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・ 1981 PBA Reinforced Filipino Conference Finals
・ 1981 PBA season
・ 1981 Peach Bowl
・ 1981 Peach Bowl (December)
・ 1981 Peach Bowl (January)
・ 1981 Penn State Nittany Lions football team
・ 1981 Pepsi Grand Slam
・ 1981 Peter Jackson Classic
・ 1981 PGA Championship
・ 1981 PGA Tour
・ 1981 Philadelphia Eagles season
・ 1981 Philadelphia Phillies season
・ 1981 Pittsburgh Panthers football team
・ 1981 Pittsburgh Pirates season
・ 1981 Pittsburgh Steelers season
1981 Playa Azul earthquake
・ 1981 Player's Canadian Open
・ 1981 Player's Canadian Open – Men's Singles
・ 1981 Portland Timbers season
・ 1981 Preakness Stakes
・ 1981 President's Cup
・ 1981 President's Cup Football Tournament
・ 1981 Presto Fun Drinks season
・ 1981 Prix de l'Arc de Triomphe
・ 1981 Pro Bowl
・ 1981 protests in Kosovo
・ 1981 Pulitzer Prize
・ 1981 Purdue Boilermakers football team
・ 1981 riots
・ 1981 Romania rugby union tour of Scotland


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1981 Playa Azul earthquake : ウィキペディア英語版
1981 Playa Azul earthquake

The 1981 Playa Azul earthquake occurred on October 25, 1981 at 03:22 UTC (on October 24, 1981 at 21:22 local time). It was located near Playa Azul, Michoacán, Mexico. The magnitude of the earthquake was Mw 7.2, or Ms 7.3. Three deaths were reported, two from Michoacán and one from Mexico City. Some buildings were damaged in both Michoacán and Mexico City. A small tsunami was registered in Acapulco with a maximum height of 9 cm.
==Tectonic setting==
The southwestern coast of Mexico lies above the convergent boundary where the Rivera Plate and Cocos Plate are being subducted beneath the North American Plate along the Middle America Trench. The area is seismically very active with large thrust type earthquakes occurring along the plate interface and normal fault type earthquakes occurring at a somewhat deeper level within the descending slab. The plate interface seismicity in this area is strongly segmented, with separate Jalisco, Michoacán, Guerrero and Colima segments being recognised. The southeastern end of the Michoacan segment coincides with the broad Orozco fracture zone within the Cocos Plate. During the 1970s, with no major earthquakes recorded since at least 1911, the segment was recognised as a major seismic gap.〔

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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