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,{"id":57128,"text":"wri811101 - 1982 - Sulfate concentration in water from the upper permeable zone of the Tertiary limestone aquifer system, southeastern United States","interactions":[],"lastModifiedDate":"2012-02-02T00:11:48","indexId":"wri811101","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"81-1101","title":"Sulfate concentration in water from the upper permeable zone of the Tertiary limestone aquifer system, southeastern United States","language":"ENGLISH","doi":"10.3133/wri811101","usgsCitation":"Sprinkle, C.L., 1982, Sulfate concentration in water from the upper permeable zone of the Tertiary limestone aquifer system, southeastern United States (WRI/OFR): U.S. Geological Survey Water-Resources Investigations Report 81-1101, map, scale 1:1,000,000, https://doi.org/10.3133/wri811101.","productDescription":"map, scale 1:1,000,000","costCenters":[],"links":[{"id":174831,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"edition":"WRI/OFR","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b05e4b07f02db699894","contributors":{"authors":[{"text":"Sprinkle, Craig L.","contributorId":41802,"corporation":false,"usgs":true,"family":"Sprinkle","given":"Craig","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":256277,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":11010,"text":"ofr82982 - 1982 - List of published articles on mineralogy and geochemistry for which translations by U.S. Geological Survey members are deposited at the USGS Library in Reston, Virginia","interactions":[],"lastModifiedDate":"2018-07-31T11:13:08","indexId":"ofr82982","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"82-982","title":"List of published articles on mineralogy and geochemistry for which translations by U.S. Geological Survey members are deposited at the USGS Library in Reston, Virginia","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr82982","usgsCitation":"Schafer, C.M., Conte, C.J., and Fleischer, M., 1982, List of published articles on mineralogy and geochemistry for which translations by U.S. Geological Survey members are deposited at the USGS Library in Reston, Virginia: U.S. Geological Survey Open-File Report 82-982, 129 p., https://doi.org/10.3133/ofr82982.","productDescription":"129 p.","costCenters":[],"links":[{"id":144074,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0982/report-thumb.jpg"},{"id":38779,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0982/report.pdf","text":"Report","size":"1.39 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Report"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b15e4b07f02db6a4f36","contributors":{"authors":[{"text":"Schafer, Constance M.","contributorId":67092,"corporation":false,"usgs":true,"family":"Schafer","given":"Constance","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":162373,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Conte, Constance J.","contributorId":80284,"corporation":false,"usgs":true,"family":"Conte","given":"Constance","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":162372,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Fleischer, Michael","contributorId":65835,"corporation":false,"usgs":true,"family":"Fleischer","given":"Michael","email":"","affiliations":[],"preferred":false,"id":162371,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":10484,"text":"ofr8263 - 1982 - Damage in Alameda and Contra Costa counties, California, in the earthquake of 18 April 1906","interactions":[],"lastModifiedDate":"2012-02-02T00:06:33","indexId":"ofr8263","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"82-63","title":"Damage in Alameda and Contra Costa counties, California, in the earthquake of 18 April 1906","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr8263","usgsCitation":"Nason, R., 1982, Damage in Alameda and Contra Costa counties, California, in the earthquake of 18 April 1906: U.S. Geological Survey Open-File Report 82-63, 48 p., ill., maps ;28 cm., https://doi.org/10.3133/ofr8263.","productDescription":"48 p., ill., maps ;28 cm.","costCenters":[],"links":[{"id":143685,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0063/report-thumb.jpg"},{"id":38349,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0063/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4acce4b07f02db67e6e4","contributors":{"authors":[{"text":"Nason, Robert","contributorId":71986,"corporation":false,"usgs":true,"family":"Nason","given":"Robert","affiliations":[],"preferred":false,"id":161476,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":11323,"text":"ofr82417 - 1982 - Review of earthquake activity and current status of seismic monitoring in the region of the Bradley Lake Hydroelectric Project, southern Kenai Peninsula, Alaska; November 27, 1980 - November 30, 1981","interactions":[],"lastModifiedDate":"2012-02-02T00:06:28","indexId":"ofr82417","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"82-417","title":"Review of earthquake activity and current status of seismic monitoring in the region of the Bradley Lake Hydroelectric Project, southern Kenai Peninsula, Alaska; November 27, 1980 - November 30, 1981","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82417","usgsCitation":"Stephens, C., Lahr, J., and Rogers, J.A., 1982, Review of earthquake activity and current status of seismic monitoring in the region of the Bradley Lake Hydroelectric Project, southern Kenai Peninsula, Alaska; November 27, 1980 - November 30, 1981: U.S. Geological Survey Open-File Report 82-417, 27 p., ill., maps ;28 cm., https://doi.org/10.3133/ofr82417.","productDescription":"27 p., ill., maps ;28 cm.","costCenters":[],"links":[{"id":144052,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0417/report-thumb.jpg"},{"id":39135,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0417/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a17e4b07f02db6040dd","contributors":{"authors":[{"text":"Stephens, C.D.","contributorId":18752,"corporation":false,"usgs":true,"family":"Stephens","given":"C.D.","email":"","affiliations":[],"preferred":false,"id":162933,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lahr, J.C.","contributorId":34892,"corporation":false,"usgs":true,"family":"Lahr","given":"J.C.","email":"","affiliations":[],"preferred":false,"id":162934,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Rogers, J. A.","contributorId":90721,"corporation":false,"usgs":true,"family":"Rogers","given":"J.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":162935,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":9422,"text":"ofr82722 - 1982 - Garnets in Montana diatremes; a key to prospecting for kimberlites","interactions":[{"subject":{"id":9422,"text":"ofr82722 - 1982 - Garnets in Montana diatremes; a key to prospecting for kimberlites","indexId":"ofr82722","publicationYear":"1982","noYear":false,"title":"Garnets in Montana diatremes; a key to prospecting for kimberlites"},"predicate":"SUPERSEDED_BY","object":{"id":34654,"text":"b1604 - 1983 - Garnets in Montana diatremes; a key to prospecting for kimberlites","indexId":"b1604","publicationYear":"1983","noYear":false,"title":"Garnets in Montana diatremes; a key to prospecting for kimberlites"},"id":1}],"supersededBy":{"id":34654,"text":"b1604 - 1983 - Garnets in Montana diatremes; a key to prospecting for kimberlites","indexId":"b1604","publicationYear":"1983","noYear":false,"title":"Garnets in Montana diatremes; a key to prospecting for kimberlites"},"lastModifiedDate":"2019-11-07T11:40:04","indexId":"ofr82722","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"82-722","title":"Garnets in Montana diatremes; a key to prospecting for kimberlites","docAbstract":"<p>No abstract available.