{"pageNumber":"1833","pageRowStart":"45800","pageSize":"25","recordCount":46614,"records":[{"id":856,"text":"856 - 1964 - Water resources data for Minnesota","interactions":[],"lastModifiedDate":"2014-08-05T12:40:50","indexId":"856","displayToPublicDate":"1964-01-01T12:39:39","publicationYear":"1964","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"title":"Water resources data for Minnesota","docAbstract":"No abstract available.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"St. Paul, MN","doi":"10.3133/856","issn":"0364-4383","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1964, Water resources data for Minnesota, https://doi.org/10.3133/856.","costCenters":[],"links":[{"id":291688,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"country":"United States","state":"Minnesota","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -97.24,43.5 ], [ -97.24,49.38 ], [ -89.49,49.38 ], [ -89.49,43.5 ], [ -97.24,43.5 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53e1efe8e4b0fe532be2def3","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":527775,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70263594,"text":"wdrCA642 - 1964 - Surface water records of California, 1964; Volume 2: Northern Great Basin and Central Valley","interactions":[],"lastModifiedDate":"2025-02-14T15:32:39.182988","indexId":"wdrCA642","displayToPublicDate":"1964-01-01T10:32:13","publicationYear":"1964","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"CA-64-2","title":"Surface water records of California, 1964; Volume 2: Northern Great Basin and Central Valley","docAbstract":"<p>The surface-water records for the 1964 water year for gaging stations, partial-record stations, and miscellaneous sites within the State of California are given in this report. For convenience there are also included records for a few pertinent gaging stations in bordering States. The records were collected and computed by the Water Resources Division of the U.S. Geological Survey, under the direction of Walter Hofmann, district engineer, Surface Water Branch.</p><p>Through September 30, 1960, the records of discharge and stage of streams and contents and stage of lakes or reservoirs were published in an annual series of U.S. Geological Survey water-supply papers entitled \"Surface Water Supply of the United States.\" Since 1951 there have been 20 volumes in the series; each volume covered an area whose boundaries coincided with those of certain natural drainage areas. The records in California were contained in parts 9, 10, and 11 of that series.</p><p>Beginning with the 1961 water year, streamflow records and related data are being released by the Geological Survey in annual reports on a State-boundary basis. Distribution of these basic data reports is limited and primarily for local needs. The records later will be published in Geological Survey water-supply papers at 5-year intervals. These 5-year water-supply papers will show daily discharge and will be compiled on the same geographical areas previously used for the annual series; however, some of the 14 parts of conterminous United States will be further subdivided.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wdrCA642","collaboration":"Prepared in cooperation with the State of California and with other agencies","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1964, Surface water records of California, 1964; Volume 2: Northern Great Basin and Central Valley: U.S. Geological Survey Water Data Report CA-64-2, xiv, 499-991 p., https://doi.org/10.3133/wdrCA642.","productDescription":"xiv, 499-991 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,{"id":70190796,"text":"70190796 - 1964 - Ground-water data, Sevier Desert, Utah","interactions":[],"lastModifiedDate":"2017-09-14T11:38:12","indexId":"70190796","displayToPublicDate":"1964-01-01T00:00:00","publicationYear":"1964","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":5497,"text":"Utah Basic-Data Report","active":false,"publicationSubtype":{"id":2}},"seriesNumber":"9","title":"Ground-water data, Sevier Desert, Utah","docAbstract":"<p>This report is intended to serve two purposes: (1) to make available to the public basic ground-water data useful in planning and studying development of water resources, and (2) to supplement an interpretive report that will be published later.</p><p>Records were collected during the period 1935-64 by the U.S. Geological survey in cooperation with the Utah State Engineer as part of the investigation of ground-water conditions in the Sevier Desert, in Juab and Millard Counties, Utah. The interpretive material will be published in a companion report by R. W. Mower and R. D. Feltis.</p><p>This report is most useful in predicting conditions likely to be found in areas that are being considered as well sites. The person considering the new well can spot the proposed site on plate 1 and examine the records of nearby wells as shown in the tables and figures. From table 1 he can note such things as depth, diameter, water level, yield, use of water, temperature of water, and depth of perforations. By comparing the depth of perforations with the drillers' logs in table 3 he can note the type of material that yields water to the wells. Table 2 and figure 2 show the historic fluctuations and trends of water levels in the vicinity. From table 4 he can note the chemical quality of the water from wells in the vicinity. Table 5 shows the amount of water discharged during 1951-63 from the pumped irrigation, public supply, and industrial wells. If the reader decides from his examination that conditions are favorable, he can place an application to drill a well with the state Engineer. If the State Engineer believes unappropriated water is available, the application may be approved after minimum statutory requirements have been satisfied.</p><p>The report is also useful when planning large-scale developments of water supply. This and other uses of the report will be helped by use of the interpretive report upon its release.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Salt Lake City, UT","collaboration":"Prepared in cooperation with the Utah State Engineer","usgsCitation":"Mower, R.W., and Feltis, R.D., 1964, Ground-water data, Sevier Desert, Utah: Utah Basic-Data Report 9, 34 p.","productDescription":"34 p.","numberOfPages":"41","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":345766,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":345765,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://www.waterrights.utah.gov/cgi-bin/docview.exe?Folder=TP21-1-180&Title=Basic+Data+Report+9"}],"country":"United States","state":"Utah","otherGeospatial":"Sevier Desert","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"59bb953ae4b091459a578228","contributors":{"authors":[{"text":"Mower, Reed W.","contributorId":32503,"corporation":false,"usgs":true,"family":"Mower","given":"Reed","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":710423,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Feltis, Richard D.","contributorId":98773,"corporation":false,"usgs":true,"family":"Feltis","given":"Richard","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":710424,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70190800,"text":"70190800 - 1964 - Selected hydrologic data, upper Sevier River basin, Utah","interactions":[],"lastModifiedDate":"2017-09-14T12:50:52","indexId":"70190800","displayToPublicDate":"1964-01-01T00:00:00","publicationYear":"1964","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":5497,"text":"Utah Basic-Data Report","active":false,"publicationSubtype":{"id":2}},"seriesNumber":"8","title":"Selected hydrologic data, upper Sevier River basin, Utah","docAbstract":"<p>This report is intended to serve two purposes: (1) to make available to the public basic ground-water data useful in planning and studying development of water resources, and (2) to supplement an interpretive report that will be published later.</p><p>Records were collected during 1961-63 by the U.S. Geological Survey in cooperation with the Utah State Engineer as a part of the investigation of ground-water conditions in the upper Sevier River basin, in parts of Garfield, Iron, Kane, Piute, and Sevier Counties, Utah. The interpretive material will be published in a companion report by Carl H. Carpenter, Gerald B. Robinson, Jr., and Louis J. Bjorklund.</p><p>This report is most useful in predicting conditions likely to be found in areas that are being considered as well sites. The person considering the new well can spot the proposed site on plate 1 and examine the records of nearby wells and springs as shown in the tables. From table 1 he can find information on wells, including depth, diameter, water level, yield, drawdown, use of water, temperature of water, and depth of perforations. Table 2 gives information on springs such as yield, use of water, temperature, and improvements. From tables 1 and 2 he can note the type of material that yields water in the vicinity. Table 3 shows the historic fluctuations and trends of water levels. Table 4 shows the type of material penetrated by wells. From table 5 he can note the chemical quality of water from wells and springs, and from table 6, the chemical quality of surface water. If the reader decides from his examination that conditions are favorable, he can place an application to drill a well with the State Engineer. If the State Engineer believes unappropriated water is available, the application may be approved after minimum statutory requirements have been satisfied.