{"pageNumber":"7090","pageRowStart":"177225","pageSize":"25","recordCount":185299,"records":[{"id":51018,"text":"ofr51121 - 1951 - Memorandum on results of pumping test at Goodrich plant site, Miami, Oklahoma","interactions":[],"lastModifiedDate":"2019-12-05T09:46:45","indexId":"ofr51121","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1951","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":"51-121","title":"Memorandum on results of pumping test at Goodrich plant site, Miami, Oklahoma","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr51121","usgsCitation":"Jacobsen, C., and Reed, E.W., 1951, Memorandum on results of pumping test at Goodrich plant site, Miami, Oklahoma: U.S. Geological Survey Open-File Report 51-121, 30 p., https://doi.org/10.3133/ofr51121.","productDescription":"30 p.","costCenters":[],"links":[{"id":178893,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1951/0121/report-thumb.jpg"},{"id":369971,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1951/0121/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Oklahoma","county":"Ottawa County","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-94.619,37],[-94.6196,36.7664],[-94.6187,36.6703],[-94.6187,36.6694],[-95.001,36.6723],[-95.0004,36.9518],[-95.0073,36.9539],[-95.0192,36.9566],[-95.0286,36.9641],[-95.0323,36.9706],[-95.0389,36.9758],[-95.0389,36.9772],[-95.0325,36.9783],[-95.0313,36.9792],[-95.0361,36.9866],[-95.0375,36.9916],[-95.0362,36.9957],[-95.0336,36.9986],[-95.0331,36.9992],[-94.8595,36.9997],[-94.619,37]]]},\"properties\":{\"name\":\"Ottawa\",\"state\":\"OK\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a2ce4b07f02db613e58","contributors":{"authors":[{"text":"Jacobsen, C.L.","contributorId":38222,"corporation":false,"usgs":true,"family":"Jacobsen","given":"C.L.","email":"","affiliations":[],"preferred":false,"id":242761,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Reed, E. W.","contributorId":69640,"corporation":false,"usgs":true,"family":"Reed","given":"E.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":242762,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":14692,"text":"ofr5171 - 1951 - Preliminary geologic map of Eagleton quadrangle, Montana","interactions":[{"subject":{"id":14692,"text":"ofr5171 - 1951 - Preliminary geologic map of Eagleton quadrangle, Montana","indexId":"ofr5171","publicationYear":"1951","noYear":false,"title":"Preliminary geologic map of Eagleton quadrangle, Montana"},"predicate":"SUPERSEDED_BY","object":{"id":62631,"text":"gq29 - 1953 - Geology of the Eagleton quadrangle, Montana","indexId":"gq29","publicationYear":"1953","noYear":false,"title":"Geology of the Eagleton quadrangle, Montana"},"id":1}],"supersededBy":{"id":62631,"text":"gq29 - 1953 - Geology of the Eagleton quadrangle, Montana","indexId":"gq29","publicationYear":"1953","noYear":false,"title":"Geology of the Eagleton quadrangle, Montana"},"lastModifiedDate":"2012-02-02T00:07:07","indexId":"ofr5171","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1951","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":"51-71","title":"Preliminary geologic map of Eagleton quadrangle, Montana","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr5171","usgsCitation":"Lindvall, R.M., 1951, Preliminary geologic map of Eagleton quadrangle, Montana: U.S. Geological Survey Open-File Report 51-71, 1 p. :ill., map ;66 x 114 cm., https://doi.org/10.3133/ofr5171.","productDescription":"1 p. :ill., map ;66 x 114 cm.","costCenters":[],"links":[{"id":148522,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac8e4b07f02db67c095","contributors":{"authors":[{"text":"Lindvall, Robert M.","contributorId":34523,"corporation":false,"usgs":true,"family":"Lindvall","given":"Robert","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":169856,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":51065,"text":"ofr51165 - 1951 - Supplemental chemical analyses of surface waters in the Little Missouri River basin, Montana and North Dakota","interactions":[],"lastModifiedDate":"2012-02-02T00:11:24","indexId":"ofr51165","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1951","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":"51-165","title":"Supplemental chemical analyses of surface waters in the Little Missouri River basin, Montana and North Dakota","language":"ENGLISH","doi":"10.3133/ofr51165","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1951, Supplemental chemical analyses of surface waters in the Little Missouri River basin, Montana and North Dakota: U.S. Geological Survey Open-File Report 51-165, 5 p., https://doi.org/10.3133/ofr51165.","productDescription":"5 p.","costCenters":[],"links":[{"id":179045,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b01e4b07f02db6984ba","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":532109,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":51064,"text":"ofr51164 - 1951 - Chemical analyses of surface waters in the Bighorn River basin, Wyoming and Montana, November 1945 to September 1949","interactions":[],"lastModifiedDate":"2012-02-02T00:11:24","indexId":"ofr51164","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1951","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":"51-164","title":"Chemical analyses of surface waters in the Bighorn River basin, Wyoming and Montana, November 1945 to September 1949","language":"ENGLISH","doi":"10.3133/ofr51164","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1951, Chemical analyses of surface waters in the Bighorn River basin, Wyoming and Montana, November 1945 to September 1949: U.S. Geological Survey Open-File Report 51-164, 17 tables, https://doi.org/10.3133/ofr51164.","productDescription":"17 tables","costCenters":[],"links":[{"id":179044,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e2e4b07f02db5e49be","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":532108,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":50951,"text":"ofr5191 - 1951 - Ground water in the Mohall area, Bottineau and Renville Counties, North Dakota","interactions":[],"lastModifiedDate":"2021-03-18T21:28:50.810463","indexId":"ofr5191","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1951","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":"51-91","title":"Ground water in the Mohall area, Bottineau and Renville Counties, North Dakota","docAbstract":"<p><span>The Mohall area includes about 120 square miles in Bottineau </span><span>and Renville Counties in northwestern North Dakota. Mohall, whose </span><span>1950 population was 1,073, is the only town in the area. </span></p><p><span>The area is part of the Drift Prairie section of the Central Lowland physiographic province. It is characterized by the gently undulating ground moraine plain which slopes regionally to the northeast. It is drained by several southeast-trending intermittent streams which run almost at right angles to the regional slope. </span></p><p><span>The geologic formations in the Mohall area may be conveniently grouped into three units: the alluvium or alluvial deposits, which are found in the valleys of the intermittent streams, the till and associated glaciofluvial deposits, and the bedrock formations. </span></p><p><span>Ground water of reasonably good quality is obtained in the area only from the alluvial deposits. Because of the limited areal extent of these deposits, only a small number of farms obtain water supplies from them. However, the municipal water supply of the town of Mohall is obtained from these deposits in Spring Coulee northeast of the town, and much water for rural domestic use is hauled from the Becker well southwest of the town, in Little Deep Creek.</span></p><p><span>The principal source of recharge to the alluvial deposits is seepage during the spring runoff period. Natural discharge occurs by underflow down the stream valleys, by evaporation from open water and marshy areas and transpiration by plants.</span></p><p><span>The coefficient of transmissibility of </span><span>the alluvium, n the basis </span><span>of short pumping tests on Mohan wells 3 </span><span>and 4, is </span><span>indicated to be </span><span>about 6,000 </span><span>gallons a day per foot </span><span>at well 3 and about 20,000 gallons </span><span>a day per foot at well 4. The specific yield was computed as 0.25 </span><span>from the pumping </span><span>test on well </span><span>3. </span><span>No gravel of importance was en</span><span>countered in the two cross sections that were drilled across Spring </span><span>Coulee near the municipal wells, and the greatest thickness of satu</span><span>rated alluvial deposits found was only about 10 feet.</span></p><p><span>A Saturated thickness of 20 feet of sand and gravel was penetrated in test drilling along Cut Bank Creek. This is the greatest thickness of saturated alluvial deposits penetrated anywhere in the area. Ground water in storage in these alluvial deposits has been estimated to be about 150 million gallons per mile. These deposits are favorably situated to receive recharge, as Cut Bank Creek drains a rather large area and contains long stretches of open water perennially, Therefore, it is believed that the alluvial deposits of Cut Bank Creek offer the best promise for the development of moderately large perennial ground-water supplies for the present and probable future needs of the town of Mohall. </span></p><p><span>Test drilling in West Cut Bank Creek and in Little Deep Creek did not reveal alluvial deposits of such character and saturated thickness as to be considered favorable for the development of moderate to large water supplies, though some of the material encountered should yield adequate quantities for farm supplies.