seismic
P-Waves. See the related links.
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
p waves
s waves
P or Primary waves are the fastest earthquake or seismic waves.
Earthquake waves are called seismic waves.
seismic waves
P-Waves. See the related links.
the waves that hit Haiti in the earthquake were as strong as a pair of balls fapping onto a wet vag
seismic waves
During an earthquake, seismic waves are released. These waves travel through the Earth and can be detected by seismographs. The main types of seismic waves are P-waves (primary waves), S-waves (secondary waves), and surface waves.
Seismic waves are released during an earthquake. These waves can be classified into two main types: body waves, which travel through the Earth's interior, and surface waves, which travel along the Earth's surface. The movement of these waves is what causes the ground shaking experienced during an earthquake.
secondary
An earthquake deep underground releases seismic energy in the form of seismic waves. These waves carry energy from the point of the earthquake's origin (the focus) and cause the ground to shake as they propagate through the Earth's crust.
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.