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North Anatolian Fault information


North Anatolian Fault
The North Anatolian Fault and slip magnitudes of earthquakes in the 20th century
The North Anatolian Fault and slip magnitudes of earthquakes in the 20th century
The North Anatolian and neighbouring faults covering most of Turkey
Coordinates41°00′N 35°00′E / 41.000°N 35.000°E / 41.000; 35.000
CountryNorth Anatolian Fault Turkey
RegionMarmara Region, Black Sea Region, Eastern Anatolia Region
CitiesIstanbul, Bursa, Bolu, Tokat, Erzincan, Erzurum
Characteristics
Elevation3,937 metres (12,917 ft)
Top depth1,370 metres (4,495 ft)
RangePontic Mountains, Köroğlu Mountains
Length1,500 kilometres (900 mi)
StrikeE-W
Tectonics
PlateAnatolian Plate, Eurasian Plate
StatusActive
EarthquakesList of earthquakes in Turkey
Typestrike-slip fault

The North Anatolian Fault (NAF) (Turkish: Kuzey Anadolu Fay Hattı) is an active right-lateral strike-slip fault in northern Anatolia, and is 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 for a length of 1200[1]−1500 kilometers.[2] 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.

  1. ^ Şengör, A.M.C.; Tüysüz, O.; İmren, C.; Sakınç, M.; Eyidoğan, H.; Görür, N.; Le Pichon, X.; Rangin, C. (2005). "The North Anatolian Fault: A new look". Annual Review of Earth and Planetary Sciences. 33: 37–112. Bibcode:2005AREPS..33...37S. doi:10.1146/annurev.earth.32.101802.120415.
  2. ^ Caperton Morton, Mary (8 March 2010). "Closing Istanbul's seismic gap". earthmagazine.org. Archived from the original on 2020-08-08. Retrieved 2020-08-08. The North Anatolian Fault is a 1,500-kilometer-long east-west trending fault that runs across most of Turkey.

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North Anatolian Fault

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The North Anatolian Fault (NAF) (Turkish: Kuzey Anadolu Fay Hattı) is an active right-lateral strike-slip fault in northern Anatolia, and is the transform...

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East Anatolian Fault

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The East Anatolian Fault (Turkish: Doğu Anadolu Fay Hattı) is a ~700 km long major strike-slip fault zone running from eastern to south-central Turkey...

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Transform fault

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number of such faults are found on land, although these are generally better-known, such as the San Andreas Fault and North Anatolian Fault. Transform boundaries...

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1939 Erzincan earthquake

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injured. The North Anatolian Fault in Asia Minor is a major transform fault boundary where the Eurasian Plate slides past the smaller Anatolian Microplate...

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1668 North Anatolia earthquake

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accommodated by a major dextral (right lateral) strike-slip fault system, the North Anatolian Fault. This 1,500 km (930 mi) long structure extends from the...

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1766 Istanbul earthquake

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the North Anatolian Fault in the Marmara region. The Sea of Marmara is a pull-apart basin formed at a releasing bend in the North Anatolian Fault ("NAF")...

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1992 Erzincan earthquake

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maximum Mercalli intensity of IX (Violent) and occurred along the North Anatolian Fault. At least 498 people died, roughly 2,000 were injured, and an unknown...

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1509 Constantinople earthquake

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the North Anatolian Fault, a right-lateral strike-slip fault. This local zone of extension occurs where this transform boundary between the Anatolian Plate...

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Geography of Turkey

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5,166 m Very severe earthquakes, especially on the North Anatolian Fault and East Anatolian Fault, occur along an arc extending from the Sea of Marmara...

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Aseismic creep

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Other examples of faults that have experienced aseismic creep include a San Andreas Fault in California and the North Anatolian Fault in Turkey. Creep...

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2019 Istanbul earthquake

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Kırklareli, Kocaeli and Sakarya. North Anatolian Fault system is a strike-slip fault system located in the northern side of Anatolian plate, which lies between...

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Geology of Turkey

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Eurasian Plate and the Anatolian Plate escapes towards the west and southwest along strike-slip faults. These are the North Anatolian Fault Zone, which forms...

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Eurasian Plate

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Eurasian Plate with the Arabian Plate in the East Anatolian Fault Zone. The boundary between the North American Plate and the Eurasian Plate in the area...

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Gulf of Corinth basin

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the westward-moving Anatolian Fault to the north. Major and minor fault planes make up the north and south margins, and its north-south extension is due...

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Turkey

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varying seismic risk levels. Anatolian plate is bordered by North Anatolian Fault zone to the north; East Anatolian Fault zone and Bitlis–Zagros collision...

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Aykut Barka

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to understanding the behaviour of the North Anatolian Fault Zone (NAFZ), one of the most dangerous active faults in the world. Barka was born in Fatih...

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Gulf of Saros

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Aegean Sea, Greece, is in short distance. The North Anatolian Fault Zone, the most prominent active fault in Turkey and the source of numerous large earthquakes...

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1766 Marmara earthquake

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interactions associated with the North Anatolian Fault. The North Anatolian Fault is a predominantly right-lateral strike-slip fault that extends from Karliova...

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Tosya

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of Markos Vafeiadis (1906–1992), a famous Greek politician. The North Anatolian Fault is located in this area. This caused a major earthquake in 1943...

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Coulomb stress transfer

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earthquake prediction occurred along Turkey's North Anatolian fault system. From 1939 to 1999, the Anatolian fault system had witnessed ten earthquakes of M6...

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Earthquake

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ruptures on strike-slip faults, like the San Andreas Fault (1857, 1906), the North Anatolian Fault in Turkey (1939), and the Denali Fault in Alaska (2002),...

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Pontic Mountains

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937 m (12,917 ft). The North Anatolian Fault and the Northeast Anatolian Fault, which are east–west-running strike-slip faults, run along the length of...

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List of fault zones

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This list covers all faults and fault-systems that are either geologically important[clarification needed] or connected to prominent seismic activity.[clarification...

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