No abstract available.
","language":"English","publisher":"American Association for the Advancement of Science","doi":"10.1126/science.149.3684.658.b","issn":"00368075","usgsCitation":"Warren, C., 1965, Wright Valley: Conjectural volcanoes: Science, v. 149, no. 3684, p. 658-658, https://doi.org/10.1126/science.149.3684.658.b.","productDescription":"1 p.","startPage":"658","endPage":"658","costCenters":[],"links":[{"id":219621,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"otherGeospatial":"Antarctica","volume":"149","issue":"3684","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bd1dee4b08c986b32f5c0","contributors":{"authors":[{"text":"Warren, C.R.","contributorId":80663,"corporation":false,"usgs":true,"family":"Warren","given":"C.R.","email":"","affiliations":[],"preferred":false,"id":359115,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70222559,"text":"70222559 - 1965 - The U. S. Geological Survey's Gravity program in California, Hawaii, Nevada, and Oregon","interactions":[],"lastModifiedDate":"2021-08-04T13:04:16.772688","indexId":"70222559","displayToPublicDate":"1965-08-04T08:01:21","publicationYear":"1965","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1578,"text":"Eos, Transactions, American Geophysical Union","onlineIssn":"2324-9250","printIssn":"0096-394","active":true,"publicationSubtype":{"id":10}},"title":"The U. S. Geological Survey's Gravity program in California, Hawaii, Nevada, and Oregon","docAbstract":"During the past 10 years, personnel of the U. S. Geological Survey have made about 14,000 observations of the Earth's gravity field in California, about 13,000 in Nevada, 3,400 in Oregon, and about 1,000 in the Hawaiian Islands. The total number of stations established in the four states is slightly in excess of 30,000.
","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR046i001p00218","usgsCitation":"Oliver, H., 1965, The U. S. 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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":70222557,"text":"70222557 - 1965 - On lantern slides","interactions":[],"lastModifiedDate":"2021-08-04T12:39:06.405434","indexId":"70222557","displayToPublicDate":"1965-08-04T07:36:54","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":"On lantern slides","docAbstract":"Before photography, look at the original from as many feet away as it is inches wide, and you will see it as it will look to the audience as a slide on the screen.
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":70222061,"text":"70222061 - 1965 - Infrared studies of saline sulfate minerals: Discussion","interactions":[],"lastModifiedDate":"2021-07-16T13:08:50.616531","indexId":"70222061","displayToPublicDate":"1965-07-16T08:05:00","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":"Infrared studies of saline sulfate minerals: Discussion","docAbstract":"No abstract available.
","language":"English","publisher":"Geological Society of America","doi":"10.1130/0016-7606(1965)76[271:ISOSSM]2.0.CO;2","usgsCitation":"Erd, R.C., Lyon, R., and Madsen, B.M., 1965, Infrared studies of saline sulfate minerals: Discussion: GSA Bulletin, v. 76, no. 2, p. 271-282, https://doi.org/10.1130/0016-7606(1965)76[271:ISOSSM]2.0.CO;2.","productDescription":"12 p.","startPage":"271","endPage":"282","costCenters":[],"links":[{"id":387214,"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":"Erd, Richard C.","contributorId":89899,"corporation":false,"usgs":true,"family":"Erd","given":"Richard","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":819355,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lyon, R.J.P.","contributorId":29064,"corporation":false,"usgs":true,"family":"Lyon","given":"R.J.P.","email":"","affiliations":[],"preferred":false,"id":819356,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Madsen, Beth M.","contributorId":82761,"corporation":false,"usgs":true,"family":"Madsen","given":"Beth","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":819357,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"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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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":5220168,"text":"5220168 - 1965 - Development and maturation of primary feathers of redhead ducklings","interactions":[],"lastModifiedDate":"2025-02-07T16:43:55.849511","indexId":"5220168","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":"Development and maturation of primary feathers of redhead ducklings","docAbstract":"A comparison of the maturation rates of the primaries of redheads (Aythya americana) hatched very early with those hatched very late was made in the 1961 season. Primaries of the early-hatched birds emerged when the birds were 36-38 days old, those of the late-hatched birds when they were 7-10 days younger. This difference was also found in the age at first flight and the age at eventual maturation of all primaries. Primaries of late-hatched birds were significantly shorter in length when mature than were the primaries of early-hatched birds.
","language":"English","publisher":"Wiley","doi":"10.2307/3798053","usgsCitation":"Smart, M., 1965, Development and maturation of primary feathers of redhead ducklings: Journal of Wildlife Management, v. 29, no. 3, p. 533-536, https://doi.org/10.2307/3798053.","productDescription":"4 p.","startPage":"533","endPage":"536","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":193646,"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":"4f4e4aa7e4b07f02db667258","contributors":{"authors":[{"text":"Smart, M.G.","contributorId":35829,"corporation":false,"usgs":true,"family":"Smart","given":"M.G.","email":"","affiliations":[],"preferred":false,"id":331444,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"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":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}]}} ,{"id":1014054,"text":"1014054 - 1965 - Simple enrichment of commercial media for growth of Hemophilus piscium","interactions":[],"lastModifiedDate":"2025-08-01T16:37:19.781793","indexId":"1014054","displayToPublicDate":"1965-07-01T00:00:00","publicationYear":"1965","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":"Simple enrichment of commercial media for growth of Hemophilus piscium","docAbstract":"No abstract available.
