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Palaeotsunamis along Canada's Pacific coast
To fully understand tsunami hazards along Canada's Pacific coast we must consider all
potential sources including local and region-wide earthquakes, volcanic activity, slope …
potential sources including local and region-wide earthquakes, volcanic activity, slope …
Repeated megaturbidite deposition in Lake Crescent, Washington, USA, triggered by Holocene ruptures of the Lake Creek-Boundary Creek fault system
Abstract Lake Crescent, a 180-m-deep, glacially carved lake located on the Olympic
Peninsula in western Washington, USA, overlies the Lake Creek-Boundary Creek fault zone …
Peninsula in western Washington, USA, overlies the Lake Creek-Boundary Creek fault zone …
Post-glacial stratigraphy and late Holocene record of great Cascadia earthquakes in Ozette Lake, Washington, USA
Ozette Lake is an~ 100-m-deep coastal lake located along the outer coast of the Olympic
Peninsula (Washington, USA); it is situated above the locked portion of the northern …
Peninsula (Washington, USA); it is situated above the locked portion of the northern …
Holocene surface rupture history of an active forearc fault redefines seismic hazard in southwestern British Columbia, Canada
Characterizing the hazard associated with Quaternary‐active faults in the forearc crust of the
northern Cascadia subduction zone has proven challenging due to historically low rates of …
northern Cascadia subduction zone has proven challenging due to historically low rates of …
Ongoing oroclinal bending in the Cascadia forearc and its relation to concave-outboard plate margin geometry
The concave-inboard (concave toward the overriding plate) geometry of most convergent
margins is considered a natural consequence of the depression of the edge of a thin …
margins is considered a natural consequence of the depression of the edge of a thin …
The Devils Mountain fault zone: An active Cascadia upper plate zone of deformation, Pacific Northwest of North America
JV Barrie, HG Greene - Sedimentary Geology, 2018 - Elsevier
Abstract The Devils Mountain Fault Zone (DMFZ) extends east to west from Washington
State to just south of Victoria, British Columbia, in the northern Strait of Juan de Fuca of …
State to just south of Victoria, British Columbia, in the northern Strait of Juan de Fuca of …
Discovery of an Active Forearc Fault in an Urban Region: Holocene Rupture on the X EOL X ELE K‐Elk Lake Fault, Victoria, British Columbia, Canada
Subduction forearcs are subject to seismic hazard from upper plate faults that are often
invisible to instrumental monitoring networks. Identifying active faults in forearcs therefore …
invisible to instrumental monitoring networks. Identifying active faults in forearcs therefore …
Paleoseismic trenching reveals Late Quaternary kinematics of the Leech River fault: Implications for forearc strain accumulation in northern Cascadia
New paleoseismic trenching indicates late Quaternary oblique right‐lateral slip on the Leech
River fault, southern Vancouver Island, Canada, and constrains permanent forearc …
River fault, southern Vancouver Island, Canada, and constrains permanent forearc …
Postglacial 7.0–7.5 Earthquakes on the North Olympic Fault Zone, Washington
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 …
in a zone of west‐northwest‐striking crustal faults herein named the North Olympic fault …
Slip and strain accumulation along the Sadie Creek fault, Olympic Peninsula, Washington
Upper‐plate faulting in the Olympic Peninsula of Washington State results from relative
motion of crustal blocks within the Cascadia forearc and earthquake cycle processes along …
motion of crustal blocks within the Cascadia forearc and earthquake cycle processes along …