{"pageNumber":"5739","pageRowStart":"143450","pageSize":"25","recordCount":184651,"records":[{"id":85372,"text":"85372 - 1979 - Lake Pepin Region, Pepin County","interactions":[],"lastModifiedDate":"2012-02-02T00:04:02","indexId":"85372","displayToPublicDate":"1979-01-01T00:00:00","publicationYear":"1979","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"title":"Lake Pepin Region, Pepin County","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Wisconsin's favorite bird haunts","largerWorkSubtype":{"id":4,"text":"Other Government Series"},"language":"English","publisher":"Wisconsin Society of Ornithology","publisherLocation":"Madison, WI","usgsCitation":"Faanes, C., 1979, Lake Pepin Region, Pepin County, chap. <i>of</i> Wisconsin's favorite bird haunts, p. 335-337 [424 pp.].","productDescription":"p. 335-337 [424 pp.]","costCenters":[{"id":480,"text":"Northern Prairie Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":127769,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b32e4b07f02db6b429f","contributors":{"editors":[{"text":"Tessen, D.D.","contributorId":112547,"corporation":false,"usgs":true,"family":"Tessen","given":"D.D.","email":"","affiliations":[],"preferred":false,"id":504445,"contributorType":{"id":2,"text":"Editors"},"rank":1}],"authors":[{"text":"Faanes, C.","contributorId":37676,"corporation":false,"usgs":true,"family":"Faanes","given":"C.","affiliations":[],"preferred":false,"id":295965,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":85601,"text":"85601 - 1979 - The role of stress in fish disease","interactions":[],"lastModifiedDate":"2012-02-02T00:15:13","indexId":"85601","displayToPublicDate":"1979-01-01T00:00:00","publicationYear":"1979","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"title":"The role of stress in fish disease","docAbstract":"Abstract not submitted to date","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Principal diseases of farm-raised catfish","largerWorkSubtype":{"id":4,"text":"Other Government Series"},"language":"English","publisher":"Auburn University","publisherLocation":"Auburn, AL","usgsCitation":"Meyer, F.P., 1979, The role of stress in fish disease, chap. <i>of</i> Principal diseases of farm-raised catfish, 7-9.","productDescription":"7-9","costCenters":[{"id":606,"text":"Upper Midwest Environmental Sciences Center","active":true,"usgs":true}],"links":[{"id":195884,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b24e4b07f02db6ae677","contributors":{"editors":[{"text":"Plumb, J.A.","contributorId":38106,"corporation":false,"usgs":true,"family":"Plumb","given":"J.A.","email":"","affiliations":[],"preferred":false,"id":504545,"contributorType":{"id":2,"text":"Editors"},"rank":1}],"authors":[{"text":"Meyer, F. P.","contributorId":96207,"corporation":false,"usgs":true,"family":"Meyer","given":"F.","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":296101,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70169182,"text":"70169182 - 1979 - Earthquakes; March-April, 1979","interactions":[],"lastModifiedDate":"2016-03-29T15:38:19","indexId":"70169182","displayToPublicDate":"1979-01-01T00:00:00","publicationYear":"1979","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, 1979","docAbstract":"<p>This was a moderately active period, seismically speaking. Three major earthquakes having magnitudes (M) ranging from 7.0 to 7.9 to only one major quake during the first 2 months of the year. Major earthquakes struck in Mexico, Indonesia, and Yugoslavia. The Yugoslavian earthquake caused considerable damage and loss of life.</p>\n<p>In the United States, a number of earthquakes were experienced, the most damaging one in southern California on March 15. The aftershocks continued in southeastern Alaska but caused no additional damage.&nbsp;</p>","language":"English","publisher":"U.S Geological Survey","usgsCitation":"Person, W., 1979, Earthquakes; March-April, 1979: Earthquake Information Bulletin (USGS), v. 11, no. 5, p. 183-186.","productDescription":"4 p.","startPage":"183","endPage":"186","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":319314,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"11","issue":"5","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"56f3be3fe4b0f59b85e02e61","contributors":{"authors":[{"text":"Person, W. J.","contributorId":91472,"corporation":false,"usgs":true,"family":"Person","given":"W. J.","affiliations":[],"preferred":false,"id":623296,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":85600,"text":"85600 - 1979 - Fish diseases","interactions":[],"lastModifiedDate":"2012-02-02T00:15:13","indexId":"85600","displayToPublicDate":"1979-01-01T00:00:00","publicationYear":"1979","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"title":"Fish diseases","docAbstract":"Abstract not submitted to date","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"The Merck Veterinary Manual","largerWorkSubtype":{"id":4,"text":"Other Government Series"},"language":"English","publisher":"Merck and Co, Inc.","publisherLocation":"Rahway, NJ","usgsCitation":"Meyer, F.P., 1979, Fish diseases, chap. <i>of</i> The Merck Veterinary Manual, 1247-1262.","productDescription":"1247-1262","costCenters":[{"id":606,"text":"Upper Midwest Environmental Sciences Center","active":true,"usgs":true}],"links":[{"id":195883,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"edition":"5th","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f9e4b07f02db5f3394","contributors":{"editors":[{"text":"Siegmund, O.H.","contributorId":112108,"corporation":false,"usgs":true,"family":"Siegmund","given":"O.H.","affiliations":[],"preferred":false,"id":504544,"contributorType":{"id":2,"text":"Editors"},"rank":1}],"authors":[{"text":"Meyer, F. P.","contributorId":96207,"corporation":false,"usgs":true,"family":"Meyer","given":"F.","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":296100,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":85624,"text":"85624 - 1979 - Correlations between residues of dichlorodiphenylethane, polychlorinated biphenyl, and dieldrin in the serum and tissues of mallard ducks (Anas platyrhynchos)","interactions":[],"lastModifiedDate":"2022-08-17T16:22:49.412067","indexId":"85624","displayToPublicDate":"1979-01-01T00:00:00","publicationYear":"1979","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"displayTitle":"Correlations between residues of dichlorodiphenylethane, polychlorinated biphenyl, and dieldrin in the serum and tissues of mallard ducks (<i>Anas platyrhynchos</i>)","title":"Correlations between residues of dichlorodiphenylethane, polychlorinated biphenyl, and dieldrin in the serum and tissues of mallard ducks (Anas platyrhynchos)","docAbstract":"<p>No abstract available.</p>","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Animals as monitors of environmental pollutants","largerWorkSubtype":{"id":12,"text":"Conference publication"},"language":"English","publisher":"National Academy of Sciences","publisherLocation":"Washington, DC","usgsCitation":"Friend, M., Haegle, M.A., Meeker, D.L., Hudson, R., and Baer, C.H., 1979, Correlations between residues of dichlorodiphenylethane, polychlorinated biphenyl, and dieldrin in the serum and tissues of mallard ducks (Anas platyrhynchos), <i>in</i> Animals as monitors of environmental pollutants, p. 319-326.","productDescription":"8 p.","startPage":"319","endPage":"326","costCenters":[{"id":456,"text":"National Wildlife Health Center","active":true,"usgs":true}],"links":[{"id":127823,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":405258,"rank":2,"type":{"id":15,"text":"Index Page"},"url":"https://nap.nationalacademies.org/catalog/19869/animals-as-monitors-of-environmental-pollutants","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad7e4b07f02db6844eb","contributors":{"authors":[{"text":"Friend, Milton 0000-0002-2882-3629","orcid":"https://orcid.org/0000-0002-2882-3629","contributorId":31332,"corporation":false,"usgs":true,"family":"Friend","given":"Milton","email":"","affiliations":[{"id":456,"text":"National Wildlife Health Center","active":true,"usgs":true}],"preferred":true,"id":296139,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Haegle, M. A.","contributorId":97449,"corporation":false,"usgs":true,"family":"Haegle","given":"M.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":296140,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Meeker, D. L.","contributorId":6790,"corporation":false,"usgs":true,"family":"Meeker","given":"D.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":296136,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Hudson, Rick","contributorId":212739,"corporation":false,"usgs":false,"family":"Hudson","given":"Rick","affiliations":[],"preferred":false,"id":296138,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Baer, C. H.","contributorId":16348,"corporation":false,"usgs":true,"family":"Baer","given":"C.