Myanmar is situated between the India and Eurasia tectonic plates, making it particularly prone to earthquakes. The recent 7.7 magnitude quake primarily impacted Mandalay, leading to substantial destruction and over 140 casualties. This region has witnessed several significant tremors throughout history, with a notable 7.3 magnitude quake in 1930 causing at least 550 deaths. Seismologists explain that earthquakes occur due to energy buildup from the movement of tectonic plates, resulting in ground shaking that can lead to further aftershocks and potentially tsunamis.
Myanmar's precarious position between the India and Eurasia tectonic plates makes it highly susceptible to seismic activity, leading to devastating consequences in the region.
The recent magnitude 7.7 earthquake had its epicenter near Mandalay, causing widespread destruction, with reports of over 140 fatalities and extensive damage to infrastructure.
This seismic event adds to Myanmar's history of significant earthquakes, including a deadly 7.3 magnitude quake in 1930 that left at least 550 people dead.
Understanding earthquakes involves recognizing that they result from the movement of tectonic plates on the Earth's surface, which can accumulate energy and cause violent shaking.
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