{"pageNumber":"6758","pageRowStart":"168925","pageSize":"25","recordCount":184617,"records":[{"id":61980,"text":"mr31 - 1962 - Talc and soapstone in the United States, exclusive of Alaska and Hawaii","interactions":[{"subject":{"id":44088,"text":"ofr6132 - 1961 - Talc and soapstone in the United States","indexId":"ofr6132","publicationYear":"1961","noYear":false,"title":"Talc and soapstone in the United States"},"predicate":"SUPERSEDED_BY","object":{"id":61980,"text":"mr31 - 1962 - Talc and soapstone in the United States, exclusive of Alaska and Hawaii","indexId":"mr31","publicationYear":"1962","noYear":false,"title":"Talc and soapstone in the United States, exclusive of Alaska and Hawaii"},"id":1}],"lastModifiedDate":"2025-05-22T16:43:39.309996","indexId":"mr31","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1962","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":324,"text":"Mineral Investigations Resource Map","code":"MR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"31","title":"Talc and soapstone in the United States, exclusive of Alaska and Hawaii","docAbstract":"<p>The locations of talc and soapstone deposits in the United States (exclusive of Alaska and Hawaii) arc shown on the accompanying map. The two types are distinguished by the shape of symbols; the relative importance of the deposits, expressed in broad ranges of tonnage, is indicated by the size of symbols. Two persistent belts in the Southeastern States are shown by patterns, and the locations of the principal deposits within these belts are shown by appropriate symbols</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/mr31","usgsCitation":"Chidester, A., and Worthington, H.W., 1962, Talc and soapstone in the United States, exclusive of Alaska and Hawaii: U.S. Geological Survey Mineral Investigations Resource Map 31, Report: 9 p.; 1 Plate: 64.06 x 40.50 inches, https://doi.org/10.3133/mr31.","productDescription":"Report: 9 p.; 1 Plate: 64.06 x 40.50 inches","costCenters":[],"links":[{"id":486397,"rank":3,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/mr/31/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":260433,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mr/31/plate-1.pdf"},{"id":179999,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/mr/31/report-thumb.jpg"}],"scale":"3168000","country":"United States","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -127.25,24.25 ], [ -127.25,49.25 ], [ -66.5,49.25 ], [ -66.5,24.25 ], [ -127.25,24.25 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adde4b07f02db686e86","contributors":{"authors":[{"text":"Chidester, A.H.","contributorId":42940,"corporation":false,"usgs":true,"family":"Chidester","given":"A.H.","email":"","affiliations":[],"preferred":false,"id":266648,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Worthington, Henry Wilson","contributorId":28299,"corporation":false,"usgs":true,"family":"Worthington","given":"Henry","email":"","middleInitial":"Wilson","affiliations":[],"preferred":false,"id":266647,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":63249,"text":"gq163 - 1962 - Geology of the Maryville quadrangle, Tennessee","interactions":[],"lastModifiedDate":"2012-02-10T00:10:44","indexId":"gq163","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1962","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":316,"text":"Geologic Quadrangle","code":"GQ","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"163","title":"Geology of the Maryville quadrangle, Tennessee","language":"ENGLISH","doi":"10.3133/gq163","usgsCitation":"Cattermole, J.M., 1962, Geology of the Maryville quadrangle, Tennessee: U.S. Geological Survey Geologic Quadrangle 163, 1 map., https://doi.org/10.3133/gq163.","productDescription":"1 map.","costCenters":[],"links":[{"id":102163,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_612.htm","linkFileType":{"id":5,"text":"html"},"description":"612"},{"id":249361,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gq/0163/report.pdf","size":"35","linkFileType":{"id":1,"text":"pdf"}},{"id":252677,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gq/0163/report-thumb.jpg"}],"scale":"24000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -84,35.75 ], [ -84,35.8675 ], [ -83.86749999999999,35.8675 ], [ -83.86749999999999,35.75 ], [ -84,35.75 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4acce4b07f02db67ea13","contributors":{"authors":[{"text":"Cattermole, John Mark","contributorId":88746,"corporation":false,"usgs":true,"family":"Cattermole","given":"John","email":"","middleInitial":"Mark","affiliations":[],"preferred":false,"id":268552,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":41823,"text":"ofr622 - 1962 - Aeromagnetic map of the Llano Uplift, Mason-Burnet area, central Texas","interactions":[{"subject":{"id":41823,"text":"ofr622 - 1962 - Aeromagnetic map of the Llano Uplift, Mason-Burnet area, central Texas","indexId":"ofr622","publicationYear":"1962","noYear":false,"title":"Aeromagnetic map of the Llano Uplift, Mason-Burnet area, central Texas"},"predicate":"SUPERSEDED_BY","object":{"id":64251,"text":"gp417 - 1963 - Aeromagnetic map of the Llano Uplift, Mason-Burnet area, central Texas","indexId":"gp417","publicationYear":"1963","noYear":false,"title":"Aeromagnetic map of the Llano Uplift, Mason-Burnet area, central Texas"},"id":1}],"supersededBy":{"id":64251,"text":"gp417 - 1963 - Aeromagnetic map of the Llano Uplift, Mason-Burnet area, central Texas","indexId":"gp417","publicationYear":"1963","noYear":false,"title":"Aeromagnetic map of the Llano Uplift, Mason-Burnet area, central Texas"},"lastModifiedDate":"2019-07-10T10:47:12","indexId":"ofr622","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1962","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":"62-2","title":"Aeromagnetic map of the Llano Uplift, Mason-Burnet area, central Texas","docAbstract":"<p>No abstract available.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr622","usgsCitation":"Andreasen, G., and Petrafeso, F., 1962, Aeromagnetic map of the Llano Uplift, Mason-Burnet area, central Texas: U.S. Geological Survey Open-File Report 62-2, 1 Plate: 54.17 x 36.18 inches , https://doi.org/10.3133/ofr622.","productDescription":"1 Plate: 54.17 x 36.18 inches ","costCenters":[],"links":[{"id":365452,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1962/0002/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":168032,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1962/0002/report-thumb.jpg"}],"country":"United States","state":"Texas","otherGeospatial":" Mason-Burnet area","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -98.82064819335938,\n              30.71940712027702\n            ],\n            [\n              -98.54187011718749,\n              30.71940712027702\n            ],\n            [\n              -98.54187011718749,\n              30.792575895440844\n            ],\n            [\n              -98.82064819335938,\n              30.792575895440844\n            ],\n            [\n              -98.82064819335938,\n              30.71940712027702\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4af4e4b07f02db691ead","contributors":{"authors":[{"text":"Andreasen, Gordon