Plateau-side terraces in arid areas around the world are commonly described as pediment remnants, although, in many cases, they may have been formed by debris-flow deposition. Pediments do exist in the area of the Aquarius and Kaiparowits Plateaus of southern Utah; however, many alluvial terraces that were classified by previous workers as pediments are actually formed of thick deposits of sediment released into valleys by episodic landslide events. Pedimentation may have implications of base level stability and aridity that are very different from the implications of landsliding, so that the identification of pediments where none exist, as has occurred for some places in the Aquarius and Kaiparowits areas, may result in erroneous interpretations of geologic history. Although both pediment and debris-flow depositional terraces have smooth, alluvium-covered upper surfaces, the two can be distinguished by the shape of the underlying bedrock surface and the process of formation. The distinction is that pedimentation produces smooth relief through erosion whereas wet debris flow produces smooth relief through deposition, although transitional phases exist. Most terraces on the flanks of the Aquarius and Kaiparowits Plateaus reflect periods of valley filling when wet debris flows rapidly deposited large quantities of sediment. The sources of the wet debris-flow sediment were large lobes of landslide debris that carried down sediment from high on the plateau sides. The relation of younger terraces to landsliding is clear, because the terrace surfaces are graded to the toes of slide lobes, but the origin of older terraces is less obvious, because older lobes of slide debris have generally been removed by erosion.
","language":"English","publisher":"University of Chicago Press","doi":"10.1086/628880","issn":"00221376","usgsCitation":"Williams, V.S., 1984, Pedimentation versus debris-flow origin of plateau-side desert terraces in southern Utah: Journal of Geology, v. 92, no. 4, p. 457-468, https://doi.org/10.1086/628880.","productDescription":"12 p.","startPage":"457","endPage":"468","numberOfPages":"12","costCenters":[],"links":[{"id":225289,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"92","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a7626e4b0c8380cd77f5c","contributors":{"authors":[{"text":"Williams, V. S.","contributorId":8876,"corporation":false,"usgs":true,"family":"Williams","given":"V.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":367316,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70014000,"text":"70014000 - 1984 - Glacier mass balance and runoff research in the U.S.A.","interactions":[],"lastModifiedDate":"2023-12-19T00:49:29.152399","indexId":"70014000","displayToPublicDate":"1984-01-01T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1767,"text":"Geografiska Annaler, Series A","active":true,"publicationSubtype":{"id":10}},"title":"Glacier mass balance and runoff research in the U.S.A.","docAbstract":"Research on glacier mass balance began in the U.S.A. about 50 years ago. More complete studies of climate, snow and ice balance, and the hydrology of glaciers were initiated for the IGY in 1957 and the IHD in 1966. Investigations included the magnitude and geographic distribution of normal mass balance processes and unusual phenomena such as out-bursting, accumulation of ice by freezing of water in firn, and ablation of glacier ice by volcanic activity and by calving. Glacier size has been found not to be a simple function of climate as is widely imagined. Glaciers can increase with a warming of climate and can shrink due to calving instability mechanisms. Numerical modeling of glacier balance and runoff have appeared in the past decade only. Glacier research has also produced a new understanding of the nation's climate, water resources, and flood hazards because glaciers exist in very moist rather than very cold climates and produce very high runoff rates.
Study of an algal, sapropelic sediment from Mangrove Lake, Bermuda shows that the mass balance of carbon and stable carbon isotopes in the major organic constituents is accounted for by a relatively straightforward model of selective preservation during diagenesis. The loss of 13C-enriched carbohydrates is the principal factor controlling the intermolecular mass balance of 13C in the sapropel. Results indicate that labile components are decomposed leaving as a residual concentrate in the sediment an insoluble humic substance that may be an original biochemical component of algae and associated bacteria. An overall decrease of up to about 4‰ in the δ 13C values of the organic matter is observed as a result of early diagenesis.
