{"pageNumber":"5639","pageRowStart":"140950","pageSize":"25","recordCount":165629,"records":[{"id":5210161,"text":"5210161 - 1972 - Biological data on PCBs in animals other than man","interactions":[],"lastModifiedDate":"2012-02-02T00:15:16","indexId":"5210161","displayToPublicDate":"2009-06-09T09:23:16","publicationYear":"1972","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"title":"Biological data on PCBs in animals other than man","docAbstract":"SUMMARY: Polychlorinated biphenyls have become ubiquitous in the world ecosystem in quantities similar to those of DDE. Experimental studies have shown that PCBs have a toxicity to mallards, pheasants, bobwhite quail, coturnix quail, red-winged blackbirds, starlings, cowbirds, and grackles that is of the same order as the toxicity of DDE to these species. Overt signs of poisoning also are similar to those caused by compounds of the DDT group. Toxic effects of DDE and Aroclor 1254 to coturnix chicks were additive, but not synergistic. PCBs containing higher percentages of chlorine are more toxic to birds than those containing lower percentages. PCBs of foreign manufacture contained contaminants to an extent that greatly increased their toxicity. Residues of PCBs in the brains of birds killed by these compounds measure in the hundreds of parts per million. PCBs may have contributed to mortality of some birds in the field. Toxicity to insects of PCBs of different degrees of chlorination is the reverse of the pattern in birds: the lower chlorinations are more toxic to insects. PCBs enhanced the toxicity of dieldrin and DDT to insects. Shrimp are very sensitive to PCBs and most will die as a result of 20-day exposure to a concentration of 5 ppb. PCBs also inhibit shell growth of oysters. Crabs are less sensitive; all accumulate residues to many times the concentrations in the water, and a test with crabs showed that they lost the residues very slowly. Growth of certain species of marine diatoms was experimentally inhibited by PCBs, but algae were not affected. The small marine crustacean, Gammarus, is sensitive to PCBs in concentrations of thousandths to tenths of a part per billion. Exposure to 5 ppb of Aroclor 1254 caused mortality of two species of fish in 14-45 days. Onset of death was delayed and was accompanied by fungus-like lesions. Rainbow trout were quickly killed by terphenyls at 10 ppb under normal oxygen conditions and at 2 ppb with reduced oxygen. Metabolic changes of PCBs have been suggested by environmental observations of different isomeric patterns in animals of different trophic levels. Quantitative differences also are pronounced, with magnifications of hundreds to thousands of times. Laboratory studies have shown no metabolic changes of PCBs by crabs and shrimps, minimal changes by fish, and pronounced changes by birds. PCBs induce microsomal enzyme activity in birds. Exposure to PCBs increased the susceptibility of mallard ducklings to duck hepatitis virus. Offspring of pheasants whose parents received high dosages of PCBs made poor choices in visual cliff tests. Egg production and hatching after pipping also were affected. Migratory restlessness was increased in English robins exposed to PCBs. Long-term studies of the reproductive effects of Aroclor 1254 on mallards and bobwhite quail and of Aroclor 1254 plus DDE on quail showed no significant differences from controls. In studies of chickens, however, egg production and hatchability were impaired by high doses of Aroclor 1254 and by low doses of Aroclor 1242. Statistical evaluations of the role that different chemicals may play in thinning eggshells of brown pelicans showed that DDE residues correlate better with shell thinning than do residues of dieldrin or PCBs, confirming observations with cormorants and white pelicans.","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Polychlorinated Biphenyls and the Environment","largerWorkSubtype":{"id":4,"text":"Other Government Series"},"language":"English","publisher":"Interdepartmental Task Force on PCBs","publisherLocation":"Washington, D.C.","collaboration":"OCLC: 6261205 ; OCLC: 1165099 ; distributed by NTIS, stock No. COM-72-10419","usgsCitation":"Stickel, L., 1972, Biological data on PCBs in animals other than man, chap. of Polychlorinated Biphenyls and the Environment, p. 158-172.","productDescription":"vii, 181","startPage":"158","endPage":"172","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":200427,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a54e4b07f02db62c473","contributors":{"authors":[{"text":"Stickel, L.F.","contributorId":41095,"corporation":false,"usgs":true,"family":"Stickel","given":"L.F.","email":"","affiliations":[],"preferred":false,"id":327875,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":5210164,"text":"5210164 - 1972 - Mercury in wild animals, Lake St. Clair, 1970","interactions":[],"lastModifiedDate":"2020-05-14T20:14:15.98799","indexId":"5210164","displayToPublicDate":"2009-06-09T09:23:16","publicationYear":"1972","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"title":"Mercury in wild animals, Lake St. Clair, 1970","docAbstract":"

No abstract available.

