A magnitude 6.2 earthquake struck the coast of British Columbia late this evening, according to the US Geological Survey.
See also
- 13 earthquake safety steps to follow when the ground starts shaking
- 43 things every Vancouverite needs in their earthquake emergency kit
- A moderate earthquake could severely damage Cambie Street Bridge: Report
- Pattullo Bridge is getting an advance wind and seismic warning system
- Canada Line now linked to earthquake early-warning sensors
The powerful seismic event at 9:30 pm PST Wednesday had an epicentre 340 km south-southwest of Kitimat, in an area of ocean between northern Vancouver Island and Haida Gwaii.
The epicentre was also near the fault line that divides the Explorer Plate and the North American Plate. The depth of the earthquake was very shallow at only 10 km.
No tsunami warning has been issued.
No tsunami threat to #BC https://t.co/6fAq6cxfmy
— Emergency Info BC (@EmergencyInfoBC) July 4, 2019
Thousands of earthquakes occur in the province every year, but only a small fraction have a magnitude of 3.0 and over. This was the most powerful earthquake in BC since October 21, 2018, when an unusual trio of major earthquakes struck within the span of an hour with magnitudes of 6.5, 6.6, and 6.8 — all in the same area off the northern coast of Vancouver Island.
An earthquake with a magnitude of 6.0 and over is considered a seismic event with significant destructive potency, especially if it were to hit with a shallow depth near population centres.
Fortunately, the epicentre of this evening’s earthquake was over 600 kms from Victoria and Vancouver.
An increase in an earthquake’s magnitude of 1.0, such as the difference between a magnitude 5.0 earthquake and a magnitude 6.0 earthquake, is a 10-fold difference in the energy of an earthquake. As a further example, a magnitude 8.0 earthquake is 1,000 times more powerful than a magnitude 5.0 earthquake.
Contrast Wednesday’s BC seismic event with the 2001 Washington State Nisqually magnitude 6.8 earthquake, which had an epicentre in southern Puget Sound in an area only about 60 km southwest of Seattle. Even though the earthquake had an extremely deep depth of 57 kms, it still created approximately USD$2 billion in property damage, caused 400 injuries and one death, and was strongly felt in Vancouver.
Downtown Seattle’s Alaskan Way Viaduct incurred serious damage from the earthquake to the extent that emergency repairs had to be made.
According to the state government, if the 2001 earthquake had lasted several seconds longer, the viaduct could have experienced a structural failure and collapse. This finding led to the recently-completed USD$3.3-billion tunnel project to replace the viaduct.
See also
- 13 earthquake safety steps to follow when the ground starts shaking
- 43 things every Vancouverite needs in their earthquake emergency kit
- A moderate earthquake could severely damage Cambie Street Bridge: Report
- Pattullo Bridge is getting an advance wind and seismic warning system
- Canada Line now linked to earthquake early-warning sensors
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