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr82722","usgsCitation":"Hearn, B., and McGee, E.S., 1982, Garnets in Montana diatremes; a key to prospecting for kimberlites: U.S. Geological Survey Open-File Report 82-722, ii, 44 p. , https://doi.org/10.3133/ofr82722.","productDescription":"ii, 44 p. ","costCenters":[],"links":[{"id":369040,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0722/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":141841,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0722/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b28e4b07f02db6b1387","contributors":{"authors":[{"text":"Hearn, B.C.","contributorId":7700,"corporation":false,"usgs":true,"family":"Hearn","given":"B.C.","affiliations":[],"preferred":false,"id":159659,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"McGee, E. S.","contributorId":75927,"corporation":false,"usgs":true,"family":"McGee","given":"E.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":159660,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":10985,"text":"ofr82819 - 1982 - Measurement of heat flow by a downhole probe technique in the San Joaquin Valley, California","interactions":[],"lastModifiedDate":"2012-02-02T00:06:22","indexId":"ofr82819","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"82-819","title":"Measurement of heat flow by a downhole probe technique in the San Joaquin Valley, California","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82819","usgsCitation":"Sass, J., Galanis, S., and Munroe, R.J., 1982, Measurement of heat flow by a downhole probe technique in the San Joaquin Valley, California: U.S. Geological Survey Open-File Report 82-819, 27 p. :ill., map ;28 cm., https://doi.org/10.3133/ofr82819.","productDescription":"27 p. :ill., map ;28 cm.","costCenters":[],"links":[{"id":143494,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0819/report-thumb.jpg"},{"id":38750,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0819/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a28e4b07f02db6110c5","contributors":{"authors":[{"text":"Sass, J.H.","contributorId":70749,"corporation":false,"usgs":true,"family":"Sass","given":"J.H.","email":"","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":162328,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Galanis, S.P.","contributorId":64242,"corporation":false,"usgs":true,"family":"Galanis","given":"S.P.","affiliations":[],"preferred":false,"id":162327,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Munroe, Robert J.","contributorId":12039,"corporation":false,"usgs":true,"family":"Munroe","given":"Robert","email":"","middleInitial":"J.","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":162326,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":9455,"text":"ofr82997 - 1982 - Geology report for proposed Norton Sound OCS sand and gravel lease sale","interactions":[],"lastModifiedDate":"2012-02-02T00:06:17","indexId":"ofr82997","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"82-997","title":"Geology report for proposed Norton Sound OCS sand and gravel lease sale","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82997","usgsCitation":"Hess, G., and Nelson, C., 1982, Geology report for proposed Norton Sound OCS sand and gravel lease sale: U.S. Geological Survey Open-File Report 82-997, 48 p., ill., maps ;28 cm., https://doi.org/10.3133/ofr82997.","productDescription":"48 p., ill., maps ;28 cm.","costCenters":[],"links":[{"id":142764,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0997/report-thumb.jpg"},{"id":37160,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0997/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67c6e1","contributors":{"authors":[{"text":"Hess, G.R.","contributorId":17606,"corporation":false,"usgs":true,"family":"Hess","given":"G.R.","email":"","affiliations":[],"preferred":false,"id":159716,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Nelson, C.H.","contributorId":88346,"corporation":false,"usgs":true,"family":"Nelson","given":"C.H.","email":"","affiliations":[],"preferred":false,"id":159717,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":9404,"text":"ofr82898 - 1982 - Uranium-lead concordia-discordia intercepts; a program for the TI-59 programmable calculator","interactions":[],"lastModifiedDate":"2012-02-02T00:06:14","indexId":"ofr82898","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"82-898","title":"Uranium-lead concordia-discordia intercepts; a program for the TI-59 programmable calculator","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82898","usgsCitation":"Haxel, G., and Wright, J., 1982, Uranium-lead concordia-discordia intercepts; a program for the TI-59 programmable calculator: U.S. Geological Survey Open-File Report 82-898, 20 p., ill. ;28 cm., https://doi.org/10.3133/ofr82898.","productDescription":"20 p., ill. ;28 cm.","costCenters":[],"links":[{"id":142197,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0898/report-thumb.jpg"},{"id":37117,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0898/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a18e4b07f02db6052ff","contributors":{"authors":[{"text":"Haxel, Gordon","contributorId":12450,"corporation":false,"usgs":true,"family":"Haxel","given":"Gordon","affiliations":[],"preferred":false,"id":159626,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wright, J.E.","contributorId":52575,"corporation":false,"usgs":true,"family":"Wright","given":"J.E.","email":"","affiliations":[],"preferred":false,"id":159627,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":11563,"text":"ofr80676 - 1982 - Estimating peak discharges of small rural streams in Massachusetts","interactions":[{"subject":{"id":11563,"text":"ofr80676 - 1982 - Estimating peak discharges of small rural streams in Massachusetts","indexId":"ofr80676","publicationYear":"1982","noYear":false,"title":"Estimating peak discharges of small rural streams in Massachusetts"},"predicate":"SUPERSEDED_BY","object":{"id":2880,"text":"wsp2214 - 1983 - Estimating peak discharges of small, rural streams in Massachusetts","indexId":"wsp2214","publicationYear":"1983","noYear":false,"title":"Estimating peak discharges of small, rural streams in Massachusetts"},"id":1}],"supersededBy":{"id":2880,"text":"wsp2214 - 1983 - Estimating peak discharges of small, rural streams in Massachusetts","indexId":"wsp2214","publicationYear":"1983","noYear":false,"title":"Estimating peak discharges of small, rural streams in Massachusetts"},"lastModifiedDate":"2022-08-09T15:49:04.64596","indexId":"ofr80676","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"80-676","title":"Estimating peak discharges of small rural streams in Massachusetts","docAbstract":"<p>Floodflows on natural-flow streams in Massachusetts with drainage areas between 0.25 square miles and 260 square miles may be estimated from drainage area, main-channel slope, mean basin elevation, and the area of swamps, lakes, and ponds. Multiple-regression techniques were used to define the relationship between a suite of basin and climatic characteristics and flood peaks in three flood-frequency regions at a total of 95 sites. Station flood-frequency data were computed following guidelines in Bulletin I7A of the U.S. Water Resources Council. The frequency analyses are based upon weighted skew values, and adjustments for high and low outliers, and historic peak data. Regression equations for estimation of peak discharges for 0.5, 0.2, 0.1, 0.04, 0.02, and 0.01 exceedance probabilities are provided for ungaged sites. An improved sample of flood peaks and gaging stations and the definition of three flood-frequency regions reduced the standard error of estimate by about 5 percent over those for the 1977 relations. Included in this analysis were the synthetic flood-frequency data at eight sites computed using historic climatic data and 10 parameters optimized by calibration of the U.S. Geological Survey's rainfall-runoff model with storm data observed over II years. The equations are applicable to streams unaffected by regulation where the usable manmade storage is less than 4.5 million cubic feet per square mile, or by diversions or urbanization. The equations are restricted to sites where the basin indices are within a specified range outside of eastern Plymouth, Barnstable, Dukes or Nantucket Counties. In these areas, the available data do not adequately define the influence of high infiltration and storage capacities of drainage basins on floodflows.