This report describes, summarizes, and interprets all known bedrock fossil and isotopic age studies for the Mount Hayes quadrangle, eastern Alaska Range, Alaska. The accompanying map shows the location of all known bedrock fossil and isotopic sample localities in the quadrangle on a generalized geologic base map. These fossil and isotopic age data are obtained from new studies, unpublished data of the U.S. Geological Survey, contributed unpublished data, and published data. This report is one result of a five-year mineral resource assessment of the quadrangle that was done during the summers of 1978 through 1982, with additional topical studiesin 1985 and 1986. This report is one part of a folio on the geological, geochemical, geophysical, and mineral-resource assessment studies of the quadrangle prepared as part of the Alaskan Mineral Resource Assessment Program (AMRAP) of the U.S. Geological Survey.
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R.","contributorId":116967,"corporation":false,"usgs":true,"family":"Stone","given":"J.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":510913,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Trask, N.J.","contributorId":31729,"corporation":false,"usgs":true,"family":"Trask","given":"N.J.","email":"","affiliations":[],"preferred":false,"id":510911,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":19788,"text":"ofr92134 - 1992 - New pressure-based water-level sensor used by the U.S. Geological Survey","interactions":[],"lastModifiedDate":"2012-02-02T00:07:35","indexId":"ofr92134","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1992","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":"92-134","title":"New pressure-based water-level sensor used by the U.S. Geological Survey","language":"ENGLISH","publisher":"U.S. Geological Survey ;","doi":"10.3133/ofr92134","usgsCitation":"Latkovich, V., 1992, New pressure-based water-level sensor used by the U.S. Geological Survey: U.S. Geological Survey Open-File Report 92-134, iv, 6 p. :ill. ;28 cm., https://doi.org/10.3133/ofr92134.","productDescription":"iv, 6 p. :ill. ;28 cm.","costCenters":[],"links":[{"id":152539,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1992/0134/report-thumb.jpg"},{"id":49264,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1992/0134/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afee4b07f02db6975b2","contributors":{"authors":[{"text":"Latkovich, V.J.","contributorId":52576,"corporation":false,"usgs":true,"family":"Latkovich","given":"V.J.","email":"","affiliations":[],"preferred":false,"id":181512,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":18924,"text":"ofr92712 - 1992 - Palynological data from Pliocene sediments, DSDP Leg 5 Site 32, northeastern Pacific Ocean","interactions":[],"lastModifiedDate":"2012-02-02T00:07:30","indexId":"ofr92712","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1992","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":"92-712","title":"Palynological data from Pliocene sediments, DSDP Leg 5 Site 32, northeastern Pacific Ocean","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr92712","usgsCitation":"Fleming, R., 1992, Palynological data from Pliocene sediments, DSDP Leg 5 Site 32, northeastern Pacific Ocean (Version 1.0): U.S. Geological Survey Open-File Report 92-712, 24 p. :ill. ;28 cm., https://doi.org/10.3133/ofr92712.","productDescription":"24 p. :ill. ;28 cm.","costCenters":[],"links":[{"id":1085,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/of92-712/","linkFileType":{"id":5,"text":"html"}},{"id":151691,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1992/0712/report-thumb.jpg"},{"id":48325,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1992/0712/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae3e4b07f02db6897bf","contributors":{"authors":[{"text":"Fleming, R. 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Surface geology is generally well \ndefined, but subsurface geology is poorly defined below about \n500 feet. Rocks that underlie the plain form the framework for a \nregional ground-water system that supplies large quantities of \nwater for irrigation and makes the plain nationally important in \nterms of agricultural production.\nThe 15,600-square-mile Snake River Plain is a grabenlike \nstructure that formed in middle Miocene time. The graben may \nhave been formed by oblique extensional forces resulting from \ninteractions between the North American and Pacific tectonic \nplates. The oldest known rocks underlying the plain, penetrated \nin a 14,007-foot-deep test hole northwest of Boise, are of middle \nMiocene age. Miocene volcanic rocks at the plain's margin that \ndip toward and underlie the plain were highly faulted and se- \nverely eroded before the plain was formed.\nFaults along the margins of the eastern part of the plain are \nnot visible at land surface and have been defined chiefly by geo- \nphysical methods. However, well-defined fault systems bound \nthe western part of the plain.\nThe eastern plain is underlain predominantly by Quaternary \nbasalt of the Snake River Group, which is intercalated with \nsedimentary rocks along the margins. Basalt crops out or is less \nthan 10 feet below land surface in the central part of the east- \nern plain and is usually less than 100 feet below land surface \nelsewhere. Geophysical data and drillers' logs indicate that \nQuaternary basalt in the central part of the eastern plain is as \nmuch as 5,000 feet thick. A test hole about 10 miles northeast \nof the Snake River near Wendell provided the first information \nabout deep subsurface stratigraphic relations in that part of the \nplain. The stratigraphic sequence penetrated in the test hole is \nsimilar to that in the north wall of the Snake River canyon be- \ntween Milner and King Hill. In that area, basalt of the Snake \nRiver Group thins toward the river and is underlain by sedi- \nmentary rocks and basalt of the Tertiary and Quaternary Idaho \nGroup.