{"pageNumber":"413","pageRowStart":"10300","pageSize":"25","recordCount":11385,"records":[{"id":45134,"text":"pp354JK - 1961 - Lituyapecten (new subgenus of Patinopecten) from Alaska and California; stratigraphic occurrence of Lituyapecten in Alaska","interactions":[],"lastModifiedDate":"2012-02-02T00:10:55","indexId":"pp354JK","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1961","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"354","chapter":"J,K","title":"Lituyapecten (new subgenus of Patinopecten) from Alaska and California; stratigraphic occurrence of Lituyapecten in Alaska","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Shorter contributions to general geology, 1959","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"ENGLISH","doi":"10.3133/pp354JK","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1961, Lituyapecten (new subgenus of Patinopecten) from Alaska and California; stratigraphic occurrence of Lituyapecten in Alaska: U.S. Geological Survey Professional Paper 354, 249 p., 43 leaves of plates : ill., map ; 29 cm. , https://doi.org/10.3133/pp354JK.","productDescription":"249 p., 43 leaves of plates : ill., map ; 29 cm. ","costCenters":[],"links":[{"id":168968,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0354j-k/report-thumb.jpg"},{"id":82269,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0354j-k/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a61e4b07f02db635b49","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":531556,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":43366,"text":"ofr61101 - 1961 - Geology of the Malaspina district, Gulf of Alaska Tertiary province, Alaska","interactions":[],"lastModifiedDate":"2012-02-02T00:10:09","indexId":"ofr61101","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1961","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":"61-101","title":"Geology of the Malaspina district, Gulf of Alaska Tertiary province, Alaska","language":"ENGLISH","doi":"10.3133/ofr61101","usgsCitation":"Miller, D.J., 1961, Geology of the Malaspina district, Gulf of Alaska Tertiary province, Alaska: U.S. Geological Survey Open-File Report 61-101, 1 map, https://doi.org/10.3133/ofr61101.","productDescription":"1 map","costCenters":[],"links":[{"id":106310,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_7987.htm","linkFileType":{"id":5,"text":"html"},"description":"7987"},{"id":162520,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":99056,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1961/0101/plate-1.pdf","size":"13461","linkFileType":{"id":1,"text":"pdf"}},{"id":99057,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1961/0101/plate-2.pdf","size":"4364","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4acce4b07f02db67ea5b","contributors":{"authors":[{"text":"Miller, Don John","contributorId":77120,"corporation":false,"usgs":true,"family":"Miller","given":"Don","email":"","middleInitial":"John","affiliations":[],"preferred":false,"id":228099,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":43365,"text":"ofr61100 - 1961 - Geology of the Lituya district, Gulf of Alaska Tertiary Province, Alaska","interactions":[],"lastModifiedDate":"2012-02-02T00:10:09","indexId":"ofr61100","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1961","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":"61-100","title":"Geology of the Lituya district, Gulf of Alaska Tertiary Province, Alaska","language":"ENGLISH","doi":"10.3133/ofr61100","usgsCitation":"Miller, D.J., 1961, Geology of the Lituya district, Gulf of Alaska Tertiary Province, Alaska: U.S. Geological Survey Open-File Report 61-100, 1 map, https://doi.org/10.3133/ofr61100.","productDescription":"1 map","costCenters":[],"links":[{"id":162519,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":81100,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1961/0100/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b23e4b07f02db6ae11d","contributors":{"authors":[{"text":"Miller, Don John","contributorId":77120,"corporation":false,"usgs":true,"family":"Miller","given":"Don","email":"","middleInitial":"John","affiliations":[],"preferred":false,"id":228098,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":43363,"text":"ofr6199 - 1961 - Geology of the Katalla district, Gulf of Alaska Tertiary