","language":"English","publisher":"Elsevier","doi":"10.1016/0146-6380(84)90016-0","usgsCitation":"Spiker, E.C., and Hatcher, P.G., 1984, Carbon isotope fractionation of sapropelic organic matter during early diagenesis: Organic Geochemistry, v. 5, no. 4, p. 283-290, https://doi.org/10.1016/0146-6380(84)90016-0.","productDescription":"8 p.","startPage":"283","endPage":"290","costCenters":[],"links":[{"id":225550,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"Bermuda","otherGeospatial":"Mangrove Lake","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -64.74165211543514,\n 32.345696412628826\n ],\n [\n -64.74165211543514,\n 32.32102617325248\n ],\n [\n -64.70426092644328,\n 32.32102617325248\n ],\n [\n -64.70426092644328,\n 32.345696412628826\n ],\n [\n -64.74165211543514,\n 32.345696412628826\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","volume":"5","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059f366e4b0c8380cd4b7a0","contributors":{"authors":[{"text":"Spiker, Elliott C.","contributorId":50174,"corporation":false,"usgs":true,"family":"Spiker","given":"Elliott","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":367355,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hatcher, Patrick G.","contributorId":93625,"corporation":false,"usgs":true,"family":"Hatcher","given":"Patrick","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":367354,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70014022,"text":"70014022 - 1984 - Optimization of electrothermal atomization parameters for simultaneous multielement atomic absorption spectrometry","interactions":[],"lastModifiedDate":"2023-03-10T17:01:58.649487","indexId":"70014022","displayToPublicDate":"1984-01-01T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":761,"text":"Analytical Chemistry","active":true,"publicationSubtype":{"id":10}},"title":"Optimization of electrothermal atomization parameters for simultaneous multielement atomic absorption spectrometry","docAbstract":"The effect of the acid matrix, the measurement mode (height or area), the atomizer surface (unpyrolyzed and pyrolyzed graphite), the atomization mode (from the wall or from a platform), and the atomization temperature on the simultaneous electrothermal atomization of Co, Cr, Cu, Fe, Mn, Mo, Ni, V, and Zn was examined. The 5% HNO3 matrix gave rise to severe irreproducibility using a pyrolyzed tube unless the tube was properly \"prepared\". The 5% HCl matrix did not exhibit this problem, and no problems were observed with either matrix using an unpyrolized tube or a pyrolyzed platform. The 5% HCl matrix gave better sensitivities with a pyrolyzed tube but the two matrices were comparable for atomization from a platform. If Mo and V are to be analyzed with the other seven elements, a high atomization temperature (2700??C or greater) is necessary regardless of the matrix, the measurement mode, the atomization mode, or the atomizer surface. Simultaneous detection limits (peak height with pyrolyzed tube atomization) were comparable to those of conventional atomic absorption spectrometry using electrothermal atomization above 280 nm. Accuracies and precisions of ??10-15% were found in the 10 to 120 ng mL-1 range for the analysis of NBS acidified water standards.","language":"English","publisher":"ACS Publications","doi":"10.1021/ac00265a014","usgsCitation":"Harnly, J.M., and Kane, J., 1984, Optimization of electrothermal atomization parameters for simultaneous multielement atomic absorption spectrometry: Analytical Chemistry, v. 56, no. 1, p. 48-54, https://doi.org/10.1021/ac00265a014.","productDescription":"7 p.","startPage":"48","endPage":"54","numberOfPages":"7","costCenters":[],"links":[{"id":225866,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"56","issue":"1","noUsgsAuthors":false,"publicationDate":"2002-05-01","publicationStatus":"PW","scienceBaseUri":"505a6ef2e4b0c8380cd7589f","contributors":{"authors":[{"text":"Harnly, J. M.","contributorId":22492,"corporation":false,"usgs":false,"family":"Harnly","given":"J.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":367397,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kane, Jean S.","contributorId":66544,"corporation":false,"usgs":true,"family":"Kane","given":"Jean S.","affiliations":[],"preferred":false,"id":367398,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70168852,"text":"70168852 - 1984 - Earthquakes, May-June 1984","interactions":[],"lastModifiedDate":"2016-03-24T15:54:09","indexId":"70168852","displayToPublicDate":"1984-01-01T00:00:00","publicationYear":"1984","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, May-June 1984","docAbstract":"No major earthquakes (7.0-7.9) occurred during this reporting period. earthquake-rated deaths were reported from Italy, the Dominican Republic, and Yugoslavia. A number of earthquakes occurred in the United States but none caused casualties or any significant damage.