</p>","largerWorkType":{"id":18,"text":"Report"},"language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr80676","collaboration":"Prepared in cooperation with the Massachusetts Department of Public Works and the U.S. Department of Highway Transportation, Federal Highway Administration","usgsCitation":"Wandle, S.W., 1982, Estimating peak discharges of small rural streams in Massachusetts: U.S. Geological Survey Open-File Report 80-676, iv, 33 p., https://doi.org/10.3133/ofr80676.","productDescription":"iv, 33 p.","costCenters":[],"links":[{"id":405034,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1980/0676/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":145810,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1980/0676/report-thumb.jpg"}],"country":"United 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William Jr.","contributorId":99562,"corporation":false,"usgs":true,"family":"Wandle","given":"S.","suffix":"Jr.","email":"","middleInitial":"William","affiliations":[],"preferred":false,"id":163363,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":9907,"text":"ofr82823 - 1982 - Illustrations of gravity models of the southeast limb of the Blacktail-Snowcrest uplift, southwest Montana","interactions":[],"lastModifiedDate":"2012-02-02T00:06:19","indexId":"ofr82823","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"82-823","title":"Illustrations of gravity models of the southeast limb of the Blacktail-Snowcrest uplift, southwest Montana","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82823","usgsCitation":"Kulik, D.M., 1982, Illustrations of gravity models of the southeast limb of the Blacktail-Snowcrest uplift, southwest Montana: U.S. Geological Survey Open-File Report 82-823, 8 p., chiefly ill., map ;28 cm., https://doi.org/10.3133/ofr82823.","productDescription":"8 p., chiefly ill., map ;28 cm.","costCenters":[],"links":[{"id":142696,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0823/report-thumb.jpg"},{"id":37699,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0823/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a09e4b07f02db5faa49","contributors":{"authors":[{"text":"Kulik, D. M.","contributorId":46948,"corporation":false,"usgs":true,"family":"Kulik","given":"D.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":160492,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":8932,"text":"ofr82616 - 1982 - Bibliography of northeast Siberian geology and geophysics","interactions":[],"lastModifiedDate":"2012-02-02T00:06:09","indexId":"ofr82616","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"82-616","title":"Bibliography of northeast Siberian geology and geophysics","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82616","usgsCitation":"Fujita, K., Dretzka, E., and Grantz, A., 1982, Bibliography of northeast Siberian geology and geophysics (2nd ed.): U.S. Geological Survey Open-File Report 82-616, 80 p., map ;28 cm., https://doi.org/10.3133/ofr82616.","productDescription":"80 p., map ;28 cm.","costCenters":[],"links":[{"id":141179,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0616/report-thumb.jpg"},{"id":36538,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0616/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"edition":"2nd ed.","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4ee4b07f02db627f9c","contributors":{"authors":[{"text":"Fujita, K.","contributorId":87935,"corporation":false,"usgs":true,"family":"Fujita","given":"K.","email":"","affiliations":[],"preferred":false,"id":158576,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Dretzka, E.E.","contributorId":18768,"corporation":false,"usgs":true,"family":"Dretzka","given":"E.E.","email":"","affiliations":[],"preferred":false,"id":158575,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Grantz, Arthur agrantz@usgs.gov","contributorId":2585,"corporation":false,"usgs":true,"family":"Grantz","given":"Arthur","email":"agrantz@usgs.gov","affiliations":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"preferred":true,"id":158574,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":8719,"text":"ofr81803 - 1982 - Hydrology of area 9, Eastern Coal Province, West Virginia","interactions":[],"lastModifiedDate":"2012-02-02T00:06:11","indexId":"ofr81803","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"81-803","title":"Hydrology of area 9, Eastern Coal Province, West Virginia","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr81803","usgsCitation":"Ehlke, T.A., Runner, G.S., and Downs, S.C., 1982, Hydrology of area 9, Eastern Coal Province, West Virginia: U.S. Geological Survey Open-File Report 81-803, v, 63 p. :ill. (some col.), maps (some col.) ;28 cm., https://doi.org/10.3133/ofr81803.","productDescription":"v, 63 p. :ill. (some col.), maps (some col.) ;28 cm.","costCenters":[],"links":[{"id":94874,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/0803/report.pdf","size":"23135","linkFileType":{"id":1,"text":"pdf"}},{"id":142015,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/0803/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a13e4b07f02db601fe5","contributors":{"authors":[{"text":"Ehlke, Theodore A.","contributorId":83523,"corporation":false,"usgs":true,"family":"Ehlke","given":"Theodore","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":158207,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Runner, Gerald S.","contributorId":90297,"corporation":false,"usgs":true,"family":"Runner","given":"Gerald","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":158208,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Downs, Sanford C.","contributorId":66233,"corporation":false,"usgs":true,"family":"Downs","given":"Sanford","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":158206,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":40254,"text":"ofr82592 - 1982 - Complete Bouguer gravity map near Crater Lake, Oregon","interactions":[],"lastModifiedDate":"2023-08-03T11:03:47.107333","indexId":"ofr82592","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"82-592","title":"Complete Bouguer gravity map near Crater Lake, Oregon","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr82592","usgsCitation":"Finn, C.A., 1982, Complete Bouguer gravity map near Crater Lake, Oregon: U.S. Geological Survey Open-File Report 82-592, 1 Plate: 42.25 × 51.65 inches, https://doi.org/10.3133/ofr82592.","productDescription":"1 Plate: 42.25 × 51.65 inches","costCenters":[],"links":[{"id":173209,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":71329,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0592/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Oregon","otherGeospatial":"Crater Lake","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -122.40918417579934,\n              43.10732505285361\n            ],\n            [\n              -122.40918417579934,\n              42.73164744995506\n            ],\n            [\n              -121.83240008555535,\n              42.73164744995506\n            ],\n            [\n              -121.83240008555535,\n              43.10732505285361\n            ],\n            [\n              -122.40918417579934,\n              43.10732505285361\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1ae4b07f02db6a8398","contributors":{"authors":[{"text":"Finn, Carol