province, Alaska","interactions":[],"lastModifiedDate":"2022-04-05T20:20:50.001887","indexId":"ofr6199","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1961","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":"61-99","title":"Geology of the Katalla district, Gulf of Alaska Tertiary province, Alaska","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr6199","usgsCitation":"Miller, D.J., 1961, Geology of the Katalla district, Gulf of Alaska Tertiary province, Alaska: U.S. Geological Survey Open-File Report 61-99, 2 Plates: 28.90 × 41.88 inches and 28.78 × 35.96 inches, https://doi.org/10.3133/ofr6199.","productDescription":"2 Plates: 28.90 × 41.88 inches and 28.78 × 35.96 inches","costCenters":[],"links":[{"id":398149,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_8013.htm"},{"id":81095,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1961/0099/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":81094,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1961/0099/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":162517,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"96000","country":"United States","state":"Alaska","otherGeospatial":"Katalla district","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -144.75,\n              59.783\n            ],\n            [\n              -143.583,\n              59.783\n            ],\n            [\n              -143.583,\n              60.586\n            ],\n            [\n              -144.75,\n              60.586\n            ],\n            [\n              -144.75,\n              59.783\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4acee4b07f02db67fb54","contributors":{"authors":[{"text":"Miller, Don John","contributorId":77120,"corporation":false,"usgs":true,"family":"Miller","given":"Don","email":"","middleInitial":"John","affiliations":[],"preferred":false,"id":228096,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70220634,"text":"70220634 - 1961 - An aeromagnetic profile from anchorage to Nome, Alaska","interactions":[],"lastModifiedDate":"2021-05-21T17:35:10.663879","indexId":"70220634","displayToPublicDate":"1961-12-31T12:31:47","publicationYear":"1961","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1808,"text":"Geophysics","active":true,"publicationSubtype":{"id":10}},"title":"An aeromagnetic profile from anchorage to Nome, Alaska","docAbstract":"<p><span>A total-intensity&nbsp;</span><span class=\"ScopusTermHighlight\">profile</span><span>&nbsp;was obtained on a 500-mile flight by a U. S. Geological Survey airplane from&nbsp;</span><span class=\"ScopusTermHighlight\">Anchorage</span><span>&nbsp;to&nbsp;</span><span class=\"ScopusTermHighlight\">Nome</span><span>,&nbsp;</span><span class=\"ScopusTermHighlight\">Alaska</span><span>, on May 4, 1954. The average flight altitude was 6,000 ft above sea level except over the&nbsp;</span><span class=\"ScopusTermHighlight\">Alaska</span><span>&nbsp;Range where the flight altitude was 9,000 ft. This&nbsp;</span><span class=\"ScopusTermHighlight\">profile</span><span>&nbsp;crossed eight of the major tectonic elements of&nbsp;</span><span class=\"ScopusTermHighlight\">Alaska</span><span>&nbsp;at right angles to their trend and gives valuable regional information in an area where other geophysical and geological information is scarce or lacking. The&nbsp;</span><span class=\"ScopusTermHighlight\">profile</span><span>&nbsp;has a net gradient downward to the northwest, most of which is ascribed to the component of the earth's main magnetic field along the flight traverse. The great variety of magnetic anomalies which are superimposed on this gradient originate from variations in lithology along the traverse. All the magnetic anomalies, except a large one over the Yukon River, are caused by magnetic rocks at or near the surface. The magnetic&nbsp;</span><span class=\"ScopusTermHighlight\">profile</span><span>&nbsp;may be divided into four major segments and nine subsegments, each having a characteristic magnetic pattern. Most of these can be related to a tectonic unit. The large plutons of the Talkeetna geanticline are clearly defined by a group of anomalies having the highest amplitudes of any on the&nbsp;</span><span class=\"ScopusTermHighlight\">profile</span><span>. The Matanuska geosyncline to the east is represented by a 25-mile section of sloping&nbsp;</span><span class=\"ScopusTermHighlight\">profile</span><span>&nbsp;consistent with a thick sedimentary section but indicating that the geosyncline is