","language":"English","publisher":"U.S Geological Survey","usgsCitation":"Person, W., 1984, Earthquakes, May-June 1984: Earthquake Information Bulletin (USGS), v. 16, no. 6, p. 228-230.","productDescription":"3 p.","startPage":"228","endPage":"230","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":318600,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"16","issue":"6","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"56dabfc9e4b015c306f84c59","contributors":{"authors":[{"text":"Person, W. J.","contributorId":91472,"corporation":false,"usgs":true,"family":"Person","given":"W. J.","affiliations":[],"preferred":false,"id":621987,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":19993,"text":"ofr84210 - 1984 - A tabulation of lead isotopic ratios for lead minerals from mines and prospects in the Belt-Purcell Basin in the United States and Canada","interactions":[],"lastModifiedDate":"2023-03-01T20:08:54.441043","indexId":"ofr84210","displayToPublicDate":"1984-01-01T00:00:00","publicationYear":"1984","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":"84-210","title":"A tabulation of lead isotopic ratios for lead minerals from mines and prospects in the Belt-Purcell Basin in the United States and Canada","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr84210","usgsCitation":"Marvin, R.F., and Zartman, R., 1984, A tabulation of lead isotopic ratios for lead minerals from mines and prospects in the Belt-Purcell Basin in the United States and Canada: U.S. Geological Survey Open-File Report 84-210, Report: 15 p.; 1 Plate: 22.60 x 28.52 inches, https://doi.org/10.3133/ofr84210.","productDescription":"Report: 15 p.; 1 Plate: 22.60 x 28.52 inches","costCenters":[],"links":[{"id":413548,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_13312.htm","linkFileType":{"id":5,"text":"html"}},{"id":49518,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1984/0210/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":49517,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1984/0210/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":151327,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1984/0210/report-thumb.jpg"}],"country":"Canada, United States","state":"Alberta, British Columbia, Idaho, Montana, Washington","otherGeospatial":"Belt-Purcell Basin","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -111.85126829051268,\n 47.51912797943302\n ],\n [\n -113.24642463223171,\n 49.2299445037211\n ],\n [\n -114.47492023333203,\n 49.696059597689924\n ],\n [\n -114.906743277857,\n 49.51010512297134\n ],\n [\n -118.92260018522668,\n 51.751386757737606\n ],\n [\n -118.27304828221179,\n 47.68012484142176\n ],\n [\n -118.64009174101372,\n 46.29225328929587\n ],\n [\n -116.00866997877048,\n 45.832081398446576\n ],\n [\n -116.02157053323668,\n 44.501410474871335\n ],\n [\n -114.84669696269859,\n 43.21667091386982\n ],\n [\n -113.43605155461651,\n 42.620718613646545\n ],\n [\n -113.22931357941593,\n 42.274790890237284\n ],\n [\n -112.2936867356251,\n 42.37994309607001\n ],\n [\n -111.6920319871947,\n 44.849539042002704\n ],\n [\n -110.46707425792073,\n 45.856035550896166\n ],\n [\n -109.28208792201963,\n 46.81971538338448\n ],\n [\n -109.85600874794352,\n 47.429809651982765\n ],\n [\n -111.85126829051268,\n 47.51912797943302\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b17e4b07f02db6a5cac","contributors":{"authors":[{"text":"Marvin, R. F.","contributorId":60597,"corporation":false,"usgs":true,"family":"Marvin","given":"R.","middleInitial":"F.","affiliations":[],"preferred":false,"id":181868,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Zartman, R. E.","contributorId":15632,"corporation":false,"usgs":true,"family":"Zartman","given":"R. E.","affiliations":[],"preferred":false,"id":181867,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70164468,"text":"70164468 - 1984 - Eyewitness account of the 1931 great earthquake at Hawke’s Bay, New Zealand","interactions":[],"lastModifiedDate":"2019-11-13T15:12:54","indexId":"70164468","displayToPublicDate":"1984-01-01T00:00:00","publicationYear":"1984","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":"Eyewitness account of the 1931 great earthquake at Hawke’s Bay, New Zealand","docAbstract":"No part of New Zealand is far from a known earthquake origin. The magnitude 7.9 earthquake of 1931 at Hawke's Bay, North Island, on February 3, 1931, was the most serious event recorded in New Zealand hsitory. It was responsible for 256 deaths. The Modified Mercalli intensity reached XI in Napier, a city of 35,000 people, and hence, caused considerable destruction to property.
