{"pageNumber":"5436","pageRowStart":"135875","pageSize":"25","recordCount":165625,"records":[{"id":70170235,"text":"70170235 - 1976 - The sound of an earthquake","interactions":[],"lastModifiedDate":"2016-04-12T15:36:05","indexId":"70170235","displayToPublicDate":"1976-01-01T00:00:00","publicationYear":"1976","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":"The sound of an earthquake","docAbstract":"<p>Historical accounts of earthquakes often include references to sounds which accompany earthquakes.&nbsp;</p>","language":"English","publisher":"U.S Geological Survey","usgsCitation":"Hill, D., 1976, The sound of an earthquake: Earthquake Information Bulletin (USGS), v. 8, no. 3, p. 15-18.","productDescription":"4 p.","startPage":"15","endPage":"18","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":319998,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"8","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"570e1c38e4b0ef3b7ca24c50","contributors":{"authors":[{"text":"Hill, D.P.","contributorId":27432,"corporation":false,"usgs":true,"family":"Hill","given":"D.P.","email":"","affiliations":[],"preferred":false,"id":626563,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70170233,"text":"70170233 - 1976 - The San Francisco cow; did she or didn’t she?","interactions":[],"lastModifiedDate":"2016-04-12T15:28:01","indexId":"70170233","displayToPublicDate":"1976-01-01T00:00:00","publicationYear":"1976","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":"The San Francisco cow; did she or didn’t she?","docAbstract":"<p>No one has suggested that Mr. Shafter's nameless cow was the cause of the 1906 earthquake, but she has been the source of as persistent a rumor as Mrs. Murphy's Chicago cow. Since 1906, \"the cow that fell in the crack\" has been a favorite subject of humorous speculation. large earthquakes have always produced large exaggerations, and, although it is difficult to exaggerate the terror humans feel in an earthquake, many scientists have said that much of what witnesses said they witnessed they did not witness at all. Huge, gaping cracks that legend says open and close in the earth, swallowing whole cities, are among those earthquake features that just aren't featured in earthquakes. True, soil may \"snap open and shut,\" but most earth scientists do not think that the cracks are wide enough or deep enough to accommodate houses.&nbsp;</p>","language":"English","publisher":"U.S Geological Survey","usgsCitation":"Hill, M., 1976, The San Francisco cow; did she or didn’t she?: Earthquake Information Bulletin (USGS), v. 8, no. 3, p. 19-23.","productDescription":"5 p.","startPage":"19","endPage":"23","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":319995,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"8","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"570e1c37e4b0ef3b7ca24c49","contributors":{"authors":[{"text":"Hill, M.","contributorId":12635,"corporation":false,"usgs":true,"family":"Hill","given":"M.","affiliations":[],"preferred":false,"id":626561,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":1003378,"text":"1003378 - 1976 - Inorganic composition of gallbladder bile from freshwater fishes","interactions":[],"lastModifiedDate":"2023-12-06T22:58:01.211122","indexId":"1003378","displayToPublicDate":"1976-01-01T00:00:00","publicationYear":"1976","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1337,"text":"Copeia","active":true,"publicationSubtype":{"id":10}},"title":"Inorganic composition of gallbladder bile from freshwater fishes","docAbstract":"<p>No abstract available.&nbsp;</p>","language":"English","publisher":"American Society of Ichthyologists and Herpetologists (ASIH)","doi":"10.2307/1443389","usgsCitation":"Hunn, J.B., 1976, Inorganic composition of gallbladder bile from freshwater fishes: Copeia, v. 1976, no. 3, p. 602-605, https://doi.org/10.2307/1443389.","productDescription":"4 p.","startPage":"602","endPage":"605","numberOfPages":"4","costCenters":[{"id":606,"text":"Upper Midwest Environmental Sciences Center","active":true,"usgs":true}],"links":[{"id":130480,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"1976","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ab0e4b07f02db66d95c","contributors":{"authors":[{"text":"Hunn, J. B.","contributorId":15133,"corporation":false,"usgs":true,"family":"Hunn","given":"J.","middleInitial":"B.","affiliations":[],"preferred":false,"id":313204,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70169202,"text":"70169202 - 1976 - Earthquakes June-July 1976","interactions":[],"lastModifiedDate":"2016-03-29T16:48:25","indexId":"70169202","displayToPublicDate":"1976-01-01T00:00:00","publicationYear":"1976","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 June-July 1976","docAbstract":"<p>This was a seismically active period, with one great earthquake, four major earthquakes, and several strong shocks worldwide. Many persons were killed and thousands were injured in three separate events-in West Irian (west New Guinea), in Bali, Indonesia, and in northeastern China.</p>\n<p>A great earthquake (one with a Richter magnitude 8.0 or above) occurred in northeastern China. Major earthquakes (those with Richter magnitudes between 7.0 and 7.9) occurred off the southwest coast of Sumatra, in West Irian (west New Guinea), at the Panama-Colombia border, and in northeastern China.</p>\n<p>In the United States, a number of States were struck by earthquakes, but no significant damage was reported.&nbsp;</p>","language":"English","publisher":"U.S Geological Survey","usgsCitation":"Person, W., 1976, Earthquakes June-July 1976: Earthquake Information Bulletin (USGS), v. 8, no. 6, p. 31-33.","productDescription":"3 p.","startPage":"31","endPage":"33","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":319290,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"8","issue":"6","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"56f3be33e4b0f59b85e02dd7","contributors":{"authors":[{"text":"Person, W. J.","contributorId":91472,"corporation":false,"usgs":true,"family":"Person","given":"W. J.","affiliations":[],"preferred":false,"id":623327,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70162477,"text":"70162477 - 1976 - Earthquake history of Rhode Island","interactions":[],"lastModifiedDate":"2019-11-13T14:18:39","indexId":"70162477","displayToPublicDate":"1976-01-01T00:00:00","publicationYear":"1976","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 history of Rhode Island","docAbstract":"<p>Only three shocks (intensity V or greater, Modified Moercalli Scale) have centered in Rhode Island, although several earthquakes in New England and the St.Lawerence Valley have been felt in the State.</p>","language":"English","publisher":"U.S Geological Survey","usgsCitation":"von Hake, C., 1976, Earthquake history of Rhode Island: Earthquake Information Bulletin (USGS), v. 8, no. 5, p. 31-32.","productDescription":"2 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,{"id":70169246,"text":"70169246 - 1976 - Monitoring Mount Baker Volcano","interactions":[],"lastModifiedDate":"2016-04-05T14:55:29","indexId":"70169246","displayToPublicDate":"1976-01-01T00:00:00","publicationYear":"1976","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 Mount Baker Volcano","docAbstract":"<p>Hisotrically active volcanoes in the conterminous United States are restricted to the Cascade Range and extend to the Cascade Range and extend from Mount Baker near the Canadian border to Lassen Peak in northern California. Since 1800 A.D, most eruptive activity has been on a relatively small scale and has not caused loss of life or significant property damage. However, future &nbsp;volcanism predictably will have more serious effects because of greatly increased use of land near volcanoes during the present century. (See \"Appraising Volcanic Hazards of the Cascade Range of the Northwestern United States,\"&nbsp;<i>Earthquake Inf. Bull.,&nbsp;</i>Sept.