","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Environmental Mercury Contamination","largerWorkSubtype":{"id":4,"text":"Other Government Series"},"language":"English","publisher":"Ann Arbor Science Publishers","publisherLocation":"Ann Arbor, Michigan","usgsCitation":"Dustman, E.H., Stickel, L., and Elder, J., 1972, Mercury in wild animals, Lake St. Clair, 1970, chap. of Environmental Mercury Contamination, p. 46-52.","productDescription":"7 p.","startPage":"46","endPage":"52","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":200429,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"Canada, United States","state":"Michigan, Ontario","otherGeospatial":"Lake St. Clair","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -82.3974609375,\n 42.367676308265196\n ],\n [\n -82.408447265625,\n 42.50754004948742\n ],\n [\n -82.61993408203125,\n 42.7016136416648\n ],\n [\n -82.76412963867188,\n 42.69959515809203\n ],\n [\n -82.88497924804688,\n 42.6026307853624\n ],\n [\n -82.93853759765625,\n 42.429538632268276\n ],\n [\n -83.02505493164062,\n 42.34738030389109\n ],\n [\n -82.99758911132812,\n 42.30067461858169\n ],\n [\n -82.85614013671875,\n 42.2905166207974\n ],\n [\n -82.63778686523438,\n 42.2752765520868\n ],\n [\n -82.42767333984375,\n 42.29661161608281\n ],\n [\n -82.3974609375,\n 42.367676308265196\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4ae4b07f02db624d5a","contributors":{"editors":[{"text":"Hartung, R.","contributorId":112905,"corporation":false,"usgs":true,"family":"Hartung","given":"R.","email":"","affiliations":[],"preferred":false,"id":506077,"contributorType":{"id":2,"text":"Editors"},"rank":1},{"text":"Dinman, B.D.","contributorId":111759,"corporation":false,"usgs":true,"family":"Dinman","given":"B.D.","email":"","affiliations":[],"preferred":false,"id":506076,"contributorType":{"id":2,"text":"Editors"},"rank":2}],"authors":[{"text":"Dustman, E. H.","contributorId":12579,"corporation":false,"usgs":true,"family":"Dustman","given":"E.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":327880,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Stickel, L.F.","contributorId":41095,"corporation":false,"usgs":true,"family":"Stickel","given":"L.F.","email":"","affiliations":[],"preferred":false,"id":327882,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Elder, J. B.","contributorId":39488,"corporation":false,"usgs":true,"family":"Elder","given":"J. B.","affiliations":[],"preferred":false,"id":327881,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":5210160,"text":"5210160 - 1972 - Los plaguicidas y la contaminacion del medio ambiente Venezolano","interactions":[],"lastModifiedDate":"2014-05-12T13:58:40","indexId":"5210160","displayToPublicDate":"2009-06-09T09:23:00","publicationYear":"1972","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"title":"Los plaguicidas y la contaminacion del medio ambiente Venezolano","docAbstract":"RESUMEN DE RECOMENDACIONES Recomendaciones para el Programa de Investigacion: 1. Establecer un sistema de muestreo biologico para detectar los niveles tendencias de los productos quimicos toxicos en un peque?o numero de si tios representativos. 2. Mantener continua vigilancia de la contaminacion ambiental, mediante la seleccion acertadamente dirigida de las zonas afectadas y de las fuentes de contaminacion. 3. Realizar estudios acerca de las poblaciones de animales silvestres, y del exito de los procesos reproductivos de las especies o grupos clayes de animales que se consideran mas gravemente afectados. 4. Preparar recomendaciones para una accion gubernamental de proteccion al hombre, a la fauna silvestre y al medio ambiente. Recomendaciones para la Accion Administrativa: 1. Establecer limites a la tolerancia de los residuos de plaguicidas en los alimentos. Constituye una medida clave para disminuir la contaminacion ambiental. 2. Establecer normas de calidad del agua para las corrientes, represas, la gos y otros cuerpos. Es la segunda medida clave para reducir la contaminacion del ambiente 3. Exigir un tratamiento adecuado de los efluentes industriales, especialmente antes de que se construyan las nuevas plantas. 4. Exigir a los agricultores que en el uso de plaguicidas sigan los consejos tecnicos autorizados y negar a los vendedores el derecho a recomendar productos por su cuenta. 5. Tomar medidas para recoger y eliminar los recipientes y sobrantes de los plaguicidas.","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Contribucion al Estudio Especial: La Agricultura y la Contaminacion del Medio Abiente de Venezuela.","largerWorkSubtype":{"id":4,"text":"Other Government Series"},"language":"Spanish","publisher":"Consejo de Bienestar Rural","publisherLocation":"Caracas, Venezuela","collaboration":"Abril de1972","usgsCitation":"Stickel, L., and Stickel, W.H., 1972, Los plaguicidas y la contaminacion del medio ambiente Venezolano, chap. of Contribucion al Estudio Especial: La Agricultura y la Contaminacion del Medio Abiente de Venezuela., 74.","productDescription":"74","numberOfPages":"74","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":201289,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a6fe4b07f02db640c99","contributors":{"authors":[{"text":"Stickel, L.F.","contributorId":41095,"corporation":false,"usgs":true,"family":"Stickel","given":"L.F.","email":"","affiliations":[],"preferred":false,"id":327874,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Stickel, W. H.","contributorId":23239,"corporation":false,"usgs":true,"family":"Stickel","given":"W.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":327873,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70047554,"text":"70047554 - 1972 - Hydraulic testing of hole UA-1-HTH-1, Amchitka Island, Alaska","interactions":[],"lastModifiedDate":"2013-09-19T13:11:24","indexId":"70047554","displayToPublicDate":"2009-01-01T09:10:00","publicationYear":"1972","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"title":"Hydraulic testing of hole UA-1-HTH-1, Amchitka Island, Alaska","docAbstract":"Total depth of the hole was 1,054 meters (3,458 feet) but, because of borehole erosion and bridging, only about 198 meters (650 feet) of the hole was·hydraulically tested with straddle packers. Some information was obtained on the lower part of the hole by use of the pressure recorders which are used with the straddle packers. The heads below land surface in that part of the hole tested with. straddle packers. ranged from·3.9 meters {12.7 feet) in the ..