{"pageNumber":"2659","pageRowStart":"66450","pageSize":"25","recordCount":68810,"records":[{"id":51157,"text":"ofr5299 - 1952 - Geology and ground-water resources of the Swan Lake-Yonna Valleys area, Klamath County, Oregon","interactions":[],"lastModifiedDate":"2012-02-02T00:11:35","indexId":"ofr5299","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1952","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":"52-99","title":"Geology and ground-water resources of the Swan Lake-Yonna Valleys area, Klamath County, Oregon","language":"ENGLISH","doi":"10.3133/ofr5299","usgsCitation":"Meyers, J.D., and Newcomb, R.C., 1952, Geology and ground-water resources of the Swan Lake-Yonna Valleys area, Klamath County, Oregon: U.S. Geological Survey Open-File Report 52-99, 151 p., 10 plates, https://doi.org/10.3133/ofr5299.","productDescription":"151 p., 10 plates","costCenters":[],"links":[{"id":177167,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1952/0099/report-thumb.jpg"},{"id":86464,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1952/0099/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":86465,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1952/0099/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":86466,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1952/0099/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adae4b07f02db685346","contributors":{"authors":[{"text":"Meyers, Joseph D.","contributorId":18837,"corporation":false,"usgs":true,"family":"Meyers","given":"Joseph","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":243066,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Newcomb, R. C.","contributorId":77907,"corporation":false,"usgs":true,"family":"Newcomb","given":"R.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":243067,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":51187,"text":"ofr52147 - 1952 - The ground-water resources of Nebraska","interactions":[],"lastModifiedDate":"2012-02-02T00:11:28","indexId":"ofr52147","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1952","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":"52-147","title":"The ground-water resources of Nebraska","language":"ENGLISH","doi":"10.3133/ofr52147","usgsCitation":"Taylor, G., 1952, The ground-water resources of Nebraska: U.S. Geological Survey Open-File Report 52-147, 9 p., https://doi.org/10.3133/ofr52147.","productDescription":"9 p.","costCenters":[],"links":[{"id":179716,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a7ee4b07f02db64853d","contributors":{"authors":[{"text":"Taylor, G.H.","contributorId":85158,"corporation":false,"usgs":true,"family":"Taylor","given":"G.H.","email":"","affiliations":[],"preferred":false,"id":243120,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":51108,"text":"ofr5234 - 1952 - Water power possibilities of the Red River and tributaries","interactions":[],"lastModifiedDate":"2012-02-02T00:11:27","indexId":"ofr5234","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1952","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":"52-34","title":"Water power possibilities of the Red River and tributaries","language":"ENGLISH","doi":"10.3133/ofr5234","usgsCitation":"Doolittle, R., 1952, Water power possibilities of the Red River and tributaries: U.S. Geological Survey Open-File Report 52-34, 22 p., https://doi.org/10.3133/ofr5234.","productDescription":"22 p.","costCenters":[],"links":[{"id":178385,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b15e4b07f02db6a4a24","contributors":{"authors":[{"text":"Doolittle, R.N.","contributorId":84441,"corporation":false,"usgs":true,"family":"Doolittle","given":"R.N.","email":"","affiliations":[],"preferred":false,"id":242963,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":51111,"text":"ofr5238 - 1952 - Water-resources investigation in the foreign assistance program","interactions":[],"lastModifiedDate":"2012-02-02T00:11:27","indexId":"ofr5238","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1952","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":"52-38","title":"Water-resources investigation in the foreign assistance program","language":"ENGLISH","doi":"10.3133/ofr5238","usgsCitation":"Eakin, T., 1952, Water-resources investigation in the foreign assistance program: U.S. Geological Survey Open-File Report 52-38, 7 p., https://doi.org/10.3133/ofr5238.","productDescription":"7 p.","costCenters":[],"links":[{"id":178459,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e2e4b07f02db5e4e19","contributors":{"authors":[{"text":"Eakin, T.E.","contributorId":101727,"corporation":false,"usgs":true,"family":"Eakin","given":"T.E.","email":"","affiliations":[],"preferred":false,"id":242966,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":51190,"text":"ofr52150 - 1952 - Index well in Ogden Valley, Utah","interactions":[],"lastModifiedDate":"2017-09-07T12:48:15","indexId":"ofr52150","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1952","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":"52-150","title":"Index well in Ogden Valley, Utah","docAbstract":"<p>No abstract available.</p>","language":"English","doi":"10.3133/ofr52150","usgsCitation":"Thomas, H.E., 1952, Index well in Ogden Valley, Utah: U.S. Geological Survey Open-File Report 52-150, 33 p., https://doi.org/10.3133/ofr52150.","productDescription":"33 p.","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":179719,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"country":"United States","state":"Utah","otherGeospatial":"Ogden Valley","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a81e4b07f02db64a243","contributors":{"authors":[{"text":"Thomas, H. E.","contributorId":12829,"corporation":false,"usgs":true,"family":"Thomas","given":"H.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":243123,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":51184,"text":"ofr52144 - 1952 - Ground water for irrigation at the Federal Correctional Institution, La Luna, Texas","interactions":[],"lastModifiedDate":"2012-02-02T00:11:28","indexId":"ofr52144","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1952","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":"52-144","title":"Ground water for irrigation at the Federal Correctional Institution, La Luna, Texas","language":"ENGLISH","doi":"10.3133/ofr52144","usgsCitation":"Sundstrom, R., 1952, Ground water for irrigation at the Federal Correctional Institution, La Luna, Texas: U.S. Geological Survey Open-File Report 52-144, 11 p., https://doi.org/10.3133/ofr52144.","productDescription":"11 p.","costCenters":[],"links":[{"id":179713,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ab0e4b07f02db66dc03","contributors":{"authors":[{"text":"Sundstrom, R.W.","contributorId":103657,"corporation":false,"usgs":true,"family":"Sundstrom","given":"R.W.","email":"","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":243117,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":51113,"text":"ofr5243 - 1952 - Records of wells and ground-water levels in Minideka County, Idaho","interactions":[],"lastModifiedDate":"2012-02-02T00:11:27","indexId":"ofr5243","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1952","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":"52-43","title":"Records of wells and ground-water levels in Minideka County, Idaho","language":"ENGLISH","doi":"10.3133/ofr5243","usgsCitation":"Fader, S., and Mower, R.W., 1952, Records of wells and ground-water levels in Minideka County, Idaho: U.S. Geological Survey Open-File Report 52-43, 173 p., 1 plate, https://doi.org/10.3133/ofr5243.","productDescription":"173 p., 1 plate","costCenters":[],"links":[{"id":178461,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a60e4b07f02db63558b","contributors":{"authors":[{"text":"Fader, S.W.","contributorId":55897,"corporation":false,"usgs":true,"family":"Fader","given":"S.W.","affiliations":[],"preferred":false,"id":242969,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Mower, R. W.","contributorId":34898,"corporation":false,"usgs":true,"family":"Mower","given":"R.