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・ 1989 U.S. Women's Hard Court Championships
・ 1989 U.S. Women's Hard Court Championships – Doubles
・ 1989 U.S. Women's Hard Court Championships – Singles
・ 1989 U.S. Women's Open Golf Championship
・ 1989 UCF Knights football team
・ 1989 UCI Road World Championships
・ 1989 UCI Road World Championships – Women's team time trial
・ 1989 UCI Road World Cup
・ 1989 UCI Track Cycling World Championships
・ 1989 UEFA Cup Final
・ 1989 UEFA European Under-16 Championship
・ 1989 Uganda Cup
・ 1989 Uganda Super League
・ 1989 UK Championship (snooker)
・ 1989 UMass Minutemen football team
1989 Ungava earthquake
・ 1989 United Jersey Bank Classic
・ 1989 United Jersey Bank Classic – Doubles
・ 1989 United Jersey Bank Classic – Singles
・ 1989 United States Grand Prix
・ 1989 United States motorcycle Grand Prix
・ 1989 Uruguayan Primera División
・ 1989 US Open (tennis)
・ 1989 US Open – Men's Doubles
・ 1989 US Open – Men's Singles
・ 1989 US Open – Mixed Doubles
・ 1989 US Open – Women's Doubles
・ 1989 US Open – Women's Singles
・ 1989 USC Trojans football team
・ 1989 V-League


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1989 Ungava earthquake : ウィキペディア英語版
1989 Ungava earthquake

The 1989 Ungava earthquake occurred at 09:24 local time (14:24 UTC) on December 25 to the north of Lac Bécard in a remote part of the Ungava Peninsula in northern Quebec.〔 It had a magnitude of 6.3 on the surface wave magnitude scale and 6.2–6.5 on the moment magnitude scale and a maximum felt intensity of only IV (''Light'') on the Mercalli intensity scale, due to its remoteness from any inhabited areas. The mainshock was preceded by a magnitude 5.1 foreshock ten hours earlier. It was the first earthquake in eastern North America known to be associated with ground rupture.〔
==Tectonic setting==
The northern part of Quebec lies mainly on the Minto block of the Superior craton. The earthquake occurred within the Utsalik domain, which consists mainly of Archean granitic and granodioritic rocks. A number of northerly trending brittle faults zones have been recognized in the domain. The area has been tectonically quiescent since the Archean. However, like most of the Canadian shield, it is currently experiencing post-glacial rebound.〔

抄文引用元・出典: フリー百科事典『 ウィキペディア(Wikipedia)
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