{"pageNumber":"6698","pageRowStart":"167425","pageSize":"25","recordCount":184617,"records":[{"id":70046301,"text":"70046301 - 1963 - Geology and ground water resources of Kidder County, North Dakota","interactions":[],"lastModifiedDate":"2024-08-29T16:54:21.876403","indexId":"70046301","displayToPublicDate":"2013-01-01T00:00:00","publicationYear":"1963","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":4,"text":"Other Government Series"},"seriesTitle":{"id":242,"text":"Bulletin","active":false,"publicationSubtype":{"id":4}},"seriesNumber":"36","title":"Geology and ground water resources of Kidder County, North Dakota","docAbstract":"Kidder County was covered with glacial ice at least three times during the Wisconsin Stage of the Pleistocene, but the entire sequence of drifts has not been observed in one exposure. The drift which covers the area was deposited during three ice advances termed the Long Lake, Burnstad and Streeter advances. 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,{"id":70046297,"text":"70046297 - 1963 - Water resources investigations in the Susquehanna River basin","interactions":[{"subject":{"id":44061,"text":"ofr63106 - 1963 - Water-resources investigations and reports in the Susquehanna River basin; conducted by the United States Geological Survey, Water Resources Division","indexId":"ofr63106","publicationYear":"1963","noYear":false,"title":"Water-resources investigations and reports in the Susquehanna River basin; conducted by the United States Geological Survey, Water Resources Division"},"predicate":"SUPERSEDED_BY","object":{"id":70046297,"text":"70046297 - 1963 - Water resources investigations in the Susquehanna River basin","indexId":"70046297","publicationYear":"1963","noYear":false,"title":"Water resources investigations in the Susquehanna River basin"},"id":1}],"lastModifiedDate":"2014-04-09T14:22:16","indexId":"70046297","displayToPublicDate":"2013-01-01T00:00:00","publicationYear":"1963","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":4,"text":"Other Government Series"},"seriesTitle":{"id":291,"text":"Technical Bulletin","active":false,"publicationSubtype":{"id":4}},"seriesNumber":"2","title":"Water resources investigations in the Susquehanna River basin","docAbstract":"No abstract available.","language":"English","publisher":"Pennsylvania Department of Forests and Waters","publisherLocation":"Harrisburg, PA","collaboration":"Conducted by the U.S. Geological Survey Water Resources Division largely in cooperation with state, municipal, and federal agencies","usgsCitation":"Page, L., and Seaber, P.R., 1963, Water resources investigations in the Susquehanna River basin: Technical Bulletin 2, 2 Plates: 33.17 x 27.29 inches and 27.67 x 32.77 inches.","productDescription":"2 Plates: 33.17 x 27.29 inches and 27.67 x 32.77 inches","costCenters":[],"links":[{"id":273326,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/70046297.jpg"},{"id":286046,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/unnumbered/70046297/plate-1.pdf"},{"id":286047,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/unnumbered/70046297/plate-2.pdf"}],"state":"New York;Pennsylvania;Maryl","otherGeospatial":"Susquehanna River Basin","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -79.416924,39.258009 ], [ -79.416924,43.186844 ], [ -74.164678,43.186844 ], [ -74.164678,39.258009 ], [ -79.416924,39.258009 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"51b05df0e4b030b51980135a","contributors":{"authors":[{"text":"Page, Leland V.","contributorId":44217,"corporation":false,"usgs":true,"family":"Page","given":"Leland V.","affiliations":[],"preferred":false,"id":479411,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Seaber, Paul R.","contributorId":67492,"corporation":false,"usgs":true,"family":"Seaber","given":"Paul","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":479412,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70039077,"text":"70039077 - 1963 - Floods of January-February 1963 in California and Nevada","interactions":[],"lastModifiedDate":"2012-07-18T01:01:44","indexId":"70039077","displayToPublicDate":"2012-07-17T00:00:00","publicationYear":"1963","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":"Floods of January-February 1963 in California and Nevada","docAbstract":"Widespread flooding occurred in central California and northwestern Nevada during January 31 - February 1, 1963, as a result of intense precipitation of about 72 hours duration. The flood-producing storm was of the warm type, with precipitation falling as rain at altitudes as high as 8,000 feet. The heavy precipitation, totaling as much as 20 inches or more in the Sierra Nevada, fell on frozen ground or on the sparse snowpack that existed in the higher altitudes. The