Magnitude 7.1 - NEAR THE SOUTH COAST OF HONSHU, JAPAN
2009 August 09 10:55:55 UTC
- This event has been reviewed by a seismologist.
|Depth||297 km (184.6 miles) set by location program|
|Region||NEAR THE SOUTH COAST OF HONSHU, JAPAN|
|Distances||170 km (105 miles) S of Hamamatsu, Honshu, Japan|
175 km (110 miles) W of Hachijo-jima, Izu Islands, Japan
205 km (130 miles) SSW of Shizuoka, Honshu, Japan
325 km (200 miles) SSW of TOKYO, Japan
|Location Uncertainty||horizontal +/- 3.2 km (2.0 miles); depth fixed by location program|
|Parameters||NST=345, Nph=345, Dmin=667.6 km, Rmss=0.77 sec, Gp= 14°,|
M-type=teleseismic moment magnitude (Mw), Version=Q
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Felt (V) at Narita; (IV) at Akiruno, Atsugi, Ayase, Chiba, Ebina, Fussa, Hamura, Sagamihara, Tokyo, Yokohama, Yokosuka and Zushi; (III) at Fuchu, Fujisawa, Hachioji, Kawasaki, Musashimurayama, Musashino, Nagoya, Osaka, Tachikawa, Tsukuba, Yamato and Zama; (II) at Misawa, Honshu. Also felt at Aizu-Wakamatsu, Akishima, Amagasaki, Chofu, Fuso, Gotemba, Hayama, Hitachi, Ibaraki, Ichikawa, Ichinoseki, Iida, Inagi, Inzai, Isehara, Isesaki, Kakuda, Kamakura, Kashiwa, Kasukabe, Kawagoe, Kawaguchi, Kiryu, Kobe, Koganei, Kokubunji, Komae, Komoro, Koriyama, Koshigaya, Machida, Maebashi, Matsumoto, Mitaka, Miura, Nakano, Obu, Ohara, Oizumi, Okaya, Ome, Saitama, Sendai, Shizuoka, Takanezawa, Takasaki, Tama, Toda, Tokorozawa, Tono, Uenohara, Urayasu, Utsunomiya, Wakayama, Yamato- Koriyama and Yatomi.
Versión en Español
The magnitude 7.1 earthquake of August 9, 2009, occurred off the south coast of Honshu within the Izu-Bonin subduction system. This system extends 1,200 km from southern Honshu to the Mariana Islands and constitutes part of the boundary between the Pacific plate and the Philippine Sea plate. The Pacific plate moves westwards relative to the Philippine Sea plate with a velocity of about 50 mm/y and subducts beneath it at the Izu-Bonin trench. The earthquake occurred at depth within the westward dipping Pacific plate, well beneath the overriding Philippine Sea plate. Subduction of the Pacific plate along the northern and western margins of the Pacific Ocean generates a large amount of seismicity. Earthquakes typically occur as thrust faulting on interfaces that separate the subducting Pacific plate from the overriding plates, and earthquakes occur within the subducting or overriding plates as the result of stresses associated with intraplate deformation. The August 9, 2009, earthquake was an intraplate event. Its focal depth of 303 km classifies it is a “deep” earthquake, an earthquake with depth greater than or equal to 300 km. Earthquakes have been accurately located to depths of 450 km in the section of the Izu-Bonin subduction system within which the August 9 earthquake occurred. Due to its great depth, the August 9 earthquake did not cause any damage and no damaging tsunami was generated.
- Preliminary Earthquake Report
- U.S. Geological Survey, National Earthquake Information Center:
World Data Center for Seismology, Denver