{"pageNumber":"1828","pageRowStart":"45675","pageSize":"25","recordCount":46615,"records":[{"id":1196,"text":"wsp1759D - 1965 - Water resources in the vicinity of municipalities on the central Mesabi Iron Range, northeastern Minnesota","interactions":[{"subject":{"id":52312,"text":"ofr6320 - 1963 - Water resources in the vicinity of municipalities on the Central Mesabi Iron Range, northeastern Minnesota","indexId":"ofr6320","publicationYear":"1963","noYear":false,"title":"Water resources in the vicinity of municipalities on the Central Mesabi Iron Range, northeastern Minnesota"},"predicate":"SUPERSEDED_BY","object":{"id":1196,"text":"wsp1759D - 1965 - Water resources in the vicinity of municipalities on the central Mesabi Iron Range, northeastern Minnesota","indexId":"wsp1759D","publicationYear":"1965","noYear":false,"chapter":"D","title":"Water resources in the vicinity of municipalities on the central Mesabi Iron Range, northeastern Minnesota"},"id":1}],"lastModifiedDate":"2018-03-05T12:35:10","indexId":"wsp1759D","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1965","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1759","chapter":"D","title":"Water resources in the vicinity of municipalities on the central Mesabi Iron Range, northeastern Minnesota","docAbstract":"<p>Additional supplies of water are available near the municipalities on the central Mesabi Iron Range. Ground water presents the greatest potential yield, and most of the productive aquifers are in the Biwabik Iron-Formation and the stratified glacial drift. /k single body of ice-contact stratified drift underlies parts of all but one of the five municipality areas mapped. Surface-water supplies are generally inadequate. The Two River system in the eastern part of the area of this report offers some possibilities. Flow data from one discharge station and one miscellaneous gaging site are presented.</p>\n<p>Analyses of water from many sources are presented as are data from many wells and test holes. Ground water commonly has a concentration of high iron and manganese and is hard. Surface water generally has a high concentration of iron and is colored.</p>","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, DC","doi":"10.3133/wsp1759D","collaboration":"Prepared in cooperation with the Minnesota Department of Iron Range Resources and Rehabilitation","usgsCitation":"Cotter, R.D., Young, H.L., Petri, L.R., and Prior, C.H., 1965, Water resources in the vicinity of municipalities on the central Mesabi Iron Range, northeastern Minnesota: U.S. Geological Survey Water Supply Paper 1759, Document: iv, 20 p.; Plate: 28.5 x 29.5 inches, https://doi.org/10.3133/wsp1759D.","productDescription":"Document: iv, 20 p.; Plate: 28.5 x 29.5 inches","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":392,"text":"Minnesota Water Science Center","active":true,"usgs":true}],"links":[{"id":137955,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1759d/report-thumb.jpg"},{"id":26066,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1759d/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":26067,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1759d/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Minnesota","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -92.925,\n              47.516667\n            ],\n            [\n              -92.925,\n              47.452778\n            ],\n            [\n              -92.833333,\n              47.452778\n            ],\n            [\n              -92.833333,\n              47.425\n            ],\n            [\n              -92.741667,\n              47.425\n            ],\n            [\n              -92.741667,\n              47.46\n            ],\n            [\n              -92.675,\n              47.46\n            ],\n            [\n              -92.675,\n              47.383333\n            ],\n            [\n              -92.583333,\n              47.383333\n            ],\n            [\n              -92.583333,\n              47.566667\n            ],\n            [\n              -92.675,\n              47.566667\n            ],\n            [\n              -92.675,\n              47.53\n            ],\n            [\n              -92.741667,\n              47.53\n            ],\n            [\n              -92.741667,\n              47.516667\n            ],\n            [\n              -92.925,\n              47.516667\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a14e4b07f02db6025b6","contributors":{"authors":[{"text":"Cotter, R. D.","contributorId":89874,"corporation":false,"usgs":true,"family":"Cotter","given":"R.","email":"","middleInitial":"D.","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":143346,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Young, H. L.","contributorId":23922,"corporation":false,"usgs":true,"family":"Young","given":"H.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":143343,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Petri, L. R.","contributorId":48944,"corporation":false,"usgs":true,"family":"Petri","given":"L.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":143344,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Prior, C. H.","contributorId":57827,"corporation":false,"usgs":true,"family":"Prior","given":"C.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":143345,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":52542,"text":"ofr6645 - 1965 - The operation and maintenance of a crest-stage gaging station","interactions":[],"lastModifiedDate":"2016-11-10T16:20:28","indexId":"ofr6645","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1965","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":"66-45","title":"The operation and maintenance of a crest-stage gaging station","docAbstract":"<p>The purpose of this manual is to familiarize field personnel with the procedures involved in operating crest-stage gaging stations. Crest-stage gages are used to determine the elevation of a peak stage occurring at a specific location in a stream.</p>\n<p>A crest-stage gage consists of a length of 14-inch diameter pipe installed in a vertical position in the stream channel (figure 1). The pipe is vented and equipped with an intake system that allows water to enter and leave the pipe as the stream rises and recedes. An equal length of aluminum \"T\" channel (staff) is inserted in the pipe and made to rest on a positive stop called a datum pin. When granulated cork is placed in the gage, the cork will float on the rising stage, then adhere to the staff after the stage recedes. The peak stage is then determined by removing the staff and measuring the distance between the cork line and the lower end of the staff.</p>\n<p>The primary purpose of a crest-stage gaging station is to collect hydrologic data for flood-frequency analyses. Collection of data for such analyses involves operating a network of stations for a period of years until sufficient peak flow data are obtained to accurately define flood-frequency curves. Because carelessness in collecting data at the gage site might result in the loss of an entire year's flood event, the importance of proper operation and maintenance of these gages can not be overemphasized.</p>\n<p>Peak discharges are related to the basin characteristics and major changes in these characteristics must be evaluated. For&euro;st fires, timber harvest, or a new road location that alters the natural drainage of the basin, may effect the intensity and timing of the runoff of the basin.</p>\n<p>Rigid datum controls must be maintained at the gage site throughout the period of record. Physical changes of the site resulting from flood flows or manmade alterations must be evaluated. If a drainage structure such as a culvert is part of the site features, free-flow conditions must be maintained or obstructions carefully documented.