{"pageNumber":"7203","pageRowStart":"180050","pageSize":"25","recordCount":184660,"records":[{"id":55570,"text":"ofr403 - 1940 - Geologic map and sections of the northern part of the Baxter Basin gas field, Sweetwater County, Wyoming","interactions":[],"lastModifiedDate":"2012-02-02T00:11:57","indexId":"ofr403","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1940","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":"40-3","title":"Geologic map and sections of the northern part of the Baxter Basin gas field, Sweetwater County, Wyoming","language":"ENGLISH","doi":"10.3133/ofr403","usgsCitation":"Kramer, W., Frasier, G., McMillan, R., and Cox, J., 1940, Geologic map and sections of the northern part of the Baxter Basin gas field, Sweetwater County, Wyoming: U.S. Geological Survey Open-File Report 40-3, 1 map, https://doi.org/10.3133/ofr403.","productDescription":"1 map","costCenters":[],"links":[{"id":181292,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":88048,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1940/0003/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b13e4b07f02db6a3835","contributors":{"authors":[{"text":"Kramer, W.B.","contributorId":38212,"corporation":false,"usgs":true,"family":"Kramer","given":"W.B.","email":"","affiliations":[],"preferred":false,"id":253733,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Frasier, G.G.","contributorId":19633,"corporation":false,"usgs":true,"family":"Frasier","given":"G.G.","email":"","affiliations":[],"preferred":false,"id":253731,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"McMillan, R.","contributorId":13305,"corporation":false,"usgs":true,"family":"McMillan","given":"R.","email":"","affiliations":[],"preferred":false,"id":253730,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Cox, J.G.","contributorId":29063,"corporation":false,"usgs":true,"family":"Cox","given":"J.G.","email":"","affiliations":[],"preferred":false,"id":253732,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":55577,"text":"ofr401 - 1940 - Geologic map of the East Lance Creek oil and gas field","interactions":[{"subject":{"id":70047941,"text":"70047941 - 1943 - Geologic map and sections of Lance Creek oil and gas field and vicinity, Niobrara County, Wyoming","indexId":"70047941","publicationYear":"1943","noYear":false,"title":"Geologic map and sections of Lance Creek oil and gas field and vicinity, Niobrara County, Wyoming"},"predicate":"SUPERSEDED_BY","object":{"id":55577,"text":"ofr401 - 1940 - Geologic map of the East Lance Creek oil and gas field","indexId":"ofr401","publicationYear":"1940","noYear":false,"title":"Geologic map of the East Lance Creek oil and gas field"},"id":1}],"lastModifiedDate":"2013-06-28T14:54:49","indexId":"ofr401","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1940","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":"40-1","title":"Geologic map of the East Lance Creek oil and gas field","language":"ENGLISH","doi":"10.3133/ofr401","usgsCitation":"Kramer, W., Dobbin, C.E., and McMillan, R., 1940, Geologic map of the East Lance Creek oil and gas field: U.S. Geological Survey Open-File Report 40-1, NA, https://doi.org/10.3133/ofr401.","productDescription":"NA","costCenters":[],"links":[{"id":181946,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b04e4b07f02db699037","contributors":{"authors":[{"text":"Kramer, W.P.","contributorId":61098,"corporation":false,"usgs":true,"family":"Kramer","given":"W.P.","email":"","affiliations":[],"preferred":false,"id":253749,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Dobbin, C. E.","contributorId":32581,"corporation":false,"usgs":true,"family":"Dobbin","given":"C.","middleInitial":"E.","affiliations":[],"preferred":false,"id":253748,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"McMillan, R.","contributorId":13305,"corporation":false,"usgs":true,"family":"McMillan","given":"R.","email":"","affiliations":[],"preferred":false,"id":253747,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":36185,"text":"b922O - 1940 - Chromite deposits of the Pilliken area, Eldorado County, California","interactions":[],"lastModifiedDate":"2021-11-19T22:15:36.890633","indexId":"b922O","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1940","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":"922","chapter":"O","title":"Chromite deposits of the Pilliken area, Eldorado County, California","docAbstract":"<p>No abstract available.</p>","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Strategic minerals investigations, 1940, part 2: L-T","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/b922O","usgsCitation":"Wells, F.G., Page, L., and James, H.L., 1940, Chromite deposits of the Pilliken area, Eldorado County, California: U.S. Geological Survey Bulletin 922, Report: iv, 44 p.; 1 plate: 15.53 × 21.21 inches, https://doi.org/10.3133/b922O.","productDescription":"Report: iv, 44 p.; 1 plate: 15.53 × 21.21 inches","costCenters":[],"links":[{"id":109556,"rank":700,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_21113.htm","linkFileType":{"id":5,"text":"html"},"description":"21113"},{"id":97271,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/0922o/plate-66.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":97270,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/0922o/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":165795,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/0922o/report-thumb.jpg"}],"country":"United States","state":"California","county":"Eldorado County","otherGeospatial":"Pilliken area","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -121.011,\n              38.792\n            ],\n            [\n              -121.081,\n              38.792\n            ],\n            [\n              -121.081,\n              38.858\n            ],\n            [\n              -121.011,\n              38.858\n            ],\n            [\n              -121.011,\n              38.792\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49dde4b07f02db5e2099","contributors":{"authors":[{"text":"Wells, Francis Gerritt","contributorId":38628,"corporation":false,"usgs":true,"family":"Wells","given":"Francis","email":"","middleInitial":"Gerritt","affiliations":[],"preferred":false,"id":215911,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Page, Lincoln R.","contributorId":63367,"corporation":false,"usgs":true,"family":"Page","given":"Lincoln R.","affiliations":[],"preferred":false,"id":215912,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"James, Harold Lloyd","contributorId":64631,"corporation":false,"usgs":true,"family":"James","given":"Harold","email":"","middleInitial":"Lloyd","affiliations":[],"preferred":false,"id":215913,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":34937,"text":"b901 - 1940 - Clay investigations in the southern states 1934-35","interactions":[],"lastModifiedDate":"2025-05-07T20:29:07.873995","indexId":"b901","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1940","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":"901","title":"Clay investigations in the southern states 1934-35","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/b901","usgsCitation":"Lang, W., King, P.B., Bramlette, M., McVay, T.N., Bay, H.S., Munyan, A.C., and Mansfield, G.R., 1940, Clay investigations in the southern states 1934-35: U.S. Geological Survey Bulletin 901, Report: x, 346 p.; 1 Plate: 32.42 × 26.40 inches, https://doi.org/10.3133/b901.","productDescription":"Report: x, 346 p.; 1 Plate: 32.42 × 26.40 