Where is Sagaing Fault?
Where is Sagaing Fault?
Myanmar
The Sagaing Fault is a major tectonic structure between the Indian Plate and Sunda Plate. The fault measures 1200 km along north–south and cuts through the centre of Myanmar. Many urban areas lie along the fault.
Is Myanmar on a fault line?
Myanmar has five major fault lines, making it one of the more earthquake-prone countries. The Sagaing fault was last active in 2011, and the other four are the Kabaw fault in the West, the Kyaukkyan fault in northern Shan State, the Thanlwin fault under the Thanlwin River and the Rakhine fault in Rakhine State.
What major event happened at Sagaing Fault?
Looking back at the historical records of earthquakes, the years 1906 and 1908 saw two major events in the northernmost end of the Sagaing Fault. The 1906 Putao earthquake on August 31 had an estimated moment magnitude of 7.0, and the 1908 earthquake measured Mw 7.5.
Where is the Anatolian fault?
Turkey
Part of Hall of Planet Earth. The Anatolian transform fault system is probably the most active in the world. It separates the Eurasian plate from the Anatolian plate in northern Turkey.
What makes the Queen Charlotte fault a transform fault?
The Queen Charlotte Fault (QCF) forms a transpressional plate boundary, and is as active as other major transform fault systems (i.e. San Andreas, Alpine) in terms of slip rates and seismogenic potential. The fault is named for the Queen Charlotte Islands (now Haida Gwaii) which lie just north of the triple junction.
Is the Anatolian Plate Continental?
The Anatolian Plate or the Turkish Plate is a continental tectonic plate comprising most of the Anatolia (Asia Minor) peninsula (and the country of Turkey). To the east, the East Anatolian Fault, a left lateral transform fault, forms a boundary with the Arabian Plate.
What type of fault is the Anatolian fault?
The North Anatolian Fault is a large transform fault in which two tectonic plates are sliding past each other. It is smilar is size to the San Andreas Fault.
How has the Queen Charlotte Fault changed over time?
Through geologic time, a change in pacific plate motion beginning as recently as approximately 6 Ma or as early as approximately 12 Ma caused an increase in convergence along the entire length of the fault and initiated underthrusting along the southern segment where convergence is highest, a process that ultimately …
What two plates made the Queen Charlotte Fault?
An important tectonic boundary, the Fairweather-Queen Charlotte fault system, runs along the western coast of the park. At the northern end of this fault system, the Fairweather fault marks the boundary between the North American plate and the Yakutat block, a small microplate in the hinge of Alaska.
How did the Anatolian fault form?
Abstract The North Anatolian Fault (NAF) is a 1200-km-long dextral strike-slip fault zone that formed by progressive strain localization in a generally westerly widening right-lateral keirogen in northern Turkey mostly along an interface juxtaposing subduction-accretion material to its south and older and stiffer …
What caused the North Anatolian fault?
What makes the Queen Charlotte Fault a transform fault?
