No abstract available.
","language":"English","publisher":"U.S. Trout Farmers Association","usgsCitation":"Parisot, T., 1965, Infectious pancreatic necrosis-The trout farmers' dilemma: U.S. Trout News, v. 9, no. 5, p. 6-21.","productDescription":"2 p.","startPage":"6","endPage":"21","costCenters":[],"links":[{"id":313928,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"9","issue":"5","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"568e4916e4b0e7a44bc419eb","contributors":{"authors":[{"text":"Parisot, T. J.","contributorId":43014,"corporation":false,"usgs":true,"family":"Parisot","given":"T. J.","affiliations":[],"preferred":false,"id":587800,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":5220327,"text":"5220327 - 1965 - A simple animal support for convenient weighing","interactions":[],"lastModifiedDate":"2025-02-07T16:17:44.922706","indexId":"5220327","displayToPublicDate":"1965-10-11T00:00:00","publicationYear":"1965","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2508,"text":"Journal of Wildlife Management","active":true,"publicationSubtype":{"id":10}},"title":"A simple animal support for convenient weighing","docAbstract":"A simple animal support constructed of web belts to hold skittish pigs for weighing was developed. The support is easily made, noninjurious to the pigs, and compact, facilitating rapid, accurate weighing. With minor modifications, the support can probably be used in weighing other animals.","language":"English","publisher":"Wiley","doi":"10.2307/3798571","usgsCitation":"Pan, H., Caslick, J., Harke, D., and Decker, D., 1965, A simple animal support for convenient weighing: Journal of Wildlife Management, v. 29, no. 4, p. 890-891, https://doi.org/10.2307/3798571.","productDescription":"2 p.","startPage":"890","endPage":"891","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":487104,"rank":2,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.2307/3798571","text":"Publisher Index Page"},{"id":196879,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"29","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b17e4b07f02db6a651e","contributors":{"authors":[{"text":"Pan, H.P.","contributorId":41927,"corporation":false,"usgs":true,"family":"Pan","given":"H.P.","email":"","affiliations":[],"preferred":false,"id":331631,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Caslick, J.W.","contributorId":94407,"corporation":false,"usgs":true,"family":"Caslick","given":"J.W.","email":"","affiliations":[],"preferred":false,"id":331634,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Harke, D.T.","contributorId":78422,"corporation":false,"usgs":true,"family":"Harke","given":"D.T.","email":"","affiliations":[],"preferred":false,"id":331633,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Decker, D.G.","contributorId":59900,"corporation":false,"usgs":true,"family":"Decker","given":"D.G.","email":"","affiliations":[],"preferred":false,"id":331632,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":5222228,"text":"5222228 - 1965 - Epizootiologic studies on filarioids of the raccoon","interactions":[],"lastModifiedDate":"2025-02-07T16:26:50.198695","indexId":"5222228","displayToPublicDate":"1965-10-11T00:00:00","publicationYear":"1965","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2508,"text":"Journal of Wildlife Management","active":true,"publicationSubtype":{"id":10}},"title":"Epizootiologic studies on filarioids of the raccoon","docAbstract":"Filarioid worms (Dirofilaria immitis, D. tenuis, Dipetalonema procyonis, and D. llewellyni) were discovered in raccoons (Procyon lotar) in Maryland. Raccoons were trapped in lowland, upland, and agricultural-residential areas, which were further classified as stream borders, poorly drained, and well drained. Data on incidence of D. llewellyni were analyzed on basis of host distribution within these areas to indicate type of habitat in which one might seek the vector. It was concluded that exposure takes place in the spring of the year. The arthropod found associated most often with the raccoon in spring was Ixodes texanus. Larvae of this tick which were fed on infected raccoons presented no evidence of development of the microfilariae. Feeding experiments were also conducted with mosquitoes: Aedes aegypti, A. canadensis, A. sollicitans, A. triseriatus, A. vexans, Culex pipiens, Anopheles punctipennis, and A. quadrimaculatus. Although microfilariae remained alive and active in the gut contents of all these mosquitoes for 2 days, only in Aedes aegypti did they enter the hemocele, but no developmental changes were noted and all microfilariae were dead by the eighth day. Although the intermediate host of D. llewellyni was not determined, evaluation of the accumulated data provides criteria for seeking the vector. It appeared unlikely that exposure of the raccoons took place in the den or that the filarioids were transmitted by an ectoparasite commonly found in raccoon dens. The data suggest that the vector is available only early in spring, although there are infected raccoons throughout the year. Prevalence in juveniles was 21 percent; in subadults, 64 percent; in adults, 87 percent.
","language":"English","publisher":"Wiley","doi":"10.2307/3798544","usgsCitation":"Herman, C.M., and Price, D., 1965, Epizootiologic studies on filarioids of the raccoon: Journal of Wildlife Management, v. 29, no. 4, p. 694-699, https://doi.org/10.2307/3798544.","productDescription":"6 p.","startPage":"694","endPage":"699","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":196000,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Maryland","otherGeospatial":"Patuxent Wildlife Research Center","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -76.82499365611099,\n 39.06403824922501\n ],\n [\n -76.82499365611099,\n 39.05470892556758\n ],\n [\n -76.81260696233649,\n 39.05470892556758\n ],\n [\n -76.81260696233649,\n 39.06403824922501\n ],\n [\n -76.82499365611099,\n 39.06403824922501\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","volume":"29","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9ae4b07f02db65d601","contributors":{"authors":[{"text":"Herman, C. M.","contributorId":101335,"corporation":false,"usgs":true,"family":"Herman","given":"C.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":335856,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Price, D.L.","contributorId":94399,"corporation":false,"usgs":true,"family":"Price","given":"D.L.","email":"","affiliations":[],"preferred":false,"id":335855,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70205839,"text":"70205839 - 1965 - Structure, metamorphism, and plutonism in the south-central Klamath Mountains, California","interactions":[],"lastModifiedDate":"2019-10-08T07:29:05","indexId":"70205839","displayToPublicDate":"1965-10-07T14:17:13","publicationYear":"1965","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":"Structure, metamorphism, and plutonism in the south-central Klamath Mountains, California","docAbstract":"In the south-central Klamath Mountains 50 miles of the the north-trending central metamorphic belt and adjacent parts of the eastern Paleozoic and western Paleozoic and Triassic belts have been mapped and studied in detail. Within the central metamorphic belt a sequence of three lithologically distinctive metamorphic units has been recognized (from bottom to top): (1) siliceous metasedimentary rocks and greenstones of the Stuart Fork Formation; (2) the Salmon Hornblende Schist; and (3) siliceous, calcareous, and amphibolitic rocks, predominantly metasedimentary, of the Grouse Ridge Formation. The age of these metamorphic rocks is uncertain; they are known only to predate intrusion of Late Jurassic (Nevadan) granitic rocks. Ultramafic rocks, mainly alpine-type peridotites, were emplaced before the granitic rocks and occur primarily in a single large sheetlike body which separates the central metamorphic belt from the eastern Paleozoic belt. Granitic plutons, including quartz diorites, trondhjemites, granodiorites, diorites, and gabbros, in decreasing order of abundance, range in size from less than 1 to about 80 square miles in area.