\ninterval 80.5 to 125. 0. meters (264- to 410 feet), the uppermost zone tested with straddle packers, to 5.1 meters (18.6 feet) in the interval 227.4 to 278.6 meters (.746 to 914 feet), the lowermost part of the hole tested with straddle packers. The composite static water level obtained following a pumping test.was 5.5 meters (18,0 feet). The composite head below 278.6 meters (914 feet), determined from a pressure recorder, was about 12.2 meters (40 feet). The head distribution. indicates a decreasing· head with depth. Water samples were collected from two intervals for chemical, radiochemical, and C-14 analysis. The unadjusted age of water in the interval 183.5 to 234.7 meters (602 to 770. feet) was determined to be 8,410 years, and for the interval 227.4 to 278.6 meters (746 to 914 feet) was 17,880 years. After adjustment the.ages of the waters may be less; however, they would still be. in the thousands of years and the relative difference probably would still be real.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Denver, CO","doi":"10.3133/70047554","usgsCitation":"Ballance, W.C., and Dinwiddie, G., 1972, Hydraulic testing of hole UA-1-HTH-1, Amchitka Island, Alaska, 27 p., https://doi.org/10.3133/70047554.","productDescription":"27 p.","numberOfPages":"32","costCenters":[],"links":[{"id":277872,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/unnumbered/70047554/report.pdf"},{"id":276298,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/unnumbered/70047554/report-thumb.jpg"}],"country":"United States","state":"Alaska","otherGeospatial":"Amchitka","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ 178.6158,51.3092 ], [ 178.6158,51.6665 ], [ 179.4688,51.6665 ], [ 179.4688,51.3092 ], [ 178.6158,51.3092 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"520a03efe4b0026c2bc11b96","contributors":{"authors":[{"text":"Ballance, Wilbur C.","contributorId":50436,"corporation":false,"usgs":true,"family":"Ballance","given":"Wilbur","email":"","middleInitial":"C.","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":482395,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Dinwiddie, G.A.","contributorId":49798,"corporation":false,"usgs":true,"family":"Dinwiddie","given":"G.A.","email":"","affiliations":[],"preferred":false,"id":482394,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70039440,"text":"70039440 - 1972 - Channel erosion surveys along proposed TAPS route, Alaska, July 1971","interactions":[],"lastModifiedDate":"2012-08-11T01:01:51","indexId":"70039440","displayToPublicDate":"2008-11-18T14:45:00","publicationYear":"1972","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"title":"Channel erosion surveys along proposed TAPS route, Alaska, July 1971","docAbstract":"The U.S. Geological Survey has the threefold responsibility along the proposed route of the Trans-Alaska Pipeline System (TAPS): to investigate possible hydroloqic hazards to the pipeline, to investigate possible impacts of the pipeline on water resources, and to develop a better understanding of Arctic hydrology. Because the proposed pipeline route lies within many stream channels, one of the obvious hydrologic hazards is channel erosion. It was considered a major hazard in a report by Hadley (1969) after a short reconnaissance of the proposed pipeline route and also in a national assessment of water resources by the Water Resources Council (1968). The U.S. Department of Interior has also recognized the channel erosion problems in considering the environmental impacts of TAPS and has stipulated conditions for their control (U.S. Dept. of Interior, 1972a, b). The Alyeska Pipeline Service Company (APSC), who would build and operate TAPS, has described methods for complying with the Department of Interior stipulations for channel and erosion control (APSC, 1971).","language":"English","publisher":"U.S Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/70039440","usgsCitation":"Childers, J.M., 1972, Channel erosion surveys along proposed TAPS route, Alaska, July 1971, 79 p., https://doi.org/10.3133/70039440.","productDescription":"79 p.","numberOfPages":"87","costCenters":[{"id":629,"text":"Water Resources Division","active":false,"usgs":true}],"links":[{"id":261578,"rank":800,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/unnumbered/70039440/report.pdf"},{"id":261579,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/unnumbered/70039440/report-thumb.jpg"}],"country":"United States","state":"Alaska","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ 173,54.666666666666664 ], [ 173,71.83333333333333 ], [ -130,71.83333333333333 ], [ -130,54.666666666666664 ], [ 173,54.666666666666664 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059f452e4b0c8380cd4bc79","contributors":{"authors":[{"text":"Childers, Joseph M.","contributorId":14379,"corporation":false,"usgs":true,"family":"Childers","given":"Joseph","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":466241,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70039525,"text":"70039525 - 1972 - A land use classification scheme for use with remote sensor data","interactions":[],"lastModifiedDate":"2012-08-11T01:01:51","indexId":"70039525","displayToPublicDate":"2008-01-16T14:25:00","publicationYear":"1972","noYear":false,"publicationType":{"id":4,"text":"Book"},"publicationSubtype":{"id":12,"text":"Conference publication"},"title":"A land use classification scheme for use with remote sensor data","docAbstract":"The needs of Federal agencies for a broad overview of national land use patterns, trends, and environmental impacts, with data inputs from both conventional sources and some of the more exotic