Results 11 to 20 of about 5,529 (170)
Earthquake occurrence modeling of large subduction events involves significant uncertainty, stemming from the scarcity of geological data and inaccuracy of dating techniques.
Katsuichiro Goda
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Filling the Gap in Cascadia: The Emergence of Low‐Amplitude Long‐Term Slow Slip
Long‐term slow slip events have been observed at several subduction zones around the globe, where they play an integral part in strain release along megathrust faults.
Carolyn P. Nuyen, David A. Schmidt
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As the number of transboundary conservation initiatives continues to grow in response to the twin threats of climate change and biodiversity loss, so too have calls for Indigenous-led conservation that recognizes Indigenous rights and supports Indigenous
Meade Krosby +3 more
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Isolating non-subduction-driven tectonic processes in Cascadia
Several tectonic processes combine to produce the crustal deformation observed across the Cascadia margin: (1) Cascadia subduction, (2) the northward propagation of the Mendocino Triple Junction (MTJ), (3) the translation of the Sierra Nevada–Great ...
K. A. McKenzie, K. P. Furlong
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Neo-Barroco, the Missing Group of the New American Poetry
The New American Poetry anthology delineated “schools” of North American poetry which have become seminal: The Black Mountain School (Charles Olson, Robert Creeley, Denise Levertov), the New York School (John Ashbery, Barbara Guest, Frank O’Hara), the ...
Paul E. Nelson
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Full margin Cascadia earthquake models
Rupture models for full margin Cascadia earthquakes. Companion data set tot he paper "Deep Coseismic Slip in the Cascadia Megathrust can be Consistent with Coastal Subsidence
Amanda M. Thomas +2 more
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Great earthquakes along the Western United States continental margin: implications for hazards, stratigraphy and turbidite lithology [PDF]
We summarize the importance of great earthquakes (<i>M</i><sub>w</sub> ≳ 8) for hazards, stratigraphy of basin floors, and turbidite lithology along the active tectonic continental margins of the Cascadia subduction ...
C. H. Nelson +3 more
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Coastal subsidence in Oregon, USA, during the Giant Cascadia earthquake of AD 1700 [PDF]
Quantitative estimates of land-level change during the giant AD 1700 Cascadia earthquake along the Oregon coast are inferred from relative sea-level changes reconstructed from fossil foraminiferal assemblages preserved within the stratigraphic record.
Nelson, A.R. +9 more
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Mapping Mantle Flows and Slab Anisotropy in the Cascadia Subduction Zone
The Cascadia margin is an unusual subduction zone characterized by the downdip movement of young and thin oceanic plates, where mantle flow and intraslab deformation are still unclear. Here we present new anisotropic tomography of the Cascadia subduction
Xuran Liang +3 more
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Rezente submarine Mineralbildungen : Abbild geochemischer Prozesse an aktiven Fluidaustrittsstellen im Aleuten- und Cascadia-Akkretionskomplex [PDF]
Subduction zones with accretionary wedges are potential areas for active fluid transport and expulsion. Upward transport of relatively cold fluids is predominately caused by tectonic compression and usually occurs along geologically predefined conduits ...
Greinert, Jens, Greinert, J.
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