inches","costCenters":[],"links":[{"id":485527,"rank":8,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_21073.htm","text":"Preliminary investigations of Florida bleaching clays","linkFileType":{"id":5,"text":"html"}},{"id":485526,"rank":7,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_21075.htm","text":"The bleaching clays of Georgia","linkFileType":{"id":5,"text":"html"}},{"id":485525,"rank":6,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_21074.htm","text":"Some ceramic clays in Alabama","linkFileType":{"id":5,"text":"html"}},{"id":403428,"rank":5,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_21072.htm","text":"Clay deposits of the San Antonio area and Morris County, Texas","linkFileType":{"id":5,"text":"html"}},{"id":485524,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_21076.htm","text":"The sedimentary kaolinitic clays of South Carolina","linkFileType":{"id":5,"text":"html"}},{"id":93004,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/0901/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":162962,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/0901/report-thumb.jpg"},{"id":93005,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/0901/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49d6e4b07f02db5de280","contributors":{"authors":[{"text":"Lang, Walter B.","contributorId":27507,"corporation":false,"usgs":true,"family":"Lang","given":"Walter B.","affiliations":[],"preferred":false,"id":213841,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"King, Philip Burke","contributorId":15607,"corporation":false,"usgs":true,"family":"King","given":"Philip","email":"","middleInitial":"Burke","affiliations":[],"preferred":false,"id":213840,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Bramlette, M. N.","contributorId":105727,"corporation":false,"usgs":true,"family":"Bramlette","given":"M. N.","affiliations":[],"preferred":false,"id":213846,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"McVay, Thomas Newkirk","contributorId":75199,"corporation":false,"usgs":true,"family":"McVay","given":"Thomas","email":"","middleInitial":"Newkirk","affiliations":[],"preferred":false,"id":213842,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Bay, Harry S.","contributorId":89191,"corporation":false,"usgs":true,"family":"Bay","given":"Harry","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":213844,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Munyan, Arthur Claude","contributorId":105353,"corporation":false,"usgs":true,"family":"Munyan","given":"Arthur","email":"","middleInitial":"Claude","affiliations":[],"preferred":false,"id":213845,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Mansfield, George Rogers","contributorId":75506,"corporation":false,"usgs":true,"family":"Mansfield","given":"George","email":"","middleInitial":"Rogers","affiliations":[],"preferred":false,"id":213843,"contributorType":{"id":1,"text":"Authors"},"rank":7}]}}
,{"id":38013,"text":"wl170 - 1940 - The annual fur catch of the United States","interactions":[],"lastModifiedDate":"2012-02-02T00:16:00","indexId":"wl170","displayToPublicDate":"1972-01-01T12:27:00","publicationYear":"1940","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":98,"text":"Wildlife Leaflet","active":false,"publicationSubtype":{"id":1}},"seriesNumber":"170","title":"The annual fur catch of the United States","language":"ENGLISH","publisher":"U.S. Fish and Wildlife Service","usgsCitation":"Division Of Wildlife Research, 1940, The annual fur catch of the United States: Wildlife Leaflet 170, 21 p.","productDescription":"21 p.","costCenters":[],"links":[{"id":112355,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://hdl.handle.net/2027/mdp.39015006161924?urlappend=%3Bseq=641"},{"id":204459,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505ba9c0e4b08c986b3224b0","contributors":{"authors":[{"text":"Division Of Wildlife Research","contributorId":128086,"corporation":true,"usgs":false,"organization":"Division Of Wildlife Research","id":529806,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70206794,"text":"70206794 - 1940 - Stratigraphic measurements in parallel folds","interactions":[],"lastModifiedDate":"2019-11-21T15:20:35","indexId":"70206794","displayToPublicDate":"1940-12-31T15:10:03","publicationYear":"1940","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1786,"text":"Geological Society of America Bulletin","active":true,"publicationSubtype":{"id":10}},"title":"Stratigraphic measurements in parallel folds","docAbstract":"<p>Folded rocks having bedding surfaces which are approximately parallel are said to lie in parallel folds. Utilizing the principle of evolutes and involutes, the author offers a more precise definition of parallel folds and points out inconsistencies in other concepts. With the idea of classifying parallel folds and possibly of deducing the mechanics of their formation, methods are presented for obtaining the differential equations of the families of involutes which, in certain cross sections, represent the traces of stratigraphic surfaces; and for obtaining the equations of the corresponding evolutes. Geometric methods are also given. These equations and geometric constructions may be deduced either from assumed structural postulates or from actual field data. Another part of the paper deals with the application of mean trigonometric functions to the measurement of thickness of strata, depth and distance to a stratum, and other stratigraphic dimensions in sections oblique to the strike of the rocks. This topic is considered under two headings: (1) where such measurements can be made from data collected at several stations along a line of traverse, and (2) where they must be made from a series of structural observations, considered in pairs. In the first case, no assumption is made regarding the curvature of the strata, but instead the mean values of the required functions are derived by mechanical integration. In the second case, the usual assumption of circular curvature is made, and the necessary functions are obtained by the use of definite integrals. Tables of the logarithms of these mean functions, with an increment of 5 degrees for the argument, are also presented. © 1940 Geological Society of America.</p>","language":"English ","publisher":"Geological Society of America","doi":"10.1130/GSAB-51-1107","issn":" 00167606","usgsCitation":"Mertie, J., 1940, Stratigraphic measurements in parallel folds: Geological Society of America Bulletin, v. 51, no. 8, p. 1107-1134, https://doi.org/10.1130/GSAB-51-1107.","productDescription":"28 p. ","startPage":"1107","endPage":"1134","costCenters":[],"links":[{"id":369416,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"51","issue":"8","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Mertie, J.B. Jr.","contributorId":29383,"corporation":false,"usgs":false,"family":"Mertie","given":"J.B.","suffix":"Jr.","affiliations":[],"preferred":false,"id":775763,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70206708,"text":"70206708 - 1940 - Glacial chronology of the Southern Rocky Mountains","interactions":[],"lastModifiedDate":"2019-11-18T13:05:00","indexId":"70206708","displayToPublicDate":"1940-12-31T12:59:54","publicationYear":"1940","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1786,"text":"Geological Society of America Bulletin","active":true,"publicationSubtype":{"id":10}},"title":"Glacial chronology of the Southern Rocky Mountains","docAbstract":"<p><span>In order to extend the chronology and validate the five substages of the Wisconsin glaciation