{"pageNumber":"6696","pageRowStart":"167375","pageSize":"25","recordCount":184617,"records":[{"id":85343,"text":"85343 - 1964 - Adventuresome waterfowl","interactions":[],"lastModifiedDate":"2012-02-02T00:04:03","indexId":"85343","displayToPublicDate":"1964-01-01T00:00:00","publicationYear":"1964","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"title":"Adventuresome waterfowl","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Waterfowl tomorrow","largerWorkSubtype":{"id":4,"text":"Other Government Series"},"language":"English","publisher":"U.S. Fish and Wildlife Service","publisherLocation":"Washington, DC","usgsCitation":"Mendall, H.L., and Nelson, H., 1964, Adventuresome waterfowl, chap. <i>of</i> Waterfowl tomorrow, p. 305-311 [770 pp.].","productDescription":"p. 305-311 [770 pp.]","costCenters":[{"id":480,"text":"Northern Prairie Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":128709,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b03e4b07f02db698ec3","contributors":{"editors":[{"text":"Linduska, J.P.","contributorId":64308,"corporation":false,"usgs":true,"family":"Linduska","given":"J.P.","email":"","affiliations":[],"preferred":false,"id":504426,"contributorType":{"id":2,"text":"Editors"},"rank":1}],"authors":[{"text":"Mendall, H. L.","contributorId":29352,"corporation":false,"usgs":true,"family":"Mendall","given":"H.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":295936,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Nelson, H.K.","contributorId":21489,"corporation":false,"usgs":true,"family":"Nelson","given":"H.K.","email":"","affiliations":[],"preferred":false,"id":295935,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":1014052,"text":"1014052 - 1964 - Pseudomonadales as fish pathogens","interactions":[],"lastModifiedDate":"2012-02-02T00:04:22","indexId":"1014052","displayToPublicDate":"1964-01-01T00:00:00","publicationYear":"1964","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1385,"text":"Developments in Industrial Microbiology","active":true,"publicationSubtype":{"id":10}},"title":"Pseudomonadales as fish pathogens","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Developments in Industrial Microbiology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","collaboration":"143a/FH","usgsCitation":"Bullock, G.L., 1964, Pseudomonadales as fish pathogens: Developments in Industrial Microbiology, v. 5, p. 101-108.","productDescription":"p. 101-108","startPage":"101","endPage":"108","numberOfPages":"8","costCenters":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"links":[{"id":131457,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"5","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a8ae4b07f02db651509","contributors":{"authors":[{"text":"Bullock, G. L.","contributorId":69498,"corporation":false,"usgs":true,"family":"Bullock","given":"G.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":319689,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":1014138,"text":"1014138 - 1964 - Selected topics on bacterial fish diseases","interactions":[],"lastModifiedDate":"2012-02-02T00:04:30","indexId":"1014138","displayToPublicDate":"1964-01-01T00:00:00","publicationYear":"1964","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1164,"text":"Canadian Fish Culturist","active":true,"publicationSubtype":{"id":10}},"title":"Selected topics on bacterial fish diseases","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Canadian Fish Culturist","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","collaboration":"144/FH","usgsCitation":"Snieszko, S.F., 1964, Selected topics on bacterial fish diseases: Canadian Fish Culturist, v. 32, p. 19-24.","productDescription":"p. 19-24","startPage":"19","endPage":"24","numberOfPages":"6","costCenters":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"links":[{"id":132254,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"32","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a01e4b07f02db5f8004","contributors":{"authors":[{"text":"Snieszko, S. F.","contributorId":13169,"corporation":false,"usgs":true,"family":"Snieszko","given":"S.","middleInitial":"F.","affiliations":[],"preferred":false,"id":319852,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":1014137,"text":"1014137 - 1964 - Remarks on some facets of epizootiology of bacterial fish diseases","interactions":[],"lastModifiedDate":"2012-02-02T00:04:30","indexId":"1014137","displayToPublicDate":"1964-01-01T00:00:00","publicationYear":"1964","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1385,"text":"Developments in Industrial Microbiology","active":true,"publicationSubtype":{"id":10}},"title":"Remarks on some facets of epizootiology of bacterial fish diseases","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Developments in Industrial Microbiology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","collaboration":"143b/FH","usgsCitation":"Snieszko, S.F., 1964, Remarks on some facets of epizootiology of bacterial fish diseases: Developments in Industrial Microbiology, v. 5, p. 97-100.","productDescription":"p. 97-100","startPage":"97","endPage":"100","numberOfPages":"4","costCenters":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"links":[{"id":132253,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"5","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a5fe4b07f02db634432","contributors":{"authors":[{"text":"Snieszko, S. F.","contributorId":13169,"corporation":false,"usgs":true,"family":"Snieszko","given":"S.","middleInitial":"F.","affiliations":[],"preferred":false,"id":319851,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":34971,"text":"b1178 - 1964 - Stratigraphy and petrography of the Pybus-Gambier area, Admiralty Island, Alaska","interactions":[{"subject":{"id":14707,"text":"ofr6189 - 1961 - Structure and stratigraphy of the Pybus-Gambier area, Alaska","indexId":"ofr6189","publicationYear":"1961","noYear":false,"title":"Structure and stratigraphy of the Pybus-Gambier area, Alaska"},"predicate":"SUPERSEDED_BY","object":{"id":34971,"text":"b1178 - 1964 - Stratigraphy and petrography of the Pybus-Gambier area, Admiralty Island, Alaska","indexId":"b1178","publicationYear":"1964","noYear":false,"title":"Stratigraphy and petrography of the Pybus-Gambier area, Admiralty Island, Alaska"},"id":1}],"lastModifiedDate":"2023-03-17T18:40:35.707136","indexId":"b1178","displayToPublicDate":"1964-01-01T00:00:00","publicationYear":"1964","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":306,"text":"Bulletin","code":"B","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1178","title":"Stratigraphy and petrography of the Pybus-Gambier area, Admiralty Island, Alaska","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/b1178","usgsCitation":"Loney, R.A., 1964, Stratigraphy and petrography of the Pybus-Gambier area, Admiralty Island, Alaska: U.S. Geological Survey Bulletin 1178, Report: vi, 103 p.; 2 Plates: 35.50 x 21.00 inches and 31.50 x 19.25 inches, https://doi.org/10.3133/b1178.","productDescription":"Report: vi, 103 p.; 2 Plates: 35.50 x 21.00 inches and 31.50 x 19.25 inches","costCenters":[],"links":[{"id":109464,"rank":5,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_20944.htm","linkFileType":{"id":5,"text":"html"},"description":"20944"},{"id":62920,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1178/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":62919,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1178/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":62921,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/1178/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":164863,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/1178/report-thumb.jpg"}],"country":"United States","state":"Alaska","otherGeospatial":"Admiralty Island, Pybus-Gambier area","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -134.333,\n              57.5\n            ],\n            [\n              -134.333,\n              57.25\n            ],\n            [\n              -133.667,\n              57.25\n            ],\n            [\n              -133.667,\n              57.5\n            ],\n            [\n              -134.333,\n              57.5\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1be4b07f02db6a8b33","contributors":{"authors":[{"text":"Loney, R. A.","contributorId":90757,"corporation":false,"usgs":true,"family":"Loney","given":"R.