Semitic wave
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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.