Some of the classic closed-basin lakes of the western United States have been resampled, and the waters have been analyzed by modern wet-chemical methods. Included are waters from Borax and Little Borax lakes and Mono Lake in California; Big Soda, Pyramid, and Walker Lakes in Nevada; Abert Lake, Oregon; and Great Salt Lake, Utah. Tributary streams and springs have also been sampled and are reported upon. © 1961, The Geological Society of America, Inc.
","language":"English","publisher":"Geological Society of America","doi":"10.1130/0016-7606(1961)72[1421:RCAOWF]2.0.CO;2","issn":"00167606","usgsCitation":"Whitehead, H., and Feth, J.H., 1961, Recent chemical analyses of waters from several closed-basin lakes and their tributaries in the western United States: Geological Society of America Bulletin, v. 72, no. 9, p. 1421-1425, https://doi.org/10.1130/0016-7606(1961)72[1421:RCAOWF]2.0.CO;2.","productDescription":"5 p. ","startPage":"1421","endPage":"1425","costCenters":[],"links":[{"id":370401,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"72","issue":"9","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Whitehead, H.C.","contributorId":50134,"corporation":false,"usgs":true,"family":"Whitehead","given":"H.C.","email":"","affiliations":[],"preferred":false,"id":777818,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Feth, J. H.","contributorId":50495,"corporation":false,"usgs":true,"family":"Feth","given":"J.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":777819,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70220596,"text":"70220596 - 1961 - Uranium migration and geochemistry of uranium deposits in sandstone above, at, and below the water table; Part 2, Relationship of uranium migration dates, geology, and chemistry of the uranium deposits","interactions":[],"lastModifiedDate":"2021-05-21T14:24:33.414608","indexId":"70220596","displayToPublicDate":"1961-12-01T15:13:27","publicationYear":"1961","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":"Uranium migration and geochemistry of uranium deposits in sandstone above, at, and below the water table; Part 2, Relationship of uranium migration dates, geology, and chemistry of the uranium deposits","docAbstract":"The time of U migration in deposits in sandstone can be determined by correlating apparent age calculations, based on radiochemical analyses, with the geology of a particular deposit. Data were obtained from U ore samples representing deposits above the water table, deposits just above and below perched water tables, and deposits at least 250 ft. below the water table in the Hulett Creek area, Wyoming. The first U deposition occurred more than 250,000 years ago for the deposits now at or above the water table. Approximately 60,000 to 80,000 years ago these deposits were oxidized, leached, and locally enriched. Accumulation of U in the deposits below the water table probably did not start before 180,000 years ago and has continued to the present.
","language":"English","publisher":"Society of Economic Geologists","doi":"10.2113/gsecongeo.56.8.1404","usgsCitation":"Robinson, C.S., and Rosholt, J.N., 1961, Uranium migration and geochemistry of uranium deposits in sandstone above, at, and below the water table; Part 2, Relationship of uranium migration dates, geology, and chemistry of the uranium deposits: Economic Geology, v. 56, no. 8, p. 1404-1420, https://doi.org/10.2113/gsecongeo.56.8.1404.","productDescription":"17 p.","startPage":"1404","endPage":"1420","costCenters":[],"links":[{"id":385812,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Montana, South Dakota, Wyoming","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -107.09472656249999,\n 43.83452678223682\n ],\n [\n -103.5791015625,\n 43.83452678223682\n ],\n [\n -103.5791015625,\n 45.36758436884978\n ],\n [\n -107.09472656249999,\n 45.36758436884978\n ],\n [\n -107.09472656249999,\n 43.83452678223682\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"56","issue":"8","noUsgsAuthors":false,"publicationDate":"1961-12-01","publicationStatus":"PW","contributors":{"authors":[{"text":"Robinson, C. S.","contributorId":23578,"corporation":false,"usgs":true,"family":"Robinson","given":"C.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":816115,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Rosholt, John Nicholas Jr.","contributorId":26370,"corporation":false,"usgs":true,"family":"Rosholt","given":"John","suffix":"Jr.","email":"","middleInitial":"Nicholas","affiliations":[],"preferred":false,"id":816116,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70220595,"text":"70220595 - 1961 - Uranium migration and geochemistry of uranium deposits in sandstone above, at, and below the water table; Part 1, Calculation of apparent dates of uranium migration in deposits above and at the water table","interactions":[],"lastModifiedDate":"2021-05-21T14:27:48.217873","indexId":"70220595","displayToPublicDate":"1961-12-01T14:50:10","publicationYear":"1961","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":"Uranium migration and geochemistry of uranium deposits in sandstone above, at, and below the water table; Part 1, Calculation of apparent dates of uranium migration in deposits above and at the water table","docAbstract":"The migration of U may be studied by the distribution of the radioactive daughter products, which serve as natural tracers in the migration of U. The distribution of the daughter products is determined by radiochemical analyses of samples from ore deposits in sandstone, and the apparent minimum and maximum dates of U introduction or redistribution may be calculated from the Pa 231 /Th 230 ratio. The primary assumption required is that the Pa and Th do not migrate in measurable quantities from the place where they were produced by the decay of the parent U isotopes. The upper limit of age determination is about 250,000 years, based on the half-lives of Pa 231 and Th 230 . The difference in the half-lives of these isotopes is reflected in their differential rates of growth and decay corresponding to migrations of the parent U during the time range considered. The growth and decay patterns, analyzed mathematically, are used to determine the apparent date of U migration. Calculations based on analyses of samples from the Hulett Creek area, Wyoming, illustrate the results for typical sandstone ore deposits that are above and at the water table.
