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4 edition of Analysis of Cenozoic subsidence at three sites in vicinity of the Seattle basin, Washington found in the catalog.

Analysis of Cenozoic subsidence at three sites in vicinity of the Seattle basin, Washington

Samuel Y. Johnson

Analysis of Cenozoic subsidence at three sites in vicinity of the Seattle basin, Washington

by Samuel Y. Johnson

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  • 5 Currently reading

Published by U.S. Dept. of the Interior, U.S. Geological Survey, [Books and Open-File Reports Section, distributor] in Denver, Colo .
Written in English

    Subjects:
  • Paleogeography -- Washington (State) -- Seattle Region.,
  • Subsidence (Earth movements) -- Washington (State) -- Seattle Region.,
  • Geology, Stratigraphic -- Cenozoic.

  • Edition Notes

    Statementby Samuel Y. Johnson.
    SeriesOpen-file report -- 93-332., U.S. Geological Survey open-file report -- 93-332.
    ContributionsGeological Survey (U.S.)
    The Physical Object
    FormatMicroform
    Pagination17 leaves
    Number of Pages17
    ID Numbers
    Open LibraryOL17751607M

    preliminary evaluation of basin margin exhumation and provenance of cenozoic strata, chuitna and beluga rivers area, cook inlet forearc basin, alaska by emily s. finzel, robert j. gillis, kenneth a. ridgway, and david l. lepain june this report has not been reviewed for technical content (except as noted in text) or forFile Size: 1MB.   Historical Geology: Cenozoic, basin and range FTCC - Geology Online. Loading Unsubscribe from FTCC - Geology Online? Cancel Unsubscribe. Working Subscribe Subscribed Unsubscribe K.

    Washington ‘ Livingston, Missoula, Montana ‘ Bluff St. #, Boulder, Colorado years ago) are widespread in the Lewiston basin and reported for the first time from the lower Salmon and Grande Ronde canyons. All of the late Cenozoic File Size: 1MB. Climate in Earth History: Studies in Geophysics. Washington, DC: The National Academies Press. doi: / Figure shows that subsidence in the area of the well follows a normal thermal contraction curve from the time of initial formation of oceanic crust (± Ma) to the Late Oligocene, when uplift associated with the High.

    These deposits preserve a high-fidelity record of late Cenozoic subsidence and basin filling that resulted from deformation in the San Andreas fault system of southern California. Existing and new paleomagnetic data, combined with new U-Pb zircon ages of two tuffs high in the section, show that the section ranges in age from ca. ± Ma. distinct geographic area bordered by the Pacific Ocean, the Strait of Juan de Fuca, and the Puget Lowlands, it contains high-relief mountains, a gradient of rainfall unmatched anywhere in the coterminous United States, forests capable of producing some of the.


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Analysis of Cenozoic subsidence at three sites in vicinity of the Seattle basin, Washington by Samuel Y. Johnson Download PDF EPUB FB2

The item Analysis of Cenozoic subsidence at three sites in vicinity of the Seattle basin, Washington, by Samuel Y. Johnson represents a specific, individual, material embodiment of a distinct intellectual or artistic creation found in Indiana State Library.

reconstruct Cenozoic subsidence at three locations in the vicinity of the Seattle basin: (1) the Mobil Kingston #1 borehole; (2) the western part of the Seattle basin; and (3) the Tiger Mountain-Newport Hills area (fig.

The constraints and uncertainties for each of theAuthor: Samuel Y. Johnson. Get this from Washington book library.

Analysis of Cenozoic subsidence at three sites in vicinity of the Seattle basin, Washington. [Samuel Y Johnson; Geological Survey (U.S.)].

Stanford Libraries' official online search tool for books, media, journals, databases, government documents and more. Buy Analysis of Cenozoic subsidence at three sites in vicinity of the Seattle basin, Washington (SuDoc I ) by Samuel Y. Johnson (ISBN:) from Amazon's Book Store.

Everyday low prices and free delivery on eligible : Samuel Y. Johnson. Subsidence analysis of the Lunpola basin exhibited a persistent subsiding history from the Eocene to the early Miocene (Ma et al., ), also supportive of our inference.