</p><p>The report is also useful when planning large-scale developments of water supply. This and other uses of the report will be helped by use of the interpretive report upon its release.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Salt Lake City, UT","collaboration":"Prepared in cooperation with the Utah State Engineer","usgsCitation":"Carpenter, C.H., Robinson, G.B., and Bjorklund, L.J., 1964, Selected hydrologic data, upper Sevier River basin, Utah: Utah Basic-Data Report 8, 29 p.","productDescription":"29 p.","numberOfPages":"37","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":345770,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":345769,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://www.waterrights.utah.gov/cgi-bin/docview.exe?Folder=TP21-1-160&Title=Basic+Data+Report+8"}],"country":"United States","state":"Utah","county":"Garfield County, Iron County, Kane County, Piute County, Sevier County","otherGeospatial":"Sevier River basi","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"59bb953ae4b091459a578226","contributors":{"authors":[{"text":"Carpenter, Carl H.","contributorId":46074,"corporation":false,"usgs":true,"family":"Carpenter","given":"Carl","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":710428,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Robinson, Gerald B. Jr.","contributorId":91837,"corporation":false,"usgs":true,"family":"Robinson","given":"Gerald","suffix":"Jr.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":710429,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Bjorklund, Louis Jay","contributorId":21138,"corporation":false,"usgs":true,"family":"Bjorklund","given":"Louis","email":"","middleInitial":"Jay","affiliations":[],"preferred":false,"id":710430,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":2000008,"text":"2000008 - 1964 - Lake Michigan chemical data, 1954-55, 1960-61","interactions":[],"lastModifiedDate":"2012-02-02T00:14:59","indexId":"2000008","displayToPublicDate":"1964-01-01T00:00:00","publicationYear":"1964","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":17,"text":"Data Report","active":false,"publicationSubtype":{"id":1}},"seriesNumber":"6","title":"Lake Michigan chemical data, 1954-55, 1960-61","docAbstract":"This report presents without interpretation methods used in and the results of chemical analyses, and supplemental observations of temperatures at depth, transparency, and meteorological conditions for Lake Michigan in 1954, 1955, 1960, and 1961.","language":"English","publisher":"U.S. Fish and Wildlife Service","collaboration":"Out-of-print","usgsCitation":"Beeton, A.M., and Moffett, J.W., 1964, Lake Michigan chemical data, 1954-55, 1960-61: Data Report 6, 102 p.","productDescription":"102 p.","startPage":"0","endPage":"102","numberOfPages":"102","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":198578,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b32e4b07f02db6b4339","contributors":{"authors":[{"text":"Beeton, Alfred M.","contributorId":94247,"corporation":false,"usgs":true,"family":"Beeton","given":"Alfred","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":324918,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Moffett, James W.","contributorId":94245,"corporation":false,"usgs":true,"family":"Moffett","given":"James","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":324917,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70046789,"text":"70046789 - 1964 - Classes of land-surface form in the United States","interactions":[],"lastModifiedDate":"2013-07-08T13:35:00","indexId":"70046789","displayToPublicDate":"1964-01-01T00:00:00","publicationYear":"1964","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"title":"Classes of land-surface form in the United States","docAbstract":"This digital dataset describes classes of land-surface form in the conterminous United States.  The source of the data is the map of land-surface form in the 1970 National Atlas of the United States, pages 62-63, which was adapted from Edwin H. Hammond, \"Classes of land surface form in the forty-eight states, U.S.A,\" Annals of the Assoc. of Am. Geographers, v.54, no. 1, 1964, map supp. no. 1, 1:5,000,000.","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"The national atlas of the United States of America","largerWorkSubtype":{"id":6,"text":"USGS Unnumbered Series"},"language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/70046789","usgsCitation":"Hammond, E., 1964, Classes of land-surface form in the United States (1.0), Datatset, https://doi.org/10.3133/70046789.","productDescription":"Datatset","onlineOnly":"Y","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":274677,"type":{"id":16,"text":"Metadata"},"url":"https://water.usgs.gov/GIS/metadata/usgswrd/XML/na70_landfrm.xml"},{"id":274684,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"country":"United States","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -127.889969,22.863141 ], [ -127.889969,51.606088 ], [ -65.349827,51.606088 ], [ -65.349827,22.863141 ], [ -127.889969,22.863141 ] ] ] } } ] }","edition":"1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"51dbdf69e4b0f81004b77ce8","contributors":{"authors":[{"text":"Hammond, Edwin","contributorId":100719,"corporation":false,"usgs":true,"family":"Hammond","given":"Edwin","email":"","affiliations":[],"preferred":false,"id":480257,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70176113,"text":"70176113 - 1964 - Surface water records of Texas, 1963","interactions":[],"lastModifiedDate":"2017-06-07T17:30:30","indexId":"70176113","displayToPublicDate":"1964-01-01T00:00:00","publicationYear":"1964","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"seriesTitle":{"id":5196,"text":"Water Data Report","active":true,"publicationSubtype":{"id":6}},"title":"Surface water records of Texas, 1963","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/70176113","usgsCitation":"U.S. Geological Survey, 1964, Surface water records of Texas, 1963: Water Data Report, 421 p., https://doi.org/10.3133/70176113.","productDescription":"421 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science 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,{"id":70010548,"text":"70010548 - 1964 - A thermodynamic study of pyrite and pyrrhotite","interactions":[],"lastModifiedDate":"2020-11-24T00:46:42.769531","indexId":"70010548","displayToPublicDate":"1964-01-01T00:00:00","publicationYear":"1964","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1759,"text":"Geochimica et Cosmochimica Acta","active":true,"publicationSubtype":{"id":10}},"title":"A thermodynamic study of pyrite and pyrrhotite","docAbstract":"<p>Through the use of the electrum-tarnish method the following equation has been found to interrelate the composition of pyrrhotite, fugacity of sulfur, and temperature: In this equation f<sub>s2</sub><span>&nbsp;</span>is the fugacity of sulfur relative to the ideal diatomic gas at 1 atm,<span>&nbsp;</span><i>N</i><span>&nbsp;</span>is the mol fraction of FeS in pyrrhotite (in the system FeS-S<sub>2</sub>), and<span>&nbsp;</span><i>T</i><span>&nbsp;</span>the absolute temperature. The experimental uncertainty in the equation is 0–003 in<span>&nbsp;</span><i>N</i>. The activity of FeS (<i>a</i><sub><i>FeS</i></sub>) in pyrrhotite relative to the pure substance at the temperature of consideration follows from the above equation by virtue of the Gibbs-Duhem relation; it is given by:</p><p>The electrum-tarnish method has permitted us to determine the f<sub>s2</sub><span>&nbsp;</span>vs.<span>&nbsp;</span><i>T</i><span>&nbsp;</span>curve for the univariant assemblage pyrrhotite-pyrite-vapor from 743 to 325°C. Our determinations of the composition of pyrrhotite are in excellent agreement with the results of Arnold. The activity of FeS in pyrite-saturated pyrrhotite is very different from unity, a fact that greatly influences the interpretation of some other phase equilibrium studies involving pyrrhotite and their application to sulfide mineral assemblages, but has little effect on the more general calculations of composition of hydrothermal or magmatic fluids.</p><p>Pressure effects calculated from available volumetric data on the phases are small.</p>","language":"English","publisher":"Elsevier","doi":"10.1016/0016-7037(64)90083-3","issn":"00167037","usgsCitation":"Toulmin, P., and Barton, P.B., 1964, A thermodynamic study of pyrite and pyrrhotite: Geochimica et Cosmochimica Acta, v. 28, no. 5, p. 641-671, https://doi.org/10.1016/0016-7037(64)90083-3.","productDescription":"31 p.","startPage":"641","endPage":"671","numberOfPages":"31","costCenters":[],"links":[{"id":218901,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"28","issue":"5","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059e5fbe4b0c8380cd4709c","contributors":{"authors":[{"text":"Toulmin, P. III","contributorId":81244,"corporation":false,"usgs":true,"family":"Toulmin","given":"P.","suffix":"III","email":"","affiliations":[],"preferred":false,"id":359152,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Barton, P. B. Jr.","contributorId":23683,"corporation":false,"usgs":true,"family":"Barton","given":"P.","suffix":"Jr.