E.","contributorId":94272,"corporation":false,"usgs":true,"family":"Andreasen","given":"Gordon E.","affiliations":[],"preferred":false,"id":225576,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Petrafeso, Frank","contributorId":22749,"corporation":false,"usgs":true,"family":"Petrafeso","given":"Frank","email":"","affiliations":[],"preferred":false,"id":225575,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":62028,"text":"mr13 - 1962 - Copper in the United States, exclusive of Alaska and Hawaii","interactions":[{"subject":{"id":40124,"text":"ofr6184 - 1961 - Copper in the United States","indexId":"ofr6184","publicationYear":"1961","noYear":false,"title":"Copper in the United States"},"predicate":"SUPERSEDED_BY","object":{"id":62028,"text":"mr13 - 1962 - Copper in the United States, exclusive of Alaska and Hawaii","indexId":"mr13","publicationYear":"1962","noYear":false,"title":"Copper in the United States, exclusive of Alaska and Hawaii"},"id":1}],"lastModifiedDate":"2025-05-02T15:56:39.841636","indexId":"mr13","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1962","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":324,"text":"Mineral Investigations Resource Map","code":"MR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"13","title":"Copper in the United States, exclusive of Alaska and Hawaii","docAbstract":"<p>The copper districts in the United States (exclusive of Alaska and Hawaii) are shown on the accompanying map. In compiling the map, the estimated total quantity of copper present before mining was used to assign districts to size categories, and both production and reserves are included without distinction as to the status of exploitation. Four categories have been distinguished: deposits that contain 50+ to 1,000 tons; 1,000 to 50,000 tons; 50,000 to 1 million tons; and over 1 million tons of copper respectively. In many of the smaller deposits copper occurs with other metals, as gold, silver; lead, or zinc, that may be quantitatively and economically more important than the contained copper. Thus, for example, a deposit that contains large values in gold or zinc may contain only a small amount of copper and is shown on this map as a small copper deposit.</p><p>Five principal morphologic types of deposits have been distinguished on the map by letter symbols. These are disseminated, replacement, vein, massive sulfide, and native copper deposits (see Explanation). They are not strictly genetic types, however, for the disseminated deposits, the massive sulfide deposits, and many of the vein deposits were formed largely or entirely by replacement processes.</p><p>The symbols show either individual mines or the approximate centers of districts. Some of the more prominent districts are identified by name on the map, and all with over 1,000 tons of copper are numbered to correspond to the Locality Index. As mining district names do not always correspond to locality names, and a name established through common usage may not be the legal name of the mining district, several names are given in the index for some localities. The index is arranged alphabetically by States. Both published and unpublished data were used, and at least one reference is given for each locality if reports on it have been published.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/mr13","usgsCitation":"Kinkel, A.R., and Peterson, N.P., 1962, Copper in the United States, exclusive of Alaska and Hawaii: U.S. Geological Survey Mineral Investigations Resource Map 13, Report: 15 p.; 1 Plate: 64.20 x 42.00 inches, https://doi.org/10.3133/mr13.","productDescription":"Report: 15 p.; 1 Plate: 64.20 x 42.00 inches","costCenters":[],"links":[{"id":485338,"rank":3,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/mr/13/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":260477,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mr/13/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":180103,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/mr/13/report-thumb.jpg"}],"scale":"3168000","country":"United States","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -127.25,24.25 ], [ -127.25,49.25 ], [ -66.5,49.25 ], [ -66.5,24.25 ], [ -127.25,24.25 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adbe4b07f02db685bf3","contributors":{"authors":[{"text":"Kinkel, Arthur R. Jr.","contributorId":27440,"corporation":false,"usgs":true,"family":"Kinkel","given":"Arthur","suffix":"Jr.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":266742,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Peterson, N. P.","contributorId":29827,"corporation":false,"usgs":true,"family":"Peterson","given":"N.","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":266743,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":62030,"text":"mr25 - 1962 - Tungsten in the United States, exclusive of Alaska and Hawaii","interactions":[{"subject":{"id":44128,"text":"ofr6187 - 1961 - Tungsten in the United States","indexId":"ofr6187","publicationYear":"1961","noYear":false,"title":"Tungsten in the United States"},"predicate":"SUPERSEDED_BY","object":{"id":62030,"text":"mr25 - 1962 - Tungsten in the United States, exclusive of Alaska and Hawaii","indexId":"mr25","publicationYear":"1962","noYear":false,"title":"Tungsten in the United States, exclusive of Alaska and Hawaii"},"id":1}],"lastModifiedDate":"2025-05-20T16:46:58.868673","indexId":"mr25","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1962","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":324,"text":"Mineral Investigations Resource Map","code":"MR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"25","title":"Tungsten in the United States, exclusive of Alaska and Hawaii","docAbstract":"<p>The accompanying map shows the tungsten deposits of the United States (exclusive of Alaska and Hawaii). The relative importance of the deposits, groups, or districts is shown by four symbols, indicating tungsten contents of: (1) greater than 10,000 short tons of tungsten metal, (2) 10,000 to 500 tons, (3) 500 to 10 tons, and (4) less than 10 tons. In assigning size, production plus estimated reserves were taken into account, and also, for some deposits or areas, the presence of tungsten in large quantity but very low concentration.</p><p>The map symbols, plotted to the nearest minute, make no distinction between individual deposits and groups of deposits or districts; about 590 map symbols represent several times this number of deposits because many symbols stand for clusters of deposits spaced too closely to show individually at the scale used. All localities are numbered consecutively in each state and are identified in the Locality Index. Unpublished information has been used extensively. The tungsten data for Colorado, Idaho, Montana, New Mexico, South Dakota, Texas, Utah, and Wyoming were compiled by Tweto, and those for the remaining states by Lemmon.