-Oct. 1974.) The recognition an impending eruption is highly important in order to minimize the potential hazard to people and property. Thus, a substantial increase in hydrothermal activity at Mount Baker in March 1975 ( see \"Mount Baker Heating Up,\" July-Aug. 1975 issue) was regarded as a possible first signal that an eruption might occur, and an intensive monitoring program was undertaken.&nbsp;</p>","language":"English","publisher":"U.S Geological Survey","usgsCitation":"Malone, S.D., and Frank, D., 1976, Monitoring Mount Baker Volcano: Earthquake Information Bulletin (USGS), v. 8, no. 2, p. 21-25.","productDescription":"5 p.","startPage":"21","endPage":"25","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":319271,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Washington","otherGeospatial":"Mt. Baker","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -121.92489624023436,\n              48.81861991362668\n            ],\n            [\n              -121.69830322265625,\n              48.83308560934761\n            ],\n            [\n              -121.6845703125,\n              48.7127125814524\n            ],\n            [\n              -121.904296875,\n              48.706369163618795\n            ],\n            [\n              -121.92489624023436,\n              48.81861991362668\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"8","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"56f3be46e4b0f59b85e02eae","contributors":{"authors":[{"text":"Malone, S. D.","contributorId":48310,"corporation":false,"usgs":true,"family":"Malone","given":"S.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":623386,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Frank, D.","contributorId":40768,"corporation":false,"usgs":true,"family":"Frank","given":"D.","email":"","affiliations":[],"preferred":false,"id":623387,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70164460,"text":"70164460 - 1976 - A revised “earthquake report” questionnaire","interactions":[],"lastModifiedDate":"2019-06-11T15:14:28","indexId":"70164460","displayToPublicDate":"1976-01-01T00:00:00","publicationYear":"1976","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3372,"text":"Seismological Research Letters","onlineIssn":"1938-2057","printIssn":"0895-0695","active":true,"publicationSubtype":{"id":10}},"title":"A revised “earthquake report” questionnaire","docAbstract":"<p><span>The revised “Earthquake Report” questionnaire introduced here is designed to restrict the replies on the effects of earthquakes as closely as possible to a set of effects that can be evaluated by use of a computer program. Differences in intensity resulting from evaluation by different individuals using their own qualitative procedures can then be eliminated and static rules for evaluating the questionnaire for the assigning of intensity values can be established.</span></p>","language":"English","publisher":"U.S Geological Survey","publisherLocation":"Reston, VA","doi":"10.1785/gssrl.47.1.3","usgsCitation":"Stover, C., Reagor, G., and Simon, R., 1976, A revised “earthquake report” questionnaire: Seismological Research Letters, v. 8, no. 4, p. 18-22, https://doi.org/10.1785/gssrl.47.1.3.","productDescription":"5 p.","startPage":"18","endPage":"22","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":316621,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"8","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"56b5d5bfe4b0cc7999817130","contributors":{"authors":[{"text":"Stover, C.","contributorId":156344,"corporation":false,"usgs":false,"family":"Stover","given":"C.","affiliations":[],"preferred":false,"id":597511,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Reagor, G.","contributorId":60671,"corporation":false,"usgs":true,"family":"Reagor","given":"G.","email":"","affiliations":[],"preferred":false,"id":597512,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Simon, R.","contributorId":45242,"corporation":false,"usgs":true,"family":"Simon","given":"R.","affiliations":[],"preferred":false,"id":597513,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70162475,"text":"70162475 - 1976 - Earthquake history of South Carolina","interactions":[],"lastModifiedDate":"2019-11-13T14:17:14","indexId":"70162475","displayToPublicDate":"1976-01-01T00:00:00","publicationYear":"1976","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 history of South Carolina","docAbstract":"<p>An estimated $23 million damage was caused by one of the great earthquakes in United States history in 1886. Charleston, S.C, and nearby cities suffered most of the damage, although points as far as 160 km away were strongly shaken. Many of the 20 earthquakes of intensity V or greater (Modified Mercalli scale) that centered within South Carolina occurred near Charleston. A 1924 shock in the western part of the State was felt over 145,000 km<sup>2</sup>. Several earthquakes outside the State borders were felt strongly in South Carolina.&nbsp;</p>","language":"English","publisher":"U.S Geological Survey","usgsCitation":"von Hake, C., 1976, Earthquake history of South Carolina: Earthquake Information Bulletin (USGS), v. 8, no. 6, p. 34-38.","productDescription":"5 p.","startPage":"34","endPage":"38","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":314798,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"South 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,{"id":67964,"text":"ha570 - 1976 - Teton Dam flood of June 1976, Menan Buttes quadrangle, Idaho","interactions":[],"lastModifiedDate":"2013-11-12T13:40:21","indexId":"ha570","displayToPublicDate":"1976-01-01T00:00:00","publicationYear":"1976","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":318,"text":"Hydrologic Atlas","code":"HA","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"570","title":"Teton Dam flood of June 1976, Menan Buttes quadrangle, Idaho","docAbstract":"The failure of the Teton Dam caused extreme flooding along the Teton River, Henrys Fork, and Snake River in southeastern Idaho on June 5-8, 1976. No flooding occurred downstream from American Falls Reservoir. The inundated areas and maximum water-surface elevations are shown in a series of 17 hydrologic atlases. The area covered by the atlases extends from Teton Dam downstream to American Falls Reservoir, a distance of 100 miles. The extent of flooding shown on the maps was obtained by field inspections and aerial photographs made during and immediately after the flood. There may be small isolated areas within the boundaries shown that were not flooded, but the identification of these sites was beyond the scope of the study. The elevation data shown are mean-sea-level elevations of high-water marks identified in the field. This particular map (in the 17-map series) shows conditions in the Menan Buttes quadrangle. (Woodard-USGS)","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ha570","usgsCitation":"Thomas, C., Ray, H.A., and Harenberg, W.A., 1976, Teton Dam flood of June 1976, Menan Buttes quadrangle, Idaho: U.S. Geological Survey Hydrologic Atlas 570, 1 Plate: 21.00 x 27.00 inches, https://doi.org/10.3133/ha570.","productDescription":"1 Plate: 21.00 x 27.00 inches","costCenters":[{"id":343,"text":"Idaho Water Science Center","active":true,"usgs":true}],"links":[{"id":185733,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":89193,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/570/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"24000","projection":"Polyconic