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Portland, OR","doi":"10.3133/ofr6645","usgsCitation":"Friday, J., 1965, The operation and maintenance of a crest-stage gaging station: U.S. Geological Survey Open-File Report 66-45, vi, 20 p., https://doi.org/10.3133/ofr6645.","productDescription":"vi, 20 p.","numberOfPages":"28","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":518,"text":"Oregon Water Science Center","active":true,"usgs":true}],"links":[{"id":173959,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr6645.jpg"},{"id":324122,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1966/0045/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a80e4b07f02db64935b","contributors":{"authors":[{"text":"Friday, John","contributorId":19160,"corporation":false,"usgs":true,"family":"Friday","given":"John","email":"","affiliations":[],"preferred":false,"id":245520,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":57734,"text":"ofr65184 - 1965 - Ground-water levels in observation wells in Oklahoma, 1963-64","interactions":[],"lastModifiedDate":"2012-02-02T00:12:13","indexId":"ofr65184","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1965","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":"65-184","title":"Ground-water levels in observation wells in Oklahoma, 1963-64","docAbstract":"The investigation of the ground-water resources of Oklahoma by the U.S. Geological Survey in cooperation with the Oklahoma Water Resources Board includes a continuing program to collect records of water levels in selected observation wells on a systematic basis. These water-level records: (1) provide an index to available ground-water supplies; (2) facilitate the prediction of trends in water levels that will indicate likely changes in storage; (3) aid in the prediction of the base flow of streams; (4) provide information for use in basic research; (5) provide long-time continuous records of fluctuations of water levels in representative wells; and (6) serve as a framework to which other types of hydrologic data my be related.\r\nPrior to 1956, measurements of water levels in observation wells in Oklahoma were included in water-supply papers published annually by the U.S. Geological Survey. Beginning with the 1956 calendar year, however, Geological Survey water-level reports will contain only records of a selected network of observation wells, and will be published at 5-year intervals. The first of this series, for the 1956-59 period was published in 1962.\r\n\r\nThis report has been prepared primarily to present water-level records of wells not included in the Federal network. However, for the sake of completeness it includes water-level records of Federal wells that either have been or will be published in water-supply papers since 1955. This report, which contains water-level records for the 2-year period (1963-64), is the third of a series presenting water-level records for all permanent observations wells in Oklahoma. The first report, published in 1963, contains water-level records for the 5-year period of (1956-60). The second report, published in 1964, contains water-level records for the 2-year period (1961-62.)\r\n\r\n(available as photostat copy only)","language":"ENGLISH","doi":"10.3133/ofr65184","usgsCitation":"Wood, P., 1965, Ground-water levels in observation wells in Oklahoma, 1963-64: U.S. Geological Survey Open-File Report 65-184, 82 p., https://doi.org/10.3133/ofr65184.","productDescription":"82 p.","costCenters":[],"links":[{"id":184448,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa8e4b07f02db66757e","contributors":{"authors":[{"text":"Wood, P.R.","contributorId":102068,"corporation":false,"usgs":true,"family":"Wood","given":"P.R.","email":"","affiliations":[],"preferred":false,"id":257664,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":13702,"text":"ofr6646 - 1965 - Gravity survey in the San Luis Valley area, Colorado","interactions":[],"lastModifiedDate":"2012-02-02T00:06:57","indexId":"ofr6646","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1965","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":"66-46","title":"Gravity survey in the San Luis Valley area, Colorado","docAbstract":"During the summers of 1963 and 1964, a regional gravity survey covering 6,000 square miles of the San Luis Valley and surrounding areas was made to determine subsurface basement configurations and to guide future crustal studies. The San Luis Valley, a large intermontane basin, is a segment of the Rio Grande trough, a reef system characterized by volcanism, normal faulting, and tilted fault blocks. \r\n\r\nThe gravity data, accurate to about 0.5 mgal, were reduced to complete-Bouguer anomaly values. The Bouguer-anomaly gravity map delineates a series of en-echelon gravity highs in the central and western San Luis Valley. These gravity highs are interpreted as horsts of Precambrian rock buried by basin fill. A series of en-echelon gravity lows along the eastern edge of the Valley is interpreted as a graben filled with sedimentary and igneous rock estimated to be up to 30,000 ft thick. The relatively high regional gravity over the Sangre de Cristo Mountains suggests that these mountains are locally uncompensated. A subcircular gravity low in the Bonanza area is interpreted as an indication of low-density volcanic rocks within a caldera structure.","language":"ENGLISH","publisher":"U.S. Geological Survey],","doi":"10.3133/ofr6646","usgsCitation":"Gaca, J.R., and Karig, D.E., 1965, Gravity survey in the San Luis Valley area, Colorado: U.S. Geological Survey Open-File Report 66-46, 21 p. ill., maps ;30 cm., https://doi.org/10.3133/ofr6646.","productDescription":"21 p. ill., maps ;30 cm.","costCenters":[],"links":[{"id":106376,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_8136.htm","linkFileType":{"id":5,"text":"html"},"description":"8136"},{"id":146838,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1966/0046/report-thumb.jpg"},{"id":42258,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1966/0046/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":42259,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1966/0046/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":42260,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1966/0046/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":42261,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1966/0046/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":42262,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1966/0046/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":42263,"rank":405,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1966/0046/plate-6.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":42264,"rank":406,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1966/0046/plate-7.