","language":"English","publisher":"U.S Geological Survey","usgsCitation":"Spall, H., 1984, Eyewitness account of the 1931 great earthquake at Hawke’s Bay, New Zealand: Earthquake Information Bulletin (USGS), v. 16, no. 1, p. 12-20.","productDescription":"9 p.","startPage":"12","endPage":"20","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":316629,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"New Zealand","otherGeospatial":"Hawkes Bay","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n 176.66015625,\n -39.753656971363085\n ],\n [\n 178.000488281,\n -39.753656971363085\n ],\n [\n 178.000488281,\n -38.8225909761771\n ],\n [\n 176.66015625,\n -38.8225909761771\n ],\n [\n 176.66015625,\n -39.753656971363085\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"16","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"56b5d5dae4b0cc79998171b4","contributors":{"authors":[{"text":"Spall, H.","contributorId":99290,"corporation":false,"usgs":true,"family":"Spall","given":"H.","affiliations":[],"preferred":false,"id":597523,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70014023,"text":"70014023 - 1984 - Concentrations and isotope ratios of carbon, nitrogen and sulfur in ocean-floor basalts","interactions":[],"lastModifiedDate":"2024-03-19T16:23:31.926842","indexId":"70014023","displayToPublicDate":"1984-01-01T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1759,"text":"Geochimica et Cosmochimica Acta","active":true,"publicationSubtype":{"id":10}},"title":"Concentrations and isotope ratios of carbon, nitrogen and sulfur in ocean-floor basalts","docAbstract":"Fresh submarine basalt glasses from Galapagos Ridge, FAMOUS area, Cayman Trough and Kilauea east rift contain 22 to 160 ppm carbon and 0.3 to 2.8 ppm nitrogen, respectively, as the sums of dissolved species and vesicle-filling gases (CO2 and N2). The large range of variation in carbon content is due to combined effect of depth-dependency of the solubility of carbon in basalt melt and varying extents of vapour loss during magma emplacement as well as in sample crushing. The isotopic ratios of indigenous carbon and nitrogen are in very narrow ranges,−6.2 ± 0.2% relative to PDB and +0.2 ± 0.6 %. relative to atmospheric nitrogen, respectively. In basalt samples from Juan de Fuca Ridge, however, isotopically light carbon (δ13C = around −24%.) predominates over the indigenous carbon; no indigenous heavy carbon was found. Except for Galapagos Ridge samples, these ocean-floor basalts contain 670 to 1100 ppm sulfur, averaging 810 ppm, in the form of both sulfide and sulfate, whereas basalts from Galapagos Ridge are higher in both sulfur (1490 and 1570 ppm) and iron (11.08% total iron as FeO). The δ34S values average +0.3 ± 0.5%. with average fractionation factor between sulfate and sulfide of +7.4 ± 1.6%.. The sulfate/sulfide ratios tend to increase with increasing water content of basalt, probably because the oxygen fugacity increases with increasing water content in basalt melt.
","language":"English","publisher":"Elsevier","doi":"10.1016/0016-7037(84)90295-3","issn":"00167037","usgsCitation":"Sakai, H., Marais, D., Ueda, A., and Moore, J., 1984, Concentrations and isotope ratios of carbon, nitrogen and sulfur in ocean-floor basalts: Geochimica et Cosmochimica Acta, v. 48, no. 12, p. 2433-2441, https://doi.org/10.1016/0016-7037(84)90295-3.","productDescription":"9 p.","startPage":"2433","endPage":"2441","numberOfPages":"9","costCenters":[],"links":[{"id":225867,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"48","issue":"12","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059f985e4b0c8380cd4d65d","contributors":{"authors":[{"text":"Sakai, H.","contributorId":92800,"corporation":false,"usgs":true,"family":"Sakai","given":"H.","email":"","affiliations":[],"preferred":false,"id":367401,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Marais, D.J.D.","contributorId":22506,"corporation":false,"usgs":true,"family":"Marais","given":"D.J.D.","email":"","affiliations":[],"preferred":false,"id":367399,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Ueda, A.","contributorId":104638,"corporation":false,"usgs":true,"family":"Ueda","given":"A.","email":"","affiliations":[],"preferred":false,"id":367402,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Moore, J.G.","contributorId":67496,"corporation":false,"usgs":true,"family":"Moore","given":"J.G.","email":"","affiliations":[],"preferred":false,"id":367400,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":70168853,"text":"70168853 - 1984 - Earthquakes, March-April 1984","interactions":[],"lastModifiedDate":"2016-03-24T15:52:38","indexId":"70168853","displayToPublicDate":"1984-01-01T00:00:00","publicationYear":"1984","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 1984","docAbstract":"There were two major earthquakes (magnitude 7.0-7.9) during this reporting period, the first on March 19 in Uzbek SSR and the second in the Kuril Islands on March 24. Six deaths were reported during the period in Japan and Italy.
\nIn the United States a destructive earthquake occurred in central California on April 24. pennsylvania and several adjoining or nearby States were shaken by a light earthquake on April 23.
","language":"English","publisher":"U.S Geological Survey","usgsCitation":"Person, W., 1984, Earthquakes, March-April 1984: Earthquake Information Bulletin (USGS), v. 16, no. 5, p. 201-204.","productDescription":"4 p.","startPage":"201","endPage":"204","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":318602,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"16","issue":"5","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"56dabfc8e4b015c306f84c54","contributors":{"authors":[{"text":"Person, W. J.","contributorId":91472,"corporation":false,"usgs":true,"family":"Person","given":"W. J.","affiliations":[],"preferred":false,"id":621988,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70168855,"text":"70168855 - 1984 - Earthquakes, January-February 1984","interactions":[],"lastModifiedDate":"2016-03-24T15:59:39","indexId":"70168855","displayToPublicDate":"1984-01-01T00:00:00","publicationYear":"1984","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, January-February 1984","docAbstract":"The first major earthquake (7.0-7.9) of the year struck in teh Solomon Islands in the PacificOcean on February 7, causing damage but no casualties. Deaths were reported in Sulawesi, Afghanistan, Pakistan, and Japan.