Two orogenic phases in the central metamorphic belt have been distinguished by structural and textural features. A late deformation uniformly affected the metamorphic terrane and the ultramafic rocks but predated granitic rocks. It was accompanied by some metamorphism in the lower to middle greenchist facies and produced upright folds that trend south and plunge gently. An earlier phase affected the various rock units differentially; it produced widespread recumbent folding and upper greenschist- to amphibolite-facies metamorphism in Salmon and Grouse Ridge rocks, but involved the underlying Stuart Fork Formation less severely, producing at least local recumbent folding and lower greenschist-facies metamorphism. The preferred interpretation of this upward increase in structural complexity and metamorphic grade is that the Salmon-Grouse Ridge sequence is a thrust sheet which overrode the Stuart Fork rocks concurrently with emplacement of the ultramafic rocks during the culmination of early recumbent folding and metamorphism. Thrusting was then followed by upright folding during the waning stages of regional metamorphism. The first deformational phase, and possibly the second, occurred during late Paleozoic time as indicated by recent isotopic ages of Salmon Hornblende Schist.
","language":"English","publisher":"GSA","doi":"10.1130/0016-7606(1965)76[933:SMAPIT]2.0.CO;2","usgsCitation":"Davis, G.A., Holdaway, M.J., Lipman, P.W., and Romey, W.D., 1965, Structure, metamorphism, and plutonism in the south-central Klamath Mountains, California: Geological Society of America Bulletin, v. 76, no. 8, p. 933-966, https://doi.org/10.1130/0016-7606(1965)76[933:SMAPIT]2.0.CO;2.","productDescription":"34 p.","startPage":"933","endPage":"966","numberOfPages":"34","onlineOnly":"Y","costCenters":[{"id":617,"text":"Volcano Science Center","active":true,"usgs":true}],"links":[{"id":368069,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"California","otherGeospatial":"South-central Klamath Mountains","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -123.2281494140625,\n 40.88444793903562\n ],\n [\n -122.5250244140625,\n 40.88444793903562\n ],\n [\n -122.5250244140625,\n 41.6195489884308\n ],\n [\n -123.2281494140625,\n 41.6195489884308\n ],\n [\n -123.2281494140625,\n 40.88444793903562\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"76","issue":"8","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Davis, Gregory A.","contributorId":219570,"corporation":false,"usgs":false,"family":"Davis","given":"Gregory","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":772571,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Holdaway, M. J.","contributorId":98047,"corporation":false,"usgs":false,"family":"Holdaway","given":"M.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":772572,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Lipman, Peter W. 0000-0001-9175-6118 plipman@usgs.gov","orcid":"https://orcid.org/0000-0001-9175-6118","contributorId":3486,"corporation":false,"usgs":true,"family":"Lipman","given":"Peter","email":"plipman@usgs.gov","middleInitial":"W.","affiliations":[{"id":5079,"text":"Pacific Regional Director's Office","active":true,"usgs":true},{"id":617,"text":"Volcano Science Center","active":true,"usgs":true}],"preferred":true,"id":772573,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Romey, W. D.","contributorId":219571,"corporation":false,"usgs":false,"family":"Romey","given":"W.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":772574,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":70221199,"text":"70221199 - 1965 - Relations of fresh and salty ground water along the southeastern U. S. Atlantic Coast","interactions":[],"lastModifiedDate":"2021-06-04T21:19:48.616707","indexId":"70221199","displayToPublicDate":"1965-10-01T16:14:21","publicationYear":"1965","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3825,"text":"Groundwater","active":true,"publicationSubtype":{"id":10}},"title":"Relations of fresh and salty ground water along the southeastern U. S. Atlantic Coast","docAbstract":"Studies of the hydrogeologic environments and the dynamic and equilibrium relations of fresh and salt water in aquifers have been intensified at several places along the southeastern Atlantic Coast. Some salt-water problems involve the coastal water-table aquifer, and others involve parts of the artesian system.
On the sandy coastal islands of North Carolina, freshwater lenses under water-table conditions float on salt water. Salt-water contamination may take place by (1) lateral encroachment from the ocean and bay; (2) vertical encroachment from below; (3) overland inundation by ocean water during storms; and (4) downward percolation of salt spray and salt-bearing precipitation.
In the Savannah, Georgia, and South Carolina area, salt-water encroachment along two of five water-bearing zones in the principal artesian (limestone) aquifer has been caused by the decline of artesian pressure due to pumping. Some wells in the limestone at nearby Parris Island, South Carolina, yield salty water when overpumped. From Savannah southward at least to Fernandina, Florida, connate salty water occurs in the artesian aquifer below the fresh water. At Brunswick, Georgia, connate salty water is stratified between fresh-water bodies in the limestone aquifer above depths of 2,000 feet. Connate salty water has contaminated the aquifer between depths of 500 and 800 feet in a small area in the city.
Along the southeast Florida coast drainage canals have been the primary cause of salt-water contamination of the highly permeable Biscayne aquifer. Criteria have been established for the operation of salinity-control dams to prevent encroachment. The salt-water front in the aquifer along the coast is dynamically stable under natural conditions.