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":42265,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1966/0046/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4abae4b07f02db671ff7","contributors":{"authors":[{"text":"Gaca, J. Robert","contributorId":23959,"corporation":false,"usgs":true,"family":"Gaca","given":"J.","email":"","middleInitial":"Robert","affiliations":[],"preferred":false,"id":168260,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Karig, Daniel E.","contributorId":98739,"corporation":false,"usgs":true,"family":"Karig","given":"Daniel","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":168261,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":64106,"text":"gp467 - 1965 - Aeromagnetic map of parts of Marquette, Dickinson, Baraga, Alger, and Schoolcraft Counties, Michigan, and its geologic interpretation","interactions":[{"subject":{"id":41753,"text":"ofr647 - 1964 - Aeromagnetic map of parts of Marquette, Dickinson, Baraga, Alger, and Schoolcraft Counties, Michigan","indexId":"ofr647","publicationYear":"1964","noYear":false,"title":"Aeromagnetic map of parts of Marquette, Dickinson, Baraga, Alger, and Schoolcraft Counties, Michigan"},"predicate":"SUPERSEDED_BY","object":{"id":64106,"text":"gp467 - 1965 - Aeromagnetic map of parts of Marquette, Dickinson, Baraga, Alger, and Schoolcraft Counties, Michigan, and its geologic interpretation","indexId":"gp467","publicationYear":"1965","noYear":false,"title":"Aeromagnetic map of parts of Marquette, Dickinson, Baraga, Alger, and Schoolcraft Counties, Michigan, and its geologic interpretation"},"id":1}],"lastModifiedDate":"2016-09-09T15:44:41","indexId":"gp467","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1965","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":317,"text":"Geophysical Investigations Map","code":"GP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"467","title":"Aeromagnetic map of parts of Marquette, Dickinson, Baraga, Alger, and Schoolcraft Counties, Michigan, and its geologic interpretation","docAbstract":"<p>The U. S. Geological Survey, in cooperation with the Geological Survey Division of the Michigan Department of Conservation, is conducting a comprehensive restudy of the iron-bearing districts of Michigan. The use of aeromagnetic data is one of the fastest and most reliable methods for outlining the areal distribution of magnetic iron-formation and thus is of material value in assessing the iron resources of the United States. As part of this program of restudy, aeromagnetic surveys of approximately 4,500 square miles of the Northern Peninsula have been made. The results of several of these surveys have been presented by Balsley and others (1949) and by Wier and others (.1953). This report is about a survey made in 1950, over an area of about 1,400 square miles in Marquette County and ad-· joining strips in northern Dickinson and northeastern Baraga Counties, and a later survey flown in 1961, over about 500 square miles in parts of Marquette, Alger, and Schoolcraft Counties. The Marquette iron range extends in an east-west direction across approximately the west-central part of the area, and iron districts of lesser importance are located at Republic, in the southwestern part of the area, and near Gwinn, in the south -central part of the area.</p><p>Aeromagnetic surveys were flown along north-south lines spaced at intervals of one-quarter mile in the western part of the area and at intervals of from about 1 to 3 miles in the eastern part. Lines were flown at approximately 500 feet above the surface or at elevations of 1,100 to 2,400 feet above sea level. The flight path of the aircraft was recorded by a gyrostabilized continuous-strip camera, and elevation was continuously recorded by a radio altimeter. Magnetic measurements were made by an AN/ASQ-3A fluxgate magnetometer. Compilation of aeromagnetic data was by standard methods, described by Balsley ( 1952 ), under the supervision of John Kirby and Frank Petrafeso. The aeromagnetic contours are relative to an arbitrary datum.</p><p>Magnetic properties of rocks were measured by W. E. Huff.</p><p>At the time the earlier aeromagnetic survey was flown, the only base maps available were planimetric maps such as the Helena NW quadrangle and county road maps. Small errors, therefore, may exist in the location of flight lines and specific aeromagnetic a nomalies.</p><p>The major magnetic anomalies and broad areas that have characteristic magnetic patterns are correlated herein with geology as determined from published reports and from mapping done since 1957 by the U. S. Geological Survey in the eastern part of the Marquette iron range. The geology north of the Marquette iron range and west of the line between R. 25 W. and R. 26 W. is based mainly on a compilation made by Robert Reed of the Geological Survey Division of the Michigan Department of Conservation from data in the files of the State Survey. In addition some aeromagnetic features have been checked by ground magnetometer in selected localities and correlated directly with the rock types. A few oriented samples have been collected for measurement of the magnetic properties of the major rock units, but many hundreds or thousands of samples would be required to obtain a full range of values of the magnetic susceptibility and remanent magnetization of the rocks over such a large area.</p><p>Although the geology of much of the area is still imperfectly known, the available aeromagnetic data together with the best obtainable geologic data are presented at this time, rather than awaiting the eventual extension or completion of the present mapping program, because the combined data provide much information on the extent and location of magnetic iron-formation and other major rock units where concealed beneath glacial, vegetative, and alluvial cover.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Washington, D.C.","doi":"10.3133/gp467","collaboration":"Prepared in cooperation with the Michigan Department of Conservation Geological Survey Division","usgsCitation":"Case, J.E., and Gair, J., 1965, Aeromagnetic map of parts of Marquette, Dickinson, Baraga, Alger, and Schoolcraft Counties, Michigan, and its geologic interpretation: U.S. Geological Survey Geophysical Investigations Map 467, Document: 10 p.; 3 Plates: 48.50 x 43.26 inches or smaller, https://doi.org/10.3133/gp467.","productDescription":"Document: 10 p.; 3 Plates: 48.50 x 43.26 inches or smaller","costCenters":[{"id":382,"text":"Michigan Water Science Center","active":true,"usgs":true}],"links":[{"id":250551,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/gp/0467/plate-1.pdf","size":"22930","linkFileType":{"id":1,"text":"pdf"}},{"id":250550,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gp/0467/report.pdf","size":"1068","linkFileType":{"id":1,"text":"pdf"}},{"id":250552,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/gp/0467/plate-2.pdf","size":"10448","linkFileType":{"id":1,"text":"pdf"}},{"id":250553,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/gp/0467/plate-3.pdf","size":"14970","linkFileType":{"id":1,"text":"pdf"}},{"id":253995,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gp/0467/report-thumb.jpg"}],"scale":"62500","country":"United States","state":"Michigan","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -88.166667,\n              46.916667\n            ],\n            [\n              -87.5,\n              46.916667\n            ],\n            [\n              -87.5,\n              46.625\n            ],\n            [\n              -87.375,\n              46.625\n            ],\n            [\n              -87.375,\n              46.666667\n            ],\n            [\n              -86.416667,\n              46.666667\n            ],\n            [\n              -86.416667,\n              46.25\n            ],\n            [\n              -87.375,\n              46.25\n            ],\n            [\n              -87.375,\n              46.125\n            ],\n            [\n              -87.5,\n              46.125\n            ],\n            [\n              -87.5,\n              46.083333\n            ],\n            [\n              -88.166667,\n              46.083333\n            ],\n            [\n              -88.166667,\n              46.916667\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afee4b07f02db6976fc","contributors":{"authors":[{"text":"Case, J. E.","contributorId":56625,"corporation":false,"usgs":true,"family":"Case","given":"J.