response of runoff to rainfall was dramatic, as streams throughout the area rose rapidly. Hardest hit were the basins of the American, Yuba, and Truckee Rivers, where flood peaks either reached record-breaking heights or rivalled the discharges attained in the memorable floods of November 1950 and December 1955. Because of the relatively short duration of the storm, the volume of flood flow in 1963 was not outstanding. Ten deaths were attributed to the storm or flood. Preliminary estimates indicate damage in excess of $16 million in foothill and valley areas, but no attempt has yet been made to assess the heavy damage to highways and drainage structures in the mountain areas. The U. S. Army, Corps of Engineirs estimates that its operation of flood-control facilities prevented additional damage of $236 million. Other reservoirs, operated primarily for water conservation or power production, were also instrumental in preventing damage.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Menlo Park, CA","doi":"10.3133/70039077","usgsCitation":"Rantz, S., and Harris, E., 1963, Floods of January-February 1963 in California and Nevada: Open-File Report, iv, 74 p., https://doi.org/10.3133/70039077.","productDescription":"iv, 74 p.","numberOfPages":"79","costCenters":[{"id":630,"text":"Water Resources Division Menlo Park California","active":false,"usgs":true}],"links":[{"id":261296,"rank":800,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/unnumbered/70039077/report.pdf"},{"id":261297,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/unnumbered/70039077/report-thumb.jpg"}],"country":"United States","state":"California;Nevada","city":"Carson City;Fresno;Oakland;Redding;Sacramento;San Francisco","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -124.4,35.25 ], [ -124.4,42 ], [ -116.5,42 ], [ -116.5,35.25 ], [ -124.4,35.25 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a11f7e4b0c8380cd5414c","contributors":{"authors":[{"text":"Rantz, S. E.","contributorId":34106,"corporation":false,"usgs":true,"family":"Rantz","given":"S. E.","affiliations":[],"preferred":false,"id":465586,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Harris, E. E.","contributorId":24328,"corporation":false,"usgs":true,"family":"Harris","given":"E. E.","affiliations":[],"preferred":false,"id":465585,"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":70039573,"text":"70039573 - 1963 - Use of hydrologic models in the analysis of flood runoff","interactions":[],"lastModifiedDate":"2012-08-14T01:01:44","indexId":"70039573","displayToPublicDate":"2012-01-01T16:11:06","publicationYear":"1963","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"seriesTitle":{"id":371,"text":"Monograph","active":false,"publicationSubtype":{"id":6}},"title":"Use of hydrologic models in the analysis of flood runoff","docAbstract":"The analog technique is applied to the analysis of flood runoff. A quasi-linear analog model has been developed for simulating the runoff-producing characteristics of a drainage system. Where storage is linear a unique relationship correlating the inflow and outflow peaks is derived. The technique for synthesizing flood-frequency distribution is also discussed. It is found that a linear-basin system would not modify the type of probability distribution of its inflow, whereas a nonlinear-basin system would.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/70039573","usgsCitation":"Shen, J., 1963, Use of hydrologic models in the analysis of flood runoff: Monograph, vii, 52 p.; ill., https://doi.org/10.3133/70039573.","productDescription":"vii, 52 p.; ill.","numberOfPages":"87","costCenters":[{"id":629,"text":"Water Resources Division","active":false,"usgs":true}],"links":[{"id":261089,"rank":800,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/unnumbered/70039573/report.pdf"},{"id":261090,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/unnumbered/70039573/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bbf28e4b08c986b3299b9","contributors":{"authors":[{"text":"Shen, John","contributorId":34109,"corporation":false,"usgs":true,"family":"Shen","given":"John","email":"","affiliations":[],"preferred":false,"id":466498,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"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":70039489,"text":"70039489 - 1963 - Crustal structure in the vicinity of Las Vegas, Nevada, from seismic and gravity observations","interactions":[],"lastModifiedDate":"2012-08-08T01:02:14","indexId":"70039489","displayToPublicDate":"2012-01-01T15:17:02","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":"12","title":"Crustal structure in the vicinity of Las Vegas, Nevada, from seismic and gravity observations","docAbstract":"A seismic-refraction profile indicates that the crust of the Earth increases in thickness by as much as 5 km over a horizontal distance of less than 25 km northeast of Las Vegas, Nevada. This feature correlates with a decrease in the Bouguer anomaly and an increase in the average surface altitude.