recognized in the Cache la Poudre Valley in the Colorado Front Range, a reconnaissance was made of the Southern Rocky Mountains, from southern Wyoming to Santa Fe, New Mexico. The chronology determined in the Cache la Poudre Valley was used to date the culture layer of the Lindenmeier (Folsom) Site in northern Colorado. The earliest or Twin Lakes substage is named for the \"early moraine\" mapped by Capps at Twin Lakes in the Upper Arkansas Valley. This substage is believed to have been contemporaneous with the Durango glaciation of the San Juan Mountains. Throughout the Southern Rocky Mountains the second, third, and fourth, or Home, Corral Creek, and Long Draw substages, can be readily correlated from valley to valley. The fifth or youngest substage, represented in some cirques by protalus ramparts, is named the Sprague substage. The validity of five distinct substages of Wisconsin ice advance, separated from one another by interstadial ice retreat or complete disappearance, is based on: (1) the character and topographic position of the moraines; (2) the relationship between successive terraces (valley trains) and the terminal moraines, as determined in the Cache la Poudre Valley; (3) the differences in weathering of the tills composing the moraines; and (4) the reported finding of an old soil zone between tills assigned to the Twin Lakes and Home substages. © 1940 Geological Society of America.</span></p>","language":"English","publisher":"Geological Society of America","doi":"10.1130/GSAB-51-1851","issn":"00167606","usgsCitation":"Ray, L., 1940, Glacial chronology of the Southern Rocky Mountains: Geological Society of America Bulletin, v. 51, no. 12, p. 1851-1917, https://doi.org/10.1130/GSAB-51-1851.","productDescription":"67 p. ","startPage":"1851","endPage":"1917","costCenters":[],"links":[{"id":369291,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"51","issue":"12","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Ray, L.L.","contributorId":73741,"corporation":false,"usgs":true,"family":"Ray","given":"L.L.","email":"","affiliations":[],"preferred":false,"id":775502,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":38015,"text":"38015 - 1940 - Suggestions for combating objectionable roosts of birds with special reference to those of starlings","interactions":[],"lastModifiedDate":"2014-07-21T10:36:55","indexId":"38015","displayToPublicDate":"1940-12-01T10:35:56","publicationYear":"1940","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":98,"text":"Wildlife Leaflet","active":false,"publicationSubtype":{"id":1}},"seriesNumber":"172","title":"Suggestions for combating objectionable roosts of birds with special reference to those of starlings","docAbstract":"No abstract available.","language":"English","publisher":"U.S. Department of the Interior","publisherLocation":"Washington, D.C.","usgsCitation":"Kalmbach, E., 1940, Suggestions for combating objectionable roosts of birds with special reference to those of starlings (Reissued with slight revisions from Wildlife Leaflet BS-81 (1937).): Wildlife Leaflet 172, 18 p.","productDescription":"18 p.","numberOfPages":"18","costCenters":[],"links":[{"id":290541,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"edition":"Reissued with slight revisions from Wildlife Leaflet BS-81 (1937).","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53cd7509e4b0b29085109fdf","contributors":{"authors":[{"text":"Kalmbach, E.R.","contributorId":21610,"corporation":false,"usgs":true,"family":"Kalmbach","given":"E.R.","email":"","affiliations":[],"preferred":false,"id":218744,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70174986,"text":"70174986 - 1940 - Geology and ground-water resources of the \"Equus beds\" area in south central Kansas","interactions":[],"lastModifiedDate":"2016-07-26T09:52:10","indexId":"70174986","displayToPublicDate":"1940-11-27T18:30:00","publicationYear":"1940","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":"Geology and ground-water resources of the \"Equus beds\" area in south central Kansas","docAbstract":"<p>This paper summarizes the results of a detailed investigation by the U. S. Geological Survey in cooperation with the Kansas State Geological Survey, Kansas State Board of Health, and the City of Wichita. The geology of the area has been remapped, and several new formations have been established, including the Emma Creek formation of middle and upper Pliocene age, and a thick loess deposit. The hydrologic studies involved extensive test drilling and resulted in the development of a new groundwater supply for the City of Wichita.</p>","language":"English","publisher":"Society of Economic Geologists, Inc","doi":"10.2113/gsecongeo.35.7.839","usgsCitation":"Lohman, S.W., and Frye, J.C., 1940, Geology and ground-water resources of the \"Equus beds\" area in south central Kansas: Economic Geology, v. 35, no. 7, p. 839-866, https://doi.org/10.2113/gsecongeo.35.7.839.","productDescription":"28 p.","startPage":"839","endPage":"866","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":353,"text":"Kansas Water Science Center","active":false,"usgs":true}],"links":[{"id":325625,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Kansas","county":"Harvey County, McPherson County, Reno County, Sedgwick County","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-97.3722,38.1744],[-97.1538,38.1745],[-97.1537,38.0879],[-97.1528,37.9129],[-97.1514,37.4764],[-97.8068,37.4746],[-97.8075,37.7108],[-97.8073,37.7335],[-97.8416,37.7337],[-98.4666,37.7345],[-98.4666,37.8252],[-98.4718,37.8256],[-98.4735,38.0677],[-98.4734,38.103],[-98.4734,38.1184],[-98.474,38.1737],[-98.2176,38.1734],[-98.2171,38.1598],[-98.1421,38.1592],[-98.1427,38.1732],[-97.922,38.1737],[-97.9213,38.2607],[-97.9242,38.2608],[-97.9262,38.5227],[-97.9261,38.6102],[-97.372,38.61],[-97.3722,38.1744]]]},\"properties\":{\"name\":\"Harvey\",\"state\":\"KS\"}}]}","volume":"35","issue":"7","noUsgsAuthors":false,"publicationDate":"1940-11-01","publicationStatus":"PW","scienceBaseUri":"579889b5e4b0589fa1c6ba58","contributors":{"authors":[{"text":"Lohman, Stanley William","contributorId":53361,"corporation":false,"usgs":true,"family":"Lohman","given":"Stanley","email":"","middleInitial":"William","affiliations":[],"preferred":false,"id":643514,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Frye, John Chapman","contributorId":48025,"corporation":false,"usgs":true,"family":"Frye","given":"John","email":"","middleInitial":"Chapman","affiliations":[],"preferred":false,"id":643515,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":38017,"text":"38017 - 1940 - Abstract of fur laws, 1940-41","interactions":[],"lastModifiedDate":"2014-07-21T10:43:57","indexId":"38017","displayToPublicDate":"1940-10-01T10:43:29","publicationYear":"1940","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":98,"text":"Wildlife Leaflet","active":false,"publicationSubtype":{"id":1}},"seriesNumber":"174","title":"Abstract of fur laws, 1940-41","docAbstract":"No abstract available.","language":"English","publisher":"U.S. Department of the Interior","publisherLocation":"Washington, D.C.","usgsCitation":"Grimes, F.G., 1940, Abstract of fur laws, 1940-41: Wildlife Leaflet 174, 39 p.","productDescription":"39 p.","numberOfPages":"39","costCenters":[],"links":[{"id":290543,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53cd4ae8e4b0b290850f00e4","contributors":{"authors":[{"text":"Grimes, Frank G.","contributorId":101567,"corporation":false,"usgs":true,"family":"Grimes","given":"Frank","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":218746,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":38016,"text":"38016 - 1940 - Fryer rabbit production","interactions":[],"lastModifiedDate":"2014-07-21T10:39:07","indexId":"38016","displayToPublicDate":"1940-10-01T10:38:42","publicationYear":"1940","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":98,"text":"Wildlife Leaflet","active":false,"publicationSubtype":{"id":1}},"seriesNumber":"173","title":"Fryer rabbit production","docAbstract":"No abstract available.","language":"English","publisher":"U.S. Department of the Interior","publisherLocation":"Washington, D.C.","usgsCitation":"Templeton, G.S., 1940, Fryer rabbit production: Wildlife Leaflet 173, 10 p.","productDescription":"10 p.","numberOfPages":"10","costCenters":[],"links":[{"id":290542,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53cd5a57e4b0b290850f9493","contributors":{"authors":[{"text":"Templeton, George S.","contributorId":22252,"corporation":false,"usgs":true,"family":"Templeton","given":"George","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":218745,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70243782,"text":"70243782 - 1940 - The northern copperhead in Iowa","interactions":[],"lastModifiedDate":"2023-05-19T14:34:17.651232","indexId":"70243782","displayToPublicDate":"1940-10-01T09:28:39","publicationYear":"1940","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":14431,"text":"Iowa State College Journal of Science","active":true,"publicationSubtype":{"id":10}},"title":"The northern copperhead in Iowa","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"Iowa State College","usgsCitation":"Bailey, R.M., 1940, The northern copperhead in Iowa: Iowa State College Journal of Science, v. 15, no. 1, p. 1-2.","productDescription":"2 p.","startPage":"1","endPage":"2","costCenters":[],"links":[{"id":417242,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":417241,"rank":1,"type":{"id":15,"text":"Index 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,{"id":70214036,"text":"70214036 - 1940 - The new international commission of snow and glaciers","interactions":[],"lastModifiedDate":"2020-09-22T13:29:52.448918","indexId":"70214036","displayToPublicDate":"1940-09-21T11:38:24","publicationYear":"1940","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3338,"text":"Science","active":true,"publicationSubtype":{"id":10}},"title":"The new international commission of snow and glaciers","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"American Association for the Advancement of Science","doi":"10.1126/science.91.2361.317","usgsCitation":"Matthes, F., 1940, The new international commission of snow and glaciers: Science, v. 91, no. 2361, p. 317-318, https://doi.org/10.1126/science.91.2361.317.","productDescription":"2 p.","startPage":"317","endPage":"318","costCenters":[],"links":[{"id":378624,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"91","issue":"2361","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Matthes, Francois E.","contributorId":240914,"corporation":false,"usgs":false,"family":"Matthes","given":"Francois E.","affiliations":[],"preferred":false,"id":799321,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70213895,"text":"70213895 - 1940 - Channel‐storage and unit‐hydrograph studies","interactions":[],"lastModifiedDate":"2020-09-18T20:30:08.504931","indexId":"70213895","displayToPublicDate":"1940-09-18T15:26:28","publicationYear":"1940","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1578,"text":"Eos, Transactions, American Geophysical Union","onlineIssn":"2324-9250","printIssn":"0096-394","active":true,"publicationSubtype":{"id":10}},"title":"Channel‐storage and unit‐hydrograph studies","docAbstract":"<p><span>Recent studies of the rainfal‐and‐runoff relation tend towards treatment of the subject in two parts, namely, (1) the ground‐phase, which includes the study of such processes as infiltration and evaporation, and (2) the channel‐phase, which comprehends the study of the flow of water in the channel‐system with particular reference to flood‐wave movement. This paper discusses the channel‐phase.</span></p>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR021i002p00620","usgsCitation":"Langbein, W.B., 1940, Channel‐storage and unit‐hydrograph studies: Eos, Transactions, American Geophysical Union, v. 21, no. 2, p. 620-627, https://doi.org/10.1029/TR021i002p00620.","productDescription":"8 p.","startPage":"620","endPage":"627","costCenters":[],"links":[{"id":378583,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"21","issue":"2","noUsgsAuthors":false,"publicationDate":"2014-08-18","publicationStatus":"PW","contributors":{"authors":[{"text":"Langbein, W. B.","contributorId":102053,"corporation":false,"usgs":true,"family":"Langbein","given":"W.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":799255,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70213893,"text":"70213893 - 1940 - Remarques sur les méthodes brock et multiplex","interactions":[],"lastModifiedDate":"2020-09-18T20:17:50.743374","indexId":"70213893","displayToPublicDate":"1940-09-18T15:15:38","publicationYear":"1940","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3050,"text":"Photogrammetria","active":true,"publicationSubtype":{"id":10}},"title":"Remarques sur les méthodes brock et multiplex","docAbstract":"<p>No abstract available.</p>","language":"French","publisher":"Elsevier","doi":"10.1016/S0031-8663(40)80027-6","usgsCitation":"Pendleton, M., 1940, Remarques sur les méthodes brock et multiplex: Photogrammetria, v. 3, no. 4, p. 157-158, https://doi.org/10.1016/S0031-8663(40)80027-6.","productDescription":"2 p.","startPage":"157","endPage":"158","costCenters":[],"links":[{"id":378581,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"3","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Pendleton, M.T.P.","contributorId":56791,"corporation":false,"usgs":true,"family":"Pendleton","given":"M.T.P.","email":"","affiliations":[],"preferred":false,"id":799253,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70213883,"text":"70213883 - 1940 - Oilfields of the United States","interactions":[],"lastModifiedDate":"2020-09-18T20:50:20.127845","indexId":"70213883","displayToPublicDate":"1940-09-18T15:10:14","publicationYear":"1940","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2840,"text":"Nature","active":true,"publicationSubtype":{"id":10}},"title":"Oilfields of the United States","docAbstract":"<p>The <span>modern petroleum industry in the United States of America dates from the drilling of the first commercial oil well in 1859. Up to the present, about a million wells have been drilled for oil and gas, and the total production of petroleum has been 22,452,498,000 barrels, which has been contributed by twenty-three of the forty-eight States.</span></p>","language":"English","publisher":"Nature Research","doi":"10.1038/146437a0","usgsCitation":"Miser, H.D., 1940, Oilfields of the United States: Nature, v. 146, no. 3700, https://doi.org/10.1038/146437a0.","productDescription":"1 p.","startPage":"437","costCenters":[],"links":[{"id":480458,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1038/146437a0","text":"Publisher Index Page"},{"id":378580,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"146","issue":"3700","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Miser, Hugh D.","contributorId":32508,"corporation":false,"usgs":true,"family":"Miser","given":"Hugh","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":799252,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70213873,"text":"70213873 - 1940 - The Vaucluse gold mine, Orange County, Virginia","interactions":[],"lastModifiedDate":"2020-09-18T20:52:06.704491","indexId":"70213873","displayToPublicDate":"1940-09-18T14:55:09","publicationYear":"1940","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":"The Vaucluse gold mine, Orange County, Virginia","docAbstract":"<p><span>The Vaucluse gold property has been worked intermittently since gold was discovered in 1832. The latest operation was carried on by the V-M Corporation from March 1935 to November 1938, producing 26,452 tons of ore of \\$143,760 gross value, of which \\$91,569.36 was won in 1938.