projection","datum":"1927 North American Datum","country":"United States","state":"Idaho","otherGeospatial":"Menan Buttes Quadrangle","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -112.0,43.75 ], [ -112.0,43.875 ], [ -111.875,43.875 ], [ -111.875,43.75 ], [ -112.0,43.75 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad7e4b07f02db684660","contributors":{"authors":[{"text":"Thomas, Cecil A.","contributorId":107373,"corporation":false,"usgs":true,"family":"Thomas","given":"Cecil A.","affiliations":[],"preferred":false,"id":277410,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ray, Herman A.","contributorId":106199,"corporation":false,"usgs":true,"family":"Ray","given":"Herman","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":277409,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Harenberg, William A.","contributorId":31773,"corporation":false,"usgs":true,"family":"Harenberg","given":"William","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":277408,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70162479,"text":"70162479 - 1976 - Earthquake history of Oregon","interactions":[],"lastModifiedDate":"2019-11-13T14:55:40","indexId":"70162479","displayToPublicDate":"1976-01-01T00:00:00","publicationYear":"1976","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 history of Oregon","docAbstract":"<p>Although situated between two States (California and Washington) that have has many violent earthquakes, Oregon is noticeably less active seismically. the greatest damage experienced resulted from a major shock near Olympia, Wash., in 1949. During the short history record available (since 1841), 34 earthquakes of intensity V, Modified Mercalli Scale, or greater have centered within Oregon or near its borders. Only 13 of the earthquakes had an intensity above V, and many of the shocks were local. However, a 1936 earthquake in the eastern Oregon-Washington region caused extensive damage and was felt over an area of 272,000 square kilometers.&nbsp;</p>","language":"English","publisher":"U.S Geological Survey","usgsCitation":"von Hake, C., 1976, Earthquake history of Oregon: Earthquake Information Bulletin (USGS), v. 8, no. 3, p. 30-33.","productDescription":"4 p.","startPage":"30","endPage":"33","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":314801,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United 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A.","contributorId":7699,"corporation":false,"usgs":true,"family":"von Hake","given":"C. A.","affiliations":[],"preferred":false,"id":589668,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":68056,"text":"ha565 - 1976 - Teton Dam flood of June 1976, Newdale quadrangle, Idaho","interactions":[],"lastModifiedDate":"2013-11-12T13:03:14","indexId":"ha565","displayToPublicDate":"1976-01-01T00:00:00","publicationYear":"1976","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":318,"text":"Hydrologic Atlas","code":"HA","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"565","title":"Teton Dam flood of June 1976, Newdale quadrangle, Idaho","docAbstract":"The failure of the Teton Dam caused extreme flooding along the Teton River, Henrys Fork, and Snake River in southeastern Idaho on June 5-8, 1976. No flooding occurred downstream from American Falls Reservoir. The inundated areas and maximum water-surface elevations are shown in a series of 17 hydrologic atlases. The area covered by the atlases extends from Teton Dam downstream to American Falls Reservoir, a distance of 100 miles. The extent of flooding shown on the maps was obtained by field inspections and aerial photographs made during and immediately after the flood. There may be small isolated areas within the boundaries shown that were not flooded, but the identification of these sites was beyond the scope of the study. The elevation data shown are mean-sea-level elevations of high-water marks identified in the field. This particular map (in the 17-map series) shows conditions in the Newdale quadrangle. (Woodard-USGS)","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ha565","usgsCitation":"Ray, H.A., Matthai, H.F., and Thomas, C., 1976, Teton Dam flood of June 1976, Newdale quadrangle, Idaho: U.S. Geological Survey Hydrologic Atlas 565, 1 Plate: 21.00 x 27.00 inches, https://doi.org/10.3133/ha565.","productDescription":"1 Plate: 21.00 x 27.00 inches","costCenters":[{"id":343,"text":"Idaho Water Science Center","active":true,"usgs":true}],"links":[{"id":186107,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":89319,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/565/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"24000","projection":"Polyconic projection","datum":"1927 North American Datum","country":"United States","state":"Idaho","otherGeospatial":"Newdale Quadrangle","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -111.625,43.875 ], [ -111.625,44.0 ], [ -111.5,44.0 ], [ -111.5,43.875 ], [ -111.625,43.875 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad6e4b07f02db683bfa","contributors":{"authors":[{"text":"Ray, Herman A.","contributorId":106199,"corporation":false,"usgs":true,"family":"Ray","given":"Herman","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":277579,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Matthai, Howard F.","contributorId":106491,"corporation":false,"usgs":true,"family":"Matthai","given":"Howard","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":277580,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Thomas, Cecil A.","contributorId":107373,"corporation":false,"usgs":true,"family":"Thomas","given":"Cecil A.","affiliations":[],"preferred":false,"id":277581,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70171164,"text":"70171164 - 1976 - Energy-related research of the U. S. Fish and Wildlife Service on the Great Lakes","interactions":[],"lastModifiedDate":"2016-05-24T10:52:09","indexId":"70171164","displayToPublicDate":"1976-01-01T00:00:00","publicationYear":"1976","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Energy-related research of the U. S. Fish and Wildlife Service on the Great Lakes","docAbstract":"<p>No abstract available.</p>","largerWorkType":{"id":24,"text":"Conference Paper"},"largerWorkTitle":"Proceedings of the Second Federal Conference on the Great Lakes","largerWorkSubtype":{"id":19,"text":"Conference Paper"},"conferenceTitle":"Second Federal Conference on the Great Lakes","conferenceDate":"March 25-27, 1975","language":"English","publisher":"Argonne National Laboratory","usgsCitation":"Yocom, T.G., and Tait, H.D., 1976, Energy-related research of the U. S. Fish and Wildlife Service on the Great Lakes, <i>in</i> Proceedings of the Second Federal Conference on the Great Lakes, March 25-27, 1975, p. 513-518.","productDescription":"6 p.","startPage":"513","endPage":"518","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":321604,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"574d64f9e4b07e28b6683dc3","contributors":{"authors":[{"text":"Yocom, Thomas G.","contributorId":38095,"corporation":false,"usgs":true,"family":"Yocom","given":"Thomas","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":630146,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Tait, Howard D.","contributorId":33805,"corporation":false,"usgs":true,"family":"Tait","given":"Howard","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":630147,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70171166,"text":"70171166 - 1976 - Ecology of mangroves in the Jewfish