","language":"English","publisher":"Society of Economic Geologists","doi":"10.2113/gsecongeo.56.8.1392","usgsCitation":"Rosholt, J.N., 1961, Uranium migration and geochemistry of uranium deposits in sandstone above, at, and below the water table; Part 1, Calculation of apparent dates of uranium migration in deposits above and at the water table: Economic Geology, v. 56, no. 8, p. 1392-1403, https://doi.org/10.2113/gsecongeo.56.8.1392.","productDescription":"12 p.","startPage":"1392","endPage":"1403","costCenters":[],"links":[{"id":385811,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"56","issue":"8","noUsgsAuthors":false,"publicationDate":"1961-12-01","publicationStatus":"PW","contributors":{"authors":[{"text":"Rosholt, John Nicholas Jr.","contributorId":26370,"corporation":false,"usgs":true,"family":"Rosholt","given":"John","suffix":"Jr.","email":"","middleInitial":"Nicholas","affiliations":[],"preferred":false,"id":816114,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70220636,"text":"70220636 - 1961 - Origin of a salt-water lens in permafrost at Kotzebue, Alaska","interactions":[],"lastModifiedDate":"2021-05-21T17:51:04.819618","indexId":"70220636","displayToPublicDate":"1961-12-01T12:44:15","publicationYear":"1961","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":5935,"text":"Bulletin of the Geological Society of America","active":true,"publicationSubtype":{"id":10}},"title":"Origin of a salt-water lens in permafrost at Kotzebue, Alaska","docAbstract":"Frozen sediments were found to a depth of 238 feet in the drilling of a 325-foot well at Kotzebue, Alaska. Between 79 and 86 feet, however, highly saline water was found in a gravel lens. The writer suggests that the salt water originated by fractionation by freezing. Analyses of this water and of slightly saline water from below the permafrost are given.
","language":"English","publisher":"Geological Society of America","doi":"10.1130/0016-7606(1961)72[1427:OOASLI]2.0.CO;2","usgsCitation":"Cedarstrom, D., 1961, Origin of a salt-water lens in permafrost at Kotzebue, Alaska: Bulletin of the Geological Society of America, v. 72, no. 9, p. 1427-1431, https://doi.org/10.1130/0016-7606(1961)72[1427:OOASLI]2.0.CO;2.","productDescription":"5 p.","startPage":"1427","endPage":"1431","costCenters":[],"links":[{"id":385856,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Alaska","city":"Kotzebue","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -163.4765625,\n 66.65297740055279\n ],\n [\n -161.630859375,\n 66.65297740055279\n ],\n [\n -161.630859375,\n 67.33986082559095\n ],\n [\n -163.4765625,\n 67.33986082559095\n ],\n [\n -163.4765625,\n 66.65297740055279\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"72","issue":"9","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Cedarstrom, D.J.","contributorId":102127,"corporation":false,"usgs":true,"family":"Cedarstrom","given":"D.J.","email":"","affiliations":[],"preferred":false,"id":816266,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70220630,"text":"70220630 - 1961 - Late quaternary history of the snake river in the American Falls region, Idaho","interactions":[],"lastModifiedDate":"2021-05-21T16:41:02.448609","indexId":"70220630","displayToPublicDate":"1961-12-01T11:34:23","publicationYear":"1961","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":5935,"text":"Bulletin of the Geological Society of America","active":true,"publicationSubtype":{"id":10}},"title":"Late quaternary history of the snake river in the American Falls region, Idaho","docAbstract":"While mapping the American Falls region, we found evidence that contributes to the middle Pleistocene to Recent history of the Snake River, and indirectly to the history of overflow of Lake Bonneville. Middle Pleistocene to recent rocks in the valley are mainly lacustrine and fluvial silts and clays, with some sand, gravel, basalt, and a few thin tuff beds. The formation of terraces can be correlated with events both up- and downstream.
