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  • Earth's Mantle: The Slowly Flowing Layer Beneath Our Feet
    The part of the Earth that flows slowly like putty is the mantle.

    Here's why:

    * Solid, but with a twist: The mantle is primarily composed of solid rock, but it's under immense pressure and heat. This causes the rock to behave in a way similar to a very viscous fluid.

    * Convection currents: The intense heat within the Earth causes convection currents in the mantle. Hotter, less dense material rises, while cooler, denser material sinks, creating a slow, circular flow.

    * Plate tectonics: These convection currents are what drive plate tectonics, the movement of the Earth's tectonic plates. The slow flow of the mantle allows the plates to shift and collide, causing earthquakes, volcanic eruptions, and the formation of mountains.

    Think of it like a lava lamp. The wax inside, while solid, moves slowly in response to heat. The mantle behaves in a similar way, though on a much larger scale and over much longer timescales.

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