{"pageNumber":"5623","pageRowStart":"140550","pageSize":"25","recordCount":184769,"records":[{"id":70012384,"text":"70012384 - 1980 - Comment on 'Thin-skinned tectonics in the crystalline southern Appalachians: COCORP seismic- reflection profiling of the Blue Ridge and Piedmont'","interactions":[],"lastModifiedDate":"2024-02-01T12:30:44.901157","indexId":"70012384","displayToPublicDate":"1980-01-01T00:00:00","publicationYear":"1980","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1796,"text":"Geology","active":true,"publicationSubtype":{"id":10}},"title":"Comment on 'Thin-skinned tectonics in the crystalline southern Appalachians: COCORP seismic- reflection profiling of the Blue Ridge and Piedmont'","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"Geological Society of America","issn":"00917613","usgsCitation":"Moench, R.H., 1980, Comment on 'Thin-skinned tectonics in the crystalline southern Appalachians: COCORP seismic- reflection profiling of the Blue Ridge and Piedmont': Geology, v. 8, no. 9.","startPage":"402","costCenters":[],"links":[{"id":222410,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"8","issue":"9","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059f7ebe4b0c8380cd4cda3","contributors":{"authors":[{"text":"Moench, R. H.","contributorId":8853,"corporation":false,"usgs":true,"family":"Moench","given":"R.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":363423,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70012351,"text":"70012351 - 1980 - Aerial photography summary record system - five years later.","interactions":[],"lastModifiedDate":"2012-03-12T17:19:07","indexId":"70012351","displayToPublicDate":"1980-01-01T00:00:00","publicationYear":"1980","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3052,"text":"Photogrammetric Engineering and Remote Sensing","active":true,"publicationSubtype":{"id":10}},"title":"Aerial photography summary record system - five years later.","docAbstract":"Describes the APSRS, an automated information system for conventional aerial photography projects, established after the formation of the National Cartographic Information Center in the US Geological Survey in 1974. -after Author","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Photogrammetric Engineering and Remote Sensing","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","usgsCitation":"Lauterborn, T., 1980, Aerial photography summary record system - five years later.: Photogrammetric Engineering and Remote Sensing, v. 46, no. 12, p. 1537-1539.","startPage":"1537","endPage":"1539","numberOfPages":"3","costCenters":[],"links":[{"id":221941,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"46","issue":"12","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059e71ae4b0c8380cd4784f","contributors":{"authors":[{"text":"Lauterborn, T.J.","contributorId":53658,"corporation":false,"usgs":true,"family":"Lauterborn","given":"T.J.","email":"","affiliations":[],"preferred":false,"id":363342,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":47013,"text":"ofr8112 - 1980 - Geologic map and coal deposits of the western part of Ninemile Gap quadrangle and the southern part of Axial quadrangle, Moffat and Rio Blanco Counties, Colorado","interactions":[],"lastModifiedDate":"2023-05-03T18:39:47.207262","indexId":"ofr8112","displayToPublicDate":"1980-01-01T00:00:00","publicationYear":"1980","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"81-12","title":"Geologic map and coal deposits of the western part of Ninemile Gap quadrangle and the southern part of Axial quadrangle, Moffat and Rio Blanco Counties, Colorado","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr8112","usgsCitation":"Nutt, C.J., 1980, Geologic map and coal deposits of the western part of Ninemile Gap quadrangle and the southern part of Axial quadrangle, Moffat and Rio Blanco Counties, Colorado: U.S. Geological Survey Open-File Report 81-12, 4 Plates: 43.00 x 36.50 inches or smaller, https://doi.org/10.3133/ofr8112.","productDescription":"4 Plates: 43.00 x 36.50 inches or smaller","costCenters":[],"links":[{"id":172264,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":416665,"rank":6,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_11916.htm","linkFileType":{"id":5,"text":"html"}},{"id":20099,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/0012/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":20100,"rank":5,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/0012/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":20098,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/0012/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":20097,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/0012/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"24000","country":"United States","state":"Colorado","county":"Moffat County, Rio Blanco County","otherGeospatial":"Axial quadrangle, Ninemile Gap quadrangle","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -107.875,\n              40.117\n            ],\n            [\n              -107.75,\n              40.117\n            ],\n            [\n              -107.75,\n              40.25\n            ],\n            [\n              -107.875,\n              40.25\n            ],\n            [\n              -107.875,\n              40.117\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b15e4b07f02db6a4e25","contributors":{"authors":[{"text":"Nutt, Constance J. cnutt@usgs.gov","contributorId":1781,"corporation":false,"usgs":true,"family":"Nutt","given":"Constance","email":"cnutt@usgs.gov","middleInitial":"J.","affiliations":[],"preferred":true,"id":234495,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":5221592,"text":"5221592 - 1980 - Early concentrations of Brown Pelicans along southern Oregon coast","interactions":[],"lastModifiedDate":"2024-10-09T16:39:14.540082","indexId":"5221592","displayToPublicDate":"1980-01-01T00:00:00","publicationYear":"1980","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2793,"text":"Murrelet","active":true,"publicationSubtype":{"id":10}},"title":"Early concentrations of Brown Pelicans along southern Oregon coast","docAbstract":"<p>The California Brown Pelican (<i>Pelecanus occidentalis californicus</i>), which nests in southern California and Mexico, wanders north along the coast after the breeding season, sometimes as far as southern British Columbia (A.O.U. 1957). Anderson and Anderson (1976) and Ainley (1972) report that Mexico-originating pelicans disperse north in late summer and fall, increasing California coastal counts from late July through early November each year. Gabrielson and Jewett (1940) and Bayer (1977) reported that the northward flight into Oregon apparently occurs in July, and there are usually few present after the first of November. Similarly, Marshall (1969) reported that the Brown Pelican appeared regularly in the Netarts-Tillamook Bay area and more southern coastal points from August through November and indicated that a recent high count in Oregon was 110 in the Netarts-Tillamook Bay area on 27 August 1967. Bayer (1977) simultaneously observed 182 immature and 12 adult Brown Pelicans in the Yaquina estuary in October 1975 but noted that the number of adult pelicans (less than 20) observed in the Yaquina estuary seemed to remain relatively unchanged from year to year. He observed no more than 60 birds at a time in the Yaquina estuary in other years.