A. 0000-0002-6178-0405 cfinn@usgs.gov","orcid":"https://orcid.org/0000-0002-6178-0405","contributorId":1326,"corporation":false,"usgs":true,"family":"Finn","given":"Carol","email":"cfinn@usgs.gov","middleInitial":"A.","affiliations":[{"id":211,"text":"Crustal Geophysics and Geochemistry Science Center","active":true,"usgs":true}],"preferred":true,"id":223183,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":8827,"text":"ofr82749 - 1982 - Geochemical and mineralogic data from the Lamprecht and Felder uranium deposits, Live Oak County, Texas","interactions":[],"lastModifiedDate":"2012-02-02T00:06:15","indexId":"ofr82749","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"82-749","title":"Geochemical and mineralogic data from the Lamprecht and Felder uranium deposits, Live Oak County, Texas","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82749","usgsCitation":"Fishman, N., Reynolds, R.L., and Goldhaber, M., 1982, Geochemical and mineralogic data from the Lamprecht and Felder uranium deposits, Live Oak County, Texas: U.S. Geological Survey Open-File Report 82-749, ii, 35 p., ill. ;28 cm., https://doi.org/10.3133/ofr82749.","productDescription":"ii, 35 p., ill. ;28 cm.","costCenters":[],"links":[{"id":141606,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0749/report-thumb.jpg"},{"id":36403,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0749/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b24e4b07f02db6ae6d8","contributors":{"authors":[{"text":"Fishman, N.S.","contributorId":59441,"corporation":false,"usgs":true,"family":"Fishman","given":"N.S.","email":"","affiliations":[],"preferred":false,"id":158398,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Reynolds, R. L. 0000-0002-4572-2942","orcid":"https://orcid.org/0000-0002-4572-2942","contributorId":79885,"corporation":false,"usgs":true,"family":"Reynolds","given":"R.","middleInitial":"L.","affiliations":[{"id":318,"text":"Geosciences and Environmental Change Science Center","active":true,"usgs":true}],"preferred":true,"id":158399,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Goldhaber, M. B. 0000-0002-1785-4243","orcid":"https://orcid.org/0000-0002-1785-4243","contributorId":103280,"corporation":false,"usgs":true,"family":"Goldhaber","given":"M. B.","affiliations":[],"preferred":false,"id":158400,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":9116,"text":"ofr82794 - 1982 - Heat-flow measurements at shot points along the 1978 Saudi Arabia seismic deep-refraction line; Part II, Discussion and interpretation","interactions":[],"lastModifiedDate":"2012-02-02T00:06:14","indexId":"ofr82794","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"82-794","title":"Heat-flow measurements at shot points along the 1978 Saudi Arabia seismic deep-refraction line; Part II, Discussion and interpretation","docAbstract":"The heat-flow profile across the Arabian Shield from Ar Riyad to Ad Darb and across the Red Sea is examined for compatibility with the lithospheric structure of the area as deduced from geologic and other geophysical data. Broad continental uplift associated with Red Sea rifting is symmetric about the Red Sea axis, and geologic and geochronologic evidence indicate that uplift has occurred mainly in the interval 25-13 Ma (mega-annum) ago. Thermal-profile changes in the upper mantle resulting from an influx of hot material associated with rifting yield the correct order of magnitude of uplift, and this mechanism is suggested as the explanation for the regional doming. A lithospheric section, constructed from seismic refraction, gravity, and regional geologic data, provides the framework for construction of thermal models. \r\n\r\nThermal gradient measurements were made in drill holes at five shot points. Geotherms for the Shield, which assume a radiogenic heat-source distribution that decreases exponentially with depth, yield temperatures of about 450?C at a depth of 40 km (base of the crust) for shot points 2 (Sabhah) and 3. The geotherm for shot point 4 (near Bishah) yields a distinctly higher temperature (about 580?C) for the same depth. \r\n\r\nStatic models used to model the heat flow in the oceanic crust of the Red Sea shelf and coastal plain either yield too small a heat flow to match the observed heat flow or give lithosphere thicknesses that are so thin as to be improbable. Dynamic (solid-state accretion) models, which account for mantle flow at the base of the lithosphere, adequately match the observed heat-flow values. In the deep-water trough of the Red Sea, which is presently undergoing active sea-floor spreading, classical models of heat flow for a moving slab with accretion at the spreading center are adequate to explain the average heat-flow level. \r\n\r\nAt shot point 5 (Ad Darb), the anomalous heat flow of 2 HFU (heat-flow units) can be explained in terms of a Shield component (0.8-1.0 HFU) and a component related to heating by the abutting oceanic crust a few kilometers away for periods exceeding 10 Ma. Analytical results are included for: 1) the cooling of a static sheet with an initial temperature distribution characteristic of a moving slab in a sea-floor spreading environment, and 2) the heating of a homogeneous quarter-space at its vertical boundary.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82794","usgsCitation":"Gettings, M.E., 1982, Heat-flow measurements at shot points along the 1978 Saudi Arabia seismic deep-refraction line; Part II, Discussion and interpretation: U.S. Geological Survey Open-File Report 82-794, ii, 43 p., ill. ;28 cm., https://doi.org/10.3133/ofr82794.","productDescription":"ii, 43 p., ill. ;28 cm.","costCenters":[],"links":[{"id":141604,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0794/report-thumb.jpg"},{"id":36728,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0794/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a69e4b07f02db63c67f","contributors":{"authors":[{"text":"Gettings, M. E.","contributorId":25148,"corporation":false,"usgs":true,"family":"Gettings","given":"M.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":159127,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":40279,"text":"ofr821073 - 1982 - Principal facts and a complete Bouguer anomaly map for a gravity study of the proposed Mt. Henry Wilderness, Montana","interactions":[],"lastModifiedDate":"2012-02-02T00:10:34","indexId":"ofr821073","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"82-1073","title":"Principal facts and a complete Bouguer anomaly map for a gravity study of the proposed Mt. Henry Wilderness, Montana","language":"ENGLISH","doi":"10.3133/ofr821073","usgsCitation":"Bankey, V., Kleinkopf, M.D., Brickey, M., and Mancinelli, J., 1982, Principal facts and a complete Bouguer anomaly map for a gravity study of the proposed Mt. Henry Wilderness, Montana: U.S. Geological Survey Open-File Report 82-1073, 1 map ;32 x 38 cm. +1 text (14 p. ; 28 cm.), https://doi.org/10.3133/ofr821073.","productDescription":"1 map ;32 x 38 cm. +1 text (14 p. ; 28 cm.)","costCenters":[],"links":[{"id":172948,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/1073/report-thumb.jpg"},{"id":71859,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/1073/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":71860,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/1073/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa9e4b07f02db668160","contributors":{"authors":[{"text":"Bankey, Viki