No abstract available.
","language":"English","publisher":"Elsevier","doi":"10.1111/j.1745-6584.1964.tb01749.x","usgsCitation":"Hackett, O.M., 1964, The father of modern ground water hydrology: Groundwater, v. 2, no. 2, p. 2-5, https://doi.org/10.1111/j.1745-6584.1964.tb01749.x.","productDescription":"4 p.","startPage":"2","endPage":"5","costCenters":[],"links":[{"id":386213,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"2","issue":"2","noUsgsAuthors":false,"publicationDate":"2006-07-06","publicationStatus":"PW","contributors":{"authors":[{"text":"Hackett, O. M.","contributorId":38527,"corporation":false,"usgs":true,"family":"Hackett","given":"O.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":816986,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70208846,"text":"70208846 - 1964 - Morphologic studies of the brachiopod genus Composita","interactions":[],"lastModifiedDate":"2020-03-03T10:18:37","indexId":"70208846","displayToPublicDate":"1964-03-31T10:13:02","publicationYear":"1964","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2412,"text":"Journal of Paleontology","active":true,"publicationSubtype":{"id":10}},"displayTitle":"Morphologic studies of the brachiopod genus Composita","title":"Morphologic studies of the brachiopod genus Composita","docAbstract":"The genus Composita consists of smooth-shelled athyroid brachiopods which in North America have a range from Late Devonian or Early Mississippian to Permian. Morphologic variation in the genus has been recognized by earlier workers, but few have tried to show exact relationships among the various forms. The present writers have attempted to trace the development of the genus through geologic time. Only North American species and varieties of Composita are treated in this paper. Forty-two species and varieties are included in a phylogenetic history of the genus. Nine other species are listed as doubtful forms. Eighteen specific and varietal names are rejected by the writers as obsolete. Morphologic intergradation among associated, synchronous forms is studied with the aid of frequency polygons. Lack of clear separation of the associated species within different maxima of the polygons indicates their dominant intergradation. These forms, previously described qualitatively, are regarded as typological species. A statistical method is used to test for differences between collections containing the same typological species. Significant differences in the slopes of reduced major axes are obtained in length-width, length-depth and depth-width plots of two collections containing Composita subtilita and Composita argentea. Significant differences also are obtained when two collections of Composita subtilita, Composita ovata and Composita elongata are compared in the same way. In spite of these results, slight nomenclatural changes are thought to be unnecessary. Use of the triangular graph as a means of distinguishing vertical subspecies is also tested. Four collections are plotted on one graph and five artificially separated groups of Composita subtilita on another. Mixed results are obtained. The method is suspect because the results are found to depend largely on the number of specimens used.
","language":"English","publisher":"Society for Sedimentary Geology","usgsCitation":"Grinnell, R.S., and Andrews, G., 1964, Morphologic studies of the brachiopod genus Composita: Journal of Paleontology, v. 38, no. 2, p. 227-248.","productDescription":"22 p.","startPage":"227","endPage":"248","costCenters":[],"links":[{"id":372845,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"38","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Grinnell, Robert S.","contributorId":222946,"corporation":false,"usgs":false,"family":"Grinnell","given":"Robert","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":783618,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Andrews, George W.","contributorId":40621,"corporation":false,"usgs":true,"family":"Andrews","given":"George W.","affiliations":[],"preferred":false,"id":783619,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70209226,"text":"70209226 - 1964 - On the standardization of geophysical observations at volcanoes","interactions":[],"lastModifiedDate":"2020-03-24T14:51:18","indexId":"70209226","displayToPublicDate":"1964-03-24T14:50:31","publicationYear":"1964","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1093,"text":"Bulletin Volcanologique","active":true,"publicationSubtype":{"id":10}},"title":"On the standardization of geophysical observations at volcanoes","docAbstract":"No abstract available.
","language":"English","publisher":"Springer","doi":"10.1007/BF02597542","usgsCitation":"Eaton, J.P., 1964, On the standardization of geophysical observations at volcanoes: Bulletin Volcanologique, v. 27, p. 417-419, https://doi.org/10.1007/BF02597542.","productDescription":"3 p.","startPage":"417","endPage":"419","costCenters":[],"links":[{"id":373488,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"27","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Eaton, J. P.","contributorId":105313,"corporation":false,"usgs":true,"family":"Eaton","given":"J.","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":785462,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70010766,"text":"70010766 - 1964 - Natural carbon-14 activity of organic substances in streams","interactions":[],"lastModifiedDate":"2026-02-13T16:12:38.718539","indexId":"70010766","displayToPublicDate":"1964-03-13T00:00:00","publicationYear":"1964","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3338,"text":"Science","active":true,"publicationSubtype":{"id":10}},"title":"Natural carbon-14 activity of organic substances in streams","docAbstract":"Carbon-14 measurements made on organic contaminants extracted from streams show percentages of industrial waste and domestic sewage. The method, used previously for studies of the atmosphere, can be used in studies of pollution sources.","language":"English","publisher":"American Association for the Advancement of Science","doi":"10.1126/science.143.3611.1163","issn":"00368075","usgsCitation":"Rosen, A., and Rubin, M., 1964, Natural carbon-14 activity of organic substances in streams: Science, v. 143, no. 3611, p. 1163-1164, https://doi.org/10.1126/science.143.3611.1163.","productDescription":"2 p.","startPage":"1163","endPage":"1164","costCenters":[],"links":[{"id":218654,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"143","issue":"3611","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a62e6e4b0c8380cd72196","contributors":{"authors":[{"text":"Rosen, A.A.","contributorId":35598,"corporation":false,"usgs":true,"family":"Rosen","given":"A.A.","email":"","affiliations":[],"preferred":false,"id":359599,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Rubin, M.","contributorId":88079,"corporation":false,"usgs":true,"family":"Rubin","given":"M.","email":"","affiliations":[],"preferred":false,"id":359600,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70209010,"text":"70209010 - 1964 - Waterfowl in the Canadian breadbasket","interactions":[],"lastModifiedDate":"2020-03-11T12:10:01","indexId":"70209010","displayToPublicDate":"1964-03-11T11:58:48","publicationYear":"1964","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"title":"Waterfowl in the Canadian breadbasket","docAbstract":"No abstract available.
