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1964 - Chemistry and movement of ground water, Nevada test site","interactions":[],"lastModifiedDate":"2014-07-16T14:08:36","indexId":"tei838","displayToPublicDate":"2013-07-16T14:06:00","publicationYear":"1964","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":"838","title":"Chemistry and movement of ground water, Nevada test site","docAbstract":"No abstract available.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Washington, D.C.","doi":"10.3133/tei838","collaboration":"Work done on behalf of the U.S. Atomic Energy Commission.","usgsCitation":"Schoff, S.L., and Moore, J.E., 1964, Chemistry and movement of ground water, Nevada test site: U.S. Geological Survey Trace Elements Investigations 838, Report: 75 p.; 1 Map, https://doi.org/10.3133/tei838.","productDescription":"Report: 75 p.; 1 Map","costCenters":[],"links":[{"id":290303,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"country":"United States","state":"Nevada","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -120.01,35.0 ], [ -120.01,42.0 ], [ -114.04,42.0 ], [ -114.04,35.0 ], [ -120.01,35.0 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53c79ee6e4b0194841642421","contributors":{"authors":[{"text":"Schoff, Stuart Leeson","contributorId":57951,"corporation":false,"usgs":true,"family":"Schoff","given":"Stuart","email":"","middleInitial":"Leeson","affiliations":[],"preferred":false,"id":284757,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Moore, John Ezra","contributorId":93582,"corporation":false,"usgs":true,"family":"Moore","given":"John","email":"","middleInitial":"Ezra","affiliations":[],"preferred":false,"id":284758,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":71779,"text":"tei826 - 1964 - Geologic map of the Paiute Ridge quadrangle, Nye and Lincoln counties, Nevada","interactions":[],"lastModifiedDate":"2014-07-16T13:08:53","indexId":"tei826","displayToPublicDate":"2013-07-16T13:03:00","publicationYear":"1964","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":"826","title":"Geologic map of the Paiute Ridge quadrangle, Nye and Lincoln counties, Nevada","docAbstract":"No abstract available.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Washington, D.C.","doi":"10.3133/tei826","collaboration":"Work done on behalf of the U.S. Atomic Energy Commission.","usgsCitation":"Byers, F.M., and Barnes, H., 1964, Geologic map of the Paiute Ridge quadrangle, Nye and Lincoln counties, Nevada: U.S. Geological Survey Trace Elements Investigations 826, Report: 4 p.; 1 Map, https://doi.org/10.3133/tei826.","productDescription":"Report: 4 p.; 1 Map","costCenters":[],"links":[{"id":290289,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"country":"United States","state":"Nevada","county":"Lincoln County;Nye County","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -118.2,35.96 ], [ -118.2,39.16 ], [ -114.05,39.16 ], [ -114.05,35.96 ], [ -118.2,35.96 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53c79ef0e4b0194841642440","contributors":{"authors":[{"text":"Byers, Frank M.","contributorId":58571,"corporation":false,"usgs":true,"family":"Byers","given":"Frank","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":284741,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Barnes, Harley","contributorId":63019,"corporation":false,"usgs":true,"family":"Barnes","given":"Harley","email":"","affiliations":[],"preferred":false,"id":284742,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70043707,"text":"70043707 - 1964 - A preliminary summary of a seismic-refraction survey in the vicinity of the Tonto Forest Observatory, Arizona","interactions":[],"lastModifiedDate":"2013-02-19T10:34:04","indexId":"70043707","displayToPublicDate":"2013-02-18T00:00:00","publicationYear":"1964","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":"23","title":"A preliminary summary of a seismic-refraction survey in the vicinity of the Tonto Forest Observatory, Arizona","docAbstract":"The U.S. Geological Survey complete d a seismic-refraction survey in the vicinity of the Tonto Forest Seismological Observatory (T.F.S.O.) in April and May 1964. More than 1200 km of reversed profiles were surveyed to determine the crustal structure and crustal and upper mantle velocities in this area. The purpose of this work was to provide information on wave-propagation paths of seismic events recorded at T.F.S.O. and to improve the performance of the Observatory in locating and identifying these events. First arrivals indicate that the