{"pageNumber":"408","pageRowStart":"10175","pageSize":"25","recordCount":10951,"records":[{"id":52498,"text":"ofr65145 - 1965 - The 1965 Mississippi River flood in Iowa","interactions":[{"subject":{"id":52498,"text":"ofr65145 - 1965 - The 1965 Mississippi River flood in Iowa","indexId":"ofr65145","publicationYear":"1965","noYear":false,"title":"The 1965 Mississippi River flood in Iowa"},"predicate":"SUPERSEDED_BY","object":{"id":941,"text":"wsp1850A - 1970 - Floods of March-May 1965 in the upper Mississippi River basin","indexId":"wsp1850A","publicationYear":"1970","noYear":false,"chapter":"A","title":"Floods of March-May 1965 in the upper Mississippi River basin"},"id":1}],"supersededBy":{"id":941,"text":"wsp1850A - 1970 - Floods of March-May 1965 in the upper Mississippi River basin","indexId":"wsp1850A","publicationYear":"1970","noYear":false,"title":"Floods of March-May 1965 in the upper Mississippi River basin"},"lastModifiedDate":"2016-02-22T10:07:18","indexId":"ofr65145","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1965","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"65-145","title":"The 1965 Mississippi River flood in Iowa","docAbstract":"<p>The great flood of 1965 on the Mississippi River, along the eastern border if the State, exceeded any flood known in 139 years. It cause damages probably in excess of ten millions of dollars in the State of Iowa. Studied now in progress will more thoroughly cover this and other phases of the flood.</p>\n<p>The underlying cause of the flood was an abnormally cold winter which prevented the melting of an excessive snow cover in the upper reaches of the basin. Heavy rains late in March followed by rapid melting triggered the runoff which caused the floods. Peak discharges experienced ranged from 276,000 cfs (cubic feet per second) at McGregor near the northern boundary of the State to 327,000 cfs at Keokuk near the southern boundary. Tributary streams in Iowa were receding as the main-stem flood peak passed their mouths. The discharge they contributed was generally insignificant except for the larger streams.</p>\n<p>Flood data compiled for the part of the River along the eastern border include flood discharges, flood elevations, and the frequency of floods of varying magnitudes. They also include the daily or more frequent stage and discharge data for both the Mississippi River and the downstream gaging stations on Iowa tributaries for the period March-May 1965. Sufficient data are presented to permit studied for preparation of plans for protective works and plans for zoning or for flood plain regulation.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Iowa City, IA","doi":"10.3133/ofr65145","collaboration":"Prepared in cooperation with the Iowa Geological Survey","usgsCitation":"Schwob, H., and Myers, R.E., 1965, The 1965 Mississippi River flood in Iowa: U.S. Geological Survey Open-File Report 65-145, Report: iv, 39 p.; 7 Plates: 19.79 x 10.66 inches and smaller, https://doi.org/10.3133/ofr65145.","productDescription":"Report: iv, 39 p.; 7 Plates: 19.79 x 10.66 inches and smaller","numberOfPages":"46","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":351,"text":"Iowa Water Science Center","active":true,"usgs":true}],"links":[{"id":286610,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":286601,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1965/0145/plate-2.pdf"},{"id":286603,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1965/0145/plate-4.pdf"},{"id":286602,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1965/0145/plate-3.pdf"},{"id":286604,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1965/0145/plate-5.pdf"},{"id":286605,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1965/0145/plate-6.pdf"},{"id":286606,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1965/0145/plate-7.pdf"},{"id":286607,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1965/0145/plate-8.pdf"},{"id":286609,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1965/0145/report.pdf"}],"country":"United States","state":"Illinois, Iowa, Wisconsin","otherGeospatial":"Mississippi River","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -92.5,40.5 ], [ -92.5,43.5 ], [ -89.5,43.5 ], [ -89.5,40.5 ], [ -92.5,40.5 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad5e4b07f02db68368c","contributors":{"authors":[{"text":"Schwob, Harlan H.","contributorId":15532,"corporation":false,"usgs":true,"family":"Schwob","given":"Harlan H.","affiliations":[],"preferred":false,"id":245443,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Myers, Richard E.","contributorId":58573,"corporation":false,"usgs":true,"family":"Myers","given":"Richard","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":245444,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"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":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":5079,"text":"Pacific Regional Director's Office","active":true,"usgs":true},{"id":617,"text":"Volcano Science Center","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":70222381,"text":"70222381 - 1965 - Isotopic ages of minerals from granitic rocks of the central Sierra Nevada and Inyo Mountains, California","interactions":[],"lastModifiedDate":"2021-07-26T13:18:56.627367","indexId":"70222381","displayToPublicDate":"1965-07-26T08:13:38","publicationYear":"1965","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1723,"text":"GSA Bulletin","active":true,"publicationSubtype":{"id":10}},"title":"Isotopic ages of minerals from granitic rocks of the central Sierra Nevada and Inyo Mountains, California","docAbstract":"<div class=\"article-section-wrapper js-article-section js-content-section  \"><p>Potassium-argon ages of biotite and hornblende from specimens of 17 granitic plutons in the central Sierra Nevada and the western Inyo Mountains, California, range from 69 to 183 m. y. The Mount Givens, Lamarck. and Round Valley Peak Granodiorites and related younger and more felsic quartz monzonites represent a pulse of magma emplaced in the general time interval of 80-90 million years ago, during Cretaceous time. Mineral ages of granitic rocks that flank these plutons on both the east and the west have been reduced during the emplacement of the Cretaceous intrusive rocks and are minimum ages for the time of crystallization. The ages of hornblende from the Tinemaha Granodiorite (150 to 180 m. y.) may approach crystallization dates. In conjunction with ages for other intrusive rocks in the Sierra Nevada and adjacent desert ranges they strongly suggest a magmatic episode during the Early Jurassic.</p></div>","language":"English","publisher":"Geological Society of America","doi":"10.1130/0016-7606(1965)76[155:IAOMFG]2.0.CO;2","usgsCitation":"Kistler, R.W., Bateman, P.C., and Brannock, W.W., 1965, Isotopic ages of minerals from granitic rocks of the central Sierra Nevada and Inyo Mountains, California: GSA Bulletin, v. 76, no. 2, https://doi.org/10.1130/0016-7606(1965)76[155:IAOMFG]2.0.CO;2.","productDescription":"11 p.","endPage":"155","numberOfPages":"164","costCenters":[],"links":[{"id":387413,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"California","otherGeospatial":"Sierra Nevada, Inyo Mountain","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -120.36621093749999,\n              36.97622678464096\n            ],\n            [\n              -117.784423828125,\n              36.97622678464096\n            ],\n            [\n              -117.784423828125,\n              38.51378825951165\n            ],\n            [\n              -120.36621093749999,\n              38.51378825951165\n            ],\n            [\n              -120.36621093749999,\n              36.97622678464096\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"76","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Kistler, R. W.","contributorId":115397,"corporation":false,"usgs":true,"family":"Kistler","given":"R.