\nThere were no significant earthquakes in the United States during this reporting period.
","language":"English","publisher":"U.S Geological Survey","usgsCitation":"Person, W., 1984, Earthquakes, January-February 1984: Earthquake Information Bulletin (USGS), v. 16, no. 5, p. 196-200.","productDescription":"5 p.","startPage":"196","endPage":"200","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":318604,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"16","issue":"5","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"56dabfc5e4b015c306f84c3a","contributors":{"authors":[{"text":"Person, W. J.","contributorId":91472,"corporation":false,"usgs":true,"family":"Person","given":"W. J.","affiliations":[],"preferred":false,"id":621990,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70168851,"text":"70168851 - 1984 - Earthquakes; November-December 1983","interactions":[],"lastModifiedDate":"2016-03-24T15:49:50","indexId":"70168851","displayToPublicDate":"1984-01-01T00:00:00","publicationYear":"1984","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; November-December 1983","docAbstract":"There were four major earthquakes (7.0-7.9) during the last 2 months of the year. The most devastating earthquake, a magnitude 6.4 which killed hundreds of people and injured many, occurred along the northwestern coast of Africa on December 22. Earthquake deaths also were reported in Afghanistan, Belgium, China, and Pakistan.
\nThe strongest earthquake in the United States during this period occurred in Hawaii on November 16 and caused injuries and considerable damage.
","language":"English","publisher":"U.S Geological Survey","usgsCitation":"Person, W., 1984, Earthquakes; November-December 1983: Earthquake Information Bulletin (USGS), v. 16, no. 4, p. 170-175.","productDescription":"6 p.","startPage":"170","endPage":"175","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":318598,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"16","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"56dabfd4e4b015c306f84c69","contributors":{"authors":[{"text":"Person, W. J.","contributorId":91472,"corporation":false,"usgs":true,"family":"Person","given":"W. J.","affiliations":[],"preferred":false,"id":621983,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70168849,"text":"70168849 - 1984 - Earthquakes; September-October 1983","interactions":[],"lastModifiedDate":"2016-03-24T15:47:01","indexId":"70168849","displayToPublicDate":"1984-01-01T00:00:00","publicationYear":"1984","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; September-October 1983","docAbstract":"Two major earthquakes (magntidue 7.0-7.9) occurred during the month of October. The first was on October 4 in northern Chile. the second occurred in the United States in the State of Idaho on October 28. This was the first major earthquake in the conterminous United States since a magnitude 7.2 event occurred near the coast of northern California on November 8, 1980, and was the first earthquake to cause fatalities in the conterminous United States since February 9, 1971. The most deadly earthquake occurred in eastern Turkey on October 30.
","language":"English","publisher":"U.S Geological Survey","usgsCitation":"Person, W., 1984, Earthquakes; September-October 1983: Earthquake Information Bulletin (USGS), v. 16, no. 3, p. 148-151.","productDescription":"4 p.","startPage":"148","endPage":"151","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":318596,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"16","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"56dabfd8e4b015c306f84c77","contributors":{"authors":[{"text":"Person, W. J.","contributorId":91472,"corporation":false,"usgs":true,"family":"Person","given":"W. J.","affiliations":[],"preferred":false,"id":621979,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70168854,"text":"70168854 - 1984 - Earthquakes, July-August 1983","interactions":[],"lastModifiedDate":"2016-03-24T15:57:33","indexId":"70168854","displayToPublicDate":"1984-01-01T00:00:00","publicationYear":"1984","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, July-August 1983","docAbstract":"There were three major earthquakes (7.0-7.9) during this reporting period, but all were in sparsely populated areas. The first occurred on July 11 in the South Shetland Islands, the second in the Aegean Sea on August 6, and the third on August 17 in Kamchatka. Earthquake-related deaths from other quakes were reported from Costa Rica, Iran, Japan, Turkey, the Philippine Islands, and Sicily.
\nIn the United States, aftershocks continued in the Coalinga, California, area; the largest was a magnitude (M) 6.0 on July 21. A magntidue 6.3 earthquake occurred in southern Alaska on July 12.