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":296137,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70169247,"text":"70169247 - 1979 - Electrical measurements as stress-strain monitors","interactions":[],"lastModifiedDate":"2016-04-05T15:00:27","indexId":"70169247","displayToPublicDate":"1979-01-01T00:00:00","publicationYear":"1979","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":"Electrical measurements as stress-strain monitors","docAbstract":"<p>Many of the measurements of phyiscal properties being made in earthquake prediction studies are based on the premise that these properties are influenced by stresses and strains, especially so near the failure point. Electrical properties of rocks are controlled by the fluid in the pores and cracks in the rocks. Because these regions are most influenced by stresses, one should expect electrical measurements to be sensitive measures of changing stresses and strains. Nevertheless, the strain changes we are dealing with are very small, and, consequently, we need very sensitive instruments to detect them. &nbsp;</p>","language":"English","publisher":"U.S Geological Survey","usgsCitation":"Madden, T.R., 1979, Electrical measurements as stress-strain monitors: Earthquake Information Bulletin (USGS), v. 11, no. 1, p. 4-8.","productDescription":"5 p.","startPage":"4","endPage":"8","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":319270,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"11","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"56f3be41e4b0f59b85e02e78","contributors":{"authors":[{"text":"Madden, T. R.","contributorId":167750,"corporation":false,"usgs":false,"family":"Madden","given":"T.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":623388,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70162500,"text":"70162500 - 1979 - The 1976 Tangshan earthquake","interactions":[],"lastModifiedDate":"2019-11-13T15:06:42","indexId":"70162500","displayToPublicDate":"1979-01-01T00:00:00","publicationYear":"1979","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 1976 Tangshan earthquake","docAbstract":"<p>The Tangshan earthquake of 1976 was one of the largest earthquakes in recent years. It occurred on July 28 at 3:42 a.m, Beijing (Peking) local time, and had magnitude 7.8, focal depth of 15 kilometers, and an epicentral intensity of XI on the New Chinese Seismic Intensity Scale; it caused serious damage and loss of life in this densely populated industrial city. Now, with the help of people from all over China, the city of Tangshan is being rebuild.&nbsp;</p>","language":"English","publisher":"U.S Geological Survey","publisherLocation":"Reston, VA","usgsCitation":"Fang, W., 1979, The 1976 Tangshan earthquake: Earthquake Information Bulletin (USGS), v. 11, no. 3, p. 106-109.","productDescription":"4 p.","startPage":"106","endPage":"109","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":314825,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"China","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              117.92724609375,\n              39.11301365149975\n            ],\n            [\n              118.24584960937499,\n              38.77978137804918\n            ],\n            [\n              118.98193359375,\n              38.53097889440024\n            ],\n            [\n              119.37744140625,\n              38.976492485539396\n            ],\n            [\n              119.7509765625,\n              39.58875727696545\n            ],\n            [\n              119.761962890625,\n              40.371658891506094\n            ],\n            [\n              118.93798828125,\n              40.82212357516945\n            ],\n            [\n              118.311767578125,\n              41.02964338716638\n            ],\n            [\n              117.27905273437499,\n              40.75557964275589\n            ],\n            [\n              116.78466796875,\n              40.98819156349393\n            ],\n            [\n              117.103271484375,\n              39.605688178320804\n            ],\n            [\n              117.92724609375,\n              39.11301365149975\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"11","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"56a7556de4b0b28f1184d890","contributors":{"authors":[{"text":"Fang, Wang","contributorId":152542,"corporation":false,"usgs":false,"family":"Fang","given":"Wang","email":"","affiliations":[],"preferred":false,"id":589695,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70162276,"text":"70162276 - 1979 - Physiological and biochemical aspects of ozone toxicity to rainbow trout (<i>Salmo gairdneri</i>)","interactions":[],"lastModifiedDate":"2016-08-15T20:55:29","indexId":"70162276","displayToPublicDate":"1979-01-01T00:00:00","publicationYear":"1979","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":"Physiological and biochemical aspects of ozone toxicity to rainbow trout (<i>Salmo gairdneri</i>)","docAbstract":"<p><span>An acute toxicity curve for dissolved ozone (O</span><sub>3</sub><span>) in soft water at 10 &deg;C, using 10&ndash;13-cm rainbow trout (</span><i>Salmo gairdneri</i><span>) as the test species was calculated. The 96-h LC50 (95%, confidence interval) was 9.3 (8.1&ndash;10.6)&ensp;&mu;g/L. The lethal threshold level was about 8&ensp;&mu;g/L mandating that a conservative margin of safety be used if ozone is employed as a fish disease control agent. Death apparently results from massive destruction of the gill lamellar epithelium together with a severe hydromineral imbalance. In partial chronic (3-mo) testing, 2&ensp;&mu;g/L caused no significant biological damage while 5&ensp;&mu;g/L caused some gill pathological changes and reduced feeding behavior. Accordingly, 2&ensp;&mu;g/L is suggested as a provisional maximum safe exposure level, pending completion of life cycle studies. Thus, if ozone-treated water is discharged into the environment, dissolved O</span><sub>3</sub><span>&nbsp;should be reduced to at least the 2&ensp;&mu;g/L level to minimize adverse impacts on salmonids in receiving waters.</span></p>","language":"English","publisher":"NRC Research Press","doi":"10.1139/f79-088","usgsCitation":"Wedemeyer, G.A., Nelson, N.C., and Yasutake, W.T., 1979, Physiological and biochemical aspects of ozone toxicity to rainbow trout (<i>Salmo gairdneri</i>): Journal of the Fisheries Research Board of Canada, v. 36, no. 6, p. 605-614, https://doi.org/10.1139/f79-088.","productDescription":"10 p.","startPage":"605","endPage":"614","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"links":[{"id":314507,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"36","issue":"6","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"569f6c46e4b0961cf27fd1b8","contributors":{"authors":[{"text":"Wedemeyer, Gary A.","contributorId":30668,"corporation":false,"usgs":true,"family":"Wedemeyer","given":"Gary","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":589079,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Nelson, Nancy C.","contributorId":152336,"corporation":false,"usgs":false,"family":"Nelson","given":"Nancy","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":589080,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Yasutake, William T.","contributorId":70444,"corporation":false,"usgs":true,"family":"Yasutake","given":"William","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":589081,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70180323,"text":"70180323 - 1979 - Paleozoic rocks on the Alaska Peninsula: A section in <i>The United States Geological Survey in Alaska: Accomplishments during 1978</i>","interactions":[{"subject":{"id":70180323,"text":"70180323 - 1979 - Paleozoic rocks on the Alaska Peninsula: A section in <i>The United States Geological Survey in Alaska: Accomplishments during 1978</i>","indexId":"70180323","publicationYear":"1979","noYear":false,"title":"Paleozoic rocks on the Alaska Peninsula: A section in <i>The United States Geological Survey in Alaska: Accomplishments during 1978</i>"},"predicate":"IS_PART_OF","object":{"id":4433,"text":"cir804B - 1979 - The United States Geological Survey in Alaska: Accomplishments during 1978","indexId":"cir804B","publicationYear":"1979","noYear":false,"title":"The United States Geological Survey in Alaska: Accomplishments during 1978"},"id":1}],"isPartOf":{"id":4433,"text":"cir804B - 1979 - The United States Geological Survey in Alaska: Accomplishments during 1978","indexId":"cir804B","publicationYear":"1979","noYear":false,"title":"The United States Geological Survey in Alaska: Accomplishments during 1978"},"lastModifiedDate":"2017-01-27T11:26:55","indexId":"70180323","displayToPublicDate":"1979-01-01T00:00:00","publicationYear":"1979","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":307,"text":"Circular","code":"CIR","onlineIssn":"2330-5703","printIssn":"1067-084X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"804-B","title":"Paleozoic rocks on the Alaska Peninsula: A section in <i>The United States Geological Survey in Alaska: Accomplishments during 1978</i>","docAbstract":"<p>Two small areas of middle Paleozoic limestone were discovered near Gertrude Creek, 16 km north of Becharof Lake on the Alaska Peninsula, during reconnaissance flying as part of the Alaska Mineral Resource Assessment Program (AMRAP) for the Alaska Peninsula. Previously, the only known occurrence of Paleozoic rocks on the Alaska Peninsula was a small exposure of middle Permian limestone on an island at the entrance to Puale Bay (Hanson, 1957). This is the first reported occurrence of middle Paleozoic rocks in what is considered to be a Mesozoic and Tertiary province.