</p>","language":"English","publisher":"Society for Northwestern Vertebrate Biology","doi":"10.2307/3535191","usgsCitation":"Henny, C.J., and Collins, J., 1980, Early concentrations of Brown Pelicans along southern Oregon coast: Murrelet, v. 61, no. 3, p. 99-100, https://doi.org/10.2307/3535191.","productDescription":"2 p.","startPage":"99","endPage":"100","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":18394,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://www.jstor.org/stable/3535191","linkFileType":{"id":5,"text":"html"}},{"id":198905,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United 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 \"}}]}","volume":"61","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a54e4b07f02db62c232","contributors":{"authors":[{"text":"Henny, Charles J.","contributorId":12578,"corporation":false,"usgs":true,"family":"Henny","given":"Charles","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":334218,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Collins, J.A.","contributorId":72412,"corporation":false,"usgs":true,"family":"Collins","given":"J.A.","email":"","affiliations":[],"preferred":false,"id":334219,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":5221607,"text":"5221607 - 1980 - Wildlife hazards from Furadan 3G applications to rice in Texas","interactions":[],"lastModifiedDate":"2024-10-28T16:09:46.407372","indexId":"5221607","displayToPublicDate":"1980-01-01T00:00:00","publicationYear":"1980","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":"Wildlife hazards from Furadan 3G applications to rice in Texas","docAbstract":"<p>Mortality of birds, fish, frogs, crayfish, earthworms, and nontarget insects occurred in rice fields after treatments of Furadan 3G granules in 3 Texas counties in 1970 and 1973-75. Three western sandpipers (<i>Ereunetes mauri</i>), 1 pectoral sandpiper (<i>Erolia melanotos</i>), and 2 red-winged blackbirds (<i>Agelaius phoeniceus</i>) were found dead or moribund between 17 and 24 hours after treatment. Cricket frogs (<i>Acris crepitans blanchardi</i>) were intoxicated 15 minutes post-treatment, and mosquito fish (<i>Gambusia affinis</i>) showed effects 1 hour post-treatment. Mortality of mosquito fish, Gulf menhaden (Brevoortia patronus), Atlantic croaker (Micropogon undulatus), and European carp (<i>Cyprinus carpio</i>) usually occurred between 24 and 28 hours after treatment. Mortality of frogs, crayfish, and nontarget insects generally occurred in rice field water between 1 and 45 hours after treatment. Mortality of earthworms in soil persisted for 52 hours. As a replacement for aldrin in Texas rice fields, Furadan 3G appeared to cause less mortality of birds than aldrin, but Furadan 3G was toxic to birds, fish, and invertebrates.</p>","language":"English","publisher":"Wiley","doi":"10.2307/3808365","usgsCitation":"Flickinger, E.L., King, K.A., Stout, W., and Mohn, M., 1980, Wildlife hazards from Furadan 3G applications to rice in Texas: Journal of Wildlife Management, v. 44, no. 1, p. 190-197, https://doi.org/10.2307/3808365.","productDescription":"8 p.","startPage":"190","endPage":"197","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":193448,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Texas","county":"Brazoria County, Colorado County, Wharton 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 \"}}]}","volume":"44","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f4e4b07f02db5f0224","contributors":{"authors":[{"text":"Flickinger, Edward L.","contributorId":48907,"corporation":false,"usgs":true,"family":"Flickinger","given":"Edward","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":334255,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"King, Kirke A.","contributorId":17727,"corporation":false,"usgs":true,"family":"King","given":"Kirke","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":334253,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Stout, W.F.","contributorId":40567,"corporation":false,"usgs":true,"family":"Stout","given":"W.F.","email":"","affiliations":[],"preferred":false,"id":334254,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Mohn, M.M.","contributorId":57169,"corporation":false,"usgs":true,"family":"Mohn","given":"M.M.","email":"","affiliations":[],"preferred":false,"id":334256,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":2001369,"text":"2001369 - 1980 - Important tapeworms of North American freshwater fishes","interactions":[],"lastModifiedDate":"2012-02-02T00:14:55","indexId":"2001369","displayToPublicDate":"1980-01-01T00:00:00","publicationYear":"1980","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":22,"text":"Fish Disease Leaflet","active":false,"publicationSubtype":{"id":1}},"seriesNumber":"59","title":"Important tapeworms of North American freshwater fishes","docAbstract":"No abstract available at this time","language":"English","publisher":"U.S. Fish and Wildlife Service","collaboration":"745/FH","usgsCitation":"Mitchell, A., and Hoffman, G.L., 1980, Important tapeworms of North American freshwater fishes: Fish Disease Leaflet 59, 18 p.","productDescription":"18 p.","startPage":"0","endPage":"18","numberOfPages":"18","costCenters":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"links":[{"id":94117,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://hdl.handle.net/2027/coo.31924000778476?urlappend=%3Bseq=179"},{"id":198856,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67c2df","contributors":{"authors":[{"text":"Mitchell, A.J.","contributorId":16345,"corporation":false,"usgs":true,"family":"Mitchell","given":"A.J.","email":"","affiliations":[],"preferred":false,"id":325605,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hoffman, G. L.","contributorId":70713,"corporation":false,"usgs":true,"family":"Hoffman","given":"G.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":325606,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":1003834,"text":"1003834 - 1980 - The isolation of a herpes virus from captive cranes with an inclusion body disease","interactions":[],"lastModifiedDate":"2019-11-13T13:44:41","indexId":"1003834","displayToPublicDate":"1980-01-01T00:00:00","publicationYear":"1980","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":948,"text":"Avian Diseases","active":true,"publicationSubtype":{"id":10}},"title":"The isolation of a herpes virus from captive cranes with an inclusion body disease","docAbstract":"<p>A viral agent, identified as a herpesvirus and tentatively called 'inclusion body disease of cranes' (IBDC), was isolated from captive cranes involved in a die-off at the International Crane Foundation near Baraboo, Wisconsin. Preliminary animal susceptibility tests, based on experimental infections, suggested that White Pekin ducklings up to 17 days old and adult coots were susceptible to the IBDC virus whereas 16-day-old White Leghorn chicks and 64-day-old Muscovy ducks were not. No serum antibody to IBDC virus was detected in 95 wild sandhill cranes collected in Wisconsin or Indiana in 1976 and 1977. However, 9 of 11 captive cranes in the affected area at the ICF had antibody to this agent.</p>","language":"English","publisher":"American Association of Avian Pathologists","doi":"10.2307/1589787","usgsCitation":"Docherty, D.E., and Henning, D., 1980, The isolation of a herpes virus from captive cranes with an inclusion body disease: Avian Diseases, v. 24, no. 1, p. 278-283, https://doi.org/10.2307/1589787.","productDescription":"6 p.","startPage":"278","endPage":"283","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":456,"text":"National Wildlife Health Center","active":true,"usgs":true}],"links":[{"id":130158,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Wisconsin","otherGeospatial":"International Crane Foundation","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -89.77726936340332,\n              43.54699285840481\n            ],\n            [\n              -89.76834297180174,\n              43.54699285840481\n            ],\n            [\n              -89.76834297180174,\n              43.550289946081115\n            ],\n            [\n              -89.77726936340332,\n              43.550289946081115\n            ],\n            [\n              -89.77726936340332,\n              43.54699285840481\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"24","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a54e4b07f02db62c62b","contributors":{"authors":[{"text":"Docherty, D. E.","contributorId":83469,"corporation":false,"usgs":true,"family":"Docherty","given":"D.