comparatively narrow near&nbsp;</span><span class=\"ScopusTermHighlight\">Anchorage</span><span>. The 200-mile central magnetic segment is relatively free from all but very minor anomalies. This segment includes the&nbsp;</span><span class=\"ScopusTermHighlight\">Alaska</span><span>&nbsp;Range geosyncline, the Tanana geanticline, and the Kuskokwim geosyncline; showing only slight magnetic contrasts between each of these elements. The two geosynclines either have thick Mesozoic sedimentary sections or have underlying crystalline rocks which are low in magnetic susceptibility at shallow depths. The rocks of the geanticline have a low but not negligible magnetic susceptibility and are predominantly Paleozoic sedimentary rocks. A single 300-gamma anomaly on the west edge of the central segment is caused by a small, mafic intrusive body in the Paleozoic metamorphic rocks of Mt. Hurst. West of this anomaly the&nbsp;</span><span class=\"ScopusTermHighlight\">profile</span><span>&nbsp;consists of a series of small sharp anomalies which are probably caused by Paleozoic metavolcanic rocks of the Ruby geanticline. The second largest anomaly on the&nbsp;</span><span class=\"ScopusTermHighlight\">profile</span><span>&nbsp;is in the Koyukuk geosyncline over the Yukon River. The source is calculated to be more than a mile deep and may be an intrusive body at least 15 miles wide. This anomaly is flanked by 20-mile sections of flat or sloping&nbsp;</span><span class=\"ScopusTermHighlight\">profile</span><span>&nbsp;which indicate areas of thick sedimentary rocks, particularly in the region west of the Yukon River. The 150-mile Norton Sound magnetic segment on the western end of the&nbsp;</span><span class=\"ScopusTermHighlight\">profile</span><span>&nbsp;consists of many closely spaced anomalies produced by rocks which are either volcanic or similar to the Seward complex. Of the four Cenozoic basins or lowlands crossed by the&nbsp;</span><span class=\"ScopusTermHighlight\">profile</span><span>, three are underlain by rocks of moderate to high magnetic susceptibility at shallow depths. These are the Cook Inlet basin, part of which overlaps rocks of the Talkeetna geanticline, the Innoko basin of central&nbsp;</span><span class=\"ScopusTermHighlight\">Alaska</span><span>&nbsp;which overlies the rocks of the Ruby geanticline, and the Norton basin, in which sedimentary deposits are thin or absent. The fourth, the Minchumina basin, is underlain by the low-susceptibility rocks at the Tanana geanticline, which are also probably close to the surface.&nbsp;</span></p>","language":"English","publisher":"Society of Exploration Geophysicists","doi":"10.1190/1.1438945","usgsCitation":"King, E.R., 1961, An aeromagnetic profile from anchorage to Nome, Alaska: Geophysics, v. 26, no. 6, p. 716-726, https://doi.org/10.1190/1.1438945.","productDescription":"11 p.","startPage":"716","endPage":"726","costCenters":[],"links":[{"id":385854,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United  States","state":"Alaska","city":"Nome","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -166.46484375,\n              63.97596090918338\n            ],\n            [\n              -163.740234375,\n              63.97596090918338\n            ],\n            [\n              -163.740234375,\n              65.10914820386473\n            ],\n            [\n              -166.46484375,\n              65.10914820386473\n            ],\n            [\n              -166.46484375,\n              63.97596090918338\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"26","issue":"6","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"King, E. R.","contributorId":93482,"corporation":false,"usgs":true,"family":"King","given":"E.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":816264,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70220626,"text":"70220626 - 1961 - Subaerially carved Arctic seavalley under a modern epicontinental sea","interactions":[],"lastModifiedDate":"2021-05-21T16:05:08.216125","indexId":"70220626","displayToPublicDate":"1961-12-31T10:54:49","publicationYear":"1961","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":5935,"text":"Bulletin of the Geological Society of America","active":true,"publicationSubtype":{"id":10}},"title":"Subaerially carved Arctic seavalley under a modern epicontinental sea","docAbstract":"<p><span class=\"ScopusTermHighlight\">A</span><span>&nbsp;shallow&nbsp;</span><span