Haida Gwaii 7.7 magnitude earthquake Saturday, October 27, 2012 about 2000 hours PDT.
This quake was caused by a sudden mostly lateral thrust of the Pacific Plate at a depth of 17 kilometres.
The lateral or sideways motion of the plate caused minimal vertical oscillations in the crust resulting in minimal collateral damage.
The quake occurred in a fault system which is distinctly separate from the fault systems to the south which include the San Andreas and Juan de Fuca faults.
An earlier earthquake September 9, 2011 off the west coast of Vancouver Island
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