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":819889,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bateman, P. C.","contributorId":27851,"corporation":false,"usgs":true,"family":"Bateman","given":"P.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":819890,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Brannock, W. W.","contributorId":74504,"corporation":false,"usgs":true,"family":"Brannock","given":"W.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":819891,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70010832,"text":"70010832 - 1965 - Holocene submergence of the Eastern Shore of Virginia","interactions":[],"lastModifiedDate":"2026-02-10T18:44:41.648721","indexId":"70010832","displayToPublicDate":"1965-06-11T00:00:00","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":"Holocene submergence of the Eastern Shore of Virginia","docAbstract":"Radiocarbon ages of basal peats 4500 years old or younger and the thickness of salt-marsh peat in the lagoon east of Wachapreague, Virginia, are nearly the same as those of equivalent samples from New Jersey and Cape Cod. This suggests that these coasts have had similar submergence histories. Data obtained from the coasts of Connecticut and northeastern Massachusetts indicate that the Atlantic coast of the United States has been differentially warped during the later Holocene.","language":"English","publisher":"American Association for the Advancement of Science","doi":"10.1126/science.148.3676.1464","issn":"00368075","usgsCitation":"Newman, W., and Rusnak, G., 1965, Holocene submergence of the Eastern Shore of Virginia: Science, v. 148, no. 3676, p. 1464-1466, https://doi.org/10.1126/science.148.3676.1464.","productDescription":"3 p.","startPage":"1464","endPage":"1466","costCenters":[],"links":[{"id":218899,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Connecticut, Massachusetts, New Jersey, Virginia","otherGeospatial":"Atlantic coast","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -71.72870898922105,\n              42.81177931670098\n            ],\n            [\n              -76.07587223384438,\n              42.81177931670098\n            ],\n            [\n              -76.07587223384438,\n              36.4511679954293\n            ],\n            [\n              -71.72870898922105,\n              36.4511679954293\n            ],\n            [\n              -71.72870898922105,\n              42.81177931670098\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","volume":"148","issue":"3676","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a31f6e4b0c8380cd5e3cc","contributors":{"authors":[{"text":"Newman, W.S.","contributorId":12187,"corporation":false,"usgs":true,"family":"Newman","given":"W.S.","email":"","affiliations":[],"preferred":false,"id":359748,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Rusnak, G.A.","contributorId":80407,"corporation":false,"usgs":true,"family":"Rusnak","given":"G.A.","email":"","affiliations":[],"preferred":false,"id":359749,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70221202,"text":"70221202 - 1965 - Stratigraphy and heavy minerals of the bays formation, Bays Mountain synclinorium, northeast Tennessee","interactions":[],"lastModifiedDate":"2021-06-04T21:33:21.794355","indexId":"70221202","displayToPublicDate":"1965-01-01T16:29:37","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":"Stratigraphy and heavy minerals of the bays formation, Bays Mountain synclinorium, northeast Tennessee","docAbstract":"<p><span>The&nbsp;</span>Bays<span>&nbsp;</span>Mountain<span>&nbsp;</span>synclinorium<span>&nbsp;is in the Valley and Ridge province in&nbsp;</span>northeast<span>&nbsp;</span>Tennessee<span>, southwest of Kingsport and west of Greeneville. The more clastic part of the&nbsp;</span>Bays<span>&nbsp;</span>formation<span>&nbsp;lies in the east section of the&nbsp;</span>synclinorium<span>. The thickness of the&nbsp;</span>Bays<span>&nbsp;decreases from about 870 feet on the east to about 600 feet on the west. Presumably, the red beds and primary features of the&nbsp;</span>Bays<span>&nbsp;</span>formation<span>&nbsp;formed under deltaic conditions. A Camarocladia Zone near its base indicates a time-transgression of the&nbsp;</span>Bays<span>. The&nbsp;</span>Bays<span>&nbsp;is older at the base to the east than at its base to the west. The&nbsp;</span>heavy<span>&nbsp;</span>minerals<span>&nbsp;of the&nbsp;</span>Bays<span>&nbsp;were compared with those of the Cambrian and Precambrian(?) sediments, volcanic rocks, and accessory&nbsp;</span>minerals<span>&nbsp;of the crystalline complex which now comprise the Blue Ridge. The&nbsp;</span>minerals<span>&nbsp;identified include nearly all those in the Cambrian and Precambrian(?) sediments as well as additional&nbsp;</span>minerals<span>&nbsp;not found in these older sediments but that are in the crystalline complex. Such&nbsp;</span>minerals<span>&nbsp;indicate that at least a part of the crystalline complex was above sea level during the Middle Ordovician.</span></p>","language":"English","publisher":"Geological Society of America","doi":"10.1130/0016-7606(1965)76[591:SAHMOT]2.0.CO;2","usgsCitation":"Cummings, D., 1965, Stratigraphy and heavy minerals of the bays formation, Bays Mountain synclinorium, northeast Tennessee: Geological Society of America Bulletin, v. 76, no. 5, p. 591-600, https://doi.org/10.1130/0016-7606(1965)76[591:SAHMOT]2.0.CO;2.","productDescription":"10 p.","startPage":"591","endPage":"600","costCenters":[],"links":[{"id":386247,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Tennessee","otherGeospatial":"northeast Tennessee","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -84.385986328125,\n              35.02999636902566\n            ],\n            [\n              -82.63916015625,\n              36.05798104702501\n            ],\n            [\n              -81.82617187499999,\n              36.28856319836237\n            ],\n            [\n              -81.6064453125,\n              36.58024660149866\n            ],\n            [\n              -82.85888671875,\n              36.62434536776987\n            ],\n            [\n              -84.17724609375,\n              36.61552763134925\n            ],\n            [\n              -85.166015625,\n              35.0120020431607\n            ],\n            [\n              -84.385986328125,\n              35.02999636902566\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"76","issue":"5","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Cummings, D.","contributorId":69705,"corporation":false,"usgs":true,"family":"Cummings","given":"D.","email":"","affiliations":[],"preferred":false,"id":817041,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70010681,"text":"70010681 - 1965 - Geochemistry of Birch Creek, Inyo County, California a travertine depositing creek in an arid climate","interactions":[],"lastModifiedDate":"2020-11-24T00:16:31.13398","indexId":"70010681","displayToPublicDate":"1965-01-01T00:00:00","publicationYear":"1965","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1759,"text":"Geochimica et Cosmochimica Acta","active":true,"publicationSubtype":{"id":10}},"title":"Geochemistry of Birch Creek, Inyo County, California a travertine depositing creek in an arid climate","docAbstract":"<div id=\"abstracts\" class=\"Abstracts u-font-serif\"><div id=\"aep-abstract-id4\" class=\"abstract author\"><div id=\"aep-abstract-sec-id5\"><p>A small stream in eastern California was studied in detail to determine the causes of travertine deposition from the stream. Although the ground water feeding the stream is slightly supersaturated to just saturated with calcite, the ground water is supersaturated with CO<sub>2</sub><span>&nbsp;</span>with respect to the overlying air. The water becomes increasingly supersaturated with calcite in a downstream direction as CO<sub>2</sub><span>&nbsp;</span>loss to the air and by photosynthesis exceeds the rate of precipitation of calcite. Water loss by evaporation was below detection and does not play an important role in calcite deposition in this case. The water loss is by seepage through the stream bed. Observations showed variations in HCO<sup>−</sup><sub>3</sub>, pH, discharge, Ca<sup>+2</sup>, relative humidity, water and air temperatures, and dissolved CO<sub>2</sub>. Comparisons of observed and equilibrium states are given for five sampling stations along the stream.