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":269960,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Gair, J. E.","contributorId":50891,"corporation":false,"usgs":true,"family":"Gair","given":"J. E.","affiliations":[],"preferred":false,"id":269959,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":6378,"text":"pp498B - 1965 - Variations in chemical character of water in the Englishtown Formation, New Jersey","interactions":[{"subject":{"id":52280,"text":"ofr62123 - 1962 - Variations in the chemical character of the water in the Englishtown formation, New Jersey","indexId":"ofr62123","publicationYear":"1962","noYear":false,"title":"Variations in the chemical character of the water in the Englishtown formation, New Jersey"},"predicate":"SUPERSEDED_BY","object":{"id":6378,"text":"pp498B - 1965 - Variations in chemical character of water in the Englishtown Formation, New Jersey","indexId":"pp498B","publicationYear":"1965","noYear":false,"chapter":"B","title":"Variations in chemical character of water in the Englishtown Formation, New Jersey"},"id":1}],"lastModifiedDate":"2017-03-15T12:57:36","indexId":"pp498B","displayToPublicDate":"1992-01-01T08:00:00","publicationYear":"1965","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":"498","chapter":"B","title":"Variations in chemical character of water in the Englishtown Formation, New Jersey","docAbstract":"<p>This investigation describes the variations in the chemical character of the water in the Englishtown Formation of Late Cretaceous age in the Atlantic Coastal Plain of New Jersey, and demonstrates the application of the concept of hydrochemical mapping to the study and evaluation of water-bearing materials.&nbsp;The chemistry of ground water is responsive to the physical environment and lends support to available geologic and hydrologic data. A study of the ground-water chemistry may even suggest concepts for which additional geologic or hydrologic data may not be obtainable by conventional methods of study. Hydrochemical mapping is particularly important in evaluating an aquifer satisfactorily, but it could be equally useful in regional geologic studies concerned with continuity of units or mineralogic differences and similarities.</p>","largerWorkTitle":"Hydrology of aquifer systems","language":"English","publisher":"U.S. Government Printing Office","doi":"10.3133/pp498B","collaboration":"Prepared in cooperation with New Jersey Division of Water Policy and Supply","usgsCitation":"Seaber, P.R., 1965, Variations in chemical character of water in the Englishtown Formation, New Jersey: U.S. Geological Survey Professional Paper 498, iii, p. B1-B35, https://doi.org/10.3133/pp498B.","productDescription":"iii, p. B1-B35","costCenters":[],"links":[{"id":33751,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0498b/report.pdf","text":"Report","size":"5.30 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Report"},{"id":121598,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0498b/report-thumb.jpg"}],"country":"United States","state":"New Jersey","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -74.28955078125,\n              40.50753459933616\n            ],\n            [\n              -74.72351074218749,\n              40.13899044275822\n            ],\n            [\n              -75.1519775390625,\n              39.882342585755744\n            ],\n            [\n              -75.3497314453125,\n              39.806426117299374\n            ],\n            [\n              -75.44860839843749,\n              39.688167045890395\n            ],\n            [\n              -75.42938232421875,\n              39.58029027440865\n            ],\n            [\n              -75.3826904296875,\n              39.56970506644249\n            ],\n            [\n              -74.11651611328125,\n              39.816975090490004\n            ],\n            [\n              -74.05334472656249,\n              39.87391156801293\n            ],\n            [\n              -74.0093994140625,\n              40.134790883048524\n            ],\n            [\n              -73.97918701171875,\n              40.361195540839\n            ],\n            [\n              -73.99566650390625,\n              40.40094763151963\n            ],\n            [\n              -74.058837890625,\n              40.44276659332215\n            ],\n            [\n              -74.15496826171874,\n              40.478292268560175\n            ],\n            [\n              -74.28955078125,\n              40.50753459933616\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a14e4b07f02db602af9","contributors":{"authors":[{"text":"Seaber, Paul R.","contributorId":67492,"corporation":false,"usgs":true,"family":"Seaber","given":"Paul","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":152609,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70112256,"text":"70112256 - 1965 - Resource understanding: a challenge to aerial methods","interactions":[],"lastModifiedDate":"2017-03-27T13:42:24","indexId":"70112256","displayToPublicDate":"1990-06-12T10:05:00","publicationYear":"1965","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3051,"text":"Photogrammetric Engineering","active":true,"publicationSubtype":{"id":10}},"title":"Resource understanding: a challenge to aerial methods","docAbstract":"<p>Aerial survey methods are speeding acquisition of survey data needed to provide and manage the nation's resources. These methods have been applied to topographic mapping for a number of years and the record clearly shows their advantages in terms of cost and speed in contrast to the ground methods that have been historically employed. Limited use is now being made of aerial methods to assist cadastral surveys, in location, acquisition and development of National Parks, in mapping the geology of the nation, in locating and developing water resources, and in surveys of the oceans. It is the purpose of this paper to call attention to these uses and to encourage the scientific community to further refine aerial methods so that their use may be increased and the veracity of data improved.</p>","language":"English","publisher":"American Society of Photogrammetry","publisherLocation":"Falls Church, VA","usgsCitation":"Udall, S.L., 1965, Resource understanding: a challenge to aerial methods: Photogrammetric Engineering, v. 31, no. 1, p. 63-75.","productDescription":"13 p.","startPage":"63","endPage":"75","numberOfPages":"13","costCenters":[{"id":222,"text":"Earth Resources Observation and Science (EROS) Center","active":true,"usgs":true}],"links":[{"id":288447,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ 173.0,16.916667 ], [ 173.0,71.833333 ], [ -66.95,71.833333 ], [ -66.95,16.916667 ], [ 173.0,16.916667 ] ] ] } } ] }","volume":"31","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"539acc13e4b0e83db6d08fdb","contributors":{"authors":[{"text":"Udall, Stewart L.","contributorId":9968,"corporation":false,"usgs":true,"family":"Udall","given":"Stewart","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":494583,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70106998,"text":"70106998 - 1965 - Water resources data for Indiana, 1965","interactions":[],"lastModifiedDate":"2014-06-02T06:09:13","indexId":"70106998","displayToPublicDate":"1966-01-01T14:16:00","publicationYear":"1965","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":"IN-65-1","title":"Water resources data for Indiana, 1965","docAbstract":"<p>The surface-water records for the 1965 water year for gaging stations, partial-record stations, and miscellaneous sites within the State of Indiana are given in this report. For convenience there are also included records for a few pertinent gaging stations in bordering States. The records were collected and computed by the Water Resources Division of the U.S. Geological Survey, under the direction of Malcolm D. Hale, district engineer, Surface Water Branch.