It need not go up and down. Assuming the wave moves "forward", the individual particles may move up and down, or left and right - or diagonally. In any case, the individual particles move at right angles to the movement of the wave, because that is what "tarnsverse" means.
S waves are more destructive than P waves because they travel in a more complex, side-to-side motion that can shake structures both vertically and horizontally. P waves, on the other hand, travel in a back-and-forth motion that may not cause as much structural damage.
Seismic waves generally speed up as they travel downward and reach the Moho, the boundary between the Earth's crust and mantle. This increase in speed is due to the change in density and composition of the Earth's layers, causing the waves to travel faster in the more rigid mantle layer compared to the crust.
P waves travel through both solid and liquid layers of the Earth in a straight line, while S waves are blocked by Earth's outer core and cannot pass through liquids. Therefore, S waves only travel through the solid layers of the Earth.
Secondary or S Waves are a form of waves which are produced as a result of shift in tectonic plates during an earthquake. Such waves only travel through solid surfaces and disintegrate upon reaching liquids. They always tend to adapt a back and forth motion as they move along. They are often referred to as "body waves".
Raleigh waves are surface waves that occur in many types of media, such as water and the Earth's crust. They cause the ground to roll up and down in a wave-like motion during an earthquake. Long waves, or long-period ocean waves, are also surface waves that have longer wavelengths and occur in the ocean due to forces such as gravity and wind.
Ocean waves travel in an up and down motion in a vertical direction.
In a vacuum, noise does not travel because there are no particles for the sound waves to travel through.
Sound does not travel in a vacuum because it requires a medium, such as air or water, to propagate. In the absence of a medium, there is no material for sound waves to travel through, so sound cannot travel up or down in a vacuum.
Sound waves are longitudinal waves; they travel from side to side, not up and down like transverse waves.
Surface Waves can propagate only along the boundary of solid.Two types are:Rayliegh Waves propagate along boundary between two dissimilar solid media, in a plane perpendicular to the surface and containing the direction of propagation.Love Waves are polarized shear wave with an associated oscillatory particle motion parallel to the free space and perpendicular to the direction wave motion.
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S waves are more destructive than P waves because they travel in a more complex, side-to-side motion that can shake structures both vertically and horizontally. P waves, on the other hand, travel in a back-and-forth motion that may not cause as much structural damage.
Seismic waves generally speed up as they travel downward and reach the Moho, the boundary between the Earth's crust and mantle. This increase in speed is due to the change in density and composition of the Earth's layers, causing the waves to travel faster in the more rigid mantle layer compared to the crust.
transverse waves are waves that go up and down
Transverse waves are disturbances in which the wave motion is perpendicular to the direction in which the waves travel. This means that the particles of the medium move up and down (or side to side) as the wave passes by, creating crests and troughs in the wave pattern. Examples of transverse waves include electromagnetic waves like light and radio waves, as well as seismic S-waves in earthquakes.
Transverse waves are the waves produced by moving a rope up and down. These are the types of waves seen in the ocean and in electromagnetic radiation (EM has two sets of waves perpendicular to one another and 90 degrees out of phase, for the electric and magnetic fields). Longitudinal waves are different...they are compression waves seen in sound.
slow down.