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,{"id":2990,"text":"wsp1792 - 1965 - Ground water in Permafrost regions--an annotated bibliography","interactions":[{"subject":{"id":52376,"text":"ofr63140 - 1963 - Ground water in permafrost regions - an annotated bibliography of publications through 1960, with glossary of terms","indexId":"ofr63140","publicationYear":"1963","noYear":false,"title":"Ground water in permafrost regions - an annotated bibliography of publications through 1960, with glossary of terms"},"predicate":"SUPERSEDED_BY","object":{"id":2990,"text":"wsp1792 - 1965 - Ground water in Permafrost regions--an annotated bibliography","indexId":"wsp1792","publicationYear":"1965","noYear":false,"title":"Ground water in Permafrost regions--an annotated bibliography"},"id":1}],"lastModifiedDate":"2012-02-02T00:05:36","indexId":"wsp1792","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1965","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1792","title":"Ground water in Permafrost regions--an annotated bibliography","language":"ENGLISH","publisher":"U. S. Govt. Print. Off.,","doi":"10.3133/wsp1792","usgsCitation":"Williams, J.R., 1965, Ground water in Permafrost regions--an annotated bibliography: U.S. Geological Survey Water Supply Paper 1792, iii, 294 p. :fold. map (in pocket) ;24 cm., https://doi.org/10.3133/wsp1792.","productDescription":"iii, 294 p. :fold. map (in pocket) ;24 cm.","costCenters":[],"links":[{"id":139447,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1792/report-thumb.jpg"},{"id":29762,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1792/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29763,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1792/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ab0e4b07f02db66daf0","contributors":{"authors":[{"text":"Williams, John R.","contributorId":107260,"corporation":false,"usgs":true,"family":"Williams","given":"John","email":"","middleInitial":"R.","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":146111,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":63347,"text":"gq428 - 1965 - Geologic map of the Blackcap Mountain quadrangle, Fresno County, California","interactions":[],"lastModifiedDate":"2012-02-10T00:10:59","indexId":"gq428","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1965","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":316,"text":"Geologic Quadrangle","code":"GQ","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"428","title":"Geologic map of the Blackcap Mountain quadrangle, Fresno County, California","language":"ENGLISH","doi":"10.3133/gq428","usgsCitation":"Bateman, P.C., 1965, Geologic map of the Blackcap Mountain quadrangle, Fresno County, California: U.S. Geological Survey Geologic Quadrangle 428, 1 map., https://doi.org/10.3133/gq428.","productDescription":"1 map.","costCenters":[],"links":[{"id":101807,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_27.htm","linkFileType":{"id":5,"text":"html"},"description":"27"},{"id":249449,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gq/0428/report.pdf","size":"32","linkFileType":{"id":1,"text":"pdf"}},{"id":252931,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gq/0428/report-thumb.jpg"}],"scale":"62500","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -119,37 ], [ -119,37.25 ], [ -118.75,37.25 ], [ -118.75,37 ], [ -119,37 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b0ce4b07f02db69ee1a","contributors":{"authors":[{"text":"Bateman, Paul Charles","contributorId":54586,"corporation":false,"usgs":true,"family":"Bateman","given":"Paul","email":"","middleInitial":"Charles","affiliations":[],"preferred":false,"id":268706,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":3991,"text":"cir507 - 1965 - Index of surface-water records to December 31, 1963--Part 7, Lower Mississippi River basin","interactions":[],"lastModifiedDate":"2012-02-02T00:05:27","indexId":"cir507","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1965","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":307,"text":"Circular","code":"CIR","onlineIssn":"2330-5703","printIssn":"1067-084X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"507","title":"Index of surface-water records to December 31, 1963--Part 7, Lower Mississippi River basin","language":"ENGLISH","publisher":"U.S. Dept. of the Interior, Geological Survey,","doi":"10.3133/cir507","usgsCitation":"Eisenhuth, H., 1965, Index of surface-water records to December 31, 1963--Part 7, Lower Mississippi River basin: U.S. Geological Survey Circular 507, 55 p. :map ;27 cm., https://doi.org/10.3133/cir507.","productDescription":"55 p. :map ;27 