viki@usgs.gov","contributorId":1238,"corporation":false,"usgs":true,"family":"Bankey","given":"Viki","email":"viki@usgs.gov","affiliations":[],"preferred":true,"id":223212,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kleinkopf, M. Dean","contributorId":37723,"corporation":false,"usgs":true,"family":"Kleinkopf","given":"M.","email":"","middleInitial":"Dean","affiliations":[],"preferred":false,"id":223214,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Brickey, Mike","contributorId":105298,"corporation":false,"usgs":true,"family":"Brickey","given":"Mike","email":"","affiliations":[],"preferred":false,"id":223215,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Mancinelli, Joe","contributorId":19180,"corporation":false,"usgs":true,"family":"Mancinelli","given":"Joe","email":"","affiliations":[],"preferred":false,"id":223213,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":9746,"text":"ofr811200 - 1982 - Analysis and characterization of urban storm-water runoff for selected basins in the Baltimore, Maryland, metropolitan area; a project plan","interactions":[],"lastModifiedDate":"2012-02-02T00:06:06","indexId":"ofr811200","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"81-1200","title":"Analysis and characterization of urban storm-water runoff for selected basins in the Baltimore, Maryland, metropolitan area; a project plan","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr811200","usgsCitation":"Katz, B., and Fisher, G.T., 1982, Analysis and characterization of urban storm-water runoff for selected basins in the Baltimore, Maryland, metropolitan area; a project plan: U.S. Geological Survey Open-File Report 81-1200, iv, 58 p. ill., maps ;28 cm., https://doi.org/10.3133/ofr811200.","productDescription":"iv, 58 p. ill., maps ;28 cm.","costCenters":[],"links":[{"id":141587,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/1200/report-thumb.jpg"},{"id":37492,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/1200/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad0e4b07f02db680c5a","contributors":{"authors":[{"text":"Katz, B. G.","contributorId":82702,"corporation":false,"usgs":true,"family":"Katz","given":"B. G.","affiliations":[],"preferred":false,"id":160224,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Fisher, G. T.","contributorId":49359,"corporation":false,"usgs":true,"family":"Fisher","given":"G.","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":160223,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":10472,"text":"ofr82232 - 1982 - Has offshore oil production become safer?","interactions":[],"lastModifiedDate":"2012-02-02T00:06:32","indexId":"ofr82232","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"82-232","title":"Has offshore oil production become safer?","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82232","usgsCitation":"Nakassis, A., 1982, Has offshore oil production become safer?: U.S. Geological Survey Open-File Report 82-232, 27 p., ill. ;28 cm., https://doi.org/10.3133/ofr82232.","productDescription":"27 p., ill. ;28 cm.","costCenters":[],"links":[{"id":143932,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0232/report-thumb.jpg"},{"id":38336,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0232/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a70e4b07f02db6410e1","contributors":{"authors":[{"text":"Nakassis, Anastase","contributorId":96691,"corporation":false,"usgs":true,"family":"Nakassis","given":"Anastase","affiliations":[],"preferred":false,"id":161460,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":8221,"text":"ofr821128 - 1982 - Contour map showing minimum depth to ground water, upper Santa Ana River valley, California, 1973-1979","interactions":[],"lastModifiedDate":"2022-09-26T20:55:48.486038","indexId":"ofr821128","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"82-1128","title":"Contour map showing minimum depth to ground water, upper Santa Ana River valley, California, 1973-1979","docAbstract":"<p>A contour map showing minimum depth to ground water from 1973 through 1979 was constructed for the upper Santa Ana River valley region. The map was prepared as an initial step in an ongoing liquefaction-potential study, but is not a liquefaction-hazard map. The contour map indicates where ground water shallower than 50 ft below land surface occurred at least once during the 1973-1979 period, and also indicates the probable future distribution of ground water shallower than 50 ft below land surface for periods when climatic conditions and water-management policies similar to those in the 1970's recur. This contour map does not show how the water table actually looked at any particular instant during the reporting period, nor does it show average or typical ground-water conditions during the reporting period. Instead, this map shows what the regional ground-water table would look like if the shallowest water level measured in each well during the 1973-1979 period is used as the basis for constructing a map of minimum depth to ground water.</p><p>This map identifies twenty areas within the upper Santa Ana River valley where water levels in wells were shallower than 50 ft below land surface at least once during the period 1973-1979. In the greater Santa Ana River area, between the San Jacinto ground-water barrier and Prado flood-control dam, ground water was shallower than 50 ft below land surface intermittently throughout the 1973-1979 period. In this area, shallow water generally reflects shallow depths to impermeable bedrock and the ease and frequency with which ground water is replenished by natural and artificial recharge. Most of the other areas of shallow ground water identified on this map experienced pervasive shallow water levels only after mid-1977. Prior to mid-1977, ground water in these areas generally was deeper than 50 ft below land surface.</p><p>During later parts of the 1973-1979 period, water tables rose mainly because of two factors: (1) wetter-than-normal winters in 1977-1978 and 19781979 contributed increased volumes of surface runoff and natural recharge in the upper Santa Ana River valley region; and (2) commencing in 1972, ground water in the Valley region has been replenished by artificial recharge of imported water derived from the California State Water Project. The accelerated natural and artificial recharge of ground water basins in 1977, 1978, and 1979 raised ground water tables throughout the Valley region.</p><p>Water-level records more recent than September 1979 indicate that for most of the twenty areas of shallow ground water, water levels have remained shallower than 50 ft below land surface through December 1981. In some areas, water levels have risen even more. For example, in the San Bernardino area, rising water locally has invaded basements, undermined roadways, and affected foundation construction. Where post-1979 water levels have continued to rise, the areas underlain by shallow ground water have expanded and now are larger than the areas shown on the contour map of this report.