Felsic rocks.
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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 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 crust is the outermost layer of the Earth, consisting of solid rock that varies in thickness from about 5 to 70 kilometers. The upper mantle lies beneath the crust and is more rigid, extending to a depth of about 660 kilometers. Both layers are part of the Earth's lithosphere.
A rigid block of crust and upper mantle-rock is known as a tectonic plate. These plates make up the Earth's lithosphere and can move and interact with each other at plate boundaries.
The mantle has two parts: the upper mantle, which is directly below the Earth's crust and makes up about 15% of the Earth's volume, and the lower mantle, which extends from the top of the lower mantle to the outer core. The mantle is mainly composed of solid rock, but it can deform and flow slowly over long periods of time.
The mantle consists of two main layers: the upper mantle and the lower mantle. The upper mantle is composed of solid rock that can flow slowly over time. The lower mantle is composed of solid rock under high pressure and temperature conditions.