</span></p><p><span>The host rock is a quartz-sericite-chlorite schist. The workings lie wholly within a well-defined shear zone up to 40 feet in width, which has been traced along the surface for several miles. The shear zone strikes N. 40 degrees -60 degrees E. and is conformable with the schistosity of the enclosing rock.</span></p><p><span>The ore is in shoots that pitch NE. at angles ranging between 30 degrees and 70 degrees and conform to fluting in the shear zone. The ore occurs along the walls of the shear zone and the location of the shoots was controlled, partly at least, by pre-mineral fractures.</span></p><p><span>Quartz, sericite, and ankerite make up most of the gangue and chlorite is abundant in the enclosing rock. Abundant pyrite is the only important sulphide; some chalcopyrite and galena are generally present. Gold is the only mineral of economic value and is intimately associated with the pyrite.</span></p><p><span>The ore was milled on the property and flotation concentrates were shipped to a smelter. Direct mining, milling, and shipping cost per ton, from December 1935 to November 1938, was $4.56. Approximately 4,500 feet of core drilling was done below the 300-foot level, which indicated about the same conditions as those present above this level.</span></p>","language":"English","publisher":"Society of Economic Geologist","doi":"10.2113/gsecongeo.35.1.79","usgsCitation":"Bass, C.E., 1940, The Vaucluse gold mine, Orange County, Virginia: Economic Geology, v. 35, no. 1, p. 79-91, https://doi.org/10.2113/gsecongeo.35.1.79.","productDescription":"13 p.","startPage":"79","endPage":"91","costCenters":[],"links":[{"id":378579,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Virginia","county":"Orange County","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-77.7043,38.3619],[-77.7103,38.3547],[-77.7158,38.3453],[-77.7206,38.3417],[-77.7166,38.3367],[-77.7232,38.3331],[-77.7269,38.325],[-77.7413,38.3125],[-77.7473,38.3067],[-77.7503,38.3041],[-77.7599,38.2956],[-77.96,38.1192],[-77.9699,38.1221],[-77.9787,38.1208],[-77.9845,38.1227],[-77.9948,38.1333],[-77.9983,38.136],[-78.0018,38.1365],[-78.0094,38.1362],[-78.0146,38.138],[-78.0199,38.1404],[-78.024,38.1404],[-78.0293,38.1382],[-78.0393,38.1356],[-78.0562,38.1381],[-78.0661,38.1418],[-78.0713,38.1428],[-78.0772,38.1433],[-78.0899,38.1489],[-78.094,38.1521],[-78.1051,38.1522],[-78.1133,38.1496],[-78.1146,38.1446],[-78.1187,38.1415],[-78.1264,38.1407],[-78.1351,38.1412],[-78.1427,38.1445],[-78.1444,38.1445],[-78.1486,38.14],[-78.1522,38.1382],[-78.1627,38.1375],[-78.1692,38.1339],[-78.1914,38.1341],[-78.2079,38.1307],[-78.3365,38.1777],[-78.3691,38.1858],[-78.2892,38.2716],[-78.2875,38.2711],[-78.2834,38.2702],[-78.2782,38.2678],[-78.2729,38.2655],[-78.2671,38.2605],[-78.2684,38.2564],[-78.2696,38.2519],[-78.2662,38.2482],[-78.2598,38.2418],[-78.2564,38.2386],[-78.2511,38.2363],[-78.2494,38.234],[-78.2365,38.2339],[-78.2348,38.2339],[-78.2296,38.2315],[-78.2237,38.2319],[-78.2201,38.2342],[-78.2171,38.2418],[-78.2112,38.2427],[-78.2071,38.2426],[-78.1959,38.2457],[-78.1929,38.247],[-78.1893,38.2529],[-78.1816,38.2596],[-78.1821,38.2646],[-78.1826,38.2668],[-78.1796,38.2695],[-78.1732,38.269],[-78.1697,38.2694],[-78.1662,38.2699],[-78.1591,38.2684],[-78.1585,38.2716],[-78.1602,38.277],[-78.1589,38.282],[-78.1565,38.2838],[-78.1524,38.2847],[-78.1466,38.2796],[-78.1443,38.28],[-78.1407,38.2836],[-78.1342,38.2836],[-78.1302,38.2817],[-78.1261,38.2826],[-78.123,38.2898],[-78.1118,38.2942],[-78.1081,38.2991],[-78.0992,38.3058],[-78.0967,38.3139],[-78.0909,38.3143],[-78.0844,38.3165],[-78.0797,38.3142],[-78.0745,38.3119],[-78.0692,38.3118],[-78.0632,38.3163],[-78.0585,38.3176],[-78.0527,38.3166],[-78.0416,38.3142],[-78.0392,38.3151],[-78.0408,38.3219],[-78.0349,38.3277],[-78.0301,38.3304],[-78.0189,38.3357],[-78.0081,38.3442],[-77.9957,38.349],[-77.9904,38.3499],[-77.9805,38.347],[-77.9775,38.3465],[-77.9758,38.3483],[-77.9762,38.3533],[-77.9756,38.3578],[-77.9714,38.3587],[-77.9668,38.3582],[-77.9597,38.3558],[-77.955,38.3571],[-77.9526,38.3607],[-77.9491,38.3625],[-77.942,38.3624],[-77.9255,38.3658],[-77.9208,38.3671],[-77.9166,38.3702],[-77.9106,38.3756],[-77.9094,38.3792],[-77.9069,38.3828],[-77.8986,38.3859],[-77.8903,38.3898],[-77.888,38.3871],[-77.8852,38.3825],[-77.8812,38.3802],[-77.8729,38.3815],[-77.8652,38.3832],[-77.8599,38.384],[-77.8547,38.3839],[-77.8494,38.3834],[-77.843,38.3779],[-77.8395,38.3769],[-77.8377,38.3792],[-77.8341,38.3818],[-77.8294,38.3827],[-77.823,38.3817],[-77.816,38.3807],[-77.8084,38.3792],[-77.798,38.3723],[-77.7898,38.3694],[-77.7823,38.3657],[-77.7788,38.3652],[-77.7764,38.3652],[-77.7752,38.3661],[-77.7763,38.3688],[-77.7798,38.3716],[-77.7862,38.3744],[-77.7873,38.3776],[-77.7848,38.3812],[-77.7818,38.3857],[-77.7782,38.3901],[-77.7734,38.3928],[-77.7687,38.3923],[-77.7641,38.3909],[-77.76,38.389],[-77.7554,38.3862],[-77.7472,38.3834],[-77.7467,38.3784],[-77.7409,38.376],[-77.7334,38.3727],[-77.7205,38.3703],[-77.713,38.3675],[-77.7066,38.3628],[-77.7043,38.3619]]]},\"properties\":{\"name\":\"Orange\",\"state\":\"VA\"}}]}","volume":"35","issue":"1","noUsgsAuthors":false,"publicationDate":"1940-01-01","publicationStatus":"PW","contributors":{"authors":[{"text":"Bass, Charles Edward","contributorId":240985,"corporation":false,"usgs":false,"family":"Bass","given":"Charles","email":"","middleInitial":"Edward","affiliations":[],"preferred":false,"id":799251,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70213863,"text":"70213863 - 1940 - Salinity of the lower Savannah River in relation to stream‐flow and tidal action","interactions":[],"lastModifiedDate":"2020-09-18T20:53:55.899578","indexId":"70213863","displayToPublicDate":"1940-09-18T14:35:06","publicationYear":"1940","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1578,"text":"Eos, Transactions, American Geophysical Union","onlineIssn":"2324-9250","printIssn":"0096-394","active":true,"publicationSubtype":{"id":10}},"title":"Salinity of the lower Savannah River in relation to stream‐flow and tidal action","docAbstract":"<p>In order to obtain information needed in planning for industrial development along the Savannah River and in the city of Savannah, Georgia, a study of the salinity of the Savannah River was undertaken by the Geological Survey, United States Department of the Interior, in cooperation with the Georgia Division of Mines, Mining, and Geology. The Works Progress Administration of Georgia and the city of Savannah also cooperated in the study.