{"pageNumber":"6646","pageRowStart":"166125","pageSize":"25","recordCount":184689,"records":[{"id":70112253,"text":"70112253 - 1965 - Photointerpretation of Alaskan post-earthquake photography","interactions":[],"lastModifiedDate":"2017-03-27T13:40:15","indexId":"70112253","displayToPublicDate":"1990-06-12T09:35:00","publicationYear":"1965","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3051,"text":"Photogrammetric Engineering","active":true,"publicationSubtype":{"id":10}},"title":"Photointerpretation of Alaskan post-earthquake photography","docAbstract":"<p>Aerial photographs taken after the March 27, 1964, Good Friday, Alaskan earthquake were examined stereoscopically to determine effects of the earthquake in areas remote from the towns, highways, and the railroad.  The two thousand black and white photographs used in this study were taking in April, after the earthquake, by the U. S. Coast & Geodetic Survey and were generously supplied to the U. S. Geological Survey.  Part of the photographs, at a scale of 1/24,000, provide blanket coverage of approximately 2,000 square miles of land area north and west of Prince William Sound, including parts of the mainland and some of the adjacent islands.  The epicenter of the earthquake, near the head of Unakwik Inlet, is located in this area.  The rest of the photographs, at scales ranging from 1/17,000 to 1/40,000, cover isolated strips of the coastline of the mainland and nearby islands in the general area of Prince William Sound.</p>\n<br/>\n<p>Figure 1 shows the area of new photo coverage used in this study.  The objective of the study was to determine quickly whether geological features resulting from the earthquake, such as faults, changes in shoreline, cracks in surficial material, pressure ridges in lake ice, fractures in glaciers and lake ice, and rock slides and avalanches, might be identifiable by photointerpretation.  The study was made without benefit of comparisons with older, or pre-earthquake photography, which was not readily available for immediate use.</p>","language":"English","publisher":"American Society of Photogrammetry","publisherLocation":"Falls Church, VA","usgsCitation":"Hackman, R., 1965, Photointerpretation of Alaskan post-earthquake photography: Photogrammetric Engineering, v. 31, no. 4, p. 604-610.","productDescription":"7 p.","startPage":"604","endPage":"610","numberOfPages":"7","costCenters":[{"id":222,"text":"Earth Resources Observation and Science (EROS) Center","active":true,"usgs":true}],"links":[{"id":288442,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Alaska","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -150.0122,59.6906 ], [ -150.0122,61.8408 ], [ -144.9482,61.8408 ], [ -144.9482,59.6906 ], [ -150.0122,59.6906 ] ] ] } } ] }","volume":"31","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"539acc05e4b0e83db6d08f77","contributors":{"authors":[{"text":"Hackman, R.J.","contributorId":95086,"corporation":false,"usgs":true,"family":"Hackman","given":"R.J.","email":"","affiliations":[],"preferred":false,"id":686346,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70112252,"text":"70112252 - 1965 - Geological exploration from orbital altitudes","interactions":[],"lastModifiedDate":"2017-03-27T13:39:05","indexId":"70112252","displayToPublicDate":"1990-06-12T09:18:00","publicationYear":"1965","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1829,"text":"Geotimes","active":true,"publicationSubtype":{"id":10}},"title":"Geological exploration from orbital altitudes","docAbstract":"The National Aeronautics & Space Administration is planning geologic exploration from orbiting spacecraft. For that purpose it is evaluating new and refined exploration tools, often called remote sensors, including devices that are sensitive to force fields, such as gravity gradient systems, and devices that record the reflection or emission of electromagnetic energy. Both passive electromagnetic sensors (those that rely on natural sources of illumination, such as the Sun) and active electromagnetic sensors (which use an artificial source of illumination) are being considered.","language":"English","publisher":"American Geological Institute","publisherLocation":"Alexandria, VA","usgsCitation":"Badgley, P.C., Fischer, W., and Lyon, R.J., 1965, Geological exploration from orbital altitudes: Geotimes, v. 10, no. 2, p. 11-14.","productDescription":"5 p.","startPage":"11","endPage":"14","numberOfPages":"5","costCenters":[{"id":222,"text":"Earth Resources Observation and Science (EROS) Center","active":true,"usgs":true}],"links":[{"id":288438,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"10","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"539acc00e4b0e83db6d08f43","contributors":{"authors":[{"text":"Badgley, Peter C.","contributorId":33625,"corporation":false,"usgs":true,"family":"Badgley","given":"Peter","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":494579,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Fischer, William A.","contributorId":47787,"corporation":false,"usgs":true,"family":"Fischer","given":"William A.","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":494580,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Lyon, Ronald J. P.","contributorId":75067,"corporation":false,"usgs":true,"family":"Lyon","given":"Ronald","email":"","middleInitial":"J. P.","affiliations":[],"preferred":false,"id":494581,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70106998,"text":"70106998 - 1965 - Water resources data for Indiana, 1965","interactions":[],"lastModifiedDate":"2014-06-02T06:09:13","indexId":"70106998","displayToPublicDate":"1966-01-01T14:16:00","publicationYear":"1965","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"IN-65-1","title":"Water resources data for Indiana, 1965","docAbstract":"<p>The surface-water records for the 1965 water year for gaging stations, partial-record stations, and miscellaneous sites within the State of Indiana are given in this report. For convenience there are also included records for a few pertinent gaging stations in bordering States. The records were collected and computed by the Water Resources Division of the U.S. Geological Survey, under the direction of Malcolm D. Hale, district engineer, Surface Water Branch.</p>\n<br/>\n<p>This report marks the beginning of a new method of presenting, annually, basic data on surface-water records by States. Through September 30, 1960, the records of discharge and stage of streams and contents and stage of lakes or reservoirs were published in an annual series of U.S. Geological Survey water-supply papers entitled \"Surface Water Supply of the United States.\" Since 1951 there have been 20 volumes in the series; each volume covered an area whose boundaries coincided with those of certain natural drainage areas. The records in Indiana were contained in Parts 3A, 4 and 5 of that series.</p>\n<br/>\n<p>Beginning with the 1961 water year, streamflow records and related data will be released by the Geological Survey in annual reports on a State-boundary basis. Distribution of these basic-data reports will be limited and primarily for local needs. The records later will be published in Geological Survey water-supply papers at 5-year intervals. These 5-year water-supply papers will show daily discharge and will be compiled on the same geographical areas previously used for the annual series; however, some of the 14 parts of coterminous United States will be further subdivided.