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The fastest waves from an earthquake, also known as push waves, are called primary waves or P-waves. These seismic waves are the first to arrive at a seismograph station and they travel through solid rock and fluid at high speeds by compressing and expanding the material they pass through.
Earthquake waves travel outward in all directions from the point of seismic activity, which is known as the focus. The waves can move through the Earth's interior in various directions, including up towards the surface, causing shaking and potential damage.
Body earthquake waves that can penetrate the Earth's core are known as primary waves, or P-waves. They are the fastest seismic waves and can travel through both solid and liquid materials, including the Earth's inner core.
Surface waves, such as Love waves or Rayleigh waves, are the seismic waves that cannot be detected on the side of Earth opposite an earthquake. These waves travel along the Earth's surface and are responsible for causing most of the damage during an earthquake.
The wave of an earthquake, known as seismic waves, travel through the Earth's crust and cause the ground to shake. These waves can result in damage to buildings, infrastructure, and the environment. They are key to understanding the intensity and impact of an earthquake.