Sagaing Fault
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Sagaing Fault
The Sagaing Fault is a major fault in Myanmar, a mainly continental right-lateral transform fault between the Indian plate and Sunda plate. It links the divergent boundary in the Andaman Sea with the zone of active continental collision along the Himalayan front. It passes through the populated cities of Mandalay, Yamethin, Pyinmana, the capital Naypyidaw, Toungoo and Pegu before dropping off into the Gulf of Martaban, running for a total length of over . Discovery and early studies A partial visualization of an active fault trace that aligns with the present-day Sagaing Fault trace was recorded by Fritz Noetling, a geologist, in the book ''The Miocene of Burma'' published in 1900. In 1913, Thomas Henry Digges La Touche of the Geological Survey of India acknowledged the existence of a plate boundary feature along the Shan Plateau's western margin in Mandalay, including the one dividing metamorphic stratas of the Sagaing Hills from the Central Tertiary Basin. While analysing ...
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Yangon
Yangon, formerly romanized as Rangoon, is the capital of the Yangon Region and the largest city of Myanmar. Yangon was the List of capitals of Myanmar, capital of Myanmar until 2005 and served as such until 2006, when the State Peace and Development Council, military government relocated the administrative functions to the purpose-built capital city of Naypyidaw in north central Myanmar. With over five million people, Yangon is Myanmar's most populous city and its most important commercial centre. Yangon boasts the largest number of colonial-era buildings in Southeast Asia, and has a unique Downtown Yangon, colonial-era urban core that is remarkably intact. The colonial-era commercial core is centered around the Sule Pagoda, which is reputed to be over 2,000 years old. The city is also home to the gilded Shwedagon Pagoda – Myanmar's most sacred and famous Buddhist pagoda. Yangon suffers from deeply inadequate infrastructure, especially compared to other major cities in Sou ...
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