The Snake River was at least once, and possibly twice, dammed and diverted by eruptions of basalt, resulting in the formation of lakes and deposition of lacustrine beds. A rather flat-lying, thin, but persistent gravel at the base of one lake bed formation may represent a glacial period, possibly Illinoian, during which the Snake River had a large volume.
Overflow of water from Lake Bonneville into the Snake River system, by way of the Marsh Creek-Portneuf valley, laid down a deltaic-fluvial deposit here named the Michaud Gravel. At this time the Snake River, greatly augmented by Lake Bonneville overflow, began to cut channels through and around a lava dam. Terraces between Aberdeen, American Falls, and Pocatello were formed during the existence of the lake in which the Michaud Gravel was deposited and by fluvial processes after drainage of the lake. At one stage in the downcutting, bars of huge basalt boulders were built across the mouths of abandoned spillways.
Radiocarbon dating and geologic evidence from the area between Preston and Soda Springs, Idaho, suggest that basalt flows diverted the Bear River into Lake Bonneville, perhaps causing it to overflow. This diversion probably occurred about 33,000 years ago. This dating accords with events in the American Falls region.
","language":"English","publisher":"Geological Society of America","doi":"10.1130/0016-7606(1961)72[1739:LQHOTS]2.0.CO;2","usgsCitation":"Trimble, D.E., and Carr, W.J., 1961, Late quaternary history of the snake river in the American Falls region, Idaho: Bulletin of the Geological Society of America, v. 72, no. 12, p. 1739-1748, https://doi.org/10.1130/0016-7606(1961)72[1739:LQHOTS]2.0.CO;2.","productDescription":"10 p.","startPage":"1739","endPage":"1748","costCenters":[],"links":[{"id":385850,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Idaho","otherGeospatial":"Snake River","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -116.82861328125001,\n 42.407234661551875\n ],\n [\n -111.29150390625,\n 42.407234661551875\n ],\n [\n -111.29150390625,\n 45.19752230305682\n ],\n [\n -116.82861328125001,\n 45.19752230305682\n ],\n [\n -116.82861328125001,\n 42.407234661551875\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"72","issue":"12","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Trimble, Donald E.","contributorId":75910,"corporation":false,"usgs":true,"family":"Trimble","given":"Donald","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":816259,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Carr, Wilfred James","contributorId":12033,"corporation":false,"usgs":true,"family":"Carr","given":"Wilfred","email":"","middleInitial":"James","affiliations":[],"preferred":false,"id":816260,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":284,"text":"284 - 1961 - Surface water records of North Dakota and South Dakota","interactions":[],"lastModifiedDate":"2014-07-15T11:53:40","indexId":"284","displayToPublicDate":"1961-09-30T11:51:26","publicationYear":"1961","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"title":"Surface water records of North Dakota and South Dakota","docAbstract":"No abstract available.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Bismarck, ND","doi":"10.3133/284","collaboration":"Prepared in cooperation with the States of North and South Dakota and other agencies.","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1961, Surface water records of North Dakota and South Dakota, https://doi.org/10.3133/284.","costCenters":[],"links":[{"id":290128,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"country":"United States","state":"North Dakota;South Dakota","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -104.06,42.48 ], [ -104.06,48.99 ], [ -96.44,48.99 ], [ -96.44,42.48 ], [ -104.06,42.48 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53c64ddbe4b0001bd51477bb","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":527282,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":1494,"text":"1494 - 1961 - Surface water records of Arkansas","interactions":[],"lastModifiedDate":"2025-11-17T15:47:34.498633","indexId":"1494","displayToPublicDate":"1961-09-30T08:59:04","publicationYear":"1961","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"title":"Surface water records of Arkansas","docAbstract":"No abstract available.