| Local date | May 18 and 19, 363 [1] |
|---|---|
| Epicenter | 32°59′56″N35°21′58″E / 32.999°N 35.366°E [ citation needed ] |
| Areas affected | Syria-Palaestina province of Byzantine Empire |
| Max. intensity | EMS-98 X (Very destructive) [2] |
The Galilee earthquake of 363 was a pair of severe earthquakes that shook the Galilee and nearby regions on May 18 and 19. [3] The maximum perceived intensity for the events was estimated to be X [4] (Very destructive) on the European macroseismic scale. The earthquakes occurred on the portion of the Dead Sea Transform (DST) fault system between the Dead Sea and the Gulf of Aqaba.
Sepphoris, north-northwest of Nazareth, was severely damaged. Nabratein and the Nabratein synagogue (northeast of Safed) were destroyed. [5] The earthquake may have been responsible for the failure of the plan to rebuild the Temple in Jerusalem with the permission of the Emperor Julian. [6]
Year 551 (DLI) was a common year starting on Sunday of the Julian calendar. The denomination 551 for this year has been used since the early medieval period, when the Anno Domini calendar era became the prevalent method in Europe for naming years.
The 1202 Syria earthquake struck at about dawn on 20 May 1202 with an epicenter in southwestern Syria. The earthquake is estimated to have killed around 30,000 people. It was felt over an extensive area, from Sicily to Mesopotamia and Anatolia to upper Egypt, mostly affecting the Ayyubid Sultanate and the Kingdom of Jerusalem. The cities of Tyre, Acre and Nablus were heavily damaged. A magnitude of Ms 7.6 has been estimated with damage up to XI on the Mercalli intensity scale.
The Galilee earthquake of 1837, often called the Safed earthquake, shook the Galilee on January 1 and is one of a number of moderate to large events that have occurred along the Dead Sea Transform fault system that marks the boundary of two tectonic plates; the African plate on the west and the Arabian plate on the east. Intensity assessments for the event were VIII (Damaging) on the Medvedev–Sponheuer–Karnik scale and VIII on the European Macroseismic Scale.
The 1759 Near East earthquakes shook a large portion of the Levant in October and November of that year. This geographical crossroads in the Eastern Mediterranean were at the time under the rule of the Ottoman Empire. The ruins of Baalbek, a settlement in the Beqaa Valley of Lebanon east of the Litani River, were badly damaged. These 1759 events, along with the earlier 1202 Syria earthquake, are likely the strongest historical earthquakes in the region.
The Nabratein synagogue or Navoraya synagogue is a former ancient synagogue and archaeological site, located in a pine forest northeast of Safed, in the Upper Galilee region of the Northern District of Israel.
The 551 Beirut earthquake occurred on 9 July with an estimated magnitude of about 7.5 on the moment magnitude scale and a maximum felt intensity of X (Extreme) on the Mercalli intensity scale. It triggered a devastating tsunami which affected the coastal towns of Byzantine Phoenicia, causing great destruction and sinking many ships. Overall large numbers of people were reported killed, with one estimate of 30,000 by the anonymous pilgrim of Piacenza for Berytus alone.
The 1953 Torud earthquake occurred at the northeastern border of the Great Salt Kavir in Torud, Semnan, Iran on 12 February. The shock had a moment magnitude of 6.6 and had a maximum Mercalli intensity of VIII (Severe). At least 800 people were killed.
The 847 Damascus earthquake occurred in AD 847. Recent scholarship suggests that the earthquake was part of a multiple earthquake stretching from Damascus to the south, to Antioch in the north and to Mosul in the east. There were an estimated 20,000 casualties in Antioch according to the 13th-century historian and writer Al-Dhahabi, and 50,000 in Mosul. It is thought to be one of the most powerful earthquakes along the Dead Sea Transform.
The National Institute of Geophysics and Volcanology is a research institute for geophysics and volcanology in Italy.
Two major earthquakes occurred in the Near East on 18 March and 29 May, AD 1068. The two earthquakes are often amalgamated by contemporary sources. The first earthquake had its epicentre somewhere in the northwestern part of the Arabian Peninsula around Tabuk, while the second was most damaging in the city of Ramla in Palestine, some 500 km to the northwest.
The 1627 Gargano earthquake struck Gargano and part of Tavoliere, southern Italy, at about mid-day on 30 July 1627. A "very large earthquake" caused a major tsunami, the largest seismic event ever recorded in the Gargano region, which "produced severe damage in the whole promontory", killing about 5,000 people. Four aftershocks were documented. The most extensive damage was noted between San Severo and Lesina.
The 1170 Syria earthquake was one of the largest earthquakes to hit Syria. It occurred early in the morning of 29 June 1170. It formed part of a sequence of large earthquakes that propagated southwards along the Dead Sea Transform, starting with the 1138 Aleppo earthquake, continuing with the 1157 Hama, 1170 and 1202 Syria events. The estimated magnitude is 7.7 on the moment magnitude scale, with the maximum intensity of X (Extreme) on the Mercalli intensity scale.
The 1971 Tuscania earthquake occurred on 6 February in Italy. It had an epicenter located halfway between Tuscania and Arlena di Castro, about 20 km west of Viterbo. It had a body wave magnitude of 4.6.
The 1872 Amik (Antakya) earthquake occurred on April 3 with an epicenter within the Amik Valley in the Ottoman Empire. Earthquake had an estimated magnitude of Mw 7.0–7.2 or Ms 7.2 and maximum MSK 64 rating of XI (Catastrophic). Turkey and Syria were devastated by this earthquake, and the region lost at least 1,800 residents.
A destructive earthquake affected present-day northwestern Syria and south-central Turkey in January 1344. Estimates of the seismic magnitude (Mw ) range between 6.8 and 7.6. The MSK 64 intensity was VII–VIII at Manbij; VI–VII at Aleppo and IV at Damascus. Thousands died in Syria and many structures were destroyed.
The 1796 Latakia earthquake struck present-day east coast of Syria on 26 April. The earthquake had an estimated surface-wave magnitude of 6.8 and maximum EMS-92 intensity of VIII–IX. Damage in Latakia was heavy and there was an estimated 1,500 people killed.
The 528 Antioch earthquake was the second major earthquake to affect the city in a span of two years. The shock occurring on 29 November, estimated at Ms 7.1, was viewed by its residents as the end of a series of disasters that had plagued Antioch. It killed at least 4,870 people and razed the remaining buildings that did not collapse in the earthquake of 526, and newly constructed ones.
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