Seismic Waves: How Are They Produced?

In summary, earthquakes are caused by the breaking of rocks. When the rocks are squeezed or stretched too much, the rocks break and seismic energy is still propagated. The strength of rocks puts a limit to the maximum magnitude of an earthquake.
  • #1
Awsom Guy
77
0
HI,
I want to know how seismic waves are produced?. I cannot find any information on it on google. Any help will be helpful.
Thanks.
 
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  • #2
Earthquakes, meteorite impact, explosions, drilling activity, hitting the ground with a hammer, kangaroos jumping on the ground, wind blowing trees and shaking the trees. Seismic waves are elastic waves (to a very good approximation), so anything that squishes, squeezes, or twists the rocks will propagate as seismic waves provided that the elastic limit of the rocks is not surpassed.
 
  • #3
So what would happen if the elastic limit was surpassed?
It would simply break, right?
 
  • #4
Yes makes very sense, thank you so much.
 
  • #5
BL4CKCR4Y0NS said:
So what would happen if the elastic limit was surpassed?
It would simply break, right?

That depends somewhat on the properties of the rock. There are some materials, like for example a spring, that when you exceed the elastic limit the spring is permanently deformed -- it doesn't break or snap, it is just stretched beyond its elastic limit.

In rocks, most of the time the rock will break when it has been squeezed or stretched too much (bearing in mind we are sticking to short time scales here -- over very long time scales the rock can behave very differently and change shape a bit like the spring). In that case the rock is squished until it can stand it no longer and it is broken, seismic energy is still propagated but the elastic limit of the rock puts a cap on the maximum amount of seismic energy that can be propagated. Interestingly, the strength of rocks puts a limit to the maximum magnitude of an earthquake (measured in ground shaking), you cannot get earthquakes larger than about a 10 on the magnitude scale, if you try to put in more energy the energy is spent in tearing up the rocks locally and is not propagated as seismic waves.
 
  • #7
Awsom Guy said:
Are you sure about "you cannot get earthquakes larger than about a 10 on the magnitude scale" cause check the table out in wikipedia. http://en.wikipedia.org/wiki/Richter_magnitude_scale

It has a 12.55. :0

Well as I said it depends on the rocks.

There are though at least two things here that need mentioning:

1) The Chicxulub event was not an earthquake, it was a huge meteorite impact that probably wiped out the dinosaurs 65 million years ago. Actually, a lot of the energy from the Chicxulub impact would've been transmitted as shock waves (which travel faster than seismic waves) which are definitely NOT elastic waves. So meteorites can make things happen which go off the chart, meteorites can also vapourize rocks and excavate huge craters -- you just can't get that with earthquakes.

2) The Richter scale is obsolete. Seismologists now use the moment magnitude scale http://en.wikipedia.org/wiki/Moment_magnitude_scale.
 
  • #8
Arrrr... moment magnitude scale. Thanks for that information. Quite impressive. Obsolete indeed. Thank you.
 

What are seismic waves?

Seismic waves are vibrations that travel through the Earth's layers, caused by energy released during earthquakes or other seismic events.

How are seismic waves produced?

Seismic waves are produced when there is sudden movement or displacement of rock along a fault line, resulting in the release of energy that propagates through the Earth as waves.

What are the different types of seismic waves?

The three main types of seismic waves are P-waves, S-waves, and surface waves. P-waves are longitudinal waves that can travel through solid, liquid, and gas, while S-waves are transverse waves that can only travel through solid. Surface waves are a combination of P and S waves that travel along the surface of the Earth.

How are seismic waves measured?

Seismic waves are measured using seismographs, which record the motion of the ground during an earthquake. The amplitude, frequency, and arrival time of the waves can be used to determine the magnitude and location of the earthquake.

What can we learn from studying seismic waves?

Studying seismic waves can help us understand the structure and composition of the Earth's interior, as well as the processes that occur during earthquakes. It can also aid in predicting and preparing for future seismic events.

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