","language":"English","publisher":"NGWA The Groundwater Association","doi":"10.1111/j.1745-6584.1965.tb01224.x","usgsCitation":"Wait, R.L., and Callahan, J., 1965, Relations of fresh and salty ground water along the southeastern U. S. Atlantic Coast: Groundwater, v. 3, no. 4, p. 3-17, https://doi.org/10.1111/j.1745-6584.1965.tb01224.x.","productDescription":"15 p.","startPage":"3","endPage":"17","costCenters":[],"links":[{"id":386244,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","otherGeospatial":"southeastern U.S. Atlantic Coast","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -88.33007812499999,\n 24.926294766395593\n ],\n [\n -75.5859375,\n 24.926294766395593\n ],\n [\n -75.5859375,\n 37.23032838760384\n ],\n [\n -88.33007812499999,\n 37.23032838760384\n ],\n [\n -88.33007812499999,\n 24.926294766395593\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"3","issue":"4","noUsgsAuthors":false,"publicationDate":"2006-07-06","publicationStatus":"PW","contributors":{"authors":[{"text":"Wait, R. L.","contributorId":15988,"corporation":false,"usgs":true,"family":"Wait","given":"R.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":817037,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Callahan, J.T.","contributorId":100920,"corporation":false,"usgs":true,"family":"Callahan","given":"J.T.","email":"","affiliations":[],"preferred":false,"id":817038,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70221194,"text":"70221194 - 1965 - Tracing the continuity of pleistocene aquifers in northern New Jersey by seismic methods","interactions":[],"lastModifiedDate":"2021-06-04T20:20:08.257589","indexId":"70221194","displayToPublicDate":"1965-10-01T14:22:09","publicationYear":"1965","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3825,"text":"Groundwater","active":true,"publicationSubtype":{"id":10}},"title":"Tracing the continuity of pleistocene aquifers in northern New Jersey by seismic methods","docAbstract":"Seismic refraction measurements were used to draw a new bedrock contour map in Morris County, New Jersey, where the major ground‐water supplies are found in Quaternary sand and gravel deposits filling pre‐Pleistocene channels. Aquifer performance tests aided in tracing the continuity of the Quaternary aquifers in these channels. In one case, the lack of continuity between two wells substantiated the seismic prediction that two separate channels were involved. The success of the seismic exploration emphasizes the value of using such methods, so that test drilling can be devoted to exploring the more favorable areas for production wells.
","language":"English","publisher":"Wiley","doi":"10.1111/j.1745-6584.1965.tb01227.x","usgsCitation":"Gill, H., Vecchioli, J., and Bonini, W., 1965, Tracing the continuity of pleistocene aquifers in northern New Jersey by seismic methods: Groundwater, v. 3, no. 4, p. 33-35, https://doi.org/10.1111/j.1745-6584.1965.tb01227.x.","productDescription":"3 p.","startPage":"33","endPage":"35","costCenters":[],"links":[{"id":386239,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"New Jersey","otherGeospatial":"northern New Jersey","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -75.25634765624999,\n 40.17047886718109\n ],\n [\n -73.89404296874999,\n 40.17047886718109\n ],\n [\n -73.89404296874999,\n 41.40153558289848\n ],\n [\n -75.25634765624999,\n 41.40153558289848\n ],\n [\n -75.25634765624999,\n 40.17047886718109\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"3","issue":"4","noUsgsAuthors":false,"publicationDate":"2006-07-06","publicationStatus":"PW","contributors":{"authors":[{"text":"Gill, H.E.","contributorId":24330,"corporation":false,"usgs":true,"family":"Gill","given":"H.E.","email":"","affiliations":[],"preferred":false,"id":817028,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Vecchioli, John","contributorId":36113,"corporation":false,"usgs":true,"family":"Vecchioli","given":"John","email":"","affiliations":[],"preferred":false,"id":817029,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Bonini, W.E.","contributorId":168860,"corporation":false,"usgs":false,"family":"Bonini","given":"W.E.","email":"","affiliations":[],"preferred":false,"id":817030,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":5220469,"text":"5220469 - 1965 - Pox infection and a secondary cutaneous mycosis in a red-tailed tropicbird (Phaethon rubricauda)","interactions":[],"lastModifiedDate":"2022-10-26T14:22:21.881307","indexId":"5220469","displayToPublicDate":"1965-10-01T12:17:34","publicationYear":"1965","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1140,"text":"Bulletin of the Wildlife Disease Association","active":true,"publicationSubtype":{"id":10}},"displayTitle":"Pox infection and a secondary cutaneous mycosis in a red-tailed tropicbird (Phaethon rubricauda)","title":"Pox infection and a secondary cutaneous mycosis in a red-tailed tropicbird (Phaethon rubricauda)","docAbstract":"No abstract available.
","language":"English","publisher":"Wildlife Disease Association","doi":"10.7589/0090-3558-1.4.60","usgsCitation":"Locke, L.N., Wirtz, W.O., and Brown, E.E., 1965, Pox infection and a secondary cutaneous mycosis in a red-tailed tropicbird (Phaethon rubricauda): Bulletin of the Wildlife Disease Association, v. 1, no. 4, p. 60-61, https://doi.org/10.7589/0090-3558-1.4.60.","productDescription":"2 p.","startPage":"60","endPage":"61","numberOfPages":"2","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":193840,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Hawaii","otherGeospatial":"Sand Island, Midway Islands","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {\n \"stroke\": \"#555555\",\n \"stroke-width\": 2,\n \"stroke-opacity\": 1,\n \"fill\": \"#555555\",\n \"fill-opacity\": 0.3\n },\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -177.40018844604492,\n 28.190513153841668\n ],\n [\n -177.31470108032227,\n 28.190513153841668\n ],\n [\n -177.31470108032227,\n 28.223793792828708\n ],\n [\n -177.40018844604492,\n 28.223793792828708\n ],\n [\n -177.40018844604492,\n 28.190513153841668\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"1","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad3e4b07f02db681cf3","contributors":{"authors":[{"text":"Locke, L. N.","contributorId":73539,"corporation":false,"usgs":true,"family":"Locke","given":"L.","email":"","middleInitial":"N.","affiliations":[],"preferred":false,"id":331863,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wirtz, W. O. II","contributorId":43452,"corporation":false,"usgs":true,"family":"Wirtz","given":"W.","suffix":"II","email":"","middleInitial":"O.","affiliations":[],"preferred":false,"id":331861,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Brown, E. E.","contributorId":52287,"corporation":false,"usgs":true,"family":"Brown","given":"E.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":331862,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":1003274,"text":"1003274 - 1965 - Diuron, fenuron, monuron, neburon, and TCA mixtures as aquatic herbicides in fish habitats","interactions":[],"lastModifiedDate":"2026-03-18T16:17:56.420224","indexId":"1003274","displayToPublicDate":"1965-10-01T00:00:00","publicationYear":"1965","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3741,"text":"Weeds","active":true,"publicationSubtype":{"id":10}},"title":"Diuron, fenuron, monuron, neburon, and TCA mixtures as aquatic herbicides in fish habitats","docAbstract":"The substituted urea herbicides were rated according to their effectiveness as aquatic herbicides in this order: diuron [3-(3,4-dichlorophenyl)-1,1-dimethylurea], monuron [3-(p-chlorophenyl)-1,1-dimethylurea], neburon [1-butyl-3-(3,4-dichlorophenyl)-1-methlyurea] and TCA(trichloroacetic acid) mixtures with them. They showed greatest potential in controlling certain aquatic plants in pre-emergence and early postemergence applications. However, relatively high concentrations were required to control filamentous algae (Cladophora, Pithophora and Spirogyra), chara (Chara), coontail (Ceratophyllum), naiad (Najas), and pondweeds (Potamogeton) for periods of time exceeding three months and up to three years. Granular formulations achieved better distribution of herbicides for control of rooted aquatic plants along the margins of lakes and ponds. Wettable powder and liquid emulsifiable concentrates were superior to granular formulations for the control of algae and emergent or floating aquatic plants.