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/70039489","collaboration":"In cooperation with the Defense Advanced Research Projects Agency","usgsCitation":"Roller, J.C., 1963, Crustal structure in the vicinity of Las Vegas, Nevada, from seismic and gravity observations: Crustal Studies Technical Letter 12, 10 p.; ill.; map, https://doi.org/10.3133/70039489.","productDescription":"10 p.; ill.; map","startPage":"1","endPage":"10","numberOfPages":"14","onlineOnly":"Y","additionalOnlineFiles":"N","costCenters":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true}],"links":[{"id":259489,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":259484,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/misc/tl/0012/","linkFileType":{"id":5,"text":"html"}},{"id":259485,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/misc/tl/0012/tl0012.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Nevada","city":"Las Vegas","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059fce9e4b0c8380cd4e4e8","contributors":{"authors":[{"text":"Roller, John C.","contributorId":60642,"corporation":false,"usgs":true,"family":"Roller","given":"John","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":466356,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70039074,"text":"70039074 - 1963 - Rockford, Illinois; Wisconsin","interactions":[],"lastModifiedDate":"2012-08-10T01:01:51","indexId":"70039074","displayToPublicDate":"2012-01-01T14:59:21","publicationYear":"1963","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"subseriesTitle":"Eastern United States 1:250,000, NK 16-4","title":"Rockford, Illinois; Wisconsin","docAbstract":"Topographic map of the Rockford, Illinois area and adjacent Wisconsin area.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Washington, D.C.","doi":"10.3133/70039074","usgsCitation":"U.S. Army Map Service, 1963, Rockford, Illinois; Wisconsin, 1 Plate: col. 74 x 56 cm., https://doi.org/10.3133/70039074.","productDescription":"1 Plate: col. 74 x 56 cm.","costCenters":[],"links":[{"id":258971,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":261295,"rank":900,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/unnumbered/70039074/plate-1.pdf"}],"scale":"250000","projection":"Transverse Mercator Projection","country":"United States","state":"Illinois;Wisconsin","city":"Beloit;Freeport;Janesville;Rockford","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -90,42 ], [ -90,43 ], [ -88,43 ], [ -88,42 ], [ -90,42 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505aae12e4b0c8380cd8700a","contributors":{"authors":[{"text":"U.S. Army Map Service","contributorId":128088,"corporation":true,"usgs":false,"organization":"U.S. Army Map Service","id":535215,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70039488,"text":"70039488 - 1963 - Crustal structure from San Francisco, California, to Eureka, Nevada, from seismic-refraction measurements","interactions":[],"lastModifiedDate":"2012-08-08T01:02:14","indexId":"70039488","displayToPublicDate":"2012-01-01T14:57:35","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":"11","title":"Crustal structure from San Francisco, California, to Eureka, Nevada, from seismic-refraction measurements","docAbstract":"Seismic-refraction measurements from chemical explosions near San Francisco, California, and Fallon and Eureka, Nevada, were made along a line extending nearly 700 km inland from San Francisco across the Coast Ranges, Great Valley, Sierra Nevada, and Basin and Range Province. The velocity of P<sub>g</sub> in the Basin and Range Province was found to be 6.0 km/sec. Between Fallon and Eureka the velocity of P<sub>n</sub> is 7.8 km/sec, and just east of the Sierra Nevada it is about 7.9 km/sec. Two prominent phases closely following the first arrival between 50 and 250 km from the source in the Basin and Range Province were interpreted as reflections from an intermediate layer and from the Mohorovicic discontinuity. The velocity of P in the possible intermediate layer, deduced from the reflected phases be cause the refracted wave expected from this layer is nowhere a first arrival, seems to be 6.6 km/sec at the top of the layer and probably increases with depth.