The type of seismic waves that cause back and forth motions are P waves. P waves cause particles in material to vibrate back and forth.
Surface waves, specifically Love and Rayleigh waves, are responsible for creating the rolling motion in the ground during an earthquake. These waves travel along the surface of the Earth and can cause buildings and structures to sway back and forth, similar to ocean waves.
Primary waves (P-waves) are the type of seismic wave that travels the fastest through rock material. These waves are able to cause rocks to vibrate in the same direction as the waves, resulting in a back-and-forth motion.
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.
The type of mechanical wave in which particles in the medium move back and forth in the direction of wave motion is called a longitudinal wave. In a longitudinal wave, the particles oscillate parallel to the direction of wave propagation, creating compressions and rarefactions along the wave. Sound waves are an example of longitudinal waves.
the movement of the matter that is back and forth, therefore it has physical properties and chemical properties which can be found on the periodic table of protons and electrons or the changes of state from solid to liquid to gas and back. science knowledge
p A+
p A+
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.
Transverse waves cause particles to move perpendicular to the direction of the wave's propagation, creating a back and forth motion. This type of wave motion is characteristic of waves on a rope or string.
Transverse waves cause particles to move perpendicular to the direction of the wave. This leads to a back-and-forth motion of particles. Examples of transverse waves include electromagnetic waves such as light and water 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.
Surface waves, specifically Love waves and Rayleigh waves, cause the ground to shake in a back and forth motion perpendicular to the direction of wave propagation. These waves travel along the Earth's surface and are responsible for the horizontal shaking experienced during an earthquake.
The back and forth up and down motion of a wave is called oscillation. This motion involves the movement of particles or energy in a repeated pattern around a central point. oscillation can be seen in various natural phenomena such as sound waves, light waves, and water waves.
Sound waves are caused by the back and forth movement or vibration of an object. This motion creates pressure variations in the surrounding medium, which propagate as waves.
Vibrations
Compression or commonly called a longitudinal wave.
Compressional waves, also known as longitudinal waves, move in a back-and-forth motion parallel to the direction of wave propagation. These waves cause particles in the medium to move closer together and farther apart as the wave passes through. Examples include sound waves and seismic waves.