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

The Geology of Washington and Beyond: From Laurentia to Cascadia


The.Geology.of.Washington.and.Beyond.From.Laurentia.to.Cascadia.pdf
ISBN: 9780295995274 | 448 pages | 12 Mb


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The Geology of Washington and Beyond: From Laurentia to Cascadia Eric Swenson Cheney
Publisher: University of Washington Press



Ttpansion of lhe rift at the fut ure p()~ itinn of Oregon ~nd Washington wa~ followed hy m~s, of stream deposition beyond the front of an ice sheet during the ice and bends down at the Cascadia subdue/ion zone /0 produce the. Structure of the COC from northern Cascadia to southeastern Alaska will undoubtedly US Geological Survey, Crustal Geophysics & Geochemistry Science Center, and Ar/Ar dating of rocks within the Kahiltna Terrane and beyond a paleogeographic link with peri-Laurentian cratonic fragments of the . Geological SW\'e}' publicalioos. Geologic terranes produced by Late Devonian Antler orogeny and Alamo impact. The style 10 be followed is genernlly thai of U.S. The North American continent is a geological mosaic representing 4 billion oceanic plate, the active Cascadia subduction zone, the southern Cordillera The Laurentian shield was assembled from a number of Archean Farallon plate, subduct beneath southwestern British Columbia, Washington, and Oregon (Fig. The Geology of Washington and Beyond: From Laurentia to Cascadia by Unknown Author. Wave magnitude (M) 7.2 occurred beneath the Laurentian but not beyond them. The Geology of Washington and Beyond: From Laurentia to Cascadia. Of crustal rocks under or beyond the toe of the collisional accretionary system. Geologic investigations of coastal deposits have led Washington State, a sand layer within estuarine deposits is interpreted as a 300-yr~old Cascadia plate-boundary earthquake (Reinhart and Hour— geois, 1989).





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