sensors in high altitude aircraft and satellite platforms led to the formation in early 1971 of an Inter-Agency Steering Committee on Land Use Information and Classification. The work of this Committee, composed of representatives from the Geological Survey of the U.S. Department of the Interior, the Earth Observations Program of the National Aeronautics and Space Administration, the Soil Conservation Service of the U.S. Department of Agriculture, as well as the Association of American Geographers and the International Geographical Union, has been supported by NASA and the EROS Program of the Interior Department and coordinated by the USGS Geographic Applications Program. The Chairman of the Inter-Agency Committee was Dr. Arch C. Gerlach, Chief Geographer of the Geological Survey until his death in May 1972. Shortly before Dr. Gerlach's death, Dr. James R. Anderson was appointed Acting Chairman of the Committee.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Washington, D.C.","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1972, A land use classification scheme for use with remote sensor data, v, 205 p.","productDescription":"v, 205 p.","numberOfPages":"215","costCenters":[],"links":[{"id":261650,"rank":800,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/confpub/70039525/report.pdf"},{"id":261651,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/confpub/70039525/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059e42fe4b0c8380cd46498","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":535338,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70039504,"text":"70039504 - 1972 - Generalized gradient and contour program","interactions":[],"lastModifiedDate":"2012-08-11T01:01:51","indexId":"70039504","displayToPublicDate":"2008-01-09T11:52:00","publicationYear":"1972","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"seriesTitle":{"id":354,"text":"Computer contribution","active":false,"publicationSubtype":{"id":6}},"seriesNumber":"22","title":"Generalized gradient and contour program","docAbstract":"This program computes estimates of gradients, prepares contour maps, and plots various sets of data provided by the user on the CalComp plotters. The gradients represent the maximum rates of change of a real variable Z=f(X,Y) with respect to the twodimensional rectangle on which the function is defined. The contours are lines of equal Z values. The program also plots special line data sets provided by the user.","language":"English","publisher":"Computer Center Division","publisherLocation":"Washington, D.C.","doi":"10.3133/70039504","usgsCitation":"Hellman, M.S., 1972, Generalized gradient and contour program: Computer contribution 22, iv, 87 p., https://doi.org/10.3133/70039504.","productDescription":"iv, 87 p.","numberOfPages":"92","costCenters":[],"links":[{"id":261636,"rank":800,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/unnumbered/70039504/report.pdf"},{"id":261637,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/unnumbered/70039504/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a1533e4b0c8380cd54cfd","contributors":{"authors":[{"text":"Hellman, Marshall Strong","contributorId":75001,"corporation":false,"usgs":true,"family":"Hellman","given":"Marshall","email":"","middleInitial":"Strong","affiliations":[],"preferred":false,"id":466379,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70039552,"text":"70039552 - 1972 - U.S. Geological Survey National Center, Reston, Virginia","interactions":[],"lastModifiedDate":"2012-08-11T01:01:51","indexId":"70039552","displayToPublicDate":"2008-01-07T13:04:00","publicationYear":"1972","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"title":"U.S. Geological Survey National Center, Reston, Virginia","docAbstract":"In 1917 the Geological Survey moved into the newly built Interior Building near the White House in Washington, D. C. Twenty years later a larger building was constructed nearby to house the expanding U. S. Department of the Interior. Height restrictions reduced the planned size of the new building, and the Geological Survey was compelled to remain in the older Interior Building now identified as the General Services Administration Building. Expansion of the Survey's programs, and particularly the overall government need for additional office space in downtown Washington, has resulted in the Survey's activities being presently housed in 30 different buildings, at 17 widely scattered locations throughout the Washington Metropolitan Area.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/70039552","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1972, U.S. Geological Survey National Center, Reston, Virginia, 25 p., https://doi.org/10.3133/70039552.","productDescription":"25 p.","numberOfPages":"29","costCenters":[],"links":[{"id":261676,"rank":800,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/unnumbered/70039552/report.pdf"},{"id":261677,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/unnumbered/70039552/report-thumb.jpg"}],"country":"United States","state":"Virginia","city":"Reston","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -77.36666666666666,38.95 ], [ -77.36666666666666,38.93333333333333 ], [ -77.35,38.93333333333333 ], [ -77.35,38.95 ], [ -77.36666666666666,38.95 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bba78e4b08c986b3281ba","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":535349,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70010171,"text":"70010171 - 1972 - Middle pleistocene mollusks from St. Lawrence Island and their significance for the paleo-oceanography of the Bering Sea","interactions":[],"lastModifiedDate":"2025-07-11T16:07:00.57417","indexId":"70010171","displayToPublicDate":"2004-11-19T00:00:00","publicationYear":"1972","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3218,"text":"Quaternary Research","active":true,"publicationSubtype":{"id":10}},"title":"Middle pleistocene mollusks from St. Lawrence Island and their significance for the paleo-oceanography of the Bering Sea","docAbstract":"

