Earthquakes are made up of 4 different seismic waves, P, S, L and R. L and R are surface waves, and have virtually nothing to do with the interior. However, P and S are body waves and do.
P waves are compressional waves, that is they push and pull against rock in the same direction as the waves move. They are the fastest. S waves vibrate material up and down. Both travel faster in more dense material, and P waves travel slower in liquid while S waves are unable to move through liquid at all.
As the Earth's outer core is liquid, and inner core is very dense, this affects the waves as they travel through the Earth. It speeds them up and slows them down according to the density. Because S can't go through the outer core, there is a "shadow zone" at a certain area on the Earth where there are no S waves at all. P waves also have a smaller shadow zone, where the waves are diflected and bent within the outer core.
It affects speed & direction of the wave.
rocks and seismic waves
body waves
no they use seismic waves
due to volcanics effects and movement of earth which affect the earth surface
why do you think scientists study earths interior?if you were a scientists ,will you undertake a study of the earths interior?
deflect
Because of the study of seismic waves from earthquakes
A body wave is a seismic wave that travels through Earths interior.
A body wave is a seismic wave that travels through Earths interior.
rocks and seismic waves
Seismic waves
body waves
body waves
body waves
From seismic interpretations of earthquake date. From computer modeling. From the study of meteorites, From geochemistry and form the study of mantle xenoliths.
Seismic data
scientists use seismic waves to map earths interior by seismographs that measure the times at witch seismic waves arrive at different distances from an earth quake.