","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Waterfowl Tomorrow","largerWorkSubtype":{"id":15,"text":"Monograph"},"language":"English","publisher":"U.S. Department of the Interior ","usgsCitation":"Paynter, E.L., and Stephen, W., 1964, Waterfowl in the Canadian breadbasket, chap. of Waterfowl Tomorrow, p. 409-416.","productDescription":"8 p.","startPage":"409","endPage":"416","costCenters":[{"id":480,"text":"Northern Prairie Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":373096,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Paynter, Ernest L.","contributorId":223205,"corporation":false,"usgs":false,"family":"Paynter","given":"Ernest","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":784526,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Stephen, W.J.D.","contributorId":223206,"corporation":false,"usgs":false,"family":"Stephen","given":"W.J.D.","email":"","affiliations":[],"preferred":false,"id":784527,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":5223144,"text":"5223144 - 1964 - Notes on the ecology of the opossum in Maryland","interactions":[],"lastModifiedDate":"2025-03-07T16:10:11.496889","indexId":"5223144","displayToPublicDate":"1964-03-06T00:00:00","publicationYear":"1964","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2373,"text":"Journal of Mammalogy","onlineIssn":"1545-1542","printIssn":"0022-2372","active":true,"publicationSubtype":{"id":10}},"title":"Notes on the ecology of the opossum in Maryland","docAbstract":"Livetrapping of opossums at the Patuxent Research Refuge in Maryland over an 8-year period resulted in the capture of 224 opossums, with 541 trap records. The maximum recorded trap life was 29 months, and the greatest estimated age was 36 months. Opossums did not enter traps readily, and the average period between consecutive captures was 31 days. Trap records indicated that opossums range over long, narrow areas rather than circular ones, probably associated with stream courses. Opossums begin to breed in Maryland in early February and young are found in the pouch until August. Evidently the first breeding period accounts for most of the young produced. The sex ratio of those trapped was slightly higher for males than females, but did not differ significantly from an expected sample from an even sex ratio. The trapping results indicated a production rate of from 4 to 5.4 young per adult female, but this is based on the assumption that young and adults have the same trap response. Opossums appear to favor low, damp woods rather than upland woods or open areas.
","language":"English","publisher":"Oxford Academic","doi":"10.2307/1377299","usgsCitation":"Llewellyn, L.M., and Dale, F.H., 1964, Notes on the ecology of the opossum in Maryland: Journal of Mammalogy, v. 45, no. 1, p. 113-122, https://doi.org/10.2307/1377299.","productDescription":"10 p.","startPage":"113","endPage":"122","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":199929,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United 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\"}}]}","volume":"45","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afce4b07f02db6969e9","contributors":{"authors":[{"text":"Llewellyn, L. M.","contributorId":104998,"corporation":false,"usgs":true,"family":"Llewellyn","given":"L.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":337974,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Dale, Fred H.","contributorId":70698,"corporation":false,"usgs":true,"family":"Dale","given":"Fred","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":337973,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70221130,"text":"70221130 - 1964 - Radioelement dispersion in a sedimentary environment and its effect on uranium exploration","interactions":[],"lastModifiedDate":"2021-06-04T12:06:39.460624","indexId":"70221130","displayToPublicDate":"1964-03-01T13:40:47","publicationYear":"1964","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1472,"text":"Economic Geology","active":true,"publicationSubtype":{"id":10}},"title":"Radioelement dispersion in a sedimentary environment and its effect on uranium exploration","docAbstract":"The radioelement content of the major part of the southeast Texas Coastal Plain sedimentary sequence falls within a range common for sandstones and shales. Exceptions to the normal limit are mainly in small, widely scattered areas. One anomalous area, however, covers several tens of square miles and contains most of the important uranium deposits. Both mechanical and chemical dispersion of radioelements takes place in the immediate vicinity of the ore deposits, though no attempt is made to extend this local dispersion model to the large, regional gamma radiation anomaly. It is suggested that the point-source concept for sedimentary uranium deposits is unrealistic and that conventional aeroradiometric survey grid spacing can be substantially enlarged without seriously reducing efficiency in uranium exploration.
