{"pageNumber":"1850","pageRowStart":"46225","pageSize":"25","recordCount":46593,"records":[{"id":70095692,"text":"tei452 - 1954 - Reconnaissance for uranium-bearing lignite in the Ekalaka Lignite Field, Carter County, Montana","interactions":[],"lastModifiedDate":"2014-05-27T15:01:17","indexId":"tei452","displayToPublicDate":"1954-01-01T15:35:00","publicationYear":"1954","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":"452","title":"Reconnaissance for uranium-bearing lignite in the Ekalaka Lignite Field, Carter County, Montana","docAbstract":"<p>Uranium-bearing lignite beds 1.5 to 8 feet thick occur in the Fort Union formation of the southern part of the Ekalaka Hills, Carter County, Mont. Data from surface outcrops indicate that an area of about 1,400 acres is underlain by 16,500,000 tons of uranium-bearing lignite containing 700 tons of uranium. The uranium content of the lignite beds ranges from 0.001 to 0.034 percent.</p> \n<br/>\n<p>Ironstone concretions in the massive coarse-grained sandstones in the upper part of the Fort Union formation contain 0.005 percent uranium in the northern and eastern parts of the area. These sandstones are good potential host rocks for uranium mineralization and are lithologically similar to the massive coarse-grained uranium-bearing sandstones of the Wasatch formation in the Pumpkin Buttes area of the Powder River Basin.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/tei452","collaboration":"This report concerns work done on behalf of the Division of Raw Materials of the U.S. Atomic Energy Commission","usgsCitation":"Gill, J.R., 1954, Reconnaissance for uranium-bearing lignite in the Ekalaka Lignite Field, Carter County, Montana: U.S. Geological Survey Trace Elements Investigations 452, 27 p., https://doi.org/10.3133/tei452.","productDescription":"27 p.","numberOfPages":"28","costCenters":[],"links":[{"id":283500,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/tei452.jpg"},{"id":284569,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/tei/0452/report.pdf"}],"country":"United States","state":"Montana","county":"Carter County","otherGeospatial":"Ekalaka Hills","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -105.0394,44.9974 ], [ -105.0394,46.1369 ], [ -104.0396,46.1369 ], [ -104.0396,44.9974 ], [ -105.0394,44.9974 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53559532e4b0120853e8c19d","contributors":{"authors":[{"text":"Gill, James R.","contributorId":44904,"corporation":false,"usgs":true,"family":"Gill","given":"James","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":491375,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70098416,"text":"tei436 - 1954 - Uranium in the Mayoworth area, Johnson County, Wyoming - a preliminary report","interactions":[],"lastModifiedDate":"2014-06-11T14:48:05","indexId":"tei436","displayToPublicDate":"1954-01-01T10:05:00","publicationYear":"1954","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":"436","title":"Uranium in the Mayoworth area, Johnson County, Wyoming - a preliminary report","docAbstract":"<p>The uranium mineral, metatyuyamunite, occurs in the basal limestone of the Sundance formation of late Jurassic age along the east flank of the Bighorn Mountains, about 2 miles southwest of the abandoned Mayoworth post office. This occurrence is of particular interest because it is the first uranium mineralization reported from a marine limestone in Wyoming. The discovery uranium claims were filed in July 1953, by J.S. Masek, Dan Oglesby, and Jack Emery of Casper, Wyo. Subsequent reconnaissance investigations have been made by private individuals and geologists of the U.S. Geological Survey and Atomic Energy Commission.<p>\n<br/>\n<p>The metatyuyamunite is concentrated in a hard gray oolitic limestone that forms the basal bed of the Sundance formation. A selected sample of limestone from a fresh face in the northernmost deposit known at the time of the field examination contained 0.70 percent equivalent uranium and 0.71 percent uranium. Eight samples of the limestone taken at the sample place by the Atomic Energy Commission contained from 0.007 to 0.22 percent uranium. A chip sample from the weathered outcrop at the top of this limestone half a mile to the southeast contained 0.17 percent equivalent uranium and 0.030 percent uranium. A dinosaur bone from the middle part of the Morrison formation contained 0.044 percent equivalent uranium and 0.004 percent uranium.</p>\n<br/>\n<p> metatyuyamunite  forms a conspicuous yellow coating along fracture planes cutting the oolitic limestone and has also replaced many of the oolites within the solid limestone and has also replaced many of the oolites within the solid limestone even where fractures are not present.</p>\n<br/>\n<p>Many radioactive spots in the basal limestone of the Sundance formation were examined in a reconnaissance fashion along the outcrop for a distance of half a mile south of the initial discovery. Samples were taken for analysis only at the northern and southern margins of this interval. Outcrops farther north and south were not studied.</p>\n<br/>\n<p>There are not sufficient data to make even rough estimates of tonnage and grade of the occurrences. The extent of the limestone, the approximate boundaries of the area of above-normal radioactivity, and the possibilities of other radioactive zones have not been thoroughly investigated. Although dinosaur bones in the Morrison formation were radioactive wherever they were tested, no significant amount of radioactivity was observed in rocks adjacent to the bones.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/tei436","collaboration":"This report concerns work done on behalf of the the Division of Raw Materials of the U.S. Atomic Energy Commission","usgsCitation":"Love, J.D., 1954, Uranium in the Mayoworth area, Johnson County, Wyoming - a preliminary report: U.S. Geological Survey Trace Elements Investigations 436, 25 p., https://doi.org/10.3133/tei436.","productDescription":"25 p.","numberOfPages":"26","costCenters":[],"links":[{"id":285846,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/tei/0436/report.pdf"},{"id":284140,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/tei436.jpg"}],"country":"United States","state":"Wyoming","county":"Johnson County","otherGeospatial":"Mayoworth","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -107.372,43.4937 ], [ -107.372,44.5653 ], [ -106.0076,44.5653 ], [ -106.0076,43.4937 ], [ -107.372,43.4937 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"535595d6e4b0120853e8c2d0","contributors":{"authors":[{"text":"Love, J. D.","contributorId":64620,"corporation":false,"usgs":true,"family":"Love","given":"J.","middleInitial":"D.","affiliations":[],"preferred":false,"id":491699,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70010825,"text":"70010825 - 1954 - Thick target bremsstrahlung spectra for 1.00-, 1.25-, and 1.40-Mev electrons","interactions":[],"lastModifiedDate":"2020-11-27T20:58:49.246707","indexId":"70010825","displayToPublicDate":"1954-01-01T00:00:00","publicationYear":"1954","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3060,"text":"Physical Review","active":true,"publicationSubtype":{"id":10}},"title":"Thick target bremsstrahlung spectra for 1.00-, 1.25-, and 1.40-Mev electrons","docAbstract":"<p><span>The spectrum of radiation produced by 1.0-, 1.25-, and 1.40-Mev electrons incident on a thick tungsten target was measured at 0° and 90° with the incident beam by a method involving the magnetic analysis of Compton electrons. The effects of electron scattering and energy loss in the target preclude any simple interpretation of this data to yield a differential bremsstrahlung cross section. However, an estimate of the spectra to be expected at 0° and 90° was obtained by combining the Sauter expression for the bremsstrahlung cross section with the available information on electron scatter and energy loss in the target and backscatter from the target. The reliability of the estimate is limited because the Sauter formula was calculated by using the Born approximation, the electron scattering calculations are applicable to an infinite medium only, and the backscatter was estimated empirically from Bothe's experimental data which were obtained with lower energy electrons (370 kev). Furthermore electron energy straggling was neglected. Nevertheless, the predicted spectral shapes at 0° and 90° and the relative intensities at these two angles are in qualitative agreement with the measured values. The absolute magnitudes of the measured intensities at both angles are about a factor of two greater than the predicted values.