</span></p><p><span>The till with its associated glaciofluvial deposits is the surface formation in the&nbsp;area except where covered by the alluvial deposits&nbsp;in the stream valleys. In the Mohall areas, this formation is not an important aquifer and fewer than half a dozen wells are known to obtain water from it. The glaciofluvial deposits penetrated&nbsp;by the test holes are not considered adequate&nbsp;sources for permanent municipal or industrial supplies because they are likely to have small-areal extent and the overlying, relatively impermeable till makes seasonal recharge to them practically impossible.</span></p><p><span>Test drilling in the Souris River Valley about 12 miles west of Mohall penetrated as mutt as 58 feet of fluvial sediments, but practi-cally all the material is clay and silt. No important aquifers were found there. </span></p><p><span>At least 50 percent of all the farm water supplies in the area are obtained from wells in the bedrock formations, which probably consist of the Fox Hills sandstone, the Cannonball formation, and the Ludlow and Tongue Rtter members of the Fort Union formation. </span></p><p><span>Underlying these formations is approximately 2,600 feet of Cretaceous shale, which'is not water bearing. Water from the \"Dakota\" sandstone (including the possible equivalent of the Fuson shale and Lakota sandstone) may be obtained at depths of about 3,200 to 3,300 feet. The \"Dakota sandstone\" probably would yield water in sufficient quantity for municipal and many industrial purposes in this areas but the water is likely to be too highly mineralized for most domestic uses.</span></p><p><span>Jurassic formations underlie the&nbsp;Cretaceous formations in the area. They do not constitute aquifers of importance, and, any water found in them is likely to be too highly mineralized for most purposes. </span></p><p><span>In the Mohall area,&nbsp;by far the most suitable water for general purposes is obtained from the shallow alluvial deposits in the stream valleys. Of the seven samples of this water water analyzed, the highest concentration of dissolved solids was 1,242 parts per million and the lowest, 317 parts. The iron content was&nbsp;higher than desirable in two samples but satisfactory in all the&nbsp;others. Total hardness ranged from 196 to 570, which is higher than desirable. Nitrate was present in all samples analyzed and was excessively high in two samples. </span></p><p><span>Water samples for analysis were not obtained from the till and associated glaciofluvial deposits but the water from these aquifers is likely to be more highly mineralized than the water from the alluvial. deposits. </span></p><p><span>The water from the upper part of the bedrock is highly mineralized, but its mineral content varies considerably. The chloride concentration of the samples analyzed ranges from 608 to 3,740 parts per million and the bicarbonate concentration ranges from 160 to 860 parts per million. The specific conductance ranges from 3,190 to 11,120 micromhos and may represent total mineralization on the order of 1,500 to more than 6,000 parts per million in the water with high chloride and bicarbonate content. </span></p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr5191","usgsCitation":"Akin, P., 1951, Ground water in the Mohall area, Bottineau and Renville Counties, North Dakota: U.S. Geological Survey Open-File Report 51-91, Report: 90 p.; 2 Plates: 8.00 x 7.80 inches and 10.30 x 5.66 inches, https://doi.org/10.3133/ofr5191.","productDescription":"Report: 90 p.; 2 Plates: 8.00 x 7.80 inches and 10.30 x 5.66 inches","costCenters":[{"id":478,"text":"North Dakota Water Science Center","active":true,"usgs":true},{"id":34685,"text":"Dakota Water Science 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,{"id":51015,"text":"ofr51118 - 1951 - Occurrence of fresh-water limestones restricts Pliocene deposits in southeastern Florida","interactions":[],"lastModifiedDate":"2019-11-14T14:36:42","indexId":"ofr51118","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1951","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":"51-118","title":"Occurrence of fresh-water limestones restricts Pliocene deposits in southeastern Florida","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr51118","usgsCitation":"Hoy, N., 1951, Occurrence of fresh-water limestones restricts Pliocene deposits in southeastern Florida: U.S. Geological Survey Open-File Report 51-118, 5 p., https://doi.org/10.3133/ofr51118.","productDescription":"5 p.","costCenters":[],"links":[{"id":369223,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1951/0118/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":178798,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1951/0118/report-thumb.jpg"}],"country":"United