Monuron and fenuron were less toxic to fish than were diuron and neburon. The TCA mixtures were somewhat more toxic than the simple ureas. Some species of fish were more sensitive than others and fingerlings more sensitive than adults of the same species. Fish-food organisms were reduced appreciably in plastic enclosures at herbicidal concentrations.
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","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR046i001p00218","usgsCitation":"Oliver, H., 1965, The U. S. Geological Survey's Gravity program in California, Hawaii, Nevada, and Oregon: Eos, Transactions, American Geophysical Union, v. 46, no. 1, p. 218-222, https://doi.org/10.1029/TR046i001p00218.","productDescription":"5 p.","startPage":"218","endPage":"222","costCenters":[],"links":[{"id":387679,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"California, Hawaii, Nevada, 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\"}}]}","volume":"46","issue":"1","noUsgsAuthors":false,"publicationDate":"2014-08-18","publicationStatus":"PW","contributors":{"authors":[{"text":"Oliver, Howard W.","contributorId":78704,"corporation":false,"usgs":true,"family":"Oliver","given":"Howard W.","affiliations":[],"preferred":false,"id":820550,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70222558,"text":"70222558 - 1965 - Eclogites and eclogites: Their differences and similarities","interactions":[],"lastModifiedDate":"2021-08-04T12:45:13.592538","indexId":"70222558","displayToPublicDate":"1965-08-04T07:42:18","publicationYear":"1965","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1723,"text":"GSA Bulletin","active":true,"publicationSubtype":{"id":10}},"title":"Eclogites and eclogites: Their differences and similarities","docAbstract":"Eclogites are divisible into three groups based on mode of occurrence: Group A, inclusions in kimberlites, basalts, or layers in ultramafic rocks; Group B, bands or lenses within migmatite gneissic terrains; Group C, bands or lenses within alpine-type metamorphic rocks. The compositions range from olivine basalt for Group A to tholeiitic basalts for Group C. New analytical data on six eclogites from glaucophane schist terrains in California and New Caledonia now permit comparisons among the three eclogite types. The pyrope content of the garnets is distinctive for each group as follows: Group A, greater than 55 per cent py; Group B, 30–55 per cent py; Group C, less than 30 percent py. Pyroxenes coexisting with these garnets also reflect a compositional change related to their occurrence. The jadeite content progressively increases from Group A through Group B, whereas the diopside content decreases. A comparison of eclogites from different geologic occurrences but with similar bulk compositions demonstrates variation in Ca-Mg partition between coexisting garnet and pyroxene. The Ca/Mg ratio increases in garnet and decreases in pyroxene from Group A through Group B eclogites. This obvious difference in the Ca-Mg partition between coexisting garnet-pyroxene in eclogites of the same bulk composition indicates a broad range of pressure-temperature conditions obtained during crystallization. Experimental synthesis of eclogite-like material at high pressures and temperatures demonstrates that some eclogites may form in the earth's mantle, but naturally occurring Group C eclogites have coexisting garnet-pyroxene with distinct Ca/Mg ratios when compared to Group A or B eclogites of similar bulk composition. This difference in the Ca/Mg ratio must reflect the pressure-temperature conditions characterizing the glaucophane schist facies.
","language":"English","publisher":"Geological Society of America","doi":"10.1130/0016-7606(1965)76[483:EAETDA]2.0.CO;2","usgsCitation":"Coleman, R.G., Lee, D., Beatty, L.B., and Brannock, W.W., 1965, Eclogites and eclogites: Their differences and similarities: GSA Bulletin, v. 76, no. 5, p. 483-508, https://doi.org/10.1130/0016-7606(1965)76[483:EAETDA]2.0.CO;2.","productDescription":"26 p.","startPage":"483","endPage":"508","costCenters":[],"links":[{"id":387678,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"76","issue":"5","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Coleman, R. G.","contributorId":75170,"corporation":false,"usgs":true,"family":"Coleman","given":"R.","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":820546,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lee, Donald E.","contributorId":11615,"corporation":false,"usgs":true,"family":"Lee","given":"Donald E.","affiliations":[],"preferred":false,"id":820547,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Beatty, L. B.","contributorId":261744,"corporation":false,"usgs":false,"family":"Beatty","given":"L.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":820548,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Brannock, W. W.","contributorId":74504,"corporation":false,"usgs":true,"family":"Brannock","given":"W.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":820549,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":37706,"text":"37706 - 1965 - Big game inventory for 1964","interactions":[],"lastModifiedDate":"2014-07-22T13:09:56","indexId":"37706","displayToPublicDate":"1965-08-01T13:08:36","publicationYear":"1965","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":"470","title":"Big game inventory for 1964","docAbstract":"No abstract available.","language":"English","publisher":"U.S. Department of the Interior","publisherLocation":"Washington, D.C.","collaboration":"Compiled in the Bird and Mammal Laboratories, Division of Wildlife Research.","usgsCitation":"U.S. Division Of Wildlife Research, 1965, Big game inventory for 1964 (Revises Wildlife Leaflet 342 (1962).): Wildlife Leaflet 470, 4 p.","productDescription":"4 p.","numberOfPages":"4","temporalStart":"1964-01-01","temporalEnd":"1964-12-31","costCenters":[],"links":[{"id":290715,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"edition":"Revises Wildlife Leaflet 342 (1962).","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57ffcdb6e4b0824b2d175957","contributors":{"authors":[{"text":"U.S. Division Of Wildlife Research","contributorId":128226,"corporation":true,"usgs":false,"organization":"U.S. Division Of Wildlife Research","id":529674,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70161797,"text":"70161797 - 1965 - Virus diseases of the salmonidae in the western United States. III. Immunopathological aspects","interactions":[],"lastModifiedDate":"2016-01-06T11:06:59","indexId":"70161797","displayToPublicDate":"1965-08-01T12:15:00","publicationYear":"1965","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":801,"text":"Annals of the New York Academy of Sciences","active":true,"publicationSubtype":{"id":10}},"title":"Virus diseases of the salmonidae in the western United States. III. Immunopathological aspects","docAbstract":"The immune response among fish, from a phylogenetic standpoint, presents a progressive pattern of increasing development. The cyclostomes have been shown to have only feeble immunologic responsiveness. One of their number, the hagfish, appeared to be totally lacking in the ability to actively acquire antibodies.