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Little Rock, AR","doi":"10.3133/1494","issn":"0565-5986","collaboration":"Prepared in cooperation with the State of Arkansas and other agencies, 1960/61-1963/64.","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1961, Surface water records of Arkansas, 4 p., https://doi.org/10.3133/1494.","productDescription":"4 p.","numberOfPages":"4","costCenters":[],"links":[{"id":289836,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"country":"United States","state":"Arkansas","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -94.6179,33.0041 ], [ -94.6179,36.4997 ], [ -89.6468,36.4997 ], [ -89.6468,33.0041 ], [ -94.6179,33.0041 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53c4fc7fe4b0b58d96eeb635","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":527863,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70243783,"text":"70243783 - 1961 - Sex ratios and age raios in North American ducks","interactions":[],"lastModifiedDate":"2023-05-19T15:00:22.628902","indexId":"70243783","displayToPublicDate":"1961-08-01T09:38:02","publicationYear":"1961","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":14432,"text":"Illinois Natural History Survey Bulletin","active":true,"publicationSubtype":{"id":10}},"title":"Sex ratios and age raios in North American ducks","docAbstract":"The sex classes and age classes of various species of ducks constitute measurable elements of the populations. The present study deals primarily with sex ratios and age ratios and the ways in which they relate to population productivity. The present study is an evaluation of sex and age ratios in North American duck populations and the ways in which, in waterfowl management, these ratios can be used to measure productivity. Drakes occurred in relatively greater numbers among diving ducks than among dabblers; however, examination of the available knowledge on the reproductive biology characterizing these two subfamilies revealed nothing which suggests that extra drakes may be more important to the maintenance of populations of diving ducks than of dabblers. Juveniles were found to be more vulnerable to hunting than adults; the vulnerability differential varied with place, time of hunting season, vear, and species. Age ratios obtained from bagged ducks and corrected for the greater vulnerability of juveniles offered the best means of determining the adult-juvenile composition of duck populations.
","language":"English","publisher":"Illinois Natural History Survey","doi":"10.21900/j.inhs.v27.175","usgsCitation":"Bellrose, F.C., Scott, T., Hawkins, A.S., and Low, J.B., 1961, Sex ratios and age raios in North American ducks: Illinois Natural History Survey Bulletin, v. 27, no. 6, p. 391-474, https://doi.org/10.21900/j.inhs.v27.175.","productDescription":"84 p.","startPage":"391","endPage":"474","costCenters":[],"links":[{"id":480381,"rank":2,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.21900/j.inhs.v27.175","text":"Publisher Index Page"},{"id":417244,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"27","issue":"6","noUsgsAuthors":false,"publicationDate":"1961-08-31","publicationStatus":"PW","contributors":{"authors":[{"text":"Bellrose, Frank C.","contributorId":305579,"corporation":false,"usgs":false,"family":"Bellrose","given":"Frank","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":873239,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Scott, Thomas G.","contributorId":305580,"corporation":false,"usgs":false,"family":"Scott","given":"Thomas G.","affiliations":[],"preferred":false,"id":873240,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hawkins, Arthur S.","contributorId":72042,"corporation":false,"usgs":true,"family":"Hawkins","given":"Arthur","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":873241,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Low, Jessop B.","contributorId":305581,"corporation":false,"usgs":false,"family":"Low","given":"Jessop","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":873242,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":70010634,"text":"70010634 - 1961 - Dating desert ground water","interactions":[],"lastModifiedDate":"2026-02-25T17:33:14.813335","indexId":"70010634","displayToPublicDate":"1961-07-14T00:00:00","publicationYear":"1961","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3338,"text":"Science","active":true,"publicationSubtype":{"id":10}},"title":"Dating desert ground water","docAbstract":"Tritium in Arabian rainfall has followed the trend observed in North America with peaks in 1958 and the spring of 1959. These measurements will be useful for future hydrologie studies. Water from wadi gravels averages 10 yr old. Carbon-14 measurements of deep waters indicate ages of several thousand years.","language":"English","publisher":"American Association for the Advancement of