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/70039488","collaboration":"In cooperation with the Defense Advanced Research Projects Agency","usgsCitation":"Eaton, J.P., 1963, Crustal structure from San Francisco, California, to Eureka, Nevada, from seismic-refraction measurements: Crustal Studies Technical Letter 11, 55 p.; ill.; map, https://doi.org/10.3133/70039488.","productDescription":"55 p.; ill.; map","startPage":"1","endPage":"55","numberOfPages":"59","onlineOnly":"Y","additionalOnlineFiles":"N","costCenters":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true}],"links":[{"id":259492,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":259482,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/misc/tl/0011/tl0011.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":259483,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/misc/tl/0011/","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"California;Nevada","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059fce8e4b0c8380cd4e4df","contributors":{"authors":[{"text":"Eaton, Jerry P.","contributorId":22341,"corporation":false,"usgs":true,"family":"Eaton","given":"Jerry","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":466355,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70040443,"text":"70040443 - 1963 - The ground-water resources of Delaware County, New York","interactions":[],"lastModifiedDate":"2012-10-19T17:16:26","indexId":"70040443","displayToPublicDate":"2012-01-01T14:49:16","publicationYear":"1963","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":4,"text":"Other Government Series"},"seriesTitle":{"id":242,"text":"Bulletin","active":false,"publicationSubtype":{"id":4}},"seriesNumber":"GW-50","title":"The ground-water resources of Delaware County, New York","language":"English","publisher":"New York State Water Resources Commission","publisherLocation":"Albany, NY","usgsCitation":"Soren, J., 1963, The ground-water resources of Delaware County, New York: Bulletin GW-50, 59 p., 2 Plates.","productDescription":"59 p., 2 Plates","numberOfPages":"59","costCenters":[{"id":474,"text":"New York Water Science Center","active":true,"usgs":true}],"links":[{"id":262738,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"New York","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -79.760000,40.480000 ], [ -79.760000,45.020000 ], [ -71.860000,45.020000 ], [ -71.860000,40.480000 ], [ -79.760000,40.480000 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"50e5072ce4b0e8fec6ce9ef4","contributors":{"authors":[{"text":"Soren, Julian","contributorId":54184,"corporation":false,"usgs":true,"family":"Soren","given":"Julian","email":"","affiliations":[],"preferred":false,"id":468336,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70040442,"text":"70040442 - 1963 - Ground-water studies in Saratoga County, New York","interactions":[],"lastModifiedDate":"2012-10-19T17:16:26","indexId":"70040442","displayToPublicDate":"2012-01-01T14:41:17","publicationYear":"1963","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":4,"text":"Other Government Series"},"seriesTitle":{"id":242,"text":"Bulletin","active":false,"publicationSubtype":{"id":4}},"seriesNumber":"GW-49","title":"Ground-water studies in Saratoga County, New York","language":"English","publisher":"New York State Water Resources Commission","publisherLocation":"Albany, NY","usgsCitation":"Heath, R., Mack, F.K., and Tannenbaum, J., 1963, Ground-water studies in Saratoga County, New York: Bulletin GW-49, 128 p., 4 Plates.","productDescription":"128 p., 4 Plates","numberOfPages":"128","costCenters":[{"id":474,"text":"New York Water Science Center","active":true,"usgs":true}],"links":[{"id":262735,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"New York","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -79.760000,40.480000 ], [ -79.760000,45.020000 ], [ -71.860000,45.020000 ], [ -71.860000,40.480000 ], [ -79.760000,40.480000 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"50de6548e4b0e31bb02a1dad","contributors":{"authors":[{"text":"Heath, R.C.","contributorId":49408,"corporation":false,"usgs":true,"family":"Heath","given":"R.C.","email":"","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":468334,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Mack, F. K.","contributorId":93471,"corporation":false,"usgs":true,"family":"Mack","given":"F.","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":468335,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Tannenbaum, J.A.","contributorId":47624,"corporation":false,"usgs":true,"family":"Tannenbaum","given":"J.A.","email":"","affiliations":[],"preferred":false,"id":468333,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70039486,"text":"70039486 - 1963 - Traveltimes and amplitudes from nuclear explosions; Nevada Test Site to Ordway, Colorado","interactions":[],"lastModifiedDate":"2012-08-08T01:02:14","indexId":"70039486","displayToPublicDate":"2012-01-01T14:27:14","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":"10","title":"Traveltimes and amplitudes from nuclear explosions; Nevada