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2008 Peloponnese earthquake : ウィキペディア英語版
2008 Peloponnese earthquake

| date =
| time = 12:25:29 UTC 〔
| duration =
| magnitude = 6.4 Mw
| depth = 〔
| location = 〔
| type = Strike-slip
| affected = Greece
| damages =
| intensity = VIII - ''Severe''
| pga =
| tsunami =
| landslide =
| foreshocks =
| aftershocks =
| casualties = 2 dead; 240 injured 〔
}}
The 2008 Peloponnese earthquake killed two people, injured more than 220 and left at least 2,000 people homeless in north western Peloponese, Greece, on June 8. The earthquake hit the area at 1525 EET (1325 UTC), with a moment magnitude of 6.5, according to the Athens Geodynamic Institute. It was strongly felt as far away as in Athens and in parts of southern Italy. The US Geological Survey reported that the quake had a magnitude of 6.4. The epicenter of the tremor was located about 15 miles (32 km) southwest of the Greek port city of Patras, at a depth of 16 km. Interior Minister Prokopis Pavlopoulos dispatched rescue and recovery teams (including members of five government agencies), the Red Cross and units of the army in order to assess the damage and the needs of survivors in the earthquake affected areas.
==Earthquake==

The earthquake of June 8, 2008, was generated by stresses resulting from the motion of the small Aegean Sea plate southwest with respect to the Eurasia plate with a velocity of about 30 mm/y. The boundary between the Aegean plate and the Eurasia plate in central Greece is diffuse. Seismicity is concentrated in east-trending and northeast-trending zones of deformation. The east-trending zones are characterized by predominantly normal faulting. The northeast-trending zones are characterized by predominately strike-slip faulting earthquakes. The focal mechanism of the earthquake of June 8 is consistent with the shock having been caused by strike-slip faulting similar to that occurring within the northeast-trending zones. Since the beginning of the twentieth century, the largest crustal earthquakes of central Greece have had magnitudes of about 7.2.

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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