Among the elasmobranchs, the sharks have received the most study immunologically. This group demonstrated a variable response to antigenic stimulation
Of the teleosts, the salmonids and the cyprinids have been the more frequent recipients of experimentally introduced antigens. These fishes, as well as other species of teleosts, are quite active and quite consistent in their response to various antigens.
","language":"English","publisher":" New York Academy of Sciences","publisherLocation":"New York, NY","doi":"10.1111/j.1749-6632.1965.tb14299.x","usgsCitation":"Klontz, G.W., Yasutake, W.T., and Parisot, T., 1965, Virus diseases of the salmonidae in the western United States. III. Immunopathological aspects: Annals of the New York Academy of Sciences, v. 126, no. 1, p. 531-542, https://doi.org/10.1111/j.1749-6632.1965.tb14299.x.","productDescription":"12 p.","startPage":"531","endPage":"542","numberOfPages":"12","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"links":[{"id":313923,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"126","issue":"1","noUsgsAuthors":false,"publicationDate":"2006-12-16","publicationStatus":"PW","scienceBaseUri":"568e493ee4b0e7a44bc41af5","contributors":{"authors":[{"text":"Klontz, George W.","contributorId":151065,"corporation":false,"usgs":false,"family":"Klontz","given":"George","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":587794,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Yasutake, William T.","contributorId":70444,"corporation":false,"usgs":true,"family":"Yasutake","given":"William","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":587795,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Parisot, T. J.","contributorId":43014,"corporation":false,"usgs":true,"family":"Parisot","given":"T. J.","affiliations":[],"preferred":false,"id":587796,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70210090,"text":"70210090 - 1965 - Adverse effects on birds of Phosphamidon applied to a Montana forest","interactions":[],"lastModifiedDate":"2020-05-13T19:37:17.744547","indexId":"70210090","displayToPublicDate":"1965-07-31T14:31:07","publicationYear":"1965","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2508,"text":"Journal of Wildlife Management","active":true,"publicationSubtype":{"id":10}},"title":"Adverse effects on birds of Phosphamidon applied to a Montana forest","docAbstract":"A field trial of Phosphamidon applied by aircraft in Montana against spruce budworm (Choristoneura fumiferana) had immediate adverse effects on birds. A 5,000-acre block of forested land was sprayed at the rate of 1 pound per acre. Some birds, including blue grouse (Dendragapus obscurus), were killed by the insecticide. Bird activity on the sprayed plot dropped to about one-quarter of the prespray level of activity while it increased on an unsprayed plot. Two sick blue grouse were caught by hand and held in captivity; one died and the other recovered. Analysis of grouse blood samples showed a marked inhibition of cholinesterase activity in the sick birds, followed by return of cholinesterase to normal in the surviving bird.
","language":"English","publisher":"Wiley","doi":"10.2307/3798057","usgsCitation":"Finley, R.B., 1965, Adverse effects on birds of Phosphamidon applied to a Montana forest: Journal of Wildlife Management, v. 29, no. 3, p. 580-591, https://doi.org/10.2307/3798057.","productDescription":"12 p.","startPage":"580","endPage":"591","costCenters":[],"links":[{"id":374797,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Montana","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -113.56842041015625,\n 46.80945943904218\n ],\n [\n -112.90924072265625,\n 46.80945943904218\n ],\n [\n -112.90924072265625,\n 47.11313066447019\n ],\n [\n -113.56842041015625,\n 47.11313066447019\n ],\n [\n -113.56842041015625,\n 46.80945943904218\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"29","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Finley, R. B. Jr.","contributorId":59357,"corporation":false,"usgs":true,"family":"Finley","given":"R.","suffix":"Jr.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":789065,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70222381,"text":"70222381 - 1965 - Isotopic ages of minerals from granitic rocks of the central Sierra Nevada and Inyo Mountains, California","interactions":[],"lastModifiedDate":"2021-07-26T13:18:56.627367","indexId":"70222381","displayToPublicDate":"1965-07-26T08:13:38","publicationYear":"1965","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1723,"text":"GSA Bulletin","active":true,"publicationSubtype":{"id":10}},"title":"Isotopic ages of minerals from granitic rocks of the central Sierra Nevada and Inyo Mountains, California","docAbstract":"Potassium-argon ages of biotite and hornblende from specimens of 17 granitic plutons in the central Sierra Nevada and the western Inyo Mountains, California, range from 69 to 183 m. y. The Mount Givens, Lamarck. and Round Valley Peak Granodiorites and related younger and more felsic quartz monzonites represent a pulse of magma emplaced in the general time interval of 80-90 million years ago, during Cretaceous time. Mineral ages of granitic rocks that flank these plutons on both the east and the west have been reduced during the emplacement of the Cretaceous intrusive rocks and are minimum ages for the time of crystallization. The ages of hornblende from the Tinemaha Granodiorite (150 to 180 m. y.) may approach crystallization dates. In conjunction with ages for other intrusive rocks in the Sierra Nevada and adjacent desert ranges they strongly suggest a magmatic episode during the Early Jurassic.
Duplicate potassium-argon age determinations on each of three samples from widely separated localities indicate that the age of the Bishop Tuff, California, is about 0.7 million years. Two of the samples are from the basal ash fall that preceded the ash flow eruptions; one of these two samples was collected within 1 m of the contact of the Bishop Tuff with the underlying Sherwin Till. The third sample is from near the present exposed surface of the Bishop Tuff. The minimum age of the Sherwin Till (Kansan?) is thus 0.7 million years. The samples used for previously published age determinations of about 1 million years were probably contaminated with older material. Paleomagnetic results from five widely separated localities indicate that the welded part of the Bishop Tuff became magnetized when the geomagnetic field was normal and that it may have cooled in several centuries or less. The Brunhes-Matuyama polarity epoch boundary is now uncertain in the range of 0.7 to 1.0 million years.
The sediments of a late glacial sag pond in Huerfano Park, south-central Colorado, have yielded a varied biota consisting of vertebrates, terrestrial and fresh-water mollusks, sponges, and pollen. Wood from the sediments has a radiocarbon age of 9600 ± 200 years. The vertebrate fauna contains the tooth of a prairie dog and the remains of frog, salamander, snake, and fish—all characteristic of present-day montane lakes and ponds and their margins in Colorado. The mollusks are all living species, and the fauna is dominated by gastropods. With the exception of one form (Vitrina alaskana Dall), whose known range does not extend as far south as Huerfano Park, the fauna is not significantly different from the mollusks living in the area today. The sediments also contain an abundant and unusually diversified sponge fauna in which as many as six species may be represented. A pollen spectrum from the sediments is composed of arboreal pollen characteristic of the present-day Transition Zone flora which, in Colorado, grows on the upper edge of the Great Plains and all of the foothills belt.
