The epicenter of the historical Seattle earthquake can be located using paleoseismic data
Paleoseismic and geological data, such as coastal subsidence, tsunami deposits, and deformed marine terraces, are standard tools used to locate and analyze historical earthquakes on faults like the Seattle fault zone.
The retrieved literature contains multiple studies confirming that paleoseismic investigations—including stratigraphic, diatom, and geomorphic analysis of Holocene deposits and marine terraces in the Puget Sound region—are directly used to study past earthquakes on the Seattle fault zone and related fault systems. There are no papers refuting the use of paleoseismic data for this purpose.
Eileen Hemphill-Haley. Diatoms as an aid in identifying late-Holocene tsunami deposits. 1996. https://doi.org/10.1177/095968369600600406
Diatom analyses of Holocene deposits help identify tsunami and earthquake sources and locations in the Puget Sound area.
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Elizabeth Davis, et al.. Supplemental Material: Deformed submarine terraces in Puget Sound, Pacific Northwest, indicate only one M >~7.5 earthquake on the Seattle fault zone in the past 11,000 yr. 2026. https://doi.org/10.1130/geol.s.31328836
Deformed submarine terraces and related paleoseismic data provide evidence regarding major earthquakes on the Seattle fault zone.
Elizabeth Davis, et al.. Supplemental Material: Deformed submarine terraces in Puget Sound, Pacific Northwest, indicate only one M >~7.5 earthquake on the Seattle fault zone in the past 11,000 yr. 2026. https://doi.org/10.1130/geol.s.31328836.v2
Paleoseismic investigations of submarine features in Puget Sound shed light on large historical earthquakes on the Seattle fault zone.
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