Chain, Exuma, Bahamas","interactions":[],"lastModifiedDate":"2016-05-24T11:03:27","indexId":"70171166","displayToPublicDate":"1976-01-01T00:00:00","publicationYear":"1976","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Ecology of mangroves in the Jewfish Chain, Exuma, Bahamas","docAbstract":"<p>The structure and function of mangrove communities in the Jewfish Chain, Exumas, Bahamas, were investigated for 3-1/2 years. Mangrove vegetation in the Jewfish Chain is similar to that in all the Caribbean-Florida area;<span>&nbsp;</span><i>Rhizophora mangle</i><span>&nbsp;</span>L. dominates and is interspersed with<span>&nbsp;</span><i>Avicennia germinans</i><span><i>&nbsp;</i></span>(L.) Lamk. and<span>&nbsp;</span><i>Laguncularia racemosa</i><span>&nbsp;</span>(L.) Gaertn. There is no apparent zonation of these three species. The mangrove communities in the Jewfish Chain occur only where they are protected from prevailing winds, storms, and tides, although all are periodically devastated by hurricanes. We found little or no evidence of coast building within these protected locations. The importance of the mangroves appears to be in providing protection and food for other flora and fauna within this unique ecosystem. Twenty-four species of algae were found in the mangroves, 9 of which had not previously been reported from the Bahamas. Distribution of these algae appears to be correlated to incident solar radiation, desiccation, and tide level. A total of 56 species of fish were found in the mangroves, 2 of which were not previously known from the Bahamas. Many fish taken were juveniles, suggesting that mangroves are a nursery ground for numerous species. Nine species of molluscs were found. Each species had a distinct distribution pattern relative to distance from the seaward edge of the mangroves, as well as a distinct vertical distribution pattern. Seventeen species of decapod crustaceans were recorded. Though several species of birds were noted in the mangroves, three species were most abundant: the white-crowned pigeon (<i>Columba leucocephala</i>) uses the mangrove for nesting but feeds in nearby shrub-thorn communities; the gray kingbird (<i>Tyrannus dominicensis</i>) and green heron (<i>Butorides virescens</i>) nest and feed in the mangroves. Our data do not completely describe a stereotyped mangrove community in the Bahamas, but they do give an indication of community structure and suggest several aspects of function.</p>","largerWorkType":{"id":24,"text":"Conference Paper"},"largerWorkTitle":"Proceedings of the International Symposium on biology and management of mangroves","largerWorkSubtype":{"id":19,"text":"Conference Paper"},"conferenceTitle":"International Symposium on biology and management of mangroves","language":"English","publisher":"University of Florida","usgsCitation":"Wilcox, L.V., Yocom, T.G., and Forbes, A.M., 1976, Ecology of mangroves in the Jewfish Chain, Exuma, Bahamas, <i>in</i> Proceedings of the International Symposium on biology and management of mangroves, p. 305-343.","productDescription":"39 p.","startPage":"305","endPage":"343","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":321607,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"574d64afe4b07e28b6683a7f","contributors":{"authors":[{"text":"Wilcox, L. V.","contributorId":169585,"corporation":false,"usgs":false,"family":"Wilcox","given":"L.","email":"","middleInitial":"V.","affiliations":[],"preferred":false,"id":630149,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Yocom, Thomas G.","contributorId":38095,"corporation":false,"usgs":true,"family":"Yocom","given":"Thomas","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":630150,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Forbes, A. M.","contributorId":169586,"corporation":false,"usgs":false,"family":"Forbes","given":"A.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":630151,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":1013699,"text":"1013699 - 1976 - Optimum level of dietary biotin for growth, feed utilization, and swimming stamina of fingerling lake trout (Salvelinus namaycush)","interactions":[],"lastModifiedDate":"2025-03-03T16:46:15.992803","indexId":"1013699","displayToPublicDate":"1976-01-01T00:00:00","publicationYear":"1976","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2543,"text":"Journal of the Fisheries Research Board of Canada","active":true,"publicationSubtype":{"id":10}},"title":"Optimum level of dietary biotin for growth, feed utilization, and swimming stamina of fingerling lake trout (Salvelinus namaycush)","docAbstract":"<p><span>Triplicate lots of fingerling lake trout (</span><i>Salvelinus namaycush</i><span>) held at 9 C for 20 wk were fed a semipurified basal diet supplemented with 1% spray-dried egg white or d-biotin at concentrations of 0.1, 0.5, 1.0, or 5.0 ppm. Trout fed the basal diet, either alone or with egg white, grew more slowly and converted feed less efficiently (</span><i>P</i><span> &lt; 0.05) than those fed supplemental biotin. Neither the growth rate nor feed conversion differed significantly among the four groups fed supplemental biotin. However, when forced to swim to exhaustion against controlled water currents, trout fed either basal diet, with or without egg white, or 0.1 ppm supplemental biotin, swam a shorter distance (</span><i>P</i><span> &lt; 0.05) than those fed more biotin. Fish fed 0.5 ppm biotin swam as far as those fed 1.0 ppm, but not as far as those fed 5.0 ppm. These results indicate that young lake trout probably need no more than 0.1 ppm biotin for optimum growth and feed conversion, but require from 0.5 to 1.0 ppm for optimum swimming stamina.</span></p>","language":"English","publisher":"Canadian Science Publishing","doi":"10.1139/f76-230","usgsCitation":"Poston, H.A., 1976, Optimum level of dietary biotin for growth, feed utilization, and swimming stamina of fingerling lake trout (Salvelinus namaycush): Journal of the Fisheries Research Board of Canada, v. 33, no. 8, p. 1803-1806, https://doi.org/10.1139/f76-230.","productDescription":"4 p.","startPage":"1803","endPage":"1806","numberOfPages":"4","costCenters":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"links":[{"id":129346,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"33","issue":"8","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aefe4b07f02db6913a6","contributors":{"authors":[{"text":"Poston, H. A.","contributorId":21893,"corporation":false,"usgs":true,"family":"Poston","given":"H.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":319076,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70010999,"text":"70010999 - 1976 - Interactive computer programs for petrologic modeling with extended Q-mode factor analysis","interactions":[],"lastModifiedDate":"2013-01-21T16:12:50","indexId":"70010999","displayToPublicDate":"1976-01-01T00:00:00","publicationYear":"1976","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1315,"text":"Computers & Geosciences","printIssn":"0098-3004","active":true,"publicationSubtype":{"id":10}},"title":"Interactive computer programs for petrologic modeling with extended Q-mode factor analysis","docAbstract":"An extended form of Q-mode factor analysis may be used if the row-sums of the data matrix are constant and can be helpful especially in developing and testing petrologic-mixing models for igneous systems. The first step is to represent the sample compositions as unit vectors in M-dimensional space and then to project them into space of fewer dimensions (m) as determined to be appropriate from a factor-variance diagram. Compositions thought to be those of possible end-members in the petrologic system then are represented as vectors in the M-dimensional space and projected into the same space as the sample vectors. If these vectors remain close to unity in length after projection, the corresponding compositions can serve as end-member compositions for the model. After m suitable end-member compositions have been identified, each sample composition is expressed as a mixture of the end-members by computation of the composition loadings. The interactive computer programs presented are useful in these procedures because of the trial-and-error nature of the modeling procedures. ?? 