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":242968,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70221526,"text":"70221526 - 1952 - Supergene and hydrothermal dispersion of heavy metals in wall rocks near ore bodies, Tintic district, Utah","interactions":[],"lastModifiedDate":"2021-06-21T18:15:32.123496","indexId":"70221526","displayToPublicDate":"1952-11-01T13:09:46","publicationYear":"1952","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":"Supergene and hydrothermal dispersion of heavy metals in wall rocks near ore bodies, Tintic district, Utah","docAbstract":"<p><span>Part I, T. S. Lovering. Preliminary work&nbsp;</span>in<span>&nbsp;the&nbsp;</span>Tintic<span>&nbsp;</span>district<span>,&nbsp;</span>Utah<span>, determined the relative distance of migration of&nbsp;</span>ore<span>&nbsp;</span>metals<span>&nbsp;</span>in<span>&nbsp;moist carbonate and silicic&nbsp;</span>wall<span>&nbsp;</span>rocks<span>&nbsp;</span>near<span>&nbsp;</span>ore<span>, and&nbsp;</span>in<span>&nbsp;ground water having a very sluggish circulation through mineralized ground. The analyses of efflorescences&nbsp;</span>in<span>&nbsp;the&nbsp;</span>Tintic<span>&nbsp;Standard mine openings at suitable localities indicated that under the conditions existing during the past 25 years lead has not moved perceptibly; gold has migrated only a few inches; copper has moved a few score feet at most and only&nbsp;</span>in<span>&nbsp;acid solutions; and zinc has traveled hundreds of feet, but not as far as some silver. Silver may travel far&nbsp;</span>in<span>&nbsp;the oxidized zone, but if it comes&nbsp;</span>in<span>&nbsp;contact with sulfides its migration is quickly halted. The chief chemical factors that influence the migration of&nbsp;</span>metals<span>&nbsp;</span>in<span>&nbsp;</span>supergene<span>&nbsp;solutions are the hydrogen ion concentration (pH) of hydrolysis of the&nbsp;</span>metal<span>&nbsp;ion, the solubility of sulfates of the&nbsp;</span>metals<span>, and the position of the&nbsp;</span>metals<span>&nbsp;</span>in<span>&nbsp;Schuermann's series if the solutions are&nbsp;</span>in<span>&nbsp;contact with sulfides for a considerable time.&nbsp;</span></p>","language":"English","publisher":"Society of Economic Geologists","doi":"10.2113/gsecongeo.47.7.685","usgsCitation":"Morris, H.T., and Lovering, T.S., 1952, Supergene and hydrothermal dispersion of heavy metals in wall rocks near ore bodies, Tintic district, Utah: Economic Geology, v. 47, no. 7, p. 685-716, https://doi.org/10.2113/gsecongeo.47.7.685.","productDescription":"32 p.","startPage":"685","endPage":"716","costCenters":[],"links":[{"id":386622,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United  States","state":"Utah","otherGeospatial":"southern Utah","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -114.01611328125,\n              36.99377838872517\n            ],\n            [\n              -109.072265625,\n              36.99377838872517\n            ],\n            [\n              -109.072265625,\n              39.977120098439634\n            ],\n            [\n              -114.01611328125,\n              39.977120098439634\n            ],\n            [\n              -114.01611328125,\n              36.99377838872517\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"47","issue":"7","noUsgsAuthors":false,"publicationDate":"1952-11-01","publicationStatus":"PW","contributors":{"authors":[{"text":"Morris, H. T.","contributorId":15585,"corporation":false,"usgs":true,"family":"Morris","given":"H.","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":817935,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lovering, T. S.","contributorId":108085,"corporation":false,"usgs":true,"family":"Lovering","given":"T.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":817936,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70221613,"text":"70221613 - 1952 - Glaciation and drainage changes in the fish Lake Plateau, Utah","interactions":[],"lastModifiedDate":"2021-06-25T14:19:04.69803","indexId":"70221613","displayToPublicDate":"1952-11-01T09:12:24","publicationYear":"1952","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":"Glaciation and drainage changes in the fish Lake Plateau, Utah","docAbstract":"<p><span>The&nbsp;</span>Fish<span>&nbsp;</span>Lake<span>&nbsp;</span>Plateau<span>, nearly centrally located among the High Plateaus of&nbsp;</span>Utah<span>, exhibits glacial and other geomorphic features of regional significance. The&nbsp;</span>plateau<span>&nbsp;is divided into two areas by&nbsp;</span>Fish<span>&nbsp;</span>Lake<span>&nbsp;and the wide valley of Sevenmile Creek. The&nbsp;</span>Fish<span>&nbsp;</span>Lake<span>&nbsp;trough is a structural basin; Sevenmile Valley may be largely erosional. Volcanic rocks of Tertiary age underlie most of the&nbsp;</span>plateau<span>; early Tertiary sedimentary rocks are also present. Glaciated canyons with well-developed cirques are especially prominent along the east-facing sides of the&nbsp;</span>Fish<span>&nbsp;</span>Lake<span>&nbsp;trough and Sevenmile Valley. Ice-eroded features occur over much of the&nbsp;</span>plateau<span>&nbsp;top. Near the mouths of several of the glaciated canyons are two conspicuous sets of moraines. The older set is more extensive and less rugged than the younger and occurs at somewhat lower elevations. Two substages of&nbsp;</span>glaciation<span>&nbsp;thus recognized are correlated with Wisconsin I and II of Ray; probable correlatives of Wisconsin III, IV, and V are represented by moraines which are younger than these two sets.&nbsp;</span>Fish<span>&nbsp;</span>Lake<span>&nbsp;drains north into Fremont River, a tributary of the Colorado River. An abandoned southern outlet and waterfall, the latter at a higher elevation than the present elevation of the original northern bedrock divide, indicate&nbsp;</span>drainage<span>&nbsp;reversal. Evidence is presented which suggests that this reversal was pre-glacial and probably the result of fault-block tilting.