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":359151,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70190980,"text":"70190980 - 1964 - Quality of surface waters in Utah, October 1962 to September 1963","interactions":[],"lastModifiedDate":"2017-09-19T16:02:03","indexId":"70190980","displayToPublicDate":"1964-01-01T00:00:00","publicationYear":"1964","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"seriesTitle":{"id":375,"text":"Open-File Report","active":false,"publicationSubtype":{"id":6}},"title":"Quality of surface waters in Utah, October 1962 to September 1963","docAbstract":"<p><span>This data release is a compilation that presents water-quality data for the period October 1962 to September 1963 for the sites listed on page 2. These preliminary data are subject to revision before final publication in the annual series of U.S. Geological Survey Water-supply papers entitled Quality of surface waters of the United States. Most of the data were obtained as part of the Geological Survey's continuing program for the investigation of the nation's water resources or as part of a cooperative program with the U.S. Bureau of Reclamation; some data were obtained as part of cooperative programs with the State Engineer of Utah and with the Soil Conservation Service.</span></p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Salt Lake City, UT","doi":"10.3133/70190980","usgsCitation":"U.S. Geological Survey, 1964, Quality of surface waters in Utah, October 1962 to September 1963: Open-File Report, v, 77 p., https://doi.org/10.3133/70190980.","productDescription":"v, 77 p.","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":345895,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"country":"United States","state":"Utah","publicComments":"Data Release 1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"59c22cb6e4b091459a61b756","contributors":{"authors":[{"text":"U.S. Geological Survey","contributorId":127955,"corporation":true,"usgs":false,"organization":"U.S. Geological Survey","id":710811,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70217324,"text":"wdrMDDE63 - 1963 - Surface water records of Maryland and Delaware, water year 1963","interactions":[],"lastModifiedDate":"2021-01-22T19:13:18.810771","indexId":"wdrMDDE63","displayToPublicDate":"2021-01-22T14:45:00","publicationYear":"1963","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"MD-DE-63","displayTitle":"Surface Water Records of Maryland and Delaware, Water Year 1963","title":"Surface water records of Maryland and Delaware, water year 1963","docAbstract":"<p>No abstract available.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wdrMDDE63","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1963, Surface water records of Maryland and Delaware, water year 1963: U.S. Geological Survey Water Data Report MD-DE-63, 114 p., https://doi.org/10.3133/wdrMDDE63.","productDescription":"114 p.","costCenters":[{"id":41514,"text":"Maryland-Delaware-District of Columbia  Water Science Center","active":true,"usgs":true}],"links":[{"id":382225,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/1963/md-de-63/swrMDDE63.pdf","text":"Report","size":"10.7 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Water Data Report MD-DE-63"},{"id":382224,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wdr/1963/md-de-63/swrMDDE63_coverthb.jpg"}],"country":"United States","state":"Delaware, 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,{"id":70159019,"text":"tei830 - 1963 - X-ray crystallographic data for minerals","interactions":[],"lastModifiedDate":"2015-10-22T11:51:13","indexId":"tei830","displayToPublicDate":"2015-06-08T09:15:00","publicationYear":"1963","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":"830","title":"X-ray crystallographic data for minerals","docAbstract":"<p>X-ray crystallographic data are of particular importance to the mineralogist. Beyond the considerations of structural chemistry they provide. one of the most accurate methods for phase and/or compositional determination and for obtaining _the molar volumes and densities of minerals {Robie and Bethke, 1962).</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/tei830","usgsCitation":"Robie, R.A., Bethke, P., Toulmin, M., and Edwards, J.L., 1963, X-ray crystallographic data for minerals: U.S. Geological Survey Trace Elements Investigations 830, 38 p., https://doi.org/10.3133/tei830.","productDescription":"38 p.","numberOfPages":"42","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":310434,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/tei/830/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":309848,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/tei830.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"561e2b3ee4b0cdb063e59d01","contributors":{"authors":[{"text":"Robie, Richard A.","contributorId":92235,"corporation":false,"usgs":true,"family":"Robie","given":"Richard","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":577267,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bethke, Philip M.","contributorId":52829,"corporation":false,"usgs":true,"family":"Bethke","given":"Philip M.","affiliations":[],"preferred":false,"id":577268,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Toulmin, M.S.","contributorId":62677,"corporation":false,"usgs":true,"family":"Toulmin","given":"M.S.","email":"","affiliations":[],"preferred":false,"id":577269,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Edwards, Jerry L.","contributorId":149197,"corporation":false,"usgs":false,"family":"Edwards","given":"Jerry","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":577270,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":71788,"text":"tei836 - 1963 - Ground-water test well 2, Nevada test site, Nye County, Nevada : a summary of lithologic data, aquifer tests, and well construction","interactions":[],"lastModifiedDate":"2014-07-16T14:03:58","indexId":"tei836","displayToPublicDate":"2013-07-16T14:01:00","publicationYear":"1963","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":"836","title":"Ground-water test well 2, Nevada test site, Nye County, Nevada : a summary of lithologic data, aquifer tests, and well construction","docAbstract":"No abstract available.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/tei836","collaboration":"Work done on behalf of the U.S. Atomic Energy Commission.","usgsCitation":"Moore, J.E., and Carroll, R.D., 1963, Ground-water test well 2, Nevada test site, Nye County, Nevada : a summary of lithologic data, aquifer tests, and well construction: U.S. Geological Survey Trace Elements Investigations 836, 73 p., https://doi.org/10.3133/tei836.","productDescription":"73 p.","costCenters":[],"links":[{"id":290301,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"country":"United States","state":"Nevada","county":"Nye County","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -118.1972,35.9618 ], [ -118.1972,39.1634 ], [ -114.999,39.1634 ], [ -114.999,35.9618 ], [ -118.1972,35.9618 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53c79ef7e4b0194841642456","contributors":{"authors":[{"text":"Moore, John Ezra","contributorId":93582,"corporation":false,"usgs":true,"family":"Moore","given":"John","email":"","middleInitial":"Ezra","affiliations":[],"preferred":false,"id":284756,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Carroll, Roderick D.","contributorId":93395,"corporation":false,"usgs":true,"family":"Carroll","given":"Roderick","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":284755,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70038668,"text":"wdrCA621 - 1963 - Surface water records of California, 1962; Volume 1: Colorado River Basin, Southern Great Basin, and Pacific Slope Basins excluding Central Valley","interactions":[],"lastModifiedDate":"2012-06-13T01:01:48","indexId":"wdrCA621","displayToPublicDate":"2012-06-04T09:06:00","publicationYear":"1963","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"CA-62-1","title":"Surface water records of California, 1962; Volume 1: Colorado River Basin, Southern Great Basin, and Pacific Slope Basins excluding Central Valley","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wdrCA621","usgsCitation":"U.S. Geological Survey, 1963, Surface water records of California, 1962; Volume 1: Colorado River Basin, Southern Great Basin, and Pacific Slope Basins excluding Central Valley: U.S. Geological Survey Water Data Report CA-62-1, 479 p., https://doi.org/10.3133/wdrCA621.","productDescription":"479 p.","temporalStart":"1961-10-01","temporalEnd":"1962-09-30","costCenters":[],"links":[{"id":257481,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/wdr_CA_62_1.jpg"},{"id":257474,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/1962/ca-62/WDR-1962-vol1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"California","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505b9fcce4b08c986b31e815"}