Mohorovicic discontinuity dips to the northeast by as much as 6 degrees under T.F.S.O., and may even be displaced vertically by as much as 5 km immediately north of the Observatory near the boundary of the Basin and Range a n d t he Colorado Plateau Provinces. A preliminary examination of the first arrivals indicates that the crust at T.F.S.O. is at least 30 km thick and is made up of at least two seismic layers. A thin veneer at the surface with a velocity of approximately 4 km/sec is underlain by a layer with a velocity of approximately 5.9 km/sec to 6.1 km/sec. An intermediate layer with velocity of 6.6 to 7.0 km/sec is probably present in the lower crust, but is not revealed by first arrivals. The velocity of seismic waves in the upper mantle is about 7.9 km/sec.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/70043707","collaboration":"In cooperation with the Defense Advanced Research Projects Agency","usgsCitation":"Roller, J., Jackson, W.H., Warren, D.H., and Healy, J.H., 1964, A preliminary summary of a seismic-refraction survey in the vicinity of the Tonto Forest Observatory, Arizona: Crustal Studies Technical Letter 23, 57 p., https://doi.org/10.3133/70043707.","productDescription":"57 p.","numberOfPages":"61","onlineOnly":"Y","costCenters":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true},{"id":379,"text":"Menlo Park Science Center","active":false,"usgs":true}],"links":[{"id":267664,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":267661,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/misc/tl/0023/"},{"id":267662,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/misc/tl/0023/tl0023.pdf"}],"country":"United States","state":"Arizona","otherGeospatial":"Tonto Forest Observatory","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -0.01638888888888889,8.333333333333334E-4 ], [ -0.01638888888888889,8.333333333333334E-4 ], [ -0.016666666666666666,8.333333333333334E-4 ], [ -0.016666666666666666,8.333333333333334E-4 ], [ -0.01638888888888889,8.333333333333334E-4 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5124acf4e4b0b6328103b327","contributors":{"authors":[{"text":"Roller, J.C.","contributorId":12507,"corporation":false,"usgs":true,"family":"Roller","given":"J.C.","email":"","affiliations":[],"preferred":false,"id":474130,"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":474131,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Warren, D. H.","contributorId":101327,"corporation":false,"usgs":true,"family":"Warren","given":"D.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":474133,"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":474132,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":70043606,"text":"70043606 - 1964 - Seismic-refraction measurements of crustal structure between American Falls Reservoir, Idaho, and Flaming Gorge Reservoir, Utah","interactions":[],"lastModifiedDate":"2013-02-15T10:07:09","indexId":"70043606","displayToPublicDate":"2013-02-13T00:00:00","publicationYear":"1964","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":"21","title":"Seismic-refraction measurements of crustal structure between American Falls Reservoir, Idaho, and Flaming Gorge Reservoir, Utah","docAbstract":"Interpretation of a reversed seismic-refraction profile recorded between American Falls reservoir and Flaming Gorge reservoir in May 1963 indicates that the depth to the Mohorovicic discontinuity is about 31 km at American Falls and 37 km at Flaming Gorge. The existence of an intermediate crustal layer at a depth of about 19 to 21 km beneath the profile is well supported by refractions and reflections. The velocity of compressional waves in the mantle just beneath the Mohorovicic discontinuity is about 7.8 km/sec, their velocity in the intermediate layer is about 6.9 km/sec, and their velocity in the upper crust (beneath the near-surface low-velocity material) is about 5.9 km/sec. A prominent phase with an apparent velocity of 8.4 km/sec was recorded at distances of 210 km to 325 km from shots at American Falls. This phase is believed to be a reflection from a boundary within the mantle.