</p></div></div></div>","language":"English","publisher":"Elsevier","doi":"10.1016/0016-7037(65)90119-5","issn":"00167037","usgsCitation":"Barnes, I., 1965, Geochemistry of Birch Creek, Inyo County, California a travertine depositing creek in an arid climate: Geochimica et Cosmochimica Acta, v. 29, no. 2, p. 85-112, https://doi.org/10.1016/0016-7037(65)90119-5.","productDescription":"28 p.","startPage":"85","endPage":"112","numberOfPages":"28","costCenters":[],"links":[{"id":219470,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"California","county":"Inyo County","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-117.8357,37.4655],[-117.8339,37.4655],[-117.7506,37.4045],[-117.7398,37.3966],[-117.684,37.3555],[-117.6414,37.3244],[-117.5857,37.2832],[-117.5789,37.2781],[-117.5715,37.2726],[-117.5108,37.2281],[-117.5046,37.2234],[-117.3489,37.1078],[-117.293,37.066],[-117.284,37.0595],[-117.275,37.053],[-117.253,37.0363],[-117.2394,37.0265],[-117.1639,36.9698],[-117.164,36.9688],[-117.0046,36.8495],[-116.981,36.8319],[-116.9783,36.8299],[-116.9641,36.8193],[-116.9237,36.7891],[-116.8912,36.7648],[-116.8806,36.7568],[-116.8453,36.7298],[-116.8424,36.7276],[-116.7895,36.6877],[-116.706,36.6248],[-116.6764,36.6024],[-116.6583,36.5888],[-116.6556,36.5867],[-116.5946,36.54],[-116.574,36.5245],[-116.5589,36.5131],[-116.5247,36.4871],[-116.5107,36.4764],[-116.3752,36.373],[-116.2954,36.3122],[-116.2834,36.3028],[-116.2311,36.2626],[-116.173,36.2174],[-116.1702,36.2152],[-116.1287,36.1829],[-116.1039,36.1636],[-116.0624,36.1314],[-116.049,36.1211],[-115.9925,36.0773],[-115.9518,36.0457],[-115.9178,36.0192],[-115.895,36.0015],[-115.6884,35.8402],[-115.6513,35.8111],[-115.7013,35.8114],[-115.7359,35.8116],[-115.7362,35.7953],[-115.7532,35.7953],[-115.7975,35.7949],[-115.8423,35.7954],[-115.8605,35.7951],[-115.8786,35.7952],[-115.8968,35.7952],[-116.0353,35.7953],[-116.0619,35.7952],[-116.0795,35.7952],[-116.1221,35.7946],[-116.1766,35.7939],[-116.1891,35.7938],[-116.2095,35.7934],[-116.2549,35.7933],[-116.2765,35.793],[-116.2952,35.793],[-116.3389,35.7929],[-116.3474,35.7931],[-116.3588,35.7929],[-116.4444,35.7943],[-116.5068,35.7954],[-116.5346,35.7956],[-116.6021,35.7964],[-116.6071,35.7965],[-116.9232,35.7961],[-116.9357,35.7959],[-116.9453,35.7957],[-117.0917,35.7946],[-117.259,35.7947],[-117.3504,35.7946],[-117.3685,35.7945],[-117.3844,35.7948],[-117.4031,35.7946],[-117.4162,35.7944],[-117.4224,35.7945],[-117.6362,35.7958],[-117.8523,35.7985],[-117.8738,35.7988],[-117.9005,35.7983],[-117.9249,35.7986],[-117.9234,35.7863],[-118.009,35.7861],[-118.0133,35.7993],[-118.0131,35.8093],[-118.009,35.8174],[-118.0015,35.8218],[-117.9975,35.8232],[-118.0065,35.8278],[-118.007,35.8337],[-118.0068,35.8441],[-118.0094,35.8555],[-118.007,35.8627],[-118.0012,35.8663],[-117.9955,35.8699],[-117.9905,35.8648],[-117.9836,35.8661],[-117.9852,35.8738],[-117.9891,35.8793],[-117.9901,35.8861],[-117.9842,35.8929],[-117.9886,35.9029],[-117.9906,35.9129],[-117.9905,35.9197],[-117.9858,35.9255],[-117.9858,35.9301],[-117.9868,35.9342],[-117.9906,35.9424],[-117.9991,35.9461],[-118.0093,35.9449],[-118.0154,35.9541],[-118.0193,35.9609],[-118.014,35.969],[-118.0139,35.974],[-118.0053,35.9784],[-118.0046,35.9811],[-118.0057,35.9839],[-118.0074,35.9875],[-118.0124,35.9935],[-118.0162,35.9985],[-118.0196,36.0013],[-118.0252,36.0045],[-118.0332,36.0051],[-118.0381,36.0151],[-118.0385,36.0265],[-118.0423,36.0329],[-118.0467,36.0415],[-118.046,36.0461],[-118.0488,36.0534],[-118.0537,36.0611],[-118.0529,36.0729],[-118.0539,36.0829],[-118.0572,36.087],[-118.06,36.0921],[-118.0668,36.0899],[-118.069,36.0963],[-118.0677,36.1062],[-118.068,36.1194],[-118.0735,36.1308],[-118.0751,36.1344],[-118.0756,36.1403],[-118.0721,36.1435],[-118.0646,36.1475],[-118.0616,36.1551],[-118.0626,36.1647],[-118.0618,36.1751],[-118.0657,36.1783],[-118.0708,36.1811],[-118.0774,36.1953],[-118.0881,36.2008],[-118.0949,36.2045],[-118.0994,36.2073],[-118.1067,36.216],[-118.1099,36.2247],[-118.1086,36.2328],[-118.1119,36.241],[-118.118,36.2515],[-118.1185,36.2533],[-118.1189,36.2624],[-118.1194,36.2656],[-118.1216,36.2729],[-118.1266,36.2793],[-118.1253,36.2888],[-118.1228,36.2979],[-118.1215,36.3069],[-118.1169,36.31],[-118.114,36.3145],[-118.115,36.3191],[-118.1018,36.3262],[-118.1005,36.3325],[-118.1021,36.338],[-118.1031,36.3434],[-118.1065,36.3476],[-118.1162,36.3481],[-118.1219,36.3486],[-118.1242,36.3505],[-118.1302,36.3628],[-118.1336,36.3674],[-118.1404,36.3693],[-118.146,36.3743],[-118.1517,36.378],[-118.1562,36.3817],[-118.1601,36.3876],[-118.1623,36.3913],[-118.1594,36.394],[-118.149,36.397],[-118.145,36.3997],[-118.1414,36.4056],[-118.1402,36.4142],[-118.1424,36.4187],[-118.1486,36.4229],[-118.1548,36.4266],[-118.1599,36.4298],[-118.165,36.4294],[-118.1748,36.4268],[-118.1823,36.426],[-118.192,36.4265],[-118.2028,36.4298],[-118.2131,36.4308],[-118.2153,36.434],[-118.2129,36.4408],[-118.2151,36.4477],[-118.2173,36.4531],[-118.2223,36.4595],[-118.2331,36.4651],[-118.238,36.4769],[-118.2483,36.4802],[-118.2516,36.4843],[-118.2447,36.4911],[-118.2395,36.4915],[-118.2394,36.4955],[-118.2411,36.5001],[-118.2409,36.5101],[-118.2413,36.5187],[-118.2458,36.5237],[-118.2498,36.5265],[-118.2513,36.5369],[-118.2587,36.5447],[-118.2666,36.5489],[-118.2774,36.5531],[-118.2894,36.5586],[-118.2938,36.5659],[-118.296,36.5755],[-118.2924,36.5836],[-118.2871,36.5899],[-118.2819,36.5957],[-118.2806,36.6021],[-118.2892,36.604],[-118.2977,36.6104],[-11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,{"id":70175593,"text":"70175593 - 1965 - Selected ground water data in the Eola-Amity Hills area, northern Willamette Valley, Oregon","interactions":[],"lastModifiedDate":"2016-08-17T12:04:25","indexId":"70175593","displayToPublicDate":"1965-01-01T00:00:00","publicationYear":"1965","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":115,"text":"Ground Water Report","active":false,"publicationSubtype":{"id":2}},"title":"Selected ground water data in the Eola-Amity Hills area, northern Willamette Valley, Oregon","docAbstract":"<p><span class=\"EXLDetailsDisplayVal\">Occurrence, quality, and availability of <span class=\"searchword\">ground</span> <span class=\"searchword\">water</span> differ considerably from place to place in the <span class=\"searchword\">Eola</span>-<span class=\"searchword\">Amity</span> <span class=\"searchword\">Hills</span> <span class=\"searchword\">area</span> because of the highly diversified geologic and hydrologic conditions. A table relates the geologic situation to the availability of <span class=\"searchword\">ground</span> <span class=\"searchword\">water</span> for four areas--<span class=\"searchword\">Eola</span>-<span class=\"searchword\">Amity</span> <span class=\"searchword\">Hills</span>, east and west <span class=\"searchword\">valley</span> plains, and <span class=\"searchword\">Willamette</span> River flood plain. Tables show well and spring records, drillers' logs, and chemical analyses of <span class=\"searchword\">ground</span> <span class=\"searchword\">water</span>. The final interpretive report will be published by the U.S. Geological Survey.</span></p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Washington, DC","usgsCitation":"Price, D., and Johnson, N.A., 1965, Selected ground water data in the Eola-Amity Hills area, northern Willamette Valley, Oregon: Ground Water Report.