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  • Mountain Formation and Height Changes: A Geological Overview
    Mountains don't actually "get taller" in the sense of growing like a plant. Here's how they form and change height:

    Formation:

    * Plate Tectonics: Mountains are primarily formed when tectonic plates collide. The immense pressure of the collision forces rock upwards, creating folds and thrust faults.

    * Volcanoes: Volcanic mountains are created when magma rises from the Earth's mantle and erupts onto the surface, building up layers of lava and ash.

    Height Changes:

    * Erosion: Over long periods of time, wind, rain, ice, and other weather forces erode mountains, gradually wearing them down. This is the primary factor in reducing mountain height.

    * Uplift: Sometimes, even after forming, mountains can experience further uplift from ongoing tectonic activity. This can lead to a gradual increase in height.

    * Faulting: Faults in the Earth's crust can cause sudden shifts in elevation, potentially leading to a mountain becoming taller or shorter.

    Key Points:

    * Slow process: Mountain formation and change in height happen over millions of years.

    * Erosion is the main force that reduces height.

    * Tectonic activity is the main force that increases height.

    So, while mountains don't "grow" like living things, they are constantly being shaped and reshaped by a combination of geological forces.

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