the mantle is 2900 kilometers wide.
The mantle is divided into the upper mantle and the lower mantle. The upper mantle lies directly beneath the Earth's crust and extends to a depth of about 410 miles. The lower mantle extends from the bottom of the upper mantle to a depth of about 1,800 miles.
The lower part of the mantle is called the "lower mantle" or "mesosphere", while the upper part of the mantle is referred to as the "upper mantle" or "asthenosphere".
The mantle is divided into two main layers: the upper mantle and the lower mantle. The upper mantle is closer to the Earth's crust and is more rigid, while the lower mantle is hotter and flows more easily due to higher temperatures and pressures.
The mantle is divided into the upper mantle, transition zone, and lower mantle. The upper mantle is beneath the lithosphere, the transition zone lies between the upper and lower mantle, and the lower mantle extends to the outer core.
The outer mantle is part of the Earth's mantle that is closer to the surface, while the inner mantle is deeper within the Earth. The outer mantle is composed of solid rock that can flow slowly over geologic time, while the inner mantle is under higher pressure and temperature, making it more solid and rigid.
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The upper mantle and the lower mantle.
The mantle is divided into the upper mantle and the lower mantle. The upper mantle lies directly beneath the Earth's crust and extends to a depth of about 410 miles. The lower mantle extends from the bottom of the upper mantle to a depth of about 1,800 miles.
the inner mantle is hotter than the outer mantle.
The lower part of the mantle is called the "lower mantle" or "mesosphere", while the upper part of the mantle is referred to as the "upper mantle" or "asthenosphere".
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Mantle Is The Below Layer Of The Crust In Earth.
Not, notnecessarily. The lithosphere consists of the crust and the upper part of the mantle. The rocks of the crust come in a wide varity of colors. Some of the more common rocks may be black, gray, white, red, brown or red. The upper part of the mantle is largely composed of peridotite, which is green.
The mantle is divided into two main layers: the upper mantle and the lower mantle. The upper mantle is closer to the Earth's crust and is more rigid, while the lower mantle is hotter and flows more easily due to higher temperatures and pressures.
The mantle is divided into the upper mantle, transition zone, and lower mantle. The upper mantle is beneath the lithosphere, the transition zone lies between the upper and lower mantle, and the lower mantle extends to the outer core.
The outer core of the earth, just inside the mantle is about 1,408 miles thick. It is most composed of iron and nickel in a molten, high pressure state.
New evidence supported by geologists world wide suggests that the earth's mantle may be the source of crude oil, in an ongoing geological process inside the earth.