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":213911,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70010464,"text":"70010464 - 1964 - Minor-element composition and organic carbon content of marine and nonmarine shales of Late Cretaceous age in the western interior of the United States","interactions":[],"lastModifiedDate":"2020-11-24T00:56:34.558115","indexId":"70010464","displayToPublicDate":"1964-01-01T00:00:00","publicationYear":"1964","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1759,"text":"Geochimica et Cosmochimica Acta","active":true,"publicationSubtype":{"id":10}},"title":"Minor-element composition and organic carbon content of marine and nonmarine shales of Late Cretaceous age in the western interior of the United States","docAbstract":"<p>The composition of nonmarine shales of Cretaceous age that contain less than 1 per cent organic carbon is assumed to represent the inherited minor-element composition of clayey sediments delivered to the Cretaceous sea that occupied the western interior region of North America. Differences in minor-element content between these samples and samples of</p><dl class=\"list\"><dt class=\"list-label\">1.</dt><dd class=\"list-description\"><p>(a) nonmarine carbonaceous shales (1 to 17 per cent organic carbon),</p></dd><dt class=\"list-label\">2.</dt><dd class=\"list-description\"><p>(b) nearshore marine shales (less than 1 per cent organic carbon), and</p></dd><dt class=\"list-label\">3.</dt><dd class=\"list-description\"><p>(c) offshore marine shales (as much as 8 per cent organic carbon), all of the same age, reveal certain aspects of the role played by clay minerals and organic materials in affecting the minor-element composition of the rocks.</p></dd></dl><p>The organic carbon in the nonmarine rocks occurs in disseminated coaly plant remains. The organic carbon in the marine rocks occurs predominantly in humic material derived from terrestrial plants. The close similarity in composition between the organic isolates from the marine samples and low-rank coal suggests that the amount of marine organic material in these rocks is small.</p><p>The minor-element content of the two kinds of nonmarine shales is the same despite the relatively large amount of organic carbon in the carbonaceous shales. The nearshore marine shales, however, contain larger median amounts of arsenic, boron, chromium, vanadium and zinc than do the nonmarine rocks; and the offshore marine shales contain even larger amounts of these elements. Cobalt, molybdenum, lead and zirconium show insignificant differences in median content between the nonmarine and marine rocks, although as much as 25 ppm molybdenum is present in some offshore marine samples. The gallium content is lower in the marine than in the nonmarine samples. Copper and selenium contents of the two kinds of nonmarine rocks and the nearshore marine samples are the same, but those of the offshore samples are larger.</p><p>In general, arsenic, chromium, copper, molybdenum, selenium, vanadium and zinc are concentrated in those offshore marine samples having the largest amounts of organic carbon, but samples with equal amounts of vanadium, for instance, may differ by a factor of 3 in their amount of organic carbon. Arsenic and molybdenum occur in some samples chiefly in syngenetic pyrite but also are present in relatively large amounts in samples that contain little pyrite.</p><p>The data on nonmarine carbonaceous shales indicate that organic matter of terrestrial origin in marine shales contributes little to the minor-element content of such rocks. It is possible that marine organic matter, even though seemingly small in amount in marine shales, contributes to the minor-element composition of the shales. In addition to any such contribution, however, the great effectiveness in sorption processes of humic materials in conjunction with clay minerals suggests that such processes must have played an important role as these materials moved from the relatively dilute solutions of the nonmarine environment to the relatively concentrated solution of sea water. The volumes of sea water sufficient to supply for sorption the amounts of most minor elements in the offshore marine samples are insignificant compared to the volumes of water with which the clay and organic matter were in contact during their transportation and sedimentation. Consequently, the chemical characteristics of the environment in which the clay minerals and organic matter accumulated and underwent diagenesis probably were the most important factors in controlling the degree to which sorption processes and the formation of syngenetic minerals affected the final composition of the rocks.</p>","language":"English","publisher":"Elsevier","doi":"10.1016/0016-7037(64)90008-0","issn":"00167037","usgsCitation":"Tourtelot, H.A., 1964, Minor-element composition and organic carbon content of marine and nonmarine shales of Late Cretaceous age in the western interior of the United States: Geochimica et Cosmochimica Acta, v. 28, no. 10-11, p. 1579-1604, https://doi.org/10.1016/0016-7037(64)90008-0.","productDescription":"26 p.","startPage":"1579","endPage":"1604","numberOfPages":"26","costCenters":[],"links":[{"id":219008,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"28","issue":"10-11","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a5b29e4b0c8380cd6f38b","contributors":{"authors":[{"text":"Tourtelot, H. A.","contributorId":79140,"corporation":false,"usgs":true,"family":"Tourtelot","given":"H.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":358984,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":1007574,"text":"1007574 - 1964 - 1,1' diacetyl-1,1'-dihydro-4,4' bipyridine and the yellow and colorless modifications of 1,1'-diacetyl-1,1',4,4'-tetrahydro-4,4' bipyridine","interactions":[],"lastModifiedDate":"2013-02-23T21:58:33","indexId":"1007574","displayToPublicDate":"1964-01-01T00:00:00","publicationYear":"1964","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2408,"text":"Journal of Organic Chemistry","active":true,"publicationSubtype":{"id":10}},"title":"1,1' diacetyl-1,1'-dihydro-4,4' bipyridine and the yellow and colorless modifications of 1,1'-diacetyl-1,1',4,4'-tetrahydro-4,4' bipyridine","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Journal of Organic Chemistry","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"American Chemical Society","doi":"10.1021/jo01031a016","usgsCitation":"Nielsen, A., Moore, D.W., Muha, G., and Highberg, K., 1964, 1,1' diacetyl-1,1'-dihydro-4,4' bipyridine and the yellow and colorless modifications of 1,1'-diacetyl-1,1',4,4'-tetrahydro-4,4' bipyridine: Journal of Organic Chemistry, v. 29, no. 8, p. 2175-2179, https://doi.org/10.1021/jo01031a016.","startPage":"2175","endPage":"2179","numberOfPages":"5","costCenters":[{"id":651,"text":"Western Ecological Research Center","active":true,"usgs":true}],"links":[{"id":268064,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1021/jo01031a016"},{"id":130194,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"29","issue":"8","noUsgsAuthors":false,"publicationDate":"2002-05-01","publicationStatus":"PW","scienceBaseUri":"4f4e4acce4b07f02db67e55e","contributors":{"authors":[{"text":"Nielsen, A.T.","contributorId":62551,"corporation":false,"usgs":true,"family":"Nielsen","given":"A.T.","email":"","affiliations":[],"preferred":false,"id":315650,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Moore, D. W.","contributorId":93431,"corporation":false,"usgs":true,"family":"Moore","given":"D.