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr821128","usgsCitation":"Carson, S.E., and Matti, J.C., 1982, Contour map showing minimum depth to ground water, upper Santa Ana River valley, California, 1973-1979: U.S. Geological Survey Open-File Report 82-1128, Report: 48 p.; 2 Plates: 65.74 x 41.40 inches and 29.29 x 28.86 inches, https://doi.org/10.3133/ofr821128.","productDescription":"Report: 48 p.; 2 Plates: 65.74 x 41.40 inches and 29.29 x 28.86 inches","costCenters":[],"links":[{"id":407364,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/1128/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":407363,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/1128/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":407362,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/1128/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":141329,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/1128/report-thumb.jpg"}],"country":"United States","state":"California","otherGeospatial":"upper Santa Ana River valley","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -117.78444444444445,33.984722222222224 ], [ -117.78444444444445,34.25 ], [ -117,34.25 ], [ -117,33.984722222222224 ], [ -117.78444444444445,33.984722222222224 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b04e4b07f02db6990f3","contributors":{"authors":[{"text":"Carson, Scott E.","contributorId":99973,"corporation":false,"usgs":true,"family":"Carson","given":"Scott","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":157366,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Matti, Jonathan C. jmatti@usgs.gov","contributorId":3666,"corporation":false,"usgs":true,"family":"Matti","given":"Jonathan","email":"jmatti@usgs.gov","middleInitial":"C.","affiliations":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"preferred":false,"id":157365,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":11361,"text":"ofr82297 - 1982 - An alternative hypothesis for sink development above salt cavities in the Detroit area","interactions":[],"lastModifiedDate":"2012-02-02T00:06:20","indexId":"ofr82297","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"82-297","title":"An alternative hypothesis for sink development above salt cavities in the Detroit area","docAbstract":"Subsidence and sink formation resulting from brining operations in the Windsor-Detroit area include the 1954 sink at the Canadian Salt Company brine field near Windsor, Ontario, and the 1971 sinks at the BASF Wyandotte Corporation brine field at Grosse Ile, Mich. Earlier investigations into both occurrences concluded that the mechanism of sink development consisted of the gradual stoping of poorly supported brine-gallery roof rock to the near surface with subsequent surface collapse. A more recent study attempted to describe the mechanism of sink development in terms of the geometry of a cylindrical chimney formed by stoping of roof rock, the height of a cavity at depth, the depth of overlying rock, and the bulking ratio of the rubble formed during stoping. \r\n\r\nPersons with extensive experience in solution mining in the Windsor-Detroit area have expressed doubt that the stoping mechanism could fully explain the development of these sinks. Further, they have proposed that the relatively shallow (300-ft-deep) Sylvania Sandstone, in this case, may be responsible for the sinks by a secondary undermining mechanism to be examined in this paper. The mechanism involves downwarping of the beds overlying the salt cavity and development of a shallower cavity in the Sylvania Sandstone by downward migration of cohesionless sand grains from the Sylvania through openings in the disturbed rock to the lower cavity. This study indicates that under natural conditions the Sylvania will not migrate, even in the presence of large underground water flows because the sandstone possesses some cohesion throughout its depth. However, further investigation has formulated a mechanism that could allow the Sylvania Sandstone to loose its cohesion in response to high horizontal stresses. These stresses could be the result of deformation that accompanies general subsidence and (or) of past geologic processes.\r\n\r\nIncluded in this study were experimental and analytical investigations. As determined by uniaxial and triaxial testing, the Sylvania Sandstone in the Detroit area has been shown to have low compressive strength. In addition, it exhibits an explosive type failure whereby over 50 percent of the sample is reduced to loose granular sand. As a result of these characteristics, the Sylvania Sandstone can loose its cohesion when subjected to high horizontal stresses. \r\n\r\nEfforts at mechanically modeling the Sylvania were made to account for the measurements and observations. Linear arch theory was used for an elastic analysis. Linear arch theory predicts two modes of failure: (1) arch crushing, a compressive failure of the upper portion of the arch due to compressive stresses exceeding the compressive strength of the material, and (2) arch collapse, a sagging of the beds due to compressive strains which reduce the arch line to a length less than the original arch length. The arch crushing mode of failure would then yield the loose granular sand as observed in laboratory testing. Arch collapse would simply result in bed sagging without granulation of the sandstone. Arch collapse is favored by thin-bedded material while arch crushing is favored by thick-bedded material. Arch crushing seems to be a likely mode of failure for the Windsor-Detroit sinks. \r\n\r\nIt is believed that after a crushing failure the sand-water slurry (specific gravity 1.2) which exceeds the density of the cavity brine will migrate downward through cracks and open joints eventually reaching the practically limitless open spaces of the rubble column and salt cavity. As the extent of the cavity within the Sylvania increases in depth and width because of sand migration, a critical span will be reached where the immediately overlying upper Sylvania and the overlying Detroit River Dolomite will fail. The collapse will allow a path for the approximately 100 ft of clay to collapse, resulting in a sink as the surface manifestation.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82297","usgsCitation":"Stump, D., Nieto, A., and Ege, J., 1982, An alternative hypothesis for sink development above salt cavities in the Detroit area: U.S. Geological Survey Open-File Report 82-297, 65 p., ill., map ;28 cm., https://doi.org/10.3133/ofr82297.","productDescription":"65 p., ill., map ;28 cm.","costCenters":[],"links":[{"id":142525,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0297/report-thumb.jpg"},{"id":39188,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0297/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adbe4b07f02db685bad","contributors":{"authors":[{"text":"Stump, Daniel","contributorId":35318,"corporation":false,"usgs":true,"family":"Stump","given":"Daniel","email":"","affiliations":[],"preferred":false,"id":163001,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Nieto, A.S.","contributorId":30629,"corporation":false,"usgs":true,"family":"Nieto","given":"A.S.","email":"","affiliations":[],"preferred":false,"id":163000,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Ege, J. R.","contributorId":106117,"corporation":false,"usgs":false,"family":"Ege","given":"J. R.","affiliations":[],"preferred":false,"id":163002,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":8141,"text":"ofr82743 - 1982 - Radioactive mineral spring precipitates, their analytical and statistical data and the uranium connection","interactions":[],"lastModifiedDate":"2012-02-02T00:06:13","indexId":"ofr82743","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"82-743","title":"Radioactive mineral spring precipitates, their analytical and statistical data and the uranium connection","docAbstract":"Major radioactive mineral springs are probably related to deep zones of active metamorphism in areas of orogenic tectonism. The most common precipitate is travertine, a chemically precipitated rock composed chiefly of calcium carbonate, but also containing other minerals. The mineral springs are surface manifestations of hydrothermal conduit systems which extend downward many kilometers to hot source rocks. Conduits are kept open by fluid pressure exerted by carbon dioxide-charged waters rising to the surface propelled by heat and gas (CO2 and steam) pressure. \r\n\r\nOn reaching the surface, the dissolved carbon dioxide is released from solution, and calcium carbonate is precipitated. Springs also contain sulfur species (for example, H2S and HS-), and radon, helium and methane as entrained or dissolved gases. The HS- ion can react to form hydrogen sulfide gas, sulfate salts, and native sulfur. Chemical salts and native sulfur precipitate at the surface. The sulfur may partly oxidize to produce detectable sulfur dioxide gas. \r\n\r\nRadioactivity is due to the presence