","language":"English","publisher":"Society of Economic Geologists","doi":"10.2113/gsecongeo.59.2.309","usgsCitation":"Moxham, R., 1964, Radioelement dispersion in a sedimentary environment and its effect on uranium exploration: Economic Geology, v. 59, no. 2, p. 309-321, https://doi.org/10.2113/gsecongeo.59.2.309.","productDescription":"13 p.","startPage":"309","endPage":"321","costCenters":[],"links":[{"id":386192,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"59","issue":"2","noUsgsAuthors":false,"publicationDate":"1964-03-01","publicationStatus":"PW","contributors":{"authors":[{"text":"Moxham, R.M.","contributorId":42234,"corporation":false,"usgs":true,"family":"Moxham","given":"R.M.","email":"","affiliations":[],"preferred":false,"id":816941,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70221131,"text":"70221131 - 1964 - Radioelement dispersion in a sedimentary environment and its effect on uranium exploration","interactions":[],"lastModifiedDate":"2021-06-02T18:44:40.729852","indexId":"70221131","displayToPublicDate":"1964-03-01T13:40:47","publicationYear":"1964","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1472,"text":"Economic Geology","active":true,"publicationSubtype":{"id":10}},"title":"Radioelement dispersion in a sedimentary environment and its effect on uranium exploration","docAbstract":"The radioelement content of the major part of the southeast Texas Coastal Plain sedimentary sequence falls within a range common for sandstones and shales. Exceptions to the normal limit are mainly in small, widely scattered areas. One anomalous area, however, covers several tens of square miles and contains most of the important uranium deposits. Both mechanical and chemical dispersion of radioelements takes place in the immediate vicinity of the ore deposits, though no attempt is made to extend this local dispersion model to the large, regional gamma radiation anomaly. It is suggested that the point-source concept for sedimentary uranium deposits is unrealistic and that conventional aeroradiometric survey grid spacing can be substantially enlarged without seriously reducing efficiency in uranium exploration.
","language":"English","publisher":"Society of Economic Geologists","doi":"10.2113/gsecongeo.59.2.309","usgsCitation":"Moxham, R., 1964, Radioelement dispersion in a sedimentary environment and its effect on uranium exploration: Economic Geology, v. 59, no. 2, p. 309-321, https://doi.org/10.2113/gsecongeo.59.2.309.","productDescription":"13 p.","startPage":"309","endPage":"321","costCenters":[],"links":[{"id":386146,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Texas","otherGeospatial":"southeast Texas","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -93.84521484375,\n 29.76437737516313\n ],\n [\n -93.75732421875,\n 30.95876857077987\n ],\n [\n -96.48193359375,\n 30.35391637229704\n ],\n [\n -98.525390625,\n 29.036960648558267\n ],\n [\n -98.94287109375,\n 26.43122806450644\n ],\n [\n -97.119140625,\n 25.918526162075153\n ],\n [\n -93.84521484375,\n 29.76437737516313\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"59","issue":"2","noUsgsAuthors":false,"publicationDate":"1964-03-01","publicationStatus":"PW","contributors":{"authors":[{"text":"Moxham, R.M.","contributorId":42234,"corporation":false,"usgs":true,"family":"Moxham","given":"R.M.","email":"","affiliations":[],"preferred":false,"id":816820,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70221129,"text":"70221129 - 1964 - New approaches to the geography of the United States: Introduction","interactions":[],"lastModifiedDate":"2021-06-02T18:39:36.919581","indexId":"70221129","displayToPublicDate":"1964-03-01T13:36:22","publicationYear":"1964","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":797,"text":"Annals of the Association of American Geographers","active":true,"publicationSubtype":{"id":10}},"title":"New approaches to the geography of the United States: Introduction","docAbstract":"No abstract available.