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":315653,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Muha, G.M.","contributorId":78687,"corporation":false,"usgs":true,"family":"Muha","given":"G.M.","email":"","affiliations":[],"preferred":false,"id":315651,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Highberg, K.","contributorId":90673,"corporation":false,"usgs":true,"family":"Highberg","given":"K.","email":"","affiliations":[],"preferred":false,"id":315652,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70010489,"text":"70010489 - 1964 - Submicroscopic spherules and color of tektites","interactions":[],"lastModifiedDate":"2020-11-24T00:49:35.2133","indexId":"70010489","displayToPublicDate":"1964-01-01T00:00:00","publicationYear":"1964","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1759,"text":"Geochimica et Cosmochimica Acta","active":true,"publicationSubtype":{"id":10}},"title":"Submicroscopic spherules and color of tektites","docAbstract":"<div id=\"abstracts\" class=\"Abstracts u-font-serif\"><div id=\"aep-abstract-id5\" class=\"abstract author\"><div id=\"aep-abstract-sec-id6\"><p>Magnetic susceptibility measurements of 18 tektites from various strewn fields have been made as a function of temperature from 77°K to room temperature. A relatively large temperature-independent component of the magnetic susceptibility was observed in all cases, and an analysis of the data shows that this component is the result of submicroscopic iron spherules in the tektites. An analysis of the color of tektites in terms of the magnetic measurements and also of the optical absorption spectra suggests that the basic color of all tektites is green or greenish-blue, and that the brown to black coloration in some tektites is due to finely dispersed Fe<sub>2</sub>O<sub>3</sub><span>&nbsp;</span>and/or many metallic spherules, both probably of colloidal size.</p></div></div></div>","language":"English","publisher":"Elsevier","doi":"10.1016/0016-7037(64)90045-6","issn":"00167037","usgsCitation":"Thorpe, A.N., and Senftle, F.E., 1964, Submicroscopic spherules and color of tektites: Geochimica et Cosmochimica Acta, v. 28, no. 6, 15 p., https://doi.org/10.1016/0016-7037(64)90045-6.","productDescription":"15 p.","costCenters":[],"links":[{"id":219304,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"28","issue":"6","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505b9d43e4b08c986b31d736","contributors":{"authors":[{"text":"Thorpe, A. N.","contributorId":53504,"corporation":false,"usgs":true,"family":"Thorpe","given":"A.","email":"","middleInitial":"N.","affiliations":[],"preferred":false,"id":359046,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Senftle, F. E.","contributorId":47788,"corporation":false,"usgs":true,"family":"Senftle","given":"F.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":359045,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70010488,"text":"70010488 - 1964 - Ignition to concentrate shelled organisms in plankton samples","interactions":[],"lastModifiedDate":"2023-09-26T16:02:08.319044","indexId":"70010488","displayToPublicDate":"1964-01-01T00:00:00","publicationYear":"1964","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1372,"text":"Deep-Sea Research and Oceanographic Abstracts","active":true,"publicationSubtype":{"id":10}},"title":"Ignition to concentrate shelled organisms in plankton samples","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"Elsevier","doi":"10.1016/0011-7471(64)90006-3","usgsCitation":"Sachs, K.N., Cifelli, R., and Bowen, V.T., 1964, Ignition to concentrate shelled organisms in plankton samples: Deep-Sea Research and Oceanographic Abstracts, v. 11, no. 4, p. 621-622, https://doi.org/10.1016/0011-7471(64)90006-3.","productDescription":"2 p.","startPage":"621","endPage":"622","numberOfPages":"2","costCenters":[],"links":[{"id":219303,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"11","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a3869e4b0c8380cd6156a","contributors":{"authors":[{"text":"Sachs, K. N. Jr.","contributorId":36282,"corporation":false,"usgs":true,"family":"Sachs","given":"K.","suffix":"Jr.","email":"","middleInitial":"N.","affiliations":[],"preferred":false,"id":359042,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Cifelli, R.","contributorId":98875,"corporation":false,"usgs":true,"family":"Cifelli","given":"R.","email":"","affiliations":[],"preferred":false,"id":359044,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Bowen, V. T.","contributorId":49102,"corporation":false,"usgs":false,"family":"Bowen","given":"V.","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":359043,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":1013660,"text":"1013660 - 1964 - Comparison of various methods of hemoglobin determination on catfish blood","interactions":[],"lastModifiedDate":"2025-08-01T16:13:04.312016","indexId":"1013660","displayToPublicDate":"1964-01-01T00:00:00","publicationYear":"1964","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3196,"text":"Progressive Fish-Culturist","active":true,"publicationSubtype":{"id":10}},"title":"Comparison of various methods of hemoglobin determination on catfish blood","docAbstract":"<p>No abstract available.&nbsp;</p>","language":"English","publisher":"American Fisheries Society","doi":"10.1577/1548-8659(1964)26[11:COVMOH]2.0.CO;2","usgsCitation":"Larsen, H., 1964, Comparison of various methods of hemoglobin determination on catfish blood: Progressive Fish-Culturist, v. 26, no. 1, p. 11-15, https://doi.org/10.1577/1548-8659(1964)26[11:COVMOH]2.0.CO;2.","productDescription":"5 p.","startPage":"11","endPage":"15","costCenters":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"links":[{"id":130248,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"26","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1ee4b07f02db6aa765","contributors":{"authors":[{"text":"Larsen, H.N.","contributorId":101601,"corporation":false,"usgs":true,"family":"Larsen","given":"H.N.","email":"","affiliations":[],"preferred":false,"id":318990,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70010495,"text":"70010495 - 1964 - Geology and trace elements: Relation to Nutrition","interactions":[],"lastModifiedDate":"2012-03-12T17:18:18","indexId":"70010495","displayToPublicDate":"1964-01-01T00:00:00","publicationYear":"1964","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Geology and trace elements: Relation to Nutrition","docAbstract":"[No abstract available]","largerWorkTitle":"Science","language":"English","issn":"00368075","usgsCitation":"Canon, H., 1964, Geology and trace elements: Relation to Nutrition, <i>in</i> Science, v. 143, no. 3607, p. 704-706.","startPage":"704","endPage":"706","numberOfPages":"3","costCenters":[],"links":[{"id":219378,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"143","issue":"3607","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a2444e4b0c8380cd57f3e","contributors":{"authors":[{"text":"Canon, H.L.","contributorId":79362,"corporation":false,"usgs":true,"family":"Canon","given":"H.L.","email":"","affiliations":[],"preferred":false,"id":359059,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70010466,"text":"70010466 - 1964 - Catalytic determination of vanadium in water","interactions":[],"lastModifiedDate":"2020-11-24T00:53:16.979681","indexId":"70010466","displayToPublicDate":"1964-01-01T00:00:00","publicationYear":"1964","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":761,"text":"Analytical Chemistry","active":true,"publicationSubtype":{"id":10}},"title":"Catalytic determination of vanadium in water","docAbstract":"<div id=\"abstracts\" class=\"Abstracts u-font-serif\"><div id=\"ab005\" class=\"abstract author\" lang=\"en\"><div id=\"as005\"><p id=\"sp1005\"><span>A kinetic determination of V(V) as a catalyst was spectrophotometrically performed by using the indicator reaction of&nbsp;Gallamine&nbsp;blue (GB</span><sup>+</sup><span>) and&nbsp;bromate&nbsp;at pH 2.0. The reaction was followed by measuring absorbance change for a fixed-time of 3</span>&nbsp;min at 537&nbsp;<span>nm. The variables such as reagent concentration, pH, buffer concentration,&nbsp;ionic strength&nbsp;and temperature were optimized to improve the selectivity and sensitivity. Under the optimized conditions, the determination of V(V) was performed in the range 1–100</span>&nbsp;μg&nbsp;L<sup>−1</sup><span>&nbsp;</span>with limits of detection and quantification of 0.31 and 0.94&nbsp;μg&nbsp;L<sup>−1</sup><span>. The developed&nbsp;kinetic method&nbsp;is sufficiently sensitive, selective and simple. It was successfully applied to the speciative determination of total V and inorganic dissolved&nbsp;vanadium&nbsp;species, V(V) and V(IV) in environmental water samples. The oxidizing property of&nbsp;permanganate&nbsp;is used to differentiate between V(IV) and V(V) species. The V(IV) content was found by subtracting the V(V) content from those of total V. The recovery is above 95% for V(V) spiked samples. Additionally, the accuracy was validated by analysis of a certified water sample, CRM TMDA-53.3, and the results were in good agreement with the certified value.