1956 Amorgos earthquake
 Istanbul
Athens
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| Date | 9 July 1956 |
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| Magnitude | 7.7 Mw |
| Depth | 20 km (12 mi) |
| Epicenter | 36°39′59″N 25°57′25″E / 36.6664°N 25.957°ECoordinates: 36°39′59″N 25°57′25″E / 36.6664°N 25.957°E |
| Areas affected | Greece, Santorini and Amorgos |
| Max. intensity | IX (Violent) |
| Tsunami | 30 m (98 ft) |
| Casualties | 53 |
The 1956 Amorgos earthquake occurred at 03:11 UTC on July 9. It had a magnitude of 7.7 on the moment magnitude scale and a maximum perceived intensity of IX on the Mercalli intensity scale. The epicentre was to the south of the island of Amorgos, the easternmost island of the Cyclades in the Aegean Sea. There was significant damage on Amorgos and the neighbouring island of Santorini. It was the largest earthquake in Greece in the 20th century. It was followed 13 minutes later by a magnitude 7.2 earthquake near Santorini. It triggered a major tsunami with a maximum run-up of 30 m. The combined effects of the earthquake shaking and the tsunami caused the deaths of 53 people with a further 100 injured.
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.
The earthquake's focal mechanism is consistent with normal faulting, trending SW-NE. From the distribution of aftershocks, it is possible to discriminate between the two nodal planes implied by the focal mechanism, indicating that the fault plane dips to the southeast at about 25°. The rupture area is estimated to be about 110 km along strike and 26 km in depth, extending into the upper mantle.
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Wikipedia