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":314419,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Henning, D.J.","contributorId":71134,"corporation":false,"usgs":true,"family":"Henning","given":"D.J.","email":"","affiliations":[],"preferred":false,"id":314418,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70012373,"text":"70012373 - 1980 - Thickness change involved in the peat-to- coal transformation for a bituminous coal of Cretaceous age in central Utah","interactions":[],"lastModifiedDate":"2024-05-23T00:38:05.243105","indexId":"70012373","displayToPublicDate":"1980-01-01T00:00:00","publicationYear":"1980","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2450,"text":"Journal of Sedimentary Petrology","active":true,"publicationSubtype":{"id":10}},"title":"Thickness change involved in the peat-to- coal transformation for a bituminous coal of Cretaceous age in central Utah","docAbstract":"<div><div id=\"12458224\" class=\"article-section-wrapper js-article-section js-content-section  \" data-section-parent-id=\"0\"><p>The ratio of the thicknesses of a layer of peat and the coal bed formed from that peat has been calculated for a bituminous coal bed in central Utah. The method used involves comparison of the thickness of peat eroded by a laterally migrating channel system with the thickness of coal now absent from the outcrop. The peat:coal thickness ratio calculated by this method is approximately 11:1.</p></div></div>","language":"English","publisher":"SEPM","doi":"10.1306/212F7B44-2B24-11D7-8648000102C1865D","issn":"00224472","usgsCitation":"Ryer, T., and Langer, A., 1980, Thickness change involved in the peat-to- coal transformation for a bituminous coal of Cretaceous age in central Utah: Journal of Sedimentary Petrology, v. 50, no. 3, p. 987-992, https://doi.org/10.1306/212F7B44-2B24-11D7-8648000102C1865D.","productDescription":"6 p.","startPage":"987","endPage":"992","numberOfPages":"6","costCenters":[],"links":[{"id":222251,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"50","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bb29ce4b08c986b3258f0","contributors":{"authors":[{"text":"Ryer, Thomas A.","contributorId":46091,"corporation":false,"usgs":true,"family":"Ryer","given":"Thomas A.","affiliations":[],"preferred":false,"id":363401,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Langer, A.W.","contributorId":58396,"corporation":false,"usgs":true,"family":"Langer","given":"A.W.","email":"","affiliations":[],"preferred":false,"id":363402,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70012385,"text":"70012385 - 1980 - Geothermal system at 21°N, East Pacific Rise: physical limits on geothermal fluid and role of adiabatic expansion","interactions":[],"lastModifiedDate":"2015-06-12T16:09:47","indexId":"70012385","displayToPublicDate":"1980-01-01T00:00:00","publicationYear":"1980","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3338,"text":"Science","active":true,"publicationSubtype":{"id":10}},"title":"Geothermal system at 21°N, East Pacific Rise: physical limits on geothermal fluid and role of adiabatic expansion","docAbstract":"<p>Pressure-volume-temperature relations for water at the depth of the magma chamber at 21<span>&deg;</span>N on the East Pacific Rise suggest that the maximum subsurface temperature of the geothermal fluid is about 420<span>&deg;</span>C. Both the chemistry of the discharging fluid and thermal balance considerations indicate that the effective water/rock ratios in the geothermal system are between 7 and 16. Such low ratios preclude effective metal transport at temperatures below 350<span>&deg;</span>C, but metal solubilization at 400<span>&deg;</span>C and above is effective even at such low ratios. It is proposed that the 420<span>&deg;</span>C fluid ascends essentially adiabatically and in the process expands, cools, and precipitates metal sulfides within the upper few hundred meters of the sea floor and on the sea floor itself.</p>","language":"English","publisher":"AAAS","doi":"10.1126/science.207.4438.1465","issn":"00368075","usgsCitation":"Bischoff, J.L., 1980, Geothermal system at 21°N, East Pacific Rise: physical limits on geothermal fluid and role of adiabatic expansion: Science, v. 207, no. 4438, p. 1465-1469, https://doi.org/10.1126/science.207.4438.1465.","productDescription":"5 p.","startPage":"1465","endPage":"1469","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":222411,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"207","issue":"4438","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a28dce4b0c8380cd5a49d","contributors":{"authors":[{"text":"Bischoff, J. L.","contributorId":28969,"corporation":false,"usgs":true,"family":"Bischoff","given":"J.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":363424,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70012401,"text":"70012401 - 1980 - An econometric model of the U.S. secondary copper industry: Recycling versus disposal","interactions":[],"lastModifiedDate":"2024-04-22T14:53:39.082162","indexId":"70012401","displayToPublicDate":"1980-01-01T00:00:00","publicationYear":"1980","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2254,"text":"Journal of Environmental Economics and Management","active":true,"publicationSubtype":{"id":10}},"title":"An econometric model of the U.S. secondary copper industry: Recycling versus disposal","docAbstract":"<p><span>In this paper, a theoretical model of secondary recovery is developed that integrates microeconomic theories of production and cost with a dynamic model of scrap generation and accumulation. The model equations are estimated for the U.S. secondary copper industry and used to assess the impacts that various policies and future events have on copper recycling rates. The alternatives considered are: subsidies for secondary production, differing energy costs, and varying ore quality in primary production.</span></p>","language":"English","publisher":"Elsevier","doi":"10.1016/0095-0696(80)90014-5","issn":"00950696","usgsCitation":"Slade, M., 1980, An econometric model of the U.S. secondary copper industry: Recycling versus disposal: Journal of Environmental Economics and Management, v. 7, no. 2, p. 123-141, https://doi.org/10.1016/0095-0696(80)90014-5.","productDescription":"19 p.","startPage":"123","endPage":"141","numberOfPages":"19","costCenters":[],"links":[{"id":222593,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"7","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059ea2be4b0c8380cd4869c","contributors":{"authors":[{"text":"Slade, M.E.","contributorId":67659,"corporation":false,"usgs":true,"family":"Slade","given":"M.E.","email":"","affiliations":[],"preferred":false,"id":363454,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70012402,"text":"70012402 - 1980 - Asymmetric measures of association, closed data, and multivariate analysis","interactions":[],"lastModifiedDate":"2012-03-12T17:19:10","indexId":"70012402","displayToPublicDate":"1980-01-01T00:00:00","publicationYear":"1980","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2554,"text":"Journal of the International Association for Mathematical Geology","active":true,"publicationSubtype":{"id":10}},"title":"Asymmetric measures of association, closed data, and multivariate analysis","docAbstract":"The association between constant-sum variables Xiand Xjexpressed as percentages can be calculated as a product-moment correlation between Xiand Xj/(100 - Xi) and a correlation between Xjand Xi/(100 - Xj). An asymmetric, square matrix may be formed from these coefficients, and multivariate analysis performed by two methods: singular value decomposition and canonical decomposition. Either analysis avoids problems in the interpretation of correlation coefficients determined from closed arrays, and provides information about dependencies among the variables beyond that obtained from the usual correlation coefficient between Xiand Xj. Two examples show the canonical decomposition to have the greater usefulness. ?? 1980 Plenum Publishing Corporation.