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,{"id":14409,"text":"ofr6182 - 1961 - Preliminary interpretation of gravity data in west-central Maine","interactions":[{"subject":{"id":14409,"text":"ofr6182 - 1961 - Preliminary interpretation of gravity data in west-central Maine","indexId":"ofr6182","publicationYear":"1961","noYear":false,"title":"Preliminary interpretation of gravity data in west-central Maine"},"predicate":"SUPERSEDED_BY","object":{"id":70047761,"text":"70047761 - 1968 - Gravity anomalies in Maine","indexId":"70047761","publicationYear":"1968","noYear":false,"chapter":"31","title":"Gravity anomalies in Maine"},"id":1}],"supersededBy":{"id":70047761,"text":"70047761 - 1968 - Gravity anomalies in Maine","indexId":"70047761","publicationYear":"1968","noYear":false,"title":"Gravity anomalies in Maine"},"lastModifiedDate":"2013-08-22T10:42:58","indexId":"ofr6182","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1961","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":"61-82","title":"Preliminary interpretation of gravity data in west-central Maine","language":"ENGLISH","publisher":"U.S. Geological Survey],","doi":"10.3133/ofr6182","usgsCitation":"Kane, M.F., and Peterson, D.L., 1961, Preliminary interpretation of gravity data in west-central Maine: U.S. Geological Survey Open-File Report 61-82, 10 leaves :folded map ;27 cm., https://doi.org/10.3133/ofr6182.","productDescription":"10 leaves :folded map ;27 cm.","costCenters":[],"links":[{"id":147679,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4abce4b07f02db673238","contributors":{"authors":[{"text":"Kane, M. F.","contributorId":45708,"corporation":false,"usgs":true,"family":"Kane","given":"M.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":169407,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Peterson, D. L.","contributorId":36484,"corporation":false,"usgs":true,"family":"Peterson","given":"D.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":169406,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":61262,"text":"mf160 - 1961 - Reconnaissance geologic map of part of the southern Peloncillo Mountains, Hidalgo County, New Mexico","interactions":[],"lastModifiedDate":"2018-12-14T11:20:21","indexId":"mf160","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1961","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":325,"text":"Miscellaneous Field Studies Map","code":"MF","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"160","title":"Reconnaissance geologic map of part of the southern Peloncillo Mountains, Hidalgo County, New Mexico","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/mf160","usgsCitation":"Wrucke, C., and Bromfield, C.S., 1961, Reconnaissance geologic map of part of the southern Peloncillo Mountains, Hidalgo County, New Mexico: U.S. Geological Survey Miscellaneous Field Studies Map 160, 32.55 x 34.62 inches, https://doi.org/10.3133/mf160.","productDescription":"32.55 x 34.62 inches","costCenters":[],"links":[{"id":360311,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/0160/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":180644,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/mf/0160/report-thumb.jpg"}],"country":"United States","state":"New Mexico","county":"Hidalgo County","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -109,31.5 ], [ -109,31.75 ], [ -108.83333333333333,31.75 ], [ -108.83333333333333,31.5 ], [ -109,31.5 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a73e4b07f02db6437cb","contributors":{"authors":[{"text":"Wrucke, C. T.","contributorId":8067,"corporation":false,"usgs":true,"family":"Wrucke","given":"C. T.","affiliations":[],"preferred":false,"id":265278,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bromfield, C. S.","contributorId":97917,"corporation":false,"usgs":true,"family":"Bromfield","given":"C.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":265279,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":64055,"text":"gp252 - 1961 - Preliminary aeroradioactivity and geologic map of the Falls City SW quadrangle, Atascosa, Karnes, and Live Oak Counties, Texas","interactions":[],"lastModifiedDate":"2012-02-10T00:10:54","indexId":"gp252","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1961","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":"252","title":"Preliminary aeroradioactivity and geologic map of the Falls City SW quadrangle, Atascosa, Karnes, and Live Oak Counties, Texas","language":"ENGLISH","doi":"10.3133/gp252","usgsCitation":"Eargle, D., Brown, R., and Moxham, R., 1961, Preliminary aeroradioactivity and geologic map of the Falls City SW quadrangle, Atascosa, Karnes, and Live Oak Counties, Texas: U.S. Geological Survey Geophysical Investigations Map 252, 1 map :col. ;46 x 41 cm. folded to 30 x 24 cm., https://doi.org/10.3133/gp252.","productDescription":"1 map :col. ;46 x 41 cm. folded to 30 x 24 cm.","costCenters":[],"links":[{"id":104146,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_3176.htm","linkFileType":{"id":5,"text":"html"},"description":"3176"},{"id":187273,"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\": [ [ [ -98.25,28.75 ], [ -98.25,28.8675 ], [ -98.11749999999999,28.8675 ], [ -98.11749999999999,28.75 ], [ -98.25,28.75 