&nbsp;</span></p>","language":"English","publisher":"Geological Society of America","doi":"10.1130/0016-7606(1952)63[1109:GADCIT]2.0.CO;2","usgsCitation":"Hardy, C.T., and Muessig, S., 1952, Glaciation and drainage changes in the fish Lake Plateau, Utah: Geological Society of America Bulletin, v. 63, no. 11, p. 1109-1116, https://doi.org/10.1130/0016-7606(1952)63[1109:GADCIT]2.0.CO;2.","productDescription":"8 p.","startPage":"1109","endPage":"1116","costCenters":[],"links":[{"id":386738,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United  States","state":"Utah","otherGeospatial":"Fish Lake Hightop","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -111.796875,\n              38.16047628099622\n            ],\n            [\n              -111.03881835937499,\n              38.16047628099622\n            ],\n            [\n              -111.03881835937499,\n              39.04478604850143\n            ],\n            [\n              -111.796875,\n              39.04478604850143\n            ],\n            [\n              -111.796875,\n              38.16047628099622\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"63","issue":"11","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Hardy, Clyde T.","contributorId":260420,"corporation":false,"usgs":false,"family":"Hardy","given":"Clyde","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":818264,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Muessig, S.","contributorId":19287,"corporation":false,"usgs":true,"family":"Muessig","given":"S.","email":"","affiliations":[],"preferred":false,"id":818265,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70198446,"text":"70198446 - 1952 - The relation between the lowering of the piezometric surface and the rate and duration of discharge of a well using ground-water storage","interactions":[],"lastModifiedDate":"2018-08-07T09:29:20","indexId":"70198446","displayToPublicDate":"1952-08-03T07:53:04","publicationYear":"1952","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"The relation between the lowering of the piezometric surface and the rate and duration of discharge of a well using ground-water storage","docAbstract":"<p>No abstract available&nbsp;&nbsp;</p>","conferenceTitle":"American Geophysical Union Transactions, 16th Annual Meeting","conferenceDate":"August 1952","conferenceLocation":"Washington, D.C.","language":"English","usgsCitation":"Theis, C.V., 1952, The relation between the lowering of the piezometric surface and the rate and duration of discharge of a well using ground-water storage, American Geophysical Union Transactions, 16th Annual Meeting, v. 16, no. 2, Washington, D.C., August 1952, p. 519-524.","productDescription":"6 p.","startPage":"519","endPage":"524","costCenters":[],"links":[{"id":356236,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":356126,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://water.usgs.gov/ogw/pubs/Theis-1935.pdf"}],"volume":"16","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Theis, Charles V.","contributorId":48080,"corporation":false,"usgs":true,"family":"Theis","given":"Charles","email":"","middleInitial":"V.","affiliations":[],"preferred":false,"id":741484,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70217842,"text":"70217842 - 1952 - Discussion of “tide‐producing forces and artesian pressures”","interactions":[],"lastModifiedDate":"2021-02-05T18:44:33.420843","indexId":"70217842","displayToPublicDate":"1952-08-01T12:40:56","publicationYear":"1952","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":"Discussion of “tide‐producing forces and artesian pressures”","docAbstract":"<p>I was an employee of the Texas State Board of Water Engineers in charge of the Fort Stockton field office at the time that the data for this paper were gathered. Since I have done both extensive and detailed ground‐water work in the Fort Stockton area, including the setting and maintaining of the water‐stage recorder at the Gonzales well, I believe I can add some pertinent hydrologic remarks about this paper.</p><p>The authors state that the principal water‐bearing formation is a limestone. This opinion is not shared by myself and most likely the majority of other geologists in this area. Adkins [1927] favored the basal Cretaceous sands as the principal source of water to Comanche Springs. I believe that the most extensive and the principal water‐bearing formation is a sand and sandstone. The crevices and channels reported in wells and exposed at the springs are only a localized condition resulting from structural weakness and solution caused by a high water surface. The piezometric surface in sand and crevice wells is essentially identical; this suggests that there exists but one principal aquifer in this area. W.N. White, former District Geologist in Texas for the U.S. Geological Survey, in a personal communication to me in 1948, reported Comanche Springs to be the most reliable springs in Texas. This reliable flow strongly supports the concept of a sand aquifer, whose catchment area, or source, is of vast and varied extent, and a great distance from its outlet.</p>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR033i004p00597","usgsCitation":"Culbertson, T., George, W., and Romberg, F.E., 1952, Discussion of “tide‐producing forces and artesian pressures”: Eos, Transactions, American Geophysical Union, v. 33, no. 4, p. 597-600, https://doi.org/10.1029/TR033i004p00597.","productDescription":"4 p.","startPage":"597","endPage":"600","costCenters":[],"links":[{"id":383059,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"33","issue":"4","noUsgsAuthors":false,"publicationDate":"2014-08-18","publicationStatus":"PW","contributors":{"authors":[{"text":"Culbertson, Tom","contributorId":248797,"corporation":false,"usgs":false,"family":"Culbertson","given":"Tom","email":"","affiliations":[],"preferred":false,"id":809882,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"George, William O.","contributorId":106016,"corporation":false,"usgs":true,"family":"George","given":"William O.","affiliations":[],"preferred":false,"id":809883,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Romberg, Frederick E.","contributorId":248796,"corporation":false,"usgs":false,"family":"Romberg","given":"Frederick","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":809884,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70221615,"text":"70221615 - 1952 - Nonsteady flow to a well of constant drawdown in an extensive aquifer","interactions":[],"lastModifiedDate":"2021-06-25T14:55:06.628535","indexId":"70221615","displayToPublicDate":"1952-08-01T09:48:48","publicationYear":"1952","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":"Nonsteady flow to a well of constant drawdown in an extensive aquifer","docAbstract":"<p>A mathematical theory is given for the discharge of a well of constant drawdown, discharging as by natural flow from an effectively infinite aquifer of uniform transmissibility and uniform compressibility. This theory is based on the solution by L. P. Smith of the analogous problem in heat conduction. The mathematical function involved in the solution, which cannot be integrated directly, is evaluated by numerical integration. A table of its values is given for a wide range of its argument. This function is compared with other,asymptotic solutions, and simple, useful approximations are given.