Seismic waves are similar to ripples that can flow through the earth's interior as well as its surface.

It's similar to the ripples that occur when a stone is thrown into the water. When an earthquake happens, it sends forth energy waves known as seismic waves.

Body waves refer to the combination of P-waves and S-waves.

P-waves, S-waves, and surface waves are the three primary forms of seismic waves. The findings could provide a glimpse of the Earth's core structure, as well as aid in the location and understanding of fault planes and the pressures and strains that act on them. Seismologists can deduce the sort of material the waves are traveling through based on the differing behavior of waves in different materials. Waves can be refracted and reflected as they travel through varying densities and stiffnesses. Seismographs are used by seismologists to record how long seismic waves take to travel across different layers of the Earth. They shake the Earth and transform soft deposits like clay into jelly for a short time (liquefaction). When an earthquake happens, energy shockwaves known as seismic waves are released from the earthquake's focal point.

Waves complete 7 list