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4acbe4b07f02db67e37c","contributors":{"authors":[{"text":"Eargle, Dolan","contributorId":106568,"corporation":false,"usgs":true,"family":"Eargle","given":"Dolan","affiliations":[],"preferred":false,"id":269839,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Brown, R.D.","contributorId":73221,"corporation":false,"usgs":true,"family":"Brown","given":"R.D.","affiliations":[],"preferred":false,"id":269838,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Moxham, Robert","contributorId":16501,"corporation":false,"usgs":true,"family":"Moxham","given":"Robert","affiliations":[],"preferred":false,"id":269837,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":64812,"text":"i332 - 1961 - Geologic map of a part of southwestern Wyoming and adjacent States","interactions":[],"lastModifiedDate":"2012-02-02T00:13:02","indexId":"i332","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1961","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":320,"text":"IMAP","code":"I","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"332","subseriesTitle":"NONE","title":"Geologic map of a part of southwestern Wyoming and adjacent States","language":"ENGLISH","doi":"10.3133/i332","usgsCitation":"Bradley, W.H., 1961, Geologic map of a part of southwestern Wyoming and adjacent States: U.S. Geological Survey IMAP 332, 1 map :col. ;86 x 131 cm. folded to 28 x 20 cm. in envelope 30 x 24 cm., https://doi.org/10.3133/i332.","productDescription":"1 map :col. ;86 x 131 cm. folded to 28 x 20 cm. in envelope 30 x 24 cm.","costCenters":[],"links":[{"id":102824,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_1290.htm","linkFileType":{"id":5,"text":"html"},"description":"1290"},{"id":187277,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":91442,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/0332/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"250000","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b12e4b07f02db6a2a5d","contributors":{"authors":[{"text":"Bradley, W. H.","contributorId":102452,"corporation":false,"usgs":true,"family":"Bradley","given":"W.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":272197,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":39145,"text":"pp282G - 1961 - Factors controlling the size and shape of stream channels in coarse noncohesive sands","interactions":[],"lastModifiedDate":"2016-11-07T10:40:00","indexId":"pp282G","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1961","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"282","chapter":"G","title":"Factors controlling the size and shape of stream channels in coarse noncohesive sands","docAbstract":"<p>The size and shape of equilibrium channels in uniform, noncohesive sands, 0.67 mm and 2.0 mm in diameter, were studied experimentally in a laboratory flume 52 feet long in which discharge, slope, sediment load, and bed and bank material could be varied independently. For each run a straight trapezoidal channel was molded in the sand and the flume set at a predetermined slope. Introduction of the discharge was accompanied by widening and aggradation until a stable channel was established. By definition a stable equilibrium existed when channel width, water surface slope, and rate of transport became constant. The duration of individual runs ranged from 2 to 52 hours depending upon the time required for establishing equilibrium. </p><p>Stability of the banks determined channel shape. In the 2.0 mm sand at a given slope and discharge, only one depth was stable. At this depth the flow was just competent to move particles along the bed of the channel. An increase in discharge produced a wider channel of the same depth and thus transport per unit width remained at a minimum. Channels in the 0.67 mm sand were somewhat more stable and permitted a 1.5 fold increase in depth above that required to start movement of the bed material. An increased transport was associated with the increase in depth. The rate of transport is adequately described in terms of the total shear or in terms of the difference between the total shear and the critical shear required to begin movement. </p><p>In these experiments the finer, or 0.67 mm, sand, began to move along the bed of the channel at a constant shear stress. Incipient movement of the coarser, or 2.0 mm, sand, varied with the shear stress as well as the mean velocity. At the initiation of movement a lower shear was associated with a higher velocity and vice versa. </p><p>Anabranches of braided rivers and some natural river channels formed in relatively noncohesive materials resemble the essential characteristics of the flume channels. For a given slope and size of bed material the discharge per unit width in the laboratory channels was similar to that computed for anabranches and river channels measured in the field. Unlike most natural channels, despite impressive bank erosion, the channels in the laboratory only meandered at supercritical flows associated with very steep slopes. These conditions involving shallow depths, high velocity, and steep slopes are uncommon in most natural rivers.