When a seismic wave is reflected, it will bounce off a boundary between different materials and change direction. This can cause the wave to be redirected back towards its source or continue traveling in a different direction.
It is called seismic wave reflection. When a seismic wave encounters a boundary between different materials with contrasting density or rigidity, some of the wave energy is reflected back towards the source.
The center of a seismic wave is called the focus or hypocenter. This is the point within the Earth where the seismic waves originate.
earthquake wave or shock wave
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.
The total energy in a seismic wave remains constant as the wave grows larger. The energy is spread out over a larger area, resulting in lower energy concentration at any specific point.
It is called seismic wave reflection. When a seismic wave encounters a boundary between different materials with contrasting density or rigidity, some of the wave energy is reflected back towards the source.
Reflection.
Seismic wave
A seismograph can locate a seismic wave.
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 seismic waves hit the Moho (Mohorovičić discontinuity), they can either be reflected back to the surface, refracted as they pass through the boundary, or converted into a different type of wave. This boundary separates the Earth's crust from the underlying mantle, resulting in changes in seismic wave behavior.
A shear wave is a type of seismic wave.
a seismic wave
the sound wave
That would be a P-wave or Primary wave which is a longitudinal seismic wave.
It is possible to have a seismic wave without having an earthquake. Any wave moving through the ground is a seismic wave, and all earthquakes are seismic waves. But seismic waves can be created by volcanic action, landslides, meteor strikes or the like. Though all earthquakes are seismic waves, not all seismic waves are earthquakes.