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Akademický článek

LiDAR and Paleoseismology Solve Earthquake Mystery in the Pacific Northwest, USA

Autor: Brian L. Sherrod, Richard J. Blakely, Craig S. Weaver

Publikováno v: Geophysical Research Letters, Vol 48, Iss 16, Pp n/a-n/a (2021)

Abstract One of the largest historical earthquakes in the U.S. Pacific Northwest occurred on December 15, 1872 near the south end of Lake Chelan. Lack of recognized surface deformation suggested that the earthquake occurred on a blind, perhaps deep,

Externí odkaz: https://doaj.org/article/ebee0655075c4887b7e9df571bb49b15

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Toward an Integrative Geological and Geophysical View of Cascadia Subduction Zone Earthquakes

Publikováno v: Annual Review of Earth and Planetary Sciences, 2021, Vol.49, pp.367-398 [Peer Reviewed Journal]

The Cascadia subduction zone (CSZ) is an exceptional geologic environment for recording evidence of land-level changes, tsunamis, and ground motion that reveals at least 19 great megathrust earthquakes over the past 10 kyr. Such earthquakes are among

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::3cdea04d0b9ac379abf78f9e853c5161
https://doi.org/10.1146/annurev-earth-071620-065605

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Improving Paleoseismic Earthquake Magnitude Estimates with Rupture Length Information: Application to the Puget Lowland, Washington State, U.S.A

Autor: Brian L. Sherrod, Richard H. Styron

Publikováno v: Bulletin of the Seismological Society of America. 111:1139-1153

Both earthquake displacement and rupture length correlate with magnitude, and, therefore, observations of each from past earthquakes can be used to estimate the magnitude of those earthquakes in the absence of instrumental records. We extend the Baye

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::adf16938f9890eefb763bb7b1170b90d
https://doi.org/10.1785/0120200193

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Postglacial Mw 7.0–7.5 Earthquakes on the North Olympic Fault Zone, Washington

Autor: Brian L. Sherrod, Elizabeth R. Schermer, Alan R. Nelson, Jaime Delano, Colin B. Amos, William Cody Duckworth, Stephen Angster

Publikováno v: Bulletin of the Seismological Society of America. 111:490-513

Holocene crustal faulting in the northern Olympic Peninsula of Washington State manifests in a zone of west-northwest-striking crustal faults herein named the North Olympic fault zone, which extends for ∼80 km along strike and includes the Lake Cre

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::7b353a162aad1b5221326256c768a16b
https://doi.org/10.1785/0120200176

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