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/mr25","usgsCitation":"Lemmon, D., and Tweto, O.L., 1962, Tungsten in the United States, exclusive of Alaska and Hawaii: U.S. Geological Survey Mineral Investigations Resource Map 25, Report: 25 p.; 1 Plate: 64.02 x 40.70 inches, https://doi.org/10.3133/mr25.","productDescription":"Report: 25 p.; 1 Plate: 64.02 x 40.70 inches","costCenters":[],"links":[{"id":180160,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/mr/25/report-thumb.jpg"},{"id":434851,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/mr/25/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":434852,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mr/25/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"3168000","country":"United States","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -127.25,24.25 ], [ -127.25,49.25 ], [ -66.5,49.25 ], [ -66.5,24.25 ], [ -127.25,24.25 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a49e4b07f02db623ffe","contributors":{"authors":[{"text":"Lemmon, D.M.","contributorId":16007,"corporation":false,"usgs":true,"family":"Lemmon","given":"D.M.","email":"","affiliations":[],"preferred":false,"id":266746,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Tweto, Ogden L.","contributorId":84435,"corporation":false,"usgs":true,"family":"Tweto","given":"Ogden","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":266747,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":62033,"text":"mr15 - 1962 - Lead in the United States, exclusive of Alaska and Hawaii","interactions":[{"subject":{"id":46121,"text":"ofr6194 - 1961 - Lead in the United States","indexId":"ofr6194","publicationYear":"1961","noYear":false,"title":"Lead in the United States"},"predicate":"SUPERSEDED_BY","object":{"id":62033,"text":"mr15 - 1962 - Lead in the United States, exclusive of Alaska and Hawaii","indexId":"mr15","publicationYear":"1962","noYear":false,"title":"Lead in the United States, exclusive of Alaska and Hawaii"},"id":1}],"lastModifiedDate":"2025-05-02T16:12:06.01515","indexId":"mr15","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1962","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":324,"text":"Mineral Investigations Resource Map","code":"MR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"15","title":"Lead in the United States, exclusive of Alaska and Hawaii","docAbstract":"<p>The productive lead districts in the United States (exclusive of Alaska and Hawaii) are shown on the accompanying map. The map is at a scale of 1: 3,168,000, (50 miles to the inch). Only those districts known or believed to contain 1,000 short tons or more of lead are shown; individual deposits within districts are not represented.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/mr15","usgsCitation":"McKnight, E.T., Heyl, A.V., and Newman, W.L., 1962, Lead in the United States, exclusive of Alaska and Hawaii: U.S. Geological Survey Mineral Investigations Resource Map 15, Report: 22 p.; 1 Plate: 64.12 x 42.00 inches, https://doi.org/10.3133/mr15.","productDescription":"Report: 22 p.; 1 Plate: 64.12 x 42.00 inches","costCenters":[],"links":[{"id":485344,"rank":3,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/mr/15/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":260480,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mr/15/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":180163,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/mr/15/report-thumb.jpg"}],"scale":"3168000","country":"United States","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -127.25,24.25 ], [ -127.25,49.25 ], [ -66.5,49.25 ], [ -66.5,24.25 ], [ -127.25,24.25 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1be4b07f02db6a88b2","contributors":{"authors":[{"text":"McKnight, Edwin Thor","contributorId":61812,"corporation":false,"usgs":true,"family":"McKnight","given":"Edwin","email":"","middleInitial":"Thor","affiliations":[],"preferred":false,"id":266752,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Heyl, Allen Van","contributorId":91078,"corporation":false,"usgs":true,"family":"Heyl","given":"Allen","email":"","middleInitial":"Van","affiliations":[],"preferred":false,"id":266753,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Newman, William Louis","contributorId":7344,"corporation":false,"usgs":true,"family":"Newman","given":"William","email":"","middleInitial":"Louis","affiliations":[],"preferred":false,"id":266751,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":66364,"text":"i353 - 1962 - Geology of the Eskay quadrangle, Chouteau and Blaine Counties, Montana","interactions":[],"lastModifiedDate":"2012-02-10T00:11:16","indexId":"i353","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1962","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":320,"text":"IMAP","code":"I","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"353","subseriesTitle":"NONE","title":"Geology of the Eskay quadrangle, Chouteau and Blaine Counties, Montana","language":"ENGLISH","doi":"10.3133/i353","usgsCitation":"Lindvall, R.M., 1962, Geology of the Eskay quadrangle, Chouteau and Blaine Counties, Montana: U.S. Geological Survey IMAP 353, 1 map., https://doi.org/10.3133/i353.","productDescription":"1 map.","costCenters":[],"links":[{"id":102905,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_1372.htm","linkFileType":{"id":5,"text":"html"},"description":"1372"},{"id":187958,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"62500","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -109.75,47.75 ], [ -109.75,48 ], [ -109.5,48 ], [ -109.5,47.75 ], [ -109.75,47.75 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad2e4b07f02db68169b","contributors":{"authors":[{"text":"Lindvall, R. M.","contributorId":53797,"corporation":false,"usgs":true,"family":"Lindvall","given":"R.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":274413,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":61979,"text":"mr35 - 1962 - Beryllium in the United States, exclusive of Alaska and Hawaii","interactions":[],"lastModifiedDate":"2025-05-09T18:43:54.792514","indexId":"mr35","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1962","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":324,"text":"Mineral Investigations Resource Map","code":"MR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"35","title":"Beryllium in the United States, exclusive of Alaska and Hawaii","docAbstract":"<p>This map shows most of the known occurrences of beryllium minerals and of rocks that contain 0.003 percent or more beryllium (0.01 percent Be0) in the United States (exclusive of Alaska and Hawaii). The occurrences are subdivided on the map according to genesis and size. The genetic types of deposits shown are: pegmatite, vein and replacement deposits (exclusive of tactite), tactite, disseminated beryl in granite and rhyolite, hot spring deposits, and residual materials. Deposits of each type that have a total production plus reserve greater than 24,000 lbs. of contained Be0 (equivalent to 1200 short ton units of Be0 or 190 tons of beryl) are shown by a large symbol. Names are given only for the districts that are of particular economic or scientific importance. Both published information and unpublished data gathered by the U. S. Geological Survey were used in preparing the map and text.