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 | 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:
Haida are an Indigenous group who have traditionally occupied Haida Gwaii, an archipelago just off the coast of British Columbia, Canada, for at least 12,500 years.
Earthquakes are caused by movements within the Earth's crust and uppermost mantle. They range from events too weak to be detectable except by sensitive instrumentation, 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.
Haida Gwaii, formerly known as the Queen Charlotte Islands, is an archipelago located between 55–125 km (34–78 mi) off the northern Pacific coast of Canada. The islands are separated from the mainland to the east by the shallow Hecate Strait. Queen Charlotte Sound lies to the south, with Vancouver Island beyond. To the north, the disputed Dixon Entrance separates Haida Gwaii from the Alexander Archipelago in the U.S. state of Alaska.
The 1929 Grand Banks earthquake occurred on November 18, 1929. The shock had a moment magnitude of 7.2 and a maximum Rossi–Forel intensity of VI and was centered in the Atlantic Ocean off the south coast of Newfoundland in the Laurentian Slope Seismic Zone.
The 1946 Aleutian Islands earthquake occurred near the Aleutian Islands, Alaska on April 1, 1946. The shock measured 8.6, Mt 9.3 or 7.4. It had a maximum Mercalli intensity of VI (Strong). It resulted in 165–173 casualties and over US $26 million in damage. The seafloor along the fault was elevated, triggering a Pacific-wide tsunami with multiple destructive waves at heights ranging from 45–138 ft (14–42 m). The tsunami obliterated the Scotch Cap Lighthouse on Unimak Island, Alaska among others, and killed all five lighthouse keepers. Despite the destruction to the Aleutian Island Unimak, the tsunami had almost an imperceptible effect on the Alaskan mainland.
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 1985 Nahanni earthquakes is the name for a continuous sequence of earthquakes that began in 1985 in the Nahanni region of the Northwest Territories, Canada. The largest of these earthquakes occurred on December 23, reaching 6.9 on the moment magnitude scale. This is one of the most significant earthquakes in Canada during the 20th century. The earthquakes had a long succession of aftershocks and jolts. The earthquakes amazed both the general public and the earth science community and have been felt in the Yukon, Alberta, Saskatchewan, British Columbia, and southeastern Alaska.
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 occurred near noon local time on 28 February. It measured Mw 7.4–7.6. Though the maximum recorded Modified Mercalli intensity was VII, damage was minimal and there were no casualties due to the remoteness of the faulting. The epicenter lies near the Alaskan border between the United States and Canada.
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