of radium-226, radon-222, radium-228, and radon-220, and other daughter products of uranium-238 and thorium-232. Uranium and thorium are not present in economically significant amounts in most radioactive spring precipitates. \r\n\r\nMost radium is coprecipitated at the surface with barite. Barite (barium sulfate) forms in the barium-containing spring water as a product of the oxidation of sulfur species to sulfate ions. The relatively insoluble barium sulfate precipitates and removes much of the radium from solution. Radium coprecipitates to a lesser extent with manganese-barium- and iron-oxy hydroxides. \r\n\r\nR-mode factor analysis of abundances of elements suggests that 65 percent of the variance of the different elements is affected by seven factors interpreted as follows: (1) Silica and silicate contamination and precipitation; (2) Carbonate travertine precipitation; (3) Radium coprecipitation; (4) Evaporite precipitation; (5) Hydrous limonite precipitation and coprecipitated elements including uranium; (6) Rare earth elements deposited with detrital contamination (?); (7) Metal carbonate adsorption and precipitation. \r\n\r\nEconomically recoverable minerals occurring at some localities in spring precipitates are ores of iron, manganese, sulfur, tungsten and barium and ornamental travertine.\r\n\r\nContinental radioactive mineral springs occur in areas of crustal thickening caused by overthrusting of crustal plates, and intrusion and metamorphism. Sedimentary rocks on the lower plate are trapped between the plates and form a zone of metamorphism. Connate waters, carbonate rocks and organic-carbon-bearing rocks react to extreme pressure and temperature to produce carbon dioxide, and steam. Fractures are forced open by gas and fluid pressures. Deep-circulating meteoric waters then come in contact with the reactive products, and a hydrothermal cell forms. When hot mineral-charged waters reach the surface they form the familiar hot mineral springs. Hot springs also occur in relation to igneous intrusive action or volcanism both of which may be products of the crustal plate overthrusting. Uranium and thorium in the sedimentary rocks undergoing metamorphism are sometimes mobilized, but mobilization is generally restricted to an acid hydrothermal environment; much is redeposited in favorable environments in the metamorphosed sediments. Radium and radon, which are highly mobile in both acid and alkaline aqueous media move upward into the hydrothermal cell and to the surface.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82743","usgsCitation":"Cadigan, R.A., and Felmlee, J., 1982, Radioactive mineral spring precipitates, their analytical and statistical data and the uranium connection: U.S. Geological Survey Open-File Report 82-743, iv, 127 p. ill., map ;28 cm., https://doi.org/10.3133/ofr82743.","productDescription":"iv, 127 p. ill., map ;28 cm.","costCenters":[],"links":[{"id":142134,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0743/report-thumb.jpg"},{"id":35744,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0743/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adae4b07f02db685961","contributors":{"authors":[{"text":"Cadigan, R. A.","contributorId":57844,"corporation":false,"usgs":true,"family":"Cadigan","given":"R.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":157217,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Felmlee, J.K.","contributorId":106114,"corporation":false,"usgs":true,"family":"Felmlee","given":"J.K.","email":"","affiliations":[],"preferred":false,"id":157218,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":11399,"text":"ofr82628 - 1982 - Water resources of southeastern Oahu, Hawaii","interactions":[],"lastModifiedDate":"2012-02-02T00:06:21","indexId":"ofr82628","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"82-628","title":"Water resources of southeastern Oahu, Hawaii","docAbstract":"Southeastern Oahu comprises the eastern end of the Koolau Range and is divided into two roughly equal parts by the crest of the range. The northside of the crest is commonly called the windward side and the southside, the leeward. Precipitous cliffs aproned by a gently sloping landscape are the main topographic features on the windward side. The leeward side is a gentle lava-flow slope incised by steep narrow valleys. \r\n\r\nThe main Koolau fissure zone, including the caldera, lies on the windward side. The leeward side includes minor rift zones that are perpendicular to and intersect the main fissure zone. Dikes in the main fissure zone strike from nearly east-west in the eastern end to about N. 55? W. in the western part. Dikes in the minor rift zones strike from north-south to slightly northeasterly. \r\n\r\nWater use is about 18 Mgal/d (million gallons per day) of which only 4 Mgal/d is obtained locally from ground-water sources. About a third of the 14 Mgal/d deficit is imported from sources northwest of the study area on the windward side and the remainder from sources in the Honolulu and Pearl Harbor areas on the leeward side. The 4 Mgal/d being developed represents only about 3 percent of the area's rainfall compared to a development-rainfall ratio of 20 percent for the rest of the island. \r\n\r\nStreams are short and flashy. Perennial streamflow to the sea occurs only in Maunawili Valley and in the Waimanalo area. Mean annual discharge is estimated at 20 Mgal/d in the windward side and at 15 Mgal/d on the leeward side. Low flow, expressed as the flow that is equaled or exceeded 90 percent of the time, is 5 Mgal/d windward of the crest and zero leeward of it. Most fresh ground water occurs in lava flows of the Koolau Volcanics. It is impounded by dikes in the rift zones and floats on saline ground water as lenses outside the rift zones. Small but important bodies of freshwater are perched in volcanic rocks of the Honolulu Group in Maunawili Valley. Fresh ground water occurs in near-shore calcareous sands that overlie a clay horizon in the Waimanalo area. Deeply buried talus and alluvium also carry fresh ground water in the Waimanalo area. \r\n\r\nWells tapping saline ground water in fresh lava flows of the Honolulu Group provide water for a sea-life park in the Makapuu area. The same aquifer is tapped by wells for disposal of the saline waste water. \r\n\r\nThe current development scheme in the windward side that utilizes only the free-flow equilibrium discharge of dike-impounded water is inefficient and does not cope with the annual weather cycle. The flow available for development under this scheme is greatest in the rainy winter months when demand is the lowest and least in the summer months when demand is the highest. A more optimal scheme would be to change this natural flow pattern by depleting storage by pumping to increase flow in the high-demand summer months and allowing the depleted storage to recover naturally in the low-demand winter months. Depleting storage would lower water levels which would provide more room for infiltration and provide less opportunity for evapotranspiration. \r\n\r\nThe basal-water reservoir in the leeward side is isolated hydrologically from abutting reservoirs outside the area and can and should be fully exploited. The existing development of the basal-water reservoir is small compared to the natural ground-water flow and that part not being developed is wasting to the sea. Because the area is hydrologically isolated, development will not be detrimental to or reduce the ground-water supply outside the area.