</span></p></div></div></div>","language":"English","publisher":"Elsevier","doi":"10.1016/j.arabjc.2012.06.006","issn":"00032700","usgsCitation":"Fishman, M.J., and Skougstad, M., 1964, Catalytic determination of vanadium in water: Analytical Chemistry, v. 36, no. 8, p. 1643-1646, https://doi.org/10.1016/j.arabjc.2012.06.006.","productDescription":"4 p.","startPage":"1643","endPage":"1646","numberOfPages":"4","costCenters":[],"links":[{"id":480367,"rank":1,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1016/j.arabjc.2012.06.006","text":"Publisher Index Page"},{"id":219071,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"36","issue":"8","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059f3b5e4b0c8380cd4b950","contributors":{"authors":[{"text":"Fishman, M. J.","contributorId":65069,"corporation":false,"usgs":true,"family":"Fishman","given":"M.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":358987,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Skougstad, M. W.","contributorId":59418,"corporation":false,"usgs":true,"family":"Skougstad","given":"M. W.","affiliations":[],"preferred":false,"id":358986,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70010494,"text":"70010494 - 1964 - Aromatic fluorine compounds. XII. N-(fluorophenyl) carbamates","interactions":[],"lastModifiedDate":"2025-02-27T17:04:20.785489","indexId":"70010494","displayToPublicDate":"1964-01-01T00:00:00","publicationYear":"1964","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2386,"text":"Journal of Medicinal Chemistry","active":true,"publicationSubtype":{"id":10}},"title":"Aromatic fluorine compounds. XII. N-(fluorophenyl) carbamates","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"American Chemical Society","doi":"10.1021/jm00334a041","issn":"00222623","usgsCitation":"Finger, G.C., Dickerson, D.R., Orlopp, D., and Ehrmantraut, J., 1964, Aromatic fluorine compounds. XII. N-(fluorophenyl) carbamates: Journal of Medicinal Chemistry, v. 7, no. 4, p. 572-573, https://doi.org/10.1021/jm00334a041.","productDescription":"2 p.","startPage":"572","endPage":"573","numberOfPages":"2","costCenters":[],"links":[{"id":219377,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"7","issue":"4","noUsgsAuthors":false,"publicationDate":"2002-05-01","publicationStatus":"PW","scienceBaseUri":"5059ed82e4b0c8380cd49857","contributors":{"authors":[{"text":"Finger, G. C.","contributorId":89277,"corporation":false,"usgs":true,"family":"Finger","given":"G.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":359058,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Dickerson, D. R.","contributorId":66837,"corporation":false,"usgs":true,"family":"Dickerson","given":"D.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":359057,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Orlopp, D.E.","contributorId":20890,"corporation":false,"usgs":true,"family":"Orlopp","given":"D.E.","email":"","affiliations":[],"preferred":false,"id":359055,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Ehrmantraut, J.W.","contributorId":44286,"corporation":false,"usgs":true,"family":"Ehrmantraut","given":"J.W.","email":"","affiliations":[],"preferred":false,"id":359056,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70010469,"text":"70010469 - 1964 - Equilibrium of talc with enstatite and quartz","interactions":[],"lastModifiedDate":"2020-11-24T00:52:13.099925","indexId":"70010469","displayToPublicDate":"1964-01-01T00:00:00","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":"Equilibrium of talc with enstatite and quartz","docAbstract":"<div class=\"panel-pane pane-highwire-panel-tabs-container article__body\"><div class=\"pane-content\"><div id=\"panels-ajax-tab-container-highwire_article_tabs\" class=\"panels-ajax-tab-container\" data-panels-ajax-tab-preloaded=\"jnl_sci_tab_art\"><div class=\"panels-ajax-tab-wrap-jnl_sci_tab_art\"><div class=\"panel-display panel-1col clearfix\"><div class=\"panel-panel panel-col\"><div><div class=\"panel-pane pane-highwire-markup\"><div class=\"pane-content\"><div class=\"highwire-markup\"><div id=\"content-block-markup\" data-highwire-cite-ref-tooltip-instance=\"highwire_reflinks_tooltip\" data-highwire-glossary-tooltip-instance=\"highwire_reflinks_tooltip\"><div class=\"article abstract-view \"><div id=\"abstract-1\" class=\"section abstract\"><p id=\"p-1\">A thermodynamic calculation of the vapor pressure of H<sub>2</sub>0 in equilibrium with talc gives p<sup>H<sub>2</sub>O</sup><span>&nbsp;</span>of one atmosphere at 718° ± 15°K in contradiction to the results of Mueller.</p></div></div><span id=\"related-urls\"></span></div></div></div></div></div></div></div></div></div></div></div>","language":"English","publisher":"AAAP","doi":"10.1126/science.143.3610.1057","issn":"00368075","usgsCitation":"Robie, R.A., 1964, Equilibrium of talc with enstatite and quartz: Science, v. 143, no. 3610, p. 1057-1057, https://doi.org/10.1126/science.143.3610.1057.","productDescription":"1 p.","startPage":"1057","endPage":"1057","costCenters":[],"links":[{"id":219074,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"143","issue":"3610","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a0a29e4b0c8380cd52210","contributors":{"authors":[{"text":"Robie, R. A.","contributorId":71237,"corporation":false,"usgs":true,"family":"Robie","given":"R.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":358992,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70010744,"text":"70010744 - 1964 - Infrared surveys of Hawaiian volcanoes","interactions":[],"lastModifiedDate":"2019-11-18T14:43:38","indexId":"70010744","displayToPublicDate":"1964-01-01T00:00:00","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":"Infrared surveys of Hawaiian volcanoes","docAbstract":"<p id=\"p-1\">Aerial infrared-sensor surveys of Kilauea volcano have depicted the areal extent and the relative intensity of abnormal thermal features in the caldera area of the volcano and along its associated rift zones. Many of these anomalies show correlation with visible steaming and reflect convective transfer of heat to the surface from subterranean sources. Structural details of the volcano, some not evident from surface observation, are also delineated by their thermal abnormalities. Several changes were observed in the patterns of infrared emission during the period of study; two such changes show correlation in location with subsequent eruptions, but the cause-and-effect relationship is uncertain.</p><p id=\"p-2\">Thermal anomalies were also observed on the southwest flank of Mauna Loa; images of other volcanoes on the island of Hawaii, and of Haleakala on the island of Maui, revealed no thermal abnormalities.</p><p id=\"p-3\">Approximately 25 large springs issuing into the ocean around the periphery of Hawaii have been detected.</p><p id=\"p-4\">Infrared emission varies widely with surface texture and composition, suggesting that similar observations may have value for estimating surface conditions on the moon or planets.</p>","language":"English","publisher":"American Association for the Advancement of Science","doi":"10.1126/science.146.3645.733","issn":"00368075","usgsCitation":"Fischer, W.A., Moxham, R., Polcyn, F., and Landis, G., 1964, Infrared surveys of Hawaiian volcanoes: Science, v. 146, no. 3645, p. 733-742, https://doi.org/10.1126/science.146.3645.733.","productDescription":"10 p.","startPage":"733","endPage":"742","numberOfPages":"10","costCenters":[{"id":222,"text":"Earth Resources Observation and Science (EROS) Center","active":true,"usgs":true}],"links":[{"id":219700,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":288982,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1126/science.146.3645.733"}],"country":"United States","state":"Hawai'i","otherGeospatial":"Haleakala, Kilauea, Mauna 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,{"id":70190800,"text":"70190800 - 1964 - Selected hydrologic data, upper Sevier River basin, Utah","interactions":[],"lastModifiedDate":"2017-09-14T12:50:52","indexId":"70190800","displayToPublicDate":"1964-01-01T00:00:00","publicationYear":"1964","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":5497,"text":"Utah Basic-Data Report","active":false,"publicationSubtype":{"id":2}},"seriesNumber":"8","title":"Selected hydrologic data, upper Sevier River basin, Utah","docAbstract":"<p>This report is intended to serve two purposes: (1) to make available to the public basic ground-water data useful in planning and studying development of water resources, and (2) to supplement an interpretive report that will be published later.