,{"id":70039490,"text":"70039490 - 1963 - Preliminary study of first motion from nuclear explosions recorded on seismograms in the first zone","interactions":[],"lastModifiedDate":"2012-08-08T01:02:14","indexId":"70039490","displayToPublicDate":"2012-01-01T15:24:52","publicationYear":"1963","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"seriesTitle":{"id":355,"text":"Crustal Studies Technical Letter","active":false,"publicationSubtype":{"id":6}},"seriesNumber":"13","title":"Preliminary study of first motion from nuclear explosions recorded on seismograms in the first zone","docAbstract":"The U.S. Geological Survey has recorded more than 300 seismograms from more than 50 underground nuclear explosions. Most were recorded at distances of less than 1,000 km. These seismograms have been studied to obtain travel times and amplitudes which have been presented in reports on crustal structure and in a new series of nuclear shot reports. This report describes preliminary studies of first motion of seismic waves generated by underground nuclear explosions. Visual inspection of all seismograms was made in an attempt to identify the direction of first motion, and to estimate the probability of recording detectable first motion at various distances for various charge sizes and in different geologic environments. In this study, a characteristic pattern of the first phase became apparent on seismograms where first motion was clearly recorded. When an interpreter became familiar with this pattern, he was frequently able to identify the polarity of the first arrival even though the direction of first motion could not be seen clearly on the seismogram. In addition, it was sometimes possible to recognize this pattern for secondary arrivals of larger amplitude. These qualitative visual observations suggest that it might be possible to define a simple criterion that could be used in a digital computer to identify polarity, not only of the first phase, but of secondary phases as well. A short segment of recordings near the first motion on 56 seismograms was digitized on an optical digitizer. Spectral analyses of these digitized recordings were made to determine the range of frequencies present, and studies were made with various simple digital filters to explore the nature of polarity as a function of frequency. These studies have not yet led to conclusive results, partly because of inaccuracies resulting from optical digitization. The work is continuing, using an electronic digitizer that will allow study of a much larger sample of more accurately digitized data.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/70039490","collaboration":"In cooperation with the Defense Advanced Research Projects Agency","usgsCitation":"Healy, J.H., and Mangan, G.B., 1963, Preliminary study of first motion from nuclear explosions recorded on seismograms in the first zone: Crustal Studies Technical Letter 13, 19 p.; ill.; map, https://doi.org/10.3133/70039490.","productDescription":"19 p.; ill.; map","startPage":"1","endPage":"19","numberOfPages":"23","onlineOnly":"Y","additionalOnlineFiles":"N","costCenters":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true}],"links":[{"id":259494,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":259486,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/misc/tl/0013/","linkFileType":{"id":5,"text":"html"}},{"id":259487,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/misc/tl/0013/tl0013.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a8ab4e4b0c8380cd7e0d6","contributors":{"authors":[{"text":"Healy, J. H.","contributorId":48968,"corporation":false,"usgs":true,"family":"Healy","given":"J.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":466357,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Mangan, G. B.","contributorId":86035,"corporation":false,"usgs":true,"family":"Mangan","given":"G.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":466358,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70039283,"text":"70039283 - 1963 - Crustal structure in the western United States; study of seismic propagation paths and regional traveltimes in the California-Nevada region","interactions":[],"lastModifiedDate":"2012-08-01T01:01:41","indexId":"70039283","displayToPublicDate":"2012-01-01T13:50:03","publicationYear":"1963","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"seriesTitle":{"id":355,"text":"Crustal Studies Technical Letter","active":false,"publicationSubtype":{"id":6}},"seriesNumber":"9","title":"Crustal structure in the western United States; study of seismic propagation paths and regional traveltimes in the California-Nevada region","docAbstract":"The U.S. Geological Survey, with the assistance of United ElectroDynamics, Inc., completed ten weeks of seismic-refraction field work during the summer of 1962 in the southwestern part of the United States. This work was a continuation of a program initiated in 1961 to study traveltimes and seismic propagation paths in the earth?s crust and upper mantle in the western United States. A total of 761 seismograms were recorded along 10 profiles from 86 explosions at 18 shotpoints. Analysis of the data is continuing, but a few conclusions can be made from a preliminary study: (1) Variations in traveltimes in the Basin and Range province are large but measurable, and perhaps predictable. (2) Traveltimes of seismic waves in adjacent geologic provinces are usually significantly different. (3) The velocity of P<sub>g</sub> along all of the profiles recorded in 1962 ranges from 5.0 to 6.5 km/sec, and averages 6.0 km/sec. (4) The average velocity of P<sub>g</sub> in extreme northern Nevada and southern Idaho is 5.6 km/sec, and it is 6.1 km/sec in most of Nevada and California. (5) The average velocity of P<sub>n</sub> is 7&ndash;9 km/ sec and ranges from 7.85 to 7.95 km/sec on reversed profiles where the true P<sub>n</sub> velocity could be computed. (6) A shallow \"intermediate\" layer with a velocity of approximately 6.8 km/sec was found in the Snake River Plain. (7) Refraction arrivals from the mantle (P<sub>n</sub>) were recorded in the Sierra Nevada. They indicate that the thickness of the crust in the Sierra Nevada is much greater than that in the Basin and Range province. (8) Many refinements in field techniques were made during the 1962 field season.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/70039283","collaboration":"In cooperation with the Defense Advanced Research Projects Agency","usgsCitation":"Roller, J., Jackson, W.H., Cooper, J., and Martina, B., 1963, Crustal structure in the western United States; study of seismic propagation paths and regional traveltimes in the California-Nevada region: Crustal Studies Technical Letter 9, 57 p.; ill.; maps, https://doi.org/10.3133/70039283.","productDescription":"57 p.; ill.; maps","startPage":"1","endPage":"57","numberOfPages":"78","onlineOnly":"Y","additionalOnlineFiles":"N","costCenters":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true}],"links":[{"id":259329,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":259316,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/misc/tl/0009/tl0009.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":259315,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/misc/tl/0009/","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"California;Nevada;Idaho","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059fce9e4b0c8380cd4e4eb","contributors":{"authors":[{"text":"Roller, J.C.","contributorId":12507,"corporation":false,"usgs":true,"family":"Roller","given":"J.C.","email":"","affiliations":[],"preferred":false,"id":465956,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Jackson, W. H.","contributorId":21153,"corporation":false,"usgs":true,"family":"Jackson","given":"W.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":465957,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Cooper, J.F.","contributorId":79739,"corporation":false,"usgs":true,"family":"Cooper","given":"J.F.","email":"","affiliations":[],"preferred":false,"id":465959,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Martina, B.A.","contributorId":68153,"corporation":false,"usgs":true,"family":"Martina","given":"B.A.","email":"","affiliations":[],"preferred":false,"id":465958,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70039537,"text":"70039537 - 1963 - Preliminary report on seismic-reflection studies of crustal structure in the western, central, and southern United States","interactions":[],"lastModifiedDate":"2012-08-11T01:01:52","indexId":"70039537","displayToPublicDate":"2012-01-01T10:12:00","publicationYear":"1963","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"seriesTitle":{"id":355,"text":"Crustal Studies Technical Letter","active":false,"publicationSubtype":{"id":6}},"seriesNumber":"14","title":"Preliminary report on seismic-reflection studies of crustal structure in the western, central, and southern United States","docAbstract":"During 1963 the U.S. Geological Survey, with the assistance of United ElectroDynamics, Inc., recorded five separate reversed seismic profiles. In addition to these profiles, the U.S. Geological Survey participated in a seismic-calibration program for the DRIBBLE experiment at Tatum Dome, Mississippi, a 20,000-pound shot near Dexter, Missouri, and in a cooperative seismic experiment in the Lake Superior region. This work is a continuation of the program started in 1961; however, the emphasis has shifted from a detailed study of the earth's crust in the western United States to a study of crustal structure in various geologic environments including the Wyoming thrust belt, Colorado Plateau, Central Lowlands, the Gulf Coastal Plain, and the southern part of the Canadian Shield. The U.S. Geological Survey has now completed reversed seismic-refraction profiles in nine different geologic provinces. These data present a promising indication that it may be possible to predict the crustal structure in unexplored areas by considering the regional geologic and physiographic environment. The following P<sub>n</sub> velocities have been determined: 8.2 km/sec in the Wyoming thrust belt, 7.9 km/sec in the Colorado Plateau, 8.1 km/sec in the Central Lowlands, and about 8.2 km/sec in the Gulf Coastal Plain. The data from the Lake Superior region have not yet been interpreted.