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I do not think humans can travel deeper than the crust because, the crust and the mantle is too thick. The crust is 600km and the mantle is 12,900km.
because the waves travel through the solid crust and simisolid mantle they help see where the epicenter from an earthquake is
what are some examples of seismic disturbances
Mohorovicic discontinuity
Andrija Mohorovicic, 1909
I do not think humans can travel deeper than the crust because, the crust and the mantle is too thick. The crust is 600km and the mantle is 12,900km.
(not seismic, seismic wave)Seismic waves are waves of energy that travel through the earth.
Seismic, or earthquake waves travel through the earth. They may travel through our crust, which is rocky, or through the more fluid parts, like the mantle, but the medium is the earth.
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because the waves travel through the solid crust and simisolid mantle they help see where the epicenter from an earthquake is
what are some examples of seismic disturbances
Mohorovicic discontinuity
Earthquakes
Seismic waves are the earths crust vibrating. there are two types of waves P-waves and S-waves (Primary and Secondary) Primary waves travel faster than s waves and can travel through solid and liquid, S-waves can only travel through solids
Pressure
Probably the cheese and pepperoni's. You need to fix your question and specify what crust.
Seismic currents in the earth's mantle.