</span></p>","language":"English","publisher":"American Physical Society","doi":"10.1103/PhysRev.96.1344","usgsCitation":"Miller, W., Motz, J.W., and Cialella, C., 1954, Thick target bremsstrahlung spectra for 1.00-, 1.25-, and 1.40-Mev electrons: Physical Review, v. 96, no. 5, p. 1344-1350, https://doi.org/10.1103/PhysRev.96.1344.","productDescription":"7 p.","startPage":"1344","endPage":"1350","numberOfPages":"7","costCenters":[],"links":[{"id":218752,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"96","issue":"5","noUsgsAuthors":false,"publicationDate":"1954-12-01","publicationStatus":"PW","scienceBaseUri":"505bb296e4b08c986b3258d5","contributors":{"authors":[{"text":"Miller, W.","contributorId":93184,"corporation":false,"usgs":true,"family":"Miller","given":"W.","affiliations":[],"preferred":false,"id":359733,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Motz, J. W.","contributorId":89278,"corporation":false,"usgs":true,"family":"Motz","given":"J.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":359732,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Cialella, C.","contributorId":68452,"corporation":false,"usgs":true,"family":"Cialella","given":"C.","email":"","affiliations":[],"preferred":false,"id":359731,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":1000160,"text":"1000160 - 1954 - Relationship of length of fish to incidence of sea lamprey scars on white suckers, Catostomus commersoni, in Lake Huron","interactions":[],"lastModifiedDate":"2016-02-15T11:13:16","indexId":"1000160","displayToPublicDate":"1954-01-01T00:00:00","publicationYear":"1954","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1337,"text":"Copeia","active":true,"publicationSubtype":{"id":10}},"title":"Relationship of length of fish to incidence of sea lamprey scars on white suckers, Catostomus commersoni, in Lake Huron","docAbstract":"<p>During the course of experimental fishing operations conducted by the staff of Hammond Bay Fishery Laboratory (a field station of Great Lakes Fishery Investigations) in 1950-1951, length measurements and records of scarring incidence and number of scars per individual were obtained for a sample of 552 white suckers, Catostomus commersoni (Lacepede). The results of this study indicate that if information on the incidence of sea lamprey scars on white suckers is to be used to judge the relative abundance of sea lampreys and the damages inflicted by that parasite on the sucker stock, data must include records of the lengths of fish. It is to be suspected strongly that a similar conclusion applies in other localities and to other species preyed upon by the sea lamprey.</p>","language":"English","publisher":"American Society of Ichthyologists and Herpetologists","doi":"10.2307/1440656","usgsCitation":"Hall, A., and Elliott, O.R., 1954, Relationship of length of fish to incidence of sea lamprey scars on white suckers, Catostomus commersoni, in Lake Huron: Copeia, v. 1954, no. 1, p. 73-74, https://doi.org/10.2307/1440656.","productDescription":"2 p.","startPage":"73","endPage":"74","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":133077,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"1954","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae0e4b07f02db687ec6","contributors":{"authors":[{"text":"Hall, A.E.","contributorId":42564,"corporation":false,"usgs":true,"family":"Hall","given":"A.E.","affiliations":[],"preferred":false,"id":308165,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Elliott, Oliver R.","contributorId":11549,"corporation":false,"usgs":true,"family":"Elliott","given":"Oliver","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":308164,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":71890,"text":"tei331 - 1953 - Search for and geology of radioactive deposits, semiannual progress report, classified data, December 1, 1952 to May 31, 1953","interactions":[],"lastModifiedDate":"2014-07-18T11:06:52","indexId":"tei331","displayToPublicDate":"2013-07-18T10:59:00","publicationYear":"1953","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":"331","title":"Search for and geology of radioactive deposits, semiannual progress report, classified data, December 1, 1952 to May 31, 1953","docAbstract":"No abstract available.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/tei331","collaboration":"Prepared by the U.S. Geological Survey for the U.S. Atomic Energy Commission.","usgsCitation":"NA, 1953, Search for and geology of radioactive deposits, semiannual progress report, classified data, December 1, 1952 to May 31, 1953: U.S. Geological Survey Trace Elements Investigations 331, 302 p., https://doi.org/10.3133/tei331.","productDescription":"302 p.","temporalStart":"1952-12-01","temporalEnd":"1953-05-31","costCenters":[],"links":[{"id":290448,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53cd71a2e4b0b29085107cd2","contributors":{"authors":[{"text":"NA","contributorId":127933,"corporation":true,"usgs":false,"organization":"NA","id":534729,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70047578,"text":"70047578 - 1953 - The measurement of total sediment load in alluvial streams","interactions":[{"subject":{"id":51094,"text":"ofr5214 - 1952 - The measurement of total sediment load in alluvial streams","indexId":"ofr5214","publicationYear":"1952","noYear":false,"title":"The measurement of total sediment load in alluvial streams"},"predicate":"SUPERSEDED_BY","object":{"id":70047578,"text":"70047578 - 1953 - The measurement of total sediment load in alluvial streams","indexId":"70047578","publicationYear":"1953","noYear":false,"title":"The measurement of total sediment load in alluvial streams"},"id":1}],"lastModifiedDate":"2017-03-09T12:18:59","indexId":"70047578","displayToPublicDate":"2013-01-01T14:31:00","publicationYear":"1953","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"The measurement of total sediment load in alluvial streams","docAbstract":"The measurement of the total sediment load transported by streams that flow in alluvial channels has been a perplexing problem to engineers and geologists for over a century. Until the last decade the development of equipment to measure bed load and suspended load was carried on almost independently, and without primary consideration of the fundamental laws governing the transportation of fluvial sediments. French investigators during the nineteenth century described methods of measurement and a mathematical approach for computing the rate of bed-load movement. The comprehensive laboratory investigations by Gilbert early in this century provided data that are still being used for studies of sediment transport. Detailed laboratory investigations of bed-load movement conducted during the last two decades by a number of investigators have resulted in the development of additional mathematical formulas for computing rates of bed-load movement. Likewise, studies of turbulent flow have provided the turbulence suspension theory for suspended sediment as it is known today.","largerWorkType":{"id":24,"text":"Conference Paper"},"largerWorkTitle":"Proceedings of the fifth Hydraulics Conference, June 9-11, 1952, arranged by the Iowa Institute of Hydraulic Research","largerWorkSubtype":{"id":19,"text":"Conference Paper"},"conferenceTitle":"Proceedings of the fifth Hydraulics Conference","conferenceDate":"June 9-11, 1952","conferenceLocation":"Iowa City, IA","language":"English","publisher":"State University of Iowa","publisherLocation":"Iowa City, Iowa","usgsCitation":"Benedict, P., and Matejka, D., 1953, The measurement of total sediment load in alluvial streams, <i>in</i> Proceedings of the fifth Hydraulics Conference, June 9-11, 1952, arranged by the Iowa Institute of Hydraulic Research, Iowa