States","state":"Florida","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -81.58447265624999,\n              25.16517336866393\n            ],\n            [\n              -79.91455078125,\n              25.16517336866393\n            ],\n            [\n              -79.91455078125,\n              28.22697003891834\n            ],\n            [\n              -81.58447265624999,\n              28.22697003891834\n            ],\n            [\n              -81.58447265624999,\n              25.16517336866393\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4af5e4b07f02db69249f","contributors":{"authors":[{"text":"Hoy, N.D.","contributorId":15618,"corporation":false,"usgs":true,"family":"Hoy","given":"N.D.","email":"","affiliations":[],"preferred":false,"id":242757,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":63733,"text":"gp86 - 1951 - Total intensity aeromagnetic map of Jay County, Indiana","interactions":[],"lastModifiedDate":"2021-12-10T21:16:49.424905","indexId":"gp86","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1951","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":317,"text":"Geophysical Investigations Map","code":"GP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"86","title":"Total intensity aeromagnetic map of Jay County, Indiana","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/gp86","usgsCitation":"Henderson, J.R., and Meuschke, J.L., 1951, Total intensity aeromagnetic map of Jay County, Indiana: U.S. Geological Survey Geophysical Investigations Map 86, 1 Plate: 43.86 × 28.88 inches, https://doi.org/10.3133/gp86.","productDescription":"1 Plate: 43.86 × 28.88 inches","costCenters":[],"links":[{"id":187135,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":392756,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_3581.htm"},{"id":260581,"rank":900,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/gp/0086/plate-1.pdf"}],"scale":"63360","country":"United States","state":"Indiana","county":"Jay County","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-85.0689,40.5688],[-84.992,40.5697],[-84.8782,40.571],[-84.8037,40.5723],[-84.8059,40.3534],[-84.8064,40.3102],[-84.901,40.3096],[-85.0186,40.3092],[-85.1302,40.3082],[-85.2182,40.3073],[-85.2205,40.379],[-85.2091,40.3793],[-85.2073,40.3789],[-85.2066,40.4804],[-85.2012,40.4804],[-85.2008,40.5679],[-85.1064,40.5683],[-85.0689,40.5688]]]},\"properties\":{\"name\":\"Jay\",\"state\":\"IN\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4ee4b07f02db6283a3","contributors":{"authors":[{"text":"Henderson, John R. Jr.","contributorId":96346,"corporation":false,"usgs":true,"family":"Henderson","given":"John","suffix":"Jr.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":269474,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Meuschke, J. L.","contributorId":53349,"corporation":false,"usgs":true,"family":"Meuschke","given":"J.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":269473,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":68822,"text":"oc42 - 1951 - Subsurface geologic cross sections of Mesozoic rocks in northeastern Colorado","interactions":[],"lastModifiedDate":"2012-02-10T00:11:24","indexId":"oc42","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1951","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":328,"text":"Oil and Gas Investigation Chart","code":"OC","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"42","title":"Subsurface geologic cross sections of Mesozoic rocks in northeastern Colorado","language":"ENGLISH","doi":"10.3133/oc42","usgsCitation":"Blair, R., 1951, Subsurface geologic cross sections of Mesozoic rocks in northeastern Colorado: U.S. Geological Survey Oil and Gas Investigation Chart 42, 2 stratigraphic sections on 2 sheets ;sheets each 127 x 81 cm., https://doi.org/10.3133/oc42.","productDescription":"2 stratigraphic sections on 2 sheets ;sheets each 127 x 81 cm.","costCenters":[],"links":[{"id":104831,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_5200.htm","linkFileType":{"id":5,"text":"html"},"description":"5200"},{"id":188522,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"6000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -105.5,39.5 ], [ -105.5,41 ], [ -102,41 ], [ -102,39.5 ], [ -105.5,39.5 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b05e4b07f02db699a98","contributors":{"authors":[{"text":"Blair, R.W.","contributorId":65514,"corporation":false,"usgs":true,"family":"Blair","given":"R.W.","email":"","affiliations":[],"preferred":false,"id":278985,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":69061,"text":"om118 - 1951 - Geologic map of the Spread Creek-Gros Ventre River area, Teton County, Wyoming","interactions":[],"lastModifiedDate":"2012-02-02T00:13:34","indexId":"om118","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1951","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":329,"text":"Oil