","language":"English","publisher":"U.S Geological Survey","usgsCitation":"Person, W., 1984, Earthquakes, July-August 1983: Earthquake Information Bulletin (USGS), v. 16, no. 1, p. 34-39.","productDescription":"6 p.","startPage":"34","endPage":"39","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":318603,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"16","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"56dabfc6e4b015c306f84c4a","contributors":{"authors":[{"text":"Person, W. J.","contributorId":91472,"corporation":false,"usgs":true,"family":"Person","given":"W. J.","affiliations":[],"preferred":false,"id":621989,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":1000357,"text":"1000357 - 1984 - Food of young-of-the-year lake trout (Salvelinus namaycush) in Presque Isle Harbor, Lake Superior","interactions":[],"lastModifiedDate":"2016-03-28T15:52:36","indexId":"1000357","displayToPublicDate":"1984-01-01T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2330,"text":"Journal of Great Lakes Research","active":true,"publicationSubtype":{"id":10}},"title":"Food of young-of-the-year lake trout (Salvelinus namaycush) in Presque Isle Harbor, Lake Superior","docAbstract":"The food habits of young lake trout (Salvelinus namaycush) were studied by examining the digestive tracts of 293 young-of-the-year collected in Presque Isle Harbor, Lake Superior. Lake trout in the 25 to 27-mm length range started to eat food organisms before all of their yolk material was absorbed. Organisms consumed by the 25 to 27-mm young-of-the-year included Chironomidae, Copepoda (Harpacticoida, Calanoida, Cyclopoida), and Cladocerea (Daphnia spp., Bosmina sp., Chydorus sp.). Chironomid pupae and chironomid larvae accounted for 74% and 5%, respectively, of the total volume of food eaten by the young lake trout in Presque Isle Harbor. Although copepods, cladocerans, and mysids were present in many stomachs, their contribution to the total volume of food was only 15%. Some lake trout in the 32 to 54-mm length range had consumed fry of sculpin (Cottus spp.) or rainbow smelt (Osmerus mordax), but the overall contribution of fish fry to the total volume of food was only 4% (frequency of occurrence, 10%). The lake trout in Presque Isle Harbor fed heavily on planktonic organisms, sparingly on benthic organisms, and were opportunistic feeders that appeared to prey on whatever forage organisms were available in the shallow nearshore waters.
","language":"English","publisher":"Elsevier","doi":"10.1016/S0380-1330(84)71841-7","usgsCitation":"Swedberg, D.V., and Peck, J.W., 1984, Food of young-of-the-year lake trout (Salvelinus namaycush) in Presque Isle Harbor, Lake Superior: Journal of Great Lakes Research, v. 10, no. 3, p. 280-285, https://doi.org/10.1016/S0380-1330(84)71841-7.","productDescription":"6 p.","startPage":"280","endPage":"285","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":133205,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"10","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b24e4b07f02db6ae67c","contributors":{"authors":[{"text":"Swedberg, Donald V.","contributorId":50115,"corporation":false,"usgs":true,"family":"Swedberg","given":"Donald","email":"","middleInitial":"V.","affiliations":[],"preferred":false,"id":308447,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Peck, James W.","contributorId":78277,"corporation":false,"usgs":true,"family":"Peck","given":"James","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":308448,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70169242,"text":"70169242 - 1984 - Old seismographs still in operation in Northern California","interactions":[],"lastModifiedDate":"2016-03-31T16:55:10","indexId":"70169242","displayToPublicDate":"1984-01-01T00:00:00","publicationYear":"1984","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":"Old seismographs still in operation in Northern California","docAbstract":"Felt earthquakes are frequent on the Cape Mendocino end of the northern San Andreas fault in Humboldt County, California. For this reason a Bosch-Omori seismograph was installed by Horace Winslow of the U.S Coast and Geodetic Survey in teh old city jail in Ferndale as early as 1932. In 1981 the seismograph was moved to the Ferndale Museum where it is monitored now by James Scalvini. Data from the seismograph are sent to the Survey's National Earthquake Information Service in Golden, Colorado.
