These are called s waves (secondary waves) while p waves move up and down s waves move side to side
The subtypes of secondary waves (S-waves) are Love waves and Rayleigh waves. Love waves cause horizontal movement, while Rayleigh waves cause both horizontal and vertical movement. Both types of waves are surface waves that move along the Earth's crust.
P waves - compress and expand the ground like a Accordion S waves - vibrate from side to side as well as up and down Surface waves - make the ground roll like ocean waves The Earthquake is produced by each of the three types of seismic waves.
P waves (primary waves) are the first seismic waves to arrive during an earthquake. While they typically don't cause significant damage, they can still shake buildings and create a buzzing or rumbling sound. P waves travel the fastest through the Earth's layers and are mostly known for their ability to provide early warning of an impending earthquake.
L waves, or Love waves, are a type of surface wave that travel near the Earth's surface and cause horizontal shaking during an earthquake. These waves are slower than other types of seismic waves but can cause significant damage due to their side-to-side motion.
Surface waves are a type of seismic wave that travels along the Earth's surface and can cause rocks and other surface materials to move in a rolling or shaking motion. This movement can lead to landslides, rockfalls, and other types of mass wasting events. The amplitude and frequency of surface waves can determine the extent of rock movement.
The movement of the waves.
The subtypes of secondary waves (S-waves) are Love waves and Rayleigh waves. Love waves cause horizontal movement, while Rayleigh waves cause both horizontal and vertical movement. Both types of waves are surface waves that move along the Earth's crust.
Transverse waves have movement that is perpendicular to the direction of the wave's propagation. This means that the particles of the medium oscillate up and down or side to side as the wave moves forward. Examples of transverse waves include electromagnetic waves (such as light) and some seismic waves.
In transverse waves, energy is transferred perpendicular to the direction of the wave's movement. This transfer happens as the wave's oscillations cause particles in the medium to move up and down or side to side, passing energy along the wave's path.
side and up/down
S waves
Seismic waves, specifically shear waves or S-waves, cause particles in rock to move back and forth during an earthquake. These waves propagate by producing a side-to-side motion that leads to the shaking and fracturing of rocks.
secondary waves
the surface waves cause vibrations invisible to the eye. these vibrations shake rocks and stuff on the surface and result in fractional movement.
Crustal movements cause earthquakes because of the sound waves and the movement underground.
Seismic waves that cause particles of rock to move in a side-to-side direction are known as S-waves or secondary waves. These waves are a type of shear wave that travel through the Earth during an earthquake, moving perpendicular to the direction of wave propagation. S-waves can only travel through solid materials, which distinguishes them from P-waves (primary waves) that can move through both solids and liquids. Their side-to-side motion is responsible for much of the shaking felt during seismic events.
Shear waves, also known as S-waves, cause particles in rocks to move perpendicular to the direction of wave propagation. These waves are a type of seismic wave that travel through the Earth's crust during an earthquake. Shear waves can cause significant damage to structures due to their side-to-side motion.