and Gas Investigation Map","code":"OM","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"118","title":"Geologic map of the Spread Creek-Gros Ventre River area, Teton County, Wyoming","language":"ENGLISH","doi":"10.3133/om118","usgsCitation":"Love, J.D., Keefer, W.R., Duncan, D., Gergquist, H., and Hose, R.K., 1951, Geologic map of the Spread Creek-Gros Ventre River area, Teton County, Wyoming: U.S. Geological Survey Oil and Gas Investigation Map 118, 1 map., https://doi.org/10.3133/om118.","productDescription":"1 map.","costCenters":[],"links":[{"id":104894,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_5264.htm","linkFileType":{"id":5,"text":"html"},"description":"5264"},{"id":187815,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"48000","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae6e4b07f02db68b09a","contributors":{"authors":[{"text":"Love, J. D.","contributorId":64620,"corporation":false,"usgs":true,"family":"Love","given":"J.","middleInitial":"D.","affiliations":[],"preferred":false,"id":279554,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Keefer, W. R.","contributorId":21538,"corporation":false,"usgs":true,"family":"Keefer","given":"W.","middleInitial":"R.","affiliations":[],"preferred":false,"id":279551,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Duncan, D.C.","contributorId":56996,"corporation":false,"usgs":true,"family":"Duncan","given":"D.C.","email":"","affiliations":[],"preferred":false,"id":279552,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Gergquist, H.R.","contributorId":106580,"corporation":false,"usgs":true,"family":"Gergquist","given":"H.R.","email":"","affiliations":[],"preferred":false,"id":279555,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Hose, R. K.","contributorId":63388,"corporation":false,"usgs":true,"family":"Hose","given":"R.","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":279553,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":71161,"text":"tei55 - 1951 - Reconnaissance for radioactive deposits along the upper Porcupine River, northeastern Alaska","interactions":[],"lastModifiedDate":"2012-02-02T00:13:45","indexId":"tei55","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1951","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":"55","title":"Reconnaissance for radioactive deposits along the upper Porcupine River, northeastern Alaska","language":"ENGLISH","doi":"10.3133/tei55","usgsCitation":"White, M.G., 1951, Reconnaissance for radioactive deposits along the upper Porcupine River, northeastern Alaska: U.S. Geological Survey Trace Elements Investigations 55, 29 p. : 2 maps ; 29 cm., https://doi.org/10.3133/tei55.","productDescription":"29 p. : 2 maps ; 29 cm.","costCenters":[],"links":[{"id":186079,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/tei/055/report-thumb.jpg"},{"id":90564,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/tei/055/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":90565,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/tei/055/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":90566,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/tei/055/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"24000","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a74e4b07f02db6444c5","contributors":{"authors":[{"text":"White, Max Gregg","contributorId":91841,"corporation":false,"usgs":true,"family":"White","given":"Max","email":"","middleInitial":"Gregg","affiliations":[],"preferred":false,"id":283747,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":71168,"text":"tei68 - 1951 - Reconnaissance of radioactive rocks of Maine","interactions":[],"lastModifiedDate":"2014-05-23T15:58:40","indexId":"tei68","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1951","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":"68","title":"Reconnaissance of radioactive rocks of Maine","docAbstract":"<p>The state of Maine was traversed with car-mounted Geiger-Mueller equipment in the late summer of 1948 and the radioactivity of approximately 4,600 miles of road was logged.</p>\n<br>\n<p>All samples were analyzed, both in the field by comparing the radioactivity of each sample to the radioactivity of a stranded measured with a simple scaling modification of a portable counter, and in the Geological Survey’s Trace Elements Section Washington Laboratory. Differences between both types of analyses were negligible. The maximum equivalent uranium content of the most radioactive rocks thus analyzed was 0.008 percent. A 1,400-square-mile abnormally radioactive province in southwestern Maine was outlined.