City, IA, June 9-11, 1952, p. 263-286.","productDescription":"24 p.","startPage":"263","endPage":"286","costCenters":[],"links":[{"id":276544,"type":{"id":15,"text":"Index Page"},"url":"https://ir.uiowa.edu/uisie/34/","text":"Conference Proceedings"},{"id":276545,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"publicComments":"University of Iowa Studies in Engineering, 34","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"520a0402e4b0026c2bc11d05","contributors":{"editors":[{"text":"McNown, John S.","contributorId":112479,"corporation":false,"usgs":true,"family":"McNown","given":"John","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":509565,"contributorType":{"id":2,"text":"Editors"},"rank":1},{"text":"Boyer, M.C.","contributorId":49038,"corporation":false,"usgs":true,"family":"Boyer","given":"M.C.","email":"","affiliations":[],"preferred":false,"id":509564,"contributorType":{"id":2,"text":"Editors"},"rank":2}],"authors":[{"text":"Benedict, P.C.","contributorId":45697,"corporation":false,"usgs":true,"family":"Benedict","given":"P.C.","email":"","affiliations":[],"preferred":false,"id":482443,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Matejka, D.Q.","contributorId":102061,"corporation":false,"usgs":true,"family":"Matejka","given":"D.Q.","affiliations":[],"preferred":false,"id":482444,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":71381,"text":"tei335 - 1953 - Montroseite, a new vanadium oxide from the Colorado plateaus","interactions":[],"lastModifiedDate":"2014-06-06T11:50:48","indexId":"tei335","displayToPublicDate":"1994-01-01T07:00:00","publicationYear":"1953","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":"335","title":"Montroseite, a new vanadium oxide from the Colorado plateaus","docAbstract":"<p>Montroseite, a new vanadium mineral named from Montrose County, Colorado, has been found in four mines in western Colorado and in two mines in eastern Utah. It is black, opaque, submetallic, and occurs in microscopic bladed crystals of the orthorhombic dipyramidal class. The axial ratio is a:b:c = 0.509:1:0.310, the common forms are b {010}, m {110}, p {121}, and a large vicinal form is approximately {0, 10, 1}. The observed specific gravity is 4.0 and the calculated specific gravity is 4.15. The composition is essentially VO(OH), with some iron commonly substituted for vanadium. Partial oxidation to VO<sub>2</sub> has taken place. Chemical analyses and X-ray diffraction data are given. Single crystal study indicated that the space group symmetry is Pbnm(D<sub>2h</sub><sup>16</sup>).</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/tei335","collaboration":"This report concerns work done on behalf of the Division of Raw Materials of the U.S. Atomic Energy Commission","usgsCitation":"Weeks, A., Cisney, E.A., and Sherwood, A.M., 1953, Montroseite, a new vanadium oxide from the Colorado plateaus: U.S. Geological Survey Trace Elements Investigations 335, 14 p., https://doi.org/10.3133/tei335.","productDescription":"14 p.","numberOfPages":"15","costCenters":[],"links":[{"id":193119,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/tei/335/report-thumb.jpg"},{"id":285646,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/tei/0335/report.pdf"}],"country":"United States","state":"Colorado;Utah","otherGeospatial":"Colorado Plateaus","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -111.4058,37.5597 ], [ -111.4058,39.3507 ], [ -107.4989,39.3507 ], [ -107.4989,37.5597 ], [ -111.4058,37.5597 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b03e4b07f02db698ed5","contributors":{"authors":[{"text":"Weeks, Alice D.","contributorId":92730,"corporation":false,"usgs":true,"family":"Weeks","given":"Alice D.","affiliations":[],"preferred":false,"id":284083,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Cisney, Evelyn A.","contributorId":70853,"corporation":false,"usgs":true,"family":"Cisney","given":"Evelyn","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":284082,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Sherwood, Alexander M.","contributorId":70061,"corporation":false,"usgs":true,"family":"Sherwood","given":"Alexander","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":284081,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":51222,"text":"ofr5333 - 1953 - Geology and geologic interpretation of seismic data--Revere Beach Parkway: Boston and Maine Railroad Crossing, Medford; Malden River, Medford-Everett; and Boston and Maine Railroad (Saugus Branch), Everett, Massachusetts","interactions":[],"lastModifiedDate":"2012-02-02T00:11:13","indexId":"ofr5333","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1953","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":"53-33","title":"Geology and geologic interpretation of seismic data--Revere Beach Parkway: Boston and Maine Railroad Crossing, Medford; Malden River, Medford-Everett; and Boston and Maine Railroad (Saugus Branch), Everett, Massachusetts","language":"ENGLISH","doi":"10.3133/ofr5333","usgsCitation":"Castle, R.O., and Linehan, D., 1953, Geology and geologic interpretation of seismic data--Revere Beach Parkway: Boston and Maine Railroad Crossing, Medford; Malden River, Medford-Everett; and Boston and Maine Railroad (Saugus Branch), Everett, Massachusetts: U.S. Geological Survey Open-File Report 53-33, 4 p., 6 plates, https://doi.org/10.3133/ofr5333.","productDescription":"4 p., 6 plates","costCenters":[],"links":[{"id":176815,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adbe4b07f02db6860aa","contributors":{"authors":[{"text":"Castle, R. O.","contributorId":79880,"corporation":false,"usgs":true,"family":"Castle","given":"R.","email":"","middleInitial":"O.","affiliations":[],"preferred":false,"id":243182,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Linehan, Daniel","contributorId":36998,"corporation":false,"usgs":true,"family":"Linehan","given":"Daniel","email":"","affiliations":[],"preferred":false,"id":243181,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":51344,"text":"ofr53183 - 1953 - Geology and geologic interpretation of seismic data for relocation of Route 20, cut, stations 116-120, westbound highway in Stockbridge, Massachusetts","interactions":[],"lastModifiedDate":"2012-02-02T00:11:14","indexId":"ofr53183","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1953","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":"53-183","title":"Geology and geologic interpretation of seismic data for relocation of Route 20, cut, stations 116-120, westbound highway in Stockbridge, Massachusetts","language":"ENGLISH","doi":"10.3133/ofr53183","usgsCitation":"Maynard, J., and Hazelwood, R., 1953, Geology and geologic interpretation of seismic data for relocation of Route 20, cut, stations 116-120, westbound highway in Stockbridge, Massachusetts: U.S. Geological Survey Open-File Report 53-183, 2 p., 1 plate, https://doi.org/10.3133/ofr53183.","productDescription":"2 p., 1 plate","costCenters":[],"links":[{"id":175369,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adbe4b07f02db686117","contributors":{"authors":[{"text":"Maynard, J.E.","contributorId":26005,"corporation":false,"usgs":true,"family":"Maynard","given":"J.E.","email":"","affiliations":[],"preferred":false,"id":243364,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hazelwood, R.M.","contributorId":41883,"corporation":false,"usgs":true,"family":"Hazelwood","given":"R.M.","email":"","affiliations":[],"preferred":false,"id":243365,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":51337,"text":"ofr53176 - 1953 - Geology and geologic interpretation of seismic data, relocation of Route 3 in Billerica, Massachusetts, cut, stations 363-383","interactions":[],"lastModifiedDate":"2012-02-02T00:11:14","indexId":"ofr53176","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1953","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":"53-176","title":"Geology and geologic interpretation of seismic data, relocation of Route 3 in Billerica, Massachusetts, cut, stations 363-383","language":"ENGLISH","doi":"10.3133/ofr53176","usgsCitation":"May, J.E., and Hazelwood, R., 1953, Geology and geologic interpretation of seismic data, relocation of Route 3 in