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/mr35","usgsCitation":"Griffitts, W.R., Larrabee, D.M., and Norton, J.J., 1962, Beryllium in the United States, exclusive of Alaska and Hawaii: U.S. Geological Survey Mineral Investigations Resource Map 35, Report: 3 p.; 1 Plate: 64.20 x 40.58 inches, https://doi.org/10.3133/mr35.","productDescription":"Report: 3 p.; 1 Plate: 64.20 x 40.58 inches","costCenters":[],"links":[{"id":485679,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mr/35/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":485678,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/mr/35/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":179998,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/mr/35/report-thumb.jpg"}],"scale":"3168000","country":"United States","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -127.25,24.25 ], [ -127.25,49.25 ], [ -66.5,49.25 ], [ -66.5,24.25 ], [ -127.25,24.25 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a52e4b07f02db62aed3","contributors":{"authors":[{"text":"Griffitts, Wallace R.","contributorId":103260,"corporation":false,"usgs":true,"family":"Griffitts","given":"Wallace","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":266646,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Larrabee, David Marcel","contributorId":49347,"corporation":false,"usgs":true,"family":"Larrabee","given":"David","email":"","middleInitial":"Marcel","affiliations":[],"preferred":false,"id":266644,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Norton, James Jennings","contributorId":59412,"corporation":false,"usgs":true,"family":"Norton","given":"James","email":"","middleInitial":"Jennings","affiliations":[],"preferred":false,"id":266645,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":36374,"text":"b1142H - 1962 - Future petroleum producing capacity of the United States","interactions":[],"lastModifiedDate":"2012-02-02T00:09:32","indexId":"b1142H","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1962","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":306,"text":"Bulletin","code":"B","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1142","chapter":"H","title":"Future petroleum producing capacity of the United States","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/b1142H","usgsCitation":"Zapp, A.D., 1962, Future petroleum producing capacity of the United States: U.S. Geological Survey Bulletin 1142, p. H1-H36, ill. ;24 cm., https://doi.org/10.3133/b1142H.","productDescription":"p. H1-H36, ill. ;24 cm.","costCenters":[],"links":[{"id":93850,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/1142h/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":166530,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/1142h/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b32e4b07f02db6b4210","contributors":{"authors":[{"text":"Zapp, Alfred Dexter","contributorId":6463,"corporation":false,"usgs":true,"family":"Zapp","given":"Alfred","email":"","middleInitial":"Dexter","affiliations":[],"preferred":false,"id":216221,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":61853,"text":"gq182 - 1962 - Geology of the Jamestown quadrangle, Kentucky","interactions":[],"lastModifiedDate":"2012-02-10T00:10:30","indexId":"gq182","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1962","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":316,"text":"Geologic Quadrangle","code":"GQ","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"182","title":"Geology of the Jamestown quadrangle, Kentucky","language":"ENGLISH","doi":"10.3133/gq182","usgsCitation":"Thaden, R.E., and Lewis, R., 1962, Geology of the Jamestown quadrangle, Kentucky: U.S. Geological Survey Geologic Quadrangle 182, 1 map., https://doi.org/10.3133/gq182.","productDescription":"1 map.","costCenters":[],"links":[{"id":102182,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_631.htm","linkFileType":{"id":5,"text":"html"},"description":"631"},{"id":248144,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gq/0182/report.pdf","size":"35","linkFileType":{"id":1,"text":"pdf"}},{"id":252887,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gq/0182/report-thumb.jpg"}],"scale":"24000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -85.11749999999999,36.8675 ], [ -85.11749999999999,37 ], [ -85,37 ], [ -85,36.8675 ], [ -85.11749999999999,36.8675 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4acee4b07f02db67fe63","contributors":{"authors":[{"text":"Thaden, Robert E.","contributorId":75502,"corporation":false,"usgs":true,"family":"Thaden","given":"Robert","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":266454,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lewis, Richard Quintin","contributorId":91097,"corporation":false,"usgs":true,"family":"Lewis","given":"Richard Quintin","affiliations":[],"preferred":false,"id":266455,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":42784,"text":"ofr6295 - 1962 - Preliminary report on the seismic investigations in the Orleans, Wellfleet, North Truro, and Provincetown quadrangles, Massachusetts","interactions":[],"lastModifiedDate":"2012-02-02T00:05:03","indexId":"ofr6295","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1962","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":"62-95","title":"Preliminary report on the seismic investigations in the Orleans, Wellfleet, North Truro, and Provincetown quadrangles, Massachusetts","language":"ENGLISH","doi":"10.3133/ofr6295","usgsCitation":"Oldale, R.N., and Tuttle, C., 1962, Preliminary report on the seismic investigations in the Orleans, Wellfleet, North Truro, and Provincetown quadrangles, Massachusetts: U.S. Geological Survey Open-File Report 62-95, 1 map :photocopy ;30 x 29 cm., on sheet 61 x 72 cm., https://doi.org/10.3133/ofr6295.","productDescription":"1 map :photocopy ;30 x 29 cm., on sheet 61 x 72 cm.","costCenters":[],"links":[{"id":135634,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":80597,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1962/0095/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aaee4b07f02db66c805","contributors":{"authors":[{"text":"Oldale, Robert N.","contributorId":38953,"corporation":false,"usgs":true,"family":"Oldale","given":"Robert","email":"","middleInitial":"N.","affiliations":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":false,"id":227114,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Tuttle, C.R.","contributorId":83894,"corporation":false,"usgs":true,"family":"Tuttle","given":"C.R.","email":"","affiliations":[],"preferred":false,"id":227115,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":3259,"text":"cir464 - 1962 - Floods in New Mexico, magnitude and frequency","interactions":[],"lastModifiedDate":"2018-01-02T20:01:15","indexId":"cir464","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1962","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":307,"text":"Circular","code":"CIR","onlineIssn":"2330-5703","printIssn":"1067-084X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"464","title":"Floods in New Mexico, magnitude and frequency","docAbstract":"This report presents a method of determining the magnitude and frequency of floods that can be expected in New Mexico The discharge of the mean annual flood for various regions in the State is defined. Curves relate mean annual flood and drainage area. Drainage area was the only basin characteristic found to have an appreciable effect on discharge of the mean annual flood except in two regions where a relation with altitude also is defined. Composite frequency curves relate discharge of the mean annual flood to the discharge of floods having recurrence intervals from 1.1 to 50 years. These relationships are based on records 5 or more years in length from gaging stations that had flow essentially unregulated.