</p>","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"The United States Geological Survey in Alaska: Accomplishments during 1978 (Circular 804-B)","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Arlington, VA","doi":"10.3133/70180323","usgsCitation":"Detterman, R.L., Case, J.E., and Wilson, F.H., 1979, Paleozoic rocks on the Alaska Peninsula: A section in <i>The United States Geological Survey in Alaska: Accomplishments during 1978</i>: U.S. Geological Survey Circular 804-B, 2 p., https://doi.org/10.3133/70180323.","productDescription":"2 p.","startPage":"B85","endPage":"B86","numberOfPages":"2","costCenters":[{"id":114,"text":"Alaska Science Center","active":true,"usgs":true}],"links":[{"id":334148,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1979/0804b/report.pdf#page=95","text":"Start page in larger work"},{"id":334149,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Alaska","otherGeospatial":"Alaska Peninsula","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"588c6ab2e4b08c8121c909a6","contributors":{"authors":[{"text":"Detterman, Robert L.","contributorId":71526,"corporation":false,"usgs":true,"family":"Detterman","given":"Robert","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":661223,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Case, James E.","contributorId":68702,"corporation":false,"usgs":true,"family":"Case","given":"James","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":661224,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Wilson, Frederic H. 0000-0003-1761-6437 fwilson@usgs.gov","orcid":"https://orcid.org/0000-0003-1761-6437","contributorId":67174,"corporation":false,"usgs":true,"family":"Wilson","given":"Frederic","email":"fwilson@usgs.gov","middleInitial":"H.","affiliations":[{"id":119,"text":"Alaska Science Center Geology Minerals","active":true,"usgs":true},{"id":114,"text":"Alaska Science Center","active":true,"usgs":true}],"preferred":true,"id":661225,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70035508,"text":"70035508 - 1979 - b values and ω<sup>−γ</sup> seismic source models: Implications for tectonic stress variations along active crustal fault zones and the estimation of high-frequency strong ground motion","interactions":[],"lastModifiedDate":"2015-06-15T10:17:18","indexId":"70035508","displayToPublicDate":"1979-01-01T00:00:00","publicationYear":"1979","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"b values and ω<sup>−γ</sup> seismic source models: Implications for tectonic stress variations along active crustal fault zones and the estimation of high-frequency strong ground motion","docAbstract":"<p><span>In this study the tectonic stress along active crustal fault zones is taken to be of the form&nbsp;</span><span class=\"math-equation-construct\" data-equation-construct=\"true\"><span class=\"math-equation-image\" data-equation-image=\"true\"><img class=\"inlineGraphic\" src=\"http://api.onlinelibrary.wiley.com/asset/v1/doi/10.1029%2FJB084iB05p02235/asset/equation%2Fjgrb2891-math-0001.gif?l=Cgg2pVVsCMwLOww28sbn56fxTbx6GilFBMCsUrZMoRcYP%2B9NZI%2F0t%2B3p7VO59umu6MIzikkO5ymj%0ANDlW1G0%2F%2BQ%3D%3D\" alt=\"inline image\" /></span></span><span>, where&nbsp;</span><span class=\"math-equation-construct\" data-equation-construct=\"true\"><span class=\"math-equation-image\" data-equation-image=\"true\"><img class=\"inlineGraphic\" src=\"http://api.onlinelibrary.wiley.com/asset/v1/doi/10.1029%2FJB084iB05p02235/asset/equation%2Fjgrb2891-math-0002.gif?l=Cgg2pVVsCMwLOww28sbn56fxTbx6GilFBMCsUrZMoRcYP%2B9NZI%2F0t%2B3p7VO59umuiedpqT79PPhK%0AOsNB85uCWA%3D%3D\" alt=\"inline image\" /></span></span><span>&nbsp;is the average tectonic stress at depth&nbsp;</span><i>y</i><span>&nbsp;and &Delta;&sigma;</span><span><i>p</i></span><span>(</span><i>x, y</i><span>) is a seismologically observable, essentially random function of both fault plane coordinates; the stress differences arising in the course of crustal faulting are derived from &Delta;&sigma;</span><i><span>p</span></i><span>(</span><i>x, y</i><span>). Empirically known frequency of occurrence statistics, moment-magnitude relationships, and the constancy of earthquake stress drops may be used to infer that the number of earthquakes&nbsp;</span><i>N</i><span>&nbsp;of dimension &ge;</span><i>r</i><span>&nbsp;is of the form&nbsp;</span><i>N</i><span>&nbsp;&sim; 1/</span><i>r</i><span>2</span><span>&nbsp;and that the spectral composition of &Delta;&sigma;</span><i><span>p</span></i><span>(</span><i>x, y</i><span>) is of the form&nbsp;</span><span class=\"math-equation-construct\" data-equation-construct=\"true\"><span class=\"math-equation-image\" data-equation-image=\"true\"><img class=\"inlineGraphic\" src=\"http://api.onlinelibrary.wiley.com/asset/v1/doi/10.1029%2FJB084iB05p02235/asset/equation%2Fjgrb2891-math-0003.gif?l=Cgg2pVVsCMwLOww28sbn56fxTbx6GilFBMCsUrZMoRcYP%2B9NZI%2F0t%2B3p7VO59umusANOiMJ6380O%0AqOQppeWKzQ%3D%3D\" alt=\"inline image\" /></span></span><span>, where&nbsp;</span><span class=\"math-equation-construct\" data-equation-construct=\"true\"><span class=\"math-equation-image\" data-equation-image=\"true\"><img class=\"inlineGraphic\" src=\"http://api.onlinelibrary.wiley.com/asset/v1/doi/10.1029%2FJB084iB05p02235/asset/equation%2Fjgrb2891-math-0004.gif?l=Cgg2pVVsCMwLOww28sbn56fxTbx6GilFBMCsUrZMoRcYP%2B9NZI%2F0t%2B3p7VO59umuGlAzWdjz2K3Q%0AG1y6nb%2F%2FjA%3D%3D\" alt=\"inline image\" /></span></span><span>&nbsp;is the two-dimensional Fourier transform of &Delta;&sigma;</span><i><span>p</span></i><span>(</span><i>x, y</i><span>) expressed in radial wave number&nbsp;</span><i>k</i><span>. The &gamma; = 2 model of the far-field shear wave displacement spectrum is consistent with the spectral composition&nbsp;</span><span class=\"math-equation-construct\" data-equation-construct=\"true\"><span class=\"math-equation-image\" data-equation-image=\"true\"><img class=\"inlineGraphic\" src=\"http://api.onlinelibrary.wiley.com/asset/v1/doi/10.1029%2FJB084iB05p02235/asset/equation%2Fjgrb2891-math-0005.gif?l=Cgg2pVVsCMwLOww28sbn56fxTbx6GilFBMCsUrZMoRcYP%2B9NZI%2F0t%2B3p7VO59umunzw%2FWHTH5Y0K%0AFHvdyv0N%2Fw%3D%3D\" alt=\"inline image\" /></span></span><span>, provided that the number of contributions to the spectral representation of the radiated field at frequency &fnof; goes as (</span><i>k</i><span>/</span><i>k</i><span>0</span><span>)</span><span>2</span><span>, consistent with the quasi-static frequency of occurrence relation&nbsp;</span><i>N</i><span>&nbsp;&sim; 1/</span><i>r</i><span>2</span><span>;</span><i>k</i><span>0</span><span>&nbsp;is a reference wave number associated with the reciprocal source dimension. Separately, a variety of seismologic observations suggests that the &gamma; = 2 model is the one generally, although certainly not always, applicable to the high-frequency spectral decay of the far-field radiation of earthquakes. In this framework, then,&nbsp;</span><i>b</i><span>&nbsp;values near 1, the general validity of the &gamma; = 2 model, and the constancy of earthquake stress drops independent of size are all related to the average spectral composition of</span><span class=\"math-equation-construct\" data-equation-construct=\"true\"><span class=\"math-equation-image\" data-equation-image=\"true\"><img class=\"inlineGraphic\" src=\"http://api.onlinelibrary.wiley.com/asset/v1/doi/10.1029%2FJB084iB05p02235/asset/equation%2Fjgrb2891-math-0006.gif?l=Cgg2pVVsCMwLOww28sbn56fxTbx6GilFBMCsUrZMoRcYP%2B9NZI%2F0t%2B3p7VO59umuaobXgGTYfS%2Fs%0AAwMugfb30g%3D%3D\" alt=\"inline