Since 2015, scientists have been gathering data on the Queen Charlotte-Fairweather fault system offsite link, a 746-mile long strike-slip fault line that extends from offshore of Vancouver Island, Canada, to the Fairweather Range of southeast Alaska. The Queen Charlotte Fault is an active transform fault that marks the boundary of the North American and the Pacific Plates. This is a strike-slip fault that marks the boundary between the Pacific crustal plate to the southwest and the North American plate to the northeast.
It occurred on the Queen Charlotte Fault (Canada’s equivalent of the San Andreas Fault) – the boundary between the Pacific and North American plates that runs underwater along the west coast of the Queen Charlotte Islands off the west coast of British Columbia.
The team has gathered high resolution bathymetric data through multibeam sonar across 5,792 square miles of the ocean bottom. The largest recorded earthquake that had previously ruptured this section of the fault was the magnitude 8.1 on August 22, 1949. The Queen Charlotte basin produces some of Canada’s largest earthquakes with magnitudes of up to 8.1 in 1949! The team has gathered high-resolution bathymetric data through multibeam sonar across 5,792 square miles of the ocean bottom.
Hope you enjoyed the presentation Any Question or Comments :) Facts The Queen Charlotte Fault is now called the Haida Gwaii. Canada's largest historical earthquake- a magnitude 8.1, occurred along this fault on August 22, 1949.
The M 7.5 earthquake occurred on the Queen Charlotte fault system. Convergence of the Pacific and North American plates along … Geomorphologic expression and surface processes associated with the QCFZ system have been revealed in unprecedented detail by recent seabed mapping surveys. The boundary between these two giant plates is the Queen Charlotte fault - Canada's equivalent of the San Andreas fault. Since 2015, scientists have been gathering data on the Queen Charlotte-Fairweather fault system, a 746-mile long strike-slip fault line that extends from offshore of Vancouver Island, Canada, to the Fairweather Range of southeast Alaska. Queen Charlotte Earthquakes What it is About the Fault A fault line is a fracture in the ground, it occurs when the Earth's tectonic plates move. A notable fault, which borders the basin to the west, is the strike-slip, right-lateral Queen Charlotte fault, which extents from southern Alaska down to the Vancouver triple point (Kristin 2000).
The active Queen Charlotte Fault on the west coast of the Queen Charlotte Islands, British Columbia,Canada, has generated three large earthquakes during … The Queen Charlotte Fault Zone (QCFZ) off western Canada is the northern equivalent to the San Andreas Fault Zone, the Pacific-North American plate boundary. The Queen Charlotte fault trends northwestward from the triple junction region, accommodating approximately 5.5 cm/yr of dextral strike-slip motion along the Pacific:North America plate boundary.
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