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/cir464","usgsCitation":"Wiard, L.A., 1962, Floods in New Mexico, magnitude and frequency: U.S. Geological Survey Circular 464, 13 p. :col. map, diagrs. ;27 cm., https://doi.org/10.3133/cir464.","productDescription":"13 p. :col. map, diagrs. ;27 cm.","costCenters":[],"links":[{"id":122608,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1962/0464/report-thumb.jpg"},{"id":30254,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1962/0464/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e5e4b07f02db5e700b","contributors":{"authors":[{"text":"Wiard, Leon A.","contributorId":99538,"corporation":false,"usgs":true,"family":"Wiard","given":"Leon","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":146533,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":3054,"text":"wsp1702 - 1962 - Surface water supply of the United States, 1960, Part 1-B, North Atlantic slope basins, New York to York River","interactions":[],"lastModifiedDate":"2012-02-02T00:05:36","indexId":"wsp1702","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1962","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":"1702","title":"Surface water supply of the United States, 1960, Part 1-B, North Atlantic slope basins, New York to York River","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/wsp1702","usgsCitation":"Hendricks, E.L., 1962, Surface water supply of the United States, 1960, Part 1-B, North Atlantic slope basins, New York to York River: U.S. Geological Survey Water Supply Paper 1702, xi, 567 p. ;23 cm., https://doi.org/10.3133/wsp1702.","productDescription":"xi, 567 p. ;23 cm.","costCenters":[],"links":[{"id":139335,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1702/report-thumb.jpg"},{"id":29908,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1702/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4af8e4b07f02db6943b2","contributors":{"authors":[{"text":"Hendricks, E. L.","contributorId":50126,"corporation":false,"usgs":true,"family":"Hendricks","given":"E.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":146212,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":1973,"text":"wsp1619U - 1962 - Methods of measuring soil moisture in the field","interactions":[],"lastModifiedDate":"2012-02-02T00:05:24","indexId":"wsp1619U","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1962","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":"1619","chapter":"U","title":"Methods of measuring soil moisture in the field","docAbstract":"For centuries, the amount of moisture in the soil has been of interest in agriculture. The subject of soil moisture is also of great importance to the hydrologist, forester, and soils engineer. \r\n\r\nMuch equipment and many methods have been developed to measure soil moisture under field conditions. This report discusses and evaluates the various methods for measurement of soil moisture and describes the equipment needed for each method. The advantages and disadvantages of each method are discussed and an extensive list of references is provided for those desiring to study the subject in more detail. \r\n\r\nThe gravimetric method is concluded to be the most satisfactory method for most problems requiring onetime moisture-content data. The radioactive method is normally best for obtaining repeated measurements of soil moisture in place. It is concluded that all methods have some limitations and that the ideal method for measurement of soil moisture under field conditions has yet to be perfected.","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/wsp1619U","usgsCitation":"Johnson, A., 1962, Methods of measuring soil moisture in the field: U.S. Geological Survey Water Supply Paper 1619, iii, 25 p. :ill. ;24 cm., https://doi.org/10.3133/wsp1619U.","productDescription":"iii, 25 p. :ill. ;24 cm.","costCenters":[],"links":[{"id":138299,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1619u/report-thumb.jpg"},{"id":27349,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1619u/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a54e4b07f02db62bee4","contributors":{"authors":[{"text":"Johnson, A.I.","contributorId":82676,"corporation":false,"usgs":true,"family":"Johnson","given":"A.I.","email":"","affiliations":[],"preferred":false,"id":144460,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":3172,"text":"wsp1496C - 1962 - Flame-photometric determination of strontium in natural water","interactions":[],"lastModifiedDate":"2012-02-02T00:05:35","indexId":"wsp1496C","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1962","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":"1496","chapter":"C","title":"Flame-photometric determination of strontium in natural water","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/wsp1496C","usgsCitation":"Horr, C.A., 1962, Flame-photometric determination of strontium in natural water: U.S. Geological Survey Water Supply Paper 1496, 33-53 p., https://doi.org/10.3133/wsp1496C.","productDescription":"33-53 p.","costCenters":[],"links":[{"id":138921,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1496c/report-thumb.jpg"},{"id":30130,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1496c/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f2e4b07f02db5ef2e1","contributors":{"authors":[{"text":"Horr, C. Albert","contributorId":43333,"corporation":false,"usgs":true,"family":"Horr","given":"C.","email":"","middleInitial":"Albert","affiliations":[],"preferred":false,"id":146368,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":2078,"text":"wsp1539W - 1962 - Hydraulics of river channels as related to navigability","interactions":[],"lastModifiedDate":"2012-02-02T00:05:23","indexId":"wsp1539W","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1962","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":"1539","chapter":"W","title":"Hydraulics of river channels as related to navigability","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/wsp1539W","usgsCitation":"Langbein, W.B., 1962, Hydraulics of river channels as related to navigability: U.S. Geological Survey Water Supply Paper 1539, iv, 30 p. :ill. ;24 cm., https://doi.org/10.3133/wsp1539W.","productDescription":"iv, 30 p. :ill. ;24 cm.","costCenters":[],"links":[{"id":138346,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1539w/report-thumb.jpg"},{"id":27638,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1539w/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a51e4b07f02db6297eb","contributors":{"authors":[{"text":"Langbein, W. B.","contributorId":102053,"corporation":false,"usgs":true,"family":"Langbein","given":"W.