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Full-Text Articles in Physical Sciences and Mathematics
The Spatial And Temporal Evolution Of The Portland And Tualatin Forearc Basins, Oregon, Usa, Darby P. Scanlon, John Bershaw, Ray E. Wells, Ashley R. Streig
The Spatial And Temporal Evolution Of The Portland And Tualatin Forearc Basins, Oregon, Usa, Darby P. Scanlon, John Bershaw, Ray E. Wells, Ashley R. Streig
Geology Faculty Publications and Presentations
The Portland and Tualatin basins are part of the Salish-Puget-Willamette Lowland, a 900-km-long, forearc depression lying between the volcanic arc and the Coast Ranges of the Cascadia convergent margin. Such inland seaways are characteristic of warm, young slab subduction. We analyzed the basins to better understand their evolution and relation to Coast Range history and to provide an improved tectonic framework for the Portland metropolitan area. We model three key horizons in the basins: (1) the top of the Columbia River Basalt Group (CRBG), (2) the bottom of the CRBG, and (3) the top of Eocene basement. Isochore maps constrain …
Late Holocene Paleoseismicity Along The Northern Oregon Coast, Mark Edward Darienzo
Late Holocene Paleoseismicity Along The Northern Oregon Coast, Mark Edward Darienzo
Dissertations and Theses
Marsh paleoseismological studies were conducted in four bays (Necanicum, Nestucca, Siletz, and Yaquina) along the northern Oregon coast and compared with completed studies in two other bays (Netarts and Alsea). Coseismically buried peats were identified in all bays, based on 1) abrupt contacts, decreases in organic content, increases in sand content, increases in beach sand, and changes in diatom assemblages, all from the peat to the overlying sediments, 2) distinct sandy layers and key plant macrofossils, such as Triglochin, above the buried peat, and 3) widespread correlation of the buried peats within the bay. The stratigraphy and the ages and …