There is no seismic wave that can only pass through the Earth's mantle. However S-waves can not travel through earth's outer core because it is a liquid.
There are two types of waves ; P waves and S waves . P waves can travel through solids , liquids , and gases . S waves can only travel through solids . The mantle is pure solid rock ; the outer core is made of liquid-iron and nickel . In other words , only P waves can travel through both the mantle and the core . Hope this helps ! Give thanks to 7th grade Earth science ! :D
It's only soft and plastic in that it is not as hard as the brittle rock of the crust and uppermost mantle.
The inner core, outer core, and the mantle.
Yes, P-waves can travel through the Earth's crust, mantle, outer core, and inner core. They are the fastest seismic waves and can travel through both solid and liquid layers of the Earth, with their speed and direction changing as they encounter different materials.
The shadow zone is a specific region on Earth's surface where P waves from earthquakes are not detected. This occurs because P waves are refracted or absorbed by the outer core, creating a gap in seismic wave detection between 105 and 140 degrees from the earthquake epicenter. P waves that pass through the mantle only can be detected beyond this shadow zone, while those that pass through both the mantle and core are detected closer to the epicenter.
Primary waves and secondary waves (body waves). Love waves and rayleigh waves (surface waves) do not travel through the earth's mantle. Though secondary waves do not go through liquids, the asthenosphere is only a semi-liquid, so secondary waves can still go through it.
There are two types of waves ; P waves and S waves . P waves can travel through solids , liquids , and gases . S waves can only travel through solids . The mantle is pure solid rock ; the outer core is made of liquid-iron and nickel . In other words , only P waves can travel through both the mantle and the core . Hope this helps ! Give thanks to 7th grade Earth science ! :D
It's only soft and plastic in that it is not as hard as the brittle rock of the crust and uppermost mantle.
The inner core, outer core, and the mantle.
S-waves travel only through solids.
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
Primary seismic waves are longitudinal waves. Longitudinal waves can travel through solids, liquids and gasses (although seismic waves are of to low a frequency to normally be heard). Secondary seismic waves are transverse waves and only travel through solids.
Yes, P-waves can travel through the Earth's crust, mantle, outer core, and inner core. They are the fastest seismic waves and can travel through both solid and liquid layers of the Earth, with their speed and direction changing as they encounter different materials.
After the mantle, the next and last layer of the earths internal structure is the core, but the only sort of barrier that exists is a kind of transistion zone that serves as a linkage between the two layers.
im pretty sure it earths crust and core or if not the top part of the mantle and the crust above it this is the only infomation i could get sorry
If you mean Earth's interior, only longitudinal waves can pass through the liquid parts.
The shadow zone is a specific region on Earth's surface where P waves from earthquakes are not detected. This occurs because P waves are refracted or absorbed by the outer core, creating a gap in seismic wave detection between 105 and 140 degrees from the earthquake epicenter. P waves that pass through the mantle only can be detected beyond this shadow zone, while those that pass through both the mantle and core are detected closer to the epicenter.