How fast do p waves travel?
It depends on the medium that they're travelling through.
P-waves (also called pressure waves and/or primary waves) are the first waves to be seen on a seismograph, which makes them the fastest travelling waves. The waves' speed depends on the medium they're moving through, such as liquid (water, oil), solid (rock), or a gas, in addition to the inclusion of fractures or vesicles in solids. Density also plays a very significant role.
The generic answer is 5 to 8 km/s, but they can travel much faster or slower depending, of course, on the matter they're moving through. The fastest speed, as shown below in the image, is the propagation through the earth's core, near 14 km/s (though it's generally referenced as approximately 13 km/s).
The speed of p-waves is relatively slow through some looser solids, like scree (smaller rocks) and substances that are mostly solid, like soil. These can be as low as 300 m/s, which is slower than the generally referenced speed of sound (about 340 m/s at sea level).
It is much faster through the more dense rock, like basalt or its intrusive cousin, granite (upwards to approximately 6 km/s each). Below is a good reference table.
Also note that I use the word "speed" while most people use "velocity" to describe the rate of propagation of the waves. Technically speaking, speed is the more correct terminology since there isn't a direction referenced for it to qualify to be labeled as a vector quantity (unless, of course, you choose to reference one, but that's not really how waves work).
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P waves travel at speeds ranging from about 1.5 to 8 kilometers per second (km/s) in the Earth's crust and upper mantle.
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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.
- What are the 3 main types of seismic waves? How do they differ from each other?
- How is the amount of energy released during an earthquake measured?
- What is the stress force that pulls on the crust where two plates are moving apart?
- What can the time lag between the first arrival of the P-wave and first arrival of the S-wave be used to determine?
- What is tension and where in the crust is this likely to occur?

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