</p><p>Records were collected during 1961-63 by the U.S. Geological Survey in cooperation with the Utah State Engineer as a part of the investigation of ground-water conditions in the upper Sevier River basin, in parts of Garfield, Iron, Kane, Piute, and Sevier Counties, Utah. The interpretive material will be published in a companion report by Carl H. Carpenter, Gerald B. Robinson, Jr., and Louis J. Bjorklund.</p><p>This report is most useful in predicting conditions likely to be found in areas that are being considered as well sites. The person considering the new well can spot the proposed site on plate 1 and examine the records of nearby wells and springs as shown in the tables. From table 1 he can find information on wells, including depth, diameter, water level, yield, drawdown, use of water, temperature of water, and depth of perforations. Table 2 gives information on springs such as yield, use of water, temperature, and improvements. From tables 1 and 2 he can note the type of material that yields water in the vicinity. Table 3 shows the historic fluctuations and trends of water levels. Table 4 shows the type of material penetrated by wells. From table 5 he can note the chemical quality of water from wells and springs, and from table 6, the chemical quality of surface water. If the reader decides from his examination that conditions are favorable, he can place an application to drill a well with the State Engineer. If the State Engineer believes unappropriated water is available, the application may be approved after minimum statutory requirements have been satisfied.</p><p>The report is also useful when planning large-scale developments of water supply. This and other uses of the report will be helped by use of the interpretive report upon its release.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Salt Lake City, UT","collaboration":"Prepared in cooperation with the Utah State Engineer","usgsCitation":"Carpenter, C.H., Robinson, G.B., and Bjorklund, L.J., 1964, Selected hydrologic data, upper Sevier River basin, Utah: Utah Basic-Data Report 8, 29 p.","productDescription":"29 p.","numberOfPages":"37","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":345770,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":345769,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://www.waterrights.utah.gov/cgi-bin/docview.exe?Folder=TP21-1-160&Title=Basic+Data+Report+8"}],"country":"United States","state":"Utah","county":"Garfield County, Iron County, Kane County, Piute County, Sevier County","otherGeospatial":"Sevier River basi","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"59bb953ae4b091459a578226","contributors":{"authors":[{"text":"Carpenter, Carl H.","contributorId":46074,"corporation":false,"usgs":true,"family":"Carpenter","given":"Carl","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":710428,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Robinson, Gerald B. Jr.","contributorId":91837,"corporation":false,"usgs":true,"family":"Robinson","given":"Gerald","suffix":"Jr.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":710429,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Bjorklund, Louis Jay","contributorId":21138,"corporation":false,"usgs":true,"family":"Bjorklund","given":"Louis","email":"","middleInitial":"Jay","affiliations":[],"preferred":false,"id":710430,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70190796,"text":"70190796 - 1964 - Ground-water data, Sevier Desert, Utah","interactions":[],"lastModifiedDate":"2017-09-14T11:38:12","indexId":"70190796","displayToPublicDate":"1964-01-01T00:00:00","publicationYear":"1964","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":5497,"text":"Utah Basic-Data Report","active":false,"publicationSubtype":{"id":2}},"seriesNumber":"9","title":"Ground-water data, Sevier Desert, Utah","docAbstract":"<p>This report is intended to serve two purposes: (1) to make available to the public basic ground-water data useful in planning and studying development of water resources, and (2) to supplement an interpretive report that will be published later.</p><p>Records were collected during the period 1935-64 by the U.S. Geological survey in cooperation with the Utah State Engineer as part of the investigation of ground-water conditions in the Sevier Desert, in Juab and Millard Counties, Utah. The interpretive material will be published in a companion report by R. W. Mower and R. D. Feltis.</p><p>This report is most useful in predicting conditions likely to be found in areas that are being considered as well sites. The person considering the new well can spot the proposed site on plate 1 and examine the records of nearby wells as shown in the tables and figures. From table 1 he can note such things as depth, diameter, water level, yield, use of water, temperature of water, and depth of perforations. By comparing the depth of perforations with the drillers' logs in table 3 he can note the type of material that yields water to the wells. Table 2 and figure 2 show the historic fluctuations and trends of water levels in the vicinity. From table 4 he can note the chemical quality of the water from wells in the vicinity. Table 5 shows the amount of water discharged during 1951-63 from the pumped irrigation, public supply, and industrial wells. If the reader decides from his examination that conditions are favorable, he can place an application to drill a well with the state Engineer. If the State Engineer believes unappropriated water is available, the application may be approved after minimum statutory requirements have been satisfied.</p><p>The report is also useful when planning large-scale developments of water supply. This and other uses of the report will be helped by use of the interpretive report upon its release.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Salt Lake City, UT","collaboration":"Prepared in cooperation with the Utah State Engineer","usgsCitation":"Mower, R.W., and Feltis, R.D., 1964, Ground-water data, Sevier Desert, Utah: Utah Basic-Data Report 9, 34 p.","productDescription":"34 p.","numberOfPages":"41","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":345766,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":345765,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://www.waterrights.utah.gov/cgi-bin/docview.exe?Folder=TP21-1-180&Title=Basic+Data+Report+9"}],"country":"United States","state":"Utah","otherGeospatial":"Sevier Desert","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"59bb953ae4b091459a578228","contributors":{"authors":[{"text":"Mower, Reed W.","contributorId":32503,"corporation":false,"usgs":true,"family":"Mower","given":"Reed","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":710423,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Feltis, Richard D.","contributorId":98773,"corporation":false,"usgs":true,"family":"Feltis","given":"Richard","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":710424,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70185924,"text":"70185924 - 1964 - Geometry of river channels: Discussion by William W. Emmett and Luna B. Leopold","interactions":[],"lastModifiedDate":"2017-03-29T14:27:05","indexId":"70185924","displayToPublicDate":"1964-01-01T00:00:00","publicationYear":"1964","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Geometry of river channels: Discussion by William W. Emmett and Luna B. Leopold","docAbstract":"<p>For many years river engineers and geomorphologists have sought a rationale for the general similarity that can be observed among river channels from various environments. Some aspects of this general comparability were noted a century ago by Playfair, and other aspects were examined in a more quantitative way approximately 10 yr ago by R. E. Horton. Such similarities with respect to the channel cross section and the associated hydraulic parameters and their changes downstream were studied by some of the engineers who attained prominence for their work on the self-adjusting irrigation canals of India, especially G. Lacy,<sup>15</sup> C. Inglis,<sup>16</sup> and T. Blench.