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  • Earth's Interior: Layers, Composition & Structure
    The Earth's interior is divided into several layers, each with its own unique properties.

    * The crust is the outermost layer of the Earth, and it is where we live. It is made up of solid rock, and it is about 35 kilometers thick on average.

    * The mantle is the layer of the Earth that lies beneath the crust. It is made up of hot, semi-solid rock, and it is about 2,900 kilometers thick.

    * The outer core is the layer of the Earth that lies beneath the mantle. It is made up of liquid iron and nickel, and it is about 2,200 kilometers thick.

    * The inner core is the innermost layer of the Earth. It is made up of solid iron and nickel, and it is about 1,220 kilometers thick.

    The temperature of the Earth's interior increases as you go deeper. The temperature at the center of the Earth is about 5,700 degrees Celsius, which is hotter than the surface of the sun.

    The pressure of the Earth's interior also increases as you go deeper. The pressure at the center of the Earth is about 3.6 million times greater than the pressure at sea level.

    The Earth's interior is constantly in motion. The mantle is convecting, which means that hot rock rises from the bottom of the mantle and cools at the top. This convection causes the Earth's tectonic plates to move, which can lead to earthquakes and volcanic eruptions.

    The Earth's interior is a complex and dynamic place, and scientists are still learning new things about it all the time.

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