H9 HODGSON, E. A., 1937. Obs. Read more about 1663 Charlevoix Earthquake: Tectonic Setting, Effects, Historical Records, Aftermath, See Also, “There was something refreshingly and wildly musical to my ears in the very name of the white mans canoe, reminding me of Charlevoix and Canadian Voyageurs. H1 HECK, N. H., and EPPLEY, R. A., 1958. J., v. 22, 325-334. P1.1 PARKER, F. H., Dec. 17 1915. J.-C. K., 1907. Soc. The 1663 Charlevoix earthquake occurred on February 5, 1663 in the Canadian province of Quebec, and was assessed to have a moment magnitude of between 7.3 and 7.9. Mem., v. 2. 1, 41-52. 3A, v. 2, 30-35. However Hodgson (H8) tentatively concluded that the seismic intensity "was not markedly greater" than that of some five other shocks occurring in the same region in more recent times. These effects were short-lived and Lalemant and other missionaries were soon left wishing for another great earthquake to help them in their cause. Earthquake title = 1663 Charlevoix earthquake caption = date = February 5, 1663 magnitude = 7 Mw depth = location = coord|47.6|N|70.1|W countries affected = Canada, United States tsunami = aftershocks = casualties = The 1663 Charlevoix earthquake "[14], Immediately after the earthquake, the missionaries, once it had become clear that no lives had been lost, regarded the earthquake not only as a timely warning to the population of New France for their sinfulness, but also as a sign of God's protection. The batteau is a sort of mongrel between the canoe and the boat, a fur-traders boat.”—Henry David Thoreau (18171862), “It is crystal clear to me that if Arabs put down a draft resolution blaming Israel for the recent earthquake in Iran it would probably have a majority, the U.S. would veto it and Britain and France would abstain.”—Amos Oz (b. The earthquake in New France, 1663: Georgetown College J., March issue. These records were scrutinized to help determine the scale of damage and estimate the magnitude of the quake in the absence of abundant records from that time period. 41-1, rev. Pub., No. The event occurred during the early European settlement of North America and some of the best recorded first hand accounts were from Catholic missionaries that were working in the area. Burrows Brothers Co. Cleveland, Ohio.This work, in 73 volumes, is a translation from the Latin originals into both English and French. On some maps one English name and one French name are used. [2] At Saint-Jean-Vianney, Quebec, there was a large earthflow landslide in a sensitive clay, interpreted to have been caused by the 1663 earthquake. Accompanied by vast landslides along the St. Maurice, Batiscan and St. Lawrence Rivers. Le dernier tremblement de terre: Soc. A large portion of eastern North America felt the effects. B3 BRIGHAM, W. T., 1870. Earthquake history of the United States. Assoc. [13] Father Charles Simon, on the other hand, was said to have limited training and some written records of his were not received as readily or without hesitation. Soc. 5. The 1663 Charlevoix earthquake occurred on February 5 in New France (now the Canadian province of Quebec), and was assessed to have a moment magnitude of between 7.3 and 7.9. The earthquake occurred at 5:30 p.m. local time and was estimated to have a maximum perceived intensity of X (Extreme) on the Mercalli intensity scale.The main shock epicentre is suggested to have occurred … Proc., v. 9, sect. Bull., v. 19, 110-113. A large portion of eastern North America felt the effects. Larger events lie outside the impact structure and have inferred nodal planes consistent with reactivation of the rift faults. N.B. 4, 151-174. This page was last modified on 9 January 2016, at 04:12. The earthquake occurred at 5:30 p.m. local time and was estimated to have a maximum perceived intensity of X (Extreme) on the Mercalli intensity scale. In a June 2011 report on the earthquake that was published in the Bulletin of the Seismological Society of America, John E. Ebel, a professor and researcher at Boston College, used these known relations that apply to earthquakes in northeastern North America and determined the magnitude to be 7.3 – 7.9. 7, 12-40. K1 KAIN, S. W., 1898. A8 ANONYMOUS, 1925. The main shock epicentre is suggested to have occurred along the Saint Lawrence River, between the mouth of the Malbaie River on the north and the mouth of the Oue… Bull., v. 5, No. 26, no. Earthquakes in eastern Canada and adjacent areas: Roy. Can. The probable epicentre of the St. Lawrence earthquake of February 5, 1663: Roy. It is well established that great quantities of tree-covered earth moved from the shores into the rivers, especially near the suggested epicentre in the St. Lawrence and along the St. Maurice. G1 GAGNON, A., 1891. The main shock epicentre is suggested to have occurred along the Saint Lawrence River,[2] between the mouth of the Malbaie River on the north and the mouth of the Ouelle River on the south. Can. Father Simon seemed to not be of the same mind as the bulk of the devoted, saying "...the Earthquake was rather a Scheme of Divine Mercy than a scourge of Justice,— especially since, in so great a confusion of affairs and perturbations of the elements, no one lost life or fortune. The 1663 Charlevoix earthquake occurred on February 5 in New France (now the Canadian province of Quebec), and was assessed to have a moment magnitude of between 7.3 and 7.9. Surv. [16], From Infogalactic: the planetary knowledge core. [11] The Saguenay region is the site of a geological graben and has been subject to several natural disasters since the turn of the seventeenth century. [12] Some very detailed, though inconsistent, summaries were given by several Jesuits, most notably Jérôme Lalemant who provided relatively reserved written accounts of the strong effects of the earthquake back to his superiors in Europe. The terms "Murray Bay" and "Murray River" appear on many maps instead of "La Malbaie" and "Rivière La Malbaie" respectively. 2, 16-22. A catalogue of destructive earthquakes A.D. 7 to A.D. 1899: Brit. Astron. Contributions to the History of East Haddam-Moodus noises: Connecticut Valley Advertiser, Moodus, Conn. S4 SULTE,, B., 1911. This is the final account of the earthquake of February 28. Sulte (S4), has shown from contemporary accounts that one of these slides practically levelled a very great waterfall at Les Grès on the St. Maurice River. A church record entry made by Reverend S. Danforth from Roxbury, Massachusetts (~ 600 km from the CSZ) indicated the initial shock was felt around 6 pm that evening and several more shocks followed the next morning. M7 MILNE, J., 1913. Part I-Continental United States and Alaska(exclusive of California and Western Nevada): U.S. Coast Geod. H10 HODGSON, E. A.,, 1945. O1 ODENBACH, F. L., S. J., 1906-1907. No loss of life was reported. L1 LAFLAMME, Msgr. [1], The earthquake was felt sharply in New England,[5] though the date recorded for the event was 26 January 1663, as New England was using the Julian calendar at the time. He further suggested that the devastation in the St. Maurice valley "does not, in all probability, indicate a separate focus there, but was due to a landslide of major proportions.". B5 BROOKS, J. E., S.J., 1960. Mém. Fear came to all, penalty to none. [3] Lalemant was said to have been a disciplined priest with diverse experience and following his time in Canada was brought back to France to be posted the provincial superior of the Society of Jesus. The 1663 Charlevoix earthquake occurred on February 5 in New France (now the Canadian province of Quebec), and was assessed to have a moment magnitude of between 7.3 and 7.9. TONDORF, F A., S. J., 1914. Records of the destruction in the St-Maurice Valley have been thought to indicate a much greater intensity for the 1663 shock. They were pleased to see all the colonists attending church regularly in the following days and that even the traffickers in wine and brandy appeared to repent. The inhabitants of the land were the Algonquin and Iroquois people as well as several thousand French settlers. Many of the smaller earthquakes do not appear to be located on the rift faults, but within the volumes of rock between them. Bull., No.
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