The #map displays the Cascadia subduction zone #offshore Oregon, indicating #seismic line 15 from cruise RR1718. Red stars mark Site 174 from DSDP Leg 18 and Site 892 from ODP Leg 146. Water depths range from 3,000 to 0-m at the #coastline. The #bathymetry uses the Global Multi-Resolution Topography (GMRT) database. Another map shows the eastern half of seismic line 15, featuring the head scarp from the 44-N slide, a debris field with large blocks, and an interpreted in situ deformation zone. Water depths range from 3,000 to 1,300-m. The bathymetry uses the GMRT database. Panel (c) provides a detailed view of the main head scarp, evacuation zone, blocks within the debris field, and frontal deformation zone. Panel (d) offers a close-up of the deformation zone, characterized by thrust faults, folding, and drape layers indicating in situ deformation from the landslide impact. Adapted from Lenz et al., (2019).
A recent study by The Ohio State University has revealed a novel method for determining the velocity of past #underwater landslides, focusing on the 44-N Slide off the Oregon #coast within the Cascadia Subduction Zone (CSZ). The CSZ, known for powerful #earthquakes, can lead to underwater #landslides and subsequent #tsunamis.
The study examined the 44-N Slide, uncovering that it covered a horizontal distance of 10 kilometers with a 13-degree slope, dropping 1,200 meters. The impact on the #seafloor occurred at a velocity of 60 meters per second, suggesting a potentially "tsunamigenic" event. Published in Geophysical Research Letters, the research underscores the significance of understanding underwater landslides to mitigate the associated #tsunami risks, emphasizing the need for improved seafloor imaging technologies.
These findings contribute not only to the protection of coastal communities but also to the preservation of underwater #cables and the formulation of effective emergency response plans. Supported by the National Science Foundation, the study's insights offer a global perspective, and the methodology developed can be valuable for researchers modeling underwater landslide deformation zones in different parts of the world. 🔎🌊⚠️
[Lenz, B. L., Griffith, W. A., & Sawyer, D. E. (2023). Impact-induced seafloor deformation from #submarine landslides: Diagnostic of slide velocity? Geophysical Research Letters, 50, e2023GL104818. https://lnkd.in/dkjjryb4]
Ph.D Geologist & Geophysicist at LAPS Consulting Ltda.
4moI love shallow water geophysics. Will be possible to see the data?