Drift, evidently of Illinoian age, was deposited on St. Lawrence Island at the margin of an ice cap that covered the highlands of the Chukotka Peninsula of Siberia and spread far eastward on the continental shelf of northern Bering Sea. Underlying the drift on the northwestward part of the island are mollusk-bearing beds deposited during the Kotzebuan Transgression.

A comparison of mollusk faunas from St. Lawrence Island, Chukotka Peninsula, and Kotzebue Sound suggests that the present northward flow through Bering and Anadyr Straits was reversed during the Kotzebuan Transgression. Cold arctic water penetrated southward and southwestward bringing an arctic fauna to the Gulf of Anadyr. Warmer Pacific water probably entered eastern Bering Sea, passed eastward and northeastward around eastern and northern St. Lawrence Island, and then became entrained in the southward currents that passed through Anadyr Strait.

","language":"English","publisher":"Elsevier","doi":"10.1016/0033-5894(72)90033-6","issn":"00335894","usgsCitation":"Hopkins, D., Rowland, R., and Patton, W.W., 1972, Middle pleistocene mollusks from St. Lawrence Island and their significance for the paleo-oceanography of the Bering Sea: Quaternary Research, v. 2, no. 2, p. 119-134, https://doi.org/10.1016/0033-5894(72)90033-6.","productDescription":"16 p.","startPage":"119","endPage":"134","costCenters":[],"links":[{"id":219670,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Alaska","otherGeospatial":"St. Lawrence Island","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -172.62707116583636,\n 64.0488182952663\n ],\n [\n -172.62707116583636,\n 62.80972983412474\n ],\n [\n -168.38785991048877,\n 62.80972983412474\n ],\n [\n -168.38785991048877,\n 64.0488182952663\n ],\n [\n -172.62707116583636,\n 64.0488182952663\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","volume":"2","issue":"2","noUsgsAuthors":false,"publicationDate":"2017-01-20","publicationStatus":"PW","scienceBaseUri":"505a56eae4b0c8380cd6d8f7","contributors":{"authors":[{"text":"Hopkins, D.M.","contributorId":103646,"corporation":false,"usgs":true,"family":"Hopkins","given":"D.M.","email":"","affiliations":[],"preferred":false,"id":358193,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Rowland, R.W.","contributorId":36153,"corporation":false,"usgs":true,"family":"Rowland","given":"R.W.","email":"","affiliations":[],"preferred":false,"id":358192,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Patton, W. W. Jr.","contributorId":11231,"corporation":false,"usgs":true,"family":"Patton","given":"W.","suffix":"Jr.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":358191,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70009939,"text":"70009939 - 1972 - Appraisal of the future climate of the Holocene in the Rocky Mountains","interactions":[],"lastModifiedDate":"2025-07-11T15:57:31.67714","indexId":"70009939","displayToPublicDate":"2004-11-19T00:00:00","publicationYear":"1972","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3218,"text":"Quaternary Research","active":true,"publicationSubtype":{"id":10}},"title":"Appraisal of the future climate of the Holocene in the Rocky Mountains","docAbstract":"

