The upper mantle is a solid layer of rock located beneath the Earth's crust. It is part of the Earth's mantle and extends from the base of the crust to a depth of about 660 kilometers. The upper mantle is mostly composed of peridotite, a dense rock made up of minerals like olivine and pyroxene.
A rock that can flow like a liquid is called a type of rock called "viscous rock," such as granite or basalt. These rocks exhibit a plastic-like behavior at high temperatures and pressures, allowing them to flow over long periods of time. This flow is known as creep.
The predominant rock in the Earth's crust and upper mantle is called silicate rock, composed mainly of silicon and oxygen. This type of rock is known as "peridotite" in the mantle and "granite" in the crust.
The upper mantle consists mainly of ultramafic rocks such as peridotite, which is rich in olivine, pyroxenes, and feldspar. These rocks are dense and typically dark in color due to their composition.
the mantle is made up of solid hot 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
The upper mantle is a solid layer of rock located beneath the Earth's crust. It is part of the Earth's mantle and extends from the base of the crust to a depth of about 660 kilometers. The upper mantle is mostly composed of peridotite, a dense rock made up of minerals like olivine and pyroxene.
The Earth's upper mantle is composed of solid rock that flows through liquid rock, also known as lava.
A portion of the upper mantle known as the asthenosphere.
The lower mantle is under greater pressure than the upper mantle, compressing the rock into a denser form.
Peridotite rock comes from the Earth's mantle, specifically the upper part of the mantle known as the upper mantle. It is formed from the cooling and solidification of magnesium- and iron-rich magma beneath the Earth's surface. Peridotite is typically brought to the surface through processes like mantle upwelling or tectonic movement.
A rock that can flow like a liquid is called a type of rock called "viscous rock," such as granite or basalt. These rocks exhibit a plastic-like behavior at high temperatures and pressures, allowing them to flow over long periods of time. This flow is known as creep.
The predominant rock in the Earth's crust and upper mantle is called silicate rock, composed mainly of silicon and oxygen. This type of rock is known as "peridotite" in the mantle and "granite" in the crust.
lithosphere
hard rock
The upper mantle consists mainly of ultramafic rocks such as peridotite, which is rich in olivine, pyroxenes, and feldspar. These rocks are dense and typically dark in color due to their composition.