</p>\n<br>\n<p>The outcrop data obtained from car traversing are evaluated statistically. Cumulative frequency distribution curves are drawn to show the distribution of outcrops at various levels of radioactivity, and straight-line extensions are made to show to maximum probable grade for various rock types and areas in Maine. A maximum grade of 0.055 percent equivalent uranium is thus predicted for the entire state. This  prediction necessarily is a broad generalization because large areas of Main are inaccessible for car traversing. A concept of evaluation of an area for possible mineral deposits is proposed on the basis of lithology, and observed and indicated ranges in grade.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/tei68","collaboration":"Prepared by the Geological Survey for the United States Atomic Energy Commission","usgsCitation":"Nelson, J.M., and Narten, P., 1951, Reconnaissance of radioactive rocks of Maine: U.S. Geological Survey Trace Elements Investigations 68, Report: 43 p.; 1 Plate: 15.49 x 23.65 inches, https://doi.org/10.3133/tei68.","productDescription":"Report: 43 p.; 1 Plate: 15.49 x 23.65 inches","numberOfPages":"43","costCenters":[],"links":[{"id":186158,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/tei/068/report-thumb.jpg"},{"id":90575,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/tei/068/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":285585,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/tei/0068/figure-1.pdf"}],"country":"United States","state":"Maine","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -71.0,43.0 ], [ -71.0,47.0 ], [ -67.0,47.0 ], [ -67.0,43.0 ], [ -71.0,43.0 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a68e4b07f02db63afe5","contributors":{"authors":[{"text":"Nelson, John M.","contributorId":83578,"corporation":false,"usgs":true,"family":"Nelson","given":"John","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":283756,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Narten, Perry F.","contributorId":59780,"corporation":false,"usgs":true,"family":"Narten","given":"Perry F.","affiliations":[],"preferred":false,"id":283755,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":71169,"text":"tei69 - 1951 - Reconnaissance of radioactive rocks of Massachusetts","interactions":[],"lastModifiedDate":"2014-05-23T15:57:55","indexId":"tei69","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1951","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":"69","title":"Reconnaissance of radioactive rocks of Massachusetts","docAbstract":"<p>During the 1948 and 1949 field seasons radiometric car traverses were made along the numbered federal and state highways and along many unnumbered roads of Massachusetts.</p>\n<br>\n<p>Near Worcester pegmatitic rocks are estimated to contain about 250\npounds of uranium and 8,500 pounds of thoria per foot of depth. Near\nSouthbridge pegmatitic rocks are estimated to contain about 6,500 pounds\nof thoria per foot of depth.</p>\n<br>\n<p>A central belt was estimated to contain about 0.003 percent equivalent uranium but less than 0.001 percent uranium in nearly all roadside\nmaterials.</p>\n<br>\n<p>Several smaller localities of radioactivity similar to that of the\ncentral belt were found but none appear to be important economically.</p>\n<br>\n<p>Massachusetts is not considered a favorable area for uranium\ndeposits, although some low-grade deposits of thorium are present.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/tei69","collaboration":"Prepared by the Geological Survey for the United States Atomic Energy Commission","usgsCitation":"Johnson, D.H., 1951, Reconnaissance of radioactive rocks of Massachusetts: U.S. Geological Survey Trace Elements Investigations 69, Report: 16 p.; 2 Plates: 15.46 x 10.93 inches and 15.93 x 16.76 inches, https://doi.org/10.3133/tei69.","productDescription":"Report: 16 p.; 2 Plates: 15.46 x 10.93 inches and 15.93 x 16.76 inches","numberOfPages":"18","costCenters":[],"links":[{"id":186159,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/tei/069/report-thumb.jpg"},{"id":90576,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/tei/069/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":285586,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/tei/0069/plate-1.pdf"},{"id":285587,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/tei/0069/plate-2.pdf"}],"scale":"24000","country":"United States","state":"Massachusetts","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -73.0,41.0 ], [ -73.0,43.0 ], [ -70.0,43.0 ], [ -70.0,41.0 ], [ -73.0,41.0 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a68e4b07f02db63aff1","contributors":{"authors":[{"text":"Johnson, Donald H.","contributorId":16084,"corporation":false,"usgs":true,"family":"Johnson","given":"Donald","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":283757,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":68908,"text":"om111 - 1951 - Geology of