Dolton, G., Powers, R.B., Khan, A.S., Popenoe, P., and Robb, J.M., 1980, Summary of regional geology, petroleum potential, resource assessment and environmental considerations for oil and gas lease sale area #56: U.S. Geological Survey Open-File Report 82-398, 61 p., https://doi.org/10.3133/ofr82398.","productDescription":"61 p.","costCenters":[],"links":[{"id":407344,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_13718.htm","linkFileType":{"id":5,"text":"html"}},{"id":35009,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0398/report.pdf","text":"Report","linkFileType":{"id":1,"text":"pdf"},"description":"Report"},{"id":140845,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0398/report-thumb.jpg"}],"country":"United States","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -81.5,\n              29\n            ],\n            [\n              -72,\n              29\n            ],\n            [\n              -72,\n              38\n            ],\n            [\n              -81.5,\n              38\n            ],\n            [\n              -81.5,\n              29\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b02e4b07f02db698b9a","contributors":{"authors":[{"text":"Dillon, William P. bdillon@usgs.gov","contributorId":79820,"corporation":false,"usgs":true,"family":"Dillon","given":"William","email":"bdillon@usgs.gov","middleInitial":"P.","affiliations":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":false,"id":704559,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Klitgord, Kim D.","contributorId":82307,"corporation":false,"usgs":true,"family":"Klitgord","given":"Kim","email":"","middleInitial":"D.","affiliations":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":false,"id":704560,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Paull, Charles K. 0000-0001-5940-3443","orcid":"https://orcid.org/0000-0001-5940-3443","contributorId":55825,"corporation":false,"usgs":false,"family":"Paull","given":"Charles","email":"","middleInitial":"K.","affiliations":[{"id":7043,"text":"University of North Carolina","active":true,"usgs":false}],"preferred":true,"id":704561,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Grow, John A.","contributorId":25943,"corporation":false,"usgs":true,"family":"Grow","given":"John","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":704562,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Ball, Mahlon M.","contributorId":27472,"corporation":false,"usgs":true,"family":"Ball","given":"Mahlon","email":"","middleInitial":"M.","affiliations":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":false,"id":704563,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Dolton, Gordon","contributorId":50509,"corporation":false,"usgs":true,"family":"Dolton","given":"Gordon","email":"","affiliations":[],"preferred":false,"id":704564,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Powers, Richard B.","contributorId":52248,"corporation":false,"usgs":true,"family":"Powers","given":"Richard","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":704565,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Khan, Abdul S.","contributorId":194534,"corporation":false,"usgs":false,"family":"Khan","given":"Abdul","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":704566,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Popenoe, Peter","contributorId":62206,"corporation":false,"usgs":true,"family":"Popenoe","given":"Peter","email":"","affiliations":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":false,"id":704567,"contributorType":{"id":1,"text":"Authors"},"rank":9},{"text":"Robb, James M.","contributorId":73272,"corporation":false,"usgs":true,"family":"Robb","given":"James","email":"","middleInitial":"M.","affiliations":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":false,"id":704568,"contributorType":{"id":1,"text":"Authors"},"rank":10}]}}
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