</p>\n<br/>\n<p>This report marks the beginning of a new method of presenting, annually, basic data on surface-water records by States. Through September 30, 1960, the records of discharge and stage of streams and contents and stage of lakes or reservoirs were published in an annual series of U.S. Geological Survey water-supply papers entitled \"Surface Water Supply of the United States.\" Since 1951 there have been 20 volumes in the series; each volume covered an area whose boundaries coincided with those of certain natural drainage areas. The records in Indiana were contained in Parts 3A, 4 and 5 of that series.</p>\n<br/>\n<p>Beginning with the 1961 water year, streamflow records and related data will be released by the Geological Survey in annual reports on a State-boundary basis. Distribution of these basic-data reports will be limited and primarily for local needs. The records later will be published in Geological Survey water-supply papers at 5-year intervals. These 5-year water-supply papers will show daily discharge and will be compiled on the same geographical areas previously used for the annual series; however, some of the 14 parts of coterminous United States will be further subdivided.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/70106998","collaboration":"Prepared in cooperation with Indiana Department of Natural Resources; Indiana State Board of Health; Indiana State Highway Commission; Corps of Engineers, U.S. Army","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1965, Water resources data for Indiana, 1965: U.S. Geological Survey Water Data Report IN-65-1, viii, 249 p., https://doi.org/10.3133/70106998.","productDescription":"viii, 249 p.","numberOfPages":"258","temporalStart":"1964-10-01","temporalEnd":"1965-09-30","costCenters":[{"id":629,"text":"Water Resources Division","active":false,"usgs":true}],"links":[{"id":287928,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":287927,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/unnumbered/70106998/report.pdf"}],"country":"United States","state":"Indiana","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -88.0979,37.7717 ], [ -88.0979,41.7607 ], [ -84.7847,41.7607 ], [ -84.7847,37.7717 ], [ -88.0979,37.7717 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"537b280de4b0929ba496abd5","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":535655,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70010461,"text":"70010461 - 1965 - Titanium dioxide in pyroclastic layers from volcanoes in the Cascade Range","interactions":[],"lastModifiedDate":"2026-02-10T17:59:26.40999","indexId":"70010461","displayToPublicDate":"1965-11-19T00:00:00","publicationYear":"1965","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3338,"text":"Science","active":true,"publicationSubtype":{"id":10}},"title":"Titanium dioxide in pyroclastic layers from volcanoes in the Cascade Range","docAbstract":"<p><span>Rapid determinations of titanium dioxide have been made by x-ray emission techniques to evaluate the potentiality of using the TiO</span><sub>2</sub><span>&nbsp;content of samples for checking field correlations and assisting in identification of pyroclastic units from Cascade volcanoes. Preliminary data suggest that the two most widespread units have characteristic ranges of TiO</span><sub>2</sub><span>&nbsp;content and that other, less extensive layers have ranges which, though characteristic, often overlap the ranges of the more widespread layers. Relative to fresh samples, weathered samples from B and C soil horizons are enriched in TiO</span><sub>2</sub><span>.</span></p>","language":"English","publisher":"American Association for the Advancement of Science","doi":"10.1126/science.150.3699.1022","issn":"00368075","usgsCitation":"Czamanske, G., and Porter, S., 1965, Titanium dioxide in pyroclastic layers from volcanoes in the Cascade Range: Science, v. 150, no. 3699, p. 1022-1025, https://doi.org/10.1126/science.150.3699.1022.","productDescription":"4 p.","startPage":"1022","endPage":"1025","costCenters":[],"links":[{"id":218952,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","otherGeospatial":"Cascade Range","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -126.3113698578322,\n              49.01003876424767\n            ],\n            [\n              -126.3113698578322,\n              38.60286391280661\n            ],\n            [\n              -121.31055440730346,\n              38.60286391280661\n            ],\n            [\n              -121.31055440730346,\n              49.01003876424767\n            ],\n            [\n              -126.3113698578322,\n              49.01003876424767\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","volume":"150","issue":"3699","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bb423e4b08c986b3261e0","contributors":{"authors":[{"text":"Czamanske, G.K.","contributorId":26300,"corporation":false,"usgs":true,"family":"Czamanske","given":"G.K.","email":"","affiliations":[],"preferred":false,"id":358975,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Porter, S.C.","contributorId":35066,"corporation":false,"usgs":true,"family":"Porter","given":"S.C.","email":"","affiliations":[],"preferred":false,"id":358976,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70221204,"text":"70221204 - 1965 - The drill‐stem test: The petroleum industry's deep‐well pumping test","interactions":[],"lastModifiedDate":"2021-06-04T21:44:46.914029","indexId":"70221204","displayToPublicDate":"1965-07-01T16:42:04","publicationYear":"1965","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3825,"text":"Groundwater","active":true,"publicationSubtype":{"id":10}},"title":"The drill‐stem test: The petroleum industry's deep‐well pumping test","docAbstract":"<p>Drill‐stem<span>&nbsp;tests provide the&nbsp;</span>petroleum<span>&nbsp;</span>industry<span>&nbsp;information on three critical properties of subsurface formations —pressure head, permeability, and water chemistry –that the ground‐water hydrologist also seeks in making&nbsp;</span>pumping<span>&nbsp;tests of water wells. As it is increasingly necessary to study the hydraulic and geochemical properties of&nbsp;</span>deep<span>‐lying rocks in order to understand the behavior of ground water, data on&nbsp;</span>drill‐stem<span>&nbsp;tests made by the&nbsp;</span>petroleum<span>&nbsp;</span>industry<span>&nbsp;become an important source of information which otherwise is unobtainable because of the high cost. Data from these tests made by methods currently in use are highly useful in water studies. An obvious conclusion is that both&nbsp;</span>petroleum<span>&nbsp;engineering and ground‐water hydrology stand to profit substantially from an increase in the interchange of ideas and techniques.</span></p>","language":"English","publisher":"Wiley Blackwell","doi":"10.1111/j.1745-6584.1965.tb01218.x","usgsCitation":"Bredehoeft, J., 1965, The drill‐stem test: The petroleum industry's deep‐well pumping test: Groundwater, v. 3, no. 3, p. 31-36, https://doi.org/10.1111/j.1745-6584.1965.tb01218.x.","productDescription":"6 p.","startPage":"31","endPage":"36","costCenters":[],"links":[{"id":386249,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"3","issue":"3","noUsgsAuthors":false,"publicationDate":"2006-07-06","publicationStatus":"PW","contributors":{"authors":[{"text":"Bredehoeft, J.D.","contributorId":12836,"corporation":false,"usgs":true,"family":"Bredehoeft","given":"J.D.","affiliations":[],"preferred":false,"id":817044,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70221190,"text":"70221190 - 1965 - Gamma-ray spectrometer studies of hydro-thermally altered rocks","interactions":[],"lastModifiedDate":"2021-06-04T18:58:38.973435","indexId":"70221190","displayToPublicDate":"1965-06-01T13:55:22","publicationYear":"1965","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1472,"text":"Economic Geology","active":true,"publicationSubtype":{"id":10}},"title":"Gamma-ray