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Denver, CO","doi":"10.3133/70039537","collaboration":"In cooperation with the Defense Advanced Research Projects Agency","usgsCitation":"Roller, J., Strozier, O., Jackson, W.H., and Healy, J.H., 1963, Preliminary report on seismic-reflection studies of crustal structure in the western, central, and southern United States: Crustal Studies Technical Letter 14, x, 55 p., https://doi.org/10.3133/70039537.","productDescription":"x, 55 p.","numberOfPages":"65","onlineOnly":"Y","costCenters":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true}],"links":[{"id":259574,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":259555,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/misc/tl/0014/","linkFileType":{"id":5,"text":"html"}},{"id":259556,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/misc/tl/0014/tl0014.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Arizona;Idaho;Mississippi;Missouri;Utah","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -113,30 ], [ -113,43 ], [ -89.25,43 ], [ -89.25,30 ], [ -113,30 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a89d2e4b0c8380cd7df61","contributors":{"authors":[{"text":"Roller, J.C.","contributorId":12507,"corporation":false,"usgs":true,"family":"Roller","given":"J.C.","email":"","affiliations":[],"preferred":false,"id":466438,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Strozier, O.P.","contributorId":96526,"corporation":false,"usgs":true,"family":"Strozier","given":"O.P.","email":"","affiliations":[],"preferred":false,"id":466441,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Jackson, W. H.","contributorId":21153,"corporation":false,"usgs":true,"family":"Jackson","given":"W.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":466439,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Healy, J. H.","contributorId":48968,"corporation":false,"usgs":true,"family":"Healy","given":"J.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":466440,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70046320,"text":"wdrNM63 - 1963 - Surface water records of New Mexico, water year 1963","interactions":[],"lastModifiedDate":"2021-01-08T17:35:09.585154","indexId":"wdrNM63","displayToPublicDate":"2012-01-01T00:00:00","publicationYear":"1963","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"NM-63","title":"Surface water records of New Mexico, water year 1963","docAbstract":"<p>The surface-water records for the 1963 water year for gaging stations, partial-record stations, and miscellaneous sites within the State of New Mexico are given in this report. For convenience there are also included. records for a few pertinent gaging stations in bordering States. The records were collected and computed by the Water Resources Division of the U. S. Geological Survey, under the direction of W. L. Heckler, district engineer, Surface Water Branch. </p><p>This report is the third in a series presenting, annually, basic data on surface-water records by States. Through September 30, 1960, the records of discharge and stage of streams and contents and stage of lakes or reservoirs were published in an annual series of U. S. Geological Survey water-supply papers entitled \"Surface Water Supply of the United States. ff Since 1951 there have been 20 volumes in the series; each volume covered an area whose boundaries coincided with those of certain natural drainage areas. The records in New Mexico were contained in Parts 7, 8, and 9 of that series.</p><p>Beginning with the 1961 water year, streamflow records and related data will be released by the Geological Survey in annual reports on a State-boundary basis. Distribution of these basic-data reports will be limited and primarily for local needs. The records later will be published in Geological Survey water-supply papers at 5- year intervals. These 5-year water-supply papers will show daily discharge and will be compiled on the same geographical areas previously used for the annual series; however, some of the 14 parts of conterminous United States will be further subdivided.</p><p>The records for New Mexico will be published in water-supply papers covering Part 7 for stations in the Lower Mississippi River drainage, Part 8 for Western Gulf of Mexico drainage, and Part 9 for Colorado River drainage. For 1960 water year, the WSP Numbers for these parts were 1711, 1712, 1713 respectively. A compilation of records for these parts through 1950 water year is contained in WSP Nos. 1311, 1312, 1313 respectively; a 1951-60 compilation series will have WSP Nos. 1731, 1732, 1733. </p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Santa Fe, NM","doi":"10.3133/wdrNM63","collaboration":"Prepared in cooperation with the State of New Mexico and with other agencies","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1963, Surface water records of New Mexico, water year 1963: U.S. Geological Survey Water Data Report NM-63, vii, 228 p., https://doi.org/10.3133/wdrNM63.","productDescription":"vii, 228 p.","numberOfPages":"237","costCenters":[],"links":[{"id":273449,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":274518,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/1963/nm-63/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"New Mexico","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -109.052,31.3322 ], [ -109.052,37.0003 ], [ -103.002,37.0003 ], [ -103.002,31.3322 ], [ -109.052,31.3322 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"51b300e8e4b01368e589e408","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":535530,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70039753,"text":"wdrCA63Water Quality - 1963 - Quality of waters in California","interactions":[],"lastModifiedDate":"2012-08-31T17:16:24","indexId":"wdrCA63Water Quality","displayToPublicDate":"2008-01-08T10:04:00","publicationYear":"1963","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"CA-63-Water Quality","title":"Quality of waters in California","docAbstract":"The quality-of-water investigations of the U.S. Geological Survey are concerned with the chemical and physical characteristics of surface and ground water supplies of the nation in conjunction with water usage and its availability. The basic records for the 1963 water year for quality of surface waters within the State of California are given in this report. For convenience and interest there are also records for a few water quality stations in bordering states. The data were collected and computed by the Water Resources Division of the U.S. Geological Survey, under the direction of Eugene Brown, district chemist, Quality of Water Branch.","language":"English","publisher":"U.S. Geological Survey, Water Division","publisherLocation":"Sacramento, CA","doi":"10.3133/wdrCA63Water Quality","collaboration":"Prepared in cooperation with California Department of Water Resources, California Water Pollution Control Board, Monterey County Flood Control and Water Conservation District, Bureau of Reclamation, United States Department of the Interior, U.S. Army Corps of Engineers","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1963, Quality of waters in California (Legacy Report): U.S. Geological Survey Water Data Report CA-63-Water Quality, ix, 352 p., https://doi.org/10.3133/wdrCA63Water Quality.","productDescription":"ix, 352 p.","costCenters":[{"id":629,"text":"Water Resources Division","active":false,"usgs":true}],"links":[{"id":259978,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":259976,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/1963/ca-63/WRD-1963-qw.