","language":"English","publisher":"U.S Geological Survey","usgsCitation":"McCormick, E., 1984, Old seismographs still in operation in Northern California: Earthquake Information Bulletin (USGS), v. 16, no. 5, p. 194-195.","productDescription":"2 p.","startPage":"194","endPage":"195","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":319275,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"16","issue":"5","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"56f3be48e4b0f59b85e02ec2","contributors":{"authors":[{"text":"McCormick, E.","contributorId":167746,"corporation":false,"usgs":false,"family":"McCormick","given":"E.","email":"","affiliations":[],"preferred":false,"id":623381,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70197498,"text":"70197498 - 1984 - Paleomagnetic constraints on the interpretation of early Cenozoic Pacific Northwest paleogeography","interactions":[],"lastModifiedDate":"2018-06-07T15:41:27","indexId":"70197498","displayToPublicDate":"1984-01-01T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":5693,"text":"Pacific Section S.E.P.M.","active":true,"publicationSubtype":{"id":10}},"title":"Paleomagnetic constraints on the interpretation of early Cenozoic Pacific Northwest paleogeography","docAbstract":"Widespread Cenozoic clockwise tectonic rotation in the Pacific Northwest is an established fact; however, the geologic reconstructions based on these rotations are the subject of continuing debate. Three basic mechanisms have been proposed to explain the rotations: (1) simple shear rotation of marginal terranes caught in the dextral shear couple between oceanic plates and North America; (2) rotation during oblique microplate collision and accretion to the continental margin; and (3) rotation of continental margin areas during episodes of intracontinental extension. In areas where detailed structure and stratigraphy are available, distributed shear rotations are amplv demonstrated paleomagnetically. However, rotation due to asymmetric interarc extension must be significant, especially for the Oregon Coast Range, in light of recent estimates of large Tertiary extension across the northern Basin and Range. The relative importance of shear versus extension is difficult to determine, but shear could account for nearly onehalf of the observed rotations. Oblique microplate collision has not contributed significantly to the observed Cenozoic rotations because most of the rotation post-dates collision-related deformation in the Oregon and Washington. Coast Range. The resultant continental reconstructions suggest that about 300 km of extension has occurred at 42°N. latitude (southern Oregon border) since early Eocene time. This reconstruction suggests that Cretaceous sedimentary basins east of the Klamath Mountains have undergone significant Tertiary extension (about f<0%) , but little rotation. Upper Cretaceous sedimentary rocks in the Blue Mountains of Oregon near Mitchell are probably rotated at least 15° and perhaps as much as 60°, which allows considerable latitude in the restoration of that part of the basin.
","largerWorkTitle":"Geology of Upper Cretaceous Hornbrook Formation, Oregon and California","language":"English","publisher":"Society for the Sedimentary Geology","usgsCitation":"Wells, R., 1984, Paleomagnetic constraints on the interpretation of early Cenozoic Pacific Northwest paleogeography: Pacific Section S.E.P.M., v. 42, p. 231-237.","productDescription":"7 p.","startPage":"231","endPage":"237","costCenters":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"links":[{"id":354831,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":354830,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://archives.datapages.com/data/pac_sepm/058/058001/pdfs/231.htm"}],"volume":"42","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Wells, Ray E. 0000-0002-7796-0160 rwells@usgs.gov","orcid":"https://orcid.org/0000-0002-7796-0160","contributorId":2692,"corporation":false,"usgs":true,"family":"Wells","given":"Ray E.","email":"rwells@usgs.gov","affiliations":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"preferred":false,"id":737462,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":1000547,"text":"1000547 - 1984 - Catches of larval rainbow smelt (Osmerus mordax) and alewife (Alosa pseudoharengus) in plankton nets of different mesh sizes","interactions":[],"lastModifiedDate":"2013-02-25T14:36:53","indexId":"1000547","displayToPublicDate":"1984-01-01T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2330,"text":"Journal of Great Lakes Research","active":true,"publicationSubtype":{"id":10}},"title":"Catches of larval rainbow smelt (Osmerus mordax) and alewife (Alosa pseudoharengus) in plankton nets of different mesh sizes","docAbstract":"Four 0.5-m plankton nets (one each of 0.355-, 0.450-, 0.560-, and 0.750-mm mesh) were used to collect larvae of the alewife (Alosa pseudoharengus) and rainbow smelt (Osmerus mordax) in northwestern Lake Huron and the St. Marys River. The number of larvae collected varied inversely with mesh size and the average length of larvae varied directly with mesh size. Numbers of each species caught in 0.355- and 0.450-mm mesh nets were significantly greater (P < 0.01) than the numbers caught in 0.560- and 0.750-mm mesh nets. Numbers of alewives caught were significantly greater (P < 0.01) in the 0.355- than in the 0.450-mm mesh, but numbers of rainbow smelt caught in the two meshes were about equal. Between the two larger-mesh nets, numbers of each species caught did not differ significantly. Nets with mesh larger than 0.355 mm were less effective at catching recently hatched larvae, and this reduced effectiveness accounted wholly for the smaller numbers caught in the 0.450-mm mesh net. Smaller numbers were caught in the 0.560- and 0.750-mm mesh nets not only because they caught fewer recently hatched larvae but also because they failed to retain older, larger larvae. Information on the effect of mesh size and towing speed on catches of larvae is important for making accurate estimates of larval densities.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Journal of Great Lakes Research","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Elsevier","publisherLocation":"Amsterdam, Netherlands","doi":"10.1016/S0380-1330(84)71809-0","usgsCitation":"O’Gorman, R., 1984, Catches of larval rainbow smelt (Osmerus mordax) and alewife (Alosa pseudoharengus) in plankton nets of different mesh sizes: Journal of Great Lakes Research, v. 10, no. 1, p. 73-77, https://doi.org/10.1016/S0380-1330(84)71809-0.","productDescription":"5 p.","startPage":"73","endPage":"77","numberOfPages":"5","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":133304,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":268254,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/S0380-1330(84)71809-0"}],"volume":"10","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e2e4b07f02db5e4fcc","contributors":{"authors":[{"text":"O’Gorman, Robert rogorman@usgs.gov","contributorId":3451,"corporation":false,"usgs":true,"family":"O’Gorman","given":"Robert","email":"rogorman@usgs.gov","affiliations":[],"preferred":true,"id":308743,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70169271,"text":"70169271 - 1984 - Likelihood of volcanic eruption at Long Valley, California, is reduced","interactions":[],"lastModifiedDate":"2016-04-07T16:06:20","indexId":"70169271","displayToPublicDate":"1984-01-01T00:00:00","publicationYear":"1984","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":"Likelihood of volcanic eruption at Long Valley, California, is reduced","docAbstract":"A relatively low level of earthquake activity as well as reduced rates of ground deformation over the past year have led U.S Geological Survey scientists to conclude that the likelihood of imminent volcanic activity at Long Valley, California, is reduced from that of mid-1982 through 1983.