</p><p>The Savannah River lies on the boundary between the States of Georgia and South Carolina. The River proper from the mouth to the junction of the Tugaloo and Senaca rivers is 314 miles in length. The area of its watershed is about 10,579 square miles, of which 9,850 square miles are above the stream‐flow gaging‐station near Clyo, Georgia. The River is tidal for about 50 miles above its mouth. The average streamflow for the Savannah River near Clyo, Georgia, was 10,410 and 10,820 second‐feet, respectively, for the years ending September 30, 1938 and 1939. The city of Savannah, Georgia, located on the Savannah River 17 miles above its mouth, is an important seaport and industrial center. The lower Savannah River near the city of Savannah is shown in Figure 1.</p>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR021i002p00463","usgsCitation":"Lamar, W.L., 1940, Salinity of the lower Savannah River in relation to stream‐flow and tidal action: Eos, Transactions, American Geophysical Union, v. 21, no. 2, p. 463-470, https://doi.org/10.1029/TR021i002p00463.","productDescription":"8 p.","startPage":"463","endPage":"470","costCenters":[],"links":[{"id":378578,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Georgia, South Carolina","otherGeospatial":"Savannah River","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -81.14227294921875,\n              31.962648655655887\n            ],\n            [\n              -80.81954956054688,\n              31.962648655655887\n            ],\n            [\n              -80.81954956054688,\n              32.19304652202036\n            ],\n            [\n              -81.14227294921875,\n              32.19304652202036\n            ],\n            [\n              -81.14227294921875,\n              31.962648655655887\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"21","issue":"2","noUsgsAuthors":false,"publicationDate":"2014-08-18","publicationStatus":"PW","contributors":{"authors":[{"text":"Lamar, William L.","contributorId":15592,"corporation":false,"usgs":true,"family":"Lamar","given":"William","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":799250,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70213853,"text":"70213853 - 1940 - On the flow of water in an elastic artesian aquifer","interactions":[],"lastModifiedDate":"2020-09-18T19:33:42.068559","indexId":"70213853","displayToPublicDate":"1940-09-18T14:23:23","publicationYear":"1940","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1578,"text":"Eos, Transactions, American Geophysical Union","onlineIssn":"2324-9250","printIssn":"0096-394","active":true,"publicationSubtype":{"id":10}},"title":"On the flow of water in an elastic artesian aquifer","docAbstract":"<p>Slichter showed in 1898 that a solution may be obtained for a given problem in the steady motion of ground‐water by solving the familiar Laplace equation and that therefore in steady‐state conditions a problem in the motion of ground‐water is mathematically analogous to a problem in the steady flow of heat or electricity [see 1 of “References” at end of paper]. More recently it has been recognized that the analogy holds also for the non‐steady‐state flow of compressible liquids, in elastic systems as well as in rigid systems.</p><p>In studying the effect of the discharge of flowing wells on the head in the Dakota sandstone, Meinzer [2, 3] concluded that the water discharged by the wells had largely been derived locally from storage. It was found that the amount of water withdrawn from storage could not be accounted for on the basis of the compressibility of water alone but that it might be accounted for on the basis of the probable compressibility of the sandstone itself. Prior to that time, estimates of water‐supplies from artesian aquifers had been based upon the assumption that artesian aquifers are perfectly incompressible and inelastic However, as Meinzer states [2, p. 289], “artesian aquifers are apparently all more or less compressible and elastic though they differ widely in the degree and relative importance of these properties. In general, the properties of compressibility and elasticity are of the most consequence in aquifers that have low permeability, slow recharge, and high head.”</p>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR021i002p00574","usgsCitation":"Jacob, C.E., 1940, On the flow of water in an elastic artesian aquifer: Eos, Transactions, American Geophysical Union, v. 21, no. 2, p. 574-586, https://doi.org/10.1029/TR021i002p00574.","productDescription":"13 p.","startPage":"574","endPage":"586","costCenters":[],"links":[{"id":378577,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"21","issue":"2","noUsgsAuthors":false,"publicationDate":"2014-08-18","publicationStatus":"PW","contributors":{"authors":[{"text":"Jacob, C. E.","contributorId":64504,"corporation":false,"usgs":true,"family":"Jacob","given":"C.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":799249,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70213852,"text":"70213852 - 1940 - Additional evidence on the relation of temperature to structure in the Salt Creek Oil field, Natrona County, Wyoming ","interactions":[],"lastModifiedDate":"2020-09-18T20:55:35.527682","indexId":"70213852","displayToPublicDate":"1940-09-18T14:17:56","publicationYear":"1940","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1808,"text":"Geophysics","active":true,"publicationSubtype":{"id":10}},"title":"Additional evidence on the relation of temperature to structure in the Salt Creek Oil field, Natrona County, Wyoming ","docAbstract":"<p>Observations of bottom hole temperatures in approximately 100 deep wells in the Salt Creek field have been made during the past few years by the Stanolind Oil and Gas Company. These recent observations confirm and extend in a remarkable manner the results obtained in the summers of 1922 and 1923&nbsp; when it was found from temperature surveys in 21 wells that the temperatures over a considerable portion of the field were definitely related to the structure. </p>","language":"English","publisher":"Society of Economic Geophysicists","doi":"10.1190/1.1441793","usgsCitation":"Van Orstrand, C.E., 1940, Additional evidence on the relation of temperature to structure in the Salt Creek Oil field, Natrona County, Wyoming : Geophysics, v. 5, no. 1, p. 47-56, https://doi.org/10.1190/1.1441793.","productDescription":"10 p.","startPage":"47","endPage":"56","costCenters":[],"links":[{"id":378576,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Wyoming","county":"Natrona County","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-107.1077,43.4996],[-107.1078,43.4942],[-107.0478,43.4947],[-107.0144,43.4949],[-106.9014,43.4949],[-106.8743,43.4951],[-106.8333,43.4943],[-106.774,43.4942],[-106.5948,43.4938],[-106.5569,43.4938],[-106.5152,43.4938],[-106.502,43.4941],[-106.4824,43.4939],[-106.4629,43.4941],[-106.4433,43.4939],[-106.4042,43.4944],[-106.3884,43.4937],[-106.3284,43.4943],[-106.3089,43.4945],[-106.2887,43.4943],[-106.2477,43.4942],[-106.0671,43.4944],[-106.0671,43.4734],[-106.0683,43.387],[-106.0687,43.3706],[-106.0696,43.3415],[-106.0705,43.2851],[-106.0709,43.271],[-106.0711,43.241],[-106.0715,43.2268],[-106.0717,43.154],[-106.0721,43.1395],[-106.072,43.0972],[-106.0724,43.0826],[-106.0724,43.039],[-106.0722,43.0235],[-106.0726,43.0089],[-106.0699,42.8588],[-106.0684,42.7792],[-106.0765,42.7789],[-106.0753,42.6643],[-106.0755,42.5898],[-106.0753,42.5752],[-106.075,42.5193],[-106.0735,42.4611],[-106.0749,42.4325],[-106.1054,42.4325],[-106.1228,42.4323],[-106.1265,42.4328],[-106.1464,42.4326],[-106.239,42.4321],[-106.2471,42.4317],[-106.2651,42.4315],[-106.3235,42.4314],[-106.3434,42.4312],[-106.3546,42.4309],[-106.3658,42.431],[-106.4323,42.4305],[-106.4435,42.4306],[-106.474,42.4305],[-106.4814,42.4306],[-106.5137,42.431],[-106.5336,42.4312],[-106.592,42.4314],[-106.6007,42.4315],[-106.6088,42.4311],[-106.6