cm.","costCenters":[],"links":[{"id":117212,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1965/0507/report-thumb.jpg"},{"id":31076,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1965/0507/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f8e4b07f02db5f306f","contributors":{"authors":[{"text":"Eisenhuth, H.P.","contributorId":38140,"corporation":false,"usgs":true,"family":"Eisenhuth","given":"H.P.","email":"","affiliations":[],"preferred":false,"id":147956,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":63274,"text":"gq408 - 1965 - Geology of the Rush quadrangle, Kentucky","interactions":[],"lastModifiedDate":"2012-02-10T00:10:41","indexId":"gq408","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1965","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":316,"text":"Geologic Quadrangle","code":"GQ","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"408","title":"Geology of the Rush quadrangle, Kentucky","language":"ENGLISH","doi":"10.3133/gq408","usgsCitation":"Carlson, J.E., 1965, Geology of the Rush quadrangle, Kentucky: U.S. Geological Survey Geologic Quadrangle 408, 1 map :col. ;57 x 44 cm., on sheet 82 x 87 cm., folded in envelope 31 x 24 cm., https://doi.org/10.3133/gq408.","productDescription":"1 map :col. ;57 x 44 cm., on sheet 82 x 87 cm., folded in envelope 31 x 24 cm.","costCenters":[],"links":[{"id":102426,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_875.htm","linkFileType":{"id":5,"text":"html"},"description":"875"},{"id":249380,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gq/0408/report.pdf","size":"34","linkFileType":{"id":1,"text":"pdf"}},{"id":252779,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gq/0408/report-thumb.jpg"}],"scale":"24000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -82.86749999999999,38.25 ], [ -82.86749999999999,38.3675 ], [ -82.75,38.3675 ], [ -82.75,38.25 ], [ -82.86749999999999,38.25 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4acce4b07f02db67e685","contributors":{"authors":[{"text":"Carlson, John Edward","contributorId":49803,"corporation":false,"usgs":true,"family":"Carlson","given":"John","email":"","middleInitial":"Edward","affiliations":[],"preferred":false,"id":268589,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":5712,"text":"pp498C - 1965 - Relation of electrochemical potentials and iron content to ground-water flow patterns","interactions":[],"lastModifiedDate":"2017-04-25T14:05:37","indexId":"pp498C","displayToPublicDate":"1993-01-01T10:00:00","publicationYear":"1965","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":"498","chapter":"C","title":"Relation of electrochemical potentials and iron content to ground-water flow patterns","docAbstract":"<p>This study was undertaken to develop means of measuring oxidation potentials in aquifer systems and to use the measured values in interpreting the behavior of iron in ground water. Anne Arundel County, Md., was selected as the area of study because of the wide range of concentration of iron-nearly zero to about 35 ppm-in the ground water and the rather complete information on the geology and hydrology. The regional geology consists of coastal plain sediments ranging in age from Early Cretaceous through the Recent. Most of the pH and oxidation-potential measurements were made in nonmarine Cretaceous deposits, only a few in the marine Eocene. Iron-bearing minerals in the area are primarily hematite or limonite and glauconite with a small amount of pyrite. </p><p>Equipment was developed that permits the measurement of oxidation potentials by use of saturated calomel and platinum electrodes in ground-water samples uncontaminated by oxygen of the atmosphere. Measured Eh values range from about +700 mv to -40 mv. Approximately 2 to 3 hours are required to measure a stable or nearly stable oxidation potential. </p><p>The mineralogy and organic content of the deposits and the ground-water flow pattern are the primary controls on the oxidation potential and pH of the water. A correlation exists between the oxidation potential and the concentration of iron in ground water; the higher concentrations occur in waters with the lowest values of Eh. The concentration of iron in the water tested shows little correlation with the pH of the water. The highest oxidation potentials were measured in water produced from shallow wells and those wells in recharge areas. The lowest potentials were measured farthest downgradient in water associated with gray and green sediments. The Eh values measured in the field are between values predicted from the solubility of Fe(OH)<sub>2</sub>(c) and values predicted from the solubility of hematite.