Want this question answered?
it is called the solar planet sunlight traveler sic check it up in ask . com
Because earths crust is denser than the mantle
"True, the Seismic Waves change speed and direction when they encounter different materials."
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.
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
It is between the Crust and the upper mantle
The Mohorovicic Discontinuity is the boundary between the crust and the mantle, where seismic waves change velocity.
It is the boundary between the earth's crust and mantle, across which there is a sudden change in the velocity of seismic waves Often shortened to Moho
Refraction Happens
The Mohorovicic Discontinuity, generally referred to as the Moho, where seismic waves increase in velocity.
it is called the solar planet sunlight traveler sic check it up in ask . com
Because earths crust is denser than the mantle
Yes, P-waves (primary waves) can travel through the Earth's mantle. P-waves are a type of seismic wave that is capable of propagating through solid, liquid, and gaseous materials. They are the fastest seismic waves and can travel through the mantle, which is the layer between the Earth's crust and core.
Yes. Compressional waves (P-waves) can travel through solids, liquids, and gases. They can propagate through every layer of earth's interior. In contrast, shear waves (S-waves) can pass through solids but not liquids or gases. As they propagate toward the center of the earth they pass through the crust, refract through the crust-mantle interface, pass through the mantle, but cannot pass through the mantel-outer core interface because the outer core is liquid.
Yes. It is called the Mohorovicic Discontinuity, where seismic waves increase in velocity.
because the waves travel through the solid crust and simisolid mantle they help see where the epicenter from an earthquake is
The Mantle--The layer directly below the crust which is delineated from the crust by the Mohorovicic Discontinuity, where seismic waves increase in velocity. The division between the mantle and the crust is a chemical one, the rocks and constituent minerals being higher in magnesium and lower in silicon and aluminum than crustal rocks. The mantle comprises 84% of Earth's volume.