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a layer of hot rock.

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The structure consists of an outer silicate solid crust, a highly viscous asthenosphere and solid mantle, a liquid outer core whose flow generates the Earth's magnetic field, and a solid inner core.

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. We believe that it's mainly metals, and in. .

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The mantle is solid, but the high heat causes the mantle to move slowly beneath the Earth's crust. . .

. inch around the seeds is a slightly harder covering, so the core of the apple has two parts.

The pressure at the exit of an air compressor is 150 psia.

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. The Earth's core is made of iron and nickle, which should be liquefied due to the intense heat but is solid because the pressure of the Earth pushing down on it makes it.

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It seems like a contradiction that the hottest part of the Earth is solid, as the minerals making up the core should be liquified or vaporized at this temperature.
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The solid inner core is about 1,220 km thick, and the outer core is about 2,300 km thick.

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The temperature of the inner core is far above the melting point of iron. Mantle. The magnetic field formed by the Earth’s core is. The mantle is the thickest section of the Earth at approximately 2,900 km. Our planet may have had a recent change of heart. Earth’s inner core is composed primarily of iron and nickel, and it is surrounded by a liquid outer core that allows it to spin independently of the Earth’s rotation.

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It is so hot that the metals inside are all liquid.

Inner core super-rotation is the eastward rotation of the inner core of Earth relative to its mantle, for a net rotation rate that is usually [clarification needed] faster than Earth as a whole.

It seems like a contradiction that the hottest part of the Earth is solid, as the minerals making up the core should be liquified or vaporized at this temperature.

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2 Size and shape.