Western Quebec Seismic Zone
In this article, we will address the topic of Western Quebec Seismic Zone from different perspectives with the aim of delving into its importance and relevance today. Western Quebec Seismic Zone is a topic that has aroused growing interest in various sectors and a detailed analysis can shed light on its many facets. Throughout the next few lines, we will explore the different aspects of Western Quebec Seismic Zone, presenting different opinions and approaches that will allow the reader to fully understand the complexity and significance of this topic. Through a multidisciplinary approach, we will delve into the consequences and challenges posed by Western Quebec Seismic Zone, thus offering a comprehensive vision that will contribute to the knowledge and understanding of this phenomenon.
The Western Quebec Seismic Zone (French: Zone sismique de l'Ouest du Québec) is a seismically active area in the Ottawa Valley in Eastern Ontario and Western Quebec. The zone stretches from Montreal to Témiscaming and from Cornwall up along the Laurentian Mountains.
Significant earthquakes associated with this seismic zone include the 1732 Montreal earthquake, the 1935 Timiskaming earthquake, the 1944 Cornwall–Massena earthquake, and the 2010 Central Canada earthquake.
Between the years 1980 and 2000 there were 16 earthquakes stronger than a Richter 4.0, with many more of a lesser magnitude. The zone averages about one seismic event every five days.
Seismological monitoring of the zone is performed by the Canadian National Seismograph Network.
Significant earthquakes
1732 Montreal earthquake
Because this is the earliest recorded local earthquake, there is little information about it. It is known that it was a powerful earthquake, leaving much devastation but few deaths. It caused panic and damage to buildings. The aftershocks could be felt for several days after the initial earthquake.
1935 Timiskaming earthquake
At the epicenter of the 1935 Timiskaming earthquake, cracks in gravel and sand could be seen. Almost all chimneys were damaged or destroyed, and some cracks developed in brick walls. The next day, Tee Lake (close to the epicenter) was clouded. It is suspected that sediment which was previously undisturbed was shaken up by the earthquake. This event scored a 7 on the Modified Mercalli Scale.
1944 Cornwall–Massena earthquake
Although it was only measured as 5.8 on the Richter magnitude scale, the Cornwall earthquake did considerable damage and also scored a 7 on the Modified Mercalli Scale. Roughly 2000 chimneys were damaged or destroyed. One school suffered heavy damage with brick falling through the roof of its gym.
2010 Central Canada earthquake
On 23 June 2010 at 1:41:42 EST, a 5.0 magnitude earthquake occurred 32 km north of Buckingham, Quebec at a depth of 18 km. It was felt throughout Western Quebec, Ottawa, and other parts of Ontario, and as far away as Maryland, Michigan, New York, Ohio, Pennsylvania and Vermont in the U.S.
2013 Central Canada earthquakes
On 17 May 2013 at 9:43:23 EST, a 5.2 magnitude earthquake occurred 17 km north of Shawville, Quebec at a depth of 5 km. At 9:53:54 EST, a 4.1 magnitude aftershock occurred 20 km north of Shawville. It was felt throughout Western Quebec, Ottawa, and other parts of Ontario, and as far away as Ohio in the U.S.
See also
References
- ^ "The Western Quebec Seismic Zone". Earthquakes Canada. Natural Resources Canada. Retrieved 1 September 2020.
- ^ "The 16 September, 1732, Montréal earthquake". Earthquakes Canada. Natural Resources Canada. Retrieved 30 April 2020.
- ^ "The 1935 Magnitude 6.1 Timiskaming earthquake". Earthquakes Canada. Natural Resources Canada. Retrieved 30 April 2020.
- ^ "The 1944 Magnitude 5.8 Cornwall-Massena earthquake". Earthquakes Canada. Natural Resources Canada. Retrieved 30 April 2020.
- ^ "Magnitude 5.0 - ONTARIO-QUEBEC BORDER REGION, CANADA". Earthquake Hazards Program. United States Geological Survey. Archived from the original on 13 October 2012. Retrieved 20 May 2012.
- ^ "2013-05-17: M=5.2 - 18 km NE of Shawville, QC - felt". Earthquakes Canada. Natural Resources Canada. Retrieved 17 May 2013.
- ^ "2013-05-17: M=4.1 - 20 km NE of Shawville, QC - aftershock". Earthquakes Canada. Natural Resources Canada. Archived from the original on 23 March 2014. Retrieved 17 May 2013.
Further reading
- Rimando, J. M.; Peace, A. L. (2021). "Reactivation Potential of Intraplate Faults in the Western Quebec Seismic Zone, Eastern Canada". Earth and Space Science. 8 (8). doi:10.1029/2021ea001825. ISSN 2333-5084.
- Rimando, J. M.; Peace, A. L.; Goda, K.; Sirous, N.; Rosset, P.; Chouinard, L. (2023). "Coseismic Coulomb stress changes on intraplate faults in the western Quebec seismic zone following three major earthquakes in the past century". Canadian Journal of Earth Sciences. doi:10.1139/cjes-2023-0025. ISSN 0008-4077.