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":518,"text":"Oregon Water Science Center","active":true,"usgs":true}],"links":[{"id":326670,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Oregon","otherGeospatial":"Willamette Valley","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57b58b58e4b03bcb0104bc68","contributors":{"authors":[{"text":"Price, Don","contributorId":30608,"corporation":false,"usgs":true,"family":"Price","given":"Don","email":"","affiliations":[],"preferred":false,"id":645787,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Johnson, Nyra A.","contributorId":173771,"corporation":false,"usgs":false,"family":"Johnson","given":"Nyra","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":645788,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70179723,"text":"70179723 - 1964 - Geology and ground-water resources of the Jordan Valley, Utah","interactions":[],"lastModifiedDate":"2017-09-06T17:26:29","indexId":"70179723","displayToPublicDate":"2016-12-01T00:00:00","publicationYear":"1964","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":5485,"text":"Utah Geological and Mineralogical Survey Water-Resources Bulletin","active":false,"publicationSubtype":{"id":2}},"seriesNumber":"7","title":"Geology and ground-water resources of the Jordan Valley, Utah","docAbstract":"<p>The Jordan Valley occupies about 400 square miles in the central part of Salt Lake County in north-central Utah. Salt Lake City, the capital of Utah, is in the northeastern part of the valley. The valley is at the eastern margin of the Basin and range physiographic province, and it is bounded on the northeast, east, south, and west by mountain ranges. The valley is drained by the Jordan River which enters through a water gap in the mountains to the south, flows north, and empties into the Great Salt Lake, which forms the northwestern border of the valley.</p>","language":"English","publisher":"Utah Geological and Mineralogical Survey","publisherLocation":"Salt Lake City, UT","collaboration":"Prepared in cooperation with the Utah State Engineer","usgsCitation":"Marine, I.W., and Price, D., 1964, Geology and ground-water resources of the Jordan Valley, Utah: Utah Geological and Mineralogical Survey Water-Resources Bulletin 7, 67 p.","productDescription":"67 p.","numberOfPages":"79","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":333200,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":333199,"rank":2,"type":{"id":22,"text":"Related Work"},"url":"https://pubs.usgs.gov/publication/70179625","text":"Utah State Engineer Water 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,{"id":70040819,"text":"70040819 - 1964 - Continental crust","interactions":[],"lastModifiedDate":"2013-01-15T11:50:00","indexId":"70040819","displayToPublicDate":"2012-01-01T00:00:00","publicationYear":"1964","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"seriesTitle":{"id":355,"text":"Crustal Studies Technical Letter","active":false,"publicationSubtype":{"id":6}},"seriesNumber":"20","title":"Continental crust","docAbstract":"The structure of the Earth’s crust (the outer shell of the earth above the M-discontinuity) has been intensively studied in many places by use of geophysical methods. The velocity of seismic compressional waves in the crust and in the upper mantle varies from place to place in the conterminous United States. The average crust is thick in the eastern two-thirds of the United States, in which the crustal and upper-mantle velocities tend to be high. The average crust is thinner in the western one-third of the United States, in which these velocities tend to be low. The concept of eastern and western superprovinces can be used to classify these differences. Crustal and upper-mantle densities probably vary directly with compressional-wave velocity, leading to the conclusion that isostasy is accomplished by the variation in densities of crustal and upper-mantle rocks as well as in crustal thickness, and that there is no single, generally valid isostatic model. The nature of the M-discontinuity is still speculative.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/70040819","collaboration":"In cooperation with the <a href=\"http://www.darpa.mil/\" target=\"_blank\">Defense Advanced Research Projects Agency</a>","usgsCitation":"Pakiser, L.C., 1964, Continental crust: Crustal Studies Technical Letter 20, iv, 24 p., https://doi.org/10.3133/70040819.","productDescription":"iv, 24 p.","numberOfPages":"28","onlineOnly":"Y","additionalOnlineFiles":"N","costCenters":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true}],"links":[{"id":263275,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/misc/tl/0020/"},{"id":263276,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/misc/tl/0020/tl0020.pdf"},{"id":263277,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"country":"United States","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ 144.616667,13.233333 ], [ 144.616667,71.833333 ], [ -64.566667,71.833333 ], [ -64.566667,13.233333 ], [ 144.616667,13.233333 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"50abfbd3e4b0afbc75eb982c","contributors":{"authors":[{"text":"Pakiser, L. C.","contributorId":83512,"corporation":false,"usgs":true,"family":"Pakiser","given":"L.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":469080,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70040815,"text":"70040815 - 1964 - Crustal structure in the eastern Colorado Plateaus Provence from seismic-refraction measurements","interactions":[],"lastModifiedDate":"2012-11-19T14:53:47","indexId":"70040815","displayToPublicDate":"2012-01-01T00:00:00","publicationYear":"1964","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"seriesTitle":{"id":355,"text":"Crustal Studies Technical Letter","active":false,"publicationSubtype":{"id":6}},"seriesNumber":"19","title":"Crustal structure in the eastern Colorado Plateaus Provence from seismic-refraction measurements","docAbstract":"A reversed seismic-refraction profile was recorded in the Colorado Plateaus Province from Hanksville, Utah, to Chinle, Arizona, The velocity of P<sub>g</sub> is 6.2 km/sec, and the true velocity of P<sub>n</sub> is 7.8 km/sec, Waves identified as reflections indicate that an intermediate layer in the crust has a velocity of approximately 6.8 km/sec. Thickness of the crust is 43 km at Chinle and 40 km at Hanksville. The P<sub>n</sub> velocity in the Colorado Plateaus Province is the same as that in the Basin and Range Province, but is significantly lower than Pn in the High Plains of Colorado.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/70040815","collaboration":"In cooperation with the <a href=\"http://www.darpa.mil/\" target=\"_blank\">Defense Advanced Research Projects Agency</a>","usgsCitation":"Roller, J.C., 1964, Crustal structure in the eastern Colorado Plateaus Provence from seismic-refraction measurements: Crustal Studies Technical Letter 19, iv, 28 p., https://doi.org/10.3133/70040815.","productDescription":"iv, 28 p.","numberOfPages":"32","onlineOnly":"Y","additionalOnlineFiles":"N","costCenters":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true}],"links":[{"id":263274,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":263273,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/misc/tl/0019/tl0019.pdf"},{"id":263272,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/misc/tl/0019/"}],"country":"United States","state":"Arizona;Colorado;Utah","city":"Chinle;Hanksville","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -111.0,35.5 ], [ -111.0,39.0 ], [ -109.0,39.0 ], [ -109.0,35.5 ], [ -111.0,35.5 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"50abfbdbe4b0afbc75eb9833","contributors":{"authors":[{"text":"Roller, John C.","contributorId":60642,"corporation":false,"usgs":true,"family":"Roller","given":"John","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":469075,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":5222351,"text":"5222351 - 1964 - A merganser die-off associated with larval eustrongylides","interactions":[],"lastModifiedDate":"2023-01-25T12:16:09.056162","indexId":"5222351","displayToPublicDate":"2010-06-16T12:17:33","publicationYear":"1964","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":948,"text":"Avian Diseases","active":true,"publicationSubtype":{"id":10}},"title":"A merganser die-off associated with larval