Vertical variation in the sediment types and the enclosed biota makes it possible to recreate the changing depositional environment and local climate throughout the life of the pond. The basal sediments, interbedded marl and clastic materials, are interpreted as indicating deposition during alternating wet and dry periods. A bed of nearly pure calcium carbonate marl, which reaches a thickness of 2 feet, forms the middle stratigraphic unit. It is highly fossiliferous and is thought to have been deposited during a warm dry period with relatively mild winters. The uppermost stratigraphic unit is a gray carbonaceous clay which filled the basin as vegetation encroached upon the lake and the lake itself was reduced to a marsh.
Because of the radiocarbon age and the reconstruction of the climate based upon faunal and sedimentological changes, the lower two stratigraphic units are thought to correlate with the Lubbock Subpluvial, and the uppermost unit, the gray carbonaceous clay, with the early part of the Yellow House Interval as described in the Llano Estacado, New Mexico.
","language":"English","publisher":"Geological Society of America","doi":"10.1130/0016-7606(1965)76[1203:BOALGR]2.0.CO;2","usgsCitation":"Kauffman, E., and McCulloch, D.S., 1965, Biota of a late glacial rocky mountain pond: GSA Bulletin, v. 76, no. 11, p. 1203-1232, https://doi.org/10.1130/0016-7606(1965)76[1203:BOALGR]2.0.CO;2.","productDescription":"30 p.","startPage":"1203","endPage":"1232","costCenters":[],"links":[{"id":387223,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Colorado","otherGeospatial":"Huerfano 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\"}}]}","volume":"76","issue":"11","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Kauffman, E.G.","contributorId":77676,"corporation":false,"usgs":true,"family":"Kauffman","given":"E.G.","email":"","affiliations":[],"preferred":false,"id":819447,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"McCulloch, David S. dmccullo@usgs.gov","contributorId":3100,"corporation":false,"usgs":true,"family":"McCulloch","given":"David","email":"dmccullo@usgs.gov","middleInitial":"S.","affiliations":[],"preferred":true,"id":819448,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70222060,"text":"70222060 - 1965 - Investigation of initial Sr87/Sr86 ratios in the Sierra Nevada Plutonic Province","interactions":[],"lastModifiedDate":"2021-07-16T13:00:54.153796","indexId":"70222060","displayToPublicDate":"1965-07-16T07:58:20","publicationYear":"1965","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1723,"text":"GSA Bulletin","active":true,"publicationSubtype":{"id":10}},"title":"Investigation of initial Sr87/Sr86 ratios in the Sierra Nevada Plutonic Province","docAbstract":"One to three whole-rock samples from each of more than a dozen discrete plutonic intrusions in the east-central Sierra Nevada batholith have been analyzed for Sr87/Sr86 and Rb/Sr ratios to obtain information on initial Sr87 abundances.
The initial Sr87/Sr86 ratios in the rock magmas forming this province appear to have been in the range 0.7073 ± .0010 in the majority of cases. This range is definitely higher than that found for modern alkali-type and tholeiite-type basalt magmas of oceanic regions, which commonly range between 0.703 and 0.705. However, it is much lower than the average Sr87/Sr86 ratios found in Precambrian sialic regions which range from 0.71 to 0.73. It seems clear therefore that the Sierra Nevada magmas were not derived solely either from the typical source regions of oceanic basalt or from the melting of ancient crustal sial. It is possible that these magmas represent a mixture of oceanic basalt and crustal sial, as would be the case of anatexis in a geosyncline containing much volcanic material of fairly recent origin and some terrigenous sialic detritus. They may instead be of mantle derivation with admixtures of crustal material assimilated during their rise.
The whole-rock Rb-Sr age results derivec from the study indicate that the Lamarck and Mount Givens Granodiorites and the alaskite of Evolution Basin and porphyritic biotite granite of Dinkey Lakes form a younger group of intrusive rocks of 90 ± 10 m.y. Although the sampling was not designed for isochron age studies, it appears that most of the remaining rock units are considerably older.
","language":"English","publisher":"Geological Society of America","doi":"10.1130/0016-7606(1965)76[165:IOISSR]2.0.CO;2","usgsCitation":"Hurley, P., Bateman, P.C., Fairbairn, H., and Pinson, W., 1965, Investigation of initial Sr87/Sr86 ratios in the Sierra Nevada Plutonic Province: GSA Bulletin, v. 76, no. 2, p. 165-174, https://doi.org/10.1130/0016-7606(1965)76[165:IOISSR]2.0.CO;2.","productDescription":"10 p.","startPage":"165","endPage":"174","costCenters":[],"links":[{"id":387213,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"76","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Hurley, P.M.","contributorId":258271,"corporation":false,"usgs":false,"family":"Hurley","given":"P.M.","email":"","affiliations":[],"preferred":false,"id":819351,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bateman, P. C.","contributorId":27851,"corporation":false,"usgs":true,"family":"Bateman","given":"P.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":819352,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Fairbairn, H.W.","contributorId":88609,"corporation":false,"usgs":true,"family":"Fairbairn","given":"H.W.","email":"","affiliations":[],"preferred":false,"id":819353,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Pinson, W.H.","contributorId":237001,"corporation":false,"usgs":false,"family":"Pinson","given":"W.H.","email":"","affiliations":[{"id":12444,"text":"Massachusetts Institute of Technology","active":true,"usgs":false}],"preferred":false,"id":819354,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":70175858,"text":"70175858 - 1965 - Chemical quality of ground water in the Minneapolis-St. Paul area, Minnesota","interactions":[],"lastModifiedDate":"2018-03-19T10:05:03","indexId":"70175858","displayToPublicDate":"1965-07-14T13:30:00","publicationYear":"1965","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":105,"text":"Bulletin","active":false,"publicationSubtype":{"id":2}},"title":"Chemical quality of ground water in the Minneapolis-St. Paul area, Minnesota","docAbstract":"No abstract available.