Test Site to Ordway, Colorado","docAbstract":"This paper treats the results of a study of seismic waves generated by eight nuclear explosions and recorded at 31 locations between the Nevada Test Site (NTS) and Ordway, Colorado. The line of recording stations crosses the eastern part of the Basin and Range Province, the Colorado Plateau, the southern Rocky Mountains, and extends into the Great Plains. In the eastern Basin and Range Province and the western margin of the Colorado Plateau (0 &le; &Delta; &le; 385 km ), the time-distance curves for P<sub>g</sub> and P<sub>n</sub> can be expressed, respectively, as T<sub>1</sub> = 0.8 + &Delta;/6.0. T<sub>3</sub> = 5.8 + &Delta;/7.6. A third phase, tentatively identified as P*, is represented by the equation T2 = 3.8 + &Delta;/6.5. Using the crustal structure and P<sub>n</sub> velocity (7.9 km/ sec) found for the NTS region by other authors, these relations indicate that the thickness of the crust increases from about 25 km at NTS to about 42 km in the western part of the Colorado Plateau Province. East of this boundary the velocity of P in the upper mantle increases to 8.0 km/sec; depth to the Mohorovicic discontinuity is approximately constant over the range 435 &le; &Delta; &le; 645 km. Beyond 850 km, first arrivals indicate an apparent velocity of about 8.4 km/sec. Amplitudes of P<sub>n</sub> attenuate according to the equation A = A<sub>o</sub> &Delta;<sup>-1/2</sup>(&Delta; -d)<sup>-3/2</sup> e<sup>-0.0022&Delta;</sup> over the distance range 150 &le; &Delta; &le; 850 km. This relation yields a value of Q, for P<sub>n</sub> of about 520. The amplitudes of P<sub>g</sub> attenuates extremely rapidly, and beyond about 130 km this phase cannot be identified with certainty. An extension of the P<sub>g</sub> traveltime branch at large distances could be associated with waves reflected beyond the critical angle, from the base of the crust. This phase, called  ?P after Mohorovicic, appears to attenuate as A = Ao e<sup>-0.076&Delta;</sup> &Delta;<sup>-1/2</sup>. The value of Q indicated by this equation is about 200.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/70039486","collaboration":"In cooperation with the Defense Advanced Research Projects Agency","usgsCitation":"Ryall, A., and Stuart, D., 1963, Traveltimes and amplitudes from nuclear explosions; Nevada Test Site to Ordway, Colorado: Crustal Studies Technical Letter 10, ill.; map, https://doi.org/10.3133/70039486.","productDescription":"ill.; map","startPage":"1","endPage":"41","numberOfPages":"45","onlineOnly":"Y","additionalOnlineFiles":"N","costCenters":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true}],"links":[{"id":259490,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":259481,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/misc/tl/0010/tl0010.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":259480,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/misc/tl/0010/","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Nevada;Colorado","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bb78ae4b08c986b327327","contributors":{"authors":[{"text":"Ryall, Alan","contributorId":16263,"corporation":false,"usgs":true,"family":"Ryall","given":"Alan","email":"","affiliations":[],"preferred":false,"id":466351,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Stuart, David J.","contributorId":25807,"corporation":false,"usgs":true,"family":"Stuart","given":"David J.","affiliations":[],"preferred":false,"id":466352,"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":70039282,"text":"70039282 - 1963 - Structure of the crust and upper mantle in the western United States","interactions":[],"lastModifiedDate":"2012-08-01T01:01:41","indexId":"70039282","displayToPublicDate":"2012-01-01T13:34:17","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":"8","title":"Structure of the crust and upper mantle in the western United States","docAbstract":"Seismic waves generated by underground nuclear and chemical explosions have been recorded in a network of nearly 2,000 stations in the western conterminous United States as a part of the VELA UNIFORM program. The network extends from eastern Colorado to the California coastline and from central Idaho to the border of the United States and Mexico. The speed of compressional waves in the upper-mantle rocks ranges from 7.7 km/sec in the southern part of the Basin and Range province to 8.2 km/sec in the Great Plains province. In general, the speed of compressional waves in the upper-mantle rocks tends to be nearly the same over large areas within individual geologic provinces. Measured crustal thickness ranges from less than 20 km in the Central Valley of California to 50 km in the Great Plains province. Changes in crustal thickness