","language":"English","publisher":"Taylor & Francis","doi":"10.1111/j.1467-8306.1964.tb00468.x","usgsCitation":"Gerlach, A.C., 1964, New approaches to the geography of the United States: Introduction: Annals of the Association of American Geographers, v. 54, no. 1, 1 p., https://doi.org/10.1111/j.1467-8306.1964.tb00468.x.","productDescription":"1 p.","costCenters":[],"links":[{"id":386145,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"54","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Gerlach, Arch C.","contributorId":78249,"corporation":false,"usgs":true,"family":"Gerlach","given":"Arch","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":816819,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70221183,"text":"70221183 - 1964 - Relation of temperature distribution to ground-water movement in carbonate rocks of central Israel","interactions":[],"lastModifiedDate":"2021-06-04T17:34:58.608687","indexId":"70221183","displayToPublicDate":"1964-03-01T12:31:10","publicationYear":"1964","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1786,"text":"Geological Society of America Bulletin","active":true,"publicationSubtype":{"id":10}},"title":"Relation of temperature distribution to ground-water movement in carbonate rocks of central Israel","docAbstract":"The Cenomanian-Turonian formations of central Israel constitute a highly permeable dolomite and limestone aquifer. In this area it is on the west limb of an anticlinorium that trends north-northeast, and it contains water under artesian pressure. A graph of water temperatures and well depths suggests that there is a very small vertical temperature gradient in local segments of the aquifer. The small gradient is believed to result from a large vertical component of flow that tends to equalize the vertical temperature distribution. On a regional scale the apparent horizontal temperature distribution indicates a westward increase with increasing depth of the aquifer, suggesting a manifestation of the regional geothermal gradient. The westward increase in temperature also implies that the lateral component of flow may be in the normal range for artesian carbonate-rock aquifers whose pores consist mainly of solution cavities. Locally, pumping appears to have affected the temperature distribution by modifying the natural flow pattern. In parts of the most intensively developed area, the aquifer is hydraulically connected with overlying coastal-plain deposits, and some cooler water has been induced to move into the aquifer from this source. At three other areas, pumping has resulted in an apparent horizontal shift of the isotherms on a temperature-distribution map. The data suggest that the spatial distribution of temperature may be used to determine some of the flow characteristics of carbonate-rock aquifers.
","language":"English","publisher":"Geological Society of America","doi":"10.1130/0016-7606(1964)75[209:ROTDTG]2.0.CO;2","usgsCitation":"Schneider, R., 1964, Relation of temperature distribution to ground-water movement in carbonate rocks of central Israel: Geological Society of America Bulletin, v. 75, no. 3, p. 209-216, https://doi.org/10.1130/0016-7606(1964)75[209:ROTDTG]2.0.CO;2.","productDescription":"8 p.","startPage":"209","endPage":"216","costCenters":[],"links":[{"id":386224,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"Israel","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n 35.57373046875,\n 33.284619968887675\n ],\n [\n 35.430908203125,\n 33.100745405144245\n ],\n [\n 35.13427734375,\n 33.100745405144245\n ],\n [\n 34.1455078125,\n 31.372399104880525\n ],\n [\n 34.9365234375,\n 29.458731185355344\n ],\n [\n 35.595703125,\n 32.13840869677249\n ],\n [\n 35.57373046875,\n 33.284619968887675\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"75","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Schneider, Robert","contributorId":102460,"corporation":false,"usgs":true,"family":"Schneider","given":"Robert","email":"","affiliations":[],"preferred":false,"id":817001,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":37750,"text":"37750 - 1964 - Improved nest structures for wood ducks","interactions":[],"lastModifiedDate":"2014-07-23T10:52:01","indexId":"37750","displayToPublicDate":"1964-03-01T10:51:16","publicationYear":"1964","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":"458","title":"Improved nest structures for wood ducks","docAbstract":"No abstract available.","language":"English","publisher":"U.s. Department of the Interior","publisherLocation":"Washington, D.C.","usgsCitation":"Webster, C.G., and Uhler, F.M., 1964, Improved nest structures for wood ducks (Revises Wildlife Leaflet 393 (1958).): Wildlife Leaflet 458, 20 p.","productDescription":"20 p.","numberOfPages":"20","costCenters":[],"links":[{"id":290774,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"edition":"Revises Wildlife Leaflet 393 (1958).","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57ffcef2e4b0824b2d175dac","contributors":{"authors":[{"text":"Webster, Clark G.","contributorId":108407,"corporation":false,"usgs":true,"family":"Webster","given":"Clark","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":218534,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Uhler, Francis M.","contributorId":49838,"corporation":false,"usgs":true,"family":"Uhler","given":"Francis","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":218533,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70043887,"text":"70043887 - 1964 - Seismic-refraction measurements of crustal structure between Nevada Test Site and