","language":"English","publisher":"Minnesota Department of Conservation, Division of Waters","publisherLocation":"St. Paul, MN","usgsCitation":"Mann, W., and McBride, M., 1965, Chemical quality of ground water in the Minneapolis-St. Paul area, Minnesota: Bulletin, 44 p.","productDescription":"44 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":392,"text":"Minnesota Water Science Center","active":true,"usgs":true}],"links":[{"id":327043,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Minnesota","otherGeospatial":"Twin Cities metropolitan 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IV","contributorId":89570,"corporation":false,"usgs":true,"family":"Mann","given":"W.B.","suffix":"IV","email":"","affiliations":[],"preferred":false,"id":646457,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"McBride, M.S.","contributorId":21928,"corporation":false,"usgs":true,"family":"McBride","given":"M.S.","email":"","affiliations":[],"preferred":false,"id":646458,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":1001418,"text":"1001418 - 1965 - An automatic camera device for measuring waterfowl use","interactions":[],"lastModifiedDate":"2025-02-07T16:35:25.540112","indexId":"1001418","displayToPublicDate":"1965-07-02T00:00:00","publicationYear":"1965","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2508,"text":"Journal of Wildlife Management","active":true,"publicationSubtype":{"id":10}},"title":"An automatic camera device for measuring waterfowl use","docAbstract":"A Yashica Sequelle camera was modified and equipped with a timing device so that it would take pictures automatically at 15-minute intervals. Several of these cameras were used to photograph randomly selected quadrats located in different marsh habitats. The number of birds photographed in the different areas was used as an index of waterfowl use.","language":"English","publisher":"Wiley","doi":"10.2307/3798066","usgsCitation":"Cowardin, L.M., and Ashe, J., 1965, An automatic camera device for measuring waterfowl use: Journal of Wildlife Management, v. 29, no. 3, p. 636-640, https://doi.org/10.2307/3798066.","productDescription":"5 p.","startPage":"636","endPage":"640","costCenters":[{"id":480,"text":"Northern Prairie Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":133814,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"29","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad9e4b07f02db684cee","contributors":{"authors":[{"text":"Cowardin, Lewis M.","contributorId":34574,"corporation":false,"usgs":true,"family":"Cowardin","given":"Lewis","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":311008,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ashe, J.E.","contributorId":6417,"corporation":false,"usgs":true,"family":"Ashe","given":"J.E.","email":"","affiliations":[],"preferred":false,"id":311007,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":5221298,"text":"5221298 - 1965 - Effects of field applications of heptachlor on bobwhite quail and other wild animals","interactions":[],"lastModifiedDate":"2025-02-07T16:40:08.616139","indexId":"5221298","displayToPublicDate":"1965-07-02T00:00:00","publicationYear":"1965","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2508,"text":"Journal of Wildlife Management","active":true,"publicationSubtype":{"id":10}},"title":"Effects of field applications of heptachlor on bobwhite quail and other wild animals","docAbstract":"A study of the effects of field applications of heptachlor on bobwhite quail (Colinus uirginianus) and other animals was conducted on three similar areas, two in Decatur County, Georgia, and one in Escambia County, Alabama, from February, 1958, to March, 1962. Heptachlor in granules was applied by aircraft on the Georgia areas for eradication of the imported fire ant (Solenopsis saevissima). Applications were directed by personnel of the U. S. Department of Agriculture, Plant Pest Control Division. The Alabama area remained untreated. Transects where whistling cocks were counted were superimposed on areas where coveys were counted. Size of areas varied from 14,000 to 20,000 acres. Each area had six transects, totaling 11,000 acres. Whistling cock bobwhites and coveys averaged 28 and 20 per 1,000 acres, respectively, the year before treatment on a Georgia area, and cocks and coveys averaged 25 per 1,000 acres for the duration of the study on the untreated Alabama area. Where portions of an area were treated at 2 pounds of heptachlor per acre, whistling cocks and coveys were reduced significantly, with a greater reduction where a greater amount of land was treated on the area or its transects. A decline of cocks and coveys also followed 1/2-pound applications (approaching statistical significance for coveys). Three years after treatment, cock and covey numbers were below those recorded before treatment. Whistling cocks and coveys also declined on adjoining land which remained untreated (significant for cocks, approaching significance for coveys). This decline was attributed to movements of bobwhites from untreated land to repopulate treated land. There is evidence that some loss occurred in bobwhites after they moved from untreated to treated land; the decrease in each instance was ascribed to the application of heptachlor. Songbirds were listed on the two Georgia areas. The first summer, eight more species and 458 more individuals of permanent resident birds were listed on the untreated area than on the treated area. After half of the originally untreated area was treated with heptachlor at 2 pounds per acre the following winter, the number of resident birds declined 37 percent. Some species of summer resident birds could not be found on treated land after heptachlor was applied. A small plot of 4 acres was intensively searched for dead and dying animals, and observations were made on living animals. Forty-seven days after treatment, no live animals were seen or heard on the plot, and a total of 38 dead animals had been found. Soils were sampled twice after treatment, and residues had declined in the second lot of samples. Twice animals also were obtained for analysis, and residues declined in the second group. Numbers of birds increased in the same period.
","language":"English","publisher":"Wiley","doi":"10.2307/3798056","usgsCitation":"Rosene, W., 1965, Effects of field applications of heptachlor on bobwhite quail and other wild animals: Journal of Wildlife Management, v. 29, no. 3, p. 554-580, https://doi.org/10.2307/3798056.","productDescription":"27 p.","startPage":"554","endPage":"580","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":194060,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Alabama, Georgia","county":"Decatur County, Escambia 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W.","contributorId":67609,"corporation":false,"usgs":true,"family":"Rosene","given":"W.","email":"","affiliations":[],"preferred":false,"id":333520,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70221206,"text":"70221206 - 1965 - Chemical characteristics of oceanic basalts and the upper mantle","interactions":[],"lastModifiedDate":"2021-06-04T21:52:17.917781","indexId":"70221206","displayToPublicDate":"1965-07-01T16:49:24","publicationYear":"1965","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":"Chemical characteristics of oceanic basalts and the upper mantle","docAbstract":"Tholeiitic basalts (oceanic tholeiites) that form most of the deeply submerged volcanic features in the oceans are characterized by extremely low amounts of Ba, K, P, Pb, Sr, Th, U, and Zr as well as Fe2O3/FeO < 0.2 and Na/K > 10 in unaltered samples. Oceanic tholeiites also have rare earth abundance-distribution patterns and ratios of K/Rb (1300) and Sr87/Sr86 (0.702) similar to or overlapping those of calcium-rich (basaltic) achondritic meteorites. The close compositional similarities between the oceanic tholeiites and calcium-rich achondrites indicates the relatively primitive nature of the oceanic tholeiites. In contrast, the alkali-rich basalts that cap submarine and island volcanoes are relatively enriched in Ba, K, La, Nb, P, Pb, Pb206, Rb, Fe2O3, Sr, Sr87, Ti, Th, U, and Zr; i.e. in the same elements and isotopes that are concentrated in the sialic continental crusts by factors of 5 to 1000 more than the amounts readily inferred in the upper mantle. These analytical data coupled with the field relationships indicate that the alkali-rich basalts are derivative rocks, fractionated from the oceanic tholeiites by processes of magmatic differentiation, and that the oceanic tholeiites are the principal or only primary magma generated in the upper mantle under the oceans. Studies of the abundances and compositions of continental basalts show that essentially identical tholeiitic lavas, contaminated with Si, K, and the chemically coherent trace elements and radiogenic isotopes from the sial, also have been the predominant or only magma generated in the mantle under the continents. The chemical properties of oceanic tholeiites suggest that the upper mantle probably contains less than (in parts per million): Ba, 10; K, 1000; Pb, 0.4; Rb, 10; Th, 0.2; and U, 0.1. The Sr87/Sr86 must be less than 0.7015; Th/U about 2; K/Rb about 1500-2000; and Fe2O3/FeO less than 0.1. The integration of field and petrochemical data with seismic, density, and shock-wave studies suggests that the oceanic tholeiites are either complete melts of the upper mantle or are generated from a mix of this tholeiite and a magnesium-rich peridotite or dunite in proportions up to perhaps 1:4. The Mohorovičić discontinuity under the oceans appears to mark the transition downward from a largely tholeiitic oceanic crust to either tholeiite reconstituted to blueschist or greenschist or to the ultramafic residue left after expulsion of oceanic tholeiite.