Billerica, Massachusetts, cut, stations 363-383: U.S. Geological Survey Open-File Report 53-176, 2 p., 3 plates, https://doi.org/10.3133/ofr53176.","productDescription":"2 p., 3 plates","costCenters":[],"links":[{"id":176944,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adbe4b07f02db68610e","contributors":{"authors":[{"text":"May, James E.","contributorId":85255,"corporation":false,"usgs":true,"family":"May","given":"James","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":243351,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hazelwood, R.M.","contributorId":41883,"corporation":false,"usgs":true,"family":"Hazelwood","given":"R.M.","email":"","affiliations":[],"preferred":false,"id":243350,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":51338,"text":"ofr53177 - 1953 - Geology and geologic interpretation of seismic data, relocation of Route 3, station 496, in Billerica, to station 6, in Chelmsford, Massachusetts","interactions":[],"lastModifiedDate":"2012-02-02T00:11:14","indexId":"ofr53177","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1953","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":"53-177","title":"Geology and geologic interpretation of seismic data, relocation of Route 3, station 496, in Billerica, to station 6, in Chelmsford, Massachusetts","language":"ENGLISH","doi":"10.3133/ofr53177","usgsCitation":"Maynard, J., and Hazelwood, R., 1953, Geology and geologic interpretation of seismic data, relocation of Route 3, station 496, in Billerica, to station 6, in Chelmsford, Massachusetts: U.S. Geological Survey Open-File Report 53-177, 2 p., 3 plates, https://doi.org/10.3133/ofr53177.","productDescription":"2 p., 3 plates","costCenters":[],"links":[{"id":176945,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adbe4b07f02db6860dd","contributors":{"authors":[{"text":"Maynard, J.E.","contributorId":26005,"corporation":false,"usgs":true,"family":"Maynard","given":"J.E.","email":"","affiliations":[],"preferred":false,"id":243352,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hazelwood, R.M.","contributorId":41883,"corporation":false,"usgs":true,"family":"Hazelwood","given":"R.M.","email":"","affiliations":[],"preferred":false,"id":243353,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":51348,"text":"ofr53187 - 1953 - Geology and geologic interpretation of seismic data for relocation of Route 20 in Lee, Massachusetts, proposed cut stations 186-204","interactions":[],"lastModifiedDate":"2012-02-02T00:11:33","indexId":"ofr53187","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1953","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":"53-187","title":"Geology and geologic interpretation of seismic data for relocation of Route 20 in Lee, Massachusetts, proposed cut stations 186-204","language":"ENGLISH","doi":"10.3133/ofr53187","usgsCitation":"Maynard, J., and Linehan, D., 1953, Geology and geologic interpretation of seismic data for relocation of Route 20 in Lee, Massachusetts, proposed cut stations 186-204: U.S. Geological Survey Open-File Report 53-187, 2 p., 3 plates, https://doi.org/10.3133/ofr53187.","productDescription":"2 p., 3 plates","costCenters":[],"links":[{"id":177083,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adbe4b07f02db686112","contributors":{"authors":[{"text":"Maynard, J.E.","contributorId":26005,"corporation":false,"usgs":true,"family":"Maynard","given":"J.E.","email":"","affiliations":[],"preferred":false,"id":243372,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Linehan, Daniel","contributorId":36998,"corporation":false,"usgs":true,"family":"Linehan","given":"Daniel","email":"","affiliations":[],"preferred":false,"id":243373,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":12778,"text":"ofr5326 - 1953 - Geology of the Plumtree area, Spruce Pine district, North Carolina","interactions":[],"lastModifiedDate":"2012-02-02T00:06:33","indexId":"ofr5326","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1953","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":"53-26","title":"Geology of the Plumtree area, Spruce Pine district, North Carolina","docAbstract":"This report describes the results of study and geologic mapping (1:12,000) in the 70-square-mile Plumtree area in the northeastern part of the Spruce Pine pegmatite district, on the Blue Ridge upland in western North Carolina. The district has been the chief domestic source of feldspar and sheet mica. The mining belt just west of the Blue Ridge Front trends northeast and is 25 miles long and 10 miles wide. The center of the Plumtree area lies 10 miles northeast of Spruce Pine pegmatite district, on the Blue Ridge upland in western North Carolina. The district has been the chief domestic source of feldspar and sheet mica. The mining belt just west of the Blue Ridge Front trends northeast and is 25 miles long and 10 miles wide. The center of the Plumtree area lies 10 miles northeast of Spruce Pine and includes parts of Mitchell and Avery Counties shown on the portions of the 7.5-minute Spruce Pine, Linville Falls, Newland, North Carolina, and Carvers Gap, North Carolina and Tennessee quadrangle.\r\n\r\nThe topography varies from rugged mountains to rounded or flat topped hills near the entrenched, meandering master streams. Old erosion surfaces are approximately 600,1,100, 1,500, and 2,500 feet above the present master stream level. The area is in late youth or early maturity after rejuvenation..\r\n\r\nThe regionally metamorphosed rocks of the amophibolite facies form three mappable units: mica gneiss, mica schist, and hornblende rock. These rocks, perhaps of Precambrian age, are intimately interlayered with thicknesses of the individual layers ranging from less than one inch to several tons of feet. Field relationships and chemical data suggest that the mica (Carolina-type) rocks were derived from sandstones, graywackes, and shales and that the hornblende-rich (Roan-type) layers were derived from impure carbonate rocks.\r\n\r\nThe igneous rocks include alaskite and associated pegmatite of early Paleozoic age (?), dunite and associated soapstone of a prepegmatite age, and a few diabasic dikes of post-pegmatite age (Triassic?).\r\n\r\nThe alaskite and pegmatite have similar bulk compositions, notably low in iron (0.3 percent). The major constituents in order of decreasing abundance are plagioclase, perthitic microcline, quartz, and muncovite. All of these minerals, as well as clay deposits derived from the weathering of alaskite under old terraces, have economic value. The zoned pegmatites contain fewer zones which are less complex mineralogically than those in the pegmatites of many other areas. These essentially unmetamorphosed bodies were intruded approximately at the peak of the regional metamorphism. Their emplacement was controlled by local structure and rock type. The source of this igneous material may have been the mobilized portions of the Cranberry gneiss which underlies the area.\r\n\r\nThe dunite bodies were intruded early in the metamorphic cycle. The bodies are commonly zoned: from the wall rock inwards (1) talc-antrophyllite-serpentine fringe, (3) serpentinized dunite, (3) granular olivine core. Dunite, chromite, vermiculite, and anthophyllite are the major economic commodities. Extensive hydrothermal alteration of dunite bodies produced soapstone.\r\n\r\nThe area is the northeast end of a southwest plunging synclinorium about 20 miles wide with the steeper limb on the northwest side. There are three structural zones: zone I on the northwest is characterized by the northeast-trending isoclinal folds with steep southeast dips; zone II on the southwest includes an area of rocks with low and variable dip; zone III is the complex central core. In the extreme northeast zones I and II have an indistinct boundary where they coalesce along the rim of the synclinorium. Six stratigraphic units are exposed totaling approximately 10,500 feet of metamorphic rocks.