1976.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Computers and Geosciences","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Elsevier","publisherLocation":"Amsterdam, Netherlands","doi":"10.1016/0098-3004(76)90039-X","issn":"00983004","usgsCitation":"Miesch, A., 1976, Interactive computer programs for petrologic modeling with extended Q-mode factor analysis: Computers & Geosciences, v. 2, no. 4, p. 439-492, https://doi.org/10.1016/0098-3004(76)90039-X.","startPage":"439","endPage":"492","numberOfPages":"54","costCenters":[],"links":[{"id":221561,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":266212,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/0098-3004(76)90039-X"}],"volume":"2","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a3cd5e4b0c8380cd630a6","contributors":{"authors":[{"text":"Miesch, A.T.","contributorId":88726,"corporation":false,"usgs":true,"family":"Miesch","given":"A.T.","affiliations":[],"preferred":false,"id":360059,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70010265,"text":"70010265 - 1976 - Foraminiferal biostratigraphy of the shelf edge: a key to late Quaternary paleoenvironments","interactions":[],"lastModifiedDate":"2013-02-19T16:19:21","indexId":"70010265","displayToPublicDate":"1976-01-01T00:00:00","publicationYear":"1976","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2996,"text":"Palaeogeography, Palaeoclimatology, Palaeoecology","printIssn":"0031-0182","active":true,"publicationSubtype":{"id":10}},"title":"Foraminiferal biostratigraphy of the shelf edge: a key to late Quaternary paleoenvironments","docAbstract":"Foraminiferal assemblages in eight piston cores from West Flower Garden Bank at the edge of the Texas continental shelf contain a nearly complete record of late Quaternary paleoclimatic and geologic events. The faunas are divisible into three distinct successive biofacies on the basis of both planktonic and benthic foraminifers: the basal Inflata Facies accumulated in cool shallow waters during late Pleistocene glaciation; the middle Crassaformis Facies represents a deepening sea that had warming surface waters; the upper Cultrata Facies is characteristic of the Holocene outer-shelf environment. Sea level was at -73 m and -53 m at the end of deposition of the Inflata and Crassaformis Facies, respectively. The biostratigraphic events at West Flower Garden Bank can be accurately correlated with those recorded in the middle and inner shelf and in deep-sea cores. The sequence of late Quaternary sea level and paleotemperature changes in the northern Gulf of Mexico can thereby be reconstructed. Eventually, this knowledge can be integrated with similar data from the shelf edge in other parts of the world to help bridge the gap between the known Quaternary record of the deep sea and that of the continents. ?? 1976.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Palaeogeography, Palaeoclimatology, Palaeoecology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Elsevier","doi":"10.1016/0031-0182(76)90040-7","issn":"00310182","usgsCitation":"Poag, C.W., and Sidner, B., 1976, Foraminiferal biostratigraphy of the shelf edge: a key to late Quaternary paleoenvironments: Palaeogeography, Palaeoclimatology, Palaeoecology, v. 19, no. 1, p. 17-37, https://doi.org/10.1016/0031-0182(76)90040-7.","startPage":"17","endPage":"37","numberOfPages":"21","costCenters":[],"links":[{"id":267788,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/0031-0182(76)90040-7"},{"id":218711,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"19","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a1309e4b0c8380cd544c2","contributors":{"authors":[{"text":"Poag, C. Wylie","contributorId":52714,"corporation":false,"usgs":true,"family":"Poag","given":"C.","email":"","middleInitial":"Wylie","affiliations":[],"preferred":false,"id":358478,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Sidner, B.R.","contributorId":57590,"corporation":false,"usgs":true,"family":"Sidner","given":"B.R.","email":"","affiliations":[],"preferred":false,"id":358479,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70010373,"text":"70010373 - 1976 - Resource data bases-Resource assessment","interactions":[],"lastModifiedDate":"2013-01-21T16:10:14","indexId":"70010373","displayToPublicDate":"1976-01-01T00:00:00","publicationYear":"1976","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1315,"text":"Computers & Geosciences","printIssn":"0098-3004","active":true,"publicationSubtype":{"id":10}},"title":"Resource data bases-Resource assessment","docAbstract":"The U.S. Geological Survey's Office of Resource Analysis is developing computer methods for the handling of mineral-resources data in order to provide improved means for addressing and manipulating data. These methods include: computerized data files and predictive resource models. Data files contain the raw or disaggregated information on mineral deposits and commodities. One operational data file is CRIB (Computerized Resources Information Bank) which is a general purpose inventory and reference file on metallic and nonmetallic mineral deposits. A computer file on resources should contain detailed information on the following main categories: record identification, name and location, description of deposit, analytical data, and production/reserves. A resource model employs postulates and inferences in conjunction with the data to make predictions about resources-as key variables concerning a mineral commodity are changed. The objective is to estimate the availability of minerals including: geological availability (occurrence models), technological availability (exploration and beneficiation models), and economic availability (economics models). ?? 1976.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Computers and Geosciences","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Elsevier","publisherLocation":"Amsterdam, Netherlands","doi":"10.1016/0098-3004(76)90057-1","issn":"00983004","usgsCitation":"Clark, A.L., 1976, Resource data bases-Resource assessment: Computers & Geosciences, v. 2, no. 3, p. 309-311, https://doi.org/10.1016/0098-3004(76)90057-1.","startPage":"309","endPage":"311","numberOfPages":"3","costCenters":[],"links":[{"id":219757,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":266210,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/0098-3004(76)90057-1"}],"volume":"2","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505aa9f0e4b0c8380cd8606a","contributors":{"authors":[{"text":"Clark, A. L.","contributorId":89502,"corporation":false,"usgs":true,"family":"Clark","given":"A.