image\" /></span></span><span>. Should one of these change as a result of premonitory effects leading to failure, as has been specifically proposed for&nbsp;</span><i>b</i><span>&nbsp;values, it seems likely that one or all of the other characteristics will change as well from their normative values. Irrespective of these associations, the far-field, high-frequency shear radiation for the &gamma; = 2 model in the presence of anelastic attenuation may be interpreted as band-limited, finite duration white noise in acceleration. Its rms value,&nbsp;</span><i>a</i><span>rms</span><span>, is given by the expression&nbsp;</span><i>a</i><span>rms</span><span>&nbsp;= 0.85[2</span><span>1/2</span><span>(2&pi;)</span><span>2</span><span>/106] (&Delta;&sigma;/&rho;</span><i>R</i><span>)(&fnof;</span><span>max</span><span>/&fnof;</span><span>0</span><span>)</span><span>1/2</span><span>, where &Delta;&sigma; is the earthquake stress drop, &rho; is density,&nbsp;</span><i>R</i><span>&nbsp;is hypocentral distance, &fnof;</span><span>0</span><span>&nbsp;is the spectral corner frequency, and &fnof;</span><span>max</span><span>&nbsp;is determined by&nbsp;</span><i>R</i><span>&nbsp;and specific attenuation 1/</span><i>Q</i><span>. For several reasons, one of which is that it may be estimated in the absence of empirically defined ground motion correlations,&nbsp;</span><i>a</i><span>rms</span><span>&nbsp;holds considerable promise as a measure of high-frequency strong ground motion for engineering purposes.</span></p>","language":"English","publisher":"AGU Publications","doi":"10.1029/JB084iB05p02235","issn":"01480227","usgsCitation":"Hanks, T.C., 1979, b values and ω<sup>−γ</sup> seismic source models: Implications for tectonic stress variations along active crustal fault zones and the estimation of high-frequency strong ground motion, v. 84, no. B5, p. 2235-2242, https://doi.org/10.1029/JB084iB05p02235.","productDescription":"8 p.","startPage":"2235","endPage":"2242","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":244197,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":216334,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1029/JB084iB05p02235"}],"volume":"84","issue":"B5","noUsgsAuthors":false,"publicationDate":"2012-09-20","publicationStatus":"PW","scienceBaseUri":"5059ef79e4b0c8380cd4a26e","contributors":{"authors":[{"text":"Hanks, Thomas C. 0000-0003-0928-0056 thanks@usgs.gov","orcid":"https://orcid.org/0000-0003-0928-0056","contributorId":3065,"corporation":false,"usgs":true,"family":"Hanks","given":"Thomas","email":"thanks@usgs.gov","middleInitial":"C.","affiliations":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true}],"preferred":true,"id":450977,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":10519,"text":"ofr791638 - 1979 - Data on ground-water resources of the Spring Mountains area, Toiyabe National Forest, Nevada","interactions":[],"lastModifiedDate":"2023-03-22T19:27:49.956626","indexId":"ofr791638","displayToPublicDate":"1979-01-01T00:00:00","publicationYear":"1979","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":"79-1638","title":"Data on ground-water resources of the Spring Mountains area, Toiyabe National Forest, Nevada","docAbstract":"This report lists data on ground-water levels for 16 wells and discharge for 18 springs in the Spring Mountain area of the Tolyabe National Forest. Water levels in wells ranged from 325 to 519 feet below land surface. The highest spring discharge listed is 107 gallons per minute. In addition, data on the chemical quality of the water from selected wells and springs are listed.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr791638","usgsCitation":"Nichols, W., and Davis, L.E., 1979, Data on ground-water resources of the Spring Mountains area, Toiyabe National Forest, Nevada: U.S. Geological Survey Open-File Report 79-1638, Report: iv, 19 p.; 1 Plate: 1.55 x 18.34 inches, https://doi.org/10.3133/ofr791638.","productDescription":"Report: iv, 19 p.; 1 Plate: 1.55 x 18.34 inches","costCenters":[],"links":[{"id":414567,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_11203.htm","linkFileType":{"id":5,"text":"html"}},{"id":38368,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1979/1638/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":38367,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1979/1638/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":144246,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1979/1638/report-thumb.jpg"}],"country":"United States","state":"Nevada","otherGeospatial":"Spring Mountains area, Toiyabe National Forest","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -115.74,\n              36.375\n            ],\n            [\n              -115.74,\n              36.206\n            ],\n            [\n              -115.526,\n              36.206\n            ],\n            [\n              -115.526,\n              36.375\n            ],\n            [\n              -115.74,\n              36.375\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afde4b07f02db69701a","contributors":{"authors":[{"text":"Nichols, William D.","contributorId":98296,"corporation":false,"usgs":true,"family":"Nichols","given":"William D.","affiliations":[],"preferred":false,"id":161532,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Davis, Louise E.","contributorId":79478,"corporation":false,"usgs":true,"family":"Davis","given":"Louise","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":161531,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70168604,"text":"70168604 - 1979 - Earthquake studies on Canada’s west coast; Pacific Geoscience Centre","interactions":[],"lastModifiedDate":"2019-11-14T08:49:52","indexId":"70168604","displayToPublicDate":"1979-01-01T00:00:00","publicationYear":"1979","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 studies on Canada’s west coast; Pacific Geoscience Centre","docAbstract":"<p>On a global scale, Canada's west coast lies within the zone of a seismicity that stretches around the Pacific Ocean. In plate tectonic terms, it is dominated by the same right-lateral shearing between the Pacific and American plates that is responsible for the seismicity of California. However, in southern British Columbia the interaction is further complicated. Between the San Andreas fault in California and the Queen Charlotte fault off British Columbia, the Pacific and American plates are separated by the small independent Juan de Fuca plate system. This is spreading away from the Pacific plate and converging with the margin of the Pacific Northwest. The resulting Cascade volcanic chain and its extension into southern British Columbia are the topograhic expression of its subduction.&nbsp;</p>","language":"English","publisher":"U.S Geological Survey","publisherLocation":"Reston, VA","usgsCitation":"Rogers, G.C., and Riddihough, R.P., 1979, Earthquake studies on Canada’s west coast; Pacific Geoscience Centre: Earthquake Information Bulletin (USGS), v. 11, no. 5, p. 175-179.","productDescription":"5 p.","startPage":"175","endPage":"179","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":318222,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"Canada","otherGeospatial":"Pacific coast","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -124.45312499999999,\n              48.45835188280866\n            ],\n            [\n              -121.904296875,\n              49.210420445650286\n            ],\n            [\n              -126.474609375,\n              52.53627304145948\n            ],\n            [\n              -129.990234375,\n              55.178867663281984\n            ],\n            [\n              -133.857421875,\n              54.16243396806779\n            ],\n            [\n              -132.099609375,\n              51.39920565355378\n            ],\n            [\n              -126.38671874999999,\n              48.69096039092549\n            ],\n            [\n              -124.45312499999999,\n              48.45835188280866\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"11","issue":"5","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"56c99c50e4b059daa47c9aba","contributors":{"authors":[{"text":"Rogers, G. C.","contributorId":167100,"corporation":false,"usgs":false,"family":"Rogers","given":"G.