Between 330 – 1923 : about 1,000 earthquakes[1]
30 major during the Byzantine Era, 10 major during the Ottoman Era
Many lasted for months, 40 days in 869, 140 days in 1034, 2 minutes on 11 May, 1766
Followed by fires, or epidemics: 1037 – 1040
Damage to the dome of Saint Sophia : 558, 986 & 1343 - 1346
Conclusions
Earthquakes[1] have been numerous. Most are small ones with strong ones (> 6 on the Richter scale) in between.
The age gap between major earthquakes varies from 73 years to 312 years with an average of 190 years.
Earthquakes in Constantinople between 350 AD and 1999 AD
Quakes :
major, minor
1999 : Izmit area
1988
1963
1957
1952
1923
1894 : 3 after socks from south to north
1855
1841
1837
1802
1790
1766: after socks for 8 months
1754
1752
1719
1712
1690
1659
1648
1556
1509 : “The Lesser Judgement Day “ shocks for 45 days, tsunami or historically Kıyamet-i Sugra ('Little Judgment Day') occurred in the Sea of Marmara on 10 September 1509 at about 10 p.m. The earthquake had an estimated magnitude of 7.2 ± 0.3 on the surface wave magnitude scale with 109 mosques, 1070 state houses, etc destroyed. A tsunami and forty-five days of aftershocks followed the earthquake. The death toll of this earthquake is poorly known, with estimates in the range of 1,000 to 13,000.
Apolytikion of Commemoration of the Earthquake
Plagal of the Fourth Tone
O Thou Who lookest on the earth and makest it tremble, deliver us from the fearful menace of earthquake, O Christ our God, and by the intercessions of the Theotokos, send down upon us Thy mercies in abundance and save us.
1489
1343 - 1346
1305
1296
1086
1064
1037 – 1040 : many
1034
1010
986
869 : for 40 days
740
The 740 Constantinople earthquake took place on 26 October, 740, in the vicinity of Constantinople and the Sea of Marmara. In Constantinople, the earthquake caused the collapse of many public buildings. The Walls of Constantinople were also damaged. The casualties in Constantinople reportedly included over 1,000 people. The earthquake reportedly destroyed a number of towns in Thrace. It also damaged the cities of Nicaea (İznik), Nicomedia (İzmit), and Praenetus. The historians Theophanes the Confessor (8th-9th century) and George Kedrenos (11th century) reported that the earthquake caused the sea to retire away from the coast in many places. The sea soon returned, and flooded many towns. The description given matches that of a seismic sea-wave (tsunami). The date of the earthquake is recorded by (among others) Anastasius Bibliothecarius (9th century), Joannes Zonaras (12th century), Carolus Sigonius (16th century), Caesar Baronius (16th-17th century), and Sethus Calvisius (16th-17th century).
732
611
582
557 - 558
554 - 555
548
542
533
527
483 – 487 : continuous
478
447 [2]
402
398
358
[1] See also: Earthquakes and plague during Byzantine times: can lessons from the past improve epidemic preparedness
Costas Tsiamis , Effie Poulakou-Rebelakou, Spyros Marketos
Abstract | Natural disasters have always been followed by a fear of infectious diseases. This raised historical debate about one of the most feared scenarios: the outbreak of bubonic plague caused by Yersinia pestis. One such event was recorded in the Indian state Maharashtra in 1994 after an earthquake. In multidisciplinary historical approach to the evolution of plague, many experts ignore the possibility of natural foci and their activation. This article presents historical records from the Byzantine Empire about outbreaks of the Plague of Justinian occurring months or even up to a year after high-magnitude earthquakes. Historical records of plague outbreaks can be used to document existence of natural foci all over the world. Knowledge of these historical records and the contemporary examples of plague support the assumption that, in terms of organising humanitarian aid, poor monitoring of natural foci could lead to unpredictable epidemiological consequences after high-magnitude earthquakes.
For the curious:
The Boudjah(Buca) - Smyrna born Alec Issigonis was an engineering genius and even after his death there is a fan base for his cars.
Sir Alexander Arnold Constantine Issigonis CBE FRS RDI (18 November 1906 – 2 October 1988) was a British-Greek automotive designer. He designed the Mini, launched by the British Motor Corporation in 1959, and voted the second most influential car of the 20th century in 1999.
Issigonis was born on 18 November 1906 in the Ottoman port city of Smyrna, the only child of Constantine Issigonis and Hulda Prokopp. His paternal grandfather, Demosthenis, had migrated to Smyrna from the Greek island of Paros in the 1830s and Constantine was a successful and wealthy shipbuilding engineer. His maternal ancestors originated in the Kingdom of Württemberg. It was through his mother's kinships that Issigonis was a first cousin once removed to BMW and Volkswagen director Bernd Pischetsrieder.
As British subjects - his father having naturalised whilst studying engineering in London in 1897 - Issigonis and his parents were evacuated to Malta by the Royal Navy in September 1922 ahead of the Great Fire of Smyrna and the Turkish capture of Smyrna at the end of the Greco-Turkish War. His father died shortly after and Issigonis and his mother moved to the United Kingdom in 1923.
Issigonis studied engineering at Battersea Polytechnic in London. Having failed his mathematics exams three times, subsequently declaring it 'the most uncreative subject you can study', Issigonis decided to enter the University of London External Programme to complete his university education.
Picture of the Issigonis factory from the Indicateur Commercial 1898-1899
(the Greek text reads: “Factories D. Issigonis, Founded in 1854,
The Oldest and the Biggest in Anatolia, Industrial Enterprises”.