Huge earthquake-caused waves are called tsunami in Japanese.
The source of earthquake waves is the epicenter of the earthquake.
Seismic waves end at an earthquake's center.
vibration that travels through earth carrying the energy released during an earthquake.
P waves arrive first at a seismograph station after an earthquake. The P waves are followed by S waves, and then surface waves.
Potential energy is transformed into seismic waves during an earthquake :)
Huge earthquake-caused waves are called tsunami in Japanese.
The source of earthquake waves is the epicenter of the earthquake.
Earthquake waves are called seismic waves.
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.
the bigger the waves the bigger the earthquake
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
earthquake waves travel through the earths crust.
Earth is the medium for earthquake waves.
seismic waves :)
surface waves
The surface waves are the slowest waves.