East Anatolian Fault
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The East Anatolian Fault 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
Lake Hazar represents a sag pond on the East Anatolian Fault
Dead Sea Transform
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The Dead Sea Transform fault system, also sometimes referred to as the Dead Sea Rift, is a series of faults that run for about 1,000 km from the Marash triple junction to the northern end of the Red S
East Anatolian Fault
…and the Eurasian plate. The East Anatolian Fault runs in a northeasterly direction, starting from the Maraş triple junction at the northern end of the Dead Sea Transform, and ending at the Karlıova triple junction where it meets the North Anatolian Fault. Another 350 km (220 mi) strand of the fault exists north of the…
Panorama of Jordan Valley