NORTH ANATOLIAN FAULT Meaning and
Definition
-
The North Anatolian Fault (NAF) is a major fault line in Turkey that extends across the northern part of the country. It is a right-lateral strike-slip fault, meaning that the movement along the fault is predominantly horizontal, with one side sliding past the other in a mainly lateral manner. The fault zone spans approximately 1,500 kilometers from the Aegean Sea in the west to the eastern part of the country, crossing numerous major cities including Istanbul.
The North Anatolian Fault is a result of the complex tectonic activity occurring in the region, where the Eurasian Plate and the Anatolian Plate interact. These two plates are constantly colliding, causing the accumulation of strain along the fault line until it eventually ruptures, releasing substantial amounts of energy in the form of earthquakes. Due to its length and high-seismicity, the NAF is considered one of the most active and hazardous fault zones in Turkey.
Historically, the North Anatolian Fault has been associated with several significant earthquakes that have resulted in widespread damage and loss of life. These include the devastating earthquakes in Erzincan in 1939, in Bolu-Düzce in 1999, and in eastern Turkey in 2011. The fault continues to pose a significant seismic risk, and ongoing monitoring and research efforts are essential for better understanding and managing the potential hazards associated with it.
Common Misspellings for NORTH ANATOLIAN FAULT
- borth anatolian fault
- morth anatolian fault
- jorth anatolian fault
- horth anatolian fault
- nirth anatolian fault
- nkrth anatolian fault
- nlrth anatolian fault
- nprth anatolian fault
- n0rth anatolian fault
- n9rth anatolian fault
- noeth anatolian fault
- nodth anatolian fault
- nofth anatolian fault
- notth anatolian fault
- no5th anatolian fault
- no4th anatolian fault
- norrh anatolian fault
- norfh anatolian fault
- norgh anatolian fault
- noryh anatolian fault
Infographic
Add the infographic to your website:
