The particles of the wave (for compressive waves). Or for transverse waves, yet the particles move parallel to the wave too.
surface waves
In a longitudinal wave, the particles do not move with the wave. The particle movement is parallel to the direction of the wave propagation. This means that the particles move left and right which in turn makes the other particles start to oscillate. This creates a wave. longitudinal pressure waves are also known as sound 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.
Disturbance in particle motion parallel to the wave velocity is called a longitudinal wave. Disturbance in particle motion perpendicular to the wave velocity is called a transverse wave.
false, they vibrate parallel
Both parallel and perpendicular to the motion of the wave at the same time/Perpendicular to the motion of the wave/Parallel to the motion of the wave - APEXPerpendicular to the motion of the wave.Parallel to the motion of the wave.Both parallel and pependicular to the motion of the wave at the same time.
Surface waves are where particles of the medium move both parallel and perpendicular to wave motion. This movement creates a circular motion pattern. An example of a surface wave is water waves on the surface of a pond.
Transverse waves cause particles to move back and forth in a direction perpendicular to the wave motion. Longitudinal waves, on the other hand, cause particles to move back and forth in a direction parallel to the wave motion.
The medium vibrates in a direction parallel to the wave's motion due to the oscillation of particles along the same axis as the wave propagation. This type of wave motion is known as a transverse wave, where the particles move perpendicular to the direction of energy transfer.
In a compressional wave, particles vibrate parallel to the direction of the wave motion. The particles move back and forth in the same direction that the wave is traveling, causing compressions and rarefactions as the wave passes through the medium.
Longitudinal waves move in the same direction as the wave energy, with particles vibrating parallel to the wave motion. Transverse waves move perpendicular to the wave energy, with particles vibrating perpendicular to the wave motion.
In a compressional wave, the particles move in the same direction as the wave, which is parallel to the motion of the wave. This results in compressions (areas of high pressure) and rarefactions (areas of low pressure) moving through the medium in the same direction as the wave.
Surface waves involve both longitudinal and transverse motion of the particles in the medium. This means the particles move both up and down, as well as back and forth, in a circular or elliptical motion. The motion of the particles is more complex compared to simple longitudinal or transverse waves.
Transverse waves occur when the motion of the medium is perpendicular to the direction of the wave. When the motion of the medium is parallel to the direction of the wave, longitudinal waves are formed. In longitudinal waves, the particles of the medium move back and forth parallel to the direction of wave propagation.
In a longitudinal wave, particles move parallel to the direction of wave propagation. As the wave travels, particles oscillate back and forth in the same direction that the wave is moving. This motion causes compressions and rarefactions to propagate through the medium.
A longitudinal wave occurs when the motion of the medium is parallel to the direction of the wave. In this type of wave, the particles of the medium move back and forth in the same direction as the wave. Examples of longitudinal waves include sound waves and seismic waves.
In a longitudinal wave, the particles of the medium move parallel to the direction of the wave. This means that the particles oscillate back and forth in the same direction that the wave is traveling. This motion creates areas of compression and rarefaction in the medium, which propagate through the material.