</p>","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/pp282G","usgsCitation":"Wolman, M.G., and Brush, L.M., 1961, Factors controlling the size and shape of stream channels in coarse noncohesive sands: U.S. Geological Survey Professional Paper 282, 28 p., https://doi.org/10.3133/pp282G.","productDescription":"28 p.","startPage":"183","endPage":"210","costCenters":[],"links":[{"id":164915,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":330811,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0282g/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a03e4b07f02db5f840b","contributors":{"authors":[{"text":"Wolman, M. Gordon","contributorId":85163,"corporation":false,"usgs":true,"family":"Wolman","given":"M.","email":"","middleInitial":"Gordon","affiliations":[],"preferred":false,"id":221036,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Brush, Lucien M. Jr.","contributorId":107343,"corporation":false,"usgs":true,"family":"Brush","given":"Lucien","suffix":"Jr.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":221037,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":64054,"text":"gp253 - 1961 - Preliminary aeroradioactivity and geologic map of the Falls City SE quadrangle, Atascosa, Karnes, and Live Oak Counties, Texas","interactions":[],"lastModifiedDate":"2012-02-10T00:10:54","indexId":"gp253","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1961","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":"253","title":"Preliminary aeroradioactivity and geologic map of the Falls City SE quadrangle, Atascosa, Karnes, and Live Oak Counties, Texas","language":"ENGLISH","doi":"10.3133/gp253","usgsCitation":"Eargle, D.H., and Moxham, R.M., 1961, Preliminary aeroradioactivity and geologic map of the Falls City SE quadrangle, Atascosa, Karnes, and Live Oak Counties, Texas: U.S. Geological Survey Geophysical Investigations Map 253, 1 map ;46 x 40 cm. folded in envelope 30 x 24 cm., https://doi.org/10.3133/gp253.","productDescription":"1 map ;46 x 40 cm. folded in envelope 30 x 24 cm.","costCenters":[],"links":[{"id":104147,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_3177.htm","linkFileType":{"id":5,"text":"html"},"description":"3177"},{"id":187272,"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\": [ [ [ -98.11749999999999,28.75 ], [ -98.11749999999999,28.8675 ], [ -98,28.8675 ], [ -98,28.75 ], [ -98.11749999999999,28.75 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4acbe4b07f02db67e373","contributors":{"authors":[{"text":"Eargle, Dolan H.","contributorId":104514,"corporation":false,"usgs":true,"family":"Eargle","given":"Dolan","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":269836,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Moxham, Robert M.","contributorId":56210,"corporation":false,"usgs":true,"family":"Moxham","given":"Robert","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":269835,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
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,{"id":57721,"text":"ofr61177 - 1961 - Ground water in the alluvial deposits of the Canadian River valley near Norman, Oklahoma","interactions":[],"lastModifiedDate":"2012-02-02T00:12:12","indexId":"ofr61177","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1961","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":"61-177","title":"Ground water in the alluvial deposits of the Canadian River valley near Norman, Oklahoma","docAbstract":"Unconsolidated water-bearing alluvial deposits border the Canadian River in the vicinity of Norman, Oklahoma. These Quaternary materials are divided on the basis of topgraphic position into 'high terrace deposits' and 'alluvium.' The high terrace lies at an elevation of 50 to 60 feet above the alluvium, which in turn lies 7 to 15 feet above the channel of the Canadian River. Southwest of Norman a relatively thick section of these deposits occur as a hydrologic unit and overlie impermeable Permian shale. The high terrace deposits contain thick beds of clay, silt, and fine sand, whereas the alluvium contains a higher percentage of coarse sand and gravel.\r\nGround-water recharge is estimated to be 23 percent of the normal annual precipitation of 33.22 inches; the specific yield is about 15 percent, and the coefficient of permeability is about 1,000 gpd/ft2. Using these figures 17,000 acre-feet of water is computed to be in storage within the area acting as a hydrologic unit. About 3.6 million gallons of water is discharged daily from the high terrace deposits through a 16,000-foot section of alluvium having a saturated thickness of 40 feet along the river.\r\n\r\nThe quality of water in the high terrace deposits meets the standards of the U.S. Public Health Service for domestic water used by Interstate carriers but nitrate content of one well is higher than recommended by the Oklahoma Department of Public Health. Water in the alluvium is of poorer quality because the water is concentrated by evapotranspiration.\r\n\r\n(available as photostat copy only)","language":"ENGLISH","doi":"10.3133/ofr61177","usgsCitation":"Stacy, B.L., 1961, Ground water in the alluvial deposits of the Canadian River valley near Norman, Oklahoma: U.S. Geological Survey Open-File Report 61-177, 61 p., https://doi.org/10.3133/ofr61177.","productDescription":"61 p.","costCenters":[],"links":[{"id":184149,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ab0e4b07f02db66d7fe","contributors":{"authors":[{"text":"Stacy, Bill L.","contributorId":99637,"corporation":false,"usgs":true,"family":"Stacy","given":"Bill","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":257637,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
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