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/70106998","collaboration":"Prepared in cooperation with Indiana Department of Natural Resources; Indiana State Board of Health; Indiana State Highway Commission; Corps of Engineers, U.S. Army","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1965, Water resources data for Indiana, 1965: U.S. Geological Survey Water Data Report IN-65-1, viii, 249 p., https://doi.org/10.3133/70106998.","productDescription":"viii, 249 p.","numberOfPages":"258","temporalStart":"1964-10-01","temporalEnd":"1965-09-30","costCenters":[{"id":629,"text":"Water Resources Division","active":false,"usgs":true}],"links":[{"id":287928,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":287927,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/unnumbered/70106998/report.pdf"}],"country":"United States","state":"Indiana","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -88.0979,37.7717 ], [ -88.0979,41.7607 ], [ -84.7847,41.7607 ], [ -84.7847,37.7717 ], [ -88.0979,37.7717 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"537b280de4b0929ba496abd5","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":535655,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70207281,"text":"70207281 - 1965 - Osmotic equilibrium and overthrust faulting","interactions":[],"lastModifiedDate":"2019-12-15T16:22:01","indexId":"70207281","displayToPublicDate":"1965-12-31T16:15:09","publicationYear":"1965","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1786,"text":"Geological Society of America Bulletin","active":true,"publicationSubtype":{"id":10}},"title":"Osmotic equilibrium and overthrust faulting","docAbstract":"<p><span>The two principal suggested modes of facilitating overthrust faulting are (1) lubrication at the sole by evaporite beds or micaceous shales and (2) flotation due to anomalously high (&gt; hydrostatic) pore-water pressures. Past rapid sedimentation and tectonic compression have been suggested as important causes of anomalously high water pressure (Hubbert and Rubey, 1959). We suggest osmosis as another important possibility. Field data on shale beds and experimental studies on compacted clays show that such material can act as semipermeable membranes that greatly retard passage of dissolved electrolytes relative to H</span><sub>2</sub><span>O. Equilibrium osmotic pressure, π, across an ideal membrane is given by (a, activity; V</span><sub>H2O</sub><sup>0</sup><sub>1</sub><span>, molar volume of distilled water). At 80°C, π is 470 bars between saturated halite solution and distilled water; it is 360 bars between saturated and 10 per cent solutions. At 25°C the values are 20 per cent lower. Other dissolved components, if present in similar proportions, will enhance the effect. Anomalous water pressures of at least 400 bars above hydrostatic have been measured in oil wells; many of these wells penetrate evaporites and/or shales which separate formation waters of differing salt concentrations. These pressures are explicable by assuming osmotic equilibrium across a membrane which separates saturated halite solution from solutions up to 10 weight per cent NaCl. Thus, osmotic equilibrium may be an important mechanism for floating thrust sheets. Lubrication of thrust sheets by shales or evaporites and flotation by anomalously high pressures may be simply different manifestations of the same geologic milieu. © 1965, The Geological Society of America, Inc.</span></p>","language":"English","publisher":"Geological Society of America","doi":"10.1130/0016-7606(1965)76[1379:OEAOF]2.0.CO;2","issn":"00167606","usgsCitation":"Hanshaw, B., and Zen, E., 1965, Osmotic equilibrium and overthrust faulting: Geological Society of America Bulletin, v. 76, no. 12, p. 1379-1385, https://doi.org/10.1130/0016-7606(1965)76[1379:OEAOF]2.0.CO;2.","productDescription":"7 p. ","startPage":"1379","endPage":"1385","costCenters":[],"links":[{"id":370288,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"76","issue":"12","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Hanshaw, B.B.","contributorId":25928,"corporation":false,"usgs":true,"family":"Hanshaw","given":"B.B.","email":"","affiliations":[],"preferred":false,"id":777530,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Zen, E-An","contributorId":47064,"corporation":false,"usgs":true,"family":"Zen","given":"E-An","email":"","affiliations":[],"preferred":false,"id":777531,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70208785,"text":"70208785 - 1965 - Late quaternary geologic history of the lower Chippewa Valley, Wisconsin","interactions":[],"lastModifiedDate":"2020-02-28T11:01:40","indexId":"70208785","displayToPublicDate":"1965-12-31T10:55:42","publicationYear":"1965","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":"Late quaternary geologic history of the lower Chippewa Valley, Wisconsin","docAbstract":"<p><span>The lower Chippewa Valley in west-central Wisconsin extends 65 miles from the Cary terminal moraine in Chippewa County to the Mississippi River Valley. The Chippewa Valley and its tributaries were filled with a valley train of sand and gravel during the maximum stand of the Cary ice, and entrenchment of this deposit has formed the Wissota terrace, a prominent geomorphic feature that can be traced the length of the valley. Several lower terraces in the valley indicate progressive downcutting of the Wissota terrace sediments. Erosion and deposition in the Mississippi Valley are closely linked to the post-Cary history of the lower Chippewa Valley, for these factors controlled the outlet level of the Chippewa River. This outlet was substantially lower than at present throughout much of post-Cary Pleistocene and early Recent time. The modern Chippewa River has built a delta into the Mississippi Valley. The Chippewa River is aggrading the lower part of its valley, a meandering river is slowly eroding the central part; stream erosion in the upper part is restricted by sills of hard bedrock.</span></p>","language":"English","publisher":"Geological Society of America","doi":"10.1130/0016-7606(1965)76[113:LQGHOT]2.0.CO;2","usgsCitation":"Andrews, G., 1965, Late quaternary geologic history of the lower Chippewa Valley, Wisconsin: Bulletin of the Geological Society of America, v. 76, no. 1, p. 113-124, https://doi.org/10.1130/0016-7606(1965)76[113:LQGHOT]2.0.CO;2.","productDescription":"12 p.","startPage":"113","endPage":"124","costCenters":[],"links":[{"id":372739,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Wisconsin","otherGeospatial":"Lower Chippewa Valley","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -92.36480712890625,\n              44.22552029849434\n            ],\n            [\n              -91.01348876953125,\n              44.22552029849434\n            ],\n            [\n              -91.01348876953125,\n              45.14911623279028\n            ],\n            [\n              -92.36480712890625,\n              45.14911623279028\n            ],\n            [\n              -92.36480712890625,\n              44.22552029849434\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"76","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Andrews, George W.","contributorId":40621,"corporation":false,"usgs":true,"family":"Andrews","given":"George W.","affiliations":[],"preferred":false,"id":783380,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70207357,"text":"70207357 - 1965 - Solute erosion and chloride balance in selected river basins of the western conterminous United States","interactions":[],"lastModifiedDate":"2019-12-18T19:48:13","indexId":"70207357","displayToPublicDate":"1965-12-31T10:20:30","publicationYear":"1965","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3722,"text":"Water Resources Research","onlineIssn":"1944-7973","printIssn":"0043-1397","active":true,"publicationSubtype":{"id":10}},"title":"Solute erosion and chloride balance in selected river basins of the western conterminous United States","docAbstract":"<p><span>The estimated average rates of annual solute erosion in 11 important western river basins range from 180 tons per square mile (Willamette basin) to 4.2 tons per square mile (Gila basin). An average rate of 58 tons per square mile is indicated for the entire 545,000‐square‐mile area drained by the 11 rivers. The wide range in tonnage is the result of a complex of causes, among which differences in geology, gross climatic environments, and activities of man are the most important. Rates of solute erosion are highest in areas of abundant precipitation and runoff, in contrast to rates of suspended‐sediment removal, which are characteristically highest in basins subjected to only 10–15 inches of effective annual precipitation. Tonnages of chloride brought into the 11 river basins by rain and snow make up an equivalent of about 1.6 to about 17% of the chloride removed in runoff during an average year. The range of percentages reflects differences in the relative importance of oceanic and continental solute contributions. This paper is not subject to U.S. copyright. Published in 1965 by the American Geophysical Union.