across provincial boundaries are not controlled by regional altitude above sea level unless the properties of the upper mantle are the same across those boundaries. The crust tends to be thick in regions where the speed of compressional waves in the upper-mantle rocks (and presumably the density) is high, and tends to be relatively thin where the speed of compressional waves in the upper-mantle rocks (and density) is lower. With in the Basin and Range province, crustal thickness seems to vary directly with regional altitude above sea level. Evidence that a layer of intermediate compressional-wave speed exists in the lower part of the crust has been accumulated from seismic waves that have traveled least-time paths, as well as secondary arrivals (particularly reflections). On a scale that includes many geologic provinces, isostatic compensation is related largely to variations in the density of the upper- mantle rocks. Within geologic provinces or adjacent provinces, isostatic compensation may be related to variations in the thickness of crustal layers. Regions of thick crust and dense upper mantle have been relatively stable in Cenozoic time. Regions of thinner crust and low-density upper mantle have had a Cenozoic history of intense diastrophism and silicic volcanism.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/70039282","collaboration":"In cooperation with the Defense Advanced Research Projects Agency","usgsCitation":"Pakiser, L.C., 1963, Structure of the crust and upper mantle in the western United States: Crustal Studies Technical Letter 8, 33 p.; ill.; maps, https://doi.org/10.3133/70039282.","productDescription":"33 p.; ill.; maps","startPage":"1","endPage":"33","numberOfPages":"37","onlineOnly":"Y","additionalOnlineFiles":"N","costCenters":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true}],"links":[{"id":259334,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":259313,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/misc/tl/0008/","linkFileType":{"id":5,"text":"html"}},{"id":259314,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/misc/tl/0008/tl0008.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505b9c63e4b08c986b31d3dc","contributors":{"authors":[{"text":"Pakiser, L. C.","contributorId":83512,"corporation":false,"usgs":true,"family":"Pakiser","given":"L.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":465955,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70039280,"text":"70039280 - 1963 - Seismic-refraction measurements of crustal structure between Santa Monica Bay and Lake Mead","interactions":[],"lastModifiedDate":"2012-08-01T01:01:41","indexId":"70039280","displayToPublicDate":"2012-01-01T12:36:37","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":"7","title":"Seismic-refraction measurements of crustal structure between Santa Monica Bay and Lake Mead","docAbstract":"A reversed seismic-refraction profile was recorded between Santa Monica Bay, California, and Lake Mead, Nevada, during November 1961. Depth to the Mohorovicic discontinuity was determined to be approximately 29 km at Santa Monica Bay, 36 km under the Transverse Ranges, 26 km under the Mojave Desert, and 30 km at Lake Mead. Prominent events on the seismograms in the distance range 30 to 150 km are interpreted as reflections from the Mohorovicic discontinuity and from a crustal layer of intermediate velocity. These reflected events are used to make a detailed interpretation of crustal structure. The velocity of compressional waves in the mantle immediately below the Mohorovicic discontinuity was determined to be 7.8 km/sec. The velocity of compressional waves in the intermediate layer is near 7.0 km/sec. The apparent velocity of the direct arrival in the crustal rocks near the surface is 6.l km/sec north-east of Santa Monica Bay, and 6.1 km/sec southwest of Lake Mead. The higher apparent velocity for the direct arrival from Santa Monica Bay seems to be the result of thinning toward the east of low-velocity rocks near the surface. These low-velocity near-surface rocks are Cenozoic sedimentary rocks and fractured and weathered granitic and metamorphic rocks. The velocity of Sg was determined to be 3.4. km/sec near Lake Mead. A prominent phase with apparent velocity of 6.3 to 6.4 km/sec was recorded at distances beyond 200 km. This phase is identified as P and is interpreted as a reflection from the intermediate layer. Amplitude measurements support the conclusion that the P phase is a reflected arrival.