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":144646,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":3180,"text":"wsp1369D - 1962 - Flow through openings in width constrictions","interactions":[],"lastModifiedDate":"2012-02-02T00:05:35","indexId":"wsp1369D","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1962","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":"1369","chapter":"D","title":"Flow through openings in width constrictions","docAbstract":"A highway embankment across a stream channel may have one or several bridge openings. In 1953, the pattern of flow through a single opening was quantitatively described by C. E. Kindsvater, R. W. Carter, and H. J. Tracy. The present investigation of the flow pattern at constrictions with two to seven openings is a continuation of the earlier study. Laboratory experiments and the analysis were directed toward the development of methods for (a) computing discharge through multiple-opening constrictions, (b) apportioning a given total discharge among the several openings, and (c) predicting the backwater caused by the constriction. \r\n\r\nThe division of flow among the openings was related to the relative area of each opening, and the relative velocity in the channel immediately upstream from each opening. On the basis of this relationship, the boundaries of the flow channel approaching each opening were established. The head-discharge and backwater characteristics of each opening were then analyzed separately. It is shown that the relations developed for the constriction with a single opening are applicable to each opening of a multiple-opening constriction once the boundaries of the separate flow channels have been established.","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/wsp1369D","usgsCitation":"Davidian, J., Carrigan, P., and Shen, J., 1962, Flow through openings in width constrictions: U.S. Geological Survey Water Supply Paper 1369, 154 p. :illus., maps. ;24 cm. :91-122 p., https://doi.org/10.3133/wsp1369D.","productDescription":"154 p. :illus., maps. ;24 cm. :91-122 p.","costCenters":[],"links":[{"id":139023,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1369d/report-thumb.jpg"},{"id":30138,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1369d/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e48cce4b07f02db544634","contributors":{"authors":[{"text":"Davidian, Jacob","contributorId":80245,"corporation":false,"usgs":true,"family":"Davidian","given":"Jacob","email":"","affiliations":[],"preferred":false,"id":146383,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Carrigan, P.H. Jr.","contributorId":21935,"corporation":false,"usgs":true,"family":"Carrigan","given":"P.H.","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":146381,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Shen, John","contributorId":34109,"corporation":false,"usgs":true,"family":"Shen","given":"John","email":"","affiliations":[],"preferred":false,"id":146382,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":3197,"text":"wsp1544B - 1962 - An application of thermometry to the study of ground water","interactions":[],"lastModifiedDate":"2018-04-02T10:17:13","indexId":"wsp1544B","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1962","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":"1544","chapter":"B","title":"An application of thermometry to the study of ground water","docAbstract":"<p>Except for studies of temperature data related to ground-water developments that induce infiltration from streams, little attention has been given to the possibility of using temperature fluctuations as a tool for studying the elements of the hydrologic cycle involving ground water.</p>\n<p>The temperature of the water discharged from large installations that induce river infiltration through alluvial deposits depends primarily on the following factors: (a) the porosity of the aquifer, (b) the specific heat of the rocks or mineral grains making it up, (c) the temperature of the ground water in storage, (d) the temperature of the river water, and (e) the amount of mixing that occurs as a result of pumping. In six installations of this type, where the annual rivertemperature fluctuations ranged from 44&deg; to 52&deg;F, the average range in groundwater temperature was 22 &deg;F. The cycles of ground-water temperature lagged behind the river-temperature cycles by 1 to 5<sup>1</sup>/<sub>2</sub> months. Under the conditions that existed, the lag of the minima of the cycles was much greater than that of the maxima, largely because of variations in pumpage and of the effect of viscosity differences on the rate of flow.</p>\n<p>An experimental study was made at Worthington in southwestern Minnesota to determine whether temperature fluctuations could be used to study rates and directions of ground-water movement or to evaluate recharge conditions. Three shallow glacial-outwash aquifers were studied by measuring temperatures at approximately monthly intervals in three municipal-supply wells whose average yields were about 60 to 150 gpm (gallons per minute). Temperatures were read with an accuracy of 0.01&deg; to 0.02&deg;C, and the data were analyzed graphically and correlated in detail with lake levels, lake temperatures, precipitation, and groundwater levels.</p>\n<p>Thermographs for 2 wells, 1 completed in a semiconfined aquifer about 200 feet from Okabena Lake and the other in a water-table aquifer about 850 feet from the lake, indicate that pumping induces water to move from the lake into the aquifers. A larger percentage of cold lake water was mixed with ground water from January to March 1958 than from January to March 1959. On the assumption that the cold or warm lake water was a distinct mass, the average time required for water to move from the lake to the well 200 feet away, under the prevailing hydraulic gradient, was 2 to 4 months; and to the well 850 feet away, 5 to 7 months.</p>\n<p>The thermograph for a well 1,800 feet from the lake, completed in an artesian aquifer that is confined by relatively impervious glacial till, indicates that the till acts as an insulating medium. However, despite the apparently low permeability of the till, the thermograph suggests that the lowering of artesian pressure, which results from pumping, induces warmer water to move downward through the till.</p>\n<p>The infiltration of relatively warm spring and summer rainfall can be detected on the thermographs of all the wells.</p>\n<p>The precise measurement of fluctuations in ground-water temperature, based on monthly readings in shallow glacial-outwash aquifers (up to about 70 feet deep), is useful in the study of ground-water movement and recharge. In addition to the study of natural phenomena in the hydrologic cycle, thermometry may be used as a tool in making detailed studies of (1) the effects of inducing the infiltration of surface water, (2) artificial recharge, (3) the effects of injecting petroleum products or radioactive or other wastes into the ground, and (4) ground-water movement in mines.