THIS IS THE REASON WHY MEGATHRUST DEMOLITION IS SCARY

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Megathrust is a type of earthquake that occurs in a subduction zone, where two tectonic plates meet and one plate dives under the other. Subduction zones are prime locations for large, powerful earthquakes because the friction between these two plates generates enormous energy.
Mechanism of Megathrust Occurrence:
1. Subduction Zone:
Subduction zones occur when a denser oceanic tectonic plate dives under a lighter continental tectonic plate. Well-known examples of subduction zones include along the Pacific Ring of Fire.
2. Accumulation of Stress:
Over time, the diving plate (called the subducting plate) presses down on the overlying plate. This stress accumulation occurs due to friction between the two slow-moving, but not smooth, plates. This stress can build up over hundreds to thousands of years.
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