On the morning of the earthquake, Myanmar and parts of Thailand experienced a catastrophic 7.7 magnitude tremor, raising fears of significant loss of life estimated in the tens of thousands. The quake originated near Mandalay, Myanmar's second-largest city, due to the dynamics of the Sagaing Fault, a major tectonic feature known for its violent earthquakes. A second quake hit shortly after, prompting further concerns about aftershocks. Seismologists highlight that Myanmar's highly active seismic landscape makes such events a pressing reality, emphasizing the danger due to the shallow nature of these quakes.
The recent massive earthquake in Myanmar has resulted in devastating losses, with estimates of fatalities ranging from 10,000 to 100,000 due to its magnitude of 7.7.
The powerful tremors originate from the highly active Sagaing Fault, where the Indian and Sunda tectonic plates interact, releasing built-up energy in violent earthquakes.
Following the initial quake, a second significant tremor occurred shortly after, raising concerns about further impending seismic activity and the potential for more damage.
Experts note that Myanmar's location on the Sagaing Fault contributes to its frequent seismic events, with the current quake not being entirely unexpected.
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