</p><p>Two graphical methods are outlined for determining the coefficients of storage and transmissibility from variations in the rate of discharge of wells flowing at constant drawdown. Data from the Grand Junction, Colo., artesian basin are treated by these methods. In the Grand Junction artesian basin there are about 25 flowing wells ranging in depth from 600 to 1600 ft, most of which obtain water from the Entrada sandstone. A few of the wells obtain water from a sandstone in the overlying Morrison formation and a few tap the underlying Wingate sandstone.</p><p>The procedure of the tests is outlined, and the “ink-well” mercury gage used to measure the artesian pressures is described. Recovery tests were run on the same wells after the discharge tests. Values of transmissibility obtained from the recovery tests check those obtained by means of the discharge tests.</p>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR033i004p00559","usgsCitation":"Jacob, C., and Lohman, S., 1952, Nonsteady flow to a well of constant drawdown in an extensive aquifer: Eos, Transactions, American Geophysical Union, v. 33, no. 4, p. 559-569, https://doi.org/10.1029/TR033i004p00559.","productDescription":"11 p.","startPage":"559","endPage":"569","costCenters":[],"links":[{"id":386739,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United  States","state":"Colorado","city":"Grand Junction","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -108.896484375,\n              38.92522904714054\n            ],\n            [\n              -108.1494140625,\n              38.92522904714054\n            ],\n            [\n              -108.1494140625,\n              39.27478966170308\n            ],\n            [\n              -108.896484375,\n              39.27478966170308\n            ],\n            [\n              -108.896484375,\n              38.92522904714054\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"33","issue":"4","noUsgsAuthors":false,"publicationDate":"2014-08-18","publicationStatus":"PW","contributors":{"authors":[{"text":"Jacob, C.E.","contributorId":260638,"corporation":false,"usgs":false,"family":"Jacob","given":"C.E.","email":"","affiliations":[],"preferred":false,"id":818266,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lohman, S.W.","contributorId":260639,"corporation":false,"usgs":false,"family":"Lohman","given":"S.W.","email":"","affiliations":[],"preferred":false,"id":818267,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70221614,"text":"70221614 - 1952 - Nonsteady flow to a well of constant drawdown in an extensive aquifer","interactions":[],"lastModifiedDate":"2021-06-26T11:10:30.966986","indexId":"70221614","displayToPublicDate":"1952-08-01T09:48:48","publicationYear":"1952","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":"Nonsteady flow to a well of constant drawdown in an extensive aquifer","docAbstract":"<p>A mathematical theory is given for the discharge of a well of constant drawdown, discharging as by natural flow from an effectively infinite aquifer of uniform transmissibility and uniform compressibility. This theory is based on the solution by L. P. Smith of the analogous problem in heat conduction. The mathematical function involved in the solution, which cannot be integrated directly, is evaluated by numerical integration. A table of its values is given for a wide range of its argument. This function is compared with other,asymptotic solutions, and simple, useful approximations are given.</p><p>Two graphical methods are outlined for determining the coefficients of storage and transmissibility from variations in the rate of discharge of wells flowing at constant drawdown. Data from the Grand Junction, Colo., artesian basin are treated by these methods. In the Grand Junction artesian basin there are about 25 flowing wells ranging in depth from 600 to 1600 ft, most of which obtain water from the Entrada sandstone. A few of the wells obtain water from a sandstone in the overlying Morrison formation and a few tap the underlying Wingate sandstone.</p><p>The procedure of the tests is outlined, and the “ink-well” mercury gage used to measure the artesian pressures is described. Recovery tests were run on the same wells after the discharge tests. Values of transmissibility obtained from the recovery tests check those obtained by means of the discharge tests.</p>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR033i004p00559","usgsCitation":"Jacob, C., and Lohman, S., 1952, Nonsteady flow to a well of constant drawdown in an extensive aquifer: Eos, Transactions, American Geophysical Union, v. 33, no. 4, p. 559-569, https://doi.org/10.1029/TR033i004p00559.","productDescription":"11 p.","startPage":"559","endPage":"569","costCenters":[],"links":[{"id":386770,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United  States","state":"Colorado","city":"Grand Junction","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -108.8525390625,\n              38.831149809348744\n            ],\n            [\n              -108.30322265624999,\n              38.831149809348744\n            ],\n            [\n              -108.30322265624999,\n              39.257778150283364\n            ],\n            [\n              -108.8525390625,\n              39.257778150283364\n            ],\n            [\n              -108.8525390625,\n              38.831149809348744\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"33","issue":"4","noUsgsAuthors":false,"publicationDate":"2014-08-18","publicationStatus":"PW","contributors":{"authors":[{"text":"Jacob, C.E.","contributorId":260638,"corporation":false,"usgs":false,"family":"Jacob","given":"C.E.","email":"","affiliations":[],"preferred":false,"id":818349,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lohman, S.W.","contributorId":260639,"corporation":false,"usgs":false,"family":"Lohman","given":"S.W.","email":"","affiliations":[],"preferred":false,"id":818350,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":71296,"text":"tei237 - 1952 - Origin of the Chattanooga shale","interactions":[],"lastModifiedDate":"2014-04-03T14:49:59","indexId":"tei237","displayToPublicDate":"1952-07-01T13:43:00","publicationYear":"1952","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":337,"text":"Trace Elements Investigations","code":"TEI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"237","title":"Origin of the Chattanooga shale","docAbstract":"<p>Tonight I will try to present to you the chief facts we have observed that have a bearing on\nthe old problem of how the black shales originated. Some of the ideas have been used before, and\nsome are new. Some of those that have been used before, have been used to support arguments for\nboth shallow and deep water, yet I shall use them again and try to show why our use of them in support\nof shallow water is justified, and the other fellow's use of them in support of deep water is not justified.</p>\n<br/>\n<p>These conclusions are strictly our own. Early in our studies we gave serious consideration to\ndeep-water possibilities, but always we ran into such highly improbable circumstances and implications\nthat we were forced to abandon them. The shallow-water theory seems to encounter no such formidable\nobstacles. We know of no facts that are incompatible with a shallow-water theory; we think that all\nknown facts lend themselves to such an explanation; and we believe that a shallow-water explanation of\nthese black shales is the simpler and sounder of the alternatives.