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/70039280","collaboration":"In cooperation with the Defense Advanced Research Projects Agency","usgsCitation":"Roller, J.C., and Healy, J., 1963, Seismic-refraction measurements of crustal structure between Santa Monica Bay and Lake Mead: Crustal Studies Technical Letter 7, 37 p.; ill.; map, https://doi.org/10.3133/70039280.","productDescription":"37 p.; ill.; map","startPage":"1","endPage":"37","numberOfPages":"41","onlineOnly":"Y","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":259303,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/misc/tl/0007/","linkFileType":{"id":5,"text":"html"}},{"id":259304,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/misc/tl/0007/tl0007.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":259310,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"country":"United States","state":"California;Nevada","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505b8b85e4b08c986b3178c5","contributors":{"authors":[{"text":"Roller, John C.","contributorId":60642,"corporation":false,"usgs":true,"family":"Roller","given":"John","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":465952,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Healy, John H.","contributorId":19562,"corporation":false,"usgs":true,"family":"Healy","given":"John H.","affiliations":[],"preferred":false,"id":465951,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"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":70039538,"text":"70039538 - 1963 - A progress report on seismic model studies","interactions":[],"lastModifiedDate":"2013-01-15T11:22:54","indexId":"70039538","displayToPublicDate":"2012-01-01T00:00:00","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":"15","title":"A progress report on seismic model studies","docAbstract":"The value of seismic-model studies as an aid to understanding wave propagation in the Earth's crust was recognized by early investigators (Tatel and Tuve, 1955). Preliminary model results were very promising, but progress in model seismology has been restricted by two problems: (1) difficulties in the development of models with continuously variable velocity-depth functions, and (2) difficulties in the construction of models of adequate size to provide a meaningful wave-length to layer-thickness ratio. The problem of a continuously variable velocity-depth function has been partly solved by a technique using two-dimensional plate models constructed by laminating plastic to aluminum, so that the ratio of plastic to aluminum controls the velocity-depth function (Healy and Press, 1960). These techniques provide a continuously variable velocity-depth function, but it is not possible to construct such models large enough to study short-period wave propagation in the crust. This report describes improvements in our ability to machine large models. Two types of models are being used: one is a cylindrical aluminum tube machined on a lathe, and the other is a large plate machined on a precision planer. Both of these modeling techniques give promising results and are a significant improvement over earlier efforts.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Denver, CO","doi":"10.3133/70039538","collaboration":"In cooperation with the Defense Advanced Research Projects Agency","usgsCitation":"Healy, J.H., and Mangan, G.B., 1963, A progress report on seismic model studies: Crustal Studies Technical Letter 15, iv, 8 p., https://doi.org/10.3133/70039538.","productDescription":"iv, 8 p.","numberOfPages":"12","onlineOnly":"Y","costCenters":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true}],"links":[{"id":259557,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/misc/tl/0015/tl0015.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":259554,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/misc/tl/0015/","linkFileType":{"id":5,"text":"html"}},{"id":259569,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059e511e4b0c8380cd46ae4","contributors":{"authors":[{"text":"Healy, J. H.","contributorId":48968,"corporation":false,"usgs":true,"family":"Healy","given":"J.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":466442,"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":466443,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"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":37749,"text":"wl457 - 1963 - 1963 Address list of refuge managers.","interactions":[],"lastModifiedDate":"2012-02-02T00:16:00","indexId":"wl457","displayToPublicDate":"2011-12-27T00:00:00","publicationYear":"1963","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":98,"text":"Wildlife Leaflet","active":false,"publicationSubtype":{"id":1}},"seriesNumber":"457","title":"1963 Address list of refuge managers.","language":"ENGLISH","publisher":"U.S. Fish and Wildlife Service","usgsCitation":"Branch Of Wildlife Refuges., 1963, 1963 Address list of refuge managers.: Wildlife Leaflet 457, 11 p.","productDescription":"11 