Ludlow, California","interactions":[],"lastModifiedDate":"2013-02-25T08:55:50","indexId":"70043887","displayToPublicDate":"1964-02-22T00:00:00","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":"26","title":"Seismic-refraction measurements of crustal structure between Nevada Test Site and Ludlow, California","docAbstract":"Seismic-refraction measurements from nuclear and chemical explosions were made along a line from the Nevada Test Site (NTS) to Ludlow, California, and additional recordings from nuclear explosions were made southward toward Calexico, California. The time of first arrivals from the Ludlow shotpoint is expressed as T0 = 0.00 + Δ/2.50 (assumed), T1 = 1.00 + Δ6.10, T2 = 2.81 + Δ/6.80, and T3 = 5.48 + ~7.76, where T is in seconds and distance Δ is in km. First arrival times from NTS fit the lines T1 = 0.74 + Δ/6.10, T2 = 2.81 + Δ/6.80 (assumed), T3 = 6.70 + Δ/8.04 to a distance of 265 km, beyond 265 km T3 = 5.83 + Δ/7.75. The difference in the apparent velocities of the Pn (T3) arrival is caused by variations in the dip of the Mohorovicic discontinuity. The thickness of the successive layers at NTS are H0 s 1.0 km (V0 ~ 2.5 km/sec), H1 = 13 km (v1 = 6.1 km/sec), and H2 = 20 km (v2 = 6.8 km/ sec); the total crustal thickness is 34 km. The successive crustal layers at Ludlow have a thickness of H0 = 1.4 km, H1 = 13 km, and H2 = 13 km; the total crustal thickness is 27 km.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/70043887","collaboration":"In cooperation with the Defense Advanced Research Projects Agency","usgsCitation":"Gibbs, J., and Roller, J., 1964, Seismic-refraction measurements of crustal structure between Nevada Test Site and Ludlow, California: Crustal Studies Technical Letter 26, iii, 30 p., https://doi.org/10.3133/70043887.","productDescription":"iii, 30 p.","additionalOnlineFiles":"N","costCenters":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true},{"id":379,"text":"Menlo Park Science Center","active":false,"usgs":true}],"links":[{"id":268196,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":268194,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/misc/tl/0026/tl0026.pdf"},{"id":268195,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/misc/tl/0026/"}],"state":"Arizona;California;Nevada","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -116.9975,32.4982 ], [ -116.9975,36.0013 ], [ 114.5009,36.0013 ], [ 114.5009,32.4982 ], [ -116.9975,32.4982 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"512c9621e4b0855fde669816","contributors":{"authors":[{"text":"Gibbs, J. F.","contributorId":50894,"corporation":false,"usgs":true,"family":"Gibbs","given":"J. 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Nevertheless, a unique study was made of the hydrologic cycle of small stream basins in Wisconsin and New Jersey on the basis of measurements relative to the peak of tritium fallout in the spring of 1958. The continental and the coastal basins received approximately the same tritium fallout. Approximately 30 percent went into ground-water storage, the remainder being exported as runoff and evapotranspiration. The mean residence time for ground-water recharge for the two basins was 45 and 30 days, respectively.","language":"English","publisher":"American Association for the Advancement of Science.","doi":"10.1126/science.143.3608.804","issn":"00368075","usgsCitation":"Carlston, C., 1964, Tritium-hydrologic research: Some results of the U.S. Geological Survey Research Program: Science, v. 143, no. 3608, p. 804-806, https://doi.org/10.1126/science.143.3608.804.","productDescription":"3 p.","startPage":"804","endPage":"806","costCenters":[],"links":[{"id":219076,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"New Jersey, Wisconsin","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -92.65443024683039,\n 47.18686471532902\n ],\n [\n -92.92337344008368,\n 44.76948314682184\n ],\n [\n -91.54422384565291,\n 43.91380985726313\n ],\n [\n -90.40331265602809,\n 42.36186629934298\n ],\n [\n -87.66640475516137,\n 42.473317234890345\n ],\n [\n -86.69378362897187,\n 45.09478563580936\n ],\n [\n -87.76789223463291,\n 45.99366780802788\n ],\n [\n -89.9402097973789,\n 46.41028342019218\n ],\n [\n -89.94150082434655,\n 47.33914537549116\n ],\n [\n -92.65443024683039,\n 47.18686471532902\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n },\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -75.03044920156037,\n 41.368918438639554\n ],\n [\n -75.21217801383332,\n 40.6314679025723\n ],\n [\n -74.81474599562263,\n 40.24767874671271\n ],\n [\n -75.6121640073091,\n 39.468177148463866\n ],\n [\n -74.80122580215662,\n 38.82749379603797\n ],\n [\n -74.0060957836949,\n 40.04453424272181\n ],\n [\n -73.96363933005574,\n 41.368918438639554\n ],\n [\n -75.03044920156037,\n 41.368918438639554\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","volume":"143","issue":"3608","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bb875e4b08c986b327884","contributors":{"authors":[{"text":"Carlston, C.W.","contributorId":26062,"corporation":false,"usgs":true,"family":"Carlston","given":"C.W.","affiliations":[],"preferred":false,"id":358994,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70010815,"text":"70010815 - 1964 - Geomagnetic polarity epochs","interactions":[],"lastModifiedDate":"2026-02-13T16:28:46.687883","indexId":"70010815","displayToPublicDate":"1964-01-24T00:00:00","publicationYear":"1964","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3338,"text":"Science","active":true,"publicationSubtype":{"id":10}},"title":"Geomagnetic polarity epochs","docAbstract":"No abstract available.
