This is a list of earthquakes in Canada.
Date | Place | Lat | Lon | Deaths | Injuries | Mag. | MMI | Comments | |
---|---|---|---|---|---|---|---|---|---|
2018-10-22 | Vancouver Island, British Columbia | 49.335 | -129.289 | 0 | 0 | 6.8 | IV | [1] | |
2017-05-01 | Stikine Region, British Columbia | 59.83 | -136.70 | 0 | 0 | 6.3 | VIII | Minor damage / Doublet earthquake | [2] |
2017-05-01 | Stikine Region, British Columbia | 59.82 | -136.71 | 0 | 0 | 6.2 | VII | [3] | |
2017-01-08 | Nunavut | 74.39 | -92.42 | 0 | 0 | 6.0 | VII | [4] | |
2015-04-24 | South of Haida Gwaii | 51.62 | -130.77 | 0 | 0 | 6.2 | V | [5] | |
2014-07-17 | Yukon | 60.35 | -140.33 | 0 | 0 | 6.0 | VI | [6] | |
2014-04-24 | West of Vancouver Island | 49.64 | -127.73 | 0 | 0 | 6.5 | VI | [7] | |
2013-09-04 | 182 km SW of Bella Bella, British Columbia | 51.18 | -130.23 | 0 | 0 | 6.0 | IV | [8] | |
2013-01-05 | Near Craig, Alaska | 55.23 | -134.86 | 0 | 0 | 7.5 | VI | First supershear earthquake observed in an oceanic plate boundary | |
2015-04-24 | South of Haida Gwaii | 51.62 | -130.77 | 0 | 0 | 6.2 | V | ||
2012-11-08 | West of Vancouver Island | 49.23 | -128.48 | 0 | 0 | 6.1 | IV | [9] | |
2012-10-30 | Haida Gwaii | 52.37 | -131.90 | 0 | 0 | 6.2 | Aftershock of 7.8 earthquake | [10] | |
2012-10-28 | Haida Gwaii | 52.67 | -132.60 | 0 | 0 | 6.3 | V | Aftershock of 7.8 earthquake | [11] |
2012-10-27 | Haida Gwaii | 52.77 | -131.93 | 1 [12] | 7.8 | V | Non-destructive tsunami | [13] | |
2011-09-09 | Vancouver Island | 49.49 | -126.97 | 6.4 Mw | 20–30 second strike-slip intraplate shock | [14] | |||
2010-06-23 | Central Canada | 45.9 | -75.5 | 5.0 Mw | VI | ||||
2009-11-17 | Queen Charlotte Islands, BC | 51.82 | -131.78 | 6.5 Mw | [15] | ||||
2009-07-07 | Baffin Bay | 75.35 | -72.45 | 0 | 0 | 6.1 | [16] | ||
2008-01-05 | Queen Charlotte Islands, BC | 51.07 | -131.06 | 6.5 Mw | Doublet (6.4 Mw shock 40 minutes later) | [15] | |||
2007-10-09 | The Nazko region | 52.88 | -124.8 | ≤4.0 | I | Swarm ended June 2008 | |||
2004-11-02 | Vancouver Island, BC | 49.28 | -128.77 | 6.7 Mw | [15] | ||||
2004-07-19 | Vancouver Island | 49.62 | -126.97 | 0 | 0 | 6.4 | VI | [17] | |
2001-04-14 | Alberta | 56.08 | 119.81 | 0 | 0 | 5.3 | VII | Slight damage | [18] |
2001-02-28 | Puget Sound | 47.19 | -122.66 | 0–1 | 400 | 6.8 Mw | VIII | One possible related heart attack in Washington. | |
2000-01-01 | Timiskaming | 46.84 | -78.92 | 5.2 mN | VI | ||||
1997-11-05 | Quebec City, QC | 46.75 | -71.35 | 1 | 5.2 mN | ||||
1989-12-25 | Ungava Region | 60.12 | -73.6 | 6.0 Mw | IV | First shock in eastern North America with surface faulting | |||
1988-11-25 | Saguenay | 48.12 | -71.18 | 5.9 Mw | VII | ||||
1985-12-23 | The Nahanni region, Northwest Territories | 62.22 | -124.24 | 6.9 Mw | The strongest of a sequence of major earthquakes | ||||
1982-01-09 | Miramichi, NB | 47.00 | -66.60 | 5.7 | Doublet (two days apart) | [19] | |||
1979-02-28 | Southern Yukon–Alaska Border | 60.59 | -141.47 | 7.2 Mw | [19] | ||||
1970-06-24 | Queen Charlotte Islands, BC | 51.77 | -130.76 | 7.4 Mw | [19] | ||||
1958-07-09 | Lituya Bay, Alaska | 58.6 | -137.10 | 5 | 7.8 Mw | XI | Rockfall caused a megatsunami (524 m (1,719 ft) runup) | ||
1949-08-22 | Queen Charlotte Islands, BC | 53.62 | -133.27 | 8.1 Mw | VIII | Non-destructive tsunami | |||
1946-06-23 | Vancouver Island, BC | 49.75 | -124.5 | 2 | 7.5 Mw | VIII | |||
1944-09-05 | Cornwall, ON/Massena, NY | 44.96 | -74.83 | 5.8 Mw | VII | ||||
1935-11-01 | Timiskaming | 46.78 | -79.07 | 6.1 Mw | VII | ||||
1933-11-20 | Baffin Bay | 73.12 | -70.01 | 7.4 Mw | Largest known earthquake north of the Arctic Circle | ||||
1929-11-18 | Grand Banks of Newfoundland | 44.54 | -56.01 | 27–28 | 7.2 Mw | VIII | Underwater slump caused destructive tsunami | ||
1929-05-26 | Queen Charlotte Islands, BC | 51.51 | -130.74 | 7.0 Mw | [19] | ||||
1925-03-01 | Charlevoix–Kamouraska, QC | 47.8 | -69.8 | 6.2 Mw | VIII | ||||
