1901 Black Sea earthquake
|Date||March 31, 1901|
|Depth||15 km (9 mi)|
|Tsunami||Up to 4 m|
The 1901 Black Sea earthquake was a 7.2 magnitude earthquake, the most powerful earthquake ever recorded in the Black Sea. The earthquake epicenter was located in the east of Cape Shabla-Kaliakra, 10 km off northwest coast of Bulgaria. In Romania, the earthquake was felt not only throughout Dobrogea, but also in Oltenia and Muntenia, and even in southern Moldova.
The earthquake was followed by a large number of local replicas and secondary earthquakes, that have occurred over many years, until 1905; the strongest aftershocks reached magnitudes of 5.5-6.0 on the Richter scale and were also felt in southern Romania, including Bucharest. After 1905, Pontic seismic activity began to subtract, although weak and moderate earthquakes were also reported in subsequent years.
Such events are rare in the Black Sea. In the last 200 years, in the Black Sea region occurred 24 tsunamis of which two were in the territory of Dobrogea. The earliest recorded tsunami in Romania dates from 104, when the city of Callatis, current Mangalia, was badly affected.
The off-shore region of Southern Dobruja, especially the epicentral area located in the south of Mangalia, including the Bulgarian off-shore of the Black Sea, has been emphasized, along the years, by earthquakes which in certain cases have been violent, reaching magnitudes of 7-7.5 on Richter scale. These are also crustal earthquakes, of low depth (5–30 km), with severe effects on the epicentral area. Sometimes, in case of earthquakes with underwater focus (as those located in the east of Shabla Cape), tsunami waves were generated, like in 1901.
Research studies carried out by experts have shown that Pontic earthquakes with destructive behaviour, comparable to that in 1901, repeat at mean periods of 300–500 years. Besides the earthquake in 1901, there are also known very strong Ponticearthquakes in 1444 (likely, with its epicentre in Varna), around year 800, in 543, etc.
The earthquake had devastating consequences in the coastal area of southern Mangalia, many villages being ruined (maximum intensity of IX-X on Mercalli scale); likewise, the earthquake generated a 4 meter-height tsunami wave and there occurred banks dislocations and other local geomorphological phenomena. In Bucharest, the seismic intensity was V-VI degrees on the Mercalli scale, causing panic among the population and light damage to buildings.
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