</p>","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/wsp1544B","collaboration":"Prepared in cooperation with the Division of Waters, Minnesota Department of Conservation","usgsCitation":"Schneider, R., 1962, An application of thermometry to the study of ground water: U.S. Geological Survey Water Supply Paper 1544, Document: iii, 16 p.; 2 Plates: 16 x 12 inches and 16 x 17 inches, https://doi.org/10.3133/wsp1544B.","productDescription":"Document: iii, 16 p.; 2 Plates: 16 x 12 inches and 16 x 17 inches","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":392,"text":"Minnesota Water Science Center","active":true,"usgs":true}],"links":[{"id":30184,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1544b/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":30182,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1544b/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":30183,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1544b/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":138321,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1544b/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adae4b07f02db68571e","contributors":{"authors":[{"text":"Schneider, Robert","contributorId":102460,"corporation":false,"usgs":true,"family":"Schneider","given":"Robert","email":"","affiliations":[],"preferred":false,"id":146417,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":3198,"text":"wsp1544C - 1962 - Methods of flow measurement in well bores","interactions":[],"lastModifiedDate":"2022-07-19T11:31:11.072932","indexId":"wsp1544C","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1962","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":"1544","chapter":"C","title":"Methods of flow measurement in well bores","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Government Printing Office","doi":"10.3133/wsp1544C","usgsCitation":"Patten, E., and Bennett, G.D., 1962, Methods of flow measurement in well bores: U.S. Geological Survey Water Supply Paper 1544, 28 p., https://doi.org/10.3133/wsp1544C.","productDescription":"28 p.","costCenters":[],"links":[{"id":138322,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1544c/report-thumb.jpg"},{"id":30185,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1544c/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a54e4b07f02db62bd13","contributors":{"authors":[{"text":"Patten, Eugene P. Jr.","contributorId":34897,"corporation":false,"usgs":true,"family":"Patten","given":"Eugene P.","suffix":"Jr.","affiliations":[],"preferred":false,"id":146419,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bennett, Gordon D.","contributorId":18740,"corporation":false,"usgs":true,"family":"Bennett","given":"Gordon","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":146418,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":2517,"text":"wsp1619C - 1962 - Subsidence in the Santa Clara Valley, California: A progress report","interactions":[{"subject":{"id":46033,"text":"ofr5792 - 1957 - Map and graph showing land subsidence and ground-water level in Santa Clara Valley, California","indexId":"ofr5792","publicationYear":"1957","noYear":false,"title":"Map and graph showing land subsidence and ground-water level in Santa Clara Valley, California"},"predicate":"SUPERSEDED_BY","object":{"id":2517,"text":"wsp1619C - 1962 - Subsidence in the Santa Clara Valley, California: A progress report","indexId":"wsp1619C","publicationYear":"1962","noYear":false,"chapter":"C","title":"Subsidence in the Santa Clara Valley, California: A progress report"},"id":1}],"lastModifiedDate":"2022-05-11T18:44:50.672005","indexId":"wsp1619C","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1962","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":"1619","chapter":"C","title":"Subsidence in the Santa Clara Valley, California: A progress report","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wsp1619C","usgsCitation":"Poland, J.F., and Green, J.H., 1962, Subsidence in the Santa Clara Valley, California: A progress report: U.S. Geological Survey Water Supply Paper 1619, iii, 16 p., https://doi.org/10.3133/wsp1619C.","productDescription":"iii, 16 p.","costCenters":[],"links":[{"id":28717,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1619c/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":138795,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1619c/report-thumb.jpg"},{"id":400532,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_24816.htm"}],"country":"United States","state":"California","otherGeospatial":"Santa Clara Valley","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -122.25,\n              37.25\n            ],\n            [\n              -121.75,\n              37.25\n            ],\n            [\n              -121.75,\n              37.567\n            ],\n            [\n              -122.25,\n              37.567\n            ],\n            [\n              -122.25,\n              37.25\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b05e4b07f02db699b5b","contributors":{"authors":[{"text":"Poland, J. F.","contributorId":64223,"corporation":false,"usgs":true,"family":"Poland","given":"J.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":145330,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Green, J. H.","contributorId":43312,"corporation":false,"usgs":true,"family":"Green","given":"J.","email":"","middleInitial":"H.","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":145329,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":3723,"text":"cir460B - 1962 - A national network of hydrological benchmarks","interactions":[],"lastModifiedDate":"2017-03-24T15:54:22","indexId":"cir460B","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1962","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":307,"text":"Circular","code":"CIR","onlineIssn":"2330-5703","printIssn":"1067-084X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"460","chapter":"B","title":"A national network of hydrological benchmarks","docAbstract":"<p>We are engaged in great national programs of water control and development. An expanding population demands ever-increasing supplies of the natural resources which are to be found in or upon the landscape soil, water, minerals, food, timber, and fiber. By his works, by his extractions, man's mark upon his environment becomes ever deeper, his effects more indelible. </p><p>We often read that water tables are falling, that floods are increasing, that springs go dry more often now than in grandfather's time, or that rivers are muddier than before. Such changes, if true, are troublesome but water is a fluctuating resource, responding over time to changes in the environment. A recurring question of our times, and one that we anticipate will be increasingly vexing to posterity, is to know how much of the change in our environment is caused by man and how much is natural. In trying to answer this question we immediately face the insurmountable fact that changes must be measured relative to some standard base or datum. What can we compare against?</p><p>The most pervasive and probably the most important of the slow and subtle changes result directly or indirectly from variations in climate. Over a shorter or longer period of time, pulsations in precipitation and temperature change the amounts of water that are evaporated or transpired by the soil and vegetation, the amount of water that replenishes soil water, the quantity of water for recharge to ground water and for riverflow. Climatic variations also cause changes in the pattern of erosion, of which some spectacular consequences can be observed in the arid zones. Changes in climatic pattern, through their effects on the hydrologic cycle, on soil, and on vegetation, can produce results remarkably similar to those effected by the works of man.