Seismic waves are released during an earthquake. These waves can be classified into two main types: body waves, which travel through the Earth's interior, and surface waves, which travel along the Earth's surface. The movement of these waves is what causes the ground shaking experienced during an earthquake.
A seismic wave.
This statement is incorrect. The point directly above the focus of an earthquake is called the epicenter, not the S wave. S waves are one type of seismic wave that travel through the Earth's interior during an earthquake.
You can feel an earthquake from far away because the energy released during the earthquake travels as seismic waves through the Earth's crust. These waves can travel great distances and still be powerful enough to be felt by people even far from the epicenter.
During an earthquake, seismic waves are released. These waves are produced due to the sudden release of energy in the Earth's crust, causing the ground to shake. Seismic waves are categorized into two main types: body waves, which travel through the Earth's interior, and surface waves, which travel along the Earth's surface.
The S-P lag time is the difference in seconds between the arrival of the S-wave and the P-wave during an earthquake. This lag time can be used to estimate the distance to the earthquake epicenter.
sunami
seismic waves
During an earthquake, seismic waves are released. These waves travel through the Earth and can be detected by seismographs. The main types of seismic waves are P-waves (primary waves), S-waves (secondary waves), and surface waves.
The P wave
A specific type of mechanical wave known as a seismic wave.
A tsunami is not a storm. It is a wave created by an earthquake or landslide. A tsunami can strike during any kind of weather.
A seismic wave.
The first shock wave of an earthquake is known as the P-wave or primary wave. It is the fastest seismic wave and can travel through both solid and liquid materials. P-waves are responsible for the initial jolt felt during an earthquake.
a tsunami
That would be the P wave, or Primary wave
I'm pretty sure that an earthquake gives off a seismic wave and that seismic wave is then written on a seismograph that tells how strong it was and what kind of wave it was. with that knowledge a scientist can estimate how far away the earthquake was when it started and where it was
The secondary wave arrived later than the primary wave during the earthquake.