","language":"English","publisher":"American Association for the Advancement of Science","doi":"10.1126/science.143.3604.351","issn":"00368075","usgsCitation":"Cox, A., Doell, R., and Dalrymple, G.B., 1964, Geomagnetic polarity epochs: Science, v. 143, no. 3604, p. 351-352, https://doi.org/10.1126/science.143.3604.351.","productDescription":"2 p.","startPage":"351","endPage":"352","costCenters":[],"links":[{"id":218742,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"California","otherGeospatial":"Sierra Nevada","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -119.53868231107185,\n 37.56150204417524\n ],\n [\n -119.53868231107185,\n 36.953435367375164\n ],\n [\n -118.57197073805631,\n 36.953435367375164\n ],\n [\n -118.57197073805631,\n 37.56150204417524\n ],\n [\n -119.53868231107185,\n 37.56150204417524\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","volume":"143","issue":"3604","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a275ce4b0c8380cd597e8","contributors":{"authors":[{"text":"Cox, A.","contributorId":89266,"corporation":false,"usgs":true,"family":"Cox","given":"A.","email":"","affiliations":[],"preferred":false,"id":359713,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Doell, Richard R.","contributorId":66683,"corporation":false,"usgs":true,"family":"Doell","given":"Richard R.","affiliations":[],"preferred":false,"id":359712,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Dalrymple, G. 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https://doi.org/10.3133/b1108.","temporalStart":"1959-01-01","temporalEnd":"1963-12-31","costCenters":[],"links":[{"id":289486,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/1108/report-thumb.jpg"},{"id":344675,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/1108/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Alaska","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ 172.44,51.21 ], [ 172.44,71.39 ], [ -129.99,71.39 ], [ -129.99,51.21 ], [ 172.44,51.21 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53bbc178e4b084059e8bfedb"} ,{"id":70095523,"text":"70095523 - 1964 - Sedimentology: general introduction and definitions : fluvial sediment and channel morphology","interactions":[],"lastModifiedDate":"2014-03-25T10:35:32","indexId":"70095523","displayToPublicDate":"1964-01-01T13:52:00","publicationYear":"1964","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"seriesTitle":{"id":375,"text":"Open-File Report","active":false,"publicationSubtype":{"id":6}},"title":"Sedimentology: general introduction and definitions : fluvial sediment and channel morphology","docAbstract":"Sedimentology, the study of sedimentary rocks and the \nprocesses by which they are formed, includes and is related \nto a large number of phenomena. Sedimentology includes the \nfive fundamental processes defined by the term sediaentation \n--weathering, erosion, transportation, deposition and \ndiagenesis. \nSedimentology shares with geomorphology the study of \nthe surface features of the earth. Sedimentology also \nshares with hydrology the study of river.--channels. River \nchannels are formed in part or in total as a result of \nflowing water and sediment transport, commonly called the \n\"work of the rivers.\" \nThis survey of published literature was made to aid in \narriving at definitions which would be acceptable to, and \nrepresentative of, a majority of professional personnel \nactively engaged in laboratory and field investigations \nrelated to the \"work of the river.\" The definitions in this \nlist are intended to explain the terms used in studies of \nfluvial sediment and channel morphology. No set of \ndefinitions can expect universal acceptance, however, i t is \nhoped that this compilation will be considered a summary \nand synthesis of present and past usage and that it will \nserve as a starting point for future usage. \nMultiple references are cited from textbooks, glossaries and dictionaries, scientific journals and u.s. Government \npublications. To obtain a mutual understanding and enhance \nprecision, many of the proposed definitions are a composite \nof those selected from papers or reports covering research \nstudies and field investigations. \n\nA draft of this glossary has been reviewed by a group of \ninterested personnel. The results of this review have been \ncarefully considered and the originally-suggested definitions \nhave been revised accordingly, resulting in the present \ncompilation. \nR. G. Wolff, with the help of Mrs. v. Blatcher, carried \nout the literature search and compilation of terms and the \nreview results. Paul c. Benedict approved or composed the \ndefinitions as presented in this report.","language":"English","publisher":"U.S. Geological Survey, Water Resources Division","publisherLocation":"Washington, DC","doi":"10.3133/70095523","usgsCitation":"Wolff, R.G., and Benedict, P., 1964, Sedimentology: general introduction and definitions : fluvial sediment and channel morphology: Open-File Report, iii, 132 p., https://doi.org/10.3133/70095523.","productDescription":"iii, 132 p.","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":283310,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/70095523.jpg"},{"id":284835,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/unnumbered/70095523/report.pdf"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5355955fe4b0120853e8c1d4","contributors":{"authors":[{"text":"Wolff, Roger G.","contributorId":19580,"corporation":false,"usgs":true,"family":"Wolff","given":"Roger","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":491227,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Benedict, Paul C.","contributorId":72293,"corporation":false,"usgs":true,"family":"Benedict","given":"Paul C.","affiliations":[],"preferred":false,"id":491228,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70094923,"text":"70094923 - 1964 - Soil mechanics and soil physics symbols and nomenclature useful in hydrologic studies","interactions":[],"lastModifiedDate":"2014-02-25T13:59:49","indexId":"70094923","displayToPublicDate":"1964-01-01T13:50:00","publicationYear":"1964","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"seriesTitle":{"id":375,"text":"Open-File Report","active":false,"publicationSubtype":{"id":6}},"title":"Soil mechanics and soil physics symbols and nomenclature useful in hydrologic studies","docAbstract":"The study of hydrology requires an interdisciplinary approach,\nincorporating knowledge from fields such as engineering, geology,\nchemistry, and agriculture. With increasing frequency, the hydrologist\nfinds it necessary to study the literature of the soil mechanics and\nsoil physics disciplines for assistance in the solution of hydrologic\nproblems. Because of the inter-relation between hydrology and soil\nmechanics and soil physics, hydrologists also are preparing an increasing\nnumber of technical papers ·for use by these two disciplines.