</span></p>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/WR001i004p00537","issn":" 00431397","usgsCitation":"Van Denburgh, A.S., and Feth, J.H., 1965, Solute erosion and chloride balance in selected river basins of the western conterminous United States: Water Resources Research, v. 1, no. 4, p. 537-541, https://doi.org/10.1029/WR001i004p00537.","productDescription":"5 p.","startPage":"537","endPage":"541","costCenters":[],"links":[{"id":370439,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -128.32031249999997,\n              22.59372606392931\n            ],\n            [\n              -66.4453125,\n              22.59372606392931\n            ],\n            [\n              -66.4453125,\n              50.064191736659104\n            ],\n            [\n              -128.32031249999997,\n              50.064191736659104\n            ],\n            [\n              -128.32031249999997,\n              22.59372606392931\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"1","issue":"4","noUsgsAuthors":false,"publicationDate":"2010-07-09","publicationStatus":"PW","contributors":{"authors":[{"text":"Van Denburgh, A. S.","contributorId":23928,"corporation":false,"usgs":true,"family":"Van Denburgh","given":"A.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":777801,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Feth, J. H.","contributorId":50495,"corporation":false,"usgs":true,"family":"Feth","given":"J.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":777802,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70206891,"text":"70206891 - 1965 - Beer can and milk bottle geology","interactions":[],"lastModifiedDate":"2019-11-26T10:08:45","indexId":"70206891","displayToPublicDate":"1965-12-31T10:04:28","publicationYear":"1965","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":5890,"text":"Undersea Technology","printIssn":"0041-6533","active":false,"publicationSubtype":{"id":10}},"title":"Beer can and milk bottle geology","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"Sheffield Publishing Co.","usgsCitation":"Manheim, F.T., 1965, Beer can and milk bottle geology: Undersea Technology, v. 6, p. 22-25.","productDescription":"7 p.","startPage":"22","endPage":"25","costCenters":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"links":[{"id":369620,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"6","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Manheim, Frank T. 0000-0003-4005-4524","orcid":"https://orcid.org/0000-0003-4005-4524","contributorId":20770,"corporation":false,"usgs":true,"family":"Manheim","given":"Frank","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":776169,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70197612,"text":"70197612 - 1965 - Ordovician, Silurian, and Devonian biostratigraphy of east-central Alaska","interactions":[],"lastModifiedDate":"2023-02-01T14:25:21.059833","indexId":"70197612","displayToPublicDate":"1965-12-31T00:00:00","publicationYear":"1965","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":"Ordovician, Silurian, and Devonian biostratigraphy of east-central Alaska","docAbstract":"<p>A predominantly shale and chert sequence has been mapped from the Canadian border at Latitude 65°00′ N. to the Nation River about 25 miles northwest. It has Ordovician and Silurian graptolites in the lower half, and Middle Devonian corals and Upper Devonian spores in the upper half.</p><p>The lower half of the sequence consists of about 400 to 900 feet of predominantly dark gray graptolitic shale with lesser amounts of grayish black laminated chert. This unit has been traced by Green and Roddick from the international border southeastward into the Dawson area of the Yukon Territory and northeastward into the Ogilvie and Richardson Mountains where it has been mapped by Jackson &amp; Lenz, Norris, and others as the Road River Formation. In the Tatonduk-Nation Rivers area the Road River Formation rests disconformably on a sequence of Middle and Upper Cambrian limestone that locally may include Lower Ordovician (Tremadoc) beds at its top. The sequence of graptolite faunas from the Road River Formation in Alaska is essentially the same as the graptolite zones established by Elles and Wood in Great Britain. All the standard series of the Ordovician and Silurian are probably represented in the formation with the exception of the Tremadoc and possibly the Arenig and Wenlock.</p><p>Overlying the Road River Formation is a formation, 200 to 800 feet thick, consisting predominantly of thinly bedded and laminated light gray to black chert and siliceous shale that is here named the McCann Hill Chert. This new formation disconformably overlies the Road River Formation, and its lower boundary is at the base of a distinctive limestone and shale member. The basal limestone and shale member of the McCann Hill Chert contains a remarkably varied fauna including corals, brachiopods, trilobites, conodonts, ostracods, and fish of Eifelian (early Middle Devonian) age. Spores from the upper part of the formation resemble those from the overlying Nation River Formation and indicate a Late Devonian age. The McCann Hill Chert is conformably overlain by the Nation River Formation—a thick succession of inter-bedded graywacke, chert conglomerate, and silty shale of Late Devonian age.</p><p>In the vicinity of Jones Ridge, only 7 miles north of exposures of the Road River Formation, Upper Cambrian limestone is overlain by a pure limestone section containing Ordovician, Middle Devonian, and perhaps Silurian shelly faunas contemporaneous with the Road River Formation and the thinner basal limestone and shale member of the McCann Hill Chert. The rapid change from graptolitic shale to limestone probably reflects changes in conditions of sedimentation, but could be a result of thrust faulting.</p><p>The Tatonduk-Nation Rivers area seems to lie in a transitional zone between an early Paleozoic eugeosynclinal belt south of the Yukon River and a contemporaneous miogeosynclinal belt along the Porcupine River. One puzzling feature of the lower Paleozoic sequence in the Tatonduk-Nation Rivers area is its thinness in contrast to the much thicker volcanic and detrital sequence on the south and the considerably thicker carbonate sequence on the north.</p>","language":"English","publisher":"American Association of Petroleum Geologists","doi":"10.1306/A6633526-16C0-11D7-8645000102C1865D","usgsCitation":"Churkin, M., and Brabb, E.E., 1965, Ordovician, Silurian, and Devonian biostratigraphy of east-central Alaska: American Association of Petroleum Geologists Bulletin, v. 49, no. 2, p. 172-185, https://doi.org/10.1306/A6633526-16C0-11D7-8645000102C1865D.","productDescription":"14 p.","startPage":"172","endPage":"185","costCenters":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"links":[{"id":355007,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Alaska","otherGeospatial":"Nation-Tatonduk Rivers area","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -142.38695878694335,\n              65.46836165464507\n            ],\n            [\n              -142.38695878694335,\n              64.62502455781637\n            ],\n            [\n              -141.00230856836862,\n              64.62502455781637\n            ],\n            [\n              -141.00230856836862,\n              65.46836165464507\n            ],\n            [\n              -142.38695878694335,\n              65.46836165464507\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","volume":"49","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Churkin, Michael Jr.","contributorId":62566,"corporation":false,"usgs":true,"family":"Churkin","given":"Michael","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":737908,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Brabb, Earl E.","contributorId":8545,"corporation":false,"usgs":true,"family":"Brabb","given":"Earl","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":737909,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70010525,"text":"70010525 - 1965 - Artifact from deposits of mid-Wisconsin age in Illinois","interactions":[],"lastModifiedDate":"2026-02-10T17:47:54.961494","indexId":"70010525","displayToPublicDate":"1965-12-24T00:00:00","publicationYear":"1965","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3338,"text":"Science","active":true,"publicationSubtype":{"id":10}},"title":"Artifact from deposits of mid-Wisconsin age in Illinois","docAbstract":"Discovery