Maavärinute

Maavärinute, often referred to as earthquakes, are natural phenomena characterized by the sudden shaking of the Earth's surface. This shaking is typically caused by the release of energy in the Earth's crust, resulting in seismic waves that propagate outwards from the epicenter. The vast majority of earthquakes originate from tectonic plate movements. These plates, which make up the Earth's lithosphere, are in constant, slow motion. When stress builds up along the boundaries between these plates, particularly at fault lines, it can eventually overcome the friction holding them together. This sudden slip or rupture is what generates the seismic energy.

The intensity of a maavärinute is measured using various scales, the most common being the Richter scale and the Moment Magnitude scale. The Richter scale quantifies the amplitude of seismic waves, while the Moment Magnitude scale provides a more accurate measure of the energy released, especially for larger earthquakes. The impact of a maavärinute depends on its magnitude, depth, distance from populated areas, and the local geological conditions. Effects can range from imperceptible tremors to widespread destruction, including collapsed buildings, landslides, and tsunamis if the earthquake occurs offshore. Understanding the causes and effects of maavärinute is crucial for earthquake preparedness and mitigation efforts worldwide.