Maapõuamisi
Maapõuamisi are geological events characterized by the sudden release of energy in the Earth's crust, resulting in seismic waves that cause the ground to shake. These phenomena are most commonly caused by the movement of tectonic plates, large slabs of rock that make up the Earth's outer layer. When these plates grind against each other, they can become stuck, building up stress over time. Eventually, this stress is released abruptly, leading to an earthquake.
The location where the earthquake originates is called the hypocenter, and the point directly above it on
Maapõuamisi can occur with varying degrees of severity, from imperceptible tremors to catastrophic events that cause