Late-Cenozoic stratigraphy and tectonic evolution within a subsiding basin, south-central Washington. Origin and evolution of the Seattle fault and Seattle basin, WashingtonCited by: The city of Seattle straddles the Seattle uplift, the Seattle fault zone, and the Seattle basin, three major bedrock structures that reflect north-south crustal shortening in the Puget Lowland.

Tertiary bedrock is exposed in isolated locations in south Seattle on the Seattle uplift, and then it drops to m below ground under the north half of the city in the Seattle basin. The city of Seattle straddles the Seattle uplift, the Seattle fault zone, and the Seattle basin, three major bedrock structures that reflect north-south crustal shortening in the Puget Lowland.

Tertiary bedrock is exposed in isolated locations in south Seattle on the Seattle uplift. Start studying Historical Geology Chapter 14 Quiz. Learn vocabulary, terms, and more with flashcards, games, and other study tools.

The mountain building events of the west coast that began in the Jurassic and continued into the Cenozoic are collectively called the Sonoma orogeny Antler orogeny the shallow restricted basin was conducive.

Along the eastern boundary of the Cenozoic North Sea Basin the Sorgenfrei–Tornquist Zone is characterized by a complex zone of major normal, reverse and strike–slip faults (Fig.

1), which were active through the Mesozoic and Cenozoic (Hansen et al.,Michelsen and Nielsen,Mogensen and Jensen,Mogensen and Korstgård, Cited by: The Cenozoic succession in the L08 block can be subdivided into two main packages, which are separated by the Mid-Miocene Unconformity (MMU).

In the lower package, a complicated fault pattern was observed, which could be mapped in detail using the volume attribute by: Geologic investigations on southern Bainbridge Island, for example, indicate that a magnitude-7 earthquake occurred about 1, years ago on the Seattle Fault.

The effects of that earthquake include 16 to 23 feet of uplift on the south side of the fault, subsidence north of the fault in the Seattle Basin. Geohistory analysis reveals: (1) moderate subsidence ( mm/yr) from ca.

to Ma; (2) rapid subsidence ( mm/yr) from to Ma; (3) moderate subsidence ( mm/yr) from to Ma; and (4) rapid uplift and erosion that Cited by: The results of a stratigraphic study of the western Victoria Land Basin, Antarctica, are summarized. This analysis is based on all existing seismic Cited by: tions based on subsidence patterns.

SUBSIDENCE ANALYSIS Subsidence analysis yields a graphic repre-sentation of the vertical movement of a strati-graphic horizon, with respect to a datum in a sedimentary basin.

It tracks the subsidence and uplift history at that location since the horizon was deposited (van Hinte, ). Data needed. Abstract. The Ganges—Brahmaputra Delta is one of the most densely populated areas of the world. The delta occupies most of the Bengal Basin and is slowly subsiding as a result of isostatic adjustment of the crust due to rise of the Himalayas and dewatering of the Proto-Bengal Fan sediments which is now buried under thick Mio-Pliocene-Pleistocene deltaic by: Slip occurs beneath area of sustained subsidence interpreted to be the result of basal subduction erosion.

(b) Seismic reflection profile across outer shelf and slope off Chile Island [Mordojovich, ], source region of great Chile earthquake (M w ). Basin is underlain by continental crust, which extends nearly to the by: minute educational film about sea floor mapping and tsunami and earthquake hazards,by Joram ten Brink For a DVD copy of the movie, please contact: Dr.

Uri ten Brink, U.S. Geological Survey, Woods Hole Science Center Woods Hole Road, Woods Hole, MA ; [email protected] The concept Geology, Stratigraphic -- Cenozoic represents the subject, aboutness, idea or notion of resources found in Brigham Young [email protected]{osti_, title = {Late Cenozoic structure and stratigraphy of south-central Washington}, author = {Reidel, S.P.

and Campbell, N.P. and Fecht, K.R. and Lindsey, K.A.}, abstractNote = {The structural framework of the Columbia Basin began developing before Columbia River Basalt Group (CRBG) volcanism. Prior to Ma, the eastern part of the basin was a relatively stable area.This file is licensed under the Creative Commons Attribution-Share Alike International license.: You are free: to share – to copy, distribute and transmit the work; to remix – to adapt the work; Under the following conditions: attribution – You must give appropriate credit, provide a link to the license, and indicate if changes were made.

You may do so in any reasonable manner, but.