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"California","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -124.4,32.5 ], [ -124.4,42 ], [ -114.13333333333334,42 ], [ -114.13333333333334,32.5 ], [ -124.4,32.5 ] ] ] } } ] }","edition":"Legacy Report","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a917de4b0c8380cd802b6","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":535386,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":71004,"text":"wdrCO631 - 1963 - Surface water records of Colorado, water year 1963","interactions":[],"lastModifiedDate":"2012-02-02T00:13:46","indexId":"wdrCO631","displayToPublicDate":"2005-08-09T00:00:00","publicationYear":"1963","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"CO-63-1","title":"Surface water records of Colorado, water year 1963","language":"ENGLISH","doi":"10.3133/wdrCO631","usgsCitation":"Geological Survey, U., 1963, Surface water records of Colorado, water year 1963: U.S. Geological Survey Water Data Report CO-63-1, 335 p., https://doi.org/10.3133/wdrCO631.","productDescription":"335 p.","costCenters":[],"links":[{"id":185750,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wdr/1963/co-63-1/report-thumb.jpg"},{"id":90532,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/1963/co-63-1/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afee4b07f02db69793b","contributors":{"authors":[{"text":"Geological Survey, U.S.","contributorId":26017,"corporation":false,"usgs":true,"family":"Geological Survey","given":"U.S.","affiliations":[],"preferred":false,"id":283480,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":32743,"text":"pp379 - 1963 - Surficial geology and soils of the Elmira-Williamsport region, New York and Pennsylvania, with a section on forest regions and great soil groups","interactions":[],"lastModifiedDate":"2022-03-29T21:42:36.762876","indexId":"pp379","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1963","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":"379","title":"Surficial geology and soils of the Elmira-Williamsport region, New York and Pennsylvania, with a section on forest regions and great soil groups","docAbstract":"<p>The Elmira-Williamsport region, lying south of the Finger Lakes in central New York and northern Pennsylvania, is part of the Appalachian Plateaus physiographic province. A small segment of the Valley and Ridge province is included near the south border. In 1953 and 1954, the authors, a geologist and a soil scientist, made a reconnaissance of about 5,000 square miles extending southward from the Finger Lakes, N.Y., to Williamsport, Pa., and eastward from Wellsboro, Pa., to Towanda, Pa. Glacial drift of Wisconsin age, covering the central and most of the northern parts of the region, belongs to the Olean substage of MacClintock and Apfel. This drift is thin and patchy, is composed of the relatively soft sandstones, siltstone, shales, and conglomerates of the plateaus, commonly has a low calcium carbonate content, and is deeply leached. Mantling its surface are extensive rubbly colluvial deposits. No conspicuous terminal moraine marks the relatively straight border of Olean drift. The Valley Heads moraine of Fairchild near the south ends of the Finger Lakes is composed of relatively thick drift containing a considerable amount of somewhat resistant sedimentary and crystalline rocks. Commonly this drift has a relatively high carbonate content and is leached to only shallow depths. The Valley Heads drift is younger than Olean, but its precise age is undetermined. The age of the Olean is perhaps between Sangamon and Farmdale, on the basis of, in part, a carbon-14 date from peat at Otto, N.Y. All differences in soil development on these two Wisconsin drifts are clearly related to the lithology of the parent material or the drainage, rather than to weathering differing in kind or in duration. The authors believe that the soils are relatively young, are in equilibrium with the present environment, and contain few, if any, features acquired during past weathering intervals. The effect of tree throw on soil profiles and the presence of soils on slopes clearly indicate that soils form rapidly. Sols Bruns Acides are the most extensive great soil group occurring throughout the region. Podzols and Gray-Brown Podzolic soils are also widespread, and on long, smooth slopes Low Humic-Gley soils are common. Organic soils are of small extent. South of the Wisconsin drift border, the surficial mantle consists chiefly of alluvial, colluvial, or residual deposits of Wisconsin or of Recent age, but there are many small isolated patches of older, strongly weathered materials of pre-Wisconsin age. Although such older materials are commonly overlain or mixed with less weathered mantle, the yellowish-red color, characteristic of the strongly weathered material, is generally not masked. Some of the older material is drift, presumed to be of Illionian age, that was probably strongly weathered to a considerable depth in Sangamon time and has been greatly eroded since the last interglacial period. No clear-cut exposure of Wisconsin drift resting on older drift or other strongly weathered mantle has been found. The old drift and the other strongly weathered materials apparently acquired their present red color in pre-Wisconsin time. Where exposed at the surface, such strongly weathered mantle is the parent material of modern Red-Yellow Podzolic soils. Sols Bruns Acides and Gray-Brown Podzolic soils, developed on slightly weathered parent materials, are found adjacent to these red soils. This suggests that these Red-Yellow Podzolic soils probably developed from strongly weathered parent materials. No buried soils were found nor were any soils recognized as relics from pre-Wisconsin time. Comparison of a map of the great soil groups with a map of the vegetation of the region, prepared by John C. Goodlett, does not reveal a close relation. Laboratory analyses of samples collected furnish data on textural, mineralogical, and chemical changes caused by weathering and soil formation. The results indicate that the amount of chemical weathering which the Wisconsin drift has undergone is slight. The Red-Yellow Podzolic soils on strongly weathered pre-Wisconsin drift have B2 horizons that have a finer texture than the A2 or C horizons. The parent materials of these soils seem to be strongly weathered because of the high chromas, reddish hues, friable condition of most rock fragments, relatively high kaolinite content, and presence of gibbsite in the clay fraction. Measurements at numerous localities show that the depth of leaching increases with decreasing carbonate content and is not a criterion of the age of the drift. Pebble counts of gravels also show that the depth of leaching of gravel is related to its limestone content. The location of the gravel deposits is probably due primarily to the presence of pebbles of resistant rock rather than to ice wastage involving abundant glacial melt water. The region is in the Susquehanna drainage basin except for its north fringe, which drains to Lake Ontario. Most of the region is a dissected plateau ranging in altitude from 700 to 2,500 feet and underlain by gently folded sedimentary rocks of Paleozoic age. Much of the region slopes moderately or steeply; the most extensive areas of gently sloping land are 011 the uplands. In the northern part are several straight and deep valleys the southern extension of the Finger Lakes basins separated by uplands with several low cuestas that face north. Similarly, some streams such as the Canisteo, Cohocton, and Chemung Rivers, and the part of the Susquehanna River that is in New York, trend at right angles to the Finger Lakes, flowing in valleys that parallel the regional strike of the bedrock. The Olean drift border is marked by a change from drift containing very few rounded or striated rock fragments to a mantle containing only angular rock fragments and traces of red, strongly weathered materials. A reconstruction of the surface of the ice sheet, at its maximum extent shows an inferred slope of its distal margin ranging from 100 to 500 feet per mile</p>","language":"English","publisher":"U.S. Government Printing Office","doi":"10.3133/pp379","usgsCitation":"Denny, C.S., Lyford, W.H., and Goodlett, J.C., 1963, Surficial geology and soils of the Elmira-Williamsport region, New York and Pennsylvania, with a section on forest regions and great soil groups: U.S. Geological Survey Professional Paper 379, Report: iv, 59 p.; 6 Plates: 41.94 × 24.00 inches or smaller, https://doi.org/10.3133/pp379.","productDescription":"Report: iv, 59 p.; 6 Plates: 41.94 × 24.00 inches or smaller","costCenters":[{"id":532,"text":"Pennsylvania Water Science Center","active":true,"usgs":true}],"links":[{"id":60663,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0379/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":60662,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0379/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":60661,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0379/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":60660,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0379/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":60659,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0379/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":60664,"rank":405,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0379/plate-6.