","language":"English","publisher":"U.S Geological Survey","usgsCitation":"Kelly, D., 1984, Likelihood of volcanic eruption at Long Valley, California, is reduced: Earthquake Information Bulletin (USGS), v. 16, no. 5, p. 191-192.","productDescription":"2 p.","startPage":"191","endPage":"192","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":319249,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"California","otherGeospatial":"Long Valley","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -118.9215087890625,\n 37.76420119453823\n ],\n [\n -118.73062133789061,\n 37.75008654795525\n ],\n [\n -118.58230590820312,\n 37.63489742852906\n ],\n [\n -118.54248046874999,\n 37.555465068186955\n ],\n [\n -118.6248779296875,\n 37.50318937824072\n ],\n [\n -118.70315551757812,\n 37.55219891098551\n ],\n [\n -118.95996093749999,\n 37.6435971887664\n ],\n [\n -119.05609130859374,\n 37.6631679243197\n ],\n [\n -119.02587890624999,\n 37.73705525336632\n ],\n [\n -119.00390625,\n 37.83473402375478\n ],\n [\n -118.99017333984375,\n 37.89436302930203\n ],\n [\n -118.90365600585939,\n 37.87268533717655\n ],\n [\n -118.92562866210938,\n 37.78482544885859\n ],\n [\n -118.9215087890625,\n 37.76420119453823\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"16","issue":"5","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"56f3be45e4b0f59b85e02ea7","contributors":{"authors":[{"text":"Kelly, D.","contributorId":167760,"corporation":false,"usgs":false,"family":"Kelly","given":"D.","email":"","affiliations":[],"preferred":false,"id":623421,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":2000016,"text":"2000016 - 1984 - Physiology and behavior","interactions":[],"lastModifiedDate":"2023-04-07T14:41:09.699464","indexId":"2000016","displayToPublicDate":"1984-01-01T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":3,"text":"Organization Series"},"seriesTitle":{"id":222,"text":"Technical Report","active":false,"publicationSubtype":{"id":3}},"seriesNumber":"40","title":"Physiology and behavior","docAbstract":"No abstract available.
","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Strategies for rehabilitation of lake trout in the Great Lakes: Proceedings of a conference on lake trout research, August 1983","largerWorkSubtype":{"id":3,"text":"Organization Series"},"language":"English","publisher":"Great Lakes Fishery Commission","usgsCitation":"Foster, N.R., 1984, Physiology and behavior: Technical Report 40, 6 p.","productDescription":"6 p.","startPage":"22","endPage":"27","numberOfPages":"6","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":198537,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":92047,"rank":2,"type":{"id":15,"text":"Index Page"},"url":"https://www.glfc.org/glfc-publications-reports.php","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adae4b07f02db68593d","contributors":{"authors":[{"text":"Foster, Neal R.","contributorId":67451,"corporation":false,"usgs":true,"family":"Foster","given":"Neal","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":324933,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":2001368,"text":"2001368 - 1984 - Enteric redmouth disease of salmonids","interactions":[],"lastModifiedDate":"2012-02-02T00:14:55","indexId":"2001368","displayToPublicDate":"1984-01-01T00:00:00","publicationYear":"1984","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":"67","title":"Enteric redmouth disease of salmonids","docAbstract":"No abstract available at this time","language":"English","publisher":"U.S. Fish and Wildlife Service","collaboration":"549/FH","usgsCitation":"Bullock, G.L., 1984, Enteric redmouth disease of salmonids: Fish Disease Leaflet 67, 14 p.","productDescription":"14 p.","startPage":"0","endPage":"14","numberOfPages":"14","costCenters":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"links":[{"id":198855,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a14e4b07f02db6025f4","contributors":{"authors":[{"text":"Bullock, G. 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