Search results
Results from the WOW.Com Content Network
The East Anatolian Fault (EAF; Turkish: Doğu Anadolu Fay Hattı) is a ~700 km long major strike-slip fault zone running from eastern to south-central Turkey. It forms the transform type tectonic boundary between the Anatolian sub-plate and the northward-moving Arabian plate . [ 1 ]
The Anatolian sub-plate [1] [2] is a continental tectonic plate that is separated from the Eurasian plate and the Arabian plate by the North Anatolian Fault and the East Anatolian Fault respectively. Most of the country of Turkey is located on the Anatolian plate. [3] Most significant earthquakes in the region have historically occurred along ...
The Anatolian sub-plate is currently being squeezed by the collision of the Eurasian plate with the Arabian plate in the East Anatolian Fault Zone. [ 5 ] [ 6 ] The boundary between the North American plate and the Eurasian plate in the area around Japan has been described as "shifty". [ 7 ]
The Karlıova triple junction is found where the east–west trending North Anatolian Fault intersects the East Anatolian Fault coming up from the southwest, and is ~700 km distant from the Maras triple junction. Because each arm of the junction is a transform fault (F), the Karlıova triple junction is an F-F-F type junction. [clarification ...
The epicentre was about 26 km east of the Turkish city of Nurdagi at a depth of about 18 km on the East Anatolian Fault. During the 20th century, the East Anatolian Fault yielded little major ...
Map of earthquakes in Turkey 1900–2023. The geology of Turkey is the product of a wide variety of tectonic processes that have shaped Anatolia over millions of years, a process which continues today as evidenced by frequent earthquakes and occasional volcanic eruptions. Topographic map of Turkey
A combined diagram of the Aegean and Anatolian plates. The southern margin of the Hellenic arc is shown, which is the trend line of the faults separating the arc and the Hellenic Trench. The body of the arc is the chain called the outer Hellenides, which includes west Peloponnesus, Crete, Rhodes, southwestern Turkey, and all the islands between.
South, with the African plate to the west and the Somali plate and the Indo-Australian plate to the east; West, a left lateral fault boundary with the African plate called the Dead Sea Transform (DST), and a divergent boundary with the African plate called the Red Sea Rift which runs the length of the Red Sea;