of an artifact of human manufacture imbedded in Roxana loess, classed as Altonian substage of the Wisconsin stage of the Pleistocene, of an age of 35,000 to 40,000 years, contributes to the determination of the age of man in the New World.","language":"English","publisher":"American Association for the Advancement of Science","doi":"10.1126/science.150.3704.1722","issn":"00368075","usgsCitation":"Munson, P., and Frye, J., 1965, Artifact from deposits of mid-Wisconsin age in Illinois: Science, v. 150, no. 3704, p. 1722-1723, https://doi.org/10.1126/science.150.3704.1722.","productDescription":"2 p.","startPage":"1722","endPage":"1723","costCenters":[],"links":[{"id":219620,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United 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,{"id":70010805,"text":"70010805 - 1965 - Vertical density currents","interactions":[],"lastModifiedDate":"2026-02-10T17:53:22.686693","indexId":"70010805","displayToPublicDate":"1965-12-10T00:00:00","publicationYear":"1965","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3338,"text":"Science","active":true,"publicationSubtype":{"id":10}},"title":"Vertical density currents","docAbstract":"These currents seem to carry particles downward much more rapidly than settling according to Stokes's law.","language":"English","publisher":"AAAS","doi":"10.1126/science.150.3702.1423","issn":"00368075","usgsCitation":"Bradley, W.H., 1965, Vertical density currents: Science, v. 150, no. 3702, p. 1423-1428, https://doi.org/10.1126/science.150.3702.1423.","productDescription":"6 p.","startPage":"1423","endPage":"1428","costCenters":[],"links":[{"id":499714,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"150","issue":"3702","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bc231e4b08c986b32a9b5","contributors":{"authors":[{"text":"Bradley, W. H.","contributorId":102452,"corporation":false,"usgs":true,"family":"Bradley","given":"W.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":359688,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70221187,"text":"70221187 - 1965 - Solubility measurements in the system CaSO4-NaCL-H2O at 35°, 50°, and 70°cand one atmosphere pressure","interactions":[],"lastModifiedDate":"2021-06-04T18:15:18.43742","indexId":"70221187","displayToPublicDate":"1965-12-01T13:11:47","publicationYear":"1965","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2420,"text":"Journal of Petrology","active":true,"publicationSubtype":{"id":10}},"title":"Solubility measurements in the system CaSO4-NaCL-H2O at 35°, 50°, and 70°cand one atmosphere pressure","docAbstract":"<p><span>The solubilities&nbsp;</span>in<span>&nbsp;the&nbsp;</span>system<span>&nbsp;CaSO</span><sub>4</sub><span>-</span>NaCl<span>-H</span><sub>2</sub><span>O,&nbsp;</span>at<span>&nbsp;1 atm&nbsp;</span>pressure<span>&nbsp;and&nbsp;</span>35°<span>,&nbsp;</span>50°<span>, and 70°C, have been determined by approaching the&nbsp;</span>solubility<span>&nbsp;curves from both the undersaturation and supersaturation sides. The experimental runs are of long duration, as much as 3 months; these rates should be commensurate with those of the appropriate geological processes, and so the results should be directly applicable to the interpretation of evaporite deposits.&nbsp;</span></p>","language":"English","publisher":"Oxford University Press","doi":"10.1093/petrology/6.1.124","usgsCitation":"Zen, E., 1965, Solubility measurements in the system CaSO4-NaCL-H2O at 35°, 50°, and 70°cand one atmosphere pressure: Journal of Petrology, v. 6, no. 1, p. 124-164, https://doi.org/10.1093/petrology/6.1.124.","productDescription":"41 p.","startPage":"124","endPage":"164","costCenters":[],"links":[{"id":386232,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"6","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Zen, E-An","contributorId":47064,"corporation":false,"usgs":true,"family":"Zen","given":"E-An","email":"","affiliations":[],"preferred":false,"id":817019,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70010461,"text":"70010461 - 1965 - Titanium dioxide in pyroclastic layers from volcanoes in the Cascade Range","interactions":[],"lastModifiedDate":"2026-02-10T17:59:26.40999","indexId":"70010461","displayToPublicDate":"1965-11-19T00:00:00","publicationYear":"1965","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3338,"text":"Science","active":true,"publicationSubtype":{"id":10}},"title":"Titanium dioxide in pyroclastic layers from volcanoes in the Cascade Range","docAbstract":"<p><span>Rapid determinations of titanium dioxide have been made by x-ray emission techniques to evaluate the potentiality of using the TiO</span><sub>2</sub><span>&nbsp;content of samples for checking field correlations and assisting in identification of pyroclastic units from Cascade volcanoes. Preliminary data suggest that the two most widespread units have characteristic ranges of TiO</span><sub>2</sub><span>&nbsp;content and that other, less extensive layers have ranges which, though characteristic, often overlap the ranges of the more widespread layers. Relative to fresh samples, weathered samples from B and C soil horizons are enriched in TiO</span><sub>2</sub><span>.</span></p>","language":"English","publisher":"American Association for the Advancement of Science","doi":"10.1126/science.150.3699.1022","issn":"00368075","usgsCitation":"Czamanske, G., and Porter, S., 1965, Titanium dioxide in pyroclastic layers from volcanoes in the Cascade Range: Science, v. 150, no. 3699, p. 1022-1025, https://doi.org/10.1126/science.150.3699.1022.","productDescription":"4 p.","startPage":"1022","endPage":"1025","costCenters":[],"links":[{"id":218952,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","otherGeospatial":"Cascade Range","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -126.3113698578322,\n              49.01003876424767\n            ],\n            [\n              -126.3113698578322,\n              38.60286391280661\n            ],\n            [\n              -121.31055440730346,\n              38.60286391280661\n            ],\n            [\n              -121.31055440730346,\n              49.01003876424767\n            ],\n            [\n              -126.3113698578322,\n              49.01003876424767\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","volume":"150","issue":"3699","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bb423e4b08c986b3261e0","contributors":{"authors":[{"text":"Czamanske, G.K.","contributorId":26300,"corporation":false,"usgs":true,"family":"Czamanske","given":"G.K.","email":"","affiliations":[],"preferred":false,"id":358975,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Porter, S.C.","contributorId":35066,"corporation":false,"usgs":true,"family":"Porter","given":"S.C.","email":"","affiliations":[],"preferred":false,"id":358976,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70221188,"text":"70221188 - 1965 - Report on S.E.G. Symposium on the chemistry of the ore-forming fluids August-September,1964","interactions":[],"lastModifiedDate":"2021-06-04T18:23:09.4074","indexId":"70221188","displayToPublicDate":"1965-11-01T13:20:38","publicationYear":"1965","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1472,"text":"Economic Geology","active":true,"publicationSubtype":{"id":10}},"title":"Report on S.E.G. Symposium on the chemistry of the ore-forming fluids August-September,1964","docAbstract":"<p><span>Sessions included presentations and discussions of the following topics: mineral stability and phase assemblages at&nbsp;</span>ore<span>-</span>forming<span>&nbsp;temperatures and pressures; high-temperature solution&nbsp;</span>chemistry<span>&nbsp;of sulfides, carbonates, and silicates, with consideration of complexing and stability, and the generation of&nbsp;</span>ore<span>&nbsp;</span>fluids<span>; hydrothermal&nbsp;</span>fluids<span>&nbsp;as deduced from wallrock alteration, from&nbsp;</span>fluid<span>&nbsp;inclusions and hot springs, from isotopic studies, and from mine studies, zoning, and so forth.