it becomes a liquid
ferro magnesium silicate rocks
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.
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.
The Mantle.
Yes. Magma is underground molten rock.
The area is known as the mantle transition zone and it is located between the upper mantle and the lower mantle. This region is characterized by high pressures and temperatures, causing rocks to undergo changes in their physical and chemical properties.
the minerals posses a number of properties that are used as an aid in their identitification
thickness 1/8( a mixture of lighter and heavier rocks which were forced out from the mantle by volcanic activity)
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.
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.