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":358765,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70010253,"text":"70010253 - 1976 - A note on the effect of fault gouge thickness on fault stability","interactions":[],"lastModifiedDate":"2013-01-18T13:31:41","indexId":"70010253","displayToPublicDate":"1976-01-01T00:00:00","publicationYear":"1976","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2071,"text":"International Journal of Rock Mechanics and Mining Sciences & Geomechanics Abstracts","active":true,"publicationSubtype":{"id":10}},"title":"A note on the effect of fault gouge thickness on fault stability","docAbstract":"At low confining pressure, sliding on saw cuts in granite is stable but at high pressure it is unstable. The pressure at which the transition takes place increases if the thickness of the crushed material between the sliding surfaces is increased. This experimental result suggests that on natural faults the stability of sliding may be affected by the width of the fault zone. ?? 1976.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"International Journal of Rock Mechanics and Mining Sciences & Geomechanics Abstracts","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Elsevier","doi":"10.1016/0148-9062(76)90226-6","issn":"01489062","usgsCitation":"Byerlee, J., and Summers, R., 1976, A note on the effect of fault gouge thickness on fault stability: International Journal of Rock Mechanics and Mining Sciences & Geomechanics Abstracts, v. 13, no. 1, p. 35-36, https://doi.org/10.1016/0148-9062(76)90226-6.","productDescription":"p.35-36","startPage":"35","endPage":"36","numberOfPages":"2","costCenters":[],"links":[{"id":265952,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/0148-9062(76)90226-6"},{"id":219675,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"13","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059e4c3e4b0c8380cd468ee","contributors":{"authors":[{"text":"Byerlee, J.","contributorId":105838,"corporation":false,"usgs":true,"family":"Byerlee","given":"J.","affiliations":[],"preferred":false,"id":358459,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Summers, R.","contributorId":65483,"corporation":false,"usgs":true,"family":"Summers","given":"R.","email":"","affiliations":[],"preferred":false,"id":358458,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70010374,"text":"70010374 - 1976 - Zoned Cr, Fe-spinel from the La Perouse layered gabbro, Fairweather Range, Alaska","interactions":[],"lastModifiedDate":"2023-12-14T12:23:42.851362","indexId":"70010374","displayToPublicDate":"1976-01-01T00:00:00","publicationYear":"1976","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":"Zoned Cr, Fe-spinel from the La Perouse layered gabbro, Fairweather Range, Alaska","docAbstract":"<div id=\"abstracts\" class=\"Abstracts u-font-serif text-s\"><div id=\"ab1\" class=\"abstract author\" lang=\"en\"><div id=\"aep-abstract-sec-id7\"><div id=\"abstracts\" class=\"Abstracts u-font-serif text-s\"><div id=\"ab1\" class=\"abstract author\" lang=\"en\"><div id=\"aep-abstract-sec-id7\"><p>Zoned spinel of unusual composition and morphology has been found in massive pyrrhotite-chalcopyrite-pent-landite ore from the La Perouse layered gabbro intrusion in the Fairweather Range, southeastern Alaska. The spinel grains show continuous zoning from cores with up to 53 wt.% Cr<sub>2</sub>O<sub>3</sub>&nbsp;to rims with less than 11 wt.% Cr<sub>2</sub>O<sub>3</sub>. Their composition is exceptional because they contain less than 0.32 wt.% MgO and less than 0.10 wt.% Al<sub>2</sub>O<sub>3</sub>&nbsp;and TiO<sub>2</sub>. Also notable are the concentrations of MnO and V<sub>2</sub>O<sub>3</sub>, which reach 4.73 and 4.50 wt.%, respectively, in the cores. The spinel is thought to have crystallized at low oxygen fugacity and at temperatures above 900°C, directly from a sulfide melt that separated by immiscibility from the gabbroic parental magma.<br></p></div></div></div></div></div></div><ul id=\"issue-navigation\" class=\"issue-navigation u-margin-s-bottom u-bg-grey1\"></ul>","language":"English","publisher":"Elsevier","doi":"10.1016/0012-821X(76)90163-1","issn":"0012821X","usgsCitation":"Czamanske, G., Himmelberg, G.R., and Goff, F., 1976, Zoned Cr, Fe-spinel from the La Perouse layered gabbro, Fairweather Range, Alaska: Earth and Planetary Science Letters, v. 33, no. 1, p. 111-118, https://doi.org/10.1016/0012-821X(76)90163-1.","productDescription":"8 p.","startPage":"111","endPage":"118","numberOfPages":"8","costCenters":[],"links":[{"id":218643,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"33","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bd294e4b08c986b32f8cb","contributors":{"authors":[{"text":"Czamanske, G.K.","contributorId":26300,"corporation":false,"usgs":true,"family":"Czamanske","given":"G.K.","email":"","affiliations":[],"preferred":false,"id":358766,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Himmelberg, G. R.","contributorId":27106,"corporation":false,"usgs":true,"family":"Himmelberg","given":"G.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":358768,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Goff, F.E.","contributorId":26808,"corporation":false,"usgs":true,"family":"Goff","given":"F.E.","email":"","affiliations":[],"preferred":false,"id":358767,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70011167,"text":"70011167 - 1976 - Intrinsic germanium detector used in borehole sonde for uranium exploration","interactions":[],"lastModifiedDate":"2019-11-19T07:19:24","indexId":"70011167","displayToPublicDate":"1976-01-01T00:00:00","publicationYear":"1976","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2906,"text":"Nuclear Instruments and Methods","active":true,"publicationSubtype":{"id":10}},"title":"Intrinsic germanium detector used in borehole sonde for uranium exploration","docAbstract":"A borehole sonde (~1.7 m long; 7.3 cm diameter) using a 200 mm<sup>2</sup> planar intrinsic germanium detector, mounted in a cryostat cooled by removable canisters of frozen propane, has been constructed and tested. The sonde is especially useful in measuring X- and low-energy gamma-ray spectra (40–400 keV). Laboratory tests in an artificial borehole facility indicate its potential for in-situ uranium analyses in boreholes irrespective of the state of equilibrium in the uranium series. Both natural gamma-ray and neutron-activation gamma-ray spectra have been measured with the sonde. Although the neutron-activation technique yields greater sensitivity, improvements being made in the resolution and efficiency of intrinsic germanium detectors suggest that it will soon be possible to use a similar sonde in the passive mode for measurement of uranium in a borehole down to about 0.1% with acceptable accuracy. Using a similar detector and neutron activation, the sonde can be used to measure uranium down to 0.01%.","language":"English","publisher":"Elsevier","doi":"10.1016/0029-554X(76)90047-1","issn":"0029554X","usgsCitation":"Senftle, F.E., Moxham, R., Tanner, A., Boynton, G.R., Philbin, P.W., and Baicker, J., 1976, Intrinsic germanium detector used in borehole sonde for uranium exploration: Nuclear Instruments and Methods, v. 138, no. 2, p. 371-380, https://doi.org/10.1016/0029-554X(76)90047-1.","productDescription":"10 p.","startPage":"371","endPage":"380","costCenters":[{"id":387,"text":"Mineral Resources Program","active":true,"usgs":true}],"links":[{"id":265735,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/0029-554X(76)90047-1"},{"id":221093,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"138","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a3dcfe4b0c8380cd6387a","contributors":{"authors":[{"text":"Senftle, F. E.","contributorId":47788,"corporation":false,"usgs":true,"family":"Senftle","given":"F.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":360443,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Moxham, R.M.","contributorId":42234,"corporation":false,"usgs":true,"family":"Moxham","given":"R.M.","email":"","affiliations":[],"preferred":false,"id":360441,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Tanner, A.B.","contributorId":44155,"corporation":false,"usgs":true,"family":"Tanner","given":"A.B.","email":"","affiliations":[],"preferred":false,"id":360442,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Boynton, G. R.","contributorId":82276,"corporation":false,"usgs":true,"family":"Boynton","given":"G.