</span></p>","language":"English","publisher":"Society of Economic Geologists","doi":"10.2113/gsecongeo.60.7.1380","usgsCitation":"Roedder, E., 1965, Report on S.E.G. Symposium on the chemistry of the ore-forming fluids August-September,1964: Economic Geology, v. 60, no. 7, p. 1380-1403, https://doi.org/10.2113/gsecongeo.60.7.1380.","productDescription":"24 p.","startPage":"1380","endPage":"1403","costCenters":[],"links":[{"id":386233,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"60","issue":"7","noUsgsAuthors":false,"publicationDate":"1965-11-01","publicationStatus":"PW","contributors":{"authors":[{"text":"Roedder, E.","contributorId":100986,"corporation":false,"usgs":true,"family":"Roedder","given":"E.","affiliations":[],"preferred":false,"id":817020,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":5220097,"text":"5220097 - 1965 - A method of approximating range size of small mammals","interactions":[],"lastModifiedDate":"2025-03-07T16:52:26.266772","indexId":"5220097","displayToPublicDate":"1965-10-30T00:00:00","publicationYear":"1965","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2373,"text":"Journal of Mammalogy","onlineIssn":"1545-1542","printIssn":"0022-2372","active":true,"publicationSubtype":{"id":10}},"title":"A method of approximating range size of small mammals","docAbstract":"<p>No abstract available.&nbsp;</p>","language":"English","publisher":"Oxford Academic","doi":"10.2307/1377944","usgsCitation":"Stickel, L.F., 1965, A method of approximating range size of small mammals: Journal of Mammalogy, v. 46, no. 4, p. 677-679, https://doi.org/10.2307/1377944.","productDescription":"3 p.","startPage":"677","endPage":"679","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":197776,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"46","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e486ee4b07f02db50c1f2","contributors":{"authors":[{"text":"Stickel, Lucille F.","contributorId":76598,"corporation":false,"usgs":true,"family":"Stickel","given":"Lucille","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":331330,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":1650,"text":"1650 - 1965 - United States earthquake research program, earthquake prediction: program issue paper","interactions":[],"lastModifiedDate":"2014-07-14T09:36:26","indexId":"1650","displayToPublicDate":"1965-10-15T09:35:09","publicationYear":"1965","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"title":"United States earthquake research program, earthquake prediction: program issue paper","docAbstract":"No abstract available.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/1650","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1965, United States earthquake research program, earthquake prediction: program issue paper, x, 6 p., https://doi.org/10.3133/1650.","productDescription":"x, 6 p.","numberOfPages":"16","costCenters":[],"links":[{"id":289840,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53c4fc8ae4b0b58d96eeb654","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":528002,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70161798,"text":"70161798 - 1965 - Infectious pancreatic necrosis-The trout farmers' dilemma","interactions":[],"lastModifiedDate":"2021-04-20T14:48:43.786074","indexId":"70161798","displayToPublicDate":"1965-10-12T00:00:00","publicationYear":"1965","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3663,"text":"U.S. Trout News","active":true,"publicationSubtype":{"id":10}},"title":"Infectious pancreatic necrosis-The trout farmers' dilemma","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Trout Farmers Association","usgsCitation":"Parisot, T., 1965, Infectious pancreatic necrosis-The trout farmers' dilemma: U.S. Trout News, v. 9, no. 5, p. 6-21.","productDescription":"2 p.","startPage":"6","endPage":"21","costCenters":[],"links":[{"id":313928,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"9","issue":"5","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"568e4916e4b0e7a44bc419eb","contributors":{"authors":[{"text":"Parisot, T. J.","contributorId":43014,"corporation":false,"usgs":true,"family":"Parisot","given":"T. J.","affiliations":[],"preferred":false,"id":587800,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":5220327,"text":"5220327 - 1965 - A simple animal support for convenient weighing","interactions":[],"lastModifiedDate":"2025-02-07T16:17:44.922706","indexId":"5220327","displayToPublicDate":"1965-10-11T00:00:00","publicationYear":"1965","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2508,"text":"Journal of Wildlife Management","active":true,"publicationSubtype":{"id":10}},"title":"A simple animal support for convenient weighing","docAbstract":"A simple animal support constructed of web belts to hold skittish pigs for weighing was developed. The support is easily made, noninjurious to the pigs, and compact, facilitating rapid, accurate weighing. With minor modifications, the support can probably be used in weighing other animals.","language":"English","publisher":"Wiley","doi":"10.2307/3798571","usgsCitation":"Pan, H., Caslick, J., Harke, D., and Decker, D., 1965, A simple animal support for convenient weighing: Journal of Wildlife Management, v. 29, no. 4, p. 890-891, https://doi.org/10.2307/3798571.","productDescription":"2 p.","startPage":"890","endPage":"891","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":487104,"rank":2,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.2307/3798571","text":"Publisher Index Page"},{"id":196879,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"29","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b17e4b07f02db6a651e","contributors":{"authors":[{"text":"Pan, H.P.","contributorId":41927,"corporation":false,"usgs":true,"family":"Pan","given":"H.P.","email":"","affiliations":[],"preferred":false,"id":331631,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Caslick, J.W.","contributorId":94407,"corporation":false,"usgs":true,"family":"Caslick","given":"J.W.","email":"","affiliations":[],"preferred":false,"id":331634,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Harke, D.T.","contributorId":78422,"corporation":false,"usgs":true,"family":"Harke","given":"D.T.","email":"","affiliations":[],"preferred":false,"id":331633,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Decker, D.G.","contributorId":59900,"corporation":false,"usgs":true,"family":"Decker","given":"D.G.","email":"","affiliations":[],"preferred":false,"id":331632,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":5222228,"text":"5222228 - 1965 - Epizootiologic studies on filarioids of the raccoon","interactions":[],"lastModifiedDate":"2025-02-07T16:26:50.198695","indexId":"5222228","displayToPublicDate":"1965-10-11T00:00:00","publicationYear":"1965","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2508,"text":"Journal of Wildlife Management","active":true,"publicationSubtype":{"id":10}},"title":"Epizootiologic studies on filarioids of the raccoon","docAbstract":"<p>Filarioid worms (<i>Dirofilaria immitis</i>, <i>D. tenuis</i>, <i>Dipetalonema procyonis</i>, and <i>D. llewellyni</i>) were discovered in raccoons (<i>Procyon lotar</i>) in Maryland. Raccoons were trapped in lowland, upland, and agricultural-residential areas, which were further classified as stream borders, poorly drained, and well drained. Data on incidence of <i>D. llewellyni</i> were analyzed on basis of host distribution within these areas to indicate type of habitat in which one might seek the vector. It was concluded that exposure takes place in the spring of the year. The arthropod found associated most often with the raccoon in spring was <i>Ixodes texanus</i>. Larvae of this tick which were fed on infected raccoons presented no evidence of development of the microfilariae. Feeding experiments were also conducted with mosquitoes: <i>Aedes aegypti</i>, <i>A. canadensis</i>, <i>A. sollicitans</i>, <i>A. triseriatus</i>, <i>A. vexans</i>, <i>Culex pipiens</i>, <i>Anopheles punctipennis</i>, and <i>A. quadrimaculatus</i>. Although microfilariae remained alive and active in the gut contents of all these mosquitoes for 2 days, only in <i>Aedes aegypti</i> did they enter the hemocele, but no developmental changes were noted and all microfilariae were dead by the eighth day. Although the intermediate host of <i>D. llewellyni</i> was not determined, evaluation of the accumulated data provides criteria for seeking the vector. It appeared unlikely that exposure of the raccoons took place in the den or that the filarioids were transmitted by an ectoparasite commonly found in raccoon dens. The data suggest that the vector is available only early in spring, although there are infected raccoons throughout the year. Prevalence in juveniles was 21 percent; in subadults, 64 percent; in adults, 87 percent.