\nTo permit the hydrologist to better understand specialized literature,\nas well as to assist him in preparing papers for these disciplines,\nthis glossary of soil mechanics and soil physics nomenclature was prepared.\nIt is a compilation from standards, dictionaries, and glossaries published\nby technical societies, and from reports by selected authorities in the\nfields of soil mechanics and soil physics. The variety of symbols and\ndefinitions presented for many of the terms demonstrates the difficulty\nthat has been encountered over the years in reaching agreement on such a\nsubject as nomenclature. Both old and new definitions and symbols are\npresented to assist the hydrologist in reading literature. Whenever\npossible the more recent symbols and nomenclature should be used by the\nhydrologist in writing papers for soil mechanics or soil physics audiences.\nWhen the hydrologist finds it necessary to use symbols or terms not included\nin the present list, he should try to select those not in conflict with the\nrecent systems presented in this report.\nSymbols are listed in alphabetical order to assist readers in finding\nthe term represented by a given symbol. Terms also are listed alphabetically,\nusually followed by recommended symbols and brief definitions.\nWhere two or more symbols or definitions are listed following a term, no\nsignificance should be placed on the order of presentation. The source is\nindicated for each symbol, term, or definition, and the sources are listed\nin the cited references.\nIt is emphasized that this report is only a compilation of nomenclature\ngenerally accepted in the soil mechanics apd soil physics disciplines.\nIt does not necessarily represent the recommendations or usage of such\nnomenclature by the Geological Survey or any part of its organization.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Denver, CO","doi":"10.3133/70094923","usgsCitation":"Johnson, A., 1964, Soil mechanics and soil physics symbols and nomenclature useful in hydrologic studies: Open-File Report, 50 p., https://doi.org/10.3133/70094923.","productDescription":"50 p.","numberOfPages":"53","costCenters":[],"links":[{"id":282776,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/70094923.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53cd732ce4b0b29085108c64","contributors":{"authors":[{"text":"Johnson, A.I.","contributorId":82676,"corporation":false,"usgs":true,"family":"Johnson","given":"A.I.","email":"","affiliations":[],"preferred":false,"id":490965,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70221133,"text":"70221133 - 1964 - Hydrologic factors pertinent to ground‐water contamination","interactions":[],"lastModifiedDate":"2021-06-02T18:50:54.556763","indexId":"70221133","displayToPublicDate":"1964-01-01T13:47:53","publicationYear":"1964","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3825,"text":"Groundwater","active":true,"publicationSubtype":{"id":10}},"title":"Hydrologic factors pertinent to ground‐water contamination","docAbstract":"Predictions of where and how a fluid waste may travel from disposal site to the water table require detailed information on the physical characteristics, location, and extent of all pervious and impervious materials in the unsaturated zone. Principles concerning the flow system in the unsaturated zone indicate the importance of choice of disposal technique in predicting the time required for the fluid waste to traverse the distance to the water table. With appropriate data on the location, extent, and physical properties of water‐bearing materials and on the boundaries of the saturated zone flow system, it is possible to analyze the relative merits of a variety of waste disposal techniques and to describe the probable consequences of each. Environments of consolidated rocks, such as granites, sandstones, and limestones, pose problems in addition to those related to unconsolidated or granular porous media in defining the fluid‐flow regimes that involve joint patterns, fracture patterns, solutional openings, and the rock structure. The consequences of ground‐water contamination can be just as damaging to water users as the pollution of surface streams. In fact it can be argued that the consequences are far more damaging because they persist over much longer periods of time after the contaminating source has been eliminated. It would appear prudent, therefore, to guard against contamination of the ground‐water resource in the first instance, rather than to engage in long expensive rehabilitation measures after the damage has been done. In 1960 Graham Walton presented data concerning contamination, by sewage or other man‐made wastes, of surface and underground waters. The circumstances attending the reported incidents of contamination, especially those involving ground‐water supplies, have aided materially in the choice of a few principles and ideas that will identify the role of some significant hydrologic factors in the underground movement of fluid wastes. Walton's discussion of ground‐water contamination refers often to physical settings into which fluid wastes are discharged at or near the land surface into cesspools, tile‐drain fields, and holding ponds. Furthermore, most reported instances of ground‐water contamination have taken place in relatively humid.