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":621008,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Riddihough, Robin P.","contributorId":51150,"corporation":false,"usgs":true,"family":"Riddihough","given":"Robin","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":621009,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70168591,"text":"70168591 - 1979 - Soviet prediction of a major earthquake","interactions":[],"lastModifiedDate":"2016-03-22T15:01:11","indexId":"70168591","displayToPublicDate":"1979-01-01T00:00:00","publicationYear":"1979","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":"Soviet prediction of a major earthquake","docAbstract":"<p>On November 1, 1978, a magnitude 7 earthquake occurred north of the Pamir Mountains near the Tadjiskistan-Kirghizia border, 150 kilometers east of Garm in Soviet Central Asia. Although the earthquake was felt in Tashkent, Dushanbe, and the Fergana Valley, the epicentral area was uninhabited at that time of year, and no damage was reported.&nbsp;</p>","language":"English","publisher":"U.S Geological Survey","usgsCitation":"Simpson, D., 1979, Soviet prediction of a major earthquake: Earthquake Information Bulletin (USGS), v. 11, no. 6, p. 234-235.","productDescription":"2 p.","startPage":"234","endPage":"235","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":318209,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"11","issue":"6","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"56c99c54e4b059daa47c9afb","contributors":{"authors":[{"text":"Simpson, D.W.","contributorId":44152,"corporation":false,"usgs":true,"family":"Simpson","given":"D.W.","email":"","affiliations":[],"preferred":false,"id":620991,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70168583,"text":"70168583 - 1979 - Records of prehistoric earthquakes in sedimentary deposits in lakes","interactions":[],"lastModifiedDate":"2016-09-12T01:44:07","indexId":"70168583","displayToPublicDate":"1979-01-01T00:00:00","publicationYear":"1979","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":"Records of prehistoric earthquakes in sedimentary deposits in lakes","docAbstract":"<p>Historic records of earthquakes are too short to allow a true assessment of their recurrence intervals. Methods are needed, therefore, that will enable the seismicity of an area to be evaluated beyond the limit of historic records.</p>\n<p>One place where a record of ancient seismic activity might be preserved is in lake sediments. Strong earthquakes often cause a phenomenon in water-saturated sediments known as liquefaction. The seismic shaking tends to reorient the sediment grains into a more compact arrangement. This usually means that the sediment liquefies and is redeposited in a smaller volume; there is an accompanying explusion of water and, in cases of severe shaking, sediment-laden water.</p>\n<p>During a strong earthquake, deformation due to liquefaction may occur in the upper layers of lake sediment. If this deformation is preserved without further deformation as new layers of sediment are deposited in the lake and if one could later find and identify these layers, one would then have a record of prehistoric earthquakes in the lake beds.&nbsp;</p>","language":"English","publisher":"U.S Geological Survey","usgsCitation":"Sims, J., 1979, Records of prehistoric earthquakes in sedimentary deposits in lakes: Earthquake Information Bulletin (USGS), v. 11, no. 6, p. 228-233.","productDescription":"6 p.","startPage":"228","endPage":"233","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":318203,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"11","issue":"6","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"56c84acce4b0b3c9ae38109e","contributors":{"editors":[{"text":"Spall, Henry","contributorId":77933,"corporation":false,"usgs":true,"family":"Spall","given":"Henry","email":"","affiliations":[],"preferred":false,"id":648561,"contributorType":{"id":2,"text":"Editors"},"rank":1}],"authors":[{"text":"Sims, J.","contributorId":167094,"corporation":false,"usgs":false,"family":"Sims","given":"J.","affiliations":[],"preferred":false,"id":648560,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70168595,"text":"70168595 - 1979 - Earthquake predictions using seismic velocity ratios","interactions":[],"lastModifiedDate":"2016-03-22T15:20:02","indexId":"70168595","displayToPublicDate":"1979-01-01T00:00:00","publicationYear":"1979","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 predictions using seismic velocity ratios","docAbstract":"<p>Since the beginning of modern seismology, seismologists have contemplated predicting earthquakes. The usefulness of earthquake predictions to the reduction of human and economic losses and the value of long-range earthquake prediction to planning is obvious. Not as clear are the long-range economic and social impacts of earthquake prediction to a speicifc area. The general consensus of opinion among scientists and government officials, however, is that the quest of earthquake prediction is a worthwhile goal and should be prusued with a sense of urgency.&nbsp;</p>","language":"English","publisher":"U.S Geological Survey","usgsCitation":"Sherburne, R.W., 1979, Earthquake predictions using seismic velocity ratios: Earthquake Information Bulletin (USGS), v. 11, no. 1, p. 18-21.","productDescription":"4 p.","startPage":"18","endPage":"21","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":318213,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"11","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"56c99c45e4b059daa47c9aad","contributors":{"authors":[{"text":"Sherburne, R. W.","contributorId":167096,"corporation":false,"usgs":false,"family":"Sherburne","given":"R.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":620997,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":2001084,"text":"2001084 - 1979 - Influences of selected environmental factors on the activity of a prospective fish toxicant, 2-(digeranyl-amino)-ethanol, in laboratory tests","interactions":[],"lastModifiedDate":"2012-02-02T00:14:53","indexId":"2001084","displayToPublicDate":"1979-01-01T00:00:00","publicationYear":"1979","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":"88","title":"Influences of selected environmental factors on the activity of a prospective fish toxicant, 2-(digeranyl-amino)-ethanol, in laboratory tests","docAbstract":"Abstract not submitted to date","language":"English","publisher":"U.S. Fish and Wildlife Service","publisherLocation":"La Crosse, WI","usgsCitation":"Launer, C., and Bills, T., 1979, Influences of selected environmental factors on the activity of a prospective fish toxicant, 2-(digeranyl-amino)-ethanol, in laboratory tests: Investigations in Fish Control 88, 4.","productDescription":"4","startPage":"0","endPage":"4","numberOfPages":"4","costCenters":[{"id":606,"text":"Upper Midwest Environmental Sciences Center","active":true,"usgs":true}],"links":[{"id":199088,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f1e4b07f02db5ee608","contributors":{"authors":[{"text":"Launer, C.A.","contributorId":102533,"corporation":false,"usgs":true,"family":"Launer","given":"C.A.","email":"","affiliations":[],"preferred":false,"id":325366,"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":325365,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":2000146,"text":"2000146 - 1979 - Distribution and status of marine birds breeding along the coasts of the Chukchi and Bering seas","interactions":[],"lastModifiedDate":"2017-09-11T10:50:01","indexId":"2000146","displayToPublicDate":"1979-01-01T00:00:00","publicationYear":"1979","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":74,"text":"Research Report","active":false,"publicationSubtype":{"id":1}},"seriesNumber":"11","title":"Distribution and status of marine birds breeding along the coasts of the Chukchi and Bering seas","docAbstract":"The Alaska coast fronting on the Chukchi and Bering seas, exclusive of the Aleutian Islands, supports seven complexes of marine bird colonies numbering more than 1 million birds each, nine colonies of 100,000 to almost 1 million birds, and many smaller colonies. Colonies are found on most headlands and islands and are dominated numerically by alcids and kittiwakes (Rissa sp.). Estuarine habitats (mainly the lowlands of northern Seward Peninsula, Yukon-Kuskokwim delta, and the north side of the Alaska Peninsula) are extremely important for breeding and migrating marine waterfowl, shorebirds, gulls (Larus sp.), and terns (Sterna sp.). Information on population size and distribution of breeding marine birds within this area is extensive for only a few of the more heavily hunted species of waterfowl. Except for the intensive and systematic censusing of a few colonies in this region, population data on cliff-, burrow-, and crevice-nesting birds are such that all but gross changes in numbers may go unnoticed, and if noticed they could not be