Shallow Faulting and Folding beneath South-Central Seattle, Washington State, from Land-Based High-Resolution Seismic-Reflection Imaging

• Published in: The Seismic record Vol. 4; no. 3; pp. 184 - 193
• Main Authors: Stephenson, William J., Odum, Jack K., Pratt, Thomas L.
• Format: Journal Article
• Language: English
• Published: Seismological Society of America 01-07-2024
• ISSN: 2694-4006; 2694-4006
• DOI: 10.1785/0320230050

The geologic framework of the Seattle fault zone (SFZ) has been extensively studied, but the structure and fault strand locations in the central portion of the fault zone through the city of Seattle have remained controversial. Much of what is known about the SFZ has come from light detection and ranging (lidar)-topographic surveys and paleoseismic investigations of fault scarps primarily west of Puget Sound, regional gravity and aeromagnetic modeling, and multiscale marine seismic imaging in waters both west and east of Seattle. We analyze ∼24 km of land-based P-wave seismic-reflection data that fill in a critical gap in our understanding of the SFZ beneath the urban areas of West Seattle, south-central Seattle, and Mercer Island. These data image deformed strata in the upper 1 km, including upwarped Tertiary rock and younger sediments. Collectively, these data provide evidence for multiple Quaternary-active thrust faults, back thrusts, and sub-basins within the SFZ beneath the city of Seattle. The results indicate that multiple and potentially active back thrusts in the upper ∼500 m extend across the length of the SFZ and the entire urban corridor that may be analogous to those on Bainbridge Island west of Puget Sound.