They bend when they go through different materials.
Source earthquake waves are seismic waves produced directly from the earthquake's source, such as the initial rupture of rocks along a fault. These waves include P-waves and S-waves that travel through the Earth and are used to locate and study earthquakes. Source earthquake waves provide valuable information about the earthquake's characteristics and help in assessing its impact.
Earthquake waves are vibrations that travel through the Earth's crust when an earthquake occurs. There are three main types of earthquake waves: primary (P) waves, secondary (S) waves, and surface waves. These waves can cause the ground to shake and can be detected by seismographs.
Seismic waves.
Earthquake generated waves are called seismic waves. These are waves of energy that travel through the Earth's layers. Their velocity depends on the elasticity and density of the medium that they travel through.
The vibrational tremors sent out from an earthquake are known as seismic waves. These waves travel through the Earth's crust and are responsible for the shaking felt during an earthquake. There are two main types of seismic waves: primary (P-waves) and secondary (S-waves).
Earthquake waves, like other types of waves, carry energy and propagate through a medium. They can be described in terms of wavelength, frequency, and amplitude. Additionally, earthquake waves can undergo reflection, refraction, and diffraction just like other waves.
The primary waves (P-waves) are the first to reach a seismograph after an earthquake. These waves are faster than other seismic waves and can travel through both solid and liquid materials.
Earthquake waves are called seismic waves.
Source earthquake waves are seismic waves produced directly from the earthquake's source, such as the initial rupture of rocks along a fault. These waves include P-waves and S-waves that travel through the Earth and are used to locate and study earthquakes. Source earthquake waves provide valuable information about the earthquake's characteristics and help in assessing its impact.
the bigger the waves the bigger the earthquake
Earthquake waves are vibrations that travel through the Earth's crust when an earthquake occurs. There are three main types of earthquake waves: primary (P) waves, secondary (S) waves, and surface waves. These waves can cause the ground to shake and can be detected by seismographs.
the crust of the earth is swithching over each other
Earth is the medium for earthquake waves.
earthquake waves travel through the earths crust.
S waves, or Secondary waves, are earthquake waves during an earthquake. They crash after P waves ( Primary waves) and are less stronger than surface waves
seismic waves :)
surface waves