</p>","language":"English","publisher":"Wiley","doi":"10.2307/3798544","usgsCitation":"Herman, C.M., and Price, D., 1965, Epizootiologic studies on filarioids of the raccoon: Journal of Wildlife Management, v. 29, no. 4, p. 694-699, https://doi.org/10.2307/3798544.","productDescription":"6 p.","startPage":"694","endPage":"699","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":196000,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Maryland","otherGeospatial":"Patuxent Wildlife Research Center","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -76.82499365611099,\n              39.06403824922501\n            ],\n            [\n              -76.82499365611099,\n              39.05470892556758\n            ],\n            [\n              -76.81260696233649,\n              39.05470892556758\n            ],\n            [\n              -76.81260696233649,\n              39.06403824922501\n            ],\n            [\n              -76.82499365611099,\n              39.06403824922501\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","volume":"29","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9ae4b07f02db65d601","contributors":{"authors":[{"text":"Herman, C. M.","contributorId":101335,"corporation":false,"usgs":true,"family":"Herman","given":"C.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":335856,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Price, D.L.","contributorId":94399,"corporation":false,"usgs":true,"family":"Price","given":"D.L.","email":"","affiliations":[],"preferred":false,"id":335855,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70205839,"text":"70205839 - 1965 - Structure, metamorphism, and plutonism in the south-central Klamath Mountains, California","interactions":[],"lastModifiedDate":"2019-10-08T07:29:05","indexId":"70205839","displayToPublicDate":"1965-10-07T14:17:13","publicationYear":"1965","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1786,"text":"Geological Society of America Bulletin","active":true,"publicationSubtype":{"id":10}},"title":"Structure, metamorphism, and plutonism in the south-central Klamath Mountains, California","docAbstract":"<p>In the south-central Klamath Mountains 50 miles of the the north-trending central metamorphic belt and adjacent parts of the eastern Paleozoic and western Paleozoic and Triassic belts have been mapped and studied in detail. Within the central metamorphic belt a sequence of three lithologically distinctive metamorphic units has been recognized (from bottom to top): (1) siliceous metasedimentary rocks and greenstones of the Stuart Fork Formation; (2) the Salmon Hornblende Schist; and (3) siliceous, calcareous, and amphibolitic rocks, predominantly metasedimentary, of the Grouse Ridge Formation. The age of these metamorphic rocks is uncertain; they are known only to predate intrusion of Late Jurassic (Nevadan) granitic rocks. Ultramafic rocks, mainly alpine-type peridotites, were emplaced before the granitic rocks and occur primarily in a single large sheetlike body which separates the central metamorphic belt from the eastern Paleozoic belt. Granitic plutons, including quartz diorites, trondhjemites, granodiorites, diorites, and gabbros, in decreasing order of abundance, range in size from less than 1 to about 80 square miles in area.</p><p>Two orogenic phases in the central metamorphic belt have been distinguished by structural and textural features. A late deformation uniformly affected the metamorphic terrane and the ultramafic rocks but predated granitic rocks. It was accompanied by some metamorphism in the lower to middle greenchist facies and produced upright folds that trend south and plunge gently. An earlier phase affected the various rock units differentially; it produced widespread recumbent folding and upper greenschist- to amphibolite-facies metamorphism in Salmon and Grouse Ridge rocks, but involved the underlying Stuart Fork Formation less severely, producing at least local recumbent folding and lower greenschist-facies metamorphism. The preferred interpretation of this upward increase in structural complexity and metamorphic grade is that the Salmon-Grouse Ridge sequence is a thrust sheet which overrode the Stuart Fork rocks concurrently with emplacement of the ultramafic rocks during the culmination of early recumbent folding and metamorphism. Thrusting was then followed by upright folding during the waning stages of regional metamorphism. The first deformational phase, and possibly the second, occurred during late Paleozoic time as indicated by recent isotopic ages of Salmon Hornblende Schist.</p>","language":"English","publisher":"GSA","doi":"10.1130/0016-7606(1965)76[933:SMAPIT]2.0.CO;2","usgsCitation":"Davis, G.A., Holdaway, M.J., Lipman, P.W., and Romey, W.D., 1965, Structure, metamorphism, and plutonism in the south-central Klamath Mountains, California: Geological Society of America Bulletin, v. 76, no. 8, p. 933-966, https://doi.org/10.1130/0016-7606(1965)76[933:SMAPIT]2.0.CO;2.","productDescription":"34 p.","startPage":"933","endPage":"966","numberOfPages":"34","onlineOnly":"Y","costCenters":[{"id":617,"text":"Volcano Science Center","active":true,"usgs":true}],"links":[{"id":368069,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"California","otherGeospatial":"South-central Klamath Mountains","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -123.2281494140625,\n              40.88444793903562\n            ],\n            [\n              -122.5250244140625,\n              40.88444793903562\n            ],\n            [\n              -122.5250244140625,\n              41.6195489884308\n            ],\n            [\n              -123.2281494140625,\n              41.6195489884308\n            ],\n            [\n              -123.2281494140625,\n              40.88444793903562\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"76","issue":"8","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Davis, Gregory A.","contributorId":219570,"corporation":false,"usgs":false,"family":"Davis","given":"Gregory","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":772571,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Holdaway, M. J.","contributorId":98047,"corporation":false,"usgs":false,"family":"Holdaway","given":"M.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":772572,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Lipman, Peter W. 0000-0001-9175-6118 plipman@usgs.gov","orcid":"https://orcid.org/0000-0001-9175-6118","contributorId":3486,"corporation":false,"usgs":true,"family":"Lipman","given":"Peter","email":"plipman@usgs.gov","middleInitial":"W.","affiliations":[{"id":617,"text":"Volcano Science Center","active":true,"usgs":true},{"id":5079,"text":"Pacific Regional Director's Office","active":true,"usgs":true}],"preferred":true,"id":772573,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Romey, W. D.","contributorId":219571,"corporation":false,"usgs":false,"family":"Romey","given":"W.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":772574,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70221199,"text":"70221199 - 1965 - Relations of fresh and salty ground water along the southeastern U. S. Atlantic Coast","interactions":[],"lastModifiedDate":"2021-06-04T21:19:48.616707","indexId":"70221199","displayToPublicDate":"1965-10-01T16:14:21","publicationYear":"1965","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3825,"text":"Groundwater","active":true,"publicationSubtype":{"id":10}},"title":"Relations of fresh and salty ground water along the southeastern U. S. Atlantic Coast","docAbstract":"<p>Studies of the hydrogeologic environments and the dynamic and equilibrium relations of fresh and salt water in aquifers have been intensified at several places along the southeastern Atlantic Coast. Some salt-water problems involve the coastal water-table aquifer, and others involve parts of the artesian system.</p><p>On the sandy coastal islands of North Carolina, freshwater lenses under water-table conditions float on salt water. Salt-water contamination may take place by (1) lateral encroachment from the ocean and bay; (2) vertical encroachment from below; (3) overland inundation by ocean water during storms; and (4) downward percolation of salt spray and salt-bearing precipitation.