Earthquake waves travel fastest in the interior of the Earth, as speed of waves increases as we go inside the Earth.
The speed of a wave depends on the properties of the medium it travels in. The wave propagates faster in the denser and heavier core.
because the waves travel through the solid crust and simisolid mantle they help see where the epicenter from an earthquake is
The waves of earthquakes help us determine information about the interior of the earth. The more geologists know about the interior of the earth, the better they can predict earthquakes and other changes in the formation of the Earth's crust.
earthquake/fissure
The Earth's crust is on the exterior, not the interior; that is why it is called the crust. It is on the outside. It is made mostly of rock, of various kinds. The rock of the crust is on average less dense than the rock of the mantle, which lies beneath the crust.
The crust and the lithosphere.
earthquake waves travel through the earths crust.
because the waves travel through the solid crust and simisolid mantle they help see where the epicenter from an earthquake is
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The waves of earthquakes help us determine information about the interior of the earth. The more geologists know about the interior of the earth, the better they can predict earthquakes and other changes in the formation of the Earth's crust.
It is cause by the Mojo Discontinuity. It is a zone that differs in density.
No. Earth's interior is so hot that you could not even make it through the crust.
A shaking of the crust of the Earth could symbolize an Earthquake. This shaking of the crust can be measured with special machines.
A crack in the Earth's crust that can lead to an earthquake is called a fault.
The epicenter is the spot on earth's crust directly above the spot where the earthquake formed.
earthquake/fissure
After the earthquake, the crust has been repositioned, and frictional tension at fault lines once again begins to mount until the next earthquake.
An earthquake an occur anywhere in the Earth's crust but they are more common along plate boundaries.