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Washington, D.C.","doi":"10.3133/cir460B","usgsCitation":"Leopold, L.B., 1962, A national network of hydrological benchmarks: U.S. Geological Survey Circular 460, 4 p., https://doi.org/10.3133/cir460B.","productDescription":"4 p.","startPage":"1","endPage":"4","numberOfPages":"7","costCenters":[],"links":[{"id":139231,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1962/0460b/report-thumb.jpg"},{"id":30783,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1962/0460b/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b23e4b07f02db6ade1d","contributors":{"authors":[{"text":"Leopold, Luna Bergere","contributorId":93884,"corporation":false,"usgs":true,"family":"Leopold","given":"Luna","email":"","middleInitial":"Bergere","affiliations":[],"preferred":false,"id":147484,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":71098,"text":"wdrMN621 - 1962 - Surface water records of Minnesota, 1962","interactions":[],"lastModifiedDate":"2012-02-02T00:14:03","indexId":"wdrMN621","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1962","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":"MN-62-1","title":"Surface water records of Minnesota, 1962","language":"ENGLISH","doi":"10.3133/wdrMN621","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1962, Surface water records of Minnesota, 1962: U.S. Geological Survey Water Data Report MN-62-1, Vii, 158 p., https://doi.org/10.3133/wdrMN621.","productDescription":"Vii, 158 p.","costCenters":[],"links":[{"id":101516,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/1962/mn-62-1/report.pdf","size":"12991","linkFileType":{"id":1,"text":"pdf"}},{"id":192886,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wdr/1962/mn-62-1/report-thumb.jpg"}],"scale":"100000","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afee4b07f02db6978e7","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":534717,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":32788,"text":"pp341B - 1962 - Geology and ore deposits of the Cachoeira do Campo, Dom Bosco, and Ouro Branco quadrangles, Minas Gerais, Brazil","interactions":[],"lastModifiedDate":"2012-02-02T00:09:20","indexId":"pp341B","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1962","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":"341","chapter":"B","title":"Geology and ore deposits of the Cachoeira do Campo, Dom Bosco, and Ouro Branco quadrangles, Minas Gerais, Brazil","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Geology and mineral resources of parts of Minas Gerais, Brazil","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"ENGLISH","doi":"10.3133/pp341B","usgsCitation":"Johnson, R., 1962, Geology and ore deposits of the Cachoeira do Campo, Dom Bosco, and Ouro Branco quadrangles, Minas Gerais, Brazil: U.S. Geological Survey Professional Paper 341, p. B1-B39, https://doi.org/10.3133/pp341B.","productDescription":"p. B1-B39","costCenters":[],"links":[{"id":119884,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0341b/report-thumb.jpg"},{"id":60749,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0341b/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":60750,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0341b/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":60751,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0341b/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad7e4b07f02db68458f","contributors":{"authors":[{"text":"Johnson, R.F.","contributorId":68794,"corporation":false,"usgs":true,"family":"Johnson","given":"R.F.","affiliations":[],"preferred":false,"id":209171,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":32767,"text":"pp426 - 1962 - Data on uranium and radium in ground water in the United States, 1954 to 1957","interactions":[],"lastModifiedDate":"2023-01-04T22:35:54.445213","indexId":"pp426","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1962","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":"426","title":"Data on uranium and radium in ground water in the United States, 1954 to 1957","docAbstract":"<p>This report is one of a series resulting from a study by the U.S. Geological Survey to determine the occurrence and distribution of naturally radioactive substances in water. From 1954-57 uranium and radium concentrations were determined in 561 samples, mainly of ground water, having wide geologic and geographic distribution. These concentrations, together with data on the hydrologic and geologic environment, the beta-gamma activity, and the chemical characteristics of each sample, are tabulated by States.</p><p>The conterminous United States was subdivided into 10 geotectonic regions to facilitate statistical interpretation of the occurrence of uranium and radium in fresh water in approximately homogeneous geologic provinces. For each geotectonic region, the range and median were determined for the concentrations of radium and uranium; for regions from which sufficient data were available, log-normal frequency distribution curves were calculated and superimposed on histograms of radium and uranium concentrations in the samples. An \"anomaly threshold\" is suggested for both radioelements for each region analyzed statistically. The western stable region had the greatest median and highest \"anomaly threshold\" for uranium. This region also had the highest \"anomaly threshold\" for radium, but the largest median for radium was found for samples collected in the Ozark-Ouachita system. The median concentration for uranium was lowest for the Atlantic and Gulf Coastal Plain and the Pacific orogenic belt. This latter region also had the lowest median-radium content.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Washington, D.C.","doi":"10.3133/pp426","usgsCitation":"Scott, R.C., and Barker, F.B., 1962, Data on uranium and radium in ground water in the United States, 1954 to 1957: U.S. Geological Survey Professional Paper 426, Report: iii, 115 p.; 2 Plates: 29.00 x 19.00 inches, https://doi.org/10.3133/pp426.","productDescription":"Report: iii, 115 p.; 2 Plates: 29.00 x 19.00 inches","numberOfPages":"120","costCenters":[{"id":114,"text":"Alaska Science Center","active":true,"usgs":true},{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":411397,"rank":5,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_4420.htm","linkFileType":{"id":5,"text":"html"}},{"id":119273,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0426/report-thumb.jpg"},{"id":60704,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0426/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":60703,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0426/plate-2.pdf","text":"Plate 2","linkFileType":{"id":1,"text":"pdf"},"linkHelpText":"Geotectonic regions of the conterminous United States"},{"id":60702,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0426/plate-1.pdf","text":"Plate 1","linkFileType":{"id":1,"text":"pdf"},"linkHelpText":"Map of the conterminous United States showing sampling sites"}],"country":"United States","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"geometry\": {\n        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