499 Nicopolis earthquake

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The 499 Nicopolis earthquake took place in September 499. It affected the cities of Nicopolis, Neocaesarea (modern Niksar), Arsamosata, and Abarne.[1]

Northern Turkey lies across the mainly transform fault boundary between the Anatolian Plate and the Eurasian Plate. The Anatolian Plate is being pushed westwards by the northward moving Arabian Plate. This motion is accommodated by a major dextral (right lateral) strike-slip fault system, the North Anatolian Fault (NAF). In detail the fault is formed of many separate segments. Movement on parts of this fault zone have been responsible for many large and damaging earthquakes. They tend to form overall westward propagating sequences that can last for many decades. The most recent sequence began with the 1939 Erzincan earthquake, continuing with major earthquakes in 1942, 1943, 1944, 1949, 1951, 1957, 1966, 1967, 1992 and two in 1999.[2]

Earthquake

The 499 earthquake is thought to have involved the rupture of the whole of the fault segment that caused the 1939 Erzincan event, 360 km in total. This interpretation is based on the result of paleoseismological investigations across the NAF using trenches to view the displacement of soil horizons that were dated using radiocarbon. Based on the interpreted rupture length, the 499 earthquake is estimated to have had a magnitude in the range Mw 7.7–8.4.[3]

Impact

Sources

References

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