\nThe western plain is underlain mainly by unconsolidated and \nweakly consolidated Tertiary and Quaternary sedimentary rocks \nas much as 5,000 feet thick. Basalt also is present in the west- \nern plain and is most extensive near Mountain Home.\nQuaternary basalt of the Snake River Group, which composes \nmuch of the Snake River Plain regional aquifer system, is highly \ntransmissive. In the eastern plain, a thick sequence of thin- \nlayered basalt flows yields large volumes of water to wells. Wells \nopen to less than 100 feet of the aquifer yield as much as 7,000 \ngallons per minute; yields of 2,000 to 3,000 gallons per minute \nwith only a few feet of drawdown are common. Transmissivity\ncommonly exceeds 100,000 feet squared per day and, in places, 1 \nmillion feet squared per day.\nLarge springs in the Snake River canyon between Milner and \nKing Hill issue at the contact between highly transmissive pil- \nlow lava and less transmissive underlying rocks. In 1980, \nground-water discharge between Milner and King Hill, largely \nspring flow, averaged about 6,000 cubic feet per second.\nIn the western plain, coarse-grained sedimentary deposits are \nthickest and transmissivity is highest along the northern mar- \ngins. The percentage of coarse-grained sedimentary deposits de- \ncreases to the southwest, where lacustrine sedimentary deposits \npredominate.\nIn most of the eastern plain, the upper part of the ground- \nwater system is unconfined. At depth and in much of the west- \nern plain, aquifers are confined.\nAcross most of the plain, Quaternary basalt aquifers overlie \naquifers in the Tertiary Idavada Volcanics and Banbury Basalt \nof the Idaho Group. The older volcanic rocks are typically much \nless transmissive than the Quaternary basalt. Faults and frac- \ntures are permeable zones for water storage and conduits for \nwater movement. In places near the margins of the plain, the \nIdavada Volcanics contains important geothermal aquifers.","language":"English","publisher":"U.S. Government Printing Office","doi":"10.3133/pp1408B","usgsCitation":"Whitehead, R., 1992, Geohydrologic framework of the Snake River plain regional aquifer system, Idaho and eastern Oregon: U.S. Geological Survey Professional Paper 1408, Report: vi, 32 p.; 6 Plates: 37.02 x 20.13 and smaller, https://doi.org/10.3133/pp1408B.","productDescription":"Report: vi, 32 p.; 6 Plates: 37.02 x 20.13 and smaller","numberOfPages":"39","costCenters":[{"id":343,"text":"Idaho Water Science Center","active":true,"usgs":true}],"links":[{"id":97417,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1408b/plate-1.pdf","size":"5843","linkFileType":{"id":1,"text":"pdf"}},{"id":97419,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1408b/plate-3.pdf","size":"2682","linkFileType":{"id":1,"text":"pdf"}},{"id":97420,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1408b/plate-4.pdf","size":"1247","linkFileType":{"id":1,"text":"pdf"}},{"id":97421,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1408b/plate-5.pdf","size":"1137","linkFileType":{"id":1,"text":"pdf"}},{"id":97422,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1408b/plate-6.pdf","size":"2015","linkFileType":{"id":1,"text":"pdf"}},{"id":97418,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1408b/plate-2.pdf","size":"1929","linkFileType":{"id":1,"text":"pdf"}},{"id":120451,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/1408b/report-thumb.jpg"},{"id":67662,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/1408b/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Idaho;Oregon","otherGeospatial":"Snake River Plain","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -111.0,42.0 ], [ -111.0,45.0 ], [ -117.0,45.0 ], [ -117.0,42.0 ], [ -111.0,42.0 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1be4b07f02db6a8eab","contributors":{"authors":[{"text":"Whitehead, R.L.","contributorId":34891,"corporation":false,"usgs":true,"family":"Whitehead","given":"R.L.","email":"","affiliations":[],"preferred":false,"id":222162,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":19850,"text":"ofr92174 - 1992 - Purgeable organic compounds in ground water at the Idaho National Engineering Laboratory, Idaho; 1990 and 1991","interactions":[],"lastModifiedDate":"2026-01-21T17:21:03.163947","indexId":"ofr92174","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1992","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":"92-174","title":"Purgeable organic compounds in ground water at the Idaho National Engineering Laboratory, Idaho; 1990 and 1991","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr92174","usgsCitation":"Liszewski, M.J., and Mann, L., 1992, Purgeable organic compounds in ground water at the Idaho National Engineering Laboratory, Idaho; 1990 and 1991: U.S. Geological Survey Open-File Report 92-174, iv, 19 p., https://doi.org/10.3133/ofr92174.","productDescription":"iv, 19 p.","costCenters":[],"links":[{"id":49329,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1992/0174/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":152651,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1992/0174/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a8fe4b07f02db65573d","contributors":{"authors":[{"text":"Liszewski, M. J.","contributorId":107308,"corporation":false,"usgs":true,"family":"Liszewski","given":"M.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":181628,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Mann, L. J.","contributorId":39392,"corporation":false,"usgs":true,"family":"Mann","given":"L. 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