1956 Amorgos earthquake
UTC time | 1956-07-09 03:11:45 |
---|---|
ISC event | 888445 |
USGS-ANSS | ComCat |
Local date | July 9, 1956 |
Local time | 05:11:45 |
Magnitude | 7.7 Mw |
Depth | 20 km (12 mi) |
Epicenter | 36°39′59″N 25°57′25″E / 36.6664°N 25.957°E |
Areas affected | Greece, Santorini and Amorgos |
Max. intensity | MMI IX (Violent) |
Tsunami | 30 m (98 ft) |
Casualties | 53 |
The 1956 Amorgos earthquake occurred at 03:11
Tectonic setting
The Cyclades island group lies within a zone of extensional tectonics in the Aegean Sea Plate, between the South Aegean Volcanic Arc to the south and the continuation of the North Anatolian Fault to the north. The extension is a result of the bulging out of the Hellenic arc due to flat-slab subduction of the African Plate.[4]
Earthquake
The earthquake's
Tsunami
The tsunami affected a large part of the Aegean Sea. The variable distribution of the observed run-ups, combined with inconsistent timing of the wave arrivals at different locations, suggest that earthquake-triggered underwater landslides were the main cause of the observed tsunami.[3]
Damage
Damage was severe, particularly on Santorini. The earthquake demolished 529 houses and left many others damaged.[2] Fifty-three people were killed as a result of the earthquake, with another three killed by the associated tsunami.[6]
See also
References
- S2CID 140605036.
- ^ a b "Comments for the Significant Earthquake". National Centers for Environmental Information. Retrieved 22 February 2016.
- ^ .
- S2CID 219542417.
- .
- ^ "Comments for the Tsunami Event". National Centers for Environmental Information. Retrieved 22 February 2016.
External links
- The International Seismological Centre has a bibliography and/or authoritative data for this event.