\r\n\r\nSmall scale structural features include a foliation, and a lineation in the planes of the foliation. Minor folding reflects the trends of the major structures. There are randomly orient","language":"ENGLISH","publisher":"U.S. Geological Survey],","doi":"10.3133/ofr5326","usgsCitation":"Brobst, D.A., 1953, Geology of the Plumtree area, Spruce Pine district, North Carolina: U.S. Geological Survey Open-File Report 53-26, 115 p, https://doi.org/10.3133/ofr5326.","productDescription":"115 p","costCenters":[],"links":[{"id":145017,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1953/0026/report-thumb.jpg"},{"id":41175,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1953/0026/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":41176,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1953/0026/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4acce4b07f02db67e853","contributors":{"authors":[{"text":"Brobst, Donald Albert","contributorId":36117,"corporation":false,"usgs":true,"family":"Brobst","given":"Donald","email":"","middleInitial":"Albert","affiliations":[],"preferred":false,"id":166691,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":50,"text":"wsp1137F - 1953 - Floods of November-December 1950 in the Central Valley basin, California","interactions":[],"lastModifiedDate":"2023-01-12T21:56:03.437077","indexId":"wsp1137F","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1953","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":"1137","chapter":"F","title":"Floods of November-December 1950 in the Central Valley basin, California","docAbstract":"The flood of November-December 1950 in the Central Valley basin was the greatest in most parts of the basin since the turn of the century and probably was exceeded in the lower San Joaquin River basin only by the historic flood of 1862. In respect to monetary loss, the 1950 flood was the most disastrous in the history of the basin. Loss of life was remarkably small when one considers the extensive damage and destruction to homes and other property, which is estimated at 33 million dollars. Outstanding features of the flood were its unprecedented occurrence so early in the winter flood season, its magnitude in respect to both peak and volume in most major tributaries, and the occurrence of a succession of near-peak flows with a period of three weeks. \r\n\r\nThe flood was caused by a series of storms during the period November 16 to December 8, which brought exceptionally warm, moisture-laden air inland against the Sierra Nevada range and caused intense rainfall, instead of snowfall, at unusually high altitudes. Basin-wide totals of rainfall during the period ranged from 30 inches over the Yuba and American River basins to 13 inches over the upper Sacramento and Feather River basins. \r\n\r\nBased on continuous records of discharge on major tributaries for periods ranging from 22 to 55 years and averaging about 43 years, the 1950 flood peaks were the greatest of record on the American, Cosumnes, Mokelumne, Stanislaus, Tuolumne, Merced, Chowchilla, Fresno, lower San Joaquin, Kings, Kaweah, Tule, and Kern Rivers. Second highest peak of record occurred during the flood of March 1928 on the Yuba, American and Mokelumne Rivers; the flood of Marcn 1940 on Cosumnes River; the flood of January 1911 on the Stanislaus and Tuolumne Rivers; the flood of December 1937 on the Merced, Kings, and Kaweah Rivers; the flood of March 1938 on the Chowchilla, Fresno, and lower San Joaquin Rivers; and the flood of March 1943 on the Tule and Kern Rivers. Peak discharges for 1950 did not exceed previous maxima on Bear, Yuba, Feather, and upper Sacramento Rivers, nor on west side tributaries of lower Sacramento River, Calaveras River, and upper San Joaquin River (above Friant Reservoir). \r\n\r\nNotable high rates of discharge were 354 cfs per square mile from 39.5 square miles in North Fork of Middle Fork Tule River, 225 cfs per square mile from 198 square miles in Rubicon River, 115 cfs per square mile from 999 square miles in North Fork of American River and 93.7 cfs per square mile from 1,921 square miles in American River at Fair Oaks. \r\n\r\nThis report presents a general description of the 1950 flood, details and estimates of the damage incurred, records of stage and discharge for the period of the flood at 171 stream-gaging stations, records of storage in 14 reservoirs, a summary of peak discharges with comparative data for previous floods at 252 measurement points, and tables showing crest stages along the main stem and major tributary channels of the Sacramento and San Joaquin Rivers. \r\n\r\nThe report also includes a discussion of meteorologic and hydrologic conditions associated with the flood, examples of the flood regulation afforded by storage reservoirs, a brief study of runoff characteristics, and a summary and comparison with previous floods in the Central Valley basin.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wsp1137F","usgsCitation":"Paulsen, C.G., 1953, Floods of November-December 1950 in the Central Valley basin, California: U.S. Geological Survey Water Supply Paper 1137, Report: ix, 85 p.; 6 Plate: 29.00 x 35.50 inches or smaller, https://doi.org/10.3133/wsp1137F.","productDescription":"Report: ix, 85 p.; 6 Plate: 29.00 x 35.50 inches or smaller","costCenters":[],"links":[{"id":411810,"rank":9,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_24230.htm","linkFileType":{"id":5,"text":"html"}},{"id":24687,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1137f/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":24686,"rank":8,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1137f/plate-6.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":24685,"rank":7,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1137f/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":24684,"rank":6,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1137f/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":24683,"rank":5,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1137f/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":24682,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1137f/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":24681,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1137f/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":137395,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1137f/report-thumb.jpg"}],"country":"United States","state":"California","otherGeospatial":"Central Valley basin","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -119.00217681950107,\n              35.13952919516764\n            ],\n            [\n              -118.44677630187559,\n              36.447316753430925\n            ],\n            [\n              -120.27199477688288,\n              38.169213736701124\n            ],\n            [\n              -121.83334007970987,\n              40.062197180496526\n            ],\n            [\n              -121.87363587923997,\n              40.74570155104911\n            ],\n            [\n              -122.73875148861515,\n              40.49630948575876\n            ],\n            [\n              -122.72263734102694,\n              39.539602288586565\n            ],\n            [\n              -121.46737875338653,\n              37.74605097908976\n            ],\n            [\n              -120.18232868135271,\n              36.10951673244216\n            ],\n            [\n              -119.33641582011342,\n              35.142729172215766\n            ],\n            [\n              -119.00217681950107,\n              35.13952919516764\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49d8e4b07f02db5df882","contributors":{"authors":[{"text":"Paulsen, C. G.","contributorId":96239,"corporation":false,"usgs":true,"family":"Paulsen","given":"C.","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":141874,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":48,"text":"wsp1137D - 1953 - Floods of May-July 1950 in southeastern Nebraska","interactions":[],"lastModifiedDate":"2012-02-02T00:05:11","indexId":"wsp1137D","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1953","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":"1137","chapter":"D","title":"Floods of May-July 1950 in southeastern Nebraska","docAbstract":"Four floods occurred in southeast Nebraska during the period of May to July 1950. Two of these were the greatest known in the State if