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・ Sagara Sangamam
・ Sagara Sanosuke
・ Sagara Subdivision
・ Sagara Sōzō
・ Sagara Taketō
・ Sagara Tomoyasu
・ Sagara Yoshiharu
・ Sagara, Karnataka
・ Sagara, Kumamoto
・ Sagara, Shizuoka
・ Sagarakatte
・ Sagami Railway
・ Sagami Railway Izumino Line
・ Sagami Railway Main Line
・ Sagami River
Sagami Trough
・ Sagami Women's University
・ Sagami-ji
・ Sagami-Kaneko Station
・ Sagami-Numata Station
・ Sagami-Ōno Station
・ Sagami-Ōtsuka Station
・ Sagamia geneionema
・ Sagamichthys
・ Sagamihara
・ Sagamihara Asamizo Park Stadium
・ Sagamihara Campus
・ Sagamihara Housing Area
・ Sagamihara Station
・ Sagamiko


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Sagami Trough : ウィキペディア英語版
Sagami Trough

The also Sagami Trench, Sagami Megathrust, or Sagami Subduction Zone is a long trough, which is the surface expression of the convergent plate boundary where the Philippine Sea Plate is being subducted under the Okhotsk Plate. It stretches from the Boso Triple Junction in the east, where it meets the Japan Trench, to Sagami Bay in the west, where it meets the Nankai Trough. It runs north of the Izu Islands chain and the Izu-Bonin-Mariana Arc (IBM).
Megathrust earthquakes associated with the Sagami Trough, known as Kantō earthquakes, are a major threat to Tokyo and the Kantō Region because of the proximity to a population center (with over 36 million living in Tokyo's metro area, with a total of 43 million living in the Kanto Region) and the magnitude the Sagami Trough can create.
==Earthquakes==
(詳細はmegathrust generated the 1703 Genroku earthquake, which was the greatest rupture along the trough in the last thousand years, and the 1855 (Ansei) and 1923 (Great Kanto or Taisho) earthquakes.

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「Sagami Trough」の詳細全文を読む



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