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/70043606","collaboration":"In cooperation with the Defense Advanced Research Projects Agency","usgsCitation":"Willden, R., 1964, Seismic-refraction measurements of crustal structure between American Falls Reservoir, Idaho, and Flaming Gorge Reservoir, Utah: Crustal Studies Technical Letter 21, 37 p., https://doi.org/10.3133/70043606.","productDescription":"37 p.","numberOfPages":"41","onlineOnly":"Y","costCenters":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true},{"id":379,"text":"Menlo Park Science Center","active":false,"usgs":true}],"links":[{"id":267545,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":267543,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/misc/tl/0021/"},{"id":267544,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/misc/tl/0021/tl0021.pdf"}],"country":"United States","state":"Idaho;Utah","otherGeospatial":"American Falls Reservoir;Flaming Gorge Reservoir","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -112.87,40.65 ], [ -112.87,42.8 ], [ -109.05,42.8 ], [ -109.05,40.65 ], [ -112.87,40.65 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"511f673ce4b03b29402c5e7b","contributors":{"authors":[{"text":"Willden, Ronald","contributorId":107368,"corporation":false,"usgs":true,"family":"Willden","given":"Ronald","affiliations":[],"preferred":false,"id":473966,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70043613,"text":"70043613 - 1964 - Crustal structure between Lake Mead, Nevada, and Mono Lake, California","interactions":[],"lastModifiedDate":"2013-02-15T10:17:42","indexId":"70043613","displayToPublicDate":"2013-02-13T00:00:00","publicationYear":"1964","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":"22","title":"Crustal structure between Lake Mead, Nevada, and Mono Lake, California","docAbstract":"Interpretation of a reversed seismic-refraction profile between Lake Mead, Nevada, and Mono Lake, California, indicates velocities of 6.15 km/sec for the upper layer of the crust, 7.10 km/sec for an intermediate layer, and 7.80 km/sec for the uppermost mantle. Phases interpreted to be reflections from the top of the intermediate layer and the Mohorovicic discontinuity were used with the refraction data to calculate depths. The depth to the Moho increases from about 30 km near Lake Mead to about 40 km near Mono Lake. Variations in arrival times provide evidence for fairly sharp flexures in the Moho. Offsets in the Moho of 4 km at one point and 2 1/2 km at another correspond to large faults at the surface, and it is suggested that fracture zones in the upper crust may displace the Moho and extend into the upper mantle. The phase P appears to be an extension of the reflection from the top of the intermediate layer beyond the critical angle. Bouguer gravity, computed for the seismic model of the crust, is in good agreement with the measured Bouguer gravity. Thus a model of the crustal structure is presented which is consistent with three semi-independent sources of geophysical data: seismic-refraction, seismic-reflection, and gravity.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/70043613","collaboration":"In cooperation with the Defense Advanced Research Projects Agency","usgsCitation":"Johnson, L.R., 1964, Crustal structure between Lake Mead, Nevada, and Mono Lake, California: Crustal Studies Technical Letter 22, 21 p., https://doi.org/10.3133/70043613.","productDescription":"21 p.","numberOfPages":"25","onlineOnly":"Y","costCenters":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true},{"id":379,"text":"Menlo Park Science Center","active":false,"usgs":true}],"links":[{"id":267548,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":267546,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/misc/tl/0022/"},{"id":267547,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/misc/tl/0022/tl0022.pdf"}],"country":"United States","state":"California;Nevada","otherGeospatial":"Lake Mead;Mono Lake","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -0.01611111111111111,8.333333333333334E-4 ], [ -0.01611111111111111,8.333333333333334E-4 ], [ -0.01638888888888889,8.333333333333334E-4 ], [ -0.01638888888888889,8.333333333333334E-4 ], [ -0.01611111111111111,8.333333333333334E-4 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"511f670fe4b03b29402c5dbc","contributors":{"authors":[{"text":"Johnson, Lane R.","contributorId":19049,"corporation":false,"usgs":true,"family":"Johnson","given":"Lane","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":473970,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70047668,"text":"70047668 - 1964 - Ground-water resources of Block Island, Rhode Island","interactions":[{"subject":{"id":42579,"text":"ofr6340 - 1963 - Preliminary map of Block Island, Rhode Island, showing availability of ground water","indexId":"ofr6340","publicationYear":"1963","noYear":false,"title":"Preliminary map of Block Island, Rhode Island, showing