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82628","usgsCitation":"Takasaki, K., and Mink, J., 1982, Water resources of southeastern Oahu, Hawaii: U.S. Geological Survey Open-File Report 82-628, viii, 97 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr82628.","productDescription":"viii, 97 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":142573,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0628/report-thumb.jpg"},{"id":39220,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0628/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49dee4b07f02db5e3158","contributors":{"authors":[{"text":"Takasaki, K. J.","contributorId":44523,"corporation":false,"usgs":true,"family":"Takasaki","given":"K. J.","affiliations":[],"preferred":false,"id":163073,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Mink, John F.","contributorId":89510,"corporation":false,"usgs":true,"family":"Mink","given":"John F.","affiliations":[],"preferred":false,"id":163074,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":10302,"text":"ofr82650 - 1982 - Water quality of Belton Lake, central Texas","interactions":[],"lastModifiedDate":"2016-08-11T15:16:38","indexId":"ofr82650","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"82-650","title":"Water quality of Belton Lake, central Texas","docAbstract":"<p>The concentrations of dissolved solids, chloride, and sulfate in Belton Lake on the Leon River in central Texas average about 240 milligrams per liter, 40 milligrams per liter, and 30 milligrams per liter, respectively. The water is hard or very hard, averaging 170 milligrams per liter as calcium carbonate. The average concentrations of these constituents and hardness are least during late summer and early fall after periods of sustained high inflow.</p>\n<p>Thermal stratification begins to develop in Belton Lake in late February or early March. The water usually is stratified into three fairly distinct layers by early June, and stratification usually persists until September or October. Thermal stratification and seasonal variations in the concentrations of dissolved constituents in inflow result in stratification of the principal dissolved constituents. Dissolved solids in water at the surface of deep sites during summer differ from those at the bottom by about 40 milligrams per liter. Thermal stratification also results in significant seasonal and areal variations in dissolved oxygen, dissolved iron, dissolved manganese, total inorganic nitrogen, and total phosphorus.</p>\n<p>Oxygen used in the oxidation of dead organisms and other organic material near the bottom of the lake is not replaced during periods of summer stagnation. Consequently, water below depths of 35 to 40 feet (10.7 to 12.2 meters) usually contains less than 1.0 milligram per liter of dissolved oxygen during these periods.</p>\n<p>Water near the surface at most sites in the lake throughout the year usually contains less than 30 micrograms per liter of dissolved iron and 20 micrograms per liter of dissolved manganese. Reducing conditions during periods of summer stagnation result in tile dissolution of iron and manganese from the sediments in deep areas of the lake. The concentrations of both constituents are greatest near the bottom at site Ac, a deep site near Belton Dam. Iron concentrations at this site during the summer have ranged from 0 to 600 micrograms per liter and have averaged about 290 micrograms per liter; manganese concentrations have ranged from 0 to 540 micrograms per liter and have averaged about 320 micrograms per liter.</p>\n<p>Concentrations of total inorganic nitrogen and total phosphorus are greatest at deep sites during periods of summer stagnation when decay of aquatic organisms and chemical reduction of bottom sediments release the constituents to the water. The concentrations of total inorganic nitrogen and total phosphorus in the bottom stratum of water at site A c during the summer average about 0.75 milligram per liter of nitrogen and 0.10 milligram per liter of phosphorus. The concentrations of these constituents in the surface stratum at site A C during the summer average about 0.02 milligram per liter of nitrogen and 0.01 milligram per liter of phosphorus.</p>\n<p>The maximum concentrations of chlorinated hydrocarbon insecticides or their degradation products detected in bottom sediments collected from the lake during four lake surveys included 1.1 micrograms per kilogram of DDT, 3.0 micrograms per kilogram of DDD, 11 micrograms per kilogram of DDE, and 2 micrograms per kilogram of chlordane.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Austin, TX","doi":"10.3133/ofr82650","usgsCitation":"Mendieta, H., and Pate, D.L., 1982, Water quality of Belton Lake, central Texas: U.S. Geological Survey Open-File Report 82-650, Report: vi, 70 p.; Plate: 10.52 x 16.63 inches, https://doi.org/10.3133/ofr82650.","productDescription":"Report: vi, 70 p.; Plate: 10.52 x 16.63 inches","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":38160,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0650/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":38161,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0650/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":144093,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0650/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e478fe4b07f02db48a09f","contributors":{"authors":[{"text":"Mendieta, H.B.","contributorId":38965,"corporation":false,"usgs":true,"family":"Mendieta","given":"H.B.","email":"","affiliations":[],"preferred":false,"id":161164,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Pate, Dale L.","contributorId":55007,"corporation":false,"usgs":true,"family":"Pate","given":"Dale","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":161165,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":9317,"text":"ofr82305 - 1982 - High-resolution seismic-reflection profiles collected aboard R/V GYRE, cruise GYRE 80-G-7A, over the continental slope and upper continental rise, offshore New Jersey","interactions":[],"lastModifiedDate":"2025-09-23T15:36:31.803828","indexId":"ofr82305","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"82-305","title":"High-resolution seismic-reflection profiles collected aboard R/V GYRE, cruise GYRE 80-G-7A, over the continental slope and upper continental rise, offshore New Jersey","docAbstract":"<p>During August 1980, the U.S. Geological Survey (USGS) collected 982 km of single-channel seismic-reflection data on the Continental Slope and upper Rise between Lindenkohl Canyon and Toms Canyon, off New Jersey (fig. 1). The work was conducted aboard R/V GYRE (cruise 80-G-7A). The trackline grid of this cruise extends and supplements a grid of seismic-reflection lines collected by the USGS over this area in 1978 and 1979 (Robb, 1980a, b). These data were collected in cooperation with the Bureau of Land Management (Memorandum of Understanding AA851-MUO-18) to map the geology and the topography of the area in order to identify potential geologic hazards to oil and gas exploration and development. The suite of profiles that was collected includes 40-in3 airgun (recorded as 4-second and 2-second) and 800-J sparker (recorded as 1-second) profiles and 3.5-kHz bathymetry, recorded as 1-second profiles. All times represent two-way travel times. Details of the sources, cables, and instruments, as well as filter settings, are shown in table 1.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr82305","usgsCitation":"Hampson, J., 1982, High-resolution seismic-reflection profiles collected aboard R/V GYRE, cruise GYRE 80-G-7A, over the continental slope and upper continental rise, offshore New Jersey: U.S. Geological Survey Open-File Report 82-305, 4 p., https://doi.org/10.3133/ofr82305.","productDescription":"4 p.","costCenters":[],"links":[{"id":495905,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0305/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":142325,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0305/report-thumb.jpg"}],"country":"United States","state":"New 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