eustrongylides","docAbstract":"A die-off of red-breasted mergansers on Lake Holly, Virginia Beach, Virginia, was found to be due to a larval Eustrongylides. Massive tissue destruction and hemorrhage was produced by the migration of the larval Eustrongylides. Earlier stages of the same Eustrongylides were found in eastern mosquitofish and silversides upon which the mergansers had been feeding. In addition, residues of DDT were found in mosquitofish, gizzard shad, and five mergansers collected from Lake Holly, and in the tissues of two mergansers from Back Bay, Virginia. However, the information available was insufficient to establish the significance of these residue levels.","language":"English","publisher":"American Association of Avian Pathologists","doi":"10.2307/1587973","usgsCitation":"Locke, L.N., DeWitt, J., Menzie, C.M., and Kerwin, J., 1964, A merganser die-off associated with larval eustrongylides: Avian Diseases, v. 8, no. 3, p. 420-427, https://doi.org/10.2307/1587973.","productDescription":"8 p.","startPage":"420","endPage":"427","numberOfPages":"8","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":193540,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Virginia","city":"Virginia Beach","otherGeospatial":"Lake Holly","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -75.97983598709106,\n              36.83364170891706\n            ],\n            [\n              -75.97174644470215,\n              36.83364170891706\n            ],\n            [\n              -75.97174644470215,\n              36.84269201960632\n            ],\n            [\n              -75.97983598709106,\n              36.84269201960632\n            ],\n            [\n              -75.97983598709106,\n              36.83364170891706\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"8","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b23e4b07f02db6ae171","contributors":{"authors":[{"text":"Locke, L. N.","contributorId":73539,"corporation":false,"usgs":true,"family":"Locke","given":"L.","email":"","middleInitial":"N.","affiliations":[],"preferred":false,"id":336134,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"DeWitt, J.B.","contributorId":89080,"corporation":false,"usgs":true,"family":"DeWitt","given":"J.B.","email":"","affiliations":[],"preferred":false,"id":336135,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Menzie, C. M.","contributorId":67608,"corporation":false,"usgs":true,"family":"Menzie","given":"C.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":336133,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Kerwin, J.A.","contributorId":105394,"corporation":false,"usgs":true,"family":"Kerwin","given":"J.A.","email":"","affiliations":[],"preferred":false,"id":336136,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":52430,"text":"ofr64141 - 1964 - Water resources of the English River, Old Mans Creek, and Clear Creek basins in Iowa","interactions":[],"lastModifiedDate":"2016-02-22T09:17:49","indexId":"ofr64141","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1964","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"64-141","title":"Water resources of the English River, Old Mans Creek, and Clear Creek basins in Iowa","docAbstract":"<p>The surface and ground water resources of a 991 square mile area comprising the drainage basins of English River, Old Mans Creek and Clear Creek are presented. These basins lie to the west and southwest of Iowa City, Iowa, and all three streams are tributary to the Iowa River. The area is comprised of rolling uplands with relatively broad valleys and is devoted mainly to agriculture and livestock farming.</p>\n<p>In general, the surface water use is adversely affected by the high variability of flows and particularly by the critically small minimum flows. Augmentation of the minimum flows by means of storage reservoirs is possible but may be uneconomical in the broad valleys which require a high area to volume ratio.</p>\n<p>The surface water supply is presented in the form of tables and graphs which show information on maximum and minimum flows, mean flow, duration of flow, frequency of low flow and flood flow and storage requirements. Low-flow discharge. profiles for the English River and South Fork English River derived from measurements at partial record and supplementary sites are also shown.</p>\n<p>Ground water is available from shallow wells in nearly all of the area; however, the wells vary widely in productivity and reliability during a drouth. Potentially excellent aquifers may be found in the alluvium which underlies the valleys since similar areas along the lower Iowa River basin have produced yield up to 100 gallons per minute. However, the best and most reliable source of good ground water is the Jordan Sandstone. This aquifer varies from 1,375 feet below ground level in the eastern part of the area to 2,200 feet below ground level at the western end of the area. It is capable of supplying as much as 1,000 gallons per minute to individual wells. Its location is shown in the report by means of map contours referenced to mean sea level.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Iowa City","doi":"10.3133/ofr64141","collaboration":"Prepared in Cooperation with the Iowa Natural Resources Council","usgsCitation":"Schwob, H., 1964, Water resources of the English River, Old Mans Creek, and Clear Creek basins in Iowa: U.S. Geological Survey Open-File Report 64-141, v, 53 p., https://doi.org/10.3133/ofr64141.","productDescription":"v, 53 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":351,"text":"Iowa Water Science Center","active":true,"usgs":true}],"links":[{"id":264318,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1964/0141/report-thumb.jpg"},{"id":264317,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1964/0141/report.pdf","size":"4108","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Iowa","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -91.56005859375,\n              41.68419444691368\n            ],\n            [\n              -91.55593872070311,\n              41.64007838467894\n            ],\n            [\n              -91.52572631835938,\n              41.57641597789266\n            ],\n            [\n              -91.52023315429688,\n              41.51371908287346\n            ],\n            [\n              -91.50100708007811,\n              41.457136982923494\n            ],\n            [\n              -91.6094970703125,\n              41.430371882652814\n            ],\n            [\n              -91.7303466796875,\n              41.38196080315539\n            ],\n            [\n              -91.8511962890625,\n              41.384021583849886\n            ],\n            [\n              -92.02423095703124,\n              41.39123380197929\n            ],\n            [\n              -92.186279296875,\n              41.422134246213616\n            ],\n            [\n              -92.35244750976562,\n              41.466399253078876\n            ],\n            [\n              -92.47055053710938,\n              41.50240661583931\n            ],\n            [\n              -92.5323486328125,\n              41.55072788140255\n            ],\n            [\n              -92.5872802734375,\n              41.62776153144345\n            ],\n            [\n              -92.69302368164062,\n              41.66162721430806\n            ],\n            [\n              -92.72735595703125,\n              41.682143207256495\n            ],\n            [\n              -92.80838012695312,\n              41.71700538790365\n            ],\n            [\n              -92.76718139648438,\n              41.76209309432243\n            ],\n            [\n              -92.5213623046875,\n              41.72315557551985\n            ],\n            [\n              -92.44720458984375,\n              41.71598029940931\n            ],\n            [\n              -92.373046875,\n              41.72110557838152\n            ],\n            [\n              -92.296142578125,\n              