<sup>17</sup> Among these men, canal characteristics were the principal objects of investigation, although natural river channels assumed an increasing share of the attention of the students of \"regime analysis,\" especially Blench. L. B. Leopold and T. Maddock<sup>18</sup> developed a scheme by which the average relationships among form and hydraulic parameters could be easily described, this description being the one on which the author chose to elaborate. </p>","largerWorkType":{"id":4,"text":"Book"},"largerWorkSubtype":{"id":12,"text":"Conference publication"},"language":"English","publisher":"American Society of Civil Engineers","publisherLocation":"ASCE Proceedings Paper 3846: ASCE Proceedings v.90, no.HY 5, pt.1","usgsCitation":"Emmett, W.W., and Leopold, L.B., 1964, Geometry of river channels: Discussion by William W. Emmett and Luna B. Leopold, v. 90, no. HY 5, p. 277-285.","productDescription":"9 p.","startPage":"277","endPage":"285","costCenters":[],"links":[{"id":338664,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"90","issue":"HY 5","publicComments":"This is a discussion of the following paper: <i>Geometry of river channels</i>, March, 1964, by Walter B. Langbein (Proc. Paper 3846)","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"58dcc831e4b02ff32c68578b","contributors":{"authors":[{"text":"Emmett, William W.","contributorId":68715,"corporation":false,"usgs":true,"family":"Emmett","given":"William","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":687101,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Leopold, Luna Bergere","contributorId":93884,"corporation":false,"usgs":true,"family":"Leopold","given":"Luna","email":"","middleInitial":"Bergere","affiliations":[],"preferred":false,"id":687102,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":52426,"text":"ofr64128 - 1964 - Ground-water reconnaissance in the Burnt River valley, Baker County, Oregon","interactions":[],"lastModifiedDate":"2025-12-04T19:36:52.263227","indexId":"ofr64128","displayToPublicDate":"1964-01-01T00:00:00","publicationYear":"1964","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"64-128","title":"Ground-water reconnaissance in the Burnt River valley, Baker County, Oregon","docAbstract":"<p>The Burnt River valley in southern Baker County, Oreg., is underlain by rocks that range in age from pre-Tertiary to Quaternary. The pre-Tertiary rocks consist mainly of argillites, schists, limestones, and intrusive igneous rocks, while the Tertiary rocks consist mainly of felsic and mafic volcanic tuffs, lava flows and breccias, and fluviolacustrine deposits. Quaternary rocks include terrace gravels of Pleistocene and Recent age, and stream-valley alluvium of Recent age. The rock units most widely exposed along the valley are the fluviolacustrine deposits of Miocene and Pliocene(?) age, which extend to depths of as much as a thousand feet below the valley floor, and the pre-Tertiary rocks.</p><p>Most of the rocks that underlie the valley are of relatively low permeability and yield only small to moderate quantities of water (generally less than 50 gpm) to wells. The fluviolacustrine deposits contain scattered lenses of relatively permeable sand and gravel, hut the unit as a whole is mainly silt and clay of low permeability. Two prospective irrigation wells in the area penetrated these deposits but were abandoned because of insufficient yield.</p><p>Perhaps the most permeable rock unit in the area is the Columbia River Basalt of Miocene and Pliocene(?) age. It is exposed extensively west of the main valley, but apparently occurs only' as discontinuous lenses beneath the valley floor.</p><p>Chemical analyses of water from seven wells in the area indicate that the ground waters have relatively large concentrations of dis-. solved mineral constituents. Water from two of the wells had excessive concentrations of boron and high sodium and salinity hazards with respect to use for irrigation.</p><p>Perhaps the most favorable site for a test irrigation well is about 8 to 10 miles east of Hereford, where the Columbia River Basalt apparently extends beneath, and is intercalated with, the fluviolacustrine deposits.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr64128","collaboration":"Prepared in cooperation with the U.S. Bureau of Reclamation","usgsCitation":"Price, D., 1964, Ground-water reconnaissance in the Burnt River valley, Baker County, Oregon: U.S. Geological Survey Open-File Report 64-128, Report: 31 p.; 2 Figures: 29.69 x 29.91 inches and 36.75 x 20.21 inches, https://doi.org/10.3133/ofr64128.","productDescription":"Report: 31 p.; 2 Figures: 29.69 x 29.91 inches and 36.75 x 20.21 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,{"id":70168893,"text":"b1160 - 1964 - Studies of pre-Selma Cretaceous core samples from the outcrop area in western Alabama","interactions":[{"subject":{"id":33633,"text":"b1160D - 1964 - A microfauna from the Coker formation, Alabama","indexId":"b1160D","publicationYear":"1964","noYear":false,"chapter":"D","title":"A microfauna from the Coker formation, Alabama"},"predicate":"IS_PART_OF","object":{"id":70168893,"text":"b1160 - 1964 - Studies of pre-Selma Cretaceous core samples from the outcrop area in western Alabama","indexId":"b1160","publicationYear":"1964","noYear":false,"title":"Studies of pre-Selma Cretaceous core samples from the outcrop area in western Alabama"},"id":1},{"subject":{"id":33769,"text":"b1160B - 1964 - Petrology of pre-Selma strata from core holes in western Alabama","indexId":"b1160B","publicationYear":"1964","noYear":false,"chapter":"B","title":"Petrology of pre-Selma strata from core holes in western Alabama"},"predicate":"IS_PART_OF","object":{"id":70168893,"text":"b1160 - 1964 - Studies of pre-Selma Cretaceous core samples from the outcrop area in western Alabama","indexId":"b1160","publicationYear":"1964","noYear":false,"title":"Studies of pre-Selma Cretaceous core samples from the outcrop area in western Alabama"},"id":2},{"subject":{"id":34057,"text":"b1160F - 1964 - General remarks on the pre-Selma Cretaceous strata of western Alabama","indexId":"b1160F","publicationYear":"1964","noYear":false,"chapter":"F","title":"General remarks on the pre-Selma Cretaceous strata of western Alabama"},"predicate":"IS_PART_OF","object":{"id":70168893,"text":"b1160 - 1964 - Studies of pre-Selma Cretaceous core samples from the outcrop area in western Alabama","indexId":"b1160","publicationYear":"1964","noYear":false,"title":"Studies of pre-Selma Cretaceous core samples from the outcrop area in western Alabama"},"id":3},{"subject":{"id":34940,"text":"b1160E - 1964 - A preliminary report on the pollen and spores of the pre-Selma Upper Cretaceous strata of western Alabama","indexId":"b1160E","publicationYear":"1964","noYear":false,"chapter":"E","title":"A preliminary report on the pollen and spores of the pre-Selma Upper Cretaceous strata of western Alabama"},"predicate":"IS_PART_OF","object":{"id":70168893,"text":"b1160 - 1964 - Studies of pre-Selma Cretaceous core samples from the outcrop area in western Alabama","indexId":"b1160","publicationYear":"1964","noYear":false,"title":"Studies of pre-Selma Cretaceous core samples from the outcrop area in western Alabama"},"id":4},{"subject":{"id":35282,"text":"b1160A - 1964 - General description of cores of pre-Selma Cretaceous strata in western Alabama","indexId":"b1160A","publicationYear":"1964","noYear":false,"chapter":"A","title":"General description of cores of pre-Selma Cretaceous strata in western Alabama"},"predicate":"IS_PART_OF","object":{"id":70168893,"text":"b1160 - 1964 - Studies of pre-Selma Cretaceous core samples from the outcrop area in western Alabama","indexId":"b1160","publicationYear":"1964","noYear":false,"title":"Studies of pre-Selma Cretaceous core samples from the outcrop area in western Alabama"},"id":5},{"subject":{"id":35920,"text":"b1160C - 1964 - Pre-Selma larger invertebrate fossils from well core samples in western Alabama","indexId":"b1160C","publicationYear":"1964","noYear":false,"chapter":"C","title":"Pre-Selma larger invertebrate fossils from well core samples in western Alabama"},"predicate":"IS_PART_OF","object":{"id":70168893,"text":"b1160 - 1964 - Studies of pre-Selma Cretaceous core samples from the outcrop area in western Alabama","indexId":"b1160","publicationYear":"1964","noYear":false,"title":"Studies of pre-Selma Cretaceous core samples from the outcrop area in western Alabama"},"id":6}],"lastModifiedDate":"2016-03-07T13:39:25","indexId":"b1160","displayToPublicDate":"1964-01-01T00:00:00","publicationYear":"1964","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":306,"text":"Bulletin","code":"B","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1160","title":"Studies of pre-Selma Cretaceous core samples from the outcrop area in western Alabama","docAbstract":"<p>In 1954 four core holes were drilled in the pre-Selma Cretaceous strata of the Alabama Coastal Plain in order to get unweathered samples within a few miles of the outcrops. During the next few years several specialists studied the cores, and their reports are published as consecutive parts of this bulletin.