Ozette Lake is located above the locked portion of the northern Cascadia megathrust and is relatively isolated from other active faults.
Ozette Lake Paleoseismology
Detailed Description
Ozette Lake is located above the locked portion of the northern Cascadia megathrust and is relatively isolated from other active faults. The lake's sediments have preserved a detailed record of seismic events, including underwater landslide events known as mass transport deposits and related turbidite layers, which were likely triggered by powerful earthquakes.
The USGS has long been involved with deep-sea fault mapping, which typically uses a combination of sonar and sediment sampling to study faults offshore, often far beneath the seafloor. Applying similar techniques to lake sediments is a relatively new and growing field.
Using a combination of high-resolution bathymetry, seismic reflection profiles, and sediment core analysis, researchers were able to reconstruct Ozette Lake's post-glacial stratigraphy and identify 30 to 34 distinct event deposits. These deposits, spanning the last 14,000 years, provide a rare glimpse into the frequency and magnitude of past earthquakes in the region.
Details
Sources/Usage
Public Domain.