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/tei237","collaboration":"This report concerns work done on behalf of the Division of Raw Materials of the U.S. Atomic Energy Commission","usgsCitation":"Conant, L.C., 1952, Origin of the Chattanooga shale: U.S. Geological Survey Trace Elements Investigations 237, 23 p., https://doi.org/10.3133/tei237.","productDescription":"23 p.","costCenters":[],"links":[{"id":283950,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/tei237.png"},{"id":285624,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/tei/0237/report.pdf"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"535594e6e4b0120853e8c0c1","contributors":{"authors":[{"text":"Conant, Louis C.","contributorId":83921,"corporation":false,"usgs":true,"family":"Conant","given":"Louis","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":283955,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":72057,"text":"tem140 - 1952 - Geology of the area adjacent to the Free Enterprise uranium-silver Mine, Boulder District, Jefferson County, Montana","interactions":[],"lastModifiedDate":"2014-02-28T13:54:59","indexId":"tem140","displayToPublicDate":"1952-01-01T15:19:00","publicationYear":"1952","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":338,"text":"Trace Elements Memorandum","code":"TEM","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"140","title":"Geology of the area adjacent to the Free Enterprise uranium-silver Mine, Boulder District, Jefferson County, Montana","docAbstract":"Uranium minerals.occur in pods associated with cryptocrystalline silica, silver minerals, and scattered sulfide mineral grains in a hydrothermal vein that cuts quartz monzonite and alaskite at the Free Enterprise mine, 2 miles west of Boulder, Mont. The Free Enterprise vein is one of many silicified reef-like structures in this area, most of which trend about N. 60° E. The cryptocrystalline silica zones of the area are lenticular and are bordered by an altered zone where quartz monzonite is the wall rock. No alteration was noticed where alaskite is adjacent to silica zones. No uranium minerals were observed at the surface, but radioactivity anomalies were noted at 57 outcrops. Underground mining has shown that leaching by downward percolating waters has removed most of the uranium from the near-surface part of the Free Enterprise vein and probably has enriched slightly, parts of the vein and the adjacent wall rock from the bottom of the leached zone to the ground-water level. It is possible that other veins that show low to moderate radioactivity at the surface may contain significant concentrations of uranium minerals at relatively shallow depth. The quartz monzonite appears to be a more favorable host rock for the cryptocrystalline silica and associated uranium minerals than the alaskite. The alaskite occurs as vertical_dikes plug-like masses, and as irregularly shaped, gently dipping masses that are believed to have been intruded into open fractures formed during the cooling of the quartz monzonite.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/tem140","collaboration":"Prepared in cooperation the the U.S. Atomic Energy Commission","usgsCitation":"Roberts, W., and Gude, A.J., 1952, Geology of the area adjacent to the Free Enterprise uranium-silver Mine, Boulder District, Jefferson County, Montana: U.S. Geological Survey Trace Elements Memorandum 140, Report: 25 p.; Plate: 30.94 inches x 31.33 inches, https://doi.org/10.3133/tem140.","productDescription":"Report: 25 p.; Plate: 30.94 inches x 31.33 inches","additionalOnlineFiles":"Y","costCenters":[],"links":[{"id":279205,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/tem/0140/report-thumb.jpg"},{"id":282985,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/tem/0140/plate-1.pdf"},{"id":282984,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/tem/0140/report.pdf"}],"country":"United States","state":"Montana","county":"Jefferson County","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -112.158652,46.250478 ], [ -112.158652,46.260749 ], [ -112.134312,46.260749 ], [ -112.134312,46.250478 ], [ -112.158652,46.250478 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"528c96aee4b0c629af44ddb3","contributors":{"authors":[{"text":"Roberts, W.A.","contributorId":13521,"corporation":false,"usgs":true,"family":"Roberts","given":"W.A.","email":"","affiliations":[],"preferred":false,"id":285054,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Gude, A. J. III","contributorId":25554,"corporation":false,"usgs":true,"family":"Gude","given":"A.","suffix":"III","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":285055,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":110,"text":"110 - 1952 - Ground water notes","interactions":[],"lastModifiedDate":"2014-08-04T13:41:09","indexId":"110","displayToPublicDate":"1952-01-01T13:39:25","publicationYear":"1952","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"title":"Ground water notes","docAbstract":"No abstract available.","language":"English","publisher":"U.S. Department of the Interior","publisherLocation":"Washington, D.C.","doi":"10.3133/110","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1952, Ground water notes, https://doi.org/10.3133/110.","costCenters":[],"links":[{"id":291616,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53e09e59e4b0beb42bdca43f","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":527184,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70048286,"text":"tem340 - 1952 - Occurrence of uranium-bearing coal, carbonaceous shale, and carbonaceous limestone in the Fall Creek area, Bonneville County, Idaho","interactions":[{"subject":{"id":70048286,"text":"tem340 - 1952 - Occurrence of uranium-bearing coal, carbonaceous shale, and carbonaceous limestone in the Fall Creek area, Bonneville County, Idaho","indexId":"tem340","publicationYear":"1952","noYear":false,"title":"Occurrence of uranium-bearing coal, carbonaceous shale, and carbonaceous limestone in the Fall Creek area, Bonneville County, Idaho"},"predicate":"SUPERSEDED_BY","object":{"id":3321,"text":"cir212 - 1952 - Uranium-bearing coal and carbonaceous rocks in the Fall Creek area, Bonneville County, Idaho","indexId":"cir212","publicationYear":"1952","noYear":false,"title":"Uranium-bearing coal and carbonaceous rocks in the Fall Creek area, Bonneville County, Idaho"},"id":1}],"supersededBy":{"id":3321,"text":"cir212 - 1952 - Uranium-bearing coal and carbonaceous rocks in the Fall Creek area, Bonneville County, Idaho","indexId":"cir212","publicationYear":"1952","noYear":false,"title":"Uranium-bearing coal and carbonaceous rocks in the Fall Creek area, Bonneville County, Idaho"},"lastModifiedDate":"2014-02-28T14:33:55","indexId":"tem340","displayToPublicDate":"1952-01-01T13:31:00","publicationYear":"1952","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":338,"text":"Trace Elements Memorandum","code":"TEM","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"340","title":"Occurrence of uranium-bearing coal, carbonaceous shale, and carbonaceous limestone in the Fall Creek area, Bonneville County, Idaho","docAbstract":"Uraniferous coal, carbonaceous shale, and carbonaceous limestone occur in the Bear River formation of Upper Crestaceous age at the Fall Creek prospect, in the Fall Creek area, Bonneville County, IDaho.  