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Journal of the International Association for Mathematical Geology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisherLocation":"Kluwer Academic Publishers-Plenum Publishers","doi":"10.1007/BF01091206","issn":"00205958","usgsCitation":"Hohn, M., and Nuhfer, E., 1980, Asymmetric measures of association, closed data, and multivariate analysis: Journal of the International Association for Mathematical Geology, v. 12, no. 3, p. 235-246, https://doi.org/10.1007/BF01091206.","startPage":"235","endPage":"246","numberOfPages":"12","costCenters":[],"links":[{"id":205281,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1007/BF01091206"},{"id":222655,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"12","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059ee97e4b0c8380cd49e4f","contributors":{"authors":[{"text":"Hohn, M.","contributorId":92427,"corporation":false,"usgs":true,"family":"Hohn","given":"M.","email":"","affiliations":[],"preferred":false,"id":363456,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Nuhfer, E.B.","contributorId":89281,"corporation":false,"usgs":true,"family":"Nuhfer","given":"E.B.","email":"","affiliations":[],"preferred":false,"id":363455,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70012396,"text":"70012396 - 1980 - U-Pb ages of uraniferous opals and implications for the history of beryllium, fluorine, and uranium mineralization at Spor Mountain, Utah","interactions":[],"lastModifiedDate":"2023-12-12T23:45:01.045105","indexId":"70012396","displayToPublicDate":"1980-01-01T00:00:00","publicationYear":"1980","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1427,"text":"Earth and Planetary Science Letters","active":true,"publicationSubtype":{"id":10}},"title":"U-Pb ages of uraniferous opals and implications for the history of beryllium, fluorine, and uranium mineralization at Spor Mountain, Utah","docAbstract":"<div id=\"abstracts\" class=\"Abstracts u-font-serif text-s\"><div id=\"ab1\" class=\"abstract author\" lang=\"en\"><div id=\"aep-abstract-sec-id6\"><p>The U-Pb isotope systematics of uraniferous opals from Spor Mountain, Utah, were investigated to determine the suitability of such material for geochronologic purposes, and to estimate the timing of uranium and associated beryllium and fluorine mineralization. The results indicate that uraniferous opals can approximate a closed system for uranium and uranium daughters, so that dating samples as young as ∼1 m.y. should be possible. In addition, the expected lack of initial<sup>230</sup>Th and<sup>231</sup>Pa in opals permits valuable information on the initial<sup>234</sup>U/<sup>238</sup>U to be obtained on suitable samples of ≲10 m.y. age. The oldest<sup>207</sup>Pb/<sup>235</sup>U apparent age observed, 20.8 ± 1m.y., was that of the opal-fluorite core of a nodule from a beryllium deposit in the Spor Mountain Formation. This age is indistinguishable from that of fission-track and K-Ar ages from the host rhyolite, and links the mineralization to the first episode of alkali rhyolite magmatism and related hydrothermal activity at Spor Mountain. Successively younger ages of 13 m.y. and 8–9 m.y. on concentric outer zones of the same nodule indicate that opal formed either episodically or continuously for over 10 m.y. Several samples of both fracture-filling and massive-nodule opal associated with beryllium deposits gave<sup>207</sup>Pb/<sup>235</sup>U apparent ages of 13–16 m.y., which may reflect a restricted period of mineralization or perhaps an averaging of 21−and&lt;13−m.y. periods of opal growth. Several samples of fracture-filling opal in volcanic rocks as young as 6 m.y. gave<sup>207</sup>Pb/<sup>235</sup>U ages of 3.4–4.8 m.y. These ages may reflect hot-spring activity after the last major eruption of alkali rhyolite.</p></div></div></div>","language":"English","publisher":"Elsevier","doi":"10.1016/0012-821X(80)90008-4","issn":"0012821X","usgsCitation":"Ludwig, K., Lindsey, D.A., Zielinski, R.A., and Simmons, K.R., 1980, U-Pb ages of uraniferous opals and implications for the history of beryllium, fluorine, and uranium mineralization at Spor Mountain, Utah: Earth and Planetary Science Letters, v. 46, no. 2, p. 221-232, https://doi.org/10.1016/0012-821X(80)90008-4.","productDescription":"12 p.","startPage":"221","endPage":"232","numberOfPages":"12","costCenters":[],"links":[{"id":222534,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Utah","otherGeospatial":"Spor Mountain","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -113.25215279540696,\n              39.81329866968747\n            ],\n            [\n              -113.25215279540696,\n              39.69188127712721\n            ],\n            [\n              -113.11757027587542,\n              39.69188127712721\n            ],\n            [\n              -113.11757027587542,\n              39.81329866968747\n            ],\n            [\n              -113.25215279540696,\n              39.81329866968747\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","volume":"46","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bb9c4e4b08c986b327dc0","contributors":{"authors":[{"text":"Ludwig, K.R.","contributorId":97112,"corporation":false,"usgs":true,"family":"Ludwig","given":"K.R.","email":"","affiliations":[{"id":218,"text":"Denver Federal Center","active":false,"usgs":true}],"preferred":false,"id":363442,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lindsey, D. A.","contributorId":49814,"corporation":false,"usgs":true,"family":"Lindsey","given":"D.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":363440,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Zielinski, R. A. 0000-0002-4047-5129","orcid":"https://orcid.org/0000-0002-4047-5129","contributorId":106930,"corporation":false,"usgs":true,"family":"Zielinski","given":"R.","email":"","middleInitial":"A.","affiliations":[{"id":164,"text":"Central Energy Resources Science Center","active":true,"usgs":true}],"preferred":false,"id":363443,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Simmons, K. R.","contributorId":68771,"corporation":false,"usgs":true,"family":"Simmons","given":"K.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":363441,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70012387,"text":"70012387 - 1980 - Heat flow and energetics of the San Andreas fault zone","interactions":[],"lastModifiedDate":"2024-07-16T16:35:20.182875","indexId":"70012387","displayToPublicDate":"1980-01-01T00:00:00","publicationYear":"1980","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":6453,"text":"Journal of Geophysical Research Solid Earth","active":true,"publicationSubtype":{"id":10}},"title":"Heat flow and energetics of the San Andreas fault zone","docAbstract":"<p><span>Approximately 100 heat flow measurements in the San Andreas fault zone indicate (1) there is no evidence for local factional heating of the main fault trace at any latitude over a 1000-km length from Cape Mendocino to San Bernardino, (2) average heat flow is high (∼2 HFU, ∼80 mW m</span><sup>−2</sup><span>) throughout the 550-km segment of the Coast Ranges that encloses the San Andreas fault zone in central California; this broad anomaly falls off rapidly toward the Great Valley to the east, and over a 200-km distance toward the Mendocino Triple Junction to the northwest. As others have pointed out, a local conductive heat flow anomaly would be detectable unless the frictional resistance allocated to heat production on the main trace were ≲100 bars. Frictional work allocated to surface energy of new fractures is probably unimportant, and hydrologic convection is not likely to invalidate the conduction assumption, since the heat discharge by thermal springs near the fault is negligible. Explanations for the low dynamic friction fall into two intergradational classes: those in which the fault is weak all of the time and those in which it is weak only during earthquakes (possibly just large ones). The first class includes faults containing anomalously weak gouge materials and faults containing materials with normal frictional properties