Seismic waves transmit energy through the Earth's layers, generated by events such as earthquakes, volcanic activity, or human-made explosions. They propagate as vibrations that can travel through solids, liquids, and gases, allowing scientists to study the Earth's internal structure. There are two main types of seismic waves: body waves (P-waves and S-waves) that travel through the Earth's interior, and surface waves that move along the Earth's surface. By analyzing these waves, researchers gain insights into geological formations and processes.
Seismic wave
A seismograph can locate a seismic wave.
You need a shotgun and shoot the wave and that's how you stop a seismic wave
the sound wave
why can s-wave can't travel but p-waves can
A seismograph can locate a seismic wave.
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
A shear wave is a type of seismic wave.
the sound wave
a seismic 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.
A body wave is a seismic wave that travels through Earths interior.
A body wave is a seismic wave that travels through Earths interior.
This type of wave is called a mechanical wave. It requires a medium (such as water or air) to travel through and can transmit energy in a specific direction at a known speed, such as sound waves or seismic waves.