availability of ground water"},"predicate":"SUPERSEDED_BY","object":{"id":70047668,"text":"70047668 - 1964 - Ground-water resources of Block Island, Rhode Island","indexId":"70047668","publicationYear":"1964","noYear":false,"title":"Ground-water resources of Block Island, Rhode Island"},"id":1}],"lastModifiedDate":"2013-08-16T16:08:58","indexId":"70047668","displayToPublicDate":"2013-01-01T16:02:00","publicationYear":"1964","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":113,"text":"Geological Bulletin","active":false,"publicationSubtype":{"id":2}},"seriesNumber":"14","title":"Ground-water resources of Block Island, Rhode Island","language":"English","publisher":"Rhode Island Water Resources Coordinating Board","publisherLocation":"Providence, RI","collaboration":"Prepared by the U.S. Geological Survey in cooperation with the Rhode Island Water Resources Coordinating Board","usgsCitation":"Hansen, A., and Schiner, G.R., 1964, Ground-water resources of Block Island, Rhode Island: Geological Bulletin 14, iv, 35 p.; Map: 1 Sheet.","productDescription":"iv, 35 p.; Map: 1 Sheet","costCenters":[],"links":[{"id":276717,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Rhode Island","otherGeospatial":"Block Island","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -71.612905,41.146656 ], [ -71.612905,41.232825 ], [ -71.544307,41.232825 ], [ -71.544307,41.146656 ], [ -71.612905,41.146656 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"520f49e4e4b0fc50304bc4db","contributors":{"authors":[{"text":"Hansen, Arnold J.","contributorId":33316,"corporation":false,"usgs":true,"family":"Hansen","given":"Arnold J.","affiliations":[],"preferred":false,"id":482676,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Schiner, George R.","contributorId":22743,"corporation":false,"usgs":true,"family":"Schiner","given":"George","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":482675,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70047876,"text":"70047876 - 1964 - Water resources of Van Buren County, Michigan","interactions":[{"subject":{"id":17901,"text":"ofr6461 - 1964 - Water resources of Van Buren County, Michigan","indexId":"ofr6461","publicationYear":"1964","noYear":false,"title":"Water resources of Van Buren County, Michigan"},"predicate":"SUPERSEDED_BY","object":{"id":70047876,"text":"70047876 - 1964 - Water resources of Van Buren County, Michigan","indexId":"70047876","publicationYear":"1964","noYear":false,"title":"Water resources of Van Buren County, Michigan"},"id":1}],"lastModifiedDate":"2017-03-23T15:50:41","indexId":"70047876","displayToPublicDate":"2013-01-01T14:28:00","publicationYear":"1964","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":142,"text":"Water Investigation","active":false,"publicationSubtype":{"id":2}},"seriesNumber":"3","title":"Water resources of Van Buren County, Michigan","docAbstract":"The water resources of Van Buren County include productive ground-water reservoirs, a network of perennial streams, about 60 major inland lakes, and Lake Michigan. Most water users obtain their supplies from wells. The ground-water reservoirs in the glacial drift can provide several times the amount of water now used, but large withdrawals of ground water may lower the levels of nearby lakes or diminish the flow of nearly streams. Permeable soils and drift account for the relatively high base flows of streams in the southeastern two-thirds of the county. Less permeable surficial materials in the northwest part of the county result in relatively low base flows there. The water from wells is generally hard and high in iron content but is otherwise suitable for most uses. Water from streams and lakes is similar to that from wells except that iron-content is not a problem, and some of the inland lakes have very soft water. The availability of ground water, the base flow of streams, and the chemical character of water in the county are summarized in maps and tables accompanying this report.