The uranium compounds are believed to have been derived from mildly radioactive silicic volcanic rocks of the Tertiary age that rest unconformably on all older rocks and once overlay the Bear River formation and its coal. Meteoric water, percolating downward through the silicic volcanic rocks and into the older rocks along joints and faults, is believed to have brought the uranium compounds into contact with the coal and carbonaceous rocks in which the uranium was absorbed.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/tem340","collaboration":"The report concerns work done on behalf of the Division of Raw Materials of the U.S. Atomic Energy Commission","usgsCitation":"Vine, J.D., and Moore, G.W., 1952, Occurrence of uranium-bearing coal, carbonaceous shale, and carbonaceous limestone in the Fall Creek area, Bonneville County, Idaho: U.S. Geological Survey Trace Elements Memorandum 340, 25 p., https://doi.org/10.3133/tem340.","productDescription":"25 p.","numberOfPages":"27","additionalOnlineFiles":"Y","costCenters":[],"links":[{"id":277882,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/tem/0340/report-thumb.jpg"},{"id":283086,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/tem/0340/report.pdf"}],"country":"United States","state":"Idaho","county":"Bonneville County","otherGeospatial":"Fall Creek","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -112.519966,43.0196 ], [ -112.519966,43.628799 ], [ -111.043997,43.628799 ], [ -111.043997,43.0196 ], [ -112.519966,43.0196 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"523c1cede4b024b60d4072fc","contributors":{"authors":[{"text":"Vine, James D.","contributorId":105287,"corporation":false,"usgs":true,"family":"Vine","given":"James","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":484246,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Moore, George W.","contributorId":21625,"corporation":false,"usgs":true,"family":"Moore","given":"George","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":484245,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70048427,"text":"tem446 - 1952 - Results of reconnaissance for uraniferous coal, lignite, and carbonaceous shale in western Montana","interactions":[{"subject":{"id":70048427,"text":"tem446 - 1952 - Results of reconnaissance for uraniferous coal, lignite, and carbonaceous shale in western Montana","indexId":"tem446","publicationYear":"1952","noYear":false,"title":"Results of reconnaissance for uraniferous coal, lignite, and carbonaceous shale in western Montana"},"predicate":"SUPERSEDED_BY","object":{"id":3839,"text":"cir251 - 1953 - Results of reconnaissance for uraniferous coal, lignite, and carbonaceous shale in western Montana","indexId":"cir251","publicationYear":"1953","noYear":false,"title":"Results of reconnaissance for uraniferous coal, lignite, and carbonaceous shale in western Montana"},"id":1}],"supersededBy":{"id":3839,"text":"cir251 - 1953 - Results of reconnaissance for uraniferous coal, lignite, and carbonaceous shale in western Montana","indexId":"cir251","publicationYear":"1953","noYear":false,"title":"Results of reconnaissance for uraniferous coal, lignite, and carbonaceous shale in western Montana"},"lastModifiedDate":"2014-03-04T13:37:44","indexId":"tem446","displayToPublicDate":"1952-01-01T10:05:00","publicationYear":"1952","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":338,"text":"Trace Elements Memorandum","code":"TEM","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"446","title":"Results of reconnaissance for uraniferous coal, lignite, and carbonaceous shale in western Montana","docAbstract":"A reconnaissance search for uraniferous lignite and carbonaceous shale was made in western Montana and adjacent parts of Idaho during the summer of 1951. Particular emphasis in the examination was placed on coal and carbonaceous shale associated with volcanic rocks, as volcanic rocks in many area appear to have released uranium to circulating ground water from which it was concentrated in carbonaceous material. Twenty-two area in Montana and one area of Idaho were examine. The coal in five of these area is of Cretaceous age. The coal and carbonaceous shale in the remaining 18 area occur in Tertiary \"lake-bed\" deposits of Oligocene and younger age.  Both the Cretaceous and Tertiary coal and carbonaceous shale are associated with contemporaneous or younger volcanic rocks and pyroclastic sequences.  A sample of carbonaceous shale from the Prickly Pear Valley northeast of Helena, Montana, contained 0.013 percent uranium. A sample of carbonaceous shale from the Flint Creek Valley southwest of Drummond, Montana, contained 0.006 percent uranium. All other samples of both Cretaceous and Tertiary coal and carbonaceous shale were essentially non-radioactive. No further work is planned on the Cretaceous and Tertiary coal and carbonaceous shale in western Montana. A few localities in Idaho will be visited in the course of other work.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/tem446","collaboration":"This report concerns work done on behalf of the Division of Raw Materials of the U.S. Atomic Energy Commission","usgsCitation":"Hail, W.J., and Gill, J.R., 1952, Results of reconnaissance for uraniferous coal, lignite, and carbonaceous shale in western Montana: U.S. Geological Survey Trace Elements Memorandum 446, Report: 22 p.; 1 Plate: 23.48 x 13.76 inches, https://doi.org/10.3133/tem446.","productDescription":"Report: 22 p.; 1 Plate: 23.48 x 13.76 inches","numberOfPages":"24","additionalOnlineFiles":"Y","costCenters":[],"links":[{"id":278113,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/tem/0446/report-thumb.jpg"},{"id":283237,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/tem/0446/report.pdf"},{"id":283238,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/tem/0446/plate-1.pdf"}],"country":"United States","state":"Idaho;Montana","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -116.05,44.3582 ], [ -116.05,47.4128 ], [ -109.6316,47.4128 ], [ -109.6316,44.3582 ], [ -116.05,44.3582 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5245576ae4b0b3d37307e1bc","contributors":{"authors":[{"text":"Hail, William J. Jr.","contributorId":99952,"corporation":false,"usgs":true,"family":"Hail","given":"William","suffix":"Jr.