","language":"English","publisher":"American Fisheries Society","doi":"10.1577/1548-8640(1965)27[163:SEOCMF]2.0.CO;2","usgsCitation":"Bullock, G.L., 1965, Simple enrichment of commercial media for growth of Hemophilus piscium: Progressive Fish-Culturist, v. 27, no. 3, p. 163-164, https://doi.org/10.1577/1548-8640(1965)27[163:SEOCMF]2.0.CO;2.","productDescription":"2 p.","startPage":"163","endPage":"164","costCenters":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"links":[{"id":131459,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"27","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f9e4b07f02db5f38ec","contributors":{"authors":[{"text":"Bullock, Graham L.","contributorId":9323,"corporation":false,"usgs":true,"family":"Bullock","given":"Graham","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":319691,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":1014141,"text":"1014141 - 1965 - Survey, reporting, and certification of diseases in fish production","interactions":[],"lastModifiedDate":"2025-08-01T16:43:20.575576","indexId":"1014141","displayToPublicDate":"1965-07-01T00:00:00","publicationYear":"1965","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":"Survey, reporting, and certification of diseases in fish production","docAbstract":"No abstract available.
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\"}}]}","volume":"27","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae0e4b07f02db68856d","contributors":{"authors":[{"text":"Snieszko, S. F.","contributorId":13169,"corporation":false,"usgs":true,"family":"Snieszko","given":"S.","middleInitial":"F.","affiliations":[],"preferred":false,"id":319854,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":1014319,"text":"1014319 - 1965 - Chlorella parasitic in bluegills","interactions":[],"lastModifiedDate":"2025-08-01T16:32:35.359245","indexId":"1014319","displayToPublicDate":"1965-07-01T00:00:00","publicationYear":"1965","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":"Chlorella parasitic in bluegills","docAbstract":"No abstract available.
","language":"English","publisher":"American Fisheries Society","doi":"10.1577/1548-8640(1965)27[175:CPIB]2.0.CO;2","usgsCitation":"Hoffman, G.L., Prescott, G., and Thompson, C.R., 1965, Chlorella parasitic in bluegills: Progressive Fish-Culturist, v. 27, no. 3, p. 175-175, https://doi.org/10.1577/1548-8640(1965)27[175:CPIB]2.0.CO;2.","productDescription":"1 p.","startPage":"175","endPage":"175","costCenters":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"links":[{"id":130960,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"27","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac8e4b07f02db67b6e3","contributors":{"authors":[{"text":"Hoffman, G. L.","contributorId":70713,"corporation":false,"usgs":true,"family":"Hoffman","given":"G.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":320185,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Prescott, G.W.","contributorId":24728,"corporation":false,"usgs":true,"family":"Prescott","given":"G.W.","email":"","affiliations":[],"preferred":false,"id":320184,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Thompson, C. R.","contributorId":100801,"corporation":false,"usgs":true,"family":"Thompson","given":"C.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":320186,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70010602,"text":"70010602 - 1965 - Tectonic deformation associated with the 1964 Alaska earthquake","interactions":[],"lastModifiedDate":"2026-02-11T15:00:12.272329","indexId":"70010602","displayToPublicDate":"1965-06-25T00:00:00","publicationYear":"1965","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3338,"text":"Science","active":true,"publicationSubtype":{"id":10}},"title":"Tectonic deformation associated with the 1964 Alaska earthquake","docAbstract":"Alaska's Good Friday earthquake of 27 March 1964 was accompanied by vertical tectonic deformation over an area of 170,000 to 200,000 square kilometers in south-central Alaska. The deformation included two major northeast-trending zones of uplift and subsidence situated between the Aleutian Trench and the Aleutian Volcanic Arc; together they are 700 to 800 kilometers long and from 150 to 250 kilometers wide. The seaward zone is one in which uplift of as much as 10 meters on land and 15 meters on the sea floor has occurred as a result of both crustal warping and local faulting. Submarine uplift within this zone generated a train of seismic sea waves with half-wave amplitudes of more than 7 meters along the coast near the source. The adjacent zone to the northwest is one of subsidence that averages about 1 meter and attains a measured maximum of 2.3 meters. A second zone of slight uplift may exist along all or part of the Aleutian and Alaska ranges northwest of the zone of subsidence.