the size of the drainage areas is considered, and the other two were not so spectacular but were of notable size and of possible hydrologic significance in their relation to the two major floods. Although property loss and damage have been exceeded in previous floods in Nebraska, notably in the flood of May-June 1935 on the Republican River, they were extremely high in the period covered by this report. Loss of life, which resulted largely from the rapid cresting of the streams, was likewise high. \r\n\r\nEach of the floods was caused by heavy precipitation, which at times reached intensities seldom recorded in the Missouri River basin. On May 8, 1950, more than 14 inches of rain fell over certain areas of the Little Nemaha River basin within a period of a few hours. One center of the storm of July 8, 1950,occurred at York, Nebr., where 11 inches of rain was recorded within a 4-hour period, and the storm total exceeded 13 inches. \r\n\r\nNotable high rates of discharge produced by the intense rainfall were 1,030 cfs per square mile from 218 square miles of drainage area in the Little Nemaha River basin on May 9, 1950; 1,020 cfs per square mile from 2.5 square miles drainage area in the Elkhorn River basin on June 2, 1950; and 3,320 cfs per square mile from 6.93 square miles of drainage area in the Big Blue River basin on July 9, 1950. \r\n\r\nThis report presents records of stage and discharge for the flood. periods at 36 stream-gaging stations in southeast Nebraska, and a summary of peak discharges, with comparative data for previously known floods at 45 measurement points. The report also includes a discussion of the weather associated with the floods and other data pertinent to the floods.","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/wsp1137D","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1953, Floods of May-July 1950 in southeastern Nebraska: U.S. Geological Survey Water Supply Paper 1137, 351-411 p. :ill., maps ;23 cm., https://doi.org/10.3133/wsp1137D.","productDescription":"351-411 p. :ill., maps ;23 cm.","costCenters":[],"links":[{"id":137531,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1137d/report-thumb.jpg"},{"id":24677,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1137d/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49d9e4b07f02db5df949","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":527160,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":12907,"text":"ofr5332 - 1953 - Drilling data in Livingston-Cobb-Linden area in the Wisconsin zinc-lead district","interactions":[],"lastModifiedDate":"2012-02-02T00:06:48","indexId":"ofr5332","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1953","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":"53-32","title":"Drilling data in Livingston-Cobb-Linden area in the Wisconsin zinc-lead district","language":"ENGLISH","publisher":"U.S. Geological Survey],","doi":"10.3133/ofr5332","usgsCitation":"Carlson, J.E., 1953, Drilling data in Livingston-Cobb-Linden area in the Wisconsin zinc-lead district: U.S. Geological Survey Open-File Report 53-32, 30 p, https://doi.org/10.3133/ofr5332.","productDescription":"30 p","numberOfPages":"30","costCenters":[],"links":[{"id":146189,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a60e4b07f02db635587","contributors":{"authors":[{"text":"Carlson, John Edward","contributorId":49803,"corporation":false,"usgs":true,"family":"Carlson","given":"John","email":"","middleInitial":"Edward","affiliations":[],"preferred":false,"id":166935,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":51333,"text":"ofr53172 - 1953 - Geology and geologic interpretations of seismic data, relocation of Route 3, stations 228-234, in Billerica, Massachusetts","interactions":[],"lastModifiedDate":"2012-02-02T00:11:14","indexId":"ofr53172","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1953","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":"53-172","title":"Geology and geologic interpretations of seismic data, relocation of Route 3, stations 228-234, in Billerica, Massachusetts","language":"ENGLISH","doi":"10.3133/ofr53172","usgsCitation":"May, J.E., and Hazelwood, R., 1953, Geology and geologic interpretations of seismic data, relocation of Route 3, stations 228-234, in Billerica, Massachusetts: U.S. Geological Survey Open-File Report 53-172, 2 p., 1 plate, https://doi.org/10.3133/ofr53172.","productDescription":"2 p., 1 plate","costCenters":[],"links":[{"id":176332,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adbe4b07f02db6860c2","contributors":{"authors":[{"text":"May, James E.","contributorId":85255,"corporation":false,"usgs":true,"family":"May","given":"James","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":243343,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hazelwood, R.M.","contributorId":41883,"corporation":false,"usgs":true,"family":"Hazelwood","given":"R.M.","email":"","affiliations":[],"preferred":false,"id":243342,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":51334,"text":"ofr53173 - 1953 - Geology and geologic interpretation of seismic data, relocation of Route 3, cut, stations 249-260, in Billerica, Massachusetts","interactions":[],"lastModifiedDate":"2012-02-02T00:11:15","indexId":"ofr53173","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1953","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":"53-173","title":"Geology and geologic interpretation of seismic data, relocation of Route 3, cut, stations 249-260, in Billerica, Massachusetts","language":"ENGLISH","doi":"10.3133/ofr53173","usgsCitation":"May, J.E., and Hazelwood, R., 1953, Geology and geologic interpretation of seismic data, relocation of Route 3, cut, stations 249-260, in Billerica, Massachusetts: U.S. Geological Survey Open-File Report 53-173, 2 p., 2 plates, https://doi.org/10.3133/ofr53173.","productDescription":"2 p., 2 plates","costCenters":[],"links":[{"id":175920,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adbe4b07f02db6860cc","contributors":{"authors":[{"text":"May, James E.","contributorId":85255,"corporation":false,"usgs":true,"family":"May","given":"James","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":243345,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hazelwood, R.M.","contributorId":41883,"corporation":false,"usgs":true,"family":"Hazelwood","given":"R.M.","email":"","affiliations":[],"preferred":false,"id":243344,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":14260,"text":"ofr53135 - 1953 - Correlation of the Cretaceous formations of Greenland and Alaska","interactions":[{"subject":{"id":14260,"text":"ofr53135 - 1953 - Correlation of the Cretaceous formations of Greenland and Alaska","indexId":"ofr53135","publicationYear":"1953","noYear":false,"title":"Correlation of the Cretaceous formations of Greenland and Alaska"},"predicate":"SUPERSEDED_BY","object":{"id":70042910,"text":"70042910 - 1954 - Correlation of the cretaceous formations of Greenland and Alaska","indexId":"70042910","publicationYear":"1954","noYear":false,"title":"Correlation of the cretaceous formations of Greenland and Alaska"},"id":1}],"supersededBy":{"id":70042910,"text":"70042910 - 1954 - Correlation of the cretaceous formations of Greenland and Alaska","indexId":"70042910","publicationYear":"1954","noYear":false,"title":"Correlation of the cretaceous formations of Greenland and Alaska"},"lastModifiedDate":"2023-07-14T19:14:02.39316","indexId":"ofr53135","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1953","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":"53-135","title":"Correlation of the Cretaceous formations of Greenland and Alaska","docAbstract":"This is  Number 10d of a series of correlation charts prepared for the Committee on Stratigraphy of the National Research Council. It has been sponsored by the U.S. Geological Survey and has required about seven months' time of both authors gathering and compiling data and evaluating fossil evidence. As the two regions dealt with in the chart are widely separated, the lists of references are also given separately. The annotations dealing with Greenland are based entirely on published information. The annotations dealing with Alaska are based on a re-examination of nearly all the Cretaceous fossils from Alaska are based on a re-examination of nearly all the Cretaceous fossils from Alaska in the collections of the Geological Survey. This has resulted in many concepts not hitherto published and in some concepts that are completely at variance with those that have been published. Naturally for large areas undergoing active exploration, such as Alaska, a correlation chart is out of date in many particulars as soon as published. Nevertheless it is valuable to the field man whose activities are confined to small areas but who must interpret much of his data in terms of surrounding areas that he has not seen. It is valuable to the student and to the general geologist because it organizes scattered information in a manner that can be applied in their field problems, makes quite unnecessary the memorization of stratigraphic correlations are based on observation and reasoning and not on a vast memory. It is probably of greatest value to the specialist who makes the chart because he discovers what areas and problems are most in need of research and can thereby direct his efforts and those of his associates in a manner that will yield the greatest results.