Earthquake is also known as:

Hint: An earthquake (also recognized as a tremor or tremblor) is the shaking of the Earth's surface, producing a sudden liberation of energy in the Earth's lithosphere that generates seismic waves. Earthquakes can vary in size from those so weak that they cannot be believed to those violent to move objects and people into the air and wreak damage across whole cities. The seismicity of an area is the frequency, sort, and size of earthquakes experienced over some time. The word tremor is also utilized for non-earthquake seismic rumbling.

Complete step-by-step solution:
When an earthquake happens, it delivers energy waves, which are remembered as Seismic waves. It is similar to the ripples produced in water if we throw a rock in it. Seismic waves are like those ripples that can travel through the inside of the earth and the surface.
Body waves are these waves that move through the earth. They begin at the earthquake's epicentre and go through the earth at incredible speeds. Surface waves are these waves that move on the surface of the earth. These waves primarily do the destruction caused by earthquakes.
S waves, also termed shear waves and secondary waves, are the second waves to kick the seismographs. They are transverse waves, which indicates that the motion is normal to the direction of wave propagation. S waves can just move through solids, and scientists have successfully mapped the earth's insides by examining the paths of these waves. P waves or Primary waves are the primary waves to kick the seismographs when an earthquake hits. They are longitudinal waves that indicate that the direction of motion and propagation are identical.
At the Earth's surface, earthquakes exhibit themselves by shaking and displacing or disturbing the ground. When the epicentre of a massive earthquake is discovered offshore, the seabed may be relocated sufficiently to create a tsunami. Tremors can also trigger landslides and, seldom, volcanic activity.
There are three significant types of error, all of which may produce an interplate earthquake: standard, reverse, and strike-slip. Normal and reverse flaws are examples of dip-slip, where the displacement by the fault is in the way of dip and where progress on them includes a vertical component. Typical flaws occur essentially in areas where the crust is being stretched, such as a divergent boundary. Reverse faults happen in areas where the crust is being compressed, such as at a convergent boundary. Strike-slip faults are vertical structures where the two sides of the flaw slip horizontally through each other; transform boundaries are a distinct type of strike-slip fault. Many earthquakes are produced by motion on faults with dip-slip and strike-slip; this is identified as oblique slip.
An earthquake has also been named a quake; tremor is the shaking of the Earth's surface resulting from a sudden liberation of energy in the Earth's lithosphere that produces seismic waves.

Note: In its most common sense, the word earthquake is utilized to explain any seismic event—whether simple or created by humans—that creates seismic waves. Earthquakes are created mainly by the rupture of geological flaws and other issues such as volcanic activity, mine blasts, landslides, and nuclear tests. An earthquake's time of primary rupture is called its hypocenter or focus. The epicenter is the location at ground level right above the hypocenter.