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":360444,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Philbin, P. W.","contributorId":25915,"corporation":false,"usgs":true,"family":"Philbin","given":"P.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":360440,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Baicker, J.A.","contributorId":8870,"corporation":false,"usgs":true,"family":"Baicker","given":"J.A.","email":"","affiliations":[],"preferred":false,"id":360439,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":70011168,"text":"70011168 - 1976 - Identification of excess 40Ar by the  40Ar 39Ar, age spectrum technique","interactions":[],"lastModifiedDate":"2021-05-11T12:55:00.459317","indexId":"70011168","displayToPublicDate":"1976-01-01T00:00:00","publicationYear":"1976","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":"Identification of excess 40Ar by the  40Ar 39Ar, age spectrum technique","docAbstract":"<div id=\"abstracts\" class=\"Abstracts u-font-serif\"><div id=\"ab1\" class=\"abstract author\" lang=\"en\"><div id=\"aep-abstract-sec-id4\"><p><sup>40</sup>Ar/<sup>39</sup>Ar incremental heating experiments on igneous plagioclase, biotite, and pyroxene that contain known amounts of excess<sup>40</sup>Ar indicate that saddle-shaped age spectra are diagnostic of excess<sup>40</sup>Ar in igneous minerals as well as in igneous rocks. The minima in the age spectra approach but do not reach the crystallization age. Neither the age spectrum diagram nor the<sup>40</sup>Ar/<sup>36</sup>Ar versus<sup>39</sup>Ar/<sup>36</sup>Ar isochron diagram reliably reveal the crystallization age in such samples.</p></div></div></div><ul id=\"issue-navigation\" class=\"issue-navigation u-margin-s-bottom u-bg-grey1\"></ul>","language":"English","publisher":"Elsevier","doi":"10.1016/0012-821X(76)90052-2","issn":"0012821X","usgsCitation":"Lanphere, M.A., and Dalrymple, G.B., 1976, Identification of excess 40Ar by the  40Ar 39Ar, age spectrum technique: Earth and Planetary Science Letters, v. 32, no. 2, p. 141-148, https://doi.org/10.1016/0012-821X(76)90052-2.","productDescription":"8 p.","startPage":"141","endPage":"148","numberOfPages":"8","costCenters":[],"links":[{"id":221094,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"32","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a3827e4b0c8380cd61474","contributors":{"authors":[{"text":"Lanphere, M. A.","contributorId":35298,"corporation":false,"usgs":true,"family":"Lanphere","given":"M.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":360445,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Dalrymple, G. Brent","contributorId":55146,"corporation":false,"usgs":true,"family":"Dalrymple","given":"G.","email":"","middleInitial":"Brent","affiliations":[],"preferred":false,"id":360446,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70011176,"text":"70011176 - 1976 - Mixing of carbonate waters","interactions":[],"lastModifiedDate":"2021-05-11T12:37:48.498321","indexId":"70011176","displayToPublicDate":"1976-01-01T00:00:00","publicationYear":"1976","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":"Mixing of carbonate waters","docAbstract":"<div id=\"abstracts\" class=\"Abstracts u-font-serif\"><div id=\"aep-abstract-id5\" class=\"abstract author\"><div id=\"aep-abstract-sec-id6\"><p>When mineral solutions of different compositions are mixed, the molalities and activities of individual ions in the mixture are often non-linear functions of their end-member values. This non-linearity is particularly significant in determining mineral saturation levels. Mixtures of saturated solutions may be either undersaturated or supersaturated depending on the end-member compositions and the physical conditions in which end-members and their mixtures exist. In carbonate solutions important non-linear effects occur due to redistribution of carbonate species. In extreme cases this causes mixture pH to be below both the end-member pH values. A simple but precise computer program (WATMIX) has been developed for calculating mixture composition for closed and open system mixing of arbitrary end-members. A number of mixing examples are considered which allow one to isolate three important processes leading to non-linear behaviour: the algebraic effect, the<span>&nbsp;</span><i>δP</i><sub><i>CO</i>2</sub><span>&nbsp;</span>effect, and the ionic strength effect.</p></div></div></div>","language":"English","publisher":"Elsevier","doi":"10.1016/0016-7037(76)90041-7","issn":"00167037","usgsCitation":"Wigley, T., and Plummer, N., 1976, Mixing of carbonate waters: Geochimica et Cosmochimica Acta, v. 40, no. 9, p. 989-995, https://doi.org/10.1016/0016-7037(76)90041-7.","productDescription":"7 p.","startPage":"989","endPage":"995","numberOfPages":"7","costCenters":[],"links":[{"id":221220,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"40","issue":"9","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a5b87e4b0c8380cd6f601","contributors":{"authors":[{"text":"Wigley, T.M.L.","contributorId":56788,"corporation":false,"usgs":true,"family":"Wigley","given":"T.M.L.","email":"","affiliations":[],"preferred":false,"id":360459,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Plummer, Niel 0000-0002-4020-1013 nplummer@usgs.gov","orcid":"https://orcid.org/0000-0002-4020-1013","contributorId":190100,"corporation":false,"usgs":true,"family":"Plummer","given":"Niel","email":"nplummer@usgs.gov","affiliations":[{"id":436,"text":"National Research Program - Eastern Branch","active":true,"usgs":true}],"preferred":true,"id":360460,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70011177,"text":"70011177 - 1976 - Tectonic implications of space-time patterns of Cenozoic magmatism in the western United States","interactions":[],"lastModifiedDate":"2021-05-11T12:33:28.427668","indexId":"70011177","displayToPublicDate":"1976-01-01T00:00:00","publicationYear":"1976","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":"Tectonic implications of space-time patterns of Cenozoic magmatism in the western United States","docAbstract":"<p>Locations of 2,100 radiometrically dated igneous rocks were plotted on a series of 20 maps, each representing an interval within the period 80 m.y. B.P. to present. Derivative maps showing the distributions in space and time of dated granitic intrusive rocks, silicic lavas and domes, ash-flow tuffs, andesitic-dacitic rocks, and basalts depict well the two main petrogenetic assemblages noted previously by others: (1) mainly intermediate andesitic-dacitic suites, including associated granitic intrusive rocks, silicic extrusive rocks, and minor basaltic lavas, are interpreted as reflecting plate interactions related to subduction along the continental margin; and (2) bimodal suites, dominantly basaltic but with minor silicic extrusive rocks, are interpreted as reflecting extensional tectonics.</p><p>Space-time distribution of the two assemblages suggests that magmatic arcs extended continously parallel to the continental margin from Canada to Mexico in latest Mesozoic and in Oligocene times. An early Cenozoic null in magmatism in the Great Basin may delineate the region where subduction was arrested temporarily by development of the proto-San Andreas fault as a transform in coastal California or, alternatively, may reflect complex subsurface configurations of subducted plates. The late Cenozoic transition from subduction-related magmatism to extention-related basaltic volcanism in the southern Cordillera occurred at different times in different areas in harmony with current concepts about the migration of the Mendocino triple junction as the modern San Andreas transform fault was formed. The plots also reveal the existence of several discrete magmatic loci where igneous activity of various kinds was characteristically more intense and long-lived than elsewhere.