Seismic waves are the forms of energy produced by an earthquake.
No, It's Seismic Waves.
Love and Rayleigh waves which are collectively known as surface waves cause the most damage during earthquakes.
A specific type of mechanical wave known as a seismic wave.
They both based on the amount of energy that is released during earthquake
energy reachs earth surface through seismic waves: P waves S waves and Surface waves
in an earthquake, movement along the fault move and break, releasing energy as________
The sudden return of elastically deformed rock to sit original shape is called elastic rebound. Elastic rebound happens when stress on rock along a fault becomes so grat that the rock breaks or fails. This failure causes the rocks on either side of the fault to jerk past one another. During this sudden motion, large amounts of energy are released. This energy travels through rock as seismic waves. These waves cause earthquakes. The strength of an earthquake is related to the amount of energy that is released during elastic rebound.
Earthquake waves are called seismic waves.
Seismic Waves
Energy released during an earthquake creates seismic waves.
No, It's Seismic Waves.
Love and Rayleigh waves which are collectively known as surface waves cause the most damage during earthquakes.
Earthquake waves are called seismic waves.
Seismic waves are produced by earthquakes, rather than the cause of them! The most damaging seismic waves are the surface waves of which there are two types. Love waves and Rayleigh waves. For more information, please see the related links and question.
It is a seismic wave.
Seismic waves
Seismograms recorded during earthquakes help scientists learn about the composition of the earth by measuring the seismic waves that travel through the different layers of the Earth. The characteristics of these waves, such as their speed and amplitude, can provide information about the density, elasticity, and temperature of the materials they pass through. By analyzing seismograms from different locations, scientists can map the structure and properties of the Earth's interior, including the boundaries between different layers and the presence of seismic discontinuities.