41.713930073371294\n            ],\n            [\n              -92.22747802734375,\n              41.73340458018376\n            ],\n            [\n              -92.16156005859375,\n              41.73442939072102\n            ],\n            [\n              -92.08602905273436,\n              41.739553198140634\n            ],\n            [\n              -92.00225830078125,\n              41.713930073371294\n            ],\n            [\n              -91.95968627929688,\n              41.75287318430239\n            ],\n            [\n              -91.94320678710938,\n              41.766190406938684\n            ],\n            [\n              -91.83609008789062,\n              41.7631174470059\n            ],\n            [\n              -91.7138671875,\n              41.75492216766298\n            ],\n            [\n              -91.60400390625,\n              41.73545418490723\n            ],\n            [\n              -91.56417846679686,\n              41.69650051162981\n            ],\n            [\n              -91.56005859375,\n              41.68419444691368\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f4e4b07f02db5f0573","contributors":{"authors":[{"text":"Schwob, H.H.","contributorId":23171,"corporation":false,"usgs":true,"family":"Schwob","given":"H.H.","email":"","affiliations":[],"preferred":false,"id":245332,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":66715,"text":"i389 - 1964 - Bedrock topography of the eastern and central Mesabi Range, northeastern Minnesota","interactions":[],"lastModifiedDate":"2018-03-19T10:40:10","indexId":"i389","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1964","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":320,"text":"IMAP","code":"I","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"389","subseriesTitle":"NONE","title":"Bedrock topography of the eastern and central Mesabi Range, northeastern Minnesota","docAbstract":"<p>The Mesabi iron-mining district or range, is in north-eastern Minnesota, 60 to 85 miles west of Lake Superior. The Mesabi Range, in this report, includes the iron-mining belt, &frac14; of a mile to 3 miles wide, that extends for 120 miles in a northeasterly direction across Itasca and St. Louis Counties. 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,{"id":63514,"text":"gp445 - 1964 - Aeromagnetic map of western Pennsylvania and parts of eastern Ohio, northern West Virginia, and western Maryland","interactions":[],"lastModifiedDate":"2025-04-24T20:18:45.86874","indexId":"gp445","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1964","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":317,"text":"Geophysical Investigations Map","code":"GP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"445","title":"Aeromagnetic map of western Pennsylvania and parts of eastern Ohio, northern West Virginia, and western Maryland","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/gp445","usgsCitation":"Popenoe, P., Petty, A.J., and Tyson, N., 1964, Aeromagnetic map of western Pennsylvania and parts of eastern Ohio, northern West Virginia, and western Maryland: U.S. Geological Survey Geophysical Investigations Map 445, 1 Plate: 37.08 x 37.06 inches, https://doi.org/10.3133/gp445.","productDescription":"1 Plate: 37.08 x 37.06 inches","costCenters":[],"links":[{"id":485034,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_3389.htm","linkFileType":{"id":5,"text":"html"}},{"id":253152,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gp/0445/report-thumb.jpg"},{"id":249638,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/gp/0445/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":249637,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gp/0445/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"250000","country":"United States","state":"Maryland, Ohio, Pennsylvania, West Virginia","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -81.4167,\n              41.25\n            ],\n            [\n              -81.4167,\n              39.5833\n            ],\n            [\n              -78.8333,\n              39.5833\n            ],\n            [\n              -78.8333,\n              41.25\n            ],\n            [\n              -81.4167,\n              41.25\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae4e4b07f02db689ea0","contributors":{"authors":[{"text":"Popenoe, Peter","contributorId":62206,"corporation":false,"usgs":true,"family":"Popenoe","given":"Peter","email":"","affiliations":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":false,"id":269024,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Petty, A. J.","contributorId":35384,"corporation":false,"usgs":true,"family":"Petty","given":"A.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":269023,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Tyson, N.S.","contributorId":28674,"corporation":false,"usgs":true,"family":"Tyson","given":"N.S.","email":"","affiliations":[],"preferred":false,"id":269022,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
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,{"id":64202,"text":"gp474 - 1964 - Aeromagnetic and geologic map of east-central Minnesota","interactions":[],"lastModifiedDate":"2022-04-11T20:36:22.949528","indexId":"gp474","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1964","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":317,"text":"Geophysical Investigations Map","code":"GP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"474","title":"Aeromagnetic and geologic map of east-central Minnesota","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/gp474","usgsCitation":"Bath, G.D., Schwartz, G.M., and Gilbert, F.P., 1964, Aeromagnetic and geologic map of east-central Minnesota: U.S. Geological Survey Geophysical Investigations Map 474, Report: 1 p.; 1 Plate: 34.62 × 26.53 inches, https://doi.org/10.3133/gp474.","productDescription":"Report: 1 p.; 1 Plate: 34.62 × 26.53 inches","costCenters":[],"links":[{"id":186955,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gp/0474/report-thumb.jpg"},{"id":100749,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/gp/0474/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":100748,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gp/0474/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"250000","country":"United States","state":"Minnesota","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -94,45.75 ], [ -94,47 ], [ -92,47 ], [ -92,45.75 ], [ -94,45.75 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b02e4b07f02db6989e0","contributors":{"authors":[{"text":"Bath, G. D.","contributorId":71968,"corporation":false,"usgs":true,"family":"Bath","given":"G.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":270195,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Schwartz, G. M.","contributorId":20380,"corporation":false,"usgs":true,"family":"Schwartz","given":"G.