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":484623,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Gill, James R.","contributorId":44904,"corporation":false,"usgs":true,"family":"Gill","given":"James","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":484622,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70045333,"text":"70045333 - 1952 - Memorandum on ground-water investigation of four proposed stock wells in Puertocito Area, Socorro County and Canoncito Area, Bernalillo and Valencia Counties, New Mexico","interactions":[],"lastModifiedDate":"2013-05-23T11:29:13","indexId":"70045333","displayToPublicDate":"1952-01-01T00:00:00","publicationYear":"1952","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"seriesTitle":{"id":375,"text":"Open-File Report","active":false,"publicationSubtype":{"id":6}},"title":"Memorandum on ground-water investigation of four proposed stock wells in Puertocito Area, Socorro County and Canoncito Area, Bernalillo and Valencia Counties, New Mexico","docAbstract":"At the request of the Navajo Service, Office ot Indian Affairs, a groundwater iinvestigation of four proposed stock wells in the Puertocito Area, Socorro county and the Canoncito Area., Bernalillo and Valencia counties,New Mexico, was made in November, 1951 (see fig. 1). Although these areas are not on the Navajo Indian Reservation, they were included in the program of study of ground-water resources or the Navajo and Hopi Indian Reservations now being conducted by the Ground Water Branch of the United States Geological Survey. The work was financed by and was in cooperation with the Navajo Service, Office of Indian Affairs.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Holbrook, AZ","doi":"10.3133/70045333","collaboration":"Prepared in in cooperation with the Navajo Service, Office of Indian Affairs","usgsCitation":"Repenning, C., and Galloway, S., 1952, Memorandum on ground-water investigation of four proposed stock wells in Puertocito Area, Socorro County and Canoncito Area, Bernalillo and Valencia Counties, New Mexico: Open-File Report, 6 p., https://doi.org/10.3133/70045333.","productDescription":"6 p.","numberOfPages":"9","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":270731,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":272721,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/unnumbered/70045333/report.pdf"}],"country":"United States","state":"New Mexico","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -107.8638,33.9889 ], [ -107.8638,35.4025 ], [ -106.3449,35.4025 ], [ -106.3449,33.9889 ], [ -107.8638,33.9889 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5165386ce4b077fa94dadfbc","contributors":{"authors":[{"text":"Repenning, C.A.","contributorId":56700,"corporation":false,"usgs":true,"family":"Repenning","given":"C.A.","affiliations":[],"preferred":false,"id":477254,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Galloway, S.E.","contributorId":85151,"corporation":false,"usgs":true,"family":"Galloway","given":"S.E.","email":"","affiliations":[],"preferred":false,"id":477255,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":95186,"text":"95186 - 1952 - Silicone water-repellents (Mimeograph)","interactions":[],"lastModifiedDate":"2012-02-02T00:03:58","indexId":"95186","displayToPublicDate":"1952-01-01T00:00:00","publicationYear":"1952","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":9,"text":"Other Report"},"title":"Silicone water-repellents (Mimeograph)","docAbstract":"No abstract available at this time","language":"English","collaboration":"24/FH","usgsCitation":"Snieszko, S.F., 1952, Silicone water-repellents (Mimeograph), 1 p.","productDescription":"1 p.","startPage":"1","numberOfPages":"1","costCenters":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"links":[{"id":128408,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49c8e4b07f02db5d5d68","contributors":{"authors":[{"text":"Snieszko, S. F.","contributorId":13169,"corporation":false,"usgs":true,"family":"Snieszko","given":"S.","middleInitial":"F.","affiliations":[],"preferred":false,"id":298645,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":1001374,"text":"1001374 - 1952 - Hybridization of Canada geese with blue geese in the wild","interactions":[],"lastModifiedDate":"2018-01-04T12:18:45","indexId":"1001374","displayToPublicDate":"1952-01-01T00:00:00","publicationYear":"1952","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3544,"text":"The Auk","onlineIssn":"1938-4254","printIssn":"0004-8038","active":true,"publicationSubtype":{"id":10}},"title":"Hybridization of Canada geese with blue geese in the wild","docAbstract":"<p>While carrying out hunter bag checks in the vicinity of Sand Lake National Wildlife Refuge, Columbia, South Dakota, during the 1950 waterfowl hunting season, the author examined two adult male geese which proved to be crosses between one of the smaller Canada Geese (possibly Richardson's Goose, <i>Branta canadensis hutchinsi</i>) and the Blue Goose, <i>Chen caerulescens</i>.</p>","language":"English","publisher":"American Ornithological Society","doi":"10.2307/4081022","usgsCitation":"Nelson, H., 1952, Hybridization of Canada geese with blue geese in the wild: The Auk, v. 69, no. 4, p. 425-428, https://doi.org/10.2307/4081022.","productDescription":"4 p.","startPage":"425","endPage":"428","costCenters":[{"id":480,"text":"Northern Prairie Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":480435,"rank":1,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.2307/4081022","text":"Publisher Index Page"},{"id":129247,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"South Dakota","otherGeospatial":"Sand Lake National Wildlife Refuge","volume":"69","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae0e4b07f02db687d9d","contributors":{"authors":[{"text":"Nelson, H.K.","contributorId":21489,"corporation":false,"usgs":true,"family":"Nelson","given":"H.K.","email":"","affiliations":[],"preferred":false,"id":310940,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70195898,"text":"70195898 - 1952 - Ground water in the Litchville area, Barnes County, North Dakota","interactions":[],"lastModifiedDate":"2018-03-07T13:42:34","indexId":"70195898","displayToPublicDate":"1952-01-01T00:00:00","publicationYear":"1952","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":5646,"text":"North Dakota Ground Water Studies","active":true,"publicationSubtype":{"id":2}},"seriesNumber":"18","title":"Ground water in the Litchville area, Barnes County, North Dakota","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"North Dakota State Water Conservation Commission","usgsCitation":"Akin, P., 1952, Ground water in the Litchville area, Barnes County, North Dakota: North Dakota Ground Water Studies 18, 51 p.","productDescription":"51 p.","costCenters":[{"id":478,"text":"North Dakota Water Science Center","active":true,"usgs":true},{"id":34685,"text":"Dakota Water Science Center","active":true,"usgs":true}],"links":[{"id":352291,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5aff6b45e4b0da30c1bfe4e6","contributors":{"authors":[{"text":"Akin, P.D.","contributorId":104471,"corporation":false,"usgs":true,"family":"Akin","given":"P.D.","email":"","affiliations":[],"preferred":false,"id":730420,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70171409,"text":"70171409 - 1952 - Origin of the Mima Mounds, Thurston County region, Washington","interactions":[],"lastModifiedDate":"2016-05-31T10:54:39","indexId":"70171409","displayToPublicDate":"1952-01-01T00:00:00","publicationYear":"1952","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2309,"text":"Journal of Geology","active":true,"publicationSubtype":{"id":10}},"title":"Origin of the Mima Mounds, Thurston County region, Washington","docAbstract":"<p><span>There has been recent favorable consideration of the idea that the Mima mounds were made by gophers. The writer believes the evidence indicates that gophers function only in the reworking of the mound material, not in the primary construction. The plausibility of the earlier glacial or periglacial theory has been increased by recent knowledge of permafrost and of the deposits made by combined water and ice in cold climates. The gopher theory, as it has been applied to the Mima mounds, contains internal disharmonies and ignores significant field evidence supporting the earlier idea.