measured.","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Conservation of marine birds of northern North America","largerWorkSubtype":{"id":1,"text":"Federal Government Series"},"language":"English","publisher":"U.S. Fish and Wildlife Service","publisherLocation":"Washington, DC","usgsCitation":"Bartonek, J., and Sealy, S., 1979, Distribution and status of marine birds breeding along the coasts of the Chukchi and Bering seas: Research Report 11, 11 p.","productDescription":"11 p.","startPage":"21","endPage":"31","numberOfPages":"11","costCenters":[{"id":480,"text":"Northern Prairie Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":199255,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a80e4b07f02db6495c0","contributors":{"authors":[{"text":"Bartonek, James C.","contributorId":38085,"corporation":false,"usgs":true,"family":"Bartonek","given":"James C.","affiliations":[],"preferred":false,"id":325170,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Sealy, S.G.","contributorId":59908,"corporation":false,"usgs":true,"family":"Sealy","given":"S.G.","affiliations":[],"preferred":false,"id":325171,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70184462,"text":"70184462 - 1979 - Dispersal and migratory patterns of San Francisco Bay produced herons, egrets, and terns","interactions":[],"lastModifiedDate":"2018-05-20T11:36:01","indexId":"70184462","displayToPublicDate":"1979-01-01T00:00:00","publicationYear":"1979","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2881,"text":"North American Bird Bander","active":true,"publicationSubtype":{"id":10}},"title":"Dispersal and migratory patterns of San Francisco Bay produced herons, egrets, and terns","docAbstract":"<p>San Francisco Bay, California, including its fringing marshes, supports a large and diverse water related avifauna (Grinnell and Wythe 19271 Sibley 1952, Gill 1973, 1977). Certain of man's alterations of the Bay's shallower wetlands have resulted in increased habitat diversity which has allowed colonization by several species of birds including some colonial nesting species. The extensive dikes associated with salt production and some areas of higher ground created by dredge spoils have provided increased tide-free substratum, some of it insular, suitable for nesting. The resulting numbers of Snowy Egrets (<i>Egretta thula)</i>, Black-crowned Night Herons (<i>Nycticorax nycticorax</i>), Forster's Terns (<i>Sterna forsteri</i>), and Caspian Terns (<i>Sterna caspia</i>) using these areas now represent a significant portion of the northern California breeding populations of these species.</p><p>In conjunction with a study of the breeding birds of the South San Francisco Bay Estuary (Gill 1973, 1977) from 1971 to 1973, we banded 187 Great Blue Herons (<i>Ardea herodias</i>), 1499 Snowy Egrets, 1615 Black-crowned Night Herons, 2943 Forster's Terns, and 743 Caspian Terns; often this represented a substantial portion of these species banded in the western states during these years (Table 1). Recoveries from these bandings through 1977 plus additional recoveries from a few earlier and some more recent bandings provide the data for this report on dispersal patterns and migration of San Francisco Bay produced herons, egrets, and terns. </p>","language":"English","publisher":"Western, Inland, and Eastern Bird Banding Associations","usgsCitation":"Gill, R., and Mewaldt, L., 1979, Dispersal and migratory patterns of San Francisco Bay produced herons, egrets, and terns: North American Bird Bander, v. 4, no. 1, p. 4-13.","productDescription":"10 p.","startPage":"4","endPage":"13","costCenters":[{"id":114,"text":"Alaska Science Center","active":true,"usgs":true}],"links":[{"id":337240,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":337239,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://www.westernbirdbanding.org/publications_NABB.html","text":"Journal's Website"}],"country":"United States","state":"California","otherGeospatial":"San Francisco Bay","volume":"4","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"58c277fae4b014cc3a3e7712","contributors":{"authors":[{"text":"Gill, Robert E. Jr. 0000-0002-6385-4500 rgill@usgs.gov","orcid":"https://orcid.org/0000-0002-6385-4500","contributorId":171747,"corporation":false,"usgs":true,"family":"Gill","given":"Robert E.","suffix":"Jr.","email":"rgill@usgs.gov","affiliations":[{"id":117,"text":"Alaska Science Center Biology WTEB","active":true,"usgs":true}],"preferred":true,"id":681612,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Mewaldt, L. Richard","contributorId":187768,"corporation":false,"usgs":false,"family":"Mewaldt","given":"L. Richard","affiliations":[],"preferred":false,"id":681613,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":11750,"text":"ofr79250 - 1979 - Stratigraphic sections of Jurassic San Rafael Group and adjacent rocks in Delta, Mesa, and Montrose Counties, Colorado","interactions":[],"lastModifiedDate":"2023-08-10T19:13:58.200658","indexId":"ofr79250","displayToPublicDate":"1979-01-01T00:00:00","publicationYear":"1979","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":"79-250","title":"Stratigraphic sections of Jurassic San Rafael Group and adjacent rocks in Delta, Mesa, and Montrose Counties, Colorado","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr79250","usgsCitation":"Wright, J.C., and Dickey, D.D., 1979, Stratigraphic sections of Jurassic San Rafael Group and adjacent rocks in Delta, Mesa, and Montrose Counties, Colorado: U.S. Geological Survey Open-File Report 79-250, i, 29 p., https://doi.org/10.3133/ofr79250.","productDescription":"i, 29 p.","costCenters":[],"links":[{"id":144747,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1979/0250/report-thumb.jpg"},{"id":419718,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1979/0250/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Colorado","county":"Delta County, Mesa County, Montrose County","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b24e4b07f02db6ae873","contributors":{"authors":[{"text":"Wright, James Clifton","contributorId":95878,"corporation":false,"usgs":true,"family":"Wright","given":"James","email":"","middleInitial":"Clifton","affiliations":[],"preferred":false,"id":163667,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Dickey, Dayton Delbert","contributorId":8472,"corporation":false,"usgs":true,"family":"Dickey","given":"Dayton","email":"","middleInitial":"Delbert","affiliations":[],"preferred":false,"id":163666,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":1003355,"text":"1003355 - 1979 - Gas-liquid chromatographic determination of Bayer 73 in fish, aquatic invertebrates, mud, and water","interactions":[],"lastModifiedDate":"2025-03-03T15:50:42.011386","indexId":"1003355","displayToPublicDate":"1979-01-01T00:00:00","publicationYear":"1979","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2533,"text":"Journal of the Association of Official Analytical Chemists","active":true,"publicationSubtype":{"id":10}},"title":"Gas-liquid chromatographic determination of Bayer 73 in fish, aquatic invertebrates, mud, and water","docAbstract":"<p><span>A gas-liquid chromatographic (GLC) method is described for determining residues of Bayer 73 (2-aminoethanol salt of 2’,5-dichloro-4’-nitrosalicylanilide) in fish muscle, aquatic invertebrates, mud, and water by analyzing for 2-chloro-4-nitroaniline (CNA), a hydrolysis product of Bayer 73. Bayer 73 residues are extracted from fish muscle tissue, invertebrates, and mud with acetone-formic acid (98+2), and partitioned from water samples with chloroform. After sample cleanup by solvent and acid-base partitioning, the concentrated extract is hydrolyzed with 2</span><i>N</i><span>&nbsp;NaOH and H</span><sub>2</sub><span>O</span><sub>2</sub><span>&nbsp;for 10 min at 95°C. The CNA is then partitioned into hexane-ethyl ether (7+3) and determined by electron capture GLC. Average recoveries were 88% for fish, 82% for invertebrates, 82% for mud, and 98% for water at 3 or more fortification levels.