North Anatolian Fault

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The North Anatolian Fault and slip magnitudes of earthquakes in the 20th century

The North Anatolian Fault (NAF) (Turkish: Kuzey Anadolu Fay Hattı) is an active right-lateral strike-slip fault in northern Anatolia which runs along the transform boundary between the Eurasian Plate and the Anatolian Plate. The fault extends westward from a junction with the East Anatolian Fault at the Karliova Triple Junction in eastern Turkey, across northern Turkey and into the Aegean Sea. It runs about 20 km south of Istanbul. The North Anatolian Fault is similar in many ways to the San Andreas Fault in California. Both are continental transforms with similar lengths and slip rates. The Sea of Marmara near Istanbul is an extensional basin similar to the Salton Trough in California, where a releasing bend in the strike-slip system creates a pull apart basin.

Significant earthquakes[edit]

Since the disastrous 1939 Erzincan earthquake, there have been seven earthquakes measuring over 7.0 in magnitude,[1] each happening at a point progressively further west.[2] Seismologists studying this pattern believe that each earthquake may trigger the next.[3] By analyzing the stresses along the fault caused by each large earthquake, they were able to predict the shock that hit the town of İzmit with devastating effect in August 1999. It is thought that the chain is not complete, and that an earthquake will soon strike further west along the fault – perhaps near the heavily populated city of Istanbul.

The North Anatolian and neighbouring faults covering most of Turkey
Event Moment magnitude Casualties
1939 Erzincan 7.9 32,962 dead
1942 Niksar-Erbaa 6.9
1943 Tosya-Ladik 7.7
1944 Bolu-Gerede 7.5
1949 Karlıova 7.1
1951 Kurşunlu 6.9 50 dead, 3,354 injured
1957 Abant 6.8
1966 Varto 6.9 2,394 dead, 1,489 injured
1967 Mudurnu Valley 7.1 86 dead, 332 injured
1992 Erzincan 6.5
1999 İzmit 7.4 17,480 dead and 43,959 injured
1999 Düzce 7.2 894 dead

Notes[edit]

External links[edit]