","language":"English","publisher":"Michigan Geological Survey","publisherLocation":"Lansing, MI","collaboration":"Prepared cooperatively by the Geological Survey U.S. Department of the Interior","usgsCitation":"Giroux, P., Hendrickson, G.E., Stoimenoff, L., and Whetstone, G., 1964, Water resources of Van Buren County, Michigan: Water Investigation 3, 144 p.","productDescription":"144 p.","costCenters":[{"id":382,"text":"Michigan Water Science Center","active":true,"usgs":true}],"links":[{"id":277118,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/70047876.JPG"},{"id":277117,"type":{"id":11,"text":"Document"},"url":"https://www.michigan.gov/documents/deq/WI_03opt_309850_7.pdf"}],"country":"United States","state":"Michigan","county":"Van Buren County","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-85.7663,42.4196],[-85.7654,42.157],[-85.7638,42.0698],[-85.9913,42.0686],[-86.2243,42.0716],[-86.2246,42.1565],[-86.2255,42.2451],[-86.3395,42.2449],[-86.3637,42.2453],[-86.3625,42.2467],[-86.3544,42.2612],[-86.3401,42.2807],[-86.3388,42.2821],[-86.327,42.3034],[-86.3133,42.332],[-86.3039,42.3507],[-86.2877,42.3906],[-86.2814,42.4065],[-86.2745,42.4201],[-86.2248,42.4191],[-85.995,42.4193],[-85.8975,42.4185],[-85.7663,42.4196]]]},\"properties\":{\"name\":\"Van Buren\",\"state\":\"MI\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"521f1beee4b0f8bf2b076187","contributors":{"authors":[{"text":"Giroux, P.R.","contributorId":59055,"corporation":false,"usgs":true,"family":"Giroux","given":"P.R.","email":"","affiliations":[],"preferred":false,"id":483203,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hendrickson, G. E.","contributorId":99958,"corporation":false,"usgs":true,"family":"Hendrickson","given":"G.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":483205,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Stoimenoff, L.E.","contributorId":34157,"corporation":false,"usgs":true,"family":"Stoimenoff","given":"L.E.","email":"","affiliations":[],"preferred":false,"id":483202,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Whetstone, G.W.","contributorId":94680,"corporation":false,"usgs":true,"family":"Whetstone","given":"G.W.","email":"","affiliations":[],"preferred":false,"id":483204,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":70047482,"text":"70047482 - 1964 - Hydrologic conditions: Dade County, Florida","interactions":[{"subject":{"id":44048,"text":"ofr60124 - 1960 - Water-table contour map, Dade County, Florida","indexId":"ofr60124","publicationYear":"1960","noYear":false,"title":"Water-table contour map, Dade County, Florida"},"predicate":"SUPERSEDED_BY","object":{"id":70047482,"text":"70047482 - 1964 - Hydrologic conditions: Dade County, Florida","indexId":"70047482","publicationYear":"1964","noYear":false,"title":"Hydrologic conditions: Dade County, Florida"},"id":1}],"lastModifiedDate":"2017-09-13T17:55:49","indexId":"70047482","displayToPublicDate":"2013-01-01T14:15:00","publicationYear":"1964","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":5489,"text":"Florida Geological Survey Report of Investigations","active":false,"publicationSubtype":{"id":2}},"seriesNumber":"24","title":"Hydrologic conditions: Dade County, Florida","docAbstract":"Thin layers of dense limestone of low permeability that occur near the top of the Biscayne aquifer in the vicinity of the north end of Levee 30 in Dade County, Florida are of hydrologic importance because they retard the downward infiltration of ponded water in Conservation Area No. 3. This retarding effect frequently results in high head differentials across the levee. Tests made in a small area adjacent to Levee 30 indicate that the coefficient of transmissibility of the aquifer is 3,600,000 gpd (gallons per day) per foot, and the coefficient of vertical permeability of the dense limestones is 13 gpd per square foot. If ground-water flow beneath the levee is laminar, the total inflow to the Levee 30 Canal from Conservation Area No. 3 will be about 350 mgd (million gallons per day), or 540 cfs (cubic feet per second), per mile length of levee when the head difference across the levee is 10 feet.","language":"English","publisher":"Florida Geological Survey","publisherLocation":"Tallahassee, FL","collaboration":"Prepared by the United States Geological Survey in cooperation with the Central and Southern Florida Flood Control District","usgsCitation":"Kohout, F.A., Klein, H., Sherwood, C., and Leach, S.D., 1964, Hydrologic conditions: Dade County, Florida: Florida Geological Survey Report of Investigations 24, Parts 1-4: Variously Paginated.","productDescription":"Parts 1-4: Variously Paginated","costCenters":[],"links":[{"id":276169,"type":{"id":11,"text":"Document"},"url":"https://ufdc.ufl.edu/UF00001208/00001/pdf?search=hydrologic+%3dconditions+%3dsherwood"},{"id":276173,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/70047482.PNG"},{"id":276171,"type":{"id":2,"text":"Additional Report Piece"},"url":"https://ufdc.ufl.edu/UF00001210/00001/pdf?search=investigations+%3dreport+%3dsherwood"},{"id":276170,"type":{"id":2,"text":"Additional