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Geometry of the plate boundary in California has changed dramatically as two triple junctions migrated along the coast; the main transform fault has progressively moved inland over the years. [3] In the port city of Prince Rupert, windows were destroyed and buildings swung. Funding for USA.gov and content contributors is made possible from the U.S. Congress, E-Government Act of 2002. The geometry of the Queen Charlotte Fault seems to have been fairly stable over tens of millions of years; triple junction complications have mostly been accommodated in oceanic crust to the south. However, the Queen Charlotte Fault is offshore, whereas the San Andreas bisects major cities. Earthquake. google_ad_client = "pub-2707004110972434"; In Terrace, on the adjacent mainland, cars were bounced around, and standing on the street was described as "like being on the heaving deck of a ship at sea". It occurred on the Queen Charlotte Fault (Canada's equivalent of the San Andreas Fault) - the boundary between the Pacific and North American plates that runs underwater along the west coast of the Haida Gwaii (formerly Queen Charlotte Islands) off the west coast of British Columbia. The offshore region of British Columbia is one of the highly active seismic regions of the world. Required fields are marked *. Welcome! However, the greatest earthquake in Canadian history was the 1700 Cascadia earthquake, a megathrust earthquake that occurred along the Pacific Northwest coast from Northern California to southwestern British Columbia which reached magnitude 9 on the Richter magnitude scale.[4]. The 1949 Queen Charlotte Islands earthquake struck the sparsely populated Queen Charlotte Islands and the Pacific Northwest coast at 8:01 p.m. PDT on August 21. Geological evidence shows that large earthquakes have in fact occurred repeatedly on the west coast in the past. The 1949 Queen Charlotte Islands earthquake struck the sparsely populated Queen Charlotte Islands and the Pacific Northwest coast at 8:01 p.m.wikipedia [3] No deaths were reported in this earthquake. The earthquake ruptured the fault for a distance more than 500 km (311 mi). Fortunately, most of them occurred offshore or in remote regions so there were few deaths and only moderate damage. World Heritage Encyclopedia™ is a registered trademark of the World Public Library Association, a non-profit organization. The 1949 Queen Charlotte Islands earthquake struck the sparsely populated Queen Charlotte Islands and the Pacific Northwest coast at 8:01 p.m. PDT on August 21. In the service community of Terrace, away on the mainland, cars were bounced around, and standing on the street was described as "like being on the heaving deck of a ship at sea". The 1949 Queen Charlotte Islands earthquake was caused by a rupture on the Queen Charlotte Fault, which forms part of the boundary between the Pacific and North American plates. In California the plates are moving at a relative rate of twenty-five miles per million years, mainly related to the San Andreas Fault. Are you certain this article is inappropriate? In the service community of Terrace, away on the mainland, cars were bounced around, and standing on the street was described as "like being on the heaving deck of a ship at sea". This page was last modified on 28 July 2015, at 21:19. The Juan de Fuca Plate is a completely different geological structure that separates the Queen Charlotte Fault from the San Andreas Fault. The shock had a surface wave magnitude of 8.1 and a maximum Mercalli Intensity of VIII. The earthquake ruptured the fault for a distance more than 500 km (311 mi). /* 728x90, created 7/15/08 */ Lua error in Module:Coordinates at line 668: callParserFunction: function "#coordinates" was not found. The Queen Charlotte Fault, off western Canada and southeast Alaska, is a boundary between the Pacific and North American plates. From Infogalactic: the planetary knowledge core. Between 1982 and 1987, a network of twelve short period analogue seismographs was established on the Queen Charlotte Islands and the adjacent mainland; this network continued to operate until early 1996. 