under near-lithostatic steady state fluid pressures. In the second class, weakening is caused by the event (for example, a thermally induced increase in fluid pressure, dehydration of clay minerals, or acoustic fluidization). In this class, unlike the first, the average strength and ambient tectonic shear stress may be large, ∼1 kbar, but the stress allocated to elastic radiation (the apparent stress) must be of similar magnitude, an apparent contradiction with seismic estimates. Unless seismic radiation is underestimated for large earthquakes, it is difficult to justify average tectonic stresses on the main trace of the San Andreas fault in excess of ∼200 bars. The development of the broad Coast Range heat flow anomaly southward from Cape Mendocino suggests that heat flow increases by a factor of 2 within 4 m.y. after the passage of the Mendocino Triple Junction. This passage leaves the San Andreas transform fault zone in its wake; the depth of the anomalous sources cannot be much greater than the depth of the seismogenic layer. Some of the anomalous heat may be supplied by conduction from the warmer mantle that must occur south of the Mendocino transform (where there is no subducting slab), and some might be supplied by shear heating in the fault zone. With no contribution from shear heating, extreme mantle upwelling would be required, and asthenosphere conditions should exist today at depths of only ∼20 km in the northernmost Coast Ranges. If there is an appreciable contribution from shear heating, the heat flow constraint implies that the seismogenic layer is partially decoupled at its base and that the basal traction is in the sense that resists right lateral motion on the fault(s). As a result of these basal tractions, the average shearing stress in the seismogenic layer would increase with distance from the main fault, and the seismogenic layer would offer substantial resistance to plate motion even though resistance on the main fault might be negligible. These speculative models have testable consequences.</span></p>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/JB085iB11p06185","issn":"01480227","usgsCitation":"Lachenbruch, A., and Sass, J., 1980, Heat flow and energetics of the San Andreas fault zone: Journal of Geophysical Research Solid Earth, v. 85, no. B11, p. 6185-6223, https://doi.org/10.1029/JB085iB11p06185.","productDescription":"39 p.","startPage":"6185","endPage":"6223","numberOfPages":"39","costCenters":[],"links":[{"id":222413,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"85","issue":"B11","noUsgsAuthors":false,"publicationDate":"2012-09-20","publicationStatus":"PW","scienceBaseUri":"505a2ff7e4b0c8380cd5d26e","contributors":{"authors":[{"text":"Lachenbruch, A.H.","contributorId":76737,"corporation":false,"usgs":true,"family":"Lachenbruch","given":"A.H.","affiliations":[],"preferred":false,"id":363427,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Sass, J.H.","contributorId":70749,"corporation":false,"usgs":true,"family":"Sass","given":"J.H.","email":"","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":363426,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70012386,"text":"70012386 - 1980 - Driving- stress waveform and the determination of rock internal friction by the stress-strain curve method.","interactions":[],"lastModifiedDate":"2013-03-12T11:31:07","indexId":"70012386","displayToPublicDate":"1980-01-01T00:00:00","publicationYear":"1980","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1804,"text":"Geophysical Journal of the Royal Astronomical Society","active":true,"publicationSubtype":{"id":10}},"title":"Driving- stress waveform and the determination of rock internal friction by the stress-strain curve method.","docAbstract":"Harmonic distortion in the stress-time function applied to rock specimens affects the measurement of rock internal friction in the seismic wave periods by the stress-strain hysteresis loop method. If neglected, the harmonic distortion can cause measurements of rock internal friction to be in error by 3O% in the linear range. The stress-time function therefore must be recorded and Fourier analysed for correct interpretation of the experimental data. Such a procedure would also yield a value for internal friction at the higher harmonic frequencies.-Author","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Geophysical Journal of the Royal Astronomical Society","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Wiley","doi":"10.1111/j.1365-246X.1980.tb02638.x","usgsCitation":"Liu, H., 1980, Driving- stress waveform and the determination of rock internal friction by the stress-strain curve method.: Geophysical Journal of the Royal Astronomical Society, v. 63, no. 2, p. 567-572, https://doi.org/10.1111/j.1365-246X.1980.tb02638.x.","startPage":"567","endPage":"572","numberOfPages":"6","costCenters":[],"links":[{"id":480592,"rank":1,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1111/j.1365-246x.1980.tb02638.x","text":"Publisher Index Page"},{"id":222412,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":269146,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1111/j.1365-246X.1980.tb02638.x"}],"volume":"63","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a03f2e4b0c8380cd506f0","contributors":{"authors":[{"text":"Liu, Hsi-Ping","contributorId":59944,"corporation":false,"usgs":true,"family":"Liu","given":"Hsi-Ping","affiliations":[],"preferred":false,"id":363425,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70012403,"text":"70012403 - 1980 - Declination and inclination errors in experimentally deposited specularite-bearing sand","interactions":[],"lastModifiedDate":"2023-12-12T23:42:12.076748","indexId":"70012403","displayToPublicDate":"1980-01-01T00:00:00","publicationYear":"1980","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1427,"text":"Earth and Planetary Science Letters","active":true,"publicationSubtype":{"id":10}},"title":"Declination and inclination errors in experimentally deposited specularite-bearing sand","docAbstract":"<div id=\"abstracts\" class=\"Abstracts u-font-serif text-s\"><div id=\"ab1\" class=\"abstract author\" lang=\"en\"><div id=\"aep-abstract-sec-id4\"><p>Naturally disaggregated specularite-bearing sandstone from the Triassic Moenkopi Formation, artificially deposited in controlled magnetic fields of ∼5 × 10<sup>−2</sup><span>&nbsp;</span>mT, acquires a stable remanent magnetization that has systematic errors in inclination and declination. Inclinations about 12° shallower than the applied fields are produced by deposition on a horizontal surface in still water. Deposition from flowing water on a surface inclined 6–10° results in inclination errors of as much as 20°. Water flowing obliquely to the applied field results in declination errors of about 10°, with declinations systematically rotated toward the upstream direction of current flow. These experimental results indicate that specularite-bearing sediment responds to the earth's field in a manner similar to magnetite-bearing sediment, and support observational evidence for a primary magnetization of depositional origin in specularite in red beds of the Moenkopi Formation.