Science","doi":"10.1126/science.134.3472.105","issn":"00368075","usgsCitation":"Thatcher, L., Rubin, M., and Brown, G.F., 1961, Dating desert ground water: Science, v. 134, no. 3472, p. 105-106.","productDescription":"2 p.","startPage":"105","endPage":"106","costCenters":[],"links":[{"id":219254,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"134","issue":"3472","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059fddee4b0c8380cd4e9a0","contributors":{"authors":[{"text":"Thatcher, L.","contributorId":38708,"corporation":false,"usgs":true,"family":"Thatcher","given":"L.","affiliations":[],"preferred":false,"id":359309,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Rubin, M.","contributorId":88079,"corporation":false,"usgs":true,"family":"Rubin","given":"M.","email":"","affiliations":[],"preferred":false,"id":359310,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Brown, Glen F.","contributorId":23943,"corporation":false,"usgs":true,"family":"Brown","given":"Glen","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":359308,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70171262,"text":"70171262 - 1961 - Use of water-well data in interpreting occurrence of aquifers in northeastern Lyon County, Minnesota","interactions":[],"lastModifiedDate":"2018-03-19T11:11:05","indexId":"70171262","displayToPublicDate":"1961-07-12T10:00:00","publicationYear":"1961","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1723,"text":"GSA Bulletin","active":true,"publicationSubtype":{"id":10}},"title":"Use of water-well data in interpreting occurrence of aquifers in northeastern Lyon County, Minnesota","docAbstract":"In northeastern Lyon County the areal distribution of aquifers of Cretaceous age determined from well-bottom altitudes suggests a series of interbedded sandstones striking northwestward and overlapping one another to the northeast. Probably the numerous thin sandstone aquifers in the area were deposited near the flanks of a Precambrian granite “high” area by a transgressing Late Cretaceous sea.
","language":"English","publisher":"Geological Society of America","publisherLocation":"Boulder, CO","doi":"10.1130/0016-7606(1961)72[1275:UOWDII]2.0.CO;2","usgsCitation":"Rodis, H.G., 1961, Use of water-well data in interpreting occurrence of aquifers in northeastern Lyon County, Minnesota: GSA Bulletin, v. 72, p. 1275-1278, https://doi.org/10.1130/0016-7606(1961)72[1275:UOWDII]2.0.CO;2.","productDescription":"4 p.","startPage":"1275","endPage":"1278","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":392,"text":"Minnesota Water Science Center","active":true,"usgs":true}],"links":[{"id":321704,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Minnesota","county":"Lyon County","volume":"72","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57481e3ee4b07e28b664dc1a","contributors":{"authors":[{"text":"Rodis, Harry G.","contributorId":25141,"corporation":false,"usgs":true,"family":"Rodis","given":"Harry","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":630359,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70220599,"text":"70220599 - 1961 - Jadeite deposits of the clear creek area, New Idria district, San Benito county, California","interactions":[],"lastModifiedDate":"2021-05-20T21:16:19.609279","indexId":"70220599","displayToPublicDate":"1961-06-01T16:10:44","publicationYear":"1961","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2420,"text":"Journal of Petrology","active":true,"publicationSubtype":{"id":10}},"title":"Jadeite deposits of the clear creek area, New Idria district, San Benito county, California","docAbstract":"Tectonic inclusions within the New Idria serpentine body contain jadeite in two distinct assemblages: (1) Lenslike inclusions containing a monomineralic green jadeite core surrounded by a calc-silicate rim. (2) Jadeite veins cross-cutting albite-crossite schist inclusions. In these veins jadeite coexists with low albite; green jadeite (Jd 75 Ac+Di+He 25) coexists with low albite within the host schist.
Albite schists are related to the pre-metamorphic keratophyres and it can be shown that desilication of such rocks produces a bulk composition similar to that of jadeite. Metamor-phism of keratophyric tectonic inclusions within serpentine produced jadeite-albite schists along margins of the inclusions. Jadeite-albite veins formed from mobilized liquids rich in the jadeite molecule and deficient in water. Geological evidence such as would indicate extreme pressures or temperatures during jadeite formation is lacking; rather, a low silica and dry system allowed its formation at reduced temperatures and pressures.
