Seismic Waves: How Are They Produced?

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SUMMARY

Seismic waves are produced by various activities that deform rocks, including earthquakes, meteorite impacts, explosions, and even minor actions like hammering the ground. When the elastic limit of rocks is exceeded, they typically break, limiting the maximum magnitude of seismic energy that can be propagated. The discussion highlights that the moment magnitude scale has replaced the obsolete Richter scale for measuring earthquake magnitudes. Notably, events like the Chicxulub impact generate shock waves, which differ from elastic seismic waves.

PREREQUISITES
  • Understanding of seismic wave propagation
  • Knowledge of elastic limits in materials
  • Familiarity with the moment magnitude scale
  • Basic concepts of geological events like earthquakes and meteorite impacts
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  • Research the differences between seismic waves and shock waves
  • Study the moment magnitude scale in detail
  • Explore the geological implications of the Chicxulub impact
  • Learn about the elastic properties of different rock types
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Geologists, seismologists, students of earth sciences, and anyone interested in understanding the mechanics of seismic wave production and measurement.

Awsom Guy
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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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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.
 
So what would happen if the elastic limit was surpassed?
It would simply break, right?
 
Yes makes very sense, thank you so much.
 
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.
 
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.
 
Arrrr... moment magnitude scale. Thanks for that information. Quite impressive. Obsolete indeed. Thank you.
 

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