A magnitude 6.4 earthquake shook southwestern Canada close to Vancouver on Thursday.The epicenter of the quake was once round 130 miles from Tofino, a small district on Vancouver Island within the Pacific Ocean off Canada’s west coast, in keeping with the U.S. Geological Survey. Tofino is round 130 miles west of Vancouver. The quake’s intensity was once round 6.2 miles.A inhabitants of round 2,000 in Tofino could be uncovered to mild shaking, the Survey mentioned.The rumbling was once first detected simply after 8 am native time. Its magnitude was once first estimated at 6.5 by means of the USGS, prior to it was once downgraded to six.4 mins later.Two extra earthquakes shook the similar house in the following few hours – a magnitude 5.4 temblor happened an hour after and some other of magnitude 4.7 hit at round 10:30 native time, USGS reported.An earthquake of a magnitude greater than 6 is thought of as robust, and may just purpose injury to “poorly built structures and different constructions” as much as round 62 miles away, in keeping with the Canadian govt.Dara Goldberg, a analysis geophysicist for USGS, mentioned “neatly over 100” magnitude 6 earthquakes are recorded every year.The USGS mentioned there was once no chance of a tsunami following the quake.The quake comes not up to per week after a magnitude 5 earthquake struck the similar house on Friday morning. The sooner earthquake additionally targeted within the Pacific Ocean off Canada’s beach, just about 150 miles from Tofino, and had the similar recorded intensity.Goldberg mentioned the most recent collection of quakes came about the place the Pacific Plate and the Juan de Fuca Plate meet. “When you have two tectonic plates assembly, it is all the time extra at risk of earthquakes than, say, the center of the continent,” she mentioned.Earthquakes additionally continuously occur in sequences, she mentioned. “You might have those stresses, those pressures that building up on the boundary between two tectonic plates,” she mentioned. An earthquake occurs “when a part of it slips, when it slides one plate in opposition to the opposite.”A magnitude 6.4 earthquake, which is rather sized, may just cause smaller earthquakes “popping off alongside the sides,” she mentioned.