the minerals posses a number of properties that are used as an aid in their identitification
the upper-mantle rocks are heavier while the lower mantle rocks are semisolid like melted plastic
the upper-mantle rocks are heavier while the lower mantle rocks are semisolid like melted plastic
A mantle is a layer of hot rocks.
Igneous rock.
When rocks are melted, they form igneous rocks. This can happen through processes like volcanic activity or within the Earth's mantle.
Crustal rock is normally less dense than mantle rock.
ferro magnesium silicate rocks
the mantle is made of hot lava with rocks and pee
Rocks that come from the mantle are called mantle rocks. These rocks are typically formed deep within the Earth's mantle and can include peridotite, dunite, and eclogite. Mantle rocks are brought to the surface through processes like volcanic eruptions or tectonic movements.
Mantle rock is classified as ultramafic igneous rock.
Few earthquakes happen in the earths mantle do to the fact that the mantle has a folded deformation. This means that the amount of pressure on the mantle caused it to deform.
Isostasy is the flotational balance achieved between rocks of the crust lithosphere and deeper mantle. This balance is maintained as lighter rocks of the crust "float" on the denser rocks of the mantle below.