class=\"ScopusTermHighlight\">seavalley</span><span>, averaging 6 feet in relief, extends from the mouth of Ogotoruk Creek, northwest Alaska, for 15 miles across the floor of the Chukchi&nbsp;</span><span class=\"ScopusTermHighlight\">Sea</span><span>&nbsp;to&nbsp;</span><span class=\"ScopusTermHighlight\">a</span><span>&nbsp;depth of 135 feet. The&nbsp;</span><span class=\"ScopusTermHighlight\">seavalley</span><span>&nbsp;is considered to be&nbsp;</span><span class=\"ScopusTermHighlight\">a</span><span>&nbsp;drowned subaerial valley of Pleistocene age, which was excavated on an eustatically emerged&nbsp;</span><span class=\"ScopusTermHighlight\">epicontinental</span><span>&nbsp;shelf during periods of glacially depressed&nbsp;</span><span class=\"ScopusTermHighlight\">sea</span><span>&nbsp;level.&nbsp;</span></p>","language":"English","publisher":"Geological Society of America","doi":"10.1130/0016-7606(1961)72[1433:SCASUA]2.0.CO;2","usgsCitation":"Scholl, D., and Sainsbury, C., 1961, Subaerially carved Arctic seavalley under a modern epicontinental sea: Bulletin of the Geological Society of America, v. 72, no. 9, p. 1433-1436, https://doi.org/10.1130/0016-7606(1961)72[1433:SCASUA]2.0.CO;2.","productDescription":"4 p.","startPage":"1433","endPage":"1436","costCenters":[],"links":[{"id":385846,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"72","issue":"9","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Scholl, David 0000-0001-6500-6962","orcid":"https://orcid.org/0000-0001-6500-6962","contributorId":204785,"corporation":false,"usgs":true,"family":"Scholl","given":"David","affiliations":[{"id":186,"text":"Coastal and Marine Geology Program","active":true,"usgs":true},{"id":520,"text":"Pacific Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":816252,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Sainsbury, C.L.","contributorId":99968,"corporation":false,"usgs":true,"family":"Sainsbury","given":"C.L.","email":"","affiliations":[],"preferred":false,"id":816253,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70220636,"text":"70220636 - 1961 - Origin of a salt-water lens in permafrost at Kotzebue, Alaska","interactions":[],"lastModifiedDate":"2021-05-21T17:51:04.819618","indexId":"70220636","displayToPublicDate":"1961-12-01T12:44:15","publicationYear":"1961","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":5935,"text":"Bulletin of the Geological Society of America","active":true,"publicationSubtype":{"id":10}},"title":"Origin of a salt-water lens in permafrost at Kotzebue, Alaska","docAbstract":"<p><span>Frozen sediments were found to&nbsp;</span><span class=\"ScopusTermHighlight\">a</span><span>&nbsp;depth of 238 feet&nbsp;</span><span class=\"ScopusTermHighlight\">in</span><span>&nbsp;the drilling of&nbsp;</span><span class=\"ScopusTermHighlight\">a</span><span>&nbsp;325-foot well&nbsp;</span><span class=\"ScopusTermHighlight\">at</span><span>&nbsp;</span><span class=\"ScopusTermHighlight\">Kotzebue</span><span>,&nbsp;</span><span class=\"ScopusTermHighlight\">Alaska</span><span>. Between 79 and 86 feet, however, highly saline water was found&nbsp;</span><span class=\"ScopusTermHighlight\">in</span><span>&nbsp;</span><span class=\"ScopusTermHighlight\">a</span><span>&nbsp;gravel&nbsp;</span><span class=\"ScopusTermHighlight\">lens</span><span>. The writer suggests that the&nbsp;</span><span class=\"ScopusTermHighlight\">salt water</span><span>&nbsp;originated by fractionation by freezing. Analyses of this water and of slightly saline water from below the&nbsp;</span><span class=\"ScopusTermHighlight\">permafrost</span><span>&nbsp;are given.&nbsp;</span></p>","language":"English","publisher":"Geological Society of America","doi":"10.1130/0016-7606(1961)72[1427:OOASLI]2.0.CO;2","usgsCitation":"Cedarstrom, D., 1961, Origin of a salt-water lens in permafrost at Kotzebue, Alaska: Bulletin of the Geological Society of America, v. 72, no. 9, p. 1427-1431, https://doi.org/10.1130/0016-7606(1961)72[1427:OOASLI]2.0.CO;2.","productDescription":"5 p.","startPage":"1427","endPage":"1431","costCenters":[],"links":[{"id":385856,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United  States","state":"Alaska","city":"Kotzebue","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -163.4765625,\n              66.65297740055279\n            ],\n            [\n              -161.630859375,\n              