</span></p>","language":"English","publisher":"Oxford Academic","doi":"10.1093/jaoac/62.5.1141","usgsCitation":"Luhning, C., Harman, P., Sills, J., Dawson, V.K., and Allen, J.L., 1979, Gas-liquid chromatographic determination of Bayer 73 in fish, aquatic invertebrates, mud, and water: Journal of the Association of Official Analytical Chemists, v. 62, no. 5, p. 1141-1145, https://doi.org/10.1093/jaoac/62.5.1141.","productDescription":"5 p.","startPage":"1141","endPage":"1145","numberOfPages":"5","costCenters":[{"id":606,"text":"Upper Midwest Environmental Sciences Center","active":true,"usgs":true}],"links":[{"id":129095,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"62","issue":"5","noUsgsAuthors":false,"publicationDate":"2020-01-22","publicationStatus":"PW","scienceBaseUri":"4f4e4b28e4b07f02db6b12d1","contributors":{"authors":[{"text":"Luhning, C.W.","contributorId":76682,"corporation":false,"usgs":true,"family":"Luhning","given":"C.W.","affiliations":[],"preferred":false,"id":313160,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Harman, P.D.","contributorId":56595,"corporation":false,"usgs":true,"family":"Harman","given":"P.D.","email":"","affiliations":[],"preferred":false,"id":313159,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Sills, J.B.","contributorId":55380,"corporation":false,"usgs":true,"family":"Sills","given":"J.B.","email":"","affiliations":[],"preferred":false,"id":313158,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Dawson, V. K.","contributorId":48900,"corporation":false,"usgs":true,"family":"Dawson","given":"V.","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":313156,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Allen, J. L.","contributorId":49295,"corporation":false,"usgs":true,"family":"Allen","given":"J.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":313157,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":2000109,"text":"2000109 - 1979 - Classification of wetlands and deepwater habitats of the United States","interactions":[],"lastModifiedDate":"2016-09-21T14:30:38","indexId":"2000109","displayToPublicDate":"1979-01-01T00:00:00","publicationYear":"1979","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":20,"text":"FWS/OBS","active":false,"publicationSubtype":{"id":1}},"seriesNumber":"79/31","title":"Classification of wetlands and deepwater habitats of the United States","docAbstract":"This classification, to be used in a new inventory of wetlands and deepwater habitats of the United States, is intended to describe ecological taxa, arrange them in a system useful to resource managers, furnish units for mapping, and provide uniformity of concepts and terms. Wetlands are defined by plants (hydrophytes), soils (hydric soils), and frequency of flooding. Ecologically related areas of deep water, traditionally not considered wetlands, are included in the classification as deepwater habitats.Systems form the highest level of the classification hierarchy; five are defined--Marine, Estuarine, Riverine, Lacustrine, and Palustrine. Marine and Estuarine systems each have two subsystems, Subtidal and Intertidal; the Riverine system has four subsystems, Tidal, Lower Perennial, Upper Perennial, and Intermittent; the Lacustrine has two, Littoral and Limnetic; and the Palustrine has no subsystem.Within the subsystems, classes are based on substrate material and flooding regime, or on vegetative life form. The same classes may appear under one or more of the systems or subsystems. Six classes are based on substrate and flooding regime: (1) Rock Bottom with a substrate of bedrock, boulders, or stones; (2) Unconsolidated Bottom with a substrate of cobbles, gravel, sand, mud, or organic material; (3) Rocky Shore with the same substrate as Rock Bottom; (4) Unconsolidated Shore with the same substrate as Unconsolidated Bottom; (5) Streambed with any of the substrates; and (6) Reef with a substrate composed of the living and dead remains of invertebrates (corals, mollusks, or worms). The bottom classes, (1) and (2) above, are flooded all or most of the time and the shore classes, (3) and (4), are exposed most of the time. The class Streambed is restricted to channels of intermittent streams and tidal channels that are dewatered at low tide. The life form of the dominant vegetation defines the five classes based on vegetative form: (1) Aquatic Bed, dominated by plants that grow principally on or below the surface of the water; (2) Moss-Lichen Wetland, dominated by mosses or lichens; (3) Emergent Wetland, dominated by emergent herbaceous angiosperms; (4) Scrub-Shrub Wetland, dominated by shrubs or small trees; and (5) Forested Wetland, dominated by large trees.The dominance type, which is named for the dominant plant or animal forms, is the lowest level of the classification hierarchy. Only examples are provided for this level; dominance types must be developed by individual users of the classification.Modifying terms applied to the classes or subclasses are essential for use of the system. In tidal areas, the type and duration of flooding are described by four water regime modifiers: subtidal, irregularly exposed, regularly flooded, and irregularly flooded. In nontidal areas, six regimes are used: permanently flooded, intermittently exposed, semipermanently flooded, seasonally flooded, saturated, temporarily flooded, intermittently flooded, and artificially flooded. A hierarchical system of water chemistry modifiers, adapted from the Venice System, is used to describe the salinity of the water. Fresh waters are further divided on the basis of pH. Use of a hierarchical system of soil modifiers taken directly from U.S. soil taxonomy is also required. Special modifiers are used where appropriate: excavated, impounded, diked, partly drained, farmed, and artificial.Regional differences important to wetland ecology are described through a regionalization that combines a system developed for inland areas by R. G. Bailey in 1976 with our Marine and Estuarine provinces.The structure of the classification allows it to be used at any of several hierarchical levels. Special data required for detailed application of the system are frequently unavailable, and thus data gathering may be prerequisite to classification. Development of rules by the user will be required for specific map scales. Dominance types and relationships of plant and animal co","language":"English","publisher":"U.S. Fish and Wildlife Service","publisherLocation":"Washington, DC","usgsCitation":"Cowardin, L., Carter, V., Golet, F., and LaRoe, E., 1979, Classification of wetlands and deepwater habitats of the United States: FWS/OBS 79/31, 103 p.","productDescription":"103 p.","costCenters":[{"id":480,"text":"Northern Prairie Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":197756,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":11908,"rank":200,"type":{"id":11,"text":"Document"},"url":"https://www.fws.gov/wetlands/Documents/Classification-of-Wetlands-and-Deepwater-Habitats-of-the-United-States.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4abbe4b07f02db672b8e","contributors":{"authors":[{"text":"Cowardin, L.M.","contributorId":106435,"corporation":false,"usgs":true,"family":"Cowardin","given":"L.M.","email":"","affiliations":[],"preferred":false,"id":325104,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Carter, V.","contributorId":61115,"corporation":false,"usgs":true,"family":"Carter","given":"V.","email":"","affiliations":[],"preferred":false,"id":325102,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Golet, F.C.","contributorId":32124,"corporation":false,"usgs":true,"family":"Golet","given":"F.C.","email":"","affiliations":[],"preferred":false,"id":325101,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"LaRoe, E.T.","contributorId":103766,"corporation":false,"usgs":true,"family":"LaRoe","given":"E.T.","email":"","affiliations":[],"preferred":false,"id":325103,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":2000011,"text":"2000011 - 1979 - Annotated list of the fishes of the Lake Ontario watershed","interactions":[],"lastModifiedDate":"2012-02-02T00:15:00","indexId":"2000011","displayToPublicDate":"1979-01-01T00:00:00","publicationYear":"1979","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":"36","title":"Annotated list of the fishes of the Lake Ontario watershed","docAbstract":"This annotated list of the fishes of Lake Ontario and its watershed is based on published distribution records, museum collections, and reports of fish surveys that confirm the occurrence of fish species dating back to the 1850's. It includes 130 forms (129 spp. + the hybrid splake), 20 of which have disappeared or are extremely rare today. Considering species present only in the lake proper, 64 were reported in 1929, and 51 of those remained in 1972-73 (13 having disappeared). Seventeen species and the splake are fishes not known to have occurred in the lake in 1929 or were introduced since then. A list of 86 references pertinent to the study of the fish fauna of the watershed is given. The present list, started in 1972, includes some information from as late as 1976.","language":"English","publisher":"Great Lakes Fishery Commission","collaboration":"Out-of-print","usgsCitation":"Crossman, E.J., and Van Meter, H.D., 1979, Annotated list of the fishes of the Lake Ontario watershed: Technical Report 36, 25 p.","productDescription":"25 p.","startPage":"0","endPage":"25","numberOfPages":"25","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":198815,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":92051,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://www.glfc.org/pubs/TechReports/Tr36.