1918-12-06 | Vancouver Island, BC | 49.44 | -126.22 | 7.2 Mw | VII | ||||
1899-09-10 | Yukon–Alaska border | 60.00 | -140.00 | 8.2-8.4 Ms | Part of a complex and not well understood sequence | [20] | |||
1899-09-04 | Yukon–Alaska border | 60.00 | -140.00 | 8.2-8.5 Ms | Part of a complex and not well understood sequence | [19] [20] | |||
1872-12-15 | Washington State | 47.9 | -120.3 | 6.5–7.0 Mw | VIII | ||||
1870-10-20 | Charlevoix, QC | 47.4 | -70.5 | 6 | 6.5 | [21] | |||
1860-10-17 | Charlevoix, QC | 47.5 | -70.1 | 6.0 | [19] | ||||
1791-12-06 | Charlevoix | 47.4 | -70.5 | 6.0 | [19] | ||||
1732-09-16 | Montreal, QC | 45.5 | -73.6 | 0–1 | 5.8 Mw | VIII–IX | |||
1700-01-26 | Pacific Northwest | 45.0 | -125.0 | 8.7–9.2 Mw | Linked to the destructive "orphan tsunami" in Japan | ||||
1663-02-05 | Charlevoix–Kamouraska, QC | 47.6 | -70.1 | 7.3–7.9 Mw | X | ||||
Abbreviations used:
Earthquakes are caused by movements within the Earth's crust and uppermost mantle. They range from weak events detectable only by seismometers, to sudden and violent events lasting many minutes which have caused some of the greatest disasters in human history. Below, earthquakes are listed by period, region or country, year, magnitude, cost, fatalities, and number of scientific studies.
Moresby Island is a large island (3,399.39 km2 [1,312.51 sq mi]) that forms part of the Haida Gwaii archipelago in British Columbia, Canada, located at 53°04′44″N132°07′40″W It is separated by the narrow Skidegate Channel from the other principal island of the group to the north, Graham Island.
The Queen Charlotte Fault is an active transform fault that marks the boundary of the North American plate and the Pacific plate. 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 south with the Cascadia subduction zone and the Explorer Ridge. The Queen Charlotte Fault (QCF) forms a transpressional plate boundary, and is as active as other major transform fault systems in terms of slip rates and seismogenic potential. It sustains the highest known deformation rates among continental or continent-ocean transform systems globally, accommodating greater than 50mm/yr dextral offset. The entire approximately 900 km offshore length has ruptured in seven greater than magnitude 7 events during the last century, making the cumulative historical seismic moment release higher than any other modern transform plate boundary system.
The 1949 Queen Charlotte Islands earthquake struck Haida Gwaii and the Pacific Northwest coast at 8:01 p.m. PDT on August 21. The earthquake had a moment magnitude of 8.0 and a surface-wave magnitude of 8.1. The maximum Mercalli Intensity in the event was VIII (Severe).
The 2012 Haida Gwaii earthquake occurred just after 8:04 p.m. PDT on October 27. The shock had a moment magnitude of 7.8 and a maximum Mercalli Intensity of V (Moderate). The earthquake's epicentre was on Moresby Island of the Haida Gwaii archipelago. This was the second largest Canadian earthquake ever recorded by a seismometer, after the 1949 Queen Charlotte Islands earthquake, about 135 kilometres (84 mi) away. One person died due to a car crash related to the tsunami in Oahu, Hawaii.
The 2013 Craig, Alaska earthquake struck on January 5, at 12:58 am (UTC–7) near the city of Craig and Hydaburg, on Prince of Wales Island. The Mw 7.5 earthquake came nearly three months after an Mw 7.8 quake struck Haida Gwaii on October 28, in 2012. The quake prompted a regional tsunami warning to British Columbia and Alaska, but it was later cancelled. Due to the remote location of the quake, there were no reports of casualties or damage.
The 1979 Saint Elias earthquake affected Alaska at 12:27 AKST on 28 February. The thrust-faulting Mw 7.5 earthquake had an epicenter in the Granite Mountains. Though the maximum recorded Modified Mercalli intensity was VII, damage was minimal and there were no casualties due to the remoteness of the faulting. Damage also extended across the border in parts of Yukon, Canada.