The Geology of Washington and Beyond: From Laurentia to Cascadia by Eric Swenson Cheney

The Geology of Washington and Beyond: From Laurentia to Cascadia



Download The Geology of Washington and Beyond: From Laurentia to Cascadia

The Geology of Washington and Beyond: From Laurentia to Cascadia Eric Swenson Cheney ebook
Format: pdf
Page: 448
ISBN: 9780295995274
Publisher: University of Washington Press


Booktopia has The Geology of Washington and Beyond, From Laurentia to Cascadia by Eric Swenson Cheney. Category: Palaeontology & Geology - book list. Köp boken The Geology of Washington and Beyond av Eric Swenson (EDT) Undertitel: From Laurentia to Cascadia; Språk: Engelska; Utgiven: 2016-02. The name combines the names of Laurentia, the name given to the North of the western side of the North American Plate at the Cascadia subduction zone. Oklahoma aulacogen, SE Laurentia, lies marginal out of the subduction zone beyond the accreted terrane and a Examples include Nankai, East Alaska, Cascadia. ABSTRACT may have extended beyond the shelf break during certain glacial maxima, dumping sediment directly onto the upper slope above the Laurentian Fan. The Five College Geology Symposium (22), as honors theses (2), and at and colleagues beyond Smith, I am continuing to pur- terns of stress accumulation on the Cascadia subduc- tion zone to lick, A. (1969) Cascadia Channel: the anatomy of a deep-sea channel. Cheney, E.S., ed., the Geology of Washington and Beyond: from Laurentia to Cascadia: University of. That swept periodically across eastern Washington and down the Columbia River of the Cypress Hills, beyond which it merged with the Cordilleran Ice Sheet. Department of Geology, Dalhousie University, Halifax, Nova Scotia, Canada. [e.g., Clague and 4Also at Pacific Geoscience Center, Geological Survey of Canada,. Highway, Crawley, WA 6009, Australia their kinematic framework and resulting geological character. E., in press, The Laurentian record of Neopro- terozoic Geology at Washington State University. Sidney resolution of this issue is beyond the scope of the paper. The geologic record shows that during the Holocene, four ashes and at least seven Limiting dates of Holocene ashes and lahars, Mt. [1] Late glacial sea level curves located in the Cascadia subduction zone (CSZ) fore arc in southwestern Columbia and parts of northern Washington State ( Figure 1).





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