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr53135","usgsCitation":"Imlay, R.W., and Reeside, J.B., 1953, Correlation of the Cretaceous formations of Greenland and Alaska: U.S. Geological Survey Open-File Report 53-135, Report: 41 p.; 1 Plate: 93.78 x 31.01 inches, https://doi.org/10.3133/ofr53135.","productDescription":"Report: 41 p.; 1 Plate: 93.78 x 31.01 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Ralph Willard","contributorId":19155,"corporation":false,"usgs":true,"family":"Imlay","given":"Ralph","email":"","middleInitial":"Willard","affiliations":[],"preferred":false,"id":169164,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Reeside, John B. Jr.","contributorId":98299,"corporation":false,"usgs":true,"family":"Reeside","given":"John","suffix":"Jr.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":169165,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":51232,"text":"ofr5349 - 1953 - Data on ground-water pumpage and water levels, Memphis, Tennessee, 1953","interactions":[],"lastModifiedDate":"2012-02-02T00:11:13","indexId":"ofr5349","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1953","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":"53-49","title":"Data on ground-water pumpage and water levels, Memphis, Tennessee, 1953","language":"ENGLISH","doi":"10.3133/ofr5349","usgsCitation":"Cushing, E.M., 1953, Data on ground-water pumpage and water levels, Memphis, Tennessee, 1953: U.S. Geological Survey Open-File Report 53-49, 18 p., https://doi.org/10.3133/ofr5349.","productDescription":"18 p.","costCenters":[],"links":[{"id":176934,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67c84d","contributors":{"authors":[{"text":"Cushing, E. M.","contributorId":94273,"corporation":false,"usgs":true,"family":"Cushing","given":"E.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":243193,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":12430,"text":"ofr533 - 1953 - Geologic map and recent drilling data of the Sinsinawa River area, Grant County, Wisconsin","interactions":[],"lastModifiedDate":"2012-02-02T00:06:33","indexId":"ofr533","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1953","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":"53-3","title":"Geologic map and recent drilling data of the Sinsinawa River area, Grant County, Wisconsin","language":"ENGLISH","publisher":"U.S. Geological Survey],","doi":"10.3133/ofr533","usgsCitation":"Allingham, J.W., Flint, A.E., and Agnew, A.F., 1953, Geologic map and recent drilling data of the Sinsinawa River area, Grant County, Wisconsin: U.S. Geological Survey Open-File Report 53-3, 21 p, https://doi.org/10.3133/ofr533.","productDescription":"21 p","numberOfPages":"21","costCenters":[],"links":[{"id":144876,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1953/0003/report-thumb.jpg"},{"id":40670,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1953/0003/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b15e4b07f02db6a492a","contributors":{"authors":[{"text":"Allingham, John Wing","contributorId":65466,"corporation":false,"usgs":true,"family":"Allingham","given":"John","email":"","middleInitial":"Wing","affiliations":[],"preferred":false,"id":166124,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Flint, Arthur Emerson","contributorId":48187,"corporation":false,"usgs":true,"family":"Flint","given":"Arthur","email":"","middleInitial":"Emerson","affiliations":[],"preferred":false,"id":166123,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Agnew, Allen Francis","contributorId":78727,"corporation":false,"usgs":true,"family":"Agnew","given":"Allen","email":"","middleInitial":"Francis","affiliations":[],"preferred":false,"id":166125,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":7529,"text":"ofr5336 - 1953 - Stratigraphic sections of the Phosphoria formation measured and sampled in 1952","interactions":[{"subject":{"id":7529,"text":"ofr5336 - 1953 - Stratigraphic sections of the Phosphoria formation measured and sampled in 1952","indexId":"ofr5336","publicationYear":"1953","noYear":false,"title":"Stratigraphic sections of the Phosphoria formation measured and sampled in 1952"},"predicate":"SUPERSEDED_BY","object":{"id":3450,"text":"cir325 - 1954 - Stratigraphic sections of the Phosphoria formation in Wyoming, 1952","indexId":"cir325","publicationYear":"1954","noYear":false,"title":"Stratigraphic sections of the Phosphoria formation in Wyoming, 1952"},"id":1}],"supersededBy":{"id":3450,"text":"cir325 - 1954 - Stratigraphic sections of the Phosphoria formation in Wyoming, 1952","indexId":"cir325","publicationYear":"1954","noYear":false,"title":"Stratigraphic sections of the Phosphoria formation in Wyoming, 1952"},"lastModifiedDate":"2025-05-30T16:51:33.704571","indexId":"ofr5336","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1953","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":"53-36","title":"Stratigraphic sections of the Phosphoria formation measured and sampled in 1952","docAbstract":"<p>A series of reports presenting detailed stratigraphic sections and analyses of samples of the Phosphoria formation in the western phosphate field is being prepared for publication as U. S. Geological Survey Circulars. To speed the availability of these data to industry and others having immediate need for such basic information, many of the tables already typed and photographed were reproduced without text and placed on open file in advance of publication. This includes six reports of data gathered during the 1947 and 1948 field seasons.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr5336","usgsCitation":"Cheney, T.M., Sheldon, R., Cressman, E.R., Smart, R., and Carswell, L., 1953, Stratigraphic sections of the Phosphoria formation measured and sampled in 1952 (Superceded by: Circular 325): U.S. Geological Survey Open-File Report 53-36, iii, 26 p., https://doi.org/10.3133/ofr5336.","productDescription":"iii, 26 p.","costCenters":[],"links":[{"id":139984,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1953/0036/report-thumb.jpg"},{"id":489305,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1953/0036/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"edition":"Superceded by: Circular 325","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b24e4b07f02db6ae514","contributors":{"authors":[{"text":"Cheney, Thomas McGiffin","contributorId":69006,"corporation":false,"usgs":true,"family":"Cheney","given":"Thomas","email":"","middleInitial":"McGiffin","affiliations":[],"preferred":false,"id":156019,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Sheldon, R.P.","contributorId":71158,"corporation":false,"usgs":true,"family":"Sheldon","given":"R.P.","email":"","affiliations":[],"preferred":false,"id":156020,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Cressman, E. R.","contributorId":83494,"corporation":false,"usgs":true,"family":"Cressman","given":"E.