66.65297740055279\n            ],\n            [\n              -161.630859375,\n              67.33986082559095\n            ],\n            [\n              -163.4765625,\n              67.33986082559095\n            ],\n            [\n              -163.4765625,\n              66.65297740055279\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"72","issue":"9","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Cedarstrom, D.J.","contributorId":102127,"corporation":false,"usgs":true,"family":"Cedarstrom","given":"D.J.","email":"","affiliations":[],"preferred":false,"id":816266,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70220633,"text":"70220633 - 1961 - The glacial history of Alaska: It's bearing on paleoclimatic theory","interactions":[],"lastModifiedDate":"2021-05-24T12:44:20.49558","indexId":"70220633","displayToPublicDate":"1961-10-01T12:24:57","publicationYear":"1961","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":801,"text":"Annals of the New York Academy of Sciences","active":true,"publicationSubtype":{"id":10}},"title":"The glacial history of Alaska: It's bearing on paleoclimatic theory","docAbstract":"<p>No abstract available.&nbsp;</p>","language":"English","publisher":"New York Academy of Sciences","doi":"10.1111/j.1749-6632.1961.tb50040.x","usgsCitation":"Karlstrom, T., 1961, The glacial history of Alaska: It's bearing on paleoclimatic theory: Annals of the New York Academy of Sciences, v. 95, no. 1, p. 290-340, https://doi.org/10.1111/j.1749-6632.1961.tb50040.x.","productDescription":"51 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,{"id":70238530,"text":"70238530 - 1961 - Renal coccidiosis in oldsquaws (Clangula hyemalis) from Alaska","interactions":[],"lastModifiedDate":"2022-11-28T18:00:06.670832","indexId":"70238530","displayToPublicDate":"1961-04-01T11:36:18","publicationYear":"1961","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2507,"text":"Journal of Wildlife Diseases","active":true,"publicationSubtype":{"id":10}},"displayTitle":"Renal coccidiosis in oldsquaws (<i>Clangula hyemalis</i>) from Alaska","title":"Renal coccidiosis in oldsquaws (Clangula hyemalis) from Alaska","docAbstract":"<p><span>Renal coccidiosis was found in 4 of 12 oldsquaw ducks (</span><i>Clangula hyemalis</i><span>) collected from the north slope of Alaska and Prince William Sound. Numerous 1 to 2 mm white foci were observed on the kidney surface of one bird. Microscopically, there was distention of renal tubules with oocysts, flattening of tubular epithelium, and interstitial accumulation of mononuclear cells. Kidneys from several other species of sea ducks from Prince William Sound were not infected.</span></p>","language":"English","publisher":"Wildlife Disease Association","doi":"10.7589/0090-3558-17.2.237","usgsCitation":"Franson, J.C., and Derksen, D.V., 1961, Renal coccidiosis in oldsquaws (Clangula hyemalis) from Alaska: Journal of Wildlife Diseases, v. 17, no. 2, p. 237-240, https://doi.org/10.7589/0090-3558-17.2.237.","productDescription":"4 p.","startPage":"237","endPage":"240","costCenters":[{"id":114,"text":"Alaska Science Center","active":true,"usgs":true}],"links":[{"id":480383,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.7589/0090-3558-17.2.237","text":"Publisher Index Page"},{"id":409714,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Alaska","otherGeospatial":"Prince William Sound, Teshekpuk Lake","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -152.85406583172656,\n              70.58233364320773\n            ],\n            [\n              -153.04712731822582,\n              70.65555334208511\n            ],\n            [\n              -153.4056700788673,\n              70.6829422184802\n            ],\n            [\n              -153.45623380152188,\n              70.71788484129243\n            ],\n            [\n              -153.6446985859617,\n              70.74215688350768\n            ],\n            [\n              -154.04461166513872,\n              70.68902356844578\n            ],\n            [\n              -154.14573911044786,\n              70.64641542000794\n            ],\n            [\n              -154.1319490042694,\n              70.5563378253344\n            ],\n            [\n              -153.93429081571054,\n              70.4919693588391\n            ],\n            [\n              -153.7871963498064,\n              70.44740499384741\n            ],\n            [\n              -153.49300741799797,\n              70.43817257466443\n            ],\n            [\n              -153.27236571914162,\n              70.51191478660377\n            ],\n            [\n              -153.05172402028526,\n              70.50577982035688\n            ],\n            [\n              -152.85406583172656,\n              70.58233364320773\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    },\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -148.32202731776306,\n              61.04696225464866\n            ],\n            [\n              -148.32202731776306,\n              60.30986188880047\n            ],\n            [\n              -145.82683744768872,\n              60.30986188880047\n            ],\n            [\n              -145.82683744768872,\n              61.04696225464866\n            ],\n            [\n              -148.32202731776306,\n              61.04696225464866\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","volume":"17","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Franson, J. Christian 0000-0002-0251-4238 jfranson@usgs.gov","orcid":"https://orcid.org/0000-0002-0251-4238","contributorId":177499,"corporation":false,"usgs":true,"family":"Franson","given":"J.","email":"jfranson@usgs.gov","middleInitial":"Christian","affiliations":[{"id":456,"text":"National Wildlife Health Center","active":true,"usgs":true}],"preferred":true,"id":857749,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Derksen, Dirk V. dderksen@usgs.gov","contributorId":2269,"corporation":false,"usgs":true,"family":"Derksen","given":"Dirk","email":"dderksen@usgs.gov","middleInitial":"V.","affiliations":[{"id":117,"text":"Alaska Science Center Biology WTEB","active":true,"usgs":true}],"preferred":true,"id":857750,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70047879,"text":"70047879 - 1961 - Correlation of tertiary formations of Alaska","interactions":[{"subject":{"id":40091,"text":"ofr6098 - 1960 - Correlation of the Tertiary rocks of Alaska","indexId":"ofr6098","publicationYear":"1960","noYear":false,"title":"Correlation of the Tertiary rocks of Alaska"},"predicate":"SUPERSEDED_BY","object":{"id":70047879,"text":"70047879 - 1961 - Correlation of tertiary formations of Alaska","indexId":"70047879","publicationYear":"1961","noYear":false,"title":"Correlation of tertiary formations of Alaska"},"id":1}],"lastModifiedDate":"2023-02-01T14:35:20.257242","indexId":"70047879","displayToPublicDate":"1961-01-01T15:06:00","publicationYear":"1961","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":701,"text":"American Association of Petroleum Geologists Bulletin","active":true,"publicationSubtype":{"id":10}},"title":"Correlation of tertiary formations of Alaska","docAbstract":"Recent stratigraphic and paleontologic studies have resulted in substantial revision of the age assignments and inter-basin correlations of the Tertiary formations of Alaska as given in both an earlier compilation by P. S. Smith (1939) and a tentative chart prepared for distribution at the First International Symposium on Arctic Geology at Calgary, Alberta (Miller, MacNeil, and Wahrhaftig, 1960). Current work in Alaska by the U. S. Geological Survey and several oil companies is furnishing new information at a rapid rate and further revisions may be expected. The correlation chart (Fig. 1), the first published chart to deal exclusively with the Tertiary of Alaska, had the benefit of a considerable amount of stratigraphic data and fossil collections from some oil companies, but recent surface mapping and drilling by other oil companies in several Tertiary basins undoubtedly must have produced much more information. Nevertheless, the extent of available data justifies the publication of a revised correlation chart at this time.","language":"English","publisher":"American Association of Petroleum Geologists","doi":"10.1306/BC743735-16BE-11D7-8645000102C1865D","usgsCitation":"MacNeil, F., Wolfe, J.A., Miller, D.J., and Hopkins, D., 1961, Correlation of tertiary formations of Alaska: American Association of Petroleum Geologists Bulletin, v. 45, no. 11, p. 1801-1809, https://doi.org/10.1306/BC743735-16BE-11D7-8645000102C1865D.","productDescription":"9 p.","startPage":"1801","endPage":"1809","costCenters":[],"links":[{"id":277127,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United 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