Earthquake Natural Disaster Essay

The seismicity or seismic activity of an area refers to the frequency, type and size of earthquakes experienced over a period of time.

So far, there have been sixty-two earthquakes in India.

Strike-slip faults are steep structures where the two sides of the fault slip horizontally past each other.

The sudden release of tension in the tectonic plates sends waves of energy that travel through the Earth. Scientists cannot view a major earthquake beforehand.

An aftershock is in the same region of the main shock but always of a smaller magnitude.

Aftershocks are formed as the crust adjusts to the effects of the main shock.

A foreshock is an earthquake that occurs before a larger earthquake, called the mainshock.

An aftershock is an earthquake that occurs after a previous earthquake, the mainshock.

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