","language":"English","publisher":"Oxford University Press","doi":"10.1093/petrology/2.2.209","usgsCitation":"Coleman, R.G., 1961, Jadeite deposits of the clear creek area, New Idria district, San Benito county, California: Journal of Petrology, v. 2, no. 2, p. 209-247, https://doi.org/10.1093/petrology/2.2.209.","productDescription":"39 p.","startPage":"209","endPage":"247","costCenters":[],"links":[{"id":385815,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"California","otherGeospatial":"Monterey Bay","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -122.18170166015625,\n 36.52288052805137\n ],\n [\n -121.51977539062499,\n 36.52288052805137\n ],\n [\n -121.51977539062499,\n 37.03983207971425\n ],\n [\n -122.18170166015625,\n 37.03983207971425\n ],\n [\n -122.18170166015625,\n 36.52288052805137\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"2","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Coleman, R. G.","contributorId":75170,"corporation":false,"usgs":true,"family":"Coleman","given":"R.","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":816121,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70220606,"text":"70220606 - 1961 - Copper, vanadium, and uranium deposits in sandstone-their distribution and geochemical cycles","interactions":[],"lastModifiedDate":"2021-05-20T22:59:15.670349","indexId":"70220606","displayToPublicDate":"1961-05-01T17:55:02","publicationYear":"1961","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":"Copper, vanadium, and uranium deposits in sandstone-their distribution and geochemical cycles","docAbstract":"Deposits of copper, vanadium, and uranium in nonmarine sandstones are numerous and widespread. Copper deposits, with or without uranium, are mainly resident in first-generation arkosic sandstones derived from granitic rock terrains; deposits rich in vanadium, with or without much uranium, are dominantly in second-generation sandstones derived from sedimentary rocks; and the uranium deposits with little or no vanadium or copper are in either first- or second-generation sandstones, many of which are associated with beds containing volcanic debris. All three metals are dispersed in igneous rocks but not in close association. Copper and uranium enter the hydrothermal environment, but the record of vanadium in hydrothermal solutions and veins is scant. Some of the uranium and most of the copper minerals in igneous rocks and veins oxidize readily and the metals go into surface- and ground-water solutions, but the vanadium in igneous rocks is not so easily mobilized-under normal geologic conditions, conceivably it may require diagenetic reactions and a second period of weathering to solubilize much vanadium. All three metals precipitate from solutions in the presence of a reducing agent, such as carbonaceous material or associated sulfide ions, either in sediments as they accumulate or in existing rocks. These geochemical habits permit the concept that copper and uranium are made available by weathering of igneous rock terrains and hence might accumulate in first-generation sediments, whereas vanadium would be commonly available only after a second period of weathering. Perhaps the oxidation or devitrification of volcanic debris may contribute uranium to ground waters as does the weathering, of igneous rocks.
","language":"English","publisher":"Society of Economic Geologists","doi":"10.2113/gsecongeo.56.3.509","usgsCitation":"Fischer, R.P., and Stewart, J.H., 1961, Copper, vanadium, and uranium deposits in sandstone-their distribution and geochemical cycles: Economic Geology, v. 56, no. 3, p. 509-520, https://doi.org/10.2113/gsecongeo.56.3.509.","productDescription":"12 p.","startPage":"509","endPage":"520","costCenters":[],"links":[{"id":385822,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"56","issue":"3","noUsgsAuthors":false,"publicationDate":"1961-05-01","publicationStatus":"PW","contributors":{"authors":[{"text":"Fischer, R. P.","contributorId":89958,"corporation":false,"usgs":true,"family":"Fischer","given":"R.","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":816138,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Stewart, J. H.","contributorId":36421,"corporation":false,"usgs":true,"family":"Stewart","given":"J.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":816139,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70175757,"text":"70175757 - 1961 - Floods in Minnesota--Magnitude and frequency","interactions":[],"lastModifiedDate":"2018-03-19T10:58:47","indexId":"70175757","displayToPublicDate":"1961-03-16T10:00:00","publicationYear":"1961","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":105,"text":"Bulletin","active":false,"publicationSubtype":{"id":2}},"seriesNumber":"12","title":"Floods in Minnesota--Magnitude and frequency","docAbstract":"No abstract available.
","language":"English","publisher":"Minnesota Department of Conservation, Division of Waters","publisherLocation":"St. Paul, MN","usgsCitation":"Prior, C.H., and Hess, J., 1961, Floods in Minnesota--Magnitude and frequency: Bulletin 12, 142 p.","productDescription":"142 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":392,"text":"Minnesota Water Science Center","active":true,"usgs":true}],"links":[{"id":326880,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United 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