Speed up
Earthquakes produce "seismic" waves. These can be split into two main types: Body Waves and Surface Waves. Body waves consist of P-waves (compression or longitudinal waves) and S-waves (shear or transverse waves). P-waves can go through solid, liquid, and gas forms but S waves can only travel through solids. The P waves reach seismic stations quicker than S waves as they travel at a greater speed. Surface waves travel more slowly than Body waves and there are two main types: The Rayleigh and Love wave.
Seismic waves are waves that travel through the Earth or other elastic body2 to 8 kilometersThe primary factor is the composition of the rock that the wave travels through. Secondarily, temperature tends to lower the wave speed and pressure tends to increase the wave speed.
a more rigid material
Moho
The speed of the waves that travel through the interior can tell the density of each layer of the Earth. Some waves can make it through certain layers, but not others.
IT travels the same speed as far as i Know
The speed of seismic waves are affected by the type of material that the waves are traveling through. in other words (as an example): some type of waves can travel through rocks but not through liquids.
In air, the seismic waves(P-wave) are simply sound waves, and travel with the speed of sound (approx. 335 m/s).
You can't travel at the speed of light. It might be possible, in theory, to approach it, but not quite to reach it.
The time-distance graph of seismic waves shows the relationship between the time it takes for seismic waves to travel and the distance they travel. It helps in determining the speed at which seismic waves propagate through the Earth's interior and provides information about the structure and composition of the Earth's layers.
It would move slightly backwards due to no air resistance------------------------------------------------------- The above answer is rubbish. It would continue travelling forward. Whilst travelling forward it would also travel down. It would continue to travel forward until it slowed down to a zero forward speed ( DUE to air resistance ) but a terminal downward speed. Whether or not it would reach a zero forward speed and terminal downward speed would depend on how high it was when it was dropped.
88mph
The speed of the waves depends on the density of the material.
"True, the Seismic Waves change speed and direction when they encounter different materials."
The velocity of seismic waves is controlled by the density and elastic properties of the material through which they travel. Solids tend to have larger elastic modulii than fluids. As the speed of a seismic wave increases as the elastic modulii increase, this means that they tend to travel faster through solids.
Earthquakes produce "seismic" waves. These can be split into two main types: Body Waves and Surface Waves. Body waves consist of P-waves (compression or longitudinal waves) and S-waves (shear or transverse waves). P-waves can go through solid, liquid, and gas forms but S waves can only travel through solids. The P waves reach seismic stations quicker than S waves as they travel at a greater speed. Surface waves travel more slowly than Body waves and there are two main types: The Rayleigh and Love wave.
Seismic waves travels faster through solid rock than water because their speed depends on the density and composition of material that they pass through.Solid rock is denser than water, hence the energy from seismic waves transfer faster through solid rock than in water.