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":60665,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0379/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":397823,"rank":9,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_4377.htm"},{"id":121752,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0379/report-thumb.jpg"}],"scale":"250000","country":"United States","state":"New York, Pennsylvania","otherGeospatial":"Elmira-Williamsport region","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -77.5,\n              41.1667\n            ],\n            [\n              -76.25,\n              41.1667\n            ],\n            [\n              -76.25,\n              42.5\n            ],\n            [\n              -77.5,\n              42.5\n            ],\n            [\n              -77.5,\n              41.1667\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae2e4b07f02db688b83","contributors":{"authors":[{"text":"Denny, Charles Storrow","contributorId":86331,"corporation":false,"usgs":true,"family":"Denny","given":"Charles","email":"","middleInitial":"Storrow","affiliations":[],"preferred":false,"id":209081,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lyford, Walter Henry","contributorId":43824,"corporation":false,"usgs":true,"family":"Lyford","given":"Walter","email":"","middleInitial":"Henry","affiliations":[],"preferred":false,"id":209080,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Goodlett, J. C.","contributorId":98771,"corporation":false,"usgs":true,"family":"Goodlett","given":"J.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":209082,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":38960,"text":"pp417B - 1963 - Some relations between streamflow characteristics and the environment in the Delaware River region","interactions":[],"lastModifiedDate":"2022-09-16T21:44:23.016232","indexId":"pp417B","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1963","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":"417","chapter":"B","title":"Some relations between streamflow characteristics and the environment in the Delaware River region","docAbstract":"<p>Streamflow characteristics are determined by a large number of factors of the meteorological and terrestrial environments. Because of lack of quantitative data to describe some of the factors and complex interrelations among them, complete analysis of the relations between streamflow and the various environmental factors is impossible. However, certain simplifying assumptions and generalizations made possible a partial analysis for the Delaware River region. For relations involving average runoff or low-flow parameters, average annual precipitation was assumed to be the principal meteorological factor, and geology (a complex of many factors) was assumed to be the principal terrestrial influence, except for that of basin size which was largely eliminated by expression of discharge in terms of unit area. As a first approximation, physiographic units were used as a basis for classifying the geology. Relations between flow parameters and precipitation are fairly well defined for some physiographic units, but not for those in which the geology varies markedly or the areal variation in average precipitation is very small. These relations provide a basis for adjusting the flow parameters to reduce or eliminate the effects of areal variations in precipitation and increase their significance in studies of the effects of terrestrial characteristics. An investigation of the residual effect of basin size (the effect remaining when discharge is expressed in terms of unit area) on relations between flow parameters and average precipitation indicates that such effect is negligible, except for very large differences in area. Parameters that are derived from base-flow recession curves and are related to a common discharge per unit area have inherent advantages as indicators of effects of terrestrial characteristics of basins, because the.y are independent of areal variations in average annual precipitation. Winter base-flow parameters are also practically independent of the effects of evapotranspiration from ground water. However, in many parts of the region these advantages are reduced or nullified by the difficulties of defining base-flow recession curves, particularly winter curves, with sufficient accuracy. In the absence of suitable base-flow recession data and a suitable basis for adjusting parameters, the ratio of the discharge equaled or exceeded 90 percent of the time to the average discharge (Qtt/Qa), or a similar duration parameter, probably is the best indicator of the influence of terrestrial characteristics, although the ratio may vary somewhat with average precipitation. In a part of the region where geologic differences are large and areal variations in average precipitation are small, values of Qm/Qa for each major geologic unit were determined from streamflow records. From these values and the percentage of area represented by each unit, a ratio for each gaging station was computed. Comparison of these computed results with the observed results indicates that nearly all of the variation in the ratio is associated with variation in geology. The investigation indicates that the original assumptions are correct; average precipitation is the principal meteorological influence and geology is the principal terrestrial influence. Together these two factors account for a very large proportion of the variation in average runoff and low-flow characteristics.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/pp417B","usgsCitation":"Hely, A., and Olmsted, F.H., 1963, Some relations between streamflow characteristics and the environment in the Delaware River region: U.S. Geological Survey Professional Paper 417, 25 p., https://doi.org/10.3133/pp417B.","productDescription":"25 p.","costCenters":[{"id":532,"text":"Pennsylvania Water Science Center","active":true,"usgs":true}],"links":[{"id":406893,"rank":5,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_4409.htm","linkFileType":{"id":5,"text":"html"}},{"id":122039,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0417b/report-thumb.jpg"},{"id":66021,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0417b/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":66023,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0417b/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":66022,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0417b/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Delaware, New Jersey, Pennsylvania","otherGeospatial":"Delaware River region","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -76.4083,\n              39.5833\n            ],\n            [\n              -74.4417,\n              39.5833\n            ],\n            [\n              -74.4417,\n              41\n            ],\n            [\n              -76.4083,\n              41\n            ],\n            [\n              -76.4083,\n              39.5833\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e8e4b07f02db5e8cd4","contributors":{"authors":[{"text":"Hely, A. G.","contributorId":14401,"corporation":false,"usgs":true,"family":"Hely","given":"A. G.","affiliations":[],"preferred":false,"id":220728,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Olmsted, F. H.","contributorId":24765,"corporation":false,"usgs":true,"family":"Olmsted","given":"F.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":220729,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":52310,"text":"ofr6317 - 1963 - Water-resources data for Alachua, Bradford, Clay, and Union Counties, Florida","interactions":[{"subject":{"id":52310,"text":"ofr6317 - 1963 - Water-resources data for Alachua, Bradford, Clay, and Union Counties, Florida","indexId":"ofr6317","publicationYear":"1963","noYear":false,"title":"Water-resources data for Alachua, Bradford, Clay, and Union Counties, Florida"},"predicate":"SUPERSEDED_BY","object":{"id":70047481,"text":"70047481 - 1964 - Water-resources data for Alachua, Bradford, Clay, and Union Counties, Florida","indexId":"70047481","publicationYear":"1964","noYear":false,"title":"Water-resources data for Alachua, Bradford, Clay, and Union Counties, Florida"},"id":1}],"supersededBy":{"id":70047481,"text":"70047481 - 1964 - Water-resources data for Alachua, Bradford, Clay, and Union Counties, Florida","indexId":"70047481","publicationYear":"1964","noYear":false,"title":"Water-resources data for Alachua, Bradford, Clay, and Union Counties, Florida"},"lastModifiedDate":"2013-08-07T13:48:17","indexId":"ofr6317","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1963","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":"63-17","title":"Water-resources data for Alachua, Bradford, Clay, and Union Counties, Florida","language":"ENGLISH","publisher":"Geological Survey (U.S.)","doi":"10.3133/ofr6317","usgsCitation":"Clark, W., Musgrove, R., Menke, C., and Cagle, J., 1963, Water-resources data for Alachua, Bradford, Clay, and Union Counties, Florida: U.S. Geological Survey Open-File Report 63-17, 162 p., https://doi.org/10.3133/ofr6317.","productDescription":"162 p.","costCenters":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"links":[{"id":177943,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e2e4b07f02db5e4f82","contributors":{"authors":[{"text":"Clark, W.E.","contributorId":68694,"corporation":false,"usgs":true,"family":"Clark","given":"W.E.","email":"","affiliations":[],"preferred":false,"id":245126,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Musgrove, R.H.","contributorId":31051,"corporation":false,"usgs":true,"family":"Musgrove","given":"R.H.","email":"","affiliations":[],"preferred":false,"id":245124,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Menke, C.G.","contributorId":20823,"corporation":false,"usgs":true,"family":"Menke","given":"C.G.","affiliations":[],"preferred":false,"id":245123,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Cagle, J.W. Jr.","contributorId":63875,"corporation":false,"usgs":true,"family":"Cagle","given":"J.W.","suffix":"Jr.","affiliations":[],"preferred":false,"id":245125,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":6219,"text":"pp422B - 1963 - Hydraulic geometry of a small tidal estuary","interactions":[],"lastModifiedDate":"2017-03-24T16:16:21","indexId":"pp422B","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1963","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":"422","chapter":"B","title":"Hydraulic geometry of a small tidal estuary","docAbstract":"<p>A tidal channel in a marsh bordering the Potomac River near Alexandria, Va., was mapped, and current-meter measurements of discharge were made at various locations and at various stages in the tidal cycle. These measurements allowed analysis of the change of width, depth, and velocity with discharge at various cross sections and along the length of the channel.