</p>","largerWorkTitle":"Hydrology of aquifer systems","language":"English","publisher":"U.S. Government Printing Office","doi":"10.3133/pp498C","usgsCitation":"Back, W., and Barnes, I., 1965, Relation of electrochemical potentials and iron content to ground-water flow patterns: U.S. Geological Survey Professional Paper 498, Report: iii, p. C1-C16; 3 Plates: 10.09 x 17.13 inches or less, https://doi.org/10.3133/pp498C.","productDescription":"Report: iii, p. C1-C16; 3 Plates: 10.09 x 17.13 inches or less","costCenters":[],"links":[{"id":32284,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0498c/report.pdf","text":"Report","size":"4.44 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Report"},{"id":139891,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0498c/report-thumb.jpg"},{"id":340291,"rank":5,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0498c/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":340289,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0498c/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":340290,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0498c/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Maryland","county":"Anne Arundel County","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -76.87957763671875,\n              38.69408504756833\n            ],\n            [\n              -76.387939453125,\n              38.69408504756833\n            ],\n            [\n              -76.387939453125,\n              39.25352462727606\n            ],\n            [\n              -76.87957763671875,\n              39.25352462727606\n            ],\n            [\n              -76.87957763671875,\n              38.69408504756833\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac8e4b07f02db67c2c3","contributors":{"authors":[{"text":"Back, William","contributorId":59007,"corporation":false,"usgs":true,"family":"Back","given":"William","email":"","affiliations":[],"preferred":false,"id":151472,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Barnes, Ivan","contributorId":56619,"corporation":false,"usgs":true,"family":"Barnes","given":"Ivan","email":"","affiliations":[],"preferred":false,"id":151471,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":6378,"text":"pp498B - 1965 - Variations in chemical character of water in the Englishtown Formation, New Jersey","interactions":[{"subject":{"id":52280,"text":"ofr62123 - 1962 - Variations in the chemical character of the water in the Englishtown formation, New Jersey","indexId":"ofr62123","publicationYear":"1962","noYear":false,"title":"Variations in the chemical character of the water in the Englishtown formation, New Jersey"},"predicate":"SUPERSEDED_BY","object":{"id":6378,"text":"pp498B - 1965 - Variations in chemical character of water in the Englishtown Formation, New Jersey","indexId":"pp498B","publicationYear":"1965","noYear":false,"chapter":"B","title":"Variations in chemical character of water in the Englishtown Formation, New Jersey"},"id":1}],"lastModifiedDate":"2017-03-15T12:57:36","indexId":"pp498B","displayToPublicDate":"1992-01-01T08:00:00","publicationYear":"1965","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":"498","chapter":"B","title":"Variations in chemical character of water in the Englishtown Formation, New Jersey","docAbstract":"<p>This investigation describes the variations in the chemical character of the water in the Englishtown Formation of Late Cretaceous age in the Atlantic Coastal Plain of New Jersey, and demonstrates the application of the concept of hydrochemical mapping to the study and evaluation of water-bearing materials.&nbsp;The chemistry of ground water is responsive to the physical environment and lends support to available geologic and hydrologic data. A study of the ground-water chemistry may even suggest concepts for which additional geologic or hydrologic data may not be obtainable by conventional methods of study. Hydrochemical mapping is particularly important in evaluating an aquifer satisfactorily, but it could be equally useful in regional geologic studies concerned with continuity of units or mineralogic differences and similarities.</p>","largerWorkTitle":"Hydrology of aquifer systems","language":"English","publisher":"U.S. Government Printing Office","doi":"10.3133/pp498B","collaboration":"Prepared in cooperation with New Jersey Division of Water Policy and Supply","usgsCitation":"Seaber, P.R., 1965, Variations in chemical character of water in the Englishtown Formation, New Jersey: U.S. Geological Survey Professional Paper 498, iii, p. B1-B35, https://doi.org/10.3133/pp498B.","productDescription":"iii, p. B1-B35","costCenters":[],"links":[{"id":33751,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0498b/report.pdf","text":"Report","size":"5.30 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Report"},{"id":121598,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0498b/report-thumb.jpg"}],"country":"United States","state":"New