
How do seismic waves travel through the Earth?
Answer
490.5k+ views
Hint: Seismology is the study of earthquakes and seismic waves that flow thru and across the earth. A seismologist is a scientist who researches earthquakes and seismic waves.
Complete answer:
Earthquakes radiate energy (in what we see as S and P waves) as each body and surface waves. Traveling through the interior of the earth, body waves arrive earlier than the surface waves emitted with the aid of using an earthquake. The body waves are of a better frequency than surface waves. The first sort of body wave is the P wave or primary wave. This may be visible on a seismograph, that is recorded with the aid of using a seismometer. Seismologists.
People who observe earthquakes. use seismographs to report the amount of time it takes seismic waves to journey through exceptional layers of the Earth. As the wave's journey through exceptional densities and stiffness, the waves may be refracted and reflected.
Because of the exceptional behavior of waves in exceptional materials, seismologists can deduce the sort of material the waves are journeying through.
The effects can offer an image of the Earth’s inner shape and assist us to discover and apprehend fault planes and the stresses and lines performing on them.
If there have been no modifications with depth, seismic waves could journey an instant direction to the alternative facet of the Earth. But wave arrivals to remote seismic stations have taught us that there are layers.
Note: Seismic waves journey through the Earth and comply with the equal legal guidelines of refraction and mirrored image as some other waves at interfaces. When they come across barriers among exceptional media, the waves react consistent with Snell’s law, and the perspective of refraction throughout the boundary will rely upon the speed of the second media relative to the first.
Complete answer:
Earthquakes radiate energy (in what we see as S and P waves) as each body and surface waves. Traveling through the interior of the earth, body waves arrive earlier than the surface waves emitted with the aid of using an earthquake. The body waves are of a better frequency than surface waves. The first sort of body wave is the P wave or primary wave. This may be visible on a seismograph, that is recorded with the aid of using a seismometer. Seismologists.
People who observe earthquakes. use seismographs to report the amount of time it takes seismic waves to journey through exceptional layers of the Earth. As the wave's journey through exceptional densities and stiffness, the waves may be refracted and reflected.
Because of the exceptional behavior of waves in exceptional materials, seismologists can deduce the sort of material the waves are journeying through.
The effects can offer an image of the Earth’s inner shape and assist us to discover and apprehend fault planes and the stresses and lines performing on them.
If there have been no modifications with depth, seismic waves could journey an instant direction to the alternative facet of the Earth. But wave arrivals to remote seismic stations have taught us that there are layers.
Note: Seismic waves journey through the Earth and comply with the equal legal guidelines of refraction and mirrored image as some other waves at interfaces. When they come across barriers among exceptional media, the waves react consistent with Snell’s law, and the perspective of refraction throughout the boundary will rely upon the speed of the second media relative to the first.
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