When a seismic wave crosses a boundary between different materials, it may undergo reflection, refraction, or diffraction. Reflection occurs when the wave bounces off the boundary, while refraction causes the wave to change speed and bend as it enters a different material. Diffraction causes the wave to spread out as it encounters an obstacle or edge.
Refraction
The center of a seismic wave is called the focus or hypocenter. This is the point within the Earth where the seismic waves originate.
Another word for seismic waves is tremors.
Seismic waves are generated when there is a sudden release of energy from within the Earth's crust, such as an earthquake or explosion. This energy travels through the Earth as waves, causing the ground to shake. The type of seismic wave produced depends on the type of energy release and the properties of the Earth's layers it travels through.
Seismic wave
That would be a P-wave or Primary wave which is a longitudinal seismic wave.
The surface wave.
S waves, or secondary waves, are transverse seismic waves, meaning that the particles being effected by the wave are moving perpendicular to the wave's propagation.
surface waves
Surface waves
A seismograph can locate a seismic wave.
secondary waves or otherwise known as s-waves
a seismic wave, earthquake, landslide
The fastest wave is the electromagnetic wave. Of the seismic waves, the P-wave is the fastest seismic wave.
You need a shotgun and shoot the wave and that's how you stop a seismic wave
When a seismic wave crosses a boundary between different materials, it may undergo reflection, refraction, or diffraction. Reflection occurs when the wave bounces off the boundary, while refraction causes the wave to change speed and bend as it enters a different material. Diffraction causes the wave to spread out as it encounters an obstacle or edge.