Search results
Results from the WOW.Com Content Network
The earthquake of c. 227 BC is associated with an uplift of more than three metres and movement on this reverse fault is considered to be the likely causative mechanism for the event. [4] The epicentral location of this event is uncertain, with modern catalogues giving locations either near Rhodes city , [ 1 ] or just south of the island of Symi .
The earthquake was particularly felt in Thesprotia and Preveza where people took to the streets, It was also felt in Ioannina, Arta, Corfu and in general in the wider area, the earthquake caused serious damage in Kanalaki. [15] (2 injures) USGS [16] 2019-11-27 Aegean Sea, offshore Antikythera: 35.63 23.21 6.1 M w: VI
The 1856 Heraklion earthquake, also known as the Crete earthquake or Rhodes earthquake, occurred on the morning of October 12 at 02:45 am local time. [1] This extremely catastrophic earthquake had an estimated magnitude of 7.7 to 8.3 at a depth of approximately 61 to 100 km. [2] The earthquake was felt over a very wide area extending from Sicily, Italy to the Levant and North Africa. [3]
Historical earthquakes is a list of significant earthquakes known to have occurred prior to the early 20th century. As the events listed here occurred before routine instrumental recordings — later followed by seismotomography imaging technique, [1] observations using space satellites from outer space, [2] artificial intelligence (AI)-based earthquake warning systems [3] — they rely mainly ...
Herodotus attributes the cause of the sudden flood to the wrath of Poseidon. [4] The large tsunami was observed in the Toronean Gulf which devastated Potidaea. [5] The tsunami sank multiple Persian ships attempting to invade the colony, drowning several hundred soldiers.
The 464 BC Spartan earthquake occurred along the Sparta fault in the year 464 BC destroying much of what was Sparta and many other city-states in ancient Greece. Historical sources suggest that the death toll may have been as high as 20,000, although modern scholars suggest that this figure is likely an exaggeration.
An earthquake is what happens when the seismic energy from plates slipping past each other rattles the planet's surface. Those seismic waves are like ripples on a pond, the USGS said.
The epicentre of the earthquake lies within a zone of active extensional faulting, but close to the southern flank of Vesuvius. Analysis of focal mechanisms from the area around Vesuvius indicates that active faulting in the area involves NW–SE and NE–SW trending oblique-slip normal faults and E–W trending normal faults, part of the zone of active extension that extends the full length ...