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac8e4b07f02db67bc9a","contributors":{"authors":[{"text":"Crossman, Edwin J.","contributorId":42678,"corporation":false,"usgs":true,"family":"Crossman","given":"Edwin","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":324925,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Van Meter, Harry D.","contributorId":36887,"corporation":false,"usgs":true,"family":"Van Meter","given":"Harry","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":324924,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":2000126,"text":"2000126 - 1979 - Sea ice as a factor in seabird distribution and ecology in the Beaufort, Chukchi, and Bering seas","interactions":[],"lastModifiedDate":"2017-10-11T10:43:19","indexId":"2000126","displayToPublicDate":"1979-01-01T00:00:00","publicationYear":"1979","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":74,"text":"Research Report","active":false,"publicationSubtype":{"id":1}},"seriesNumber":"11","title":"Sea ice as a factor in seabird distribution and ecology in the Beaufort, Chukchi, and Bering seas","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Conservation of marine birds of northern North America","largerWorkSubtype":{"id":1,"text":"Federal Government Series"},"language":"English","publisher":"U.S. Fish and Wildlife Service","publisherLocation":"Washington, DC","usgsCitation":"Divoky, G., 1979, Sea ice as a factor in seabird distribution and ecology in the Beaufort, Chukchi, and Bering seas: Research Report 11, 8 p.","productDescription":"8 p.","startPage":"9","endPage":"17","costCenters":[{"id":480,"text":"Northern Prairie Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":198528,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":94578,"rank":200,"type":{"id":11,"text":"Document"},"url":"https://www.archive.org/details/conservationofma00naturich","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adbe4b07f02db685e29","contributors":{"authors":[{"text":"Divoky, G.J.","contributorId":15971,"corporation":false,"usgs":true,"family":"Divoky","given":"G.J.","affiliations":[],"preferred":false,"id":325135,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70012528,"text":"70012528 - 1979 - Geochemical surveys in the United States in relation to health.","interactions":[],"lastModifiedDate":"2013-01-21T18:18:16","indexId":"70012528","displayToPublicDate":"1979-01-01T00:00:00","publicationYear":"1979","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3048,"text":"Philosophical Transactions of the Royal Society B: Biological Sciences","active":true,"publicationSubtype":{"id":10}},"title":"Geochemical surveys in the United States in relation to health.","docAbstract":"Geochemical surveys in relation to health may be classified as having one, two or three dimensions. One-dimensional surveys examine relations between concentrations of elements such as Pb in soils and other media and burdens of the same elements in humans, at a given time. The spatial distributions of element concentrations are not investigated. The primary objective of two-dimensional surveys is to map the distributions of element concentrations, commonly according to stratified random sampling designs based on either conceptual landscape units or artificial sampling strata, but systematic sampling intervals have also been used. Political units have defined sample areas that coincide with the units used to accumulate epidemiological data. Element concentrations affected by point sources have also been mapped. Background values, location of natural or technological anomalies and the geographic scale of variation for several elements often are determined. Three-dimensional surveys result when two-dimensional surveys are repeated to detect environmental changes. -Author","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Philosophical Transactions of the Royal Society B: Biological Sciences","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1098/rstb.1979.0094","usgsCitation":"Tourtelot, H.A., 1979, Geochemical surveys in the United States in relation to health.: Philosophical Transactions of the Royal Society B: Biological Sciences, v. 288, no. 1026, p. 113-125, https://doi.org/10.1098/rstb.1979.0094.","startPage":"113","endPage":"125","numberOfPages":"13","costCenters":[],"links":[{"id":222728,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":266213,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1098/rstb.1979.0094"}],"volume":"288","issue":"1026","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a16c2e4b0c8380cd55257","contributors":{"authors":[{"text":"Tourtelot, H. A.","contributorId":79140,"corporation":false,"usgs":true,"family":"Tourtelot","given":"H.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":363824,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70012429,"text":"70012429 - 1979 - Improved signal discrimination in tectonomagnetism: Discovery of a volcanomagnetic effect at Kilauea, Hawaii","interactions":[],"lastModifiedDate":"2013-02-13T13:50:57","indexId":"70012429","displayToPublicDate":"1979-01-01T00:00:00","publicationYear":"1979","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3071,"text":"Physics of the Earth and Planetary Interiors","active":true,"publicationSubtype":{"id":10}},"title":"Improved signal discrimination in tectonomagnetism: Discovery of a volcanomagnetic effect at Kilauea, Hawaii","docAbstract":"Cancellation of extraterrestrial magnetic disturbances by taking simple differences between total field readings at spaced stations is imperfect. It is shown that improvement is possible when three component observatory data are available from a single station in the general, but not necessarily immediate, vicinity of an array of total field stations used in a tectonomagnetic study. The local effects of a magnetic disturbance field depend upon its orientation, so that local field differences are more effectively generated by certain orientations of the disturbance field. The orientation of the disturbance field which correlates best with a local difference field is determined by a least-squares method, so that the correlated vector signal can be routinely subtracted from the difference field record. Application of the technique to daily averages of records from three synchronised proton magnetometers on Kilauea volcano reveals a 1.5-nT change in the local field at the time of a flank eruption in May, 1973. This effect was obscured by noise in the raw difference field data. ?? 1979.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Physics of the Earth and Planetary Interiors","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Elsevier","publisherLocation":"Amsterdam, Netherlands","doi":"10.1016/0031-9201(79)90005-0","issn":"00319201","usgsCitation":"Davis, P., Stacey, F., Zablocki, C., and Olson, J., 1979, Improved signal discrimination in tectonomagnetism: Discovery of a volcanomagnetic effect at Kilauea, Hawaii: Physics of the Earth and Planetary Interiors, v. 19, no. 4, p. 331-336, https://doi.org/10.1016/0031-9201(79)90005-0.","startPage":"331","endPage":"336","numberOfPages":"6","costCenters":[],"links":[{"id":222138,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":267348,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/0031-9201(79)90005-0"}],"volume":"19","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a3964e4b0c8380cd618e5","contributors":{"authors":[{"text":"Davis, P.M.","contributorId":15229,"corporation":false,"usgs":true,"family":"Davis","given":"P.M.","email":"","affiliations":[],"preferred":false,"id":363557,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Stacey, F.D.","contributorId":59176,"corporation":false,"usgs":true,"family":"Stacey","given":"F.D.","email":"","affiliations":[],"preferred":false,"id":363559,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Zablocki, C.J.","contributorId":52178,"corporation":false,"usgs":true,"family":"Zablocki","given":"C.J.","affiliations":[],"preferred":false,"id":363558,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Olson, J.V.","contributorId":71836,"corporation":false,"usgs":true,"family":"Olson","given":"J.V.","email":"","affiliations":[],"preferred":false,"id":363560,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
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