</p><p>In the Savannah, Georgia, and South Carolina area, salt-water encroachment along two of five water-bearing zones in the principal artesian (limestone) aquifer has been caused by the decline of artesian pressure due to pumping. Some wells in the limestone at nearby Parris Island, South Carolina, yield salty water when overpumped. From Savannah southward at least to Fernandina, Florida, connate salty water occurs in the artesian aquifer below the fresh water. At Brunswick, Georgia, connate salty water is stratified between fresh-water bodies in the limestone aquifer above depths of 2,000 feet. Connate salty water has contaminated the aquifer between depths of 500 and 800 feet in a small area in the city.</p><p>Along the southeast Florida coast drainage canals have been the primary cause of salt-water contamination of the highly permeable Biscayne aquifer. Criteria have been established for the operation of salinity-control dams to prevent encroachment. The salt-water front in the aquifer along the coast is dynamically stable under natural conditions.</p>","language":"English","publisher":"NGWA The Groundwater Association","doi":"10.1111/j.1745-6584.1965.tb01224.x","usgsCitation":"Wait, R.L., and Callahan, J., 1965, Relations of fresh and salty ground water along the southeastern U. S. Atlantic Coast: Groundwater, v. 3, no. 4, p. 3-17, https://doi.org/10.1111/j.1745-6584.1965.tb01224.x.","productDescription":"15 p.","startPage":"3","endPage":"17","costCenters":[],"links":[{"id":386244,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United  States","otherGeospatial":"southeastern U.S. Atlantic Coast","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -88.33007812499999,\n              24.926294766395593\n            ],\n            [\n              -75.5859375,\n              24.926294766395593\n            ],\n            [\n              -75.5859375,\n              37.23032838760384\n            ],\n            [\n              -88.33007812499999,\n              37.23032838760384\n            ],\n            [\n              -88.33007812499999,\n              24.926294766395593\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"3","issue":"4","noUsgsAuthors":false,"publicationDate":"2006-07-06","publicationStatus":"PW","contributors":{"authors":[{"text":"Wait, R. L.","contributorId":15988,"corporation":false,"usgs":true,"family":"Wait","given":"R.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":817037,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Callahan, J.T.","contributorId":100920,"corporation":false,"usgs":true,"family":"Callahan","given":"J.T.","email":"","affiliations":[],"preferred":false,"id":817038,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70221194,"text":"70221194 - 1965 - Tracing the continuity of pleistocene aquifers in northern New Jersey by seismic methods","interactions":[],"lastModifiedDate":"2021-06-04T20:20:08.257589","indexId":"70221194","displayToPublicDate":"1965-10-01T14:22:09","publicationYear":"1965","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3825,"text":"Groundwater","active":true,"publicationSubtype":{"id":10}},"title":"Tracing the continuity of pleistocene aquifers in northern New Jersey by seismic methods","docAbstract":"<p>Seismic<span>&nbsp;refraction measurements were used to draw a&nbsp;</span>new<span>&nbsp;bedrock contour map&nbsp;</span>in<span>&nbsp;Morris County,&nbsp;</span>New<span>&nbsp;</span>Jersey<span>, where the major ground‐water supplies are found&nbsp;</span>in<span>&nbsp;Quaternary sand and gravel deposits filling pre‐</span>Pleistocene<span>&nbsp;channels.&nbsp;</span>Aquifer<span>&nbsp;performance tests aided&nbsp;</span>in<span>&nbsp;</span>tracing<span>&nbsp;the&nbsp;</span>continuity<span>&nbsp;of the Quaternary&nbsp;</span>aquifers<span>&nbsp;</span>in<span>&nbsp;these channels.&nbsp;</span>In<span>&nbsp;one case, the lack of&nbsp;</span>continuity<span>&nbsp;between two wells substantiated the&nbsp;</span>seismic<span>&nbsp;prediction that two separate channels were involved. The success of the&nbsp;</span>seismic<span>&nbsp;exploration emphasizes the value of using such&nbsp;</span>methods<span>, so that test drilling can be devoted to exploring the more favorable areas for production wells.</span></p>","language":"English","publisher":"Wiley","doi":"10.1111/j.1745-6584.1965.tb01227.x","usgsCitation":"Gill, H., Vecchioli, J., and Bonini, W., 1965, Tracing the continuity of pleistocene aquifers in northern New Jersey by seismic methods: Groundwater, v. 3, no. 4, p. 33-35, https://doi.org/10.1111/j.1745-6584.1965.tb01227.x.","productDescription":"3 p.","startPage":"33","endPage":"35","costCenters":[],"links":[{"id":386239,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United  States","state":"New Jersey","otherGeospatial":"northern New Jersey","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -75.25634765624999,\n              40.17047886718109\n            ],\n            [\n              -73.89404296874999,\n              40.17047886718109\n            ],\n            [\n              -73.89404296874999,\n              41.40153558289848\n            ],\n            [\n              -75.25634765624999,\n              41.40153558289848\n            ],\n            [\n              -75.25634765624999,\n              40.17047886718109\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"3","issue":"4","noUsgsAuthors":false,"publicationDate":"2006-07-06","publicationStatus":"PW","contributors":{"authors":[{"text":"Gill, H.E.","contributorId":24330,"corporation":false,"usgs":true,"family":"Gill","given":"H.E.","email":"","affiliations":[],"preferred":false,"id":817028,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Vecchioli, John","contributorId":36113,"corporation":false,"usgs":true,"family":"Vecchioli","given":"John","email":"","affiliations":[],"preferred":false,"id":817029,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Bonini, W.E.","contributorId":168860,"corporation":false,"usgs":false,"family":"Bonini","given":"W.E.","email":"","affiliations":[],"preferred":false,"id":817030,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":5220469,"text":"5220469 - 1965 - Pox infection and a secondary cutaneous mycosis in a red-tailed tropicbird (Phaethon rubricauda)","interactions":[],"lastModifiedDate":"2022-10-26T14:22:21.881307","indexId":"5220469","displayToPublicDate":"1965-10-01T12:17:34","publicationYear":"1965","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1140,"text":"Bulletin of the Wildlife Disease Association","active":true,"publicationSubtype":{"id":10}},"displayTitle":"Pox infection and a secondary cutaneous mycosis in a red-tailed tropicbird (<i>Phaethon rubricauda</i>)","title":"Pox infection and a secondary cutaneous mycosis in a red-tailed tropicbird (Phaethon rubricauda)","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"Wildlife Disease Association","doi":"10.7589/0090-3558-1.4.60","usgsCitation":"Locke, L.N., Wirtz, W.O., and Brown, E.E., 1965, Pox infection and a secondary cutaneous mycosis in a red-tailed tropicbird (Phaethon rubricauda): Bulletin of the Wildlife Disease Association, v. 1, no. 4, p. 60-61, https://doi.org/10.7589/0090-3558-1.4.60.","productDescription":"2 p.","startPage":"60","endPage":"61","numberOfPages":"2","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":193840,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Hawaii","otherGeospatial":"Sand Island, Midway Islands","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {\n        \"stroke\": \"#555555\",\n        \"stroke-width\": 2,\n        \"stroke-opacity\": 1,\n        \"fill\": \"#555555\",\n        \"fill-opacity\": 0.3\n      },\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -177.40018844604492,\n              28.190513153841668\n            ],\n            [\n              -177.31470108032227,\n              28.190513153841668\n            ],\n            [\n              -177.31470108032227,\n              28.223793792828708\n            ],\n            [\n              -177.40018844604492,\n              28.223793792828708\n            ],\n            [\n              -177.40018844604492,\n              28.190513153841668\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"1","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad3e4b07f02db681cf3","contributors":{"authors":[{"text":"Locke, L. N.","contributorId":73539,"corporation":false,"usgs":true,"family":"Locke","given":"L.","email":"","middleInitial":"N.","affiliations":[],"preferred":false,"id":331863,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wirtz, W. O. II","contributorId":43452,"corporation":false,"usgs":true,"family":"Wirtz","given":"W.","suffix":"II","email":"","middleInitial":"O.","affiliations":[],"preferred":false,"id":331861,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Brown, E. E.","contributorId":52287,"corporation":false,"usgs":true,"family":"Brown","given":"E.