spectrometer studies of hydro-thermally altered rocks","docAbstract":"<p><span>The uranium, thorium, and potassium content of hydrothermally&nbsp;</span>altered<span>&nbsp;</span>rocks<span>&nbsp;in the vicinity of several copper and copper-lead-zinc deposits in Arizona was determined by chemical analysis. Potassium in the more intensely&nbsp;</span>altered<span>&nbsp;zones is about twice that in unaltered areas. There is no corresponding increase in thorium, so a higher potassium/thorium ratio also results from alteration; abnormally high uranium, locally in secular disequilibrium, was observed at the Bagdad porphyry copper deposit. A truck-mounted gammarray&nbsp;</span>spectrometer<span>&nbsp;was used to obtain a spectrum of&nbsp;</span>gamma<span>&nbsp;emission at each sample location. Equating the spectrometric with the chemical data gave standard errors of 0.6 percent potassium, 3 ppm thorium, and 10 ppm uranium for the outcrop analyses with the&nbsp;</span>spectrometer<span>. The amount of potassium introduced by hydrothermal alteration is thought sufficient in quantity to be detected by either surface or aerial spectrometry; spectrometric detection of anomalous uranium is probably marginal, owing to the disequilibrium. The potassium/thorium ratio may provide a means of distinguishing, in such surveys, between hydrothermally&nbsp;</span>altered<span>&nbsp;high-potassium zones and unaltered extrinsically high-potassium intrusives.&nbsp;</span></p>","language":"English","publisher":"Society of Economic Geologists","doi":"10.2113/gsecongeo.60.4.653","usgsCitation":"Moxham, R., Foote, R., and Bunker, C.M., 1965, Gamma-ray spectrometer studies of hydro-thermally altered rocks: Economic Geology, v. 60, no. 4, p. 653-671, https://doi.org/10.2113/gsecongeo.60.4.653.","productDescription":"19 p.","startPage":"653","endPage":"671","costCenters":[],"links":[{"id":386235,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"60","issue":"4","noUsgsAuthors":false,"publicationDate":"1965-06-01","publicationStatus":"PW","contributors":{"authors":[{"text":"Moxham, R.M.","contributorId":42234,"corporation":false,"usgs":true,"family":"Moxham","given":"R.M.","email":"","affiliations":[],"preferred":false,"id":817022,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Foote, R.S.","contributorId":259302,"corporation":false,"usgs":false,"family":"Foote","given":"R.S.","email":"","affiliations":[],"preferred":false,"id":817023,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Bunker, C. M.","contributorId":75138,"corporation":false,"usgs":true,"family":"Bunker","given":"C.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":817024,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70221195,"text":"70221195 - 1965 - Geology and biology of the sea floor as deduced from simulaneous photographs and samples","interactions":[],"lastModifiedDate":"2021-06-04T20:30:18.324547","indexId":"70221195","displayToPublicDate":"1965-04-01T15:26:14","publicationYear":"1965","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2620,"text":"Limnology and Oceanography","active":true,"publicationSubtype":{"id":10}},"title":"Geology and biology of the sea floor as deduced from simulaneous photographs and samples","docAbstract":"<p>During 1963, 260 paired photographs and large bottom samples were taken on the continental shelf and slope off northeastern United States. The photographs revealed surface characteristics of the sediments and natural attitudes of benthic animals; the samples retrieved specimens for geological and biological examination and identification.</p><p>Samples are the best source materials for making textural studies of sediments consisting mostly of sand, silt, or clay, but photographs are better than samples for bottoms too bouldery for proper sampling. Ripple marks and other surface irregularities revealed by the photographs supplement textural studies of the samples in deducing effects of wave movements and currents upon bottom materials.</p><p>For biological studies, the photographs yield much information on relationships of the benthic fauna to bottom materials, but they fail to provide useful data on biomasses. Biomasses and accurate taxonomic identifications are far better made upon samples. Thus, a combination of photographs and accompanying samples provides maximum information for biological as well as geological purposes.</p>","language":"English","publisher":"Association for the Sciences of Limnology and Oceanography","doi":"10.4319/lo.1965.10.1.0001","usgsCitation":"Emery, K., Merrill, A., and Trumbull, J.V., 1965, Geology and biology of the sea floor as deduced from simulaneous photographs and samples: Limnology and Oceanography, v. 10, no. 1, p. 1-21, https://doi.org/10.4319/lo.1965.10.1.0001.","productDescription":"21 p.","startPage":"1","endPage":"21","costCenters":[],"links":[{"id":480357,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.4319/lo.1965.10.1.0001","text":"Publisher Index Page"},{"id":386240,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"10","issue":"1","noUsgsAuthors":false,"publicationDate":"2003-12-22","publicationStatus":"PW","contributors":{"authors":[{"text":"Emery, K.O.","contributorId":67865,"corporation":false,"usgs":true,"family":"Emery","given":"K.O.","email":"","affiliations":[],"preferred":false,"id":817031,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Merrill, A.S.","contributorId":36676,"corporation":false,"usgs":true,"family":"Merrill","given":"A.S.","email":"","affiliations":[],"preferred":false,"id":817032,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Trumbull, James V. A.","contributorId":8457,"corporation":false,"usgs":true,"family":"Trumbull","given":"James","email":"","middleInitial":"V. A.","affiliations":[],"preferred":false,"id":817033,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70207282,"text":"70207282 - 1965 - Relation of carbon 14 concentrations to saline water contamination of coastal aquifers","interactions":[],"lastModifiedDate":"2019-12-17T07:00:43","indexId":"70207282","displayToPublicDate":"1965-03-31T16:24:40","publicationYear":"1965","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3721,"text":"Water Resources Management","onlineIssn":"1573-1650","printIssn":"0920-4741","active":true,"publicationSubtype":{"id":10}},"title":"Relation of carbon 14 concentrations to saline water contamination of coastal aquifers","docAbstract":"<p><span>Naturally occurring stable or radioactive isotopes may be used in some places to identify the origin of saline water that contaminates some coastal aquifers. In a recent study to determine the origin of saline water in the Ocala Limestone aquifer near Brunswick, Georgia, the following sources were analyzed for C</span><sup>14</sup><span>&nbsp;and deuterium concentrations: potable water from the Ocala Limestone, contaminated water from the Ocala Limestone, saune water from the underlying Claiborne Group, and nearby ocean water. The chloride concentration of the groundwater ranges from about 25 ppm in the potable water to more than 2000 ppm in the deeper part of the Claiborne Group. From an interpretation of piezometric maps and other hydrologic data, previous investigators had concluded that the source of the contaminating water was the Claiborne Group and not the nearby ocean. The essentially uniform range of low values of −965 to −987‰ of the modern standard (National Bureau Standard C</span><sup>14</sup><span>&nbsp;oxalic acid) for the C</span><sup>14</sup><span>&nbsp;activity of the groundwater samples (regardless of the degree of contamination) is in agreement with this conclusion. If recent ocean water, which had a C</span><sup>14</sup><span>&nbsp;value of +285‰, were the source of contamination, the contaminated water would have had a C</span><sup>14</sup><span>&nbsp;activity higher than the activity of the fresh water. Deuterium analyses are not inconsistent with the interpretation that water from the Claiborne Group, rather than recent ocean water, is the source of the contaminating water. The concurrence of the hydrologic and the isotopic data in this area where the hydrology is well known suggests that isotopic analysis may be used to identify the origin of water in different portions of a hydrologic environment.