</p>\n<p>Watson H. Monroe, who spent many years studying the Coastal Plain strata in Alabama and Mississippi, conceived and supervised the drilling and planned the later studies. His earlier published report (W. H. Monroe, 1955, Cores of pre-Selma Cretaceous rocks in the outcrop area in western Alabama: Gulf Coast Geol. Societies Trans., v. 5, p. 11-37) contains a brief description of the stratigraphy, together with logs and other information regarding the core holes, and he has provided the introductory chapter to this bulletin. Richard E. Bergenback studied the petrology of the cores, which included finding the distribution of grain sizes, determining the mineralogy of the grains and the matrix of the sediments, and having X-Ray identifications made of the clay minerals. Norman F. Sohl studied the mollusks and other large fossils obtained from the cores and compared them with other faunal suites collected in Alaban1a and Texas. Esther R. Applin studied the sparse microfauna, comparing it with faunas obtained from deep wells downdip in Georgia, Alabama, and Mississippi and with outcrop samples fron1 Texas, and has described a new species of Foraminifera. Estella B. Leopold and Helen M. Pakiser obtained a large pollen and spore assemblage by digesting carbonaceous layers of some of the cores in acid; this flora includes much new material, which is not described here.</p>\n<p>The Bergenback, Sohl, and Applin reports discuss the probable environment in which the sediments accumulated. Louis C. Conant, who spent several years studying and mapping these sediments, has written a summary chapter integrating some of the surface and subsurface information.</p>\n<p>Quarter-cuts of the cores belonging to the U.S. National Museum have been deposited on indefinite loan with the Alabama Geological Survey at University, Ala., and with the Shell Oil Co. at Jackson, Miss. They are available there for inspection and study.</p>","language":"English","publisher":"U.S. G.P.O.","doi":"10.3133/b1160","usgsCitation":"Monroe, W.H., Bergenback, R.E., Sohl, N.F., Applin, E.R., Leopold, E.B., Pakiser, H.M., and Conant, L.C., 1964, Studies of pre-Selma Cretaceous core samples from the outcrop area in western Alabama: U.S. Geological Survey Bulletin 1160, Report: ix, 108 p.; Plate: 17 x 22.25 inches, https://doi.org/10.3133/b1160.","productDescription":"Report: ix, 108 p.; Plate: 17 x 22.25 inches","numberOfPages":"162","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":318661,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/b1160.jpg"},{"id":318660,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1160a/plate-1.pdf","text":"Plate 1","linkFileType":{"id":1,"text":"pdf"}},{"id":318659,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/1160/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"56deb472e4b015c306fb8a78","contributors":{"authors":[{"text":"Monroe, Watson Hiner","contributorId":93020,"corporation":false,"usgs":true,"family":"Monroe","given":"Watson","email":"","middleInitial":"Hiner","affiliations":[],"preferred":false,"id":622087,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bergenback, Richard E.","contributorId":65897,"corporation":false,"usgs":true,"family":"Bergenback","given":"Richard","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":622088,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Sohl, Norman F.","contributorId":27906,"corporation":false,"usgs":true,"family":"Sohl","given":"Norman","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":622089,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Applin, Esther R.","contributorId":40974,"corporation":false,"usgs":true,"family":"Applin","given":"Esther","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":622090,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Leopold, Estella B.","contributorId":30979,"corporation":false,"usgs":true,"family":"Leopold","given":"Estella","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":622091,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Pakiser, Helen M.","contributorId":167378,"corporation":false,"usgs":false,"family":"Pakiser","given":"Helen","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":622092,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Conant, Louis C.","contributorId":83921,"corporation":false,"usgs":true,"family":"Conant","given":"Louis","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":622093,"contributorType":{"id":1,"text":"Authors"},"rank":7}]}}
,{"id":36025,"text":"b1199C - 1964 - Bauxite deposits of the Tippah-Benton district, Mississippi","interactions":[],"lastModifiedDate":"2023-03-02T22:19:44.988522","indexId":"b1199C","displayToPublicDate":"1964-01-01T00:00:00","publicationYear":"1964","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":306,"text":"Bulletin","code":"B","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1199","chapter":"C","title":"Bauxite deposits of the Tippah-Benton district, Mississippi","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/b1199C","usgsCitation":"Tourtelot, H.A., 1964, Bauxite deposits of the Tippah-Benton district, Mississippi: U.S. Geological Survey Bulletin 1199, Report: iv, 31 p.; 2 Plates: 13.50 x 20.50 inches and 18.50 x 28.50 inches, https://doi.org/10.3133/b1199C.","productDescription":"Report: iv, 31 p.; 2 Plates: 13.50 x 20.50 inches and 18.50 x 28.50 inches","costCenters":[],"links":[{"id":63970,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/1199c/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":63969,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1199c/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":63968,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1199c/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":166769,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/1199c/report-thumb.jpg"},{"id":109491,"rank":5,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_20972.htm","linkFileType":{"id":5,"text":"html"},"description":"20972"}],"country":"United States","state":"Mississippi","otherGeospatial":"Tippah-Benton district","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -89.123,\n              34.888\n            ],\n            [\n              -89.123,\n              34.642\n            ],\n            [\n              -88.928,\n              34.642\n            ],\n            [\n              -88.928,\n              34.888\n            ],\n            [\n              -89.123,\n              34.888\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a6ce4b07f02db63e09f","contributors":{"authors":[{"text":"Tourtelot, Harry Allison","contributorId":77937,"corporation":false,"usgs":true,"family":"Tourtelot","given":"Harry","email":"","middleInitial":"Allison","affiliations":[],"preferred":false,"id":215635,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":87139,"text":"87139 - 1964 - White-fronts","interactions":[],"lastModifiedDate":"2017-10-20T09:44:48","indexId":"87139","displayToPublicDate":"1964-01-01T00:00:00","publicationYear":"1964","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3733,"text":"Waterfowl Tomorrow","active":true,"publicationSubtype":{"id":10}},"title":"White-fronts","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Waterfowl