Consideration of the history of Holocene climate in the Rocky Mountains indicates that the over-all trend during the past 2500 yr has been toward increasing warmth, interrupted by cooler times of minor advances of cirque glaciers. Comparison of Holocene climatic history with the record of past interglacials in the region suggests that the present interglacial is not complete and that the climate may become first warmer and subsequently wetter before it is completed. Correlation of the timing of the regional glacial-interglacial record for the past 140,000 yr with the record of major sea level changes and with the calculated changes in the earth's insolation suggest that the present interglacial may be completed within a few millenia and that it may be followed by a significant cooling of the climate.

","language":"English","publisher":"Elsevier","doi":"10.1016/0033-5894(72)90051-8","issn":"00335894","usgsCitation":"Richmond, G., 1972, Appraisal of the future climate of the Holocene in the Rocky Mountains: Quaternary Research, v. 2, no. 3, p. 315-322, https://doi.org/10.1016/0033-5894(72)90051-8.","productDescription":"8 p.","startPage":"315","endPage":"322","costCenters":[],"links":[{"id":219115,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"Canada, United States","otherGeospatial":"Rocky Mountain region","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -126.51511131378889,\n 60.2309575319278\n ],\n [\n -116.18429597454725,\n 42.750947322770955\n ],\n [\n -108.87838224399725,\n 36.86506804817596\n ],\n [\n -105.40760189448564,\n 35.35379898384873\n ],\n [\n -104.83911650777394,\n 41.21864052034894\n ],\n [\n -108.6656330679895,\n 48.208352104843684\n ],\n [\n -121.0355086645085,\n 59.62239173453176\n ],\n [\n -126.51511131378889,\n 60.2309575319278\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","volume":"2","issue":"3","noUsgsAuthors":false,"publicationDate":"2017-01-20","publicationStatus":"PW","scienceBaseUri":"5059ecd8e4b0c8380cd49509","contributors":{"authors":[{"text":"Richmond, G.M.","contributorId":104066,"corporation":false,"usgs":true,"family":"Richmond","given":"G.M.","email":"","affiliations":[],"preferred":false,"id":357495,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70010081,"text":"70010081 - 1972 - Pleistocene tectonic accretion of the continental slope off Washington","interactions":[],"lastModifiedDate":"2025-04-16T23:18:17.015983","indexId":"70010081","displayToPublicDate":"2003-04-07T00:00:00","publicationYear":"1972","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2667,"text":"Marine Geology","active":true,"publicationSubtype":{"id":10}},"title":"Pleistocene tectonic accretion of the continental slope off Washington","docAbstract":"