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":270193,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Gilbert, F. P.","contributorId":53033,"corporation":false,"usgs":true,"family":"Gilbert","given":"F.","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":270194,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":63516,"text":"gp358 - 1964 - Aeroradioactivity of parts of east-central New York and west-central New England","interactions":[],"lastModifiedDate":"2021-11-26T22:44:33.941515","indexId":"gp358","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1964","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":317,"text":"Geophysical Investigations Map","code":"GP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"358","title":"Aeroradioactivity of parts of east-central New York and west-central New England","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/gp358","usgsCitation":"Popenoe, P., 1964, Aeroradioactivity of parts of east-central New York and west-central New England: U.S. Geological Survey Geophysical Investigations Map 358, 1 Plate: 53.62 × 39.38 inches, https://doi.org/10.3133/gp358.","productDescription":"1 Plate: 53.62 × 39.38 inches","costCenters":[],"links":[{"id":253154,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gp/0358/report-thumb.jpg"},{"id":249642,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/gp/0358/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":392163,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_3293.htm"},{"id":249641,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gp/0358/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"250000","country":"United States","state":"Massachusetts, New Hampshire, New York, Vermont","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -74.9583,\n              42\n            ],\n            [\n              -71.0833,\n              42\n            ],\n            [\n              -71.0833,\n              43.75\n            ],\n            [\n              -74.9583,\n              43.75\n            ],\n            [\n              -74.9583,\n              42\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae4e4b07f02db689b10","contributors":{"authors":[{"text":"Popenoe, Peter","contributorId":62206,"corporation":false,"usgs":true,"family":"Popenoe","given":"Peter","email":"","affiliations":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":false,"id":269026,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":52399,"text":"ofr6458 - 1964 - Ground water in the Navajo Sandstone at the east entrance, Zion National Park, Utah","interactions":[],"lastModifiedDate":"2017-09-06T16:39:30","indexId":"ofr6458","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1964","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"64-58","title":"Ground water in the Navajo Sandstone at the east entrance, Zion National Park, Utah","docAbstract":"<p>No abstract available.</p>","language":"English","doi":"10.3133/ofr6458","usgsCitation":"Gates, J.S., 1964, Ground water in the Navajo Sandstone at the east entrance, Zion National Park, Utah: U.S. Geological Survey Open-File Report 64-58, 23 p., https://doi.org/10.3133/ofr6458.","productDescription":"23 p.","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":177778,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"country":"United States","state":"Utah","otherGeospatial":"Zion National Park","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ab0e4b07f02db66d925","contributors":{"authors":[{"text":"Gates, J. S.","contributorId":99553,"corporation":false,"usgs":true,"family":"Gates","given":"J.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":245281,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":12572,"text":"ofr6410 - 1964 - Lower Permian stratigraphy of east-central Nevada and adjacent Utah","interactions":[],"lastModifiedDate":"2026-01-20T18:51:18.957146","indexId":"ofr6410","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1964","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"64-10","title":"Lower Permian stratigraphy of east-central Nevada and adjacent Utah","docAbstract":"<p>The Permian section near Ely, Nevada, consists of, in ascending order: Riepe Spring Limestone, a bluff-forming limestone with abundant corals, and Reipetown Sandstone, a buff to red very coarse-grained siltstone with minor carbonates, both formations of Steele (1960); Arcturus Formation, divisible into a Lower Member composed of alternating medium-bedded limestone and buff siltstone, and an Upper Member composed of alternating thin-bedded limestone and buff to red siltstone and gypsum; and Kaibab Limestone, a massive bioclastic limestone. The Wolfcamp-Leonard boundary occurs within the Arcturus Formation. West of Ely the Riepe Spring Limestone and Reipetown Sandstone thin and change into thin-bedded cherty limestone. These beds, plus the basal part of the Arcturus Formation, form the Carbon Ridge Formation at Dry Mountain at Eureka. At Dry Mountain, minor clastic chert occurs in the Arcturus Formation, and beyond to the west clastic chert replaces most of the limestone to form the conglomeratic Garden Valley Formation. The cherty limestone at the base of the Garden Valley is apparently equivalent to the upper part of the Carbon Ridge Formation at Carbon Ridge. Eastward in Utah the Riepe Spring Limestone is recognizable in the Confusion Range, but is almost unrecognizable in the Needle Range. The dolomite content in the Reipetown Sandstone usually increases to 25 percent of the formation in the Confusion and Needle ranges. The Arcturus Formation thins and undergoes moderate lithologic changes. It is equivalent to the rocks above a horizon 300 feet below Bed A of the Arcturus Formation as mapped in the Confusion Range by Hose and Repenning (1959, 1963).</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr6410","usgsCitation":"Barosh, P.J., 1964, Lower Permian stratigraphy of east-central Nevada and adjacent Utah: U.S. Geological Survey Open-File Report 64-10, Report: 144 p.;  10 Plates: 79.84 x 42.75 inches ; 3 Tables, https://doi.org/10.3133/ofr6410.","productDescription":"Report: 144 p.;  10 Plates: 79.84 x 42.75 inches ; 3 Tables","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":311529,"rank":15,"type":{"id":27,"text":"Table"},"url":"https://pubs.usgs.gov/of/1964/0010/table-03.pdf","text":"Table 3","linkFileType":{"id":1,"text":"pdf"}},{"id":311527,"rank":13,"type":{"id":27,"text":"Table"},"url":"https://pubs.usgs.gov/of/1964/0010/table-01.pdf","text":"Table 1","linkFileType":{"id":1,"text":"pdf"}},{"id":311526,"rank":12,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1964/0010/plate-12.pdf","text":"Plate 12","linkFileType":{"id":1,"text":"pdf"}},{"id":311525,"rank":11,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1964/0010/plate-11.pdf","text":"Plate 11","linkFileType":{"id":1,"text":"pdf"}},{"id":311524,"rank":10,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1964/0010/plate-10.pdf","text":"Plate 10","linkFileType":{"id":1,"text":"pdf"}},{"id":498785,"rank":16,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_119130.htm","linkFileType":{"id":5,"text":"html"}},{"id":311523,"rank":9,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1964/0010/plate-09.pdf","text":"Plate 9","linkFileType":{"id":1,"text":"pdf"}},{"id":311522,"rank":8,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1964/0010/plate-08.pdf","text":"Plate 8","linkFileType":{"id":1,"text":"pdf"}},{"id":311528,"rank":14,"type":{"id":27,"text":"Table"},"url":"https://pubs.usgs.gov/of/1964/0010/table-02.pdf","text":"Table 2","linkFileType":{"id":1,"text":"pdf"}},{"id":311521,"rank":7,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1964/0010/plate-07.pdf","text":"Plate 7","linkFileType":{"id":1,"text":"pdf"}},{"id":311520,"rank":6,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1964/0010/plate-06.pdf","text":"Plate 6","linkFileType":{"id":1,"text":"pdf"}},{"id":311519,"rank":5,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1964/0010/plate-05.pdf","text":"Plate 5","linkFileType":{"id":1,"text":"pdf"}},{"id":311518,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1964/0010/plate-04.pdf","text":"Plate 4","linkFileType":{"id":1,"text":"pdf"}},{"id":146246,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1964/0010/report-thumb.jpg"},{"id":40963,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1964/0010/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":311517,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1964/0010/plate-03.pdf","text":"Plate 3","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Nevada, Utah","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -116.2,\n              39.9\n            ],\n            [\n              -116.2,\n              38.7\n            ],\n            [\n              -113.5,\n              38.7\n            ],\n            [\n              -113.5,\n              39.9\n            ],\n            [\n              -116.2,\n              39.9\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a7fe4b07f02db648961","contributors":{"authors":[{"text":"Barosh, Patrick