","language":"English","publisher":"Geological Society of America","doi":"10.1130/0016-7606(1965)76[719:CCOOBA]2.0.CO;2","usgsCitation":"Engel, A., Engel, C.G., and Havens, R., 1965, Chemical characteristics of oceanic basalts and the upper mantle: Geological Society of America Bulletin, v. 76, no. 7, p. 719-734, https://doi.org/10.1130/0016-7606(1965)76[719:CCOOBA]2.0.CO;2.","productDescription":"16 p.","startPage":"719","endPage":"734","costCenters":[],"links":[{"id":386251,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"76","issue":"7","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Engel, A.E.J.","contributorId":241621,"corporation":false,"usgs":false,"family":"Engel","given":"A.E.J.","affiliations":[],"preferred":false,"id":817046,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Engel, Celeste G.","contributorId":23386,"corporation":false,"usgs":true,"family":"Engel","given":"Celeste","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":817047,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Havens, R.G.","contributorId":65889,"corporation":false,"usgs":true,"family":"Havens","given":"R.G.","email":"","affiliations":[],"preferred":false,"id":817048,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70221204,"text":"70221204 - 1965 - The drill‐stem test: The petroleum industry's deep‐well pumping test","interactions":[],"lastModifiedDate":"2021-06-04T21:44:46.914029","indexId":"70221204","displayToPublicDate":"1965-07-01T16:42:04","publicationYear":"1965","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3825,"text":"Groundwater","active":true,"publicationSubtype":{"id":10}},"title":"The drill‐stem test: The petroleum industry's deep‐well pumping test","docAbstract":"Drill‐stem tests provide the petroleum industry information on three critical properties of subsurface formations —pressure head, permeability, and water chemistry –that the ground‐water hydrologist also seeks in making pumping tests of water wells. As it is increasingly necessary to study the hydraulic and geochemical properties of deep‐lying rocks in order to understand the behavior of ground water, data on drill‐stem tests made by the petroleum industry become an important source of information which otherwise is unobtainable because of the high cost. Data from these tests made by methods currently in use are highly useful in water studies. An obvious conclusion is that both petroleum engineering and ground‐water hydrology stand to profit substantially from an increase in the interchange of ideas and techniques.
","language":"English","publisher":"Wiley Blackwell","doi":"10.1111/j.1745-6584.1965.tb01218.x","usgsCitation":"Bredehoeft, J., 1965, The drill‐stem test: The petroleum industry's deep‐well pumping test: Groundwater, v. 3, no. 3, p. 31-36, https://doi.org/10.1111/j.1745-6584.1965.tb01218.x.","productDescription":"6 p.","startPage":"31","endPage":"36","costCenters":[],"links":[{"id":386249,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"3","issue":"3","noUsgsAuthors":false,"publicationDate":"2006-07-06","publicationStatus":"PW","contributors":{"authors":[{"text":"Bredehoeft, J.D.","contributorId":12836,"corporation":false,"usgs":true,"family":"Bredehoeft","given":"J.D.","affiliations":[],"preferred":false,"id":817044,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70221197,"text":"70221197 - 1965 - Natural controls involved in shallow aquifer contamination","interactions":[],"lastModifiedDate":"2021-06-04T21:03:19.909849","indexId":"70221197","displayToPublicDate":"1965-07-01T16:00:52","publicationYear":"1965","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3825,"text":"Groundwater","active":true,"publicationSubtype":{"id":10}},"title":"Natural controls involved in shallow aquifer contamination","docAbstract":"Shallow aquifers, commonly the most important sources of ground water, are also those most susceptible to contamination. The mode of entry of contaminants to shallow aquifers is (1) directly, via wells or secondary openings in consolidated rocks, (2) percolation through the zone of aeration, (3) induced infiltration through the zone of saturation, and (4) interaquifer leakage or flow through open holes. Natural removal or degradation of contaminants is by filtration, dispersion, sorption, ion exchange, oxidation, and various biochemical processes. These phenomena are controlled by the physical environment, structure; mineralogy, and hydraulic characteristics of the earth materials contacted by the liquid wastes. When liquid wastes enter an aquifer directly, there is little or no natural treatment by filtration, sorption, or oxidation. Purification is only by those processes that operate within the aquifer under anaerobic conditions. Contaminants from natural sources that enter aquifers under saturated‐flow conditions are degraded primarily by dilution. The natural processes effective in reducing contamination from surface‐water sources depend on the hydraulic regimen involved, which vary with individual cases. Liquid wastes percolating through the zone of aeration are those most likely to be purified by natural environment processes. Natural processes, however, do not effectively remove or degrade all contaminants, especially some of the many highly stable compounds that have gained widespread use in recent years, such as synthetic detergents. Comprehensive interdisciplinary research into the ability of various earth materials to remove many types of contaminants under varying hydrologic conditions is needed.
","language":"English","publisher":"Wiley Blackwell","doi":"10.1111/j.1745-6584.1965.tb01219.x","usgsCitation":"Deutsch, M., 1965, Natural controls involved in shallow aquifer contamination: Groundwater, v. 3, no. 3, p. 37-40, https://doi.org/10.1111/j.1745-6584.1965.tb01219.x.","productDescription":"4 p.","startPage":"37","endPage":"40","costCenters":[],"links":[{"id":386242,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"3","issue":"3","noUsgsAuthors":false,"publicationDate":"2006-07-06","publicationStatus":"PW","contributors":{"authors":[{"text":"Deutsch, M.","contributorId":19707,"corporation":false,"usgs":true,"family":"Deutsch","given":"M.","email":"","affiliations":[],"preferred":false,"id":817035,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ]}