Interpretation of reflection profiles across the Washington continental margin suggests deformation of Cascadia basin strata against the continental slope. Individual reflecting horizons can be traced across the slope-basin boundary. The sense of offset along faults on the continental slope is predominantly, but not entirely, west side up. Two faults of small displacement are seen to be west-dipping reverse faults. Magnetic anomalies on the Juan de Fuca plate can be traced 40–100 km eastward under the slope, and structural interpretation combined with calculated rates of subduction suggests that approximately 50 km of the outer continental slope may have been formed in Pleistocene time. Rocks of Pleistocene age dredge from a ridge exposing acoustic “basement” on the slope, plus the results of deep-sea drilling off northern Oregon, are consistent with this interpretation. The question of whether or not subduction is occurring at present is unresolved because significant strain has not affected the upper 200 m of section in the Cascadia basin. However, deformation of the outer part of the slope has been episodic and may reflect episodic yield, deposition rate, subduction rate, or some combination of these factors.

","language":"English","publisher":"Elsevier","doi":"10.1016/0025-3227(72)90053-9","issn":"00253227","usgsCitation":"Silver, E.A., 1972, Pleistocene tectonic accretion of the continental slope off Washington: Marine Geology, v. 13, no. 4, p. 239-249, https://doi.org/10.1016/0025-3227(72)90053-9.","productDescription":"11 p.","startPage":"239","endPage":"249","costCenters":[],"links":[{"id":219428,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Washington","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -127.66113281249999,\n 45.644768217751924\n ],\n [\n -121.2451171875,\n 45.644768217751924\n ],\n [\n -121.2451171875,\n 48.545705491847464\n ],\n [\n -127.66113281249999,\n 48.545705491847464\n ],\n [\n -127.66113281249999,\n 45.644768217751924\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"13","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a7c54e4b0c8380cd79919","contributors":{"authors":[{"text":"Silver, E. A.","contributorId":18491,"corporation":false,"usgs":true,"family":"Silver","given":"E.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":357854,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70010180,"text":"70010180 - 1972 - Influence of grounding ice on the Arctic shelf of Alaska","interactions":[],"lastModifiedDate":"2025-04-16T23:14:25.067807","indexId":"70010180","displayToPublicDate":"2003-04-02T00:00:00","publicationYear":"1972","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2667,"text":"Marine Geology","active":true,"publicationSubtype":{"id":10}},"title":"Influence of grounding ice on the Arctic shelf of Alaska","docAbstract":"

Alaska's Beaufort Sea shelf is characterized by small-scale relief with an average amplitude of 1–2 m and wavelength of 50–100 m. Diving observations confirm that much of the bottom roughness reflects the action of grounded ice. Except for areas in the shadow of islands, bars, and offshore bathymetric highs, the entire shelf surface from the beach to at least the 75-m contour is now or has been modified by ice gouging. Ice contact with the bottom is more common, and rates of sedimentation higher on the inner shelf than on the outer shelf; the density of gouge features is about equal in both areas. Therefore, the chances are that an area of gouging on the inner shelf contains younger gouges than a similar area on the outer shelf.

When ice grounds, it becomes an important agent in the sedimentary and morphologic environment of the Arctic shelf, directly by deforming bottom deposits and secondarily by affecting the current regime near the sediment/ice contact. While bulldozing action and rafting do not seem to contribute significantly to the direct transport of sediment, re-suspension of bottom material during bulldozing, which makes sediment available for transport, may be significant.

