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Earthquakes are sudden movements of the Earth's crust that occur when stress builds up along fault lines and is suddenly released. They are one of the most powerful and destructive natural phenomena on our planet.
The primary cause of earthquakes is the movement of tectonic plates. The Earth's outer shell consists of several large plates that constantly move, albeit very slowly. When these plates collide, separate, or slide past each other, enormous stress builds up along the boundaries. When this stress exceeds the strength of the rocks, they break suddenly, releasing energy in the form of seismic waves.
There are three main types of plate boundaries where earthquakes commonly occur:
The most destructive earthquakes typically occur at convergent and transform boundaries.
Earthquakes are measured using two main scales:
The Richter Scale measures the magnitude of an earthquake, which represents the amount of energy released. It's a logarithmic scale ranging from 1 to 10, where each whole number represents a tenfold increase in amplitude.
The Mercalli Scale measures the intensity of an earthquake based on observed effects and damage. It ranges from I (not felt) to XII (total destruction).
Earthquakes can have both primary and secondary effects:
Understanding earthquakes is crucial for:
::: summary Key Points to Remember:
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