Rocks of the mantle are peridotite, dunite, and eclogite. In deeper regions, the olivine may be replaced by more stable minerals.
ferro magnesium silicate rocks
The heat from the mantle and core.
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.
Igneous rock.
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.
Crustal rock is normally less dense than mantle rock.
ferro magnesium silicate rocks
the mantle is made of hot lava with rocks and pee
Mantle rock is classified as ultramafic igneous rock.
The heat from the mantle and core.
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.
The Mantle.