&nbsp;</span></p>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/WR001i001p00109","issn":"00431397","usgsCitation":"Hanshaw, B., Back, W., Rubin, M., and Wait, R.L., 1965, Relation of carbon 14 concentrations to saline water contamination of coastal aquifers: Water Resources Management, v. 1, no. 1, p. 109-114, https://doi.org/10.1029/WR001i001p00109.","productDescription":"6 p. ","startPage":"109","endPage":"114","costCenters":[],"links":[{"id":370289,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Georgia","county":"Glynn County","city":"Brunswick","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -81.73828125,\n              30.92107637538488\n            ],\n            [\n              -81.221923828125,\n              30.92107637538488\n            ],\n            [\n              -81.221923828125,\n              31.39115752282472\n            ],\n            [\n              -81.73828125,\n              31.39115752282472\n            ],\n            [\n              -81.73828125,\n              30.92107637538488\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"1","issue":"1","noUsgsAuthors":false,"publicationDate":"2010-07-09","publicationStatus":"PW","contributors":{"authors":[{"text":"Hanshaw, B.B.","contributorId":25928,"corporation":false,"usgs":true,"family":"Hanshaw","given":"B.B.","email":"","affiliations":[],"preferred":false,"id":777532,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Back, W.","contributorId":33839,"corporation":false,"usgs":true,"family":"Back","given":"W.","email":"","affiliations":[],"preferred":false,"id":777533,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Rubin, Meyer","contributorId":107283,"corporation":false,"usgs":true,"family":"Rubin","given":"Meyer","email":"","affiliations":[],"preferred":false,"id":777690,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Wait, Robert L.","contributorId":12839,"corporation":false,"usgs":true,"family":"Wait","given":"Robert","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":777691,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":877,"text":"877 - 1965 - Water resources data for Utah","interactions":[],"lastModifiedDate":"2014-08-05T16:42:43","indexId":"877","displayToPublicDate":"1965-01-01T16:41:27","publicationYear":"1965","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"title":"Water resources data for Utah","docAbstract":"No abstract available.","language":"English","publisher":"U.S. Department of the Interior","publisherLocation":"Salt Lake City, UT","doi":"10.3133/877","issn":"0360-1633","collaboration":"Prepared in cooperation with the state of Utah and with other agencies.","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1965, Water resources data for Utah, https://doi.org/10.3133/877.","costCenters":[],"links":[{"id":291738,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"country":"United States","state":"Utah","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -114.05,37.0 ], [ -114.05,42.0 ], [ -109.04,42.0 ], [ -109.04,37.0 ], [ -114.05,37.0 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53e1eff1e4b0fe532be2df63","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":527796,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70221200,"text":"70221200 - 1965 - Earthquake magnitudes from hydroseismic data","interactions":[],"lastModifiedDate":"2021-06-04T21:23:32.190063","indexId":"70221200","displayToPublicDate":"1965-01-01T16:20:46","publicationYear":"1965","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3825,"text":"Groundwater","active":true,"publicationSubtype":{"id":10}},"title":"Earthquake magnitudes from hydroseismic data","docAbstract":"<p><span>If earthquakes are recorded on your water‐level charts, you can make your own estimate of&nbsp;</span>earthquake<span>&nbsp;</span>magnitudes<span>! As an aid in doing this, this paper presents two graphs: one to calculate distance from well to&nbsp;</span>earthquake<span>&nbsp;epicenter; the other, a nomogram from which to read&nbsp;</span>hydroseismic<span>&nbsp;</span>magnitude<span>&nbsp;plus log C. Examples given show (1) direct computation of m</span><sub>s</sub><span>+ log C, (2) use of aftershocks to estimate total water‐level fluctuation caused by a major&nbsp;</span>earthquake<span>&nbsp;(when the recorder drum has spun around or when reversals cover up the record), and (3) how to determine if aftershocks theoretically should have been recorded.&nbsp;</span>Hydroseismic<span>&nbsp;</span>magnitude<span>&nbsp;is the surface‐wave&nbsp;</span>magnitude<span>&nbsp;(M</span><sub>s</sub><span>) calculated from seismically induced water‐level fluctuations in wells. As yet it must be computed indirectly from m</span><sub>s</sub><span>+ log C but because log C is a variable the result is only approximate. Log C is believed to represent a resultant controlled by magnification, period of the surface waves, instrumental frictions, well lag, and resonance if the well is underdamped.&nbsp;</span></p>","language":"English","publisher":"NGWA The Groundwater Association","doi":"10.1111/j.1745-6584.1965.tb01196.x","usgsCitation":"Vorhis, R., 1965, Earthquake magnitudes from hydroseismic data: Groundwater, v. 3, no. 1, p. 12-20, https://doi.org/10.1111/j.1745-6584.1965.tb01196.x.","productDescription":"9 p.","startPage":"12","endPage":"20","costCenters":[],"links":[{"id":386245,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"3","issue":"1","noUsgsAuthors":false,"publicationDate":"2006-07-06","publicationStatus":"PW","contributors":{"authors":[{"text":"Vorhis, R.C.","contributorId":32512,"corporation":false,"usgs":true,"family":"Vorhis","given":"R.C.","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":817039,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":880,"text":"880 - 1965 - Water resources data for West Virginia","interactions":[],"lastModifiedDate":"2014-08-05T15:37:29","indexId":"880","displayToPublicDate":"1965-01-01T15:35:39","publicationYear":"1965","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"title":"Water resources data for West Virginia","docAbstract":"No abstract available.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Charleston, WV","doi":"10.3133/880","issn":"0364-4421","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1965, Water resources data for West Virginia, https://doi.org/10.3133/880.","costCenters":[],"links":[{"id":291732,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"country":"United States","state":"West Virginia","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -82.64,37.2 ], [ -82.64,40.64 ], [ -77.72,40.64 ], [ -77.72,37.2 ], [ -82.64,37.2 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53e1eff5e4b0fe532be2df7a","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":527799,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":881,"text":"881 - 1965 - Water resources data for Wisconsin","interactions":[],"lastModifiedDate":"2014-08-05T15:29:22","indexId":"881","displayToPublicDate":"1965-01-01T15:27:19","publicationYear":"1965","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"title":"Water resources data for Wisconsin","docAbstract":"No abstract available.","language":"English","publisher":"U.S. Department of the Interior","publisherLocation":"Madison, WI","doi":"10.3133/881","issn":"0740-8803","collaboration":"Prepared in cooperation with the State