p.","costCenters":[],"links":[{"id":112349,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://hdl.handle.net/2027/mdp.39015007539110?urlappend=%3Bseq=17"},{"id":204171,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53cd4910e4b0b290850eed93","contributors":{"authors":[{"text":"Branch Of Wildlife Refuges.","contributorId":128062,"corporation":true,"usgs":false,"organization":"Branch Of Wildlife Refuges.","id":529699,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":5220154,"text":"5220154 - 1963 - Relation of screening to field testing in development of plant control methods","interactions":[],"lastModifiedDate":"2012-02-02T00:14:38","indexId":"5220154","displayToPublicDate":"2010-06-16T12:17:33","publicationYear":"1963","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3171,"text":"Proceedings of the Northeastern Weed Control Conference","active":true,"publicationSubtype":{"id":10}},"title":"Relation of screening to field testing in development of plant control methods","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Proceedings of the Northeastern Weed Control Conference","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","usgsCitation":"Steenis, J., 1963, Relation of screening to field testing in development of plant control methods: Proceedings of the Northeastern Weed Control Conference, v. 17, p. 439-442.","productDescription":"439-442","startPage":"439","endPage":"442","numberOfPages":"4","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":193636,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"17","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a7ee4b07f02db648577","contributors":{"authors":[{"text":"Steenis, J.H.","contributorId":73694,"corporation":false,"usgs":true,"family":"Steenis","given":"J.H.","email":"","affiliations":[],"preferred":false,"id":331417,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":5220122,"text":"5220122 - 1963 - Abnormalities among brown-headed cowbirds trapped in Alabama","interactions":[],"lastModifiedDate":"2023-11-04T00:22:22.354143","indexId":"5220122","displayToPublicDate":"2010-06-16T12:17:33","publicationYear":"1963","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1054,"text":"Bird-Banding","active":true,"publicationSubtype":{"id":10}},"title":"Abnormalities among brown-headed cowbirds trapped in Alabama","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"Association of Field Ornithologists","doi":"10.2307/4511029","usgsCitation":"Stewart, P., 1963, Abnormalities among brown-headed cowbirds trapped in Alabama: Bird-Banding, v. 34, no. 4, p. 199-202, https://doi.org/10.2307/4511029.","productDescription":"4 p.","startPage":"199","endPage":"202","numberOfPages":"4","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":502560,"rank":2,"type":{"id":41,"text":"Open Access External Repository Page"},"url":"https://digitalcommons.usf.edu/bird_banding/vol34/iss4/3","text":"External Repository"},{"id":193668,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"34","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b13e4b07f02db6a39ff","contributors":{"authors":[{"text":"Stewart, P.A.","contributorId":12133,"corporation":false,"usgs":true,"family":"Stewart","given":"P.A.","email":"","affiliations":[],"preferred":false,"id":331374,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":5221291,"text":"5221291 - 1963 - Fish and wildlife aspects of chemical mosquito control","interactions":[],"lastModifiedDate":"2017-09-19T11:43:36","indexId":"5221291","displayToPublicDate":"2010-06-16T12:17:33","publicationYear":"1963","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3145,"text":"Proceedings of the Annual Meeting of the New Jersey Mosquito Extermination Association","active":true,"publicationSubtype":{"id":10}},"title":"Fish and wildlife aspects of chemical mosquito control","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"New Jersey Mosquito Extermination Association","usgsCitation":"Springer, P.F., 1963, Fish and wildlife aspects of chemical mosquito control: Proceedings of the Annual Meeting of the New Jersey Mosquito Extermination Association, v. 50, p. 194-203.","productDescription":"194-203","startPage":"194","endPage":"203","numberOfPages":"10","costCenters":[{"id":480,"text":"Northern Prairie Wildlife Research Center","active":true,"usgs":true},{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":197194,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"50","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f9e4b07f02db5f30ca","contributors":{"authors":[{"text":"Springer, P. F.","contributorId":56590,"corporation":false,"usgs":false,"family":"Springer","given":"P.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":333505,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
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