The Queen Charlotte Fault is an active transform fault that marks the boundary of the North American and the Pacific Plates.It is Canada's right-lateral strike-slip equivalent to the San Andreas Fault to the south in California. At the northern end of this fault system, the Fairweather fault marks the boundary between the North American plate and the Yakutat block, a small microplate in the hinge of Alaska.
The Sitka Sound Science Center is part of an international team of scientists probing the depths of the northeast Pacific offshore of Alaska and British Columbia, Canada, to better understand hazards associated with the Queen Charlotte Fault, which forms a 700 mile boundary between the Pacific and North American tectonic plates. Queen Charlotte Fault: | | ||| | Tectonic map of Alaska and northwestern Canada showing... World Heritage Encyclopedia, the aggregation of the largest online encyclopedias available, and the most definitive collection ever assembled. Here, the Pacific plate and the North America plate are moving along each other. It is Canada's right-lateral strike-slip equivalent to the San Andreas Fault to the south in California. The Queen Charlotte fault, often called the ‘San Andreas of the North,’ is a strike-slip plate boundary that separates the Pacific and North American tectonic plates offshore western Canada and Southeast Alaska. Details. Detailed Description. Queen Charlotte Terrace The Queen Charlotte Terrace is a 25 kilometre wide zone of built up marine sediment immediately west of the active Queen Charlotte fault. A transform fault is a horizontal motion that occurs when two plates are forced to move along each other (see figure 2). On Haida Gwaii, the earth’s crust is 18 kilometres thick at the eastern edge. Between 2012 and 2014, renewed seismic events on the Queen Charlotte-Fairweather Fault system caused a series of moderate to large earthquakes, including the 2012 M7.8 Haida Gwaii earthquake, the 2013 M7.5 Craig earthquake and the 2014 M6.0 Palma Bay earthquake. Between 2012 and 2014, renewed seismic events on the Queen Charlotte-Fairweather Fault system caused a series of moderate to large earthquakes, including the 2012 M7.8 Haida Gwaii earthquake, the 2013 M7.5 Craig earthquake and the 2014 M6.0 Palma Bay earthquake. An important tectonic boundary, the Fairweather-Queen Charlotte fault system, runs along the western coast of the park. The Queen Charlotte Fault is an active transform fault that marks the boundary of the North American and the Pacific Plates.It is Canada's right-lateral strike-slip equivalent to the San Andreas Fault to the south in California.The Queen Charlotte Fault forms a triple junction on its south with the Cascadia subduction zone and the Explorer Ridge (the Queen Charlotte Triple Junction). The Queen Charlotte Fault is an active transform fault that marks the boundary of the North American and the Pacific Plates. The Queen Charlotte Fault forms a triple junction on its south with the Cascadia subduction zone and the Explorer Ridge (the Queen Charlotte Triple Junction). Seabed expression of the Queen Charlotte Fault in southeastern Alaska.
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