1949 Queen Charlotte Islands earthquake: | | 1949 Queen Charlotte Islands earthquake | | | | ... World Heritage Encyclopedia, the aggregation of the largest online encyclopedias available, and the most definitive collection ever assembled. Ask questions, get answers World Heritage Encyclopedia content is assembled from numerous content providers, Open Access Publishing, and in compliance with The Fair Access to Science and Technology Research Act (FASTR), Wikimedia Foundation, Inc., Public Library of Science, The Encyclopedia of Life, Open Book Publishers (OBP), PubMed, U.S. National Library of Medicine, National Center for Biotechnology Information, U.S. National Library of Medicine, National Institutes of Health (NIH), U.S. Department of Health & Human Services, and USA.gov, which sources content from all federal, state, local, tribal, and territorial government publication portals (.gov, .mil, .edu). The 1949 Queen Charlotte Islands earthquake was caused by a rupture on the Queen Charlotte Fault, which forms part of the boundary between the Pacific and North American plates. google_ad_slot = "4852765988"; EnviroZine: Environment Canada's Online Newsmagazine, https://infogalactic.com/w/index.php?title=1949_Queen_Charlotte_Islands_earthquake&oldid=4241746, Creative Commons Attribution-ShareAlike License, About Infogalactic: the planetary knowledge core. Because this quake occurred before the modern surface wave magnitude scale was developed and widely implemented, this earthquake may have only had the same overall intensity as the 2012 Haida Gwaii earthquake. Because this quake occurred before the modern surface wave magnitude scale was developed and widely implemented, this earthquake may have only had the same overall intensity as the 2012 Haida Gwaii earthquake. The 1949 Queen Charlotte Islands earthquake struck the sparsely populated Queen Charlotte Islands and the Pacific Northwest coast at 8:01 p.m.wikipedia. In Prince Rupert, windows were shattered and buildings swayed. In the service community of Terrace, away on the mainland, cars were bounced around, and standing on the street was described as "like being on the heaving deck of a ship at sea". The Queen Charlotte Islands earthquake of 1949 was a magnitude 8.1 interplate earthquake that struck the sparsely populated Queen Charlotte Islands and the Pacific Northwest coast on August 22, 1949.. This is the talk page for discussing improvements to the 1949 Queen Charlotte Islands earthquake article. google_ad_width = 728; However, the greatest earthquake in Canadian history was the 1700 Cascadia earthquake, a megathrust earthquake that occurred along the Pacific Northwest coast from Northern California to southwestern British Columbia which reached magnitude 9 on the Richter magnitude scale.[4]. Excessive Violence The shock had a surface wave magnitude of 8.1 and a maximum Mercalli Intensity of VIII (Severe). The M8.1 Haida Gwaii (formerly Queen Charlotte Islands) Earthquake of August 22, 1949, Local Date and Time: August 21, 1949 at 08:01:12 pm Pacific time. 1949 Natural Disasters: 1949 Queen Charlotte Islands Earthquake, 1949 Tierra del Fuego Earthquake, | Books, LLC, Books, LLC | ISBN: 9781156047491 | Kostenloser Versand für alle Bücher mit Versand und Verkauf duch Amazon. The Juan de Fuca Plate is a large part of the Pacific Ocean seabed which is slowly moving, driven by tectonic forces deep within the earth, and pushing under the coast of Oregon, Washington, and British Columbia. The shaking was so severe on the Haida Gwaii that cows were knocked off their feet, and a geologist with the Geological Survey of Canada working on the north end of Graham Island could not stand up. There were no deaths from this earthquake but there were landslides and other damage. No deaths were reported in this earthquake. The 1949 Queen Charlotte Islands earthquake struck the sparsely populated Queen Charlotte Islands and the Pacific Northwest coast at 8:01 p.m. PDT on August 21. Prior to the mid-1980s, very little was known about the detailed distribution of earthquakes in this area as there was no local seismograph network to detect and locate small earthquakes. Shaking was felt throughout British Columbia, parts of Washington, Oregon, Alberta, the Yukon, and Alaska. A geologist working on the north end of Graham Island, the biggest island of the Queen Charlottes, could not stand up. Charlotte Observer (October 6, 1989), “The problem of the twentieth century is the problem of the color-line—the relation of the darker to the lighter races of men in Asia and Africa, in America and the islands of the sea. Ontario, Quebec City, Quebec, Ottawa, Aboriginal peoples in Canada, Idaho, Columbia River, Portland, Oregon, Kansas, Montana, Republican Party (United States), Anchorage, Alaska, Democratic Party (United States), Canada, United States, Canada, Manitoba, New Brunswick, Newfoundland and Labrador, Ontario, Calgary, Edmonton, Canada, Northwest Territories, Montana, Hawaii, Oregon, California, Indonesia, 1949 Queen Charlotte Islands earthquake, Haida Gwaii, Alaska, %s%s, Earthquakes, San Andreas Fault, History of Canada, Ontario, 1873 in Canada, Canada, 1946 in Canada, British Columbia, Canada, Haida Gwaii, Haida language, Pacific Ocean, Canada, New York City, New York, Quebec City, Toronto,

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