187,42.4312],[-106.6864,42.4315],[-106.7076,42.4317],[-106.7169,42.4322],[-106.738,42.4324],[-106.7834,42.4324],[-106.7958,42.4325],[-106.8219,42.4328],[-106.8362,42.4324],[-106.8492,42.4321],[-106.8642,42.4322],[-106.8747,42.4323],[-106.9387,42.4333],[-106.9412,42.4333],[-106.9455,42.4334],[-106.9574,42.433],[-106.9704,42.4331],[-107.0742,42.4343],[-107.0934,42.4345],[-107.173,42.4346],[-107.1916,42.4347],[-107.2885,42.4343],[-107.3084,42.4349],[-107.3457,42.4346],[-107.3873,42.4344],[-107.4041,42.4345],[-107.4234,42.4341],[-107.4426,42.4342],[-107.5209,42.4336],[-107.5408,42.4332],[-107.5414,42.4473],[-107.5412,42.465],[-107.5412,42.4791],[-107.5411,42.4918],[-107.5415,42.5182],[-107.5421,42.52],[-107.542,42.5341],[-107.5419,42.5486],[-107.5416,42.5932],[-107.5422,42.6077],[-107.5421,42.6222],[-107.542,42.635],[-107.5418,42.6568],[-107.5416,42.6968],[-107.5415,42.7113],[-107.5429,42.7813],[-107.4992,42.7812],[-107.4989,42.8244],[-107.4994,42.8394],[-107.4993,42.8539],[-107.4998,42.8676],[-107.4995,42.9108],[-107.4999,42.9403],[-107.4998,42.9567],[-107.502,42.9995],[-107.5025,43.014],[-107.5024,43.0286],[-107.5017,43.0431],[-107.4941,43.1295],[-107.5142,43.1296],[-107.5131,43.2024],[-107.513,43.2146],[-107.5127,43.2551],[-107.5124,43.2993],[-107.5121,43.342],[-107.5114,43.3566],[-107.5124,43.3862],[-107.5108,43.428],[-107.5105,43.4722],[-107.5351,43.4718],[-107.5343,43.4991],[-107.5116,43.4995],[-107.4914,43.4994],[-107.4731,43.4998],[-107.4504,43.4997],[-107.3513,43.4988],[-107.2314,43.5],[-107.203,43.4998],[-107.1847,43.4997],[-107.1456,43.4994],[-107.1077,43.4996]]]},\"properties\":{\"name\":\"Natrona\",\"state\":\"WY\"}}]}","volume":"5","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Van Orstrand, C. E.","contributorId":37231,"corporation":false,"usgs":true,"family":"Van Orstrand","given":"C.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":799248,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70213842,"text":"70213842 - 1940 - A brief review of ground‐water conditions in Michigan","interactions":[],"lastModifiedDate":"2020-09-18T20:57:02.601391","indexId":"70213842","displayToPublicDate":"1940-09-18T13:59:19","publicationYear":"1940","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1578,"text":"Eos, Transactions, American Geophysical Union","onlineIssn":"2324-9250","printIssn":"0096-394","active":true,"publicationSubtype":{"id":10}},"title":"A brief review of ground‐water conditions in Michigan","docAbstract":"<p><span>The State of Michigan makes up about one‐half of the area of the great Michigan Synclinal Basin, the remainder of which embraces Lakes Michigan and Huron and small parts of Wisconsin, Illinois, Indiana, Ohio, and Ontario [see 1 (p. 7) of “References” at end of paper]. The Basin has characteristics of both a geosyncline and a major structural basin. The geosynclinal origin is indicated by the facts that the Basin has been progressively downwarped, the beds thicken markedly into the central area, the outline of the course of the outcropping rocks is roughly oval, and the minor structures within the Basin are mostly parallel to the longer diameter of the downwarp. Evidence of several periods of isolation and evaporation and the absence of thick series of coarse clastic sediments in the post‐Cambrian rock‐column are features that are more characteristic of structural basins.</span></p>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR021i004p01122","usgsCitation":"McGuinness, C., 1940, A brief review of ground‐water conditions in Michigan: Eos, Transactions, American Geophysical Union, v. 21, no. 4, p. 1122-1126, https://doi.org/10.1029/TR021i004p01122.","productDescription":"5 p.","startPage":"1122","endPage":"1126","costCenters":[],"links":[{"id":378575,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United 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,{"id":70213832,"text":"70213832 - 1940 - The contamination of ground‐water by salt water near Parlin, New Jersey","interactions":[],"lastModifiedDate":"2020-09-18T20:58:18.757831","indexId":"70213832","displayToPublicDate":"1940-09-18T13:49:11","publicationYear":"1940","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1578,"text":"Eos, Transactions, American Geophysical Union","onlineIssn":"2324-9250","printIssn":"0096-394","active":true,"publicationSubtype":{"id":10}},"title":"The contamination of ground‐water by salt water near Parlin, New Jersey","docAbstract":"<p><span>The classic studies of Badon Ghyben [see 1 of “References” at end of paper] and Alexander Herzoerg [2].that defined the basic principles governing the relation between salt water and fresh water in water‐bearing sands are now fairly well known. They showed that fresh water floats on the heavier salt Water and that, under static conditions, the ratio between the head of the fresh water above mean sea‐level and the depth of the contact between fresh and salt water below mean sea‐level, is determined by the relative specific gravities of the two waters. Other studies have shown that under ordinary conditions there is little mixing between the fresh and salt waters, so that the zone of contact is narrow. Instances have been observed in which the chloride‐content of the water has ranged from a few parts to several thousand parts per million within a few feet. It would seem, therefore, that the basic conditions under which fresh and salt water occur together in water‐bearing sands are somewhat similar to those in the tidal estuaries of streams. The principal differences are caused by the frictional resistance of the sand which prevents rapid movements of both fluids and probably retards their mixing.</span></p>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR021i002p00471","usgsCitation":"Barksdale, H., 1940, The contamination of ground‐water by salt water near Parlin, New Jersey: Eos, Transactions, American Geophysical Union, v. 21, no. 2, p. 471-474, https://doi.org/10.1029/TR021i002p00471.","productDescription":"4 p.","startPage":"471","endPage":"474","costCenters":[],"links":[{"id":378574,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"New Jersey","city":"Parlin","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -74.41280364990234,\n              40.44093755756703\n            ],\n            [\n              -74.33624267578125,\n              40.44093755756703\n            ],\n            [\n              -74.33624267578125,\n              40.492653934148\n            ],\n            [\n              -74.41280364990234,\n              40.492653934148\n            ],\n            [\n              -74.41280364990234,\n              40.44093755756703\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"21","issue":"2","noUsgsAuthors":false,"publicationDate":"2014-08-18","publicationStatus":"PW","contributors":{"authors":[{"text":"Barksdale, H.C.","contributorId":65912,"corporation":false,"usgs":true,"family":"Barksdale","given":"H.C.","email":"","affiliations":[],"preferred":false,"id":799246,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70213822,"text":"70213822 - 1940 - Ground‐water recharge in areas of deep water‐table in the Great Plains","interactions":[],"lastModifiedDate":"2020-09-18T21:00:35.5027","indexId":"70213822","displayToPublicDate":"1940-09-18T13:41:29","publicationYear":"1940","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1578,"text":"Eos, Transactions, American Geophysical Union","onlineIssn":"2324-9250","printIssn":"0096-394","active":true,"publicationSubtype":{"id":10}},"title":"Ground‐water recharge in areas of deep water‐table in the Great Plains","docAbstract":"<p><span>It is unanimously agreed, I think, that of the water which falls upon the Earth's surface, a part runs off toward the sea, a part is at least temporarily detained, a part of it evaporates, and a part sinks beneath the ground‐surface. But among students of that water which sinks beneath the Earth's surface, complete agreement as to the course it then takes has not always prevailed. Ground‐water hydrologists have assumed that water can and does reach the water‐table by descending through a great thickness of subsoil in the semi‐arid upland divides of the Great Plains. But many students of soil‐moisture and its use by vegetation in the Great Plains have concluded from their soil‐moisture sampling that water does not descend to the water‐table where the depth to the water‐table is great. Thus Cole and Mathews state in Technical Bulletin 637 of the United States Department of Agriculture, page 69, that “It can be safely said, however, that on the short‐grass land of the Great Plains there is no penetration of upland surface‐water to the water‐table.”