","language":"English","publisher":"Wiley Blackwell","doi":"10.1111/j.1745-6584.1964.tb01739.x","usgsCitation":"Brown, R., 1964, Hydrologic factors pertinent to ground‐water contamination: Groundwater, v. 2, no. 1, p. 5-12, https://doi.org/10.1111/j.1745-6584.1964.tb01739.x.","productDescription":"8 p.","startPage":"5","endPage":"12","costCenters":[],"links":[{"id":386147,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"2","issue":"1","noUsgsAuthors":false,"publicationDate":"2006-07-06","publicationStatus":"PW","contributors":{"authors":[{"text":"Brown, R.","contributorId":101419,"corporation":false,"usgs":true,"family":"Brown","given":"R.","affiliations":[],"preferred":false,"id":816821,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70221132,"text":"70221132 - 1964 - Hydrologic factors pertinent to ground‐water contamination","interactions":[],"lastModifiedDate":"2021-06-04T12:04:08.414151","indexId":"70221132","displayToPublicDate":"1964-01-01T13:47:53","publicationYear":"1964","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3825,"text":"Groundwater","active":true,"publicationSubtype":{"id":10}},"title":"Hydrologic factors pertinent to ground‐water contamination","docAbstract":"Predictions of where and how a fluid waste may travel from disposal site to the water table require detailed information on the physical characteristics, location, and extent of all pervious and impervious materials in the unsaturated zone. Principles concerning the flow system in the unsaturated zone indicate the importance of choice of disposal technique in predicting the time required for the fluid waste to traverse the distance to the water table. With appropriate data on the location, extent, and physical properties of water‐bearing materials and on the boundaries of the saturated zone flow system, it is possible to analyze the relative merits of a variety of waste disposal techniques and to describe the probable consequences of each. Environments of consolidated rocks, such as granites, sandstones, and limestones, pose problems in addition to those related to unconsolidated or granular porous media in defining the fluid‐flow regimes that involve joint patterns, fracture patterns, solutional openings, and the rock structure. The consequences of ground‐water contamination can be just as damaging to water users as the pollution of surface streams. In fact it can be argued that the consequences are far more damaging because they persist over much longer periods of time after the contaminating source has been eliminated. It would appear prudent, therefore, to guard against contamination of the ground‐water resource in the first instance, rather than to engage in long expensive rehabilitation measures after the damage has been done. In 1960 Graham Walton presented data concerning contamination, by sewage or other man‐made wastes, of surface and underground waters. The circumstances attending the reported incidents of contamination, especially those involving ground‐water supplies, have aided materially in the choice of a few principles and ideas that will identify the role of some significant hydrologic factors in the underground movement of fluid wastes. Walton's discussion of ground‐water contamination refers often to physical settings into which fluid wastes are discharged at or near the land surface into cesspools, tile‐drain fields, and holding ponds. Furthermore, most reported instances of ground‐water contamination have taken place in relatively humid.
","language":"English","publisher":"NGWA The Groundwater Association","doi":"10.1111/j.1745-6584.1964.tb01739.x","usgsCitation":"Brown, R., 1964, Hydrologic factors pertinent to ground‐water contamination: Groundwater, v. 2, no. 1, p. 5-12, https://doi.org/10.1111/j.1745-6584.1964.tb01739.x.","productDescription":"8 p.","startPage":"5","endPage":"12","costCenters":[],"links":[{"id":386191,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"2","issue":"1","noUsgsAuthors":false,"publicationDate":"2006-07-06","publicationStatus":"PW","contributors":{"authors":[{"text":"Brown, R.","contributorId":101419,"corporation":false,"usgs":true,"family":"Brown","given":"R.","affiliations":[],"preferred":false,"id":816940,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":37483,"text":"37483 - 1964 - Waterfowl status report, 1964","interactions":[],"lastModifiedDate":"2014-07-15T13:33:00","indexId":"37483","displayToPublicDate":"1964-01-01T13:31:20","publicationYear":"1964","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":83,"text":"Special Scientific Report - Wildlife","active":false,"publicationSubtype":{"id":1}},"seriesNumber":"86","title":"Waterfowl status report, 1964","docAbstract":"No abstract available.","language":"English","publisher":"U.S. Fish and Wildlife Service","publisherLocation":"Washington, D.C.","usgsCitation":"Hansen, H., 1964, Waterfowl status report, 1964: Special Scientific Report - Wildlife 86, ii, 142 p.","productDescription":"ii, 142 p.","numberOfPages":"144","costCenters":[],"links":[{"id":290141,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53c64debe4b0001bd51477da","contributors":{"authors":[{"text":"Hansen, Henry A.","contributorId":15533,"corporation":false,"usgs":true,"family":"Hansen","given":"Henry A.","affiliations":[],"preferred":false,"id":218149,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":846,"text":"846 - 1964 - Water resources data for Indiana","interactions":[],"lastModifiedDate":"2014-08-05T13:21:31","indexId":"846","displayToPublicDate":"1964-01-01T13:20:04","publicationYear":"1964","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"title":"Water resources data for Indiana","docAbstract":"No abstract available.","language":"English","publisher":"U.S. Department of the Interior","publisherLocation":"Indianapolis, IN","doi":"10.3133/846","issn":"0364-4340","collaboration":"Prepared in cooperation with the State of Indiana and other State and Federal agencies.","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1964, Water resources data for Indiana, https://doi.org/10.3133/846.","costCenters":[],"links":[{"id":291702,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"country":"United States","state":"Indiana","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -88.0979,37.7717 ], [ -88.0979,41.7607 ], [ -84.7847,41.7607 ], [ -84.7847,37.7717 ], [ -88.0979,37.7717 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53e1efe4e4b0fe532be2dec4","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":527765,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ]}