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":156021,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Smart, R.A.","contributorId":6039,"corporation":false,"usgs":true,"family":"Smart","given":"R.A.","email":"","affiliations":[],"preferred":false,"id":156017,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Carswell, L.D.","contributorId":6435,"corporation":false,"usgs":true,"family":"Carswell","given":"L.D.","email":"","affiliations":[],"preferred":false,"id":156018,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":51712,"text":"ofr54188 - 1953 - Ground-water data collected in the Missouri River basin units in Kansas during 1952","interactions":[],"lastModifiedDate":"2018-06-13T10:10:21","indexId":"ofr54188","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1953","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":"54-188","title":"Ground-water data collected in the Missouri River basin units in Kansas during 1952","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr54188","usgsCitation":"Mason, B., and Underwood, S., 1953, Ground-water data collected in the Missouri River basin units in Kansas during 1952: U.S. Geological Survey Open-File Report 54-188, 61 p., https://doi.org/10.3133/ofr54188.","productDescription":"61 p.","costCenters":[],"links":[{"id":176726,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"country":"United States","state":"Kansas","otherGeospatial":"Missouri River basin","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -102.030029296875,\n              38.44498466889473\n            ],\n            [\n              -97.415771484375,\n              38.44498466889473\n            ],\n            [\n              -97.415771484375,\n              40.002371935876475\n            ],\n            [\n              -102.030029296875,\n              40.002371935876475\n            ],\n            [\n              -102.030029296875,\n              38.44498466889473\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aafe4b07f02db66d00e","contributors":{"authors":[{"text":"Mason, B.J.","contributorId":53029,"corporation":false,"usgs":true,"family":"Mason","given":"B.J.","email":"","affiliations":[],"preferred":false,"id":244174,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Underwood, S.J.","contributorId":101734,"corporation":false,"usgs":true,"family":"Underwood","given":"S.J.","email":"","affiliations":[],"preferred":false,"id":244175,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":2692,"text":"wsp1220 - 1953 - Irrigation and streamflow depletion in Columbia River basin above The Dalles, Oregon","interactions":[],"lastModifiedDate":"2023-09-27T20:37:28.914126","indexId":"wsp1220","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1953","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":"1220","title":"Irrigation and streamflow depletion in Columbia River basin above The Dalles, Oregon","docAbstract":"The Columbia River is the largest stream in western United States. Above The Dalles, Oregon, it drains an area of 237,000 square miles, of which 39,000 square miles is in Canada. This area is largely mountainous and lies between the Rocky Mountains and the Cascade Range. The Kootenai, Pend Oreille, and Snake Rivers are the principal tributaries. Precipitation varies from 7 inches near Kennewick, Wash. to over 100 inches in some of the mountainous regions. Most of the runoff occurs in the spring and summer months as a result of melting snow. Precipitation is generally light during the summer months, and irrigation is necessary for sustained crop production. \r\n\r\nHistorical data indicate that irrigation in the Columbia River basin began prior to 1840 at the site of missions established near Walla Walla, Wash. and Lewiston, Idaho. During the next half century the increase in irrigated area was slow and by 1890 included only 506,000 acres. The period 1890 to 1910 was marked by phenomenal increase to a total of 2,276,000 acres in 1910. Since that time there has been more gradual addition to a total of 4,004,S00 acres of irrigated land in 1946 in the Columbia River basin above The Dalles, Oreg. Of this total 918,000 acres were located in the Columbia Basin above the mouth of the Snake River; 2,830,000 acres in the Snake River basin, and the balance, 256,000 acres below the mouth of the Snake River. \r\n\r\nValues of net consumptive use were determined or estimated for various tributary basins of the Columbia River basin and compared to available experimental data. These values were then used to compute the average depletion which could be directly attributed to irrigation. The yield of a drainage basin was considered to be the rum of the ob- served runoff and the estimated depletion. For purposes of comparison, the depletion was expressed both in terms of acre-feet and as a percentage of the yield of the basin. This percentage depletion varied from less than 1 percent for many tributary basins to 53 percent for the portion of the Snake River basin between Heise and King Hill, Idaho. For the Columbia River near The Dalles, Oreg., the average depletion during the period 1921 through 1945, amounted to 4,7 percent of the yield and the depletion represented by the 1946 stage of irrigation development amounted to 5.3 percent of the long-term yield.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wsp1220","usgsCitation":"Simons, W.D., 1953, Irrigation and streamflow depletion in Columbia River basin above The Dalles, Oregon: U.S. Geological Survey Water Supply Paper 1220, iv, 126 p., https://doi.org/10.3133/wsp1220.","productDescription":"iv, 126 p.","costCenters":[{"id":518,"text":"Oregon Water Science Center","active":true,"usgs":true}],"links":[{"id":138818,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1220/report-thumb.jpg"},{"id":421287,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_24239.htm","linkFileType":{"id":5,"text":"html"}},{"id":29049,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1220/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Oregon, Washington","otherGeospatial":"Columbia River basin","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -112,\n              49\n            ],\n            [\n              -121.25,\n              49\n            ],\n            [\n              -121.25,\n              42\n            ],\n            [\n              -112,\n              42\n            ],\n            [\n              -112,\n              49\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9fe4b07f02db6618fa","contributors":{"authors":[{"text":"Simons, Wilbur Douglas","contributorId":102469,"corporation":false,"usgs":true,"family":"Simons","given":"Wilbur","email":"","middleInitial":"Douglas","affiliations":[],"preferred":false,"id":145619,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":51339,"text":"ofr53178 - 1953 - Geology and geologic interpretation of seismic data, relocation of Route 7, cut, stations 274-277 in Great Barrington, Massachusetts","interactions":[],"lastModifiedDate":"2012-02-02T00:11:14","indexId":"ofr53178","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1953","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":"53-178","title":"Geology and geologic interpretation of seismic data, relocation of Route 7, cut, stations 274-277 in Great Barrington, Massachusetts","language":"ENGLISH","doi":"10.3133/ofr53178","usgsCitation":"Maynard, J., and Hazelwood, R., 1953, Geology and geologic interpretation of seismic data, relocation of Route 7, cut, stations 274-277 in Great Barrington, Massachusetts: U.S. Geological Survey Open-File Report 53-178, 2 p., 1 plate, https://doi.org/10.3133/ofr53178.","productDescription":"2 p., 1 plate","costCenters":[],"links":[{"id":176946,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adbe4b07f02db6860a3","contributors":{"authors":[{"text":"Maynard, J.E.","contributorId":26005,"corporation":false,"usgs":true,"family":"Maynard","given":"J.E.","email":"","affiliations":[],"preferred":false,"id":243354,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hazelwood, R.M.","contributorId":41883,"corporation":false,"usgs":true,"family":"Hazelwood","given":"R.M.","email":"","affiliations":[],"preferred":false,"id":243355,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
]}