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Elsinore Fault Zone : ウィキペディア英語版 | Elsinore Fault Zone
The Elsinore Fault Zone is a large right-lateral strike-slip geological fault structure in Southern California. The fault is part of the trilateral split of the San Andreas fault system and is one of the largest, though quietest faults in Southern California.〔(【引用サイトリンク】 THE SAN ANDREAS FAULT SYSTEM )〕〔(【引用サイトリンク】 Elsinore Fault Zone )〕 == Fault characteristics == The Elsinore fault zone, not including Whittier, Chino, and Laguna Salada faults, is long with a slip-rate of 4.0 millimeters/year (0.15 in/yr). It is estimated that this zone is capable of producing a quake of 6.5–7.5 MW. The projected interval between major rupture events is 250 years. The last major rupture event on the main Elsinore fault was in 1910 with a 6 MW earthquake centered just northwest of the city of Lake Elsinore.〔(【引用サイトリンク】Elsinore Earthquake )〕
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