</span></p>","language":"English","publisher":"University of Chicago Press","doi":"10.1086/625998","usgsCitation":"Newcomb, R.C., 1952, Origin of the Mima Mounds, Thurston County region, Washington: Journal of Geology, v. 60, no. 5, p. 461-472, https://doi.org/10.1086/625998.","productDescription":"12 p.","startPage":"461","endPage":"472","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":622,"text":"Washington Water Science Center","active":true,"usgs":true}],"links":[{"id":321897,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"60","issue":"5","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"574eb5dae4b0ee97d51a83e6","contributors":{"authors":[{"text":"Newcomb, R. C.","contributorId":77907,"corporation":false,"usgs":true,"family":"Newcomb","given":"R.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":630909,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":1000314,"text":"1000314 - 1952 - Movements of yellow perch marked in southern Green Bay, Lake Michigan, in 1950","interactions":[],"lastModifiedDate":"2016-02-15T14:12:53","indexId":"1000314","displayToPublicDate":"1952-01-01T00:00:00","publicationYear":"1952","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3624,"text":"Transactions of the American Fisheries Society","active":true,"publicationSubtype":{"id":10}},"title":"Movements of yellow perch marked in southern Green Bay, Lake Michigan, in 1950","docAbstract":"<div class=\"paragraph\">To obtain information on the post-spawning movements of yellow perch that spawn in southern Green Bay, Lake Michigan, 4,172 fish caught in drop nets were marked by tagging with monel-metal strap tags attached to the right operculum and 24,799 were marked by clipping off the second or membranous dorsal fin. Marking was done during the period from May 3 to 17, 1950, at six main stations, all located in the southern end of Green Bay.</div>\n<div class=\"paragraph\">The average length of the tagged perch was 7.3 inches and all fell within the range 5.5&ndash;14.4 inches. Most (90.9 percent) of the fish were below the minimum legal length of 8.0 inches. The follow-up procedure consisted of informing commercial and sports fishermen of the program and enlisting their cooperation in watching for marked fish; accounts of the investigation were released through newspapers and descriptive posters were distributed. The personnel connected with the investigation examined catches frequently.</div>\n<div class=\"paragraph\">The large majority (101 or 79.5 percent) of the 127 tagged perch recaptured in the experimental nets during the marking operations were retaken at the tagging station at which they were released.</div>\n<div class=\"paragraph\">Of the 108 tagged perch captured by commercial fishermen and anglers following the opening of the season on May 20, 96 were taken by drop nets, 6 by gill nets, and 6 by hook and line. The mean lengths for the three groups were 7.7, 7.1, and 9.25 inches, respectively. All recoveries were made in the Wisconsin waters of Green Bay.</div>\n<div class=\"paragraph\">Most of the &ldquo;open-season&rdquo; recoveries (86 fish; 79.6 percent) were made during the period May 20-May 31. Recaptures during subsequent months were: June&ndash;14; July&ndash;7; August&ndash;none; September&ndash;1. Of the 86 perch recaptured May 20&ndash;31, 70 were retaken inside and 16 outside the tagging area. The majority (14 of 22) of those recovered after May 31 were retaken outside the tagging area.</div>\n<div class=\"paragraph\">The average length of the 20 tagged yellow perch recaptured by drop nets (data restricted to fish from a single type of net to avoid bias from gear selectivity) outside the tagging area (8.42 inches) was 0.96 inch greater than the mean length (7.46 inches) of the 76 fish retaken inside the area. This statistically highly significant difference lends support to the belief of commercial fishermen that the larger of the yellow perch that spawn in southern Green Bay move out soon after spawning.</div>\n<div class=\"paragraph\">The percentage of recapture of tagged perch increased sharply with increase in the size of the fish. Not one of 169 tagged fish less than 6.5 inches long was recovered. The rates of recapture at greater lengths were: 6.5 to 8.9 inches&ndash;2.5 percent; 9.0 to 9.9 inches&ndash;11.4 percent; 10.0 to 14.4 inches&ndash;16.7 percent. Among the several factors suggested in explanation of this relationship, the most important appear to be the lesser ability of the smaller fish to survive the rigors of handling and tagging, greater loss of tags from the smaller fish, and the greater likelihood of overlooking the smaller of the tagged fish in the sorting of the catch.</div>\n<div class=\"paragraph\">The factors just mentioned and the lack of knowledge of the efficiency of measures taken to obtain records of recoveries preclude the 2.6-percent return of all tagged fish from being accepted as an approximation of the rate of recapture. Neither should the 6.6-percent return of tagged fish of legal size (8 inches and longer) be taken as an estimate of the rate of exploitation.</div>\n<div class=\"paragraph\">Although 465 fin-clipped perch were recovered in the experimental nets during the marking operations, only 68 of 24,799 fish so marked were recovered after the fishing season opened. All but one of these 68 were retaken near the point of marking. The difficulty of detecting a perch with a missing membranous dorsal is believed to be a major cause of the poor returns from fin-clipped fish.</div>\n<div class=\"paragraph\">These investigations have demonstrated that for studying migration of yellow perch, tagging is superior to fin-clipping as a method of marking. The technique of the tagging, however, needs to be improved, and better means must be found to trace tagged fish of small size. Furthermore certain small regions in the bay not at present open to commercial fishing must be explored in order to obtain more comprehensive information as to migration.</div>","language":"English","publisher":"Taylor & Francis","doi":"10.1577/1548-8659(1951)81[150:MOYPMI]2.0.CO;2","usgsCitation":"Mraz, D., 1952, Movements of yellow perch marked in southern Green Bay, Lake Michigan, in 1950: Transactions of the American Fisheries Society, v. 81, no. 1, p. 150-161, https://doi.org/10.1577/1548-8659(1951)81[150:MOYPMI]2.0.CO;2.","productDescription":"12 p.","startPage":"150","endPage":"161","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":131664,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"81","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b32e4b07f02db6b482f","contributors":{"authors":[{"text":"Mraz, Donald","contributorId":21502,"corporation":false,"usgs":true,"family":"Mraz","given":"Donald","email":"","affiliations":[],"preferred":false,"id":308377,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
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