","language":"English","publisher":"Elsevier","doi":"10.1016/0025-3227(72)90014-X","issn":"00253227","usgsCitation":"Reimnitz, E., Barnes, P., Forgatsch, T., and Rodeick, C., 1972, Influence of grounding ice on the Arctic shelf of Alaska: Marine Geology, v. 13, no. 5, p. 323-334, https://doi.org/10.1016/0025-3227(72)90014-X.","productDescription":"12 p.","startPage":"323","endPage":"334","costCenters":[],"links":[{"id":218631,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Alaska","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -146.44775390625,\n 69.89256519285392\n ],\n [\n -145.04150390625,\n 69.89256519285392\n ],\n [\n -145.04150390625,\n 70.18510275498964\n ],\n [\n -146.44775390625,\n 70.18510275498964\n ],\n [\n -146.44775390625,\n 69.89256519285392\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"13","issue":"5","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a3b3de4b0c8380cd62358","contributors":{"authors":[{"text":"Reimnitz, E.","contributorId":61557,"corporation":false,"usgs":true,"family":"Reimnitz","given":"E.","affiliations":[],"preferred":false,"id":358221,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Barnes, P.","contributorId":73331,"corporation":false,"usgs":true,"family":"Barnes","given":"P.","affiliations":[],"preferred":false,"id":358222,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Forgatsch, T.","contributorId":15335,"corporation":false,"usgs":true,"family":"Forgatsch","given":"T.","email":"","affiliations":[],"preferred":false,"id":358219,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Rodeick, C.","contributorId":19280,"corporation":false,"usgs":true,"family":"Rodeick","given":"C.","affiliations":[],"preferred":false,"id":358220,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":70188907,"text":"70188907 - 1972 - An inventory of suspended sediment stations and type of data analysis for Pennsylvania streams, 1947-1970","interactions":[],"lastModifiedDate":"2017-07-12T15:17:55","indexId":"70188907","displayToPublicDate":"2000-03-11T00:00:00","publicationYear":"1972","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"seriesTitle":{"id":375,"text":"Open-File Report","active":false,"publicationSubtype":{"id":6}},"title":"An inventory of suspended sediment stations and type of data analysis for Pennsylvania streams, 1947-1970","docAbstract":"

Data concerning suspended sediment concentrations and loads, frequency of occurrence of suspended sediment concentrations, and long-term trends of annual suspended sediment loads are important tools for today's environmental manager. These data are required background for those concerned with establishing and enforcing erosion and sedimentation control regulations and sediment concentration or turbidity standards for water-quality criteria, or those concerned with designing for adequate long-term water storage in reservoirs (sediment load), for efficient municipal and industrial plant operation (sediment concentration frequency), etc.

This is a compilation of the location, period of record, sampling frequency and type of data synthesis for suspended sediment carried by Pennsylvania streams. Figures 1 and 2 show the approximate locations of sediment sampling stations in Pennsylvania. All of the sediment data listed were collected by the U. S. Geological Survey mainly in cooperation with the following Federal, State, and local agencies.

Pennsylvania Department of Environmental Resources
     Bureau of Engineering and Construction
     Soil and Water Conservation Commission
Pennsylvania Department of Transportation
City of Philadelphia
Brandywine Valley Association
Delaware Geological Survey
Conestoga Valley Association
Lehigh County Soil and Water Conservation District
Corps of Engineers, U. S. Army

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The quality of water, sediment, and biota was determined at four sites in canals and drainage ditches at Miami International Airport (MIA) during high- and low-water periods and during summer and winter 1971–72. Concentrations of common ions, such as calcium, sodium, chloride, and magnesium, tended to be above average for fresh water because of periodic salt-water intrusion. Nitrogen, phosphorus, and pesticides were in higher concentrations than typical for undisturbed areas of south Florida, but not higher than usual for the urban coastal area, so it is not known to what extent these chemicals are attributable to surrounding urbanization. Heavy metals, oil and grease, and PCB's (polychlorinated biphenyls) were the best indicators of the effects of MIA on water quality. Concentations of the above were quite variable, high values for each were recorded and were probably associated with recent discharges from industrial sources. Arsenic, lead, iron, and chromium all exceeded, in one or more samples, the U.S. Public Health Service's recommended upper limits for metals in water. Only iron normally exceeds these standards in the natural waters of south Florida. PCB's were detected in most samples and were in concentrations up to 1,000 micrograms per kilogram in fish. In addition to pesticides and PCB's, another group of persistant chlorinated compounds, PCN's (polychlorinated naphthalenes) were detected in water, sediment, and fish. This is the first known detection of these compounds in the environment.

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St. Petersburg Coastal and Marine Science Center
U.S. Geological Survey
600 4th Street South
St. Petersburg, FL 33701

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