</p></div></div></div>","language":"English","publisher":"Elsevier","doi":"10.1016/0012-821X(80)90184-3","issn":"0012821X","usgsCitation":"Bressler, S., and Elston, D.P., 1980, Declination and inclination errors in experimentally deposited specularite-bearing sand: Earth and Planetary Science Letters, v. 48, no. 1, p. 227-232, https://doi.org/10.1016/0012-821X(80)90184-3.","productDescription":"6 p.","startPage":"227","endPage":"232","numberOfPages":"6","costCenters":[],"links":[{"id":222656,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"48","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059fe07e4b0c8380cd4ea9d","contributors":{"authors":[{"text":"Bressler, S.L.","contributorId":40221,"corporation":false,"usgs":true,"family":"Bressler","given":"S.L.","email":"","affiliations":[],"preferred":false,"id":363457,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Elston, D. P.","contributorId":96334,"corporation":false,"usgs":true,"family":"Elston","given":"D.","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":363458,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":46216,"text":"ofr80441 - 1980 - Maps showing hydrologic conditions in the San Francisco River area, Greenlee County, Arizona, 1978: A reconnaissance study","interactions":[],"lastModifiedDate":"2022-12-09T21:01:32.102478","indexId":"ofr80441","displayToPublicDate":"1980-01-01T00:00:00","publicationYear":"1980","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"80-441","title":"Maps showing hydrologic conditions in the San Francisco River area, Greenlee County, Arizona, 1978: A reconnaissance study","docAbstract":"<p>The San Francisco River area includes about 950 square miles in Greenlee County in east-central Arizona. Water-resources development has been slight compared with that in many areas in Arizona. In 1978 about 500 acre-feet of water was diverted for irrigation from the San Francisco and Blue Rivers, and about 550 acre-feet of ground water was withdrawn from wells for municipal use at Clifton. Surface water and ground water generally contained less than 500 milligrams per liter of dissolved solids; however, in the San Francisco River the dissolved-solids concentration increased from 263 to 885 milligrams per liter as the water moved downstream. The increase in dissolved solids was caused by inflow from springs near Clifton, one of which contained 11,700 milligrams per liter of dissolved solids. Information shown on the maps includes altitude of the water level, depth to water, well depth, streamflow characteristics of the San Francisco and Blue Rivers, and dissolved-solids and fluoride concentrations.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr80441","usgsCitation":"Mann, L.J., 1980, Maps showing hydrologic conditions in the San Francisco River area, Greenlee County, Arizona, 1978: A reconnaissance study (WRI/OFR): U.S. Geological Survey Open-File Report 80-441, 2 Plate: 27.50 × 33.00 inches and 27.92 × 33.53 inches, https://doi.org/10.3133/ofr80441.","productDescription":"2 Plate: 27.50 × 33.00 inches and 27.92 × 33.53 inches","costCenters":[],"links":[{"id":170844,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":410221,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_11635.htm","linkFileType":{"id":5,"text":"html"}},{"id":83191,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/0441/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":83190,"rank":1,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/0441/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Arizona","county":"Greenlee county","otherGeospatial":"San Francisco River area","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -109.464,\n              33.75\n            ],\n            [\n              -109.464,\n              33\n            ],\n            [\n              -109.05,\n              33\n            ],\n            [\n              -109.05,\n              33.75\n            ],\n            [\n              -109.464,\n              33.75\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","edition":"WRI/OFR","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a19e4b07f02db605ad4","contributors":{"authors":[{"text":"Mann, Larry J.","contributorId":48531,"corporation":false,"usgs":true,"family":"Mann","given":"Larry","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":232852,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70170291,"text":"70170291 - 1980 - Eruptions on Mount Etna during 1979","interactions":[],"lastModifiedDate":"2016-04-15T15:56:17","indexId":"70170291","displayToPublicDate":"1980-01-01T00:00:00","publicationYear":"1980","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1435,"text":"Earthquake Information Bulletin (USGS)","active":true,"publicationSubtype":{"id":10}},"title":"Eruptions on Mount Etna during 1979","language":"English","publisher":"U.S Geological Survey","usgsCitation":"Guest, J., Murray, J., Kilburn, C., and Lopes, R., 1980, Eruptions on Mount Etna during 1979: Earthquake Information Bulletin (USGS), v. 12, no. 4, p. 154-160.","productDescription":"7 p.","startPage":"154","endPage":"160","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":320082,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"12","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"571210b0e4b0ef3b7ca643dc","contributors":{"authors":[{"text":"Guest, J.","contributorId":168628,"corporation":false,"usgs":false,"family":"Guest","given":"J.","affiliations":[],"preferred":false,"id":626789,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Murray, J.","contributorId":94837,"corporation":false,"usgs":true,"family":"Murray","given":"J.","affiliations":[],"preferred":false,"id":626790,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Kilburn, C.","contributorId":149562,"corporation":false,"usgs":false,"family":"Kilburn","given":"C.","email":"","affiliations":[],"preferred":false,"id":626791,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Lopes, R.","contributorId":61554,"corporation":false,"usgs":true,"family":"Lopes","given":"R.","affiliations":[],"preferred":false,"id":626792,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70012419,"text":"70012419 - 1980 - Submarine volcanic features west of Kealakekua Bay, Hawaii","interactions":[],"lastModifiedDate":"2012-03-12T17:19:08","indexId":"70012419","displayToPublicDate":"1980-01-01T00:00:00","publicationYear":"1980","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2499,"text":"Journal of Volcanology and Geothermal Research","active":true,"publicationSubtype":{"id":10}},"title":"Submarine volcanic features west of Kealakekua Bay, Hawaii","docAbstract":"Visual observations of submarine volcanic vents were made from the submersible vehicle DSV \"Sea Cliff\" in water depths between 1310 and 690 m, west of Kealakekua Bay, Hawaii. Glass-rich, shelly submarine lavas surround circular 1- to 3-m-diameter volcanic vents between 1050 and 690 m depth in an area west-northwest of the southernpoint (Keei Pt.) of Kealakekua Bay. Eye-witness accounts indicate that this area was the site of a submarine eruption on February 24, 1877. Chemical analyses of lavas from these possible seafloor vent areas indicate that the eruptive products are very similar in composition to volcanic rocks produced by historic eruptions of Mauna Loa volcano. ?? 1980.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Journal of Volcanology and Geothermal Research","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","issn":"03770273","usgsCitation":"Fornari, D., Lockwood, J.P., Lipman, P.W., Rawson, M., and Malahoff, A., 1980, Submarine volcanic features west of Kealakekua Bay, Hawaii: Journal of Volcanology and Geothermal Research, v. 7, no. 3-4, p. 323-337.","startPage":"323","endPage":"337","numberOfPages":"15","costCenters":[],"links":[{"id":221948,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"7","issue":"3-4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505b9d3be4b08c986b31d705","contributors":{"authors":[{"text":"Fornari, D.J.","contributorId":49520,"corporation":false,"usgs":true,"family":"Fornari","given":"D.J.","email":"","affiliations":[],"preferred":false,"id":363502,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lockwood, J. P.","contributorId":104473,"corporation":false,"usgs":true,"family":"Lockwood","given":"J.","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":363505,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Lipman, P. W.","contributorId":93470,"corporation":false,"usgs":true,"family":"Lipman","given":"P.","middleInitial":"W.","affiliations":[],"preferred":false,"id":363504,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Rawson, M.","contributorId":10156,"corporation":false,"usgs":true,"family":"Rawson","given":"M.","email":"","affiliations":[],"preferred":false,"id":363501,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Malahoff, A.","contributorId":54344,"corporation":false,"usgs":true,"family":"Malahoff","given":"A.","email":"","affiliations":[],"preferred":false,"id":363503,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":1001437,"text":"1001437 - 1980 - Breeding biology of eastern phoebes in northern Wisconsin","interactions":[],"lastModifiedDate":"2017-10-20T11:00:53","indexId":"1001437","displayToPublicDate":"1980-01-01T00:00:00","publicationYear":"1980","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3783,"text":"The Wilson Bulletin","printIssn":"0043-5643","active":true,"publicationSubtype":{"id":10}},"title":"Breeding biology of eastern phoebes in northern Wisconsin","docAbstract":"Abstract has not been submitted","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Wilson Bulletin","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","usgsCitation":"Faanes, C.A., 1980, Breeding biology of eastern phoebes in northern Wisconsin: The Wilson Bulletin, v. 92, no. 1, p. 107-110.","productDescription":"4 p.","startPage":"107","endPage":"110","costCenters":[{"id":480,"text":"Northern Prairie Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":129011,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"92","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ce4b07f02db5fc64f","contributors":{"authors":[{"text":"Faanes, C. A.","contributorId":8790,"corporation":false,"usgs":true,"family":"Faanes","given":"C.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":311027,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":1001421,"text":"1001421 - 1980 - The comparison of usage and availability measurements for evaluating resource preference","interactions":[],"lastModifiedDate":"2017-12-27T12:44:50","indexId":"1001421","displayToPublicDate":"1980-01-01T00:00:00","publicationYear":"1980","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1465,"text":"Ecology","active":true,"publicationSubtype":{"id":10}},"title":"The comparison of usage and availability measurements for evaluating resource preference","docAbstract":"<p><span>Modern ecological research often involves the comparison of the usage of habitat types or food items to the availability of those resources to the animal. Widely used methods of determining preference from measurements of usage and availability depend critically on the array of components that the researcher, often with a degree of arbitrariness, deems available to the animal. This paper proposes a new method, based on ranks of components by usage and by availability. A virtue of the rank procedure is that it provides comparable results whether a questionable component is included or excluded from consideration. Statistical tests of significance are given for the method. The paper also offers a hierarchical ordering of selection processes. This hierarchy resolves certain inconsistencies among studies of selection and is compatible with the analytic technique offered in this paper.</span></p>","language":"English","publisher":"Ecological Society of America","doi":"10.2307/1937156","usgsCitation":"Johnson, D.H., 1980, The comparison of usage and availability measurements for evaluating resource preference: Ecology, v. 61, no. 1, p. 65-71, https://doi.org/10.2307/1937156.","productDescription":"7 p.","startPage":"65","endPage":"71","costCenters":[{"id":480,"text":"Northern Prairie Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":133833,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"61","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aaae4b07f02db668fae","contributors":{"authors":[{"text":"Johnson, Douglas H. 0000-0002-7778-6641 douglas_h_johnson@usgs.gov","orcid":"https://orcid.org/0000-0002-7778-6641","contributorId":1387,"corporation":false,"usgs":true,"family":"Johnson","given":"Douglas","email":"douglas_h_johnson@usgs.gov","middleInitial":"H.","affiliations":[{"id":480,"text":"Northern Prairie Wildlife Research Center","active":true,"usgs":true}],"preferred":true,"id":311012,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70012328,"text":"70012328 - 1980 - Ocean eddy structure by satellite radar altimetry required for iceberg towing","interactions":[],"lastModifiedDate":"2023-09-21T15:36:33.749133","indexId":"70012328","displayToPublicDate":"1980-01-01T00:00:00","publicationYear":"1980","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1264,"text":"Cold Regions Science and Technology","active":true,"publicationSubtype":{"id":10}},"title":"Ocean eddy structure by satellite radar altimetry required for iceberg towing","docAbstract":"<p><span>Models for the towing of large tabular icebergs give towing speeds of 0.5 knots to 1.0 knots relative to the ambient near surface current. Recent oceanographic research indicates that the world oceans are not principally composed of large steady-state current systems, like the Gulf Stream, but that most of the ocean momentum is probably involved in intense rings, formed by meanders of the large streams, and in mid-ocean eddies. These rings and eddies have typical dimensions on the order of 200 km with dynamic height anomalies across them of tens-of-centimeters to a meter. They migrate at speeds on the order of a few cm/sec. Current velocities as great as 3 knots have been observed in rings, and currents of 1 knot are common. Thus, the successful towing of icebergs is dependent on the ability to locate, measure, and track ocean rings and eddies. To accomplish this systematically on synoptic scales appears to be possible only by using satelliteborne radar altimeters. Ocean current and eddy structures as observed by the radar altimeters on the GEOS-3 and Seasat-1 satellites are presented and compared. Several satellite programs presently being planned call for flying radar altimeters in polar or near-polar orbits in the mid-1980 time frame. Thus, by the time tows of large icebergs will probably be attempted, it is possible synoptic observations of ocean rings and eddies which can be used to ascertain their location, size, intensity, and translation velocity will be a reality.</span></p>","language":"English","publisher":"Elsevier","doi":"10.1016/0165-232X(80)90049-X","usgsCitation":"Campbell, W.J., Cheney, R.E., Marsh, J.G., and Mognard, N.M., 1980, Ocean eddy structure by satellite radar altimetry required for iceberg towing: Cold Regions Science and Technology, v. 1, no. 3-4, p. 211-221, https://doi.org/10.1016/0165-232X(80)90049-X.","productDescription":"11 p.","startPage":"211","endPage":"221","numberOfPages":"11","costCenters":[],"links":[{"id":222131,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"1","issue":"3-4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a6c8ee4b0c8380cd74caa","contributors":{"authors":[{"text":"Campbell, W. J.","contributorId":8614,"corporation":false,"usgs":true,"family":"Campbell","given":"W.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":363286,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Cheney, R. E.","contributorId":87290,"corporation":false,"usgs":false,"family":"Cheney","given":"R.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":363289,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Marsh, J. G.","contributorId":53952,"corporation":false,"usgs":false,"family":"Marsh","given":"J.","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":363288,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Mognard, N. M.","contributorId":27612,"corporation":false,"usgs":false,"family":"Mognard","given":"N.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":363287,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70164458,"text":"70164458 - 1980 - Earthquake alarm; operating the seismograph station at the University of California, Berkeley.","interactions":[],"lastModifiedDate":"2016-03-22T10:44:53","indexId":"70164458","displayToPublicDate":"1980-01-01T00:00:00","publicationYear":"1980","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1435,"text":"Earthquake Information Bulletin (USGS)","active":true,"publicationSubtype":{"id":10}},"title":"Earthquake alarm; operating the seismograph station at the University of California, Berkeley.","docAbstract":"<p>An alarm bell rings at the seismographic station and at the office of the campus police. It is 3:00 on a foggy San Francisco morning. Somewhere in the world an earthquake has occurred. The police telephone the duty seismologist at home telling him that the alarm has triggered. He makes his way into the seismograph station, bathrobe and all, to locate the earthquake and determine its magnitude. In this way, many seismology graduate students have been initiated into the responsibilities of running a seismographic station.