What is the difference between S-Waves and P-Waves?
P and S waves refer to Primary and Secondary and Longitudinal waves. See explanation.
Waves travel through either a solid or a fluid medium (
liquid or gas). Consequently, this propagation has velocity.
In the direction of the velocity, if the propagation is similar or dissimilar, the
If a wave is longitudinal, it is referred to as transverse.
waves.
Primary waves travel in a bundle of longitudinal waves.
through media that are both solid and liquid.
Transverse waves bundled together as secondary waves are incapable of
propagate readily in a solid medium. Its rate is dependent upon the
the medium's resistance (shear force). Consequently, the
resistance comes primarily from solids. This resistance does, in fact
impacts how primary waves propagate.
Waves are caused by ground movement that is perpendicular to the
direction of the propagation velocity.
Citation:
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P-waves, also known as primary or pressure waves, are longitudinal seismic waves that can travel through solids, liquids, and gases faster than S-waves and that cause particles in the material to move in the same direction as the wave. S-waves, also known as secondary or shear waves, are transverse seismic waves that can only propagate through solid materials and move perpendicular to the direction of wave propagation.
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The main differences between S-waves (secondary or shear waves) and P-waves (primary or pressure waves) are:
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Propagation: P-waves are longitudinal waves, meaning they propagate by compressing and expanding the material in the direction of wave travel, whereas S-waves are transverse waves, propagating by oscillating perpendicular to the direction of wave travel.
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Speed: P-waves travel faster than S-waves. In solid materials, P-waves typically travel at around 1.7 times the speed of S-waves.
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Propagation Medium: P-waves can travel through solids, liquids, and gases, while S-waves cannot propagate through liquids or gases, as they require a solid medium.
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Effect on Material: P-waves cause particles in the material to move back and forth in the same direction as the wave, leading to compression and expansion. S-waves, on the other hand, cause particles to move perpendicular to the direction of wave travel, leading to shearing or twisting of the material.
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Nature of Oscillation: P-waves oscillate parallel to the direction of wave propagation, while S-waves oscillate perpendicular to the direction of wave propagation.
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Arrival Time: During seismic events, P-waves typically arrive at seismograph stations before S-waves, allowing seismologists to determine the distance to the earthquake's epicenter and providing early warning in earthquake detection systems.
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When evaluating a one-sided limit, you need to be careful when a quantity is approaching zero since its sign is different depending on which way it is approaching zero from. Let us look at some examples.
When evaluating a one-sided limit, you need to be careful when a quantity is approaching zero since its sign is different depending on which way it is approaching zero from. Let us look at some examples.
When evaluating a one-sided limit, you need to be careful when a quantity is approaching zero since its sign is different depending on which way it is approaching zero from. Let us look at some examples.
When evaluating a one-sided limit, you need to be careful when a quantity is approaching zero since its sign is different depending on which way it is approaching zero from. Let us look at some examples.

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