[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.

[6] On the shores of Massachusetts Bay, the tops of chimneys were broken on houses and pewter (a malleable metal alloy) was jarred from shelves.

A lower magnitude range would be preferred if the soil in the area was soft and loosely compacted and a range based on firm ground or bedrock would be proportionately higher. 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. The landslide explanation is accepted as final in this report because the great release of seismic energy necessary to explain the effects along river banks is incompatible with the minor damage sustained by buildings in the area. Le tremblement de terre de 1663 dans la Nouvelle France: Roy. B4 BRIGHAM, W. T., 1871. 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. 1, 27-35. Murray Bay is the name of a landing a few miles from La Malbaie. Mém. Contributions to the History of East Haddam-Moodus noises: Connecticut Valley Advertiser, Moodus, Conn. S4 SULTE,, B., 1911. 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. H1 HECK, N. H., and EPPLEY, R. A., 1958.

Other damage was confined to cracked chimneys and the like. 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. Géophys. 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. These effects were short-lived and Lalemant and other missionaries were soon left wishing for another great earthquake to help them in their cause. No loss of life was reported. H10 HODGSON, E. A.,, 1945. Qué. Mem., v. 2. J., v. 22, 325-334. T1.4 THWAITES, R. G. The Jesuit Relations and allied documents- travels and explorations of the Jesuit missionaries in New France 1610-1791: v. 12-71.
Only 750 sets were printed.v. The main structures of the area are faults of the Saint Lawrence rift system that run parallel to the river, formed during the break-up of the supercontinent Rodinia in the late Neoproterozoic and early Paleozoic. Historical notes on the earthquakes of New England 1638-1869: Reprinted from Boston Soc. [1] These things together suggest that the Charlevoix earthquake was similar in size to the largest of the New Madrid earthquakes and was at least a magnitude 6.8 event. Felt over the entire eastern part of North America - 750,000 square miles. (1956) ed. 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. Soc. [2] Landslides and underwater sediment slumps were a primary characteristic of the event with much of the destruction occurring near the epicentral region of the St. Lawrence estuary and also in the area of the Saguenay Graben. [8], Great landslides along the Saint Lawrence, Saint-Maurice, and Batiscan Rivers made these rivers muddy after the shock, with the waters of the St. Lawrence being affected for up to one month. M7 MILNE, J., 1913. The description that follows is taken verbatim from: Smith, W E T, 1962.

List of recorded earthquakes in New Brunswick: Natural Hist. L1 LAFLAMME, Msgr. [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. Focal mechanisms for earthquakes in this zone are consistent with rupture on both reverse faults and strike-slip faults of varied orientation. Fear came to all, penalty to none.

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. The probable epicentre of the St. Lawrence earthquake of February 5, 1663: Roy. The terms "Murray Bay" and "Murray River" appear on many maps instead of "La Malbaie" and "Rivière La Malbaie" respectively. Am. A large portion of eastern North America felt the effects. A large portion of eastern North America felt the effects. Bull., No. 3, 205-211. Twelfth annual report of the Meteorological Observatory at St. Ignatius College, Cleveland,7-15. Can. Roy. TONDORF, F A., S. J., 1914. 47, 255, 297-299, 319; v. 48, 27, 37-65, 71-73, 157-161,183, 187-223; v. 49, 53, 89; v. 52, 223; v. 59, 29; v. 71, 304.

This paper contains a brief account of a number of the larger shocks in eastern Canada. Accompanied by vast landslides along the St. Maurice, Batiscan and St. Lawrence Rivers. B5 BROOKS, J. E., S.J., 1960. O1 ODENBACH, F. L., S. J., 1906-1907.

An appendix discusses the previous seismic record of the St.Lawrence Valley. They described it as "miraculous" rather than a disaster,[15] regarding the date of the earthquake as particularly important, coming on the last day of the carnival, just before Mardi Gras. Soc. A8 ANONYMOUS, 1925. Natural Hist. 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. Part II-Earthquakes of northeastern United States and eastern Canada: Obs. [9] Near Trois-Rivières several waterfalls were transformed by these landslides,[9] and one waterfall on the St. Maurice River near Les Grès was said to have been nearly leveled. 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. Géog. 4, 157-183.

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. G1 GAGNON, A., 1891.

In 1996 it was the site of the largest flood in 20th-century Canadian history, which led to the investigation of the fjord bottom using bathymetric data to determine slope stability. Lua error in Module:Coordinates at line 668: callParserFunction: function "#coordinates" was not found.

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