&nbsp;</p>\n<p>At the University of California seismographic stations, the task of locating and determining magnitudes for both local and distant earthquakes is a continuous one. Teleseisms must be located rapidly so that events that occur in the Pacific can be identified and the Pacific Tsunami Warning System alerted. For great earthquakes anywhere, there is a responsibility to notify public agencies such as the California Office of Emergency Services, the Federal Disaster Assistance Administration, the Earthquake Engineering Research Institute, the California Seismic Safety Commission, and the American Red Cross. In the case of damaging local earthquakes, it is necessary to alert also the California Department of Water Resources, California Division of Mines and Geology, U.S Army Corps of Engineers, Federal Bureau of Reclamation, and the Bay Area Rapid Transit. These days, any earthquakes that are felt in northern California cause immediate inquiries from the news media and an interested public. The series of earthquakes that jolted the Livermore area from January 24 to 26 1980, is a good case in point.&nbsp;</p>","language":"English","publisher":"U.S Geological Survey","usgsCitation":"Stump, B., 1980, Earthquake alarm; operating the seismograph station at the University of California, Berkeley.: Earthquake Information Bulletin (USGS), v. 12, no. 3, p. 88-97.","productDescription":"10 p.","startPage":"88","endPage":"97","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":316619,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"12","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"56b5d5d1e4b0cc7999817179","contributors":{"authors":[{"text":"Stump, B.","contributorId":156269,"corporation":false,"usgs":false,"family":"Stump","given":"B.","email":"","affiliations":[],"preferred":false,"id":597506,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":64774,"text":"i1254A - 1980 - Map showing water circulation and rates of sedimentation in the Port Isabel 1 degree by 2 degrees quadrangle, Texas","interactions":[],"lastModifiedDate":"2023-08-29T18:31:13.927695","indexId":"i1254A","displayToPublicDate":"1980-01-01T00:00:00","publicationYear":"1980","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":320,"text":"IMAP","code":"I","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1254","subseriesTitle":"MGA","chapter":"A","title":"Map showing water circulation and rates of sedimentation in the Port Isabel 1 degree by 2 degrees quadrangle, Texas","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/i1254A","usgsCitation":"Berryhill, H.L., and Trippet, A., 1980, Map showing water circulation and rates of sedimentation in the Port Isabel 1 degree by 2 degrees quadrangle, Texas: U.S. Geological Survey IMAP 1254, Report: 1 p.; 1 Plate: 46.83 x 24.80 inches, https://doi.org/10.3133/i1254A.","productDescription":"Report: 1 p.; 1 Plate: 46.83 x 24.80 inches","costCenters":[],"links":[{"id":255197,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/1254a/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":255198,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/imap/1254a/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":420252,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_9078.htm","linkFileType":{"id":5,"text":"html"}},{"id":255199,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/imap/1254a/report-thumb.jpg"}],"scale":"250000","country":"United States","state":"Texas","otherGeospatial":"Port Isabel 1 degree x 2 degrees quadrangle","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -97.5,\n              28\n            ],\n            [\n              -97.5,\n              27\n            ],\n            [\n              -96,\n              27\n            ],\n            [\n              -96,\n              28\n            ],\n            [\n              -97.5,\n              28\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a6fe4b07f02db640e0a","contributors":{"authors":[{"text":"Berryhill, H. L. Jr.","contributorId":35361,"corporation":false,"usgs":true,"family":"Berryhill","given":"H.","suffix":"Jr.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":272129,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Trippet, A. R.","contributorId":105377,"corporation":false,"usgs":true,"family":"Trippet","given":"A. R.","affiliations":[],"preferred":false,"id":272130,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70164349,"text":"70164349 - 1980 - Monitoring active volcanoes","interactions":[],"lastModifiedDate":"2016-03-21T15:27:11","indexId":"70164349","displayToPublicDate":"1980-01-01T00:00:00","publicationYear":"1980","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1435,"text":"Earthquake Information Bulletin (USGS)","active":true,"publicationSubtype":{"id":10}},"title":"Monitoring active volcanoes","docAbstract":"<p>One of the most spectacular, awesomely beautiful, and at times, most destructive displays of natural energy is an erupting volcano, belching fume and ash thousands of feet into the atmoshpehere and pouring out red-hot molten lava in fountains and streams.&nbsp;</p>","language":"English","publisher":"U.S Geological Survey","usgsCitation":"Tilling, R., 1980, Monitoring active volcanoes: Earthquake Information Bulletin (USGS), v. 12, no. 4, p. 131-134.","productDescription":"4 p.","startPage":"131","endPage":"134","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":316425,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"12","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"56b08fe1e4b010e2af2a5de5","contributors":{"authors":[{"text":"Tilling, R.I. 0000-0003-4263-7221","orcid":"https://orcid.org/0000-0003-4263-7221","contributorId":98311,"corporation":false,"usgs":true,"family":"Tilling","given":"R.I.","affiliations":[],"preferred":false,"id":597086,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70169176,"text":"70169176 - 1980 - Earthquakes; March-April 1980","interactions":[],"lastModifiedDate":"2016-03-29T14:36:47","indexId":"70169176","displayToPublicDate":"1980-01-01T00:00:00","publicationYear":"1980","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1435,"text":"Earthquake Information Bulletin (USGS)","active":true,"publicationSubtype":{"id":10}},"title":"Earthquakes; March-April 1980","docAbstract":"<p>Two of the three major (7.0-7.9) earthquakes during this reporting period occurred in the South Pacific on March 8 and April 13. The third, in the Fox Islands, Aleutian Islands, on March 23, was the first major earthquake of the year in the United States. In the State of Washington, thousands of earthquakes associated with Mount St. Helens volcano have occurred since March 20. There were no earthquake-related deaths reported during the second 2 months of the year.&nbsp;</p>","language":"English","publisher":"U.S Geological Survey","usgsCitation":"Person, W., 1980, Earthquakes; March-April 1980: Earthquake Information Bulletin (USGS), v. 12, no. 6, p. 228-231.","productDescription":"4 p.","startPage":"228","endPage":"231","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":319320,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"12","issue":"6","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"56f3be3ee4b0f59b85e02e56","contributors":{"authors":[{"text":"Person, W. J.","contributorId":91472,"corporation":false,"usgs":true,"family":"Person","given":"W. J.","affiliations":[],"preferred":false,"id":623290,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
]}