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What are source earthquake 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.
What are earthquake waves?
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.
What is another name for earthquake waves?
Seismic waves.
What are huge waves call caused by earthquakes?
Huge waves caused by earthquakes are called tsunamis. These are large ocean waves generated by the displacement of water due to undersea seismic activity, such as an earthquake. Tsunamis can travel across oceans and cause widespread destruction along coastlines.
What are earthquake generated waves called?
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.
What do you call the waves of energy formed by an earthquake?
Potential energy is transformed into seismic waves during an earthquake :)
What is the kind of earthquake released during an earthquake?
Earthquake waves are called seismic waves.
What are source earthquake 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.
Which layer of the earth is the place where earthquake waves unexpectedly slow down?
Direct Answer: AsthenosphereExplained Answer: Earthquake waves normally go faster with increasing depth. However, below the lithosphere, the upper mantle contains a curious layer in which earthquake waves unexpectedly slow down. Geologists call this layer the asthenosphere.
How is a focus of an earthquake related to seismic waves?
the bigger the waves the bigger the earthquake
What are earthquake waves?
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.
What is the medium for earthquake waves.?
Earth is the medium for earthquake waves.
What do earthquake waves travel through?
earthquake waves travel through the earths crust.
What are known as s waves?
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
What are the waves from an earthquake know as?
seismic waves :)
Which earthquake waves are slowest?
surface waves
What are the slowest earthquake waves?
The surface waves are the slowest waves.