","language":"English","publisher":"American Association for the Advancement of Science","doi":"10.1126/science.148.3678.1675","issn":"00368075","usgsCitation":"Plafker, G., 1965, Tectonic deformation associated with the 1964 Alaska earthquake: Science, v. 148, no. 3678, p. 1675-1687, https://doi.org/10.1126/science.148.3678.1675.","productDescription":"13 p.","startPage":"1675","endPage":"1687","costCenters":[],"links":[{"id":219101,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Alaska","otherGeospatial":"Aleutian Trench","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -179.9,\n 52.89848022223302\n ],\n [\n -179.9,\n 50.34742724365566\n ],\n [\n -165.90072947118094,\n 52.38515601893195\n ],\n [\n -157.1802921694297,\n 54.89759776829018\n ],\n [\n -155.36618380411227,\n 56.73058764922936\n ],\n [\n -158.829392131228,\n 58.11065126044281\n ],\n [\n -172.99044772182424,\n 53.805294237333726\n ],\n [\n -179.9,\n 52.89848022223302\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n },\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n 179.9,\n 52.84464206876427\n ],\n [\n 172,\n 54.15161662224946\n ],\n [\n 172,\n 51.89469832853055\n ],\n [\n 179.9,\n 50.32814578749236\n ],\n [\n 179.9,\n 52.84464206876427\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","volume":"148","issue":"3678","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505ba44ce4b08c986b320232","contributors":{"authors":[{"text":"Plafker, George 0000-0003-3972-0390","orcid":"https://orcid.org/0000-0003-3972-0390","contributorId":36603,"corporation":false,"usgs":true,"family":"Plafker","given":"George","affiliations":[],"preferred":false,"id":359251,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70010832,"text":"70010832 - 1965 - Holocene submergence of the Eastern Shore of Virginia","interactions":[],"lastModifiedDate":"2026-02-10T18:44:41.648721","indexId":"70010832","displayToPublicDate":"1965-06-11T00:00:00","publicationYear":"1965","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3338,"text":"Science","active":true,"publicationSubtype":{"id":10}},"title":"Holocene submergence of the Eastern Shore of Virginia","docAbstract":"Radiocarbon ages of basal peats 4500 years old or younger and the thickness of salt-marsh peat in the lagoon east of Wachapreague, Virginia, are nearly the same as those of equivalent samples from New Jersey and Cape Cod. This suggests that these coasts have had similar submergence histories. Data obtained from the coasts of Connecticut and northeastern Massachusetts indicate that the Atlantic coast of the United States has been differentially warped during the later Holocene.","language":"English","publisher":"American Association for the Advancement of Science","doi":"10.1126/science.148.3676.1464","issn":"00368075","usgsCitation":"Newman, W., and Rusnak, G., 1965, Holocene submergence of the Eastern Shore of Virginia: Science, v. 148, no. 3676, p. 1464-1466, https://doi.org/10.1126/science.148.3676.1464.","productDescription":"3 p.","startPage":"1464","endPage":"1466","costCenters":[],"links":[{"id":218899,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Connecticut, Massachusetts, New Jersey, Virginia","otherGeospatial":"Atlantic coast","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -71.72870898922105,\n 42.81177931670098\n ],\n [\n -76.07587223384438,\n 42.81177931670098\n ],\n [\n -76.07587223384438,\n 36.4511679954293\n ],\n [\n -71.72870898922105,\n 36.4511679954293\n ],\n [\n -71.72870898922105,\n 42.81177931670098\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","volume":"148","issue":"3676","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a31f6e4b0c8380cd5e3cc","contributors":{"authors":[{"text":"Newman, W.S.","contributorId":12187,"corporation":false,"usgs":true,"family":"Newman","given":"W.S.","email":"","affiliations":[],"preferred":false,"id":359748,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Rusnak, G.A.","contributorId":80407,"corporation":false,"usgs":true,"family":"Rusnak","given":"G.A.","email":"","affiliations":[],"preferred":false,"id":359749,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":5210065,"text":"5210065 - 1965 - The occurrence of protozoan blood parasites in Anatidae","interactions":[],"lastModifiedDate":"2020-03-13T12:46:33","indexId":"5210065","displayToPublicDate":"1965-06-09T09:23:16","publicationYear":"1965","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"title":"The occurrence of protozoan blood parasites in Anatidae","docAbstract":"No abstract available.
","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"International Union of Game Biologists, Transactions of the VIth Congress","largerWorkSubtype":{"id":4,"text":"Other Government Series"},"language":"English","publisher":"Nature Conservancy","publisherLocation":"London","collaboration":"OCLC: 2347707","usgsCitation":"Herman, C.M., 1965, The occurrence of protozoan blood parasites in Anatidae, chap. of International Union of Game Biologists, Transactions of the VIth Congress, p. 341-349.","productDescription":"9 p.","startPage":"341","endPage":"349","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":201284,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a80e4b07f02db649407","contributors":{"editors":[{"text":"Blank, T.H.","contributorId":114091,"corporation":false,"usgs":true,"family":"Blank","given":"T.H.","email":"","affiliations":[],"preferred":false,"id":505959,"contributorType":{"id":2,"text":"Editors"},"rank":1}],"authors":[{"text":"Herman, C. M.","contributorId":101335,"corporation":false,"usgs":true,"family":"Herman","given":"C.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":327702,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ]}