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They are both very hot
They don't. The presence of magma at mid-ocean ridges is due to the effect of less pressure on the mantle below known as "decompressional melting". Mantle rock is extremely hot, yet it remains in solid state because it is under immense pressure. At mid-ocean ridges, where tectonic plates are pulling apart, the crust is thinner, meaning less pressure on the mantle rocks below, thus they are able to melt, become less dense and rise.
Below the mantle is the core.
the layer under the mantle layer is the outer core
Upper Mantlemantle
it will steady as liquid form and hot
The lower mantle is under greater pressure than the upper mantle, compressing the rock into a denser form.
No. The mantle is under such great pressure that any pore space would close immediately.
it would harden just like silly putty
They are both very hot
They don't. The presence of magma at mid-ocean ridges is due to the effect of less pressure on the mantle below known as "decompressional melting". Mantle rock is extremely hot, yet it remains in solid state because it is under immense pressure. At mid-ocean ridges, where tectonic plates are pulling apart, the crust is thinner, meaning less pressure on the mantle rocks below, thus they are able to melt, become less dense and rise.
Diamonds form under great pressure and heat in the mantle. The mantle surrounds the core. Diamonds are found in intrusive lava, (underground deposits)
Below the mantle is the core.
under the upper mantle
the brain can work under heavy pressure, giving the brain a challenge make the human personality react differently and provide confidence to the conscience mind.
The mantle rock is not hot enough to melt while under the pressure that exists at the depth it is at.When the crust cracks like it does at the spreading centers at mid-ocean ridges, the pressure is released just enough to allow melting of the top layer of the mantle, producing very dense basaltic lava.
from being under the mantle the gas pressure builds up and forces magma out forming a hot spot.