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Whittier Narrows earthquake : ウィキペディア英語版
1987 Whittier Narrows earthquake

|duration =
|magnitude = 5.9 ML
|intensity = VIII (''Severe'')
|PGA =
|depth = 〔
|location = 〔
|type = Blind thrust
|countries affected = Southern California
United States
|damage = $358 million
|aftershocks =
|casualties = 8 killed 〔
}}
The 1987 Whittier Narrows earthquake occurred in the southern San Gabriel Valley and surrounding communities of southern California at on October 1. The moderate 5.9 magnitude blind thrust earthquake was centered several miles north of Whittier in the town of Rosemead, had a relatively shallow depth, and was felt throughout southern California and southern Nevada. A large number of homes and businesses were impacted, along with roadway disruptions, mainly in Los Angeles and Orange counties. Damage totals amounted to $358 million USD, with many injuries, three directly-related deaths, and five additional fatalities that were associated with the event.
Mercalli Intensity values for the greater Los Angeles area varied with ranges from VI (''Strong'') to VII (''Very Strong''). Only Whittier experienced a level of VIII (''Severe''), the highest experienced during the event, with the historic uptown area suffering the greatest damage. A separate M5.3 strike-slip event occurred three days later and several kilometers to the northwest that also caused damage and one additional death. Because of the earthquake activity in the Los Angeles Metropolitan area, buildings and other public structures had been equipped with accelerometers, and both the mainshock and the primary aftershock provided additional data for seismologists to analyze and compare with other southern California events.
==Tectonic setting==

Beginning with the 1983 Coalinga earthquake, a blind thrust event in the central coast ranges of California, a change in perspective was brought about regarding these types of (concealed) faults. The October 1987 shock occurred on a previously unrecognized blind thrust fault that is now known as the Puente Hills thrust system. The fault was delineated by the mainshock and aftershock focal mechanisms, fault plane reflection studies, and high resolution seismic profiles, which also revealed that the fault runs from downtown Los Angeles to near Puente Hills. The system is considered one of the highest-risk faults in the United States due to its moderate dip and its location under a large metropolitan area.

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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