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・ 1918 St. Louis Browns season
・ 1918 St. Louis Cardinals season
・ 1918 Stanley Cup Finals
・ 1918 Stanley Cup playoffs
・ 1918 State of the Union Address
・ 1918 Svenska Mästerskapet Final
・ 1918 Tennessee Volunteers football team
・ 1918 The Citadel Bulldogs football team
・ 1918 Toronto anti-Greek riot
・ 1918 Tulane Olive and Blue football team
・ 1918 Tyler tornado
・ 1918 U.S. National Championships (tennis)
・ 1918 Uruguayan Primera División
・ 1918 USC Trojans football team
・ 1918 Vancouver general strike
1918 Vancouver Island earthquake
・ 1918 Vanderbilt Commodores football team
・ 1918 VFA season
・ 1918 VFL Grand Final
・ 1918 VFL season
・ 1918 VPI Gobblers football team
・ 1918 Washington Senators season
・ 1918 Wisconsin Badgers football team
・ 1918 World Series
・ 1918 Úrvalsdeild
・ 1918–19 (January) Northern Rugby Football Union Wartime Emergency League season
・ 1918–19 Austrian football championship
・ 1918–19 Belfast & District League
・ 1918–19 Blackpool F.C. season
・ 1918–19 Connecticut Aggies men's basketball team


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1918 Vancouver Island earthquake : ウィキペディア英語版
1918 Vancouver Island earthquake

| magnitude = 7.2 Mw
| depth =
| location =
| countries affected = British Columbia
Canada
| tsunami =
| aftershocks =
| intensity = VII (''Very Strong'')
| casualties =
}}
The 1918 Vancouver Island earthquake occurred in British Columbia, Canada at 12:41 a.m. Pacific Standard Time on December 6.〔(【引用サイトリンク】title=The M7 Vancouver Island Earthquake of December 6, 1918 )
The earthquake was most likely of the strike-slip type, and was estimated to have a maximum perceived intensity of VII (''Very Strong'') on the Mercalli intensity scale. The epicenter was located east of the Stewardson inlet on the west coast of Vancouver Island, with damage occurring at the Estevan Point lighthouse on the Hesquiat Peninsula. The event registered 7.2 on the moment magnitude scale and was felt as far as northern Washington state and the interior of British Columbia.
The earthquake took place in the vicinity of the Cascadia subduction zone where the Juan de Fuca Plate and the Explorer Plate are being subducted under the North American Plate at a rate of and less than per year respectively, but the event was a crustal intraplate earthquake and was produced from the complicated interaction between the plates in the area. The source of the earthquake was the Nootka transform fault, which separates the Juan de Fuca and Explorer plates and has been the origin of at least five additional moderate to large events since 1918.
==See also==

*List of earthquakes in 1918
*List of earthquakes in Canada
*1946 Vancouver Island earthquake

抄文引用元・出典: フリー百科事典『 ウィキペディア(Wikipedia)
ウィキペディアで「1918 Vancouver Island earthquake」の詳細全文を読む



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