</span></p>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR021i002p00570","usgsCitation":"Cady, R., 1940, Ground‐water recharge in areas of deep water‐table in the Great Plains: Eos, Transactions, American Geophysical Union, v. 21, no. 2, p. 570-574, https://doi.org/10.1029/TR021i002p00570.","productDescription":"5 p.","startPage":"570","endPage":"574","costCenters":[],"links":[{"id":378573,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Nebraska","county":"Box Butte County, Keith County","otherGeospatial":"Great Plains","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"MultiPolygon\",\"coordinates\":[[[[-102.7742,42.4402],[-102.7499,42.4394],[-102.7498,42.3576],[-102.7477,42.3531],[-102.7476,42.2708],[-102.7428,42.1809],[-102.7431,42.0923],[-102.7035,42.0922],[-102.6989,42.0051],[-102.8149,42.0026],[-102.936,42.0022],[-103.0521,42.0027],[-103.1689,42.0021],[-103.3605,42.0037],[-103.3995,42.004],[-103.4012,42.0903],[-103.4457,42.0905],[-103.4438,42.176],[-103.4432,42.2646],[-103.4444,42.4387],[-103.361,42.4377],[-103.2416,42.4376],[-103.0893,42.4381],[-102.8885,42.4391],[-102.7742,42.4402]]],[[[-101.2702,41.3959],[-101.2688,41.0488],[-101.2487,41.0476],[-101.248,41.005],[-101.3618,41.0035],[-102.0504,41.0037],[-102.0505,41.0477],[-102.0542,41.0481],[-102.0556,41.2214],[-102.0551,41.3939],[-101.9853,41.3955],[-101.4055,41.3954],[-101.2702,41.3959]]]]},\"properties\":{\"name\":\"Box Butte\",\"state\":\"NE\"}}]}","volume":"21","issue":"2","noUsgsAuthors":false,"publicationDate":"2014-08-18","publicationStatus":"PW","contributors":{"authors":[{"text":"Cady, R.C.","contributorId":44905,"corporation":false,"usgs":true,"family":"Cady","given":"R.C.","email":"","affiliations":[],"preferred":false,"id":799245,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70213812,"text":"70213812 - 1940 - Ground‐water problems in Ohio, with special reference to the industrial area of Cincinnati in Butler and Hamilton counties","interactions":[],"lastModifiedDate":"2020-09-18T21:02:13.937359","indexId":"70213812","displayToPublicDate":"1940-09-18T13:27:42","publicationYear":"1940","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1578,"text":"Eos, Transactions, American Geophysical Union","onlineIssn":"2324-9250","printIssn":"0096-394","active":true,"publicationSubtype":{"id":10}},"title":"Ground‐water problems in Ohio, with special reference to the industrial area of Cincinnati in Butler and Hamilton counties","docAbstract":"<p><span>The importance of ground‐water as a natural resource to be used for water‐supply and industrial purposes is often overlooked by the general public. A recent survey conducted by the Engineering News‐Record [see 1 of “References” at end of paper], based on data obtained from State Sanitary engineers, shows that 9,100 out of a total of 12,700 public water‐supply systems in the United States obtain water from underground sources. Of the total population served by public water‐supplies, about 28 per cent or 22,500,000 people are served by systems using ground‐water. In addition to the quantities of water pumped for public supplies, many million gallons of ground‐water are pumped daily for rural, domestic, and industrial purposes. In many of the cities that have public supplies from surface‐sources, there is nevertheless heavy pumping from private wells for industrial purposes.</span></p>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR021i004p01126","usgsCitation":"Klaer, F., 1940, Ground‐water problems in Ohio, with special reference to the industrial area of Cincinnati in Butler and Hamilton counties: Eos, Transactions, American Geophysical Union, v. 21, no. 4, p. 1126-1131, https://doi.org/10.1029/TR021i004p01126.","productDescription":"6 p.","startPage":"1126","endPage":"1131","costCenters":[],"links":[{"id":378572,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United 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,{"id":70213811,"text":"70213811 - 1940 - Committee on chemistry of natural waters, 1939–40","interactions":[],"lastModifiedDate":"2020-09-18T21:03:03.118227","indexId":"70213811","displayToPublicDate":"1940-09-18T13:16:53","publicationYear":"1940","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1578,"text":"Eos, Transactions, American Geophysical Union","onlineIssn":"2324-9250","printIssn":"0096-394","active":true,"publicationSubtype":{"id":10}},"title":"Committee on chemistry of natural waters, 1939–40","docAbstract":"<p>The membership of this Committee is as follows: I. A. Dennison, National Bureau of Standards, Washington, D.C.; C. S. Scofield, Bureau of Plant Industry, Department of Agriculture, Washington, D.C.; D. G. Thompson, United States Geological Survey, Washington, D.C.; Prof. T. G. Thompson, University of Washington, Seattle, Washington; and C. S. Howard (Chairman), United States Geological Survey, Washington, D.C.</p><p>The Committee arranged for the presentation of the following five papers at the 1940 Spring meeting: (1) Salt‐water intrusion in the Connecticut River, by C. S. Howard, United States Geological Survey; (2) Salinity‐movement and its causes in the Delaware River Estuary, by William D. Mason and Wallace R. Pietsch, Sun Oil Company; (3) Salinity of, lower Savannah River in relation to tidal action and stream‐flow, by William L. Lamar, United States Geological Survey; (4) Corrosion of ferrous and nonferrous metals and the behavior of metallic coatings in tidal marsh, by I. A. Dennison, National Bureau of Standards; (5) The contamination of underground waters by salt water near Parlin, New Jersey, by H. C. Barksdale, United States Geological Survey.</p>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR021i002p00369","usgsCitation":"Howard, C.S., 1940, Committee on chemistry of natural waters, 1939–40: Eos, Transactions, American Geophysical Union, v. 21, no. 2, p. 369-370, https://doi.org/10.1029/TR021i002p00369.","productDescription":"2 p.","startPage":"369","endPage":"370","costCenters":[],"links":[{"id":378571,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"21","issue":"2","noUsgsAuthors":false,"publicationDate":"2014-08-18","publicationStatus":"PW","contributors":{"authors":[{"text":"Howard, C. S.","contributorId":73180,"corporation":false,"usgs":true,"family":"Howard","given":"C.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":799243,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
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