Report Piece"},"url":"https://ufdc.ufl.edu/UF00001209/00001/2j?search=investigations+%3dreport+%3dsherwood"},{"id":276172,"type":{"id":2,"text":"Additional Report Piece"},"url":"https://ufdc.ufl.edu/UF00001211/00001/pdf?search=investigations+%3dreport+%3d24"}],"country":"United States","county":"Miami-dade County","otherGeospatial":"Dade County","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -80.8736,25.1374 ], [ -80.8736,25.9792 ], [ -80.0428,25.9792 ], [ -80.0428,25.1374 ], [ -80.8736,25.1374 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5203a37be4b02bdb1bc63fc0","contributors":{"authors":[{"text":"Kohout, Francis Anthony","contributorId":11200,"corporation":false,"usgs":true,"family":"Kohout","given":"Francis","email":"","middleInitial":"Anthony","affiliations":[],"preferred":false,"id":482154,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Klein, Howard","contributorId":62189,"corporation":false,"usgs":true,"family":"Klein","given":"Howard","email":"","affiliations":[],"preferred":false,"id":482156,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Sherwood, C. 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S. Geological Survey in cooperation with the Florida Geological Survey during the period 1957-61. The results of this study will be published by the Florida Geological Survey in the following reports by William E. Clark, Rufus H. Musgrove, Clarence G. Menke, and Joseph W. Cagle, Jr.: \"Interim Report on the Water Resources of Alachua, Bradford, Clay, and Union Counties, Florida,\" \"Water Resources of Alachua, Bradford, Clay, and Union Counties, Florida,\" and \"Hydrology of Brooklyn Lake, near Keystone Heights, Florida.\"","language":"English","publisher":"Florida Geological Survey","publisherLocation":"Tallahassee, FL","collaboration":"Prepared by the United States Geological Survey in cooperation with the Florida Geological Survey","usgsCitation":"Clark, W.E., Musgrove, R.H., Menke, C.G., and Cagle, J.W., 1964, Water-resources data for Alachua, Bradford, Clay, and Union Counties, Florida: Florida Geological Survey Information Circular 43, iii, 154 p.","productDescription":"iii, 154 p.","costCenters":[],"links":[{"id":276168,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/70047481.PNG"},{"id":276167,"type":{"id":15,"text":"Index Page"},"url":"https://ufdc.ufl.edu/UF00001103/00001"}],"country":"United States","state":"Florida","county":"Alachua County, Bradford County, Clay County, Union County","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -82.658554,29.417057 ], [ -82.658554,30.193466 ], [ -81.581207,30.193466 ], [ -81.581207,29.417057 ], [ -82.658554,29.417057 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5203a37de4b02bdb1bc63feb","contributors":{"authors":[{"text":"Clark, William E.","contributorId":105365,"corporation":false,"usgs":true,"family":"Clark","given":"William","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":482153,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Musgrove, Rufus H.","contributorId":20245,"corporation":false,"usgs":true,"family":"Musgrove","given":"Rufus","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":482150,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Menke, Clarence G.","contributorId":25450,"corporation":false,"usgs":true,"family":"Menke","given":"Clarence","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":482151,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Cagle, Joseph W. 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Part 3: Report of Investigations of the North Carolina Department of Water and Air Resources, Division of Ground Water 4, vi, 22 p.","productDescription":"vi, 22 p.","costCenters":[{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true}],"links":[{"id":276751,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","otherGeospatial":"Cape Hatteras National Seashore","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -76.0148,35.0648 ], [ -76.0148,35.9063 ], [ -75.4599,35.9063 ], [ -75.4599,35.0648 ], [ -76.0148,35.0648 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"52136e34e4b0b08f446198f0","contributors":{"authors":[{"text":"Harris, William H.","contributorId":45999,"corporation":false,"usgs":true,"family":"Harris","given":"William","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":482714,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wilder, Hugh B.","contributorId":83899,"corporation":false,"usgs":true,"family":"Wilder","given":"Hugh","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":482715,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70038669,"text":"wdrCA631 - 1964 - Surface water records of California, 1963; Volume 1: Colorado River Basin, Southern Great Basin, and Pacific Slope Basins excluding Central Valley","interactions":[],"lastModifiedDate":"2012-06-13T01:01:48","indexId":"wdrCA631","displayToPublicDate":"2012-06-04T09:11:00","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-63-1","title":"Surface water records of California, 1963; 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/wdrCA631","usgsCitation":"U.S. Geological Survey, 1964, Surface water records of California, 1963; Volume 1: Colorado River Basin, Southern Great Basin, and Pacific Slope Basins excluding Central Valley: U.S. Geological Survey Water Data Report CA-63-1, 463 p., https://doi.org/10.3133/wdrCA631.","productDescription":"463 p.","costCenters":[],"links":[{"id":257482,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/wdr_CA_63_1.bmp"},{"id":257475,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/1963/ca-63/WDR-1963-vol1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"California","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505b9fcce4b08c986b31e818"} ,{"id":70038394,"text":"wdrCA64 - 1964 - Water Quality Records in California","interactions":[],"lastModifiedDate":"2012-05-22T01:01:41","indexId":"wdrCA64","displayToPublicDate":"2012-05-13T11:48:00","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","title":"Water Quality Records 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 1964 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","publisherLocation":"Reston, VA","doi":"10.3133/wdrCA64","usgsCitation":"U.S. Geological Survey, 1964, Water Quality Records in California: U.S. Geological Survey Water Data Report CA-64, x, 348 p., https://doi.org/10.3133/wdrCA64.","productDescription":"x, 348 p.","costCenters":[],"links":[{"id":256911,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":256906,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/1964/ca-64/WDR-1964-wq.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"California","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bc413e4b08c986b32b4af"} ,{"id":70040599,"text":"bGW53 - 1964 - Ground water in the Niagara Falls area, New York, with emphasis on the water-bearing characteristics of the bedrock","interactions":[],"lastModifiedDate":"2012-11-02T13:09:05","indexId":"bGW53","displayToPublicDate":"2012-01-02T00:00:00","publicationYear":"1964","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-53","title":"Ground water in the Niagara Falls area, New York, with emphasis on the water-bearing characteristics of the bedrock","language":"English","publisher":"New York State Water Resources Commission","publisherLocation":"Albany, NY","usgsCitation":"Johnson, R., 1964, Ground water in the Niagara Falls area, New York, with emphasis on the water-bearing characteristics of the bedrock: Bulletin GW-53, 93 p.; 3 Plates.","productDescription":"93 p.; 3 Plates","numberOfPages":"93","costCenters":[{"id":474,"text":"New York Water Science Center","active":true,"usgs":true}],"links":[{"id":262951,"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":"5094ebbbe4b0e5cfc2acdcc9","contributors":{"authors":[{"text":"Johnson, R.H.","contributorId":7041,"corporation":false,"usgs":true,"family":"Johnson","given":"R.H.","email":"","affiliations":[],"preferred":false,"id":468658,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70040445,"text":"70040445 - 1964 - Water resources of the Lake Erie-Niagara area, New York, a preliminary appraisal","interactions":[],"lastModifiedDate":"2012-10-19T17:16:26","indexId":"70040445","displayToPublicDate":"2012-01-01T15:01:26","publicationYear":"1964","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-52","title":"Water resources of the Lake Erie-Niagara area, New York, a preliminary appraisal","language":"English","publisher":"New York State Water Resources Commission","publisherLocation":"Albany, NY","usgsCitation":"La Sala, A., Harding, W.E., and Archer, R., 1964, Water resources of the Lake Erie-Niagara area, New York, a preliminary appraisal: Bulletin GW-52, 8 p.","productDescription":"8 p.","numberOfPages":"8","costCenters":[{"id":474,"text":"New York Water Science Center","active":true,"usgs":true}],"links":[{"id":262737,"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":"50e57c05e4b0a4aa5bb0842b","contributors":{"authors":[{"text":"La Sala, A.M. 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