of Wisconsin and other agencies.","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1965, Water resources data for Wisconsin, https://doi.org/10.3133/881.","costCenters":[],"links":[{"id":291731,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"country":"United States","state":"Wisconsin","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -92.89,42.49 ], [ -92.89,47.08 ], [ -86.76,47.08 ], [ -86.76,42.49 ], [ -92.89,42.49 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53e1eff6e4b0fe532be2df80","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":527800,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":882,"text":"882 - 1965 - Water resources data for Wyoming","interactions":[],"lastModifiedDate":"2014-08-04T14:23:17","indexId":"882","displayToPublicDate":"1965-01-01T14:21:59","publicationYear":"1965","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"title":"Water resources data for Wyoming","docAbstract":"No abstract available.","language":"English","publisher":"U.S. Department of the Interior","publisherLocation":"Cheyenne, WY","doi":"10.3133/882","issn":"0364-3565","collaboration":"Prepared in cooperation with the State of Wyoming and other agencies.","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1965, Water resources data for Wyoming, https://doi.org/10.3133/882.","costCenters":[],"links":[{"id":291629,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"country":"United States","state":"Wyoming","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -111.0569,40.9947 ], [ -111.0569,45.0059 ], [ -104.0522,45.0059 ], [ -104.0522,40.9947 ], [ -111.0569,40.9947 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53e09e61e4b0beb42bdca4e1","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":527801,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":834,"text":"834 - 1965 - Water resources data for Alabama","interactions":[],"lastModifiedDate":"2014-08-05T14:10:35","indexId":"834","displayToPublicDate":"1965-01-01T14:06:17","publicationYear":"1965","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"title":"Water resources data for Alabama","docAbstract":"No abstract available.","language":"English","publisher":"Water Resources Division, U.S. Geological Survey","publisherLocation":"University, AL","doi":"10.3133/834","issn":"0364-4316","collaboration":"Prepared in cooperation with the State of Alabama and other agencies.","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1965, Water resources data for Alabama, https://doi.org/10.3133/834.","costCenters":[],"links":[{"id":291718,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"country":"United States","state":"Alabama","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -88.4732,30.1941 ], [ -88.4732,35.0079 ], [ -84.8882,35.0079 ], [ -84.8882,30.1941 ], [ -88.4732,30.1941 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53e1efe1e4b0fe532be2dea5","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":527753,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":837,"text":"837 - 1965 - Water resources data for Arkansas","interactions":[],"lastModifiedDate":"2014-08-05T13:57:22","indexId":"837","displayToPublicDate":"1965-01-01T13:56:06","publicationYear":"1965","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"title":"Water resources data for Arkansas","docAbstract":"No abstract available.","language":"English","publisher":"U.S. Department of the Interior","publisherLocation":"Little Rock, AK","doi":"10.3133/837","collaboration":"Prepared in cooperation with the Arkansas Geological Commission and with other state and federal agencies.","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1965, Water resources data for Arkansas, https://doi.org/10.3133/837.","costCenters":[],"links":[{"id":291714,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"country":"United States","state":"Arkansas","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -94.6179,33.0041 ], [ -94.6179,36.4997 ], [ -89.6468,36.4997 ], [ -89.6468,33.0041 ], [ -94.6179,33.0041 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53e1efe1e4b0fe532be2deab","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":527756,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":838,"text":"838 - 1965 - Water resources data for California","interactions":[],"lastModifiedDate":"2014-08-05T13:53:36","indexId":"838","displayToPublicDate":"1965-01-01T13:52:14","publicationYear":"1965","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"title":"Water resources data for California","docAbstract":"No abstract available.","language":"English","publisher":"U.S. Department of the Interior","publisherLocation":"Menlo Park, CA","doi":"10.3133/838","issn":"0364-4057","collaboration":"Prepared in cooperation with the California Department of Water Resources and other agencies.","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1965, Water resources data for California, https://doi.org/10.3133/838.","costCenters":[],"links":[{"id":291711,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"country":"United States","state":"California","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -124.41,32.53 ], [ -124.41,42.01 ], [ -114.13,42.01 ], [ -114.13,32.53 ], [ -124.41,32.53 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53e1efe2e4b0fe532be2dead","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":527757,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":839,"text":"839 - 1965 - Water resources data for Colorado","interactions":[],"lastModifiedDate":"2014-08-05T13:50:08","indexId":"839","displayToPublicDate":"1965-01-01T13:48:56","publicationYear":"1965","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"title":"Water resources data for Colorado","docAbstract":"No abstract available.","language":"English","publisher":"U.S. Department of the Interior","publisherLocation":"Lakewood, CO","doi":"10.3133/839","collaboration":"Prepared in cooperation with the state of Colorado and other agencies.","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1965, Water resources data for Colorado, https://doi.org/10.3133/839.","costCenters":[],"links":[{"id":291710,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"country":"United States","state":"Colorado","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -109.0603,36.9924 ], [ -109.0603,41.0034 ], [ -102.0409,41.0034 ], [ -102.0409,36.9924 ], [ -109.0603,36.9924 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53e1efe2e4b0fe532be2deaf","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":527758,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":841,"text":"841 - 1965 - Water resources data for Florida","interactions":[],"lastModifiedDate":"2014-08-05T13:47:06","indexId":"841","displayToPublicDate":"1965-01-01T13:45:42","publicationYear":"1965","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"title":"Water resources data for Florida","docAbstract":"No abstract available.","language":"English","publisher":"U.S. Department of the Interior","publisherLocation":"Tallahassee, FL","doi":"10.3133/841","issn":"0275-2689","collaboration":"Prepared in cooperation with the state of Florida and other agencies.","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1965, Water resources data for Florida, https://doi.org/10.3133/841.","costCenters":[],"links":[{"id":291709,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"country":"United States","state":"Florida","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -87.6349,24.5211 ], [ -87.6349,31.001 ], [ -80.0311,31.001 ], [ -80.0311,24.5211 ], [ -87.6349,24.5211 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53e1efe3e4b0fe532be2deb3","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":527760,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
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