waves occur all the time but after an earthquake tidal waves occur. Tidal waves are the cause of the tectonic plates colliding underwater. After the collision over time the wave goes form a small bump in the water to growing bigger and bigger into giant super wave capable of destroying towns.
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 fastest seismic waves, P-waves, will arrive first at a seismograph station after an earthquake. P-waves are compressional waves that can travel through both solids and liquids, allowing them to arrive at a station before the slower S-waves and surface 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.
Foreshocks can occur hours, days, or even weeks before a larger earthquake, but there is no definitive timeline. Foreshocks are smaller earthquakes that precede a larger mainshock, and their occurrence can vary depending on the specific earthquake event.
Seismic waves.
sciesmic waves ;]
when an earthquake occurs
Shadow zone
Yes.
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.
Waves can occur in any liquid. Waves can also be propagated through rock, during an earthquake, and the same mathematics that describes water waves also describes waves in electromagnetic energy such as light or radio.
Seismic waves occur when there is an earthquake.
Such waves have nothing to do with tides. The preferred term is tsunami.
Earthquake waves are called seismic waves.
The fastest seismic waves, P-waves, will arrive first at a seismograph station after an earthquake. P-waves are compressional waves that can travel through both solids and liquids, allowing them to arrive at a station before the slower S-waves and surface 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.
It happens due to the shifting of the earths plates.. Jus like a earthquake but it happens in the ocean!