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":331862,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70238528,"text":"70238528 - 1965 - Avian cholera in a trumpeter swan (Olor buccinator)","interactions":[],"lastModifiedDate":"2022-11-28T17:32:05.360785","indexId":"70238528","displayToPublicDate":"1965-10-01T11:27:27","publicationYear":"1965","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1140,"text":"Bulletin of the Wildlife Disease Association","active":true,"publicationSubtype":{"id":10}},"displayTitle":"Avian cholera in a trumpeter swan (<i>Olor buccinator</i>)","title":"Avian cholera in a trumpeter swan (Olor buccinator)","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"Wildlife Disease Association","doi":"10.7589/0090-3558-1.4.54","usgsCitation":"Gritman, R.B., and Jensen, W.I., 1965, Avian cholera in a trumpeter swan (Olor buccinator): Bulletin of the Wildlife Disease Association, v. 1, no. 4, p. 54-55, https://doi.org/10.7589/0090-3558-1.4.54.","productDescription":"2 p.","startPage":"54","endPage":"55","costCenters":[],"links":[{"id":409711,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"1","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Gritman, R. B.","contributorId":225175,"corporation":false,"usgs":false,"family":"Gritman","given":"R.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":857747,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Jensen, W. I.","contributorId":74705,"corporation":false,"usgs":true,"family":"Jensen","given":"W.","email":"","middleInitial":"I.","affiliations":[],"preferred":false,"id":857748,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":1003274,"text":"1003274 - 1965 - Diuron, fenuron, monuron, neburon, and TCA mixtures as aquatic herbicides in fish habitats","interactions":[],"lastModifiedDate":"2026-03-18T16:17:56.420224","indexId":"1003274","displayToPublicDate":"1965-10-01T00:00:00","publicationYear":"1965","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3741,"text":"Weeds","active":true,"publicationSubtype":{"id":10}},"title":"Diuron, fenuron, monuron, neburon, and TCA mixtures as aquatic herbicides in fish habitats","docAbstract":"<p><span>The substituted urea herbicides were rated according to their effectiveness as aquatic herbicides in this order: diuron [3-(3,4-dichlorophenyl)-1,1-dimethylurea], monuron [3-(p-chlorophenyl)-1,1-dimethylurea], neburon [1-butyl-3-(3,4-dichlorophenyl)-1-methlyurea] and TCA(trichloroacetic acid) mixtures with them. They showed greatest potential in controlling certain aquatic plants in pre-emergence and early postemergence applications. However, relatively high concentrations were required to control filamentous algae&nbsp;</span><span class=\"italic\">(<i>Cladophora</i>, <i>Pithophora</i></span><span>&nbsp;and&nbsp;</span><span class=\"italic\"><i>Spirogyra</i>)</span><span>, chara&nbsp;</span><span class=\"italic\">(<i>Chara</i>)</span><span>, coontail&nbsp;</span><span class=\"italic\">(<i>Ceratophyllum</i>)</span><span>, naiad&nbsp;</span><span class=\"italic\">(<i>Najas</i>)</span><span>, and pondweeds&nbsp;</span><span class=\"italic\">(<i>Potamogeton</i>)</span><span>&nbsp;for periods of time exceeding three months and up to three years. Granular formulations achieved better distribution of herbicides for control of rooted aquatic plants along the margins of lakes and ponds. Wettable powder and liquid emulsifiable concentrates were superior to granular formulations for the control of algae and emergent or floating aquatic plants.</span></p><p><span>Monuron and fenuron were less toxic to fish than were diuron and neburon. The TCA mixtures were somewhat more toxic than the simple ureas. Some species of fish were more sensitive than others and fingerlings more sensitive than adults of the same species. Fish-food organisms were reduced appreciably in plastic enclosures at herbicidal concentrations.</span></p>","language":"English","publisher":"Cambridge University Press","doi":"10.2307/4040879","usgsCitation":"Walker, C., 1965, Diuron, fenuron, monuron, neburon, and TCA mixtures as aquatic herbicides in fish habitats: Weeds, v. 13, no. 4, p. 297-301, https://doi.org/10.2307/4040879.","productDescription":"5 p.","startPage":"297","endPage":"301","costCenters":[{"id":606,"text":"Upper Midwest Environmental Sciences Center","active":true,"usgs":true}],"links":[{"id":178347,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"13","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a6be4b07f02db63d887","contributors":{"authors":[{"text":"Walker, C.R.","contributorId":69097,"corporation":false,"usgs":true,"family":"Walker","given":"C.R.","email":"","affiliations":[],"preferred":false,"id":313053,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70010462,"text":"70010462 - 1965 - Meteorites and craters of Campo del Cielo, Argentina","interactions":[],"lastModifiedDate":"2026-02-10T18:22:12.965992","indexId":"70010462","displayToPublicDate":"1965-09-03T00:00:00","publicationYear":"1965","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3338,"text":"Science","active":true,"publicationSubtype":{"id":10}},"title":"Meteorites and craters of Campo del Cielo, Argentina","docAbstract":"Field studies have thrown new light on a unique prehistoric encounter of a cosmic body with the earth.","language":"English","publisher":"American Association for the Advancement of Science","doi":"10.1126/science.149.3688.1055","issn":"00368075","usgsCitation":"Cassidy, W., Villar, L., Bunch, T., Kohman, T., and Milton, D., 1965, Meteorites and craters of Campo del Cielo, Argentina: Science, v. 149, no. 3688, p. 1055-1064, https://doi.org/10.1126/science.149.3688.1055.","productDescription":"10 p.","startPage":"1055","endPage":"1064","costCenters":[],"links":[{"id":218953,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"Argentina","otherGeospatial":"Campo del Cielo","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -61.90296896475709,\n              -27.79239255213136\n            ],\n            [\n              -61.90296896475709,\n              -27.952206617216753\n            ],\n            [\n              -61.70062908028608,\n              -27.952206617216753\n            ],\n            [\n              -61.70062908028608,\n              -27.79239255213136\n            ],\n            [\n              -61.90296896475709,\n              -27.79239255213136\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","volume":"149","issue":"3688","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a5513e4b0c8380cd6d108","contributors":{"authors":[{"text":"Cassidy, W.A.","contributorId":31903,"corporation":false,"usgs":true,"family":"Cassidy","given":"W.A.","email":"","affiliations":[],"preferred":false,"id":358978,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Villar, L.M.","contributorId":90459,"corporation":false,"usgs":true,"family":"Villar","given":"L.M.","email":"","affiliations":[],"preferred":false,"id":358981,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Bunch, T.E.","contributorId":17364,"corporation":false,"usgs":true,"family":"Bunch","given":"T.E.","email":"","affiliations":[],"preferred":false,"id":358977,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Kohman, T.P.","contributorId":52715,"corporation":false,"usgs":true,"family":"Kohman","given":"T.P.","email":"","affiliations":[],"preferred":false,"id":358980,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Milton, D.J.","contributorId":44121,"corporation":false,"usgs":true,"family":"Milton","given":"D.J.","email":"","affiliations":[],"preferred":false,"id":358979,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
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