</p><p>There is also presented a theoretical development of some, of these same relations based on hydraulic principles and on the assumption of a uniform distribution of energy and a minimum rate of work in the system as a whole.</p><p>The change of width, depth, and velocity with discharge downstream developed from the field data checked closely with the theoretically derived values.</p><p>The estuarine channel differs from a terrestrial one in that discharge at any section in an estuary varies depending on how the flow shaped the entire length of the channel between the point in question and the main body of tidal water. The result is that a tidal channel changes more rapidly in width and less rapidly in depth as discharge changes downstream than does a terrestrial channel. </p>","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/pp422B","usgsCitation":"Myrick, R.M., and Leopold, L.B., 1963, Hydraulic geometry of a small tidal estuary: U.S. Geological Survey Professional Paper 422, 19 p., https://doi.org/10.3133/pp422B.","productDescription":"19 p.","startPage":"B1","endPage":"B18","numberOfPages":"22","costCenters":[],"links":[{"id":140192,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0422b/report-thumb.jpg"},{"id":94745,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0422b/report.pdf","size":"2291","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Virginia","city":"Alexandria, VA","otherGeospatial":"Potomac River, Wrecked Recorded Creek","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -77.05480098724365,\n              38.7592035579107\n            ],\n            [\n              -77.04287052154541,\n              38.7592035579107\n            ],\n            [\n              -77.04287052154541,\n              38.77817551784403\n            ],\n            [\n              -77.05480098724365,\n              38.77817551784403\n            ],\n            [\n              -77.05480098724365,\n              38.7592035579107\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a51e4b07f02db62a200","contributors":{"authors":[{"text":"Myrick, Robert M.","contributorId":24345,"corporation":false,"usgs":true,"family":"Myrick","given":"Robert","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":152320,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Leopold, Luna Bergere","contributorId":93884,"corporation":false,"usgs":true,"family":"Leopold","given":"Luna","email":"","middleInitial":"Bergere","affiliations":[],"preferred":false,"id":152321,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":6361,"text":"pp346 - 1963 - The Belt series in Montana, with a geologic map and a section on paleontologic criteria","interactions":[],"lastModifiedDate":"2016-07-27T09:42:42","indexId":"pp346","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1963","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":"346","title":"The Belt series in Montana, with a geologic map and a section on paleontologic criteria","docAbstract":"<p>Problems related to the Belt series have been discussed for nearly a hundred years, but the amount of detailed mapping and other quantitative data available, even now, is not commensurate with the importance of the problem. &nbsp;The present paper is an attempt to summarize existing data in the light of recent fieldwork by the writer and his associates. &nbsp;While the report deals mainly with the rocks in Montana, where the series was first recognized, it necessarily includes consideration of the series in Idaho and parts of Canada as well as of related rocks in more distant areas.</p>","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/pp346","usgsCitation":"Ross, C.P., Skipp, B., and Rezak, R., 1963, The Belt series in Montana, with a geologic map and a section on paleontologic criteria: U.S. Geological Survey Professional Paper 346, Report: v, 122 p.; 6 Plates: 38.23 x 39.21 inches or smaller; Table 9, https://doi.org/10.3133/pp346.","productDescription":"Report: v, 122 p.; 6 Plates: 38.23 x 39.21 inches or smaller; Table 9","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":139502,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/pp346.jpg"},{"id":112813,"rank":406,"type":{"id":27,"text":"Table"},"url":"https://pubs.usgs.gov/pp/0346/plate-table_9.pdf","text":"Table 9","size":"809","linkFileType":{"id":1,"text":"pdf"},"description":"Table 9"},{"id":112812,"rank":405,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0346/plate-3.pdf","text":"Plate 3","size":"2471","linkFileType":{"id":1,"text":"pdf"},"description":"Plate 3"},{"id":325689,"rank":407,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0346/report.pdf","text":"Report","linkFileType":{"id":1,"text":"pdf"}},{"id":112808,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0346/plate-1_nw.pdf","text":"Plate 1 NW","size":"9054","linkFileType":{"id":1,"text":"pdf"},"description":"Plate 1 NW"},{"id":112811,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0346/plate-2.pdf","text":"Plate 2","size":"2606","linkFileType":{"id":1,"text":"pdf"},"description":"Plate 2"},{"id":112807,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0346/plate-1_ne.pdf","text":"Plate 1 NE","size":"5535","linkFileType":{"id":1,"text":"pdf"},"description":"Plate 1 NE"},{"id":112809,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0346/plate-1_se.pdf","text":"Plate 1 SE","size":"7841","linkFileType":{"id":1,"text":"pdf"},"description":"Plate 1 SE"},{"id":112810,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0346/plate-1_sw.pdf","text":"Plate 1 SW","size":"6379","linkFileType":{"id":1,"text":"pdf"},"description":"Plate 1 SW"}],"country":"United States","state":"Montana","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad3e4b07f02db682647","contributors":{"authors":[{"text":"Ross, Clyde Polhemus","contributorId":71954,"corporation":false,"usgs":true,"family":"Ross","given":"Clyde","email":"","middleInitial":"Polhemus","affiliations":[],"preferred":false,"id":152578,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Skipp, B.A.L.","contributorId":26679,"corporation":false,"usgs":true,"family":"Skipp","given":"B.A.L.","email":"","affiliations":[],"preferred":false,"id":152576,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Rezak, Richard","contributorId":48963,"corporation":false,"usgs":true,"family":"Rezak","given":"Richard","email":"","affiliations":[],"preferred":false,"id":152577,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":52335,"text":"ofr6362 - 1963 - The hydrologic laboratory","interactions":[],"lastModifiedDate":"2013-11-08T10:18:36","indexId":"ofr6362","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1963","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":"63-62","title":"The hydrologic laboratory","docAbstract":"The knowledge of soil and rock testing, including the application of the test or analysis data to field problems, is still in its infancy. By learning more about the basic laws and principles of nature we can more accurately predict hydrologic phenomena of the future, as well as solve more efficiently the hydrologic problems of the present Our reservoir of fundamental facts and basic knowledge has been, and can be even more fully, increased by the analysis and research work of the Hydrologic Laboratory.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Denver, CO","doi":"10.3133/ofr6362","usgsCitation":"Johnson, A., 1963, The hydrologic laboratory: U.S. Geological Survey Open-File Report 63-62, iii, 27 p., https://doi.org/10.3133/ofr6362.","productDescription":"iii, 27 p.","numberOfPages":"31","costCenters":[],"links":[{"id":114598,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1963/0062/report.pdf","size":"5791","linkFileType":{"id":1,"text":"pdf"}},{"id":178818,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1963/0062/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b01e4b07f02db69851b","contributors":{"authors":[{"text":"Johnson, A.I.","contributorId":82676,"corporation":false,"usgs":true,"family":"Johnson","given":"A.I.","email":"","affiliations":[],"preferred":false,"id":245180,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
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