James","contributorId":42184,"corporation":false,"usgs":true,"family":"Barosh","given":"Patrick","email":"","middleInitial":"James","affiliations":[],"preferred":false,"id":166359,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":1042,"text":"wsp1779N - 1964 - Geology and ground-water resources in eastern Cheyenne and Kiowa Counties, Colorado","interactions":[],"lastModifiedDate":"2022-12-30T21:06:03.016628","indexId":"wsp1779N","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1964","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":"1779","chapter":"N","title":"Geology and ground-water resources in eastern Cheyenne and Kiowa Counties, Colorado","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wsp1779N","usgsCitation":"Boettcher, A.J., and Horr, C.A., 1964, Geology and ground-water resources in eastern Cheyenne and Kiowa Counties, Colorado: U.S. Geological Survey Water Supply Paper 1779, Report: iv, 32 p.; 3 Plates: 17.00 x 35.70 inches or smaller, https://doi.org/10.3133/wsp1779N.","productDescription":"Report: iv, 32 p.; 3 Plates: 17.00 x 35.70 inches or smaller","costCenters":[],"links":[{"id":110016,"rank":6,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_24963.htm","linkFileType":{"id":5,"text":"html"},"description":"24963"},{"id":25695,"rank":5,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1779n/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":25694,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1779n/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":25696,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1779n/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":25693,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1779n/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":138007,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1779n/report-thumb.jpg"}],"country":"United States","state":"Colorado","county":"Cheyenne County, Kiowa County","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -103.164,\n              39.042\n            ],\n            [\n              -103.164,\n              38.265\n            ],\n            [\n              -102.044,\n              38.265\n            ],\n            [\n              -102.044,\n              39.042\n            ],\n            [\n              -103.164,\n              39.042\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a61e4b07f02db635b3e","contributors":{"authors":[{"text":"Boettcher, Arnold J.","contributorId":93025,"corporation":false,"usgs":true,"family":"Boettcher","given":"Arnold","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":143080,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Horr, C. Albert","contributorId":43333,"corporation":false,"usgs":true,"family":"Horr","given":"C.","email":"","middleInitial":"Albert","affiliations":[],"preferred":false,"id":143079,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":3662,"text":"cir494 - 1964 - Ground water east of Jackson Lake, Grand Teton National Park, Wyoming","interactions":[],"lastModifiedDate":"2022-02-02T21:31:15.484531","indexId":"cir494","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1964","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":"494","title":"Ground water east of Jackson Lake, Grand Teton National Park, Wyoming","docAbstract":"The project area, which lies east of and adjacent to Jackson Lake is on the downthrown eastern block of the Teton fault, a normal fault that trends northward along the west edge of Jackson Lake. Rocks of pre-Cretaceous age are deeply buried beneath this area. Sedimentary rocks of Cretaceous age and sedimentary and volcanic rocks of Tertiary age, which have an aggregate thickness of about 30,000 feet, are exposed in the northern and eastern parts of the area. Along most of the east side of Jackson Lake, unconsolidated glacial and interglacial deposits of Quaternary age overlie the rocks of Cretaceous and Tertiary age. The unconsolidated deposits were penetrated by test drilling to a depth of 206 feet, but the maximum thickness is probably much greater. Test wells were drilled in five localities to evaluate the deposits of Quaternary age as possible sources of ground water for National Park Service facilities. In the Pilgrim Creek valley, test wells were capable of yielding 200 gpm (gallons per minute); properly constructed production wells could obtain much greater yields. Test wells at Lizard Point and Jackson Lake Campgrounds yielded more than 100 gpm, and a test well near the confluence of the Buffalo Fork and Snake rivers yielded 30 gpm. A test hole drilled in the NW1/4 sec. 36, T. 46 N., R. 115 W., was dry at 200 feet. Unconsolidated deposits of Quaternary age are the most promising source of additional ground water. Because of the extreme range in grain size and sorting, these deposits vary greatly in permeability. Their saturated thickness ranges from 0 to more than 130 feet and changes seasonally; variations of as much as 36 feet were measured (1961-62) in the Pilgrim Creek valley. In most localities where deposits of Quaternary age are ,present, small to moderate ground-water supplies can be developed; larger ground-water supplies can be developed in parts of the Pilgrim Creek valley. One well taps the Bivouac Formation of Late Pliocene or Pleistocene age, but no other wells are known to tap rocks of possible pre-Quaternary age. The Harebell Formation and Bacon Ridge Sandstone of Late Cretaceous age and the Bivouac Formation offer the best possibilities for development of additional water supplies from the consolidated rocks. Chemical analyses of water samples from 11 wells in the deposits of Quaternary age and 1 well in the Bivouac Formation indicate that the water is of generally good quality for drinking and most other purposes. Water from one well tapping lacustrine(?) sand had a dissolved-solids content of 321 ppm (parts per million); all other samples had from 87 to 145 ppm.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Washington, D.C.","doi":"10.3133/cir494","collaboration":"Prepared in cooperation with the National Park Service","usgsCitation":"McGreevy, L., and Gordon, E.D., 1964, Ground water east of Jackson Lake, Grand Teton National Park, Wyoming: U.S. Geological Survey Circular 494, Report: iv, 27 p.; 1 Plate: 16.90 x 21.58 inches, https://doi.org/10.3133/cir494.","productDescription":"Report: iv, 27 p.; 1 Plate: 16.90 x 21.58 inches","numberOfPages":"32","costCenters":[],"links":[{"id":395311,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_23905.htm"},{"id":30702,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/0494/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":124436,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/0494/report-thumb.jpg"},{"id":271081,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/circ/0494/plate-1.pdf"}],"country":"United States","state":"Wyoming","otherGeospatial":"Grand Teton National Park, Jackson Lake","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -110.753173828125,\n              43.8008364060122\n            ],\n            [\n              -110.753173828125,\n              44.067853669357596\n            ],\n            [\n              -110.4345703125,\n              44.067853669357596\n            ],\n            [\n              -110.4345703125,\n              43.8008364060122\n            ],\n            [\n              -110.753173828125,\n              43.8008364060122\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ab0e4b07f02db66dc4f","contributors":{"authors":[{"text":"McGreevy, Laurence J.","contributorId":98706,"corporation":false,"usgs":true,"family":"McGreevy","given":"Laurence J.","affiliations":[],"preferred":false,"id":147362,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Gordon, Ellis D.","contributorId":12451,"corporation":false,"usgs":true,"family":"Gordon","given":"Ellis","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":147361,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
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