the Hardin area, Big Horn and Yellowstone Counties, Montana","interactions":[],"lastModifiedDate":"2019-12-27T12:55:08","indexId":"om111","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1951","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":329,"text":"Oil and Gas Investigation Map","code":"OM","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"111","title":"Geology of the Hardin area, Big Horn and Yellowstone Counties, Montana","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/om111","usgsCitation":"Richards, P.W., and Rogers, C., 1951, Geology of the Hardin area, Big Horn and Yellowstone Counties, Montana: U.S. Geological Survey Oil and Gas Investigation Map 111, Plate: 41.21 x 53.83 inches, https://doi.org/10.3133/om111.","productDescription":"Plate: 41.21 x 53.83 inches","costCenters":[],"links":[{"id":189460,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":104887,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_5257.htm","linkFileType":{"id":5,"text":"html"},"description":"5257"}],"scale":"63360","country":"United States","state":"Montana","county":"Big Horn County, Yellowstone County","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -108.0917,\n              45.1667\n            ],\n            [\n              -107.4500,\n              45.1667\n            ],\n            [\n              -107.4500,\n              45.7583\n            ],\n            [\n              -108.0917,\n              45.7583\n            ],\n            [\n              -108.0917,\n              45.1667\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4acfe4b07f02db68001f","contributors":{"authors":[{"text":"Richards, Paul W.","contributorId":13248,"corporation":false,"usgs":true,"family":"Richards","given":"Paul","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":279198,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Rogers, C.P. Jr.","contributorId":14897,"corporation":false,"usgs":true,"family":"Rogers","given":"C.P.","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":279199,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":62801,"text":"gq9 - 1951 - Mount Toby, Massachusetts Surficial geology","interactions":[],"lastModifiedDate":"2012-02-10T00:10:48","indexId":"gq9","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1951","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":316,"text":"Geologic Quadrangle","code":"GQ","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"9","title":"Mount Toby, Massachusetts Surficial geology","language":"ENGLISH","doi":"10.3133/gq9","usgsCitation":"Jahns, R.H., 1951, Mount Toby, Massachusetts Surficial geology: U.S. Geological Survey Geologic Quadrangle 9, 1 map., https://doi.org/10.3133/gq9.","productDescription":"1 map.","costCenters":[],"links":[{"id":102571,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_1020.htm","linkFileType":{"id":5,"text":"html"},"description":"1020"},{"id":186892,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"680","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -72.61749999999999,42.3675 ], [ -72.61749999999999,42.5 ], [ -72.5,42.5 ], [ -72.5,42.3675 ], [ -72.61749999999999,42.3675 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b02e4b07f02db698cfa","contributors":{"authors":[{"text":"Jahns, Richard Henry","contributorId":45291,"corporation":false,"usgs":true,"family":"Jahns","given":"Richard","email":"","middleInitial":"Henry","affiliations":[],"preferred":false,"id":267875,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":4582,"text":"wsp1124 - 1951 - Surface water supply of the United States, 1948, Part XIV, Pacific slope basins in Oregon and lower Columbia River basin","interactions":[],"lastModifiedDate":"2012-02-02T00:05:48","indexId":"wsp1124","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1951","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1124","title":"Surface water supply of the United States, 1948, Part XIV, Pacific slope basins in Oregon and lower Columbia River basin","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/wsp1124","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1951, Surface water supply of the United States, 1948, Part XIV, Pacific slope basins in Oregon and lower Columbia River basin: U.S. Geological Survey Water Supply Paper 1124, viii, 273 p. :ill. ;23 cm., https://doi.org/10.3133/wsp1124.","productDescription":"viii, 273 p. :ill. ;23 cm.","costCenters":[],"links":[{"id":139861,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1124/report-thumb.jpg"},{"id":31639,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1124/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afce4b07f02db696727","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":528277,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
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