Ad
related to: northern anatolian fault map of europe region 3 and 5 philippines
Search results
Results From The WOW.Com Content Network
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 sub-plate. The fault extends westward from a junction with the East Anatolian Fault at the Karliova triple junction in eastern Turkey ...
The devastating 2023 Turkey–Syria earthquakes occurred along the active East Anatolian Fault at a strike-slip fault where the Arabian plate is sliding past the Anatolian plate horizontally. [4] [5] According to the American Museum of Natural History, the Anatolian transform fault system is "probably the most active in the world". [6]
[2] [3] Ridges like the Mid-Atlantic ridge form at a divergent plate boundary. They are located deep underwater and very difficult to study. Scientists know less about ocean ridges than they do the planets of the solar system. [4] There is another triple junction where the Eurasian plate meets the Anatolian sub-plate and the Arabian plate.
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 African plate is subducting under the Aegean plate at a rate of about 40 mm/year, causing shallow earthquakes near the fault and deeper earthquakes near the Greek volcanic arc. [8] Some seismic activity is a result of the extension of the plate, which creates east–west trending faults that can slip and cause earthquakes. [9]
During the 20th century, the East Anatolian Fault yielded little major seismic activity. ... Eleven minutes after the initial quake, the region was hit by a 6.7-magnitude aftershock. A 7.5 ...
[4] [3] It extends from Davao Gulf in the south, bisects the Caraga region at the Agusan River basin, crosses to Leyte and Masbate islands, and traverses Quezon province in eastern Luzon before passing through Nueva Ecija up to the Ilocos region in northwest Luzon. The northern and southern extensions of the PFZ are characterized by branching ...
The North Anatolian Fault (NAF) and East Anatolian Fault (EAF) are currently strike-slipping. Adapted from Armijo, 1999 The Gulf of Corinth basin , or Corinth rift , is an active extensional marine sedimentary basin thought to have started deforming during the late Miocene – Pleistocene epoch.