Jersey","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -74.28955078125,\n              40.50753459933616\n            ],\n            [\n              -74.72351074218749,\n              40.13899044275822\n            ],\n            [\n              -75.1519775390625,\n              39.882342585755744\n            ],\n            [\n              -75.3497314453125,\n              39.806426117299374\n            ],\n            [\n              -75.44860839843749,\n              39.688167045890395\n            ],\n            [\n              -75.42938232421875,\n              39.58029027440865\n            ],\n            [\n              -75.3826904296875,\n              39.56970506644249\n            ],\n            [\n              -74.11651611328125,\n              39.816975090490004\n            ],\n            [\n              -74.05334472656249,\n              39.87391156801293\n            ],\n            [\n              -74.0093994140625,\n              40.134790883048524\n            ],\n            [\n              -73.97918701171875,\n              40.361195540839\n            ],\n            [\n              -73.99566650390625,\n              40.40094763151963\n            ],\n            [\n              -74.058837890625,\n              40.44276659332215\n            ],\n            [\n              -74.15496826171874,\n              40.478292268560175\n            ],\n            [\n              -74.28955078125,\n              40.50753459933616\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a14e4b07f02db602af9","contributors":{"authors":[{"text":"Seaber, Paul R.","contributorId":67492,"corporation":false,"usgs":true,"family":"Seaber","given":"Paul","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":152609,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70112256,"text":"70112256 - 1965 - Resource understanding: a challenge to aerial methods","interactions":[],"lastModifiedDate":"2017-03-27T13:42:24","indexId":"70112256","displayToPublicDate":"1990-06-12T10:05:00","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":"Resource understanding: a challenge to aerial methods","docAbstract":"<p>Aerial survey methods are speeding acquisition of survey data needed to provide and manage the nation's resources. These methods have been applied to topographic mapping for a number of years and the record clearly shows their advantages in terms of cost and speed in contrast to the ground methods that have been historically employed. Limited use is now being made of aerial methods to assist cadastral surveys, in location, acquisition and development of National Parks, in mapping the geology of the nation, in locating and developing water resources, and in surveys of the oceans. It is the purpose of this paper to call attention to these uses and to encourage the scientific community to further refine aerial methods so that their use may be increased and the veracity of data improved.</p>","language":"English","publisher":"American Society of Photogrammetry","publisherLocation":"Falls Church, VA","usgsCitation":"Udall, S.L., 1965, Resource understanding: a challenge to aerial methods: Photogrammetric Engineering, v. 31, no. 1, p. 63-75.","productDescription":"13 p.","startPage":"63","endPage":"75","numberOfPages":"13","costCenters":[{"id":222,"text":"Earth Resources Observation and Science (EROS) Center","active":true,"usgs":true}],"links":[{"id":288447,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ 173.0,16.916667 ], [ 173.0,71.833333 ], [ -66.95,71.833333 ], [ -66.95,16.916667 ], [ 173.0,16.916667 ] ] ] } } ] }","volume":"31","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"539acc13e4b0e83db6d08fdb","contributors":{"authors":[{"text":"Udall, Stewart L.","contributorId":9968,"corporation":false,"usgs":true,"family":"Udall","given":"Stewart","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":494583,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"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":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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 \"}}]}","volume":"150","issue":"3704","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059eda7e4b0c8380cd4991e","contributors":{"authors":[{"text":"Munson, P.J.","contributorId":20805,"corporation":false,"usgs":true,"family":"Munson","given":"P.J.","email":"","affiliations":[],"preferred":false,"id":359113,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Frye, J.C.","contributorId":35067,"corporation":false,"usgs":true,"family":"Frye","given":"J.C.","email":"","affiliations":[],"preferred":false,"id":359114,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"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}]}}
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