</p>","language":"English","publisher":"Elsevier","doi":"10.1016/0012-821X(76)90189-8","issn":"0012821X","usgsCitation":"Snyder, W., Dickinson, W., and Silberman, M., 1976, Tectonic implications of space-time patterns of Cenozoic magmatism in the western United States: Earth and Planetary Science Letters, v. 32, no. 1, p. 91-106, https://doi.org/10.1016/0012-821X(76)90189-8.","productDescription":"16 p.","startPage":"91","endPage":"106","numberOfPages":"16","costCenters":[],"links":[{"id":221221,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -126.474609375,\n              28.69058765425071\n            ],\n            [\n              -102.216796875,\n              28.69058765425071\n            ],\n            [\n              -102.216796875,\n              50.064191736659104\n            ],\n            [\n              -126.474609375,\n              50.064191736659104\n            ],\n            [\n              -126.474609375,\n              28.69058765425071\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"32","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505ba468e4b08c986b3202ff","contributors":{"authors":[{"text":"Snyder, W.S.","contributorId":107428,"corporation":false,"usgs":true,"family":"Snyder","given":"W.S.","email":"","affiliations":[],"preferred":false,"id":360463,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Dickinson, W.R.","contributorId":64801,"corporation":false,"usgs":true,"family":"Dickinson","given":"W.R.","email":"","affiliations":[],"preferred":false,"id":360462,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Silberman, M.L.","contributorId":10013,"corporation":false,"usgs":true,"family":"Silberman","given":"M.L.","affiliations":[],"preferred":false,"id":360461,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70011024,"text":"70011024 - 1976 - Observations of eruption clouds from Sakura-zima volcano, Kyushu, Japan from Skylab 4","interactions":[],"lastModifiedDate":"2012-03-12T17:19:05","indexId":"70011024","displayToPublicDate":"1976-01-01T00:00:00","publicationYear":"1976","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":"Observations of eruption clouds from Sakura-zima volcano, Kyushu, Japan from Skylab 4","docAbstract":"Hasselblad and Nikon stereographic photographs taken from Skylab between 9 June 1973 and 1 February 1974 give synoptic plan views of several entire eruption clouds emanating from Sakura-zima volcano in Kagoshima Bay, Kyushu, Japan. Analytical plots of these stereographic pairs, studied in combination with meteorological data, indicate that the eruption clouds did not penetrate the tropopause and thus did not create a stratospheric dust veil of long residence time. A horizontal eddy diffusivity of the order of 106 cm2 s-1 and a vertical eddy diffusivity of the order of 105 cm2 s-1 were calculated from the observed plume dimensions and from available meteorological data. These observations are the first, direct evidence that explosive eruption at an estimated energy level of about 1018 ergs per paroxysm may be too small under atmospheric conditions similar to those prevailing over Sakura-zima for volcanic effluents to penetrate low-level tropospheric temperature inversions and, consequently, the tropopause over northern middle latitudes. Maximum elevation of the volcanic clouds was determined to be 3.4 km. The cumulative thermal energy release in the rise of volcanic plumes for 385 observed explosive eruptions was estimated to be 1020 to 1021 ergs (1013 to 1014 J), but the entire thermal energy release associated with pyroclastic activity may be of the order of 2.5 ?? 1022 ergs (2.5 ?? 1015 J). Estimation of the kinetic energy component of explosive eruptions via satellite observation and meteorological consideration of eruption clouds is thus useful in volcanology as an alternative technique to confirm the kinetic energy estimates made by ground-based geological and geophysical methods, and to aid in construction of physical models of potential and historical tephra-fallout sectors with implications for volcano-hazard prediction. ?? 1976.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Journal of Volcanology and Geothermal Research","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","issn":"03770273","usgsCitation":"Friedman, J.D., Heiken, G., Randerson, D., and McKay, D., 1976, Observations of eruption clouds from Sakura-zima volcano, Kyushu, Japan from Skylab 4: Journal of Volcanology and Geothermal Research, v. 1, no. 4, p. 305-329.","startPage":"305","endPage":"329","numberOfPages":"25","costCenters":[],"links":[{"id":221790,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"1","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a6a91e4b0c8380cd74242","contributors":{"authors":[{"text":"Friedman, J. D.","contributorId":99157,"corporation":false,"usgs":true,"family":"Friedman","given":"J.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":360106,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Heiken, G.","contributorId":11768,"corporation":false,"usgs":true,"family":"Heiken","given":"G.","email":"","affiliations":[],"preferred":false,"id":360104,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Randerson, D.","contributorId":94162,"corporation":false,"usgs":true,"family":"Randerson","given":"D.","email":"","affiliations":[],"preferred":false,"id":360105,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"McKay, D.S.","contributorId":11329,"corporation":false,"usgs":true,"family":"McKay","given":"D.S.","email":"","affiliations":[],"preferred":false,"id":360103,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":2001152,"text":"2001152 - 1976 - Toxicity of rotenone to fish in standardized laboratory tests","interactions":[],"lastModifiedDate":"2012-02-02T00:14:54","indexId":"2001152","displayToPublicDate":"1976-01-01T00:00:00","publicationYear":"1976","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":39,"text":"Investigations in Fish Control","active":false,"publicationSubtype":{"id":1}},"seriesNumber":"72","title":"Toxicity of rotenone to fish in standardized laboratory tests","docAbstract":"Abstract not submitted to date","language":"English","publisher":"U.S. Fish and Wildlife Service","publisherLocation":"La Crosse, WI","usgsCitation":"Marking, L.L., and Bills, T., 1976, Toxicity of rotenone to fish in standardized laboratory tests: Investigations in Fish Control 72, 11.","productDescription":"11","startPage":"0","endPage":"11","numberOfPages":"11","costCenters":[{"id":606,"text":"Upper Midwest Environmental Sciences Center","active":true,"usgs":true}],"links":[{"id":199182,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4ee4b07f02db627fa2","contributors":{"authors":[{"text":"Marking, L. L.","contributorId":90661,"corporation":false,"usgs":true,"family":"Marking","given":"L.","middleInitial":"L.","affiliations":[],"preferred":false,"id":325477,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bills, T.D.","contributorId":6393,"corporation":false,"usgs":true,"family":"Bills","given":"T.D.","email":"","affiliations":[],"preferred":false,"id":325476,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
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