tomorrow","largerWorkSubtype":{"id":9,"text":"Other Report"},"language":"English","publisher":"U.S. Fish and Wildlife Service","publisherLocation":"Washington, DC","usgsCitation":"Dzubin, A., Miller, H., and Schildman, G., 1964, White-fronts: Waterfowl Tomorrow, p. 135-143.","productDescription":"9 p.","startPage":"135","endPage":"143","costCenters":[{"id":480,"text":"Northern Prairie Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":127812,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e1e4b07f02db5e488a","contributors":{"editors":[{"text":"Linduska, J.P.","contributorId":64308,"corporation":false,"usgs":true,"family":"Linduska","given":"J.P.","email":"","affiliations":[],"preferred":false,"id":504821,"contributorType":{"id":2,"text":"Editors"},"rank":1}],"authors":[{"text":"Dzubin, Alexander","contributorId":35673,"corporation":false,"usgs":true,"family":"Dzubin","given":"Alexander","email":"","affiliations":[],"preferred":false,"id":297457,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Miller, H.W.","contributorId":102825,"corporation":false,"usgs":true,"family":"Miller","given":"H.W.","email":"","affiliations":[],"preferred":false,"id":297458,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Schildman, G.V.","contributorId":8787,"corporation":false,"usgs":true,"family":"Schildman","given":"G.V.","email":"","affiliations":[],"preferred":false,"id":297456,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70175637,"text":"70175637 - 1964 - Chemical analyses of water from observation wells in the Edwards and associated limestones, San Antonio area, Texas, 1963","interactions":[],"lastModifiedDate":"2016-08-17T14:06:21","indexId":"70175637","displayToPublicDate":"1964-01-01T00:00:00","publicationYear":"1964","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":5177,"text":"Edwards Underground Water District Bulletin","active":true,"publicationSubtype":{"id":2}},"seriesNumber":"4","title":"Chemical analyses of water from observation wells in the Edwards and associated limestones, San Antonio area, Texas, 1963","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"Edwards Underground Water District","usgsCitation":"Garza, S., 1964, Chemical analyses of water from observation wells in the Edwards and associated limestones, San Antonio area, Texas, 1963: Edwards Underground Water District Bulletin 4, 15 p.","productDescription":"15 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":326723,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57b58abfe4b03bcb0104bb64","contributors":{"authors":[{"text":"Garza, Sergio","contributorId":88713,"corporation":false,"usgs":true,"family":"Garza","given":"Sergio","email":"","affiliations":[],"preferred":false,"id":645903,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":1000486,"text":"1000486 - 1964 - Bottom sediments of Saginaw Bay, Michigan","interactions":[],"lastModifiedDate":"2013-02-12T08:07:19","indexId":"1000486","displayToPublicDate":"1964-01-01T00:00:00","publicationYear":"1964","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2450,"text":"Journal of Sedimentary Petrology","active":true,"publicationSubtype":{"id":10}},"title":"Bottom sediments of Saginaw Bay, Michigan","docAbstract":"Saginaw Bay is a southwest extension of Lake Huron on the east shore of the Southern Peninsula of Michigan. It is a shallow-water derivative of the Pleistocene Lake Saginaw. Sixty-one bottom samples were collected on a semigrid pattern and analyzed physically. Findings were treated statistically. Sediments range in size from large pebbles to clay. Medium- to fine-grained clear quartz sand is common to all parts of the bay. Currents and wave action are primarily responsible for both median diameter and sorting distribution patterns. Only a very general correlation can be established between depth and median diameter. Heavy minerals occur in abundance locally and show an affinity to shallow-water areas subject to prevailing currents. Shape also locally determines heavy mineral concentrations. Only general conclusions can be established from roundness and sphericity and acid-soluble content. Increased organic content is correlative with quiet water environments. The shallow-water, heterogeneous nature of Saginaw Bay is not conducive to the recognition of sedimentary criteria suitable for correlations in other than a local environment.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Journal of Sedimentary Petrology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"SEPM Society for Sedimentary Geology","publisherLocation":"Tulsa, OK","doi":"10.1306/74D71000-2B21-11D7-8648000102C1865D","collaboration":"Out-of-print","usgsCitation":"Wood, L.E., 1964, Bottom sediments of Saginaw Bay, Michigan: Journal of Sedimentary Petrology, v. 34, no. 1, p. 173-184, https://doi.org/10.1306/74D71000-2B21-11D7-8648000102C1865D.","productDescription":"12 p.","startPage":"173","endPage":"184","numberOfPages":"12","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":131764,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":267262,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1306/74D71000-2B21-11D7-8648000102C1865D"}],"volume":"34","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ce4b07f02db5fcdf1","contributors":{"authors":[{"text":"Wood, Leonard E.","contributorId":73157,"corporation":false,"usgs":true,"family":"Wood","given":"Leonard","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":308612,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70175579,"text":"70175579 - 1964 - Records of wells and springs, water levels, and chemical quality of ground water in the East Portland area, Oregon","interactions":[],"lastModifiedDate":"2016-08-17T11:24:53","indexId":"70175579","displayToPublicDate":"1963-12-29T00:00:00","publicationYear":"1964","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":115,"text":"Ground Water Report","active":false,"publicationSubtype":{"id":2}},"title":"Records of wells and springs, water levels, and chemical quality of ground water in the East Portland area, Oregon","docAbstract":"<p><span class=\"EXLDetailsDisplayVal\">Data are presented on more than 300 <span class=\"searchword\">wells</span>, including many new ones whose <span class=\"searchword\">records</span> will not be a part of a forthcoming interpretative report on the occurrence of <span class=\"searchword\">ground</span> <span class=\"searchword\">water</span> in this <span class=\"searchword\">area</span>. A brief description of the geomorphic features is given, and the characteristics of the rock units are summarized in a table. Principal aquifers are beds of loose sand and gravel in the early Pliocene Troutdale Formation, late Pleistocene fluviolacustrine deposits, and Recent alluvium. Locally, Columbia River Basalt (Miocene) and the Boring Lava (late Pliocene to Pleistocene) yield substantial amounts of wate.. In addition to well <span class=\"searchword\">records</span> there are 124 driller's logs and a table of <span class=\"searchword\">chemical</span> analyses of the <span class=\"searchword\">ground</span> <span class=\"searchword\">water</span>.</span></p>","language":"English","usgsCitation":"Foxworthy, B., Hogenson, G., and Hampton, E.R., 1964, Records of wells and springs, water levels, and chemical quality of ground water in the East Portland area, Oregon: Ground Water Report.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":518,"text":"Oregon Water Science Center","active":true,"usgs":true}],"links":[{"id":326649,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Oregon","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57b58b57e4b03bcb0104bc4d","contributors":{"authors":[{"text":"Foxworthy, B. L.","contributorId":45686,"corporation":false,"usgs":true,"family":"Foxworthy","given":"B. L.","affiliations":[],"preferred":false,"id":645748,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hogenson, G.M.","contributorId":69957,"corporation":false,"usgs":true,"family":"Hogenson","given":"G.M.","affiliations":[],"preferred":false,"id":645749,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hampton, E. R.","contributorId":57038,"corporation":false,"usgs":true,"family":"Hampton","given":"E.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":645750,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
]}