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  • Geosphere: Definition, Layers, and Composition - Earth Science
    The geosphere refers to the solid, rocky, non-living parts of the Earth. This includes:

    * The Earth's crust: The outermost layer, composed of rocks and minerals.

    * The Earth's mantle: A thick layer beneath the crust, mostly composed of solid rock but containing a partially molten layer called the asthenosphere.

    * The Earth's core: The innermost layer, composed mostly of iron and nickel, divided into a liquid outer core and a solid inner core.

    Essentially, the geosphere is everything you can physically stand on or dig into.

    It's important to note that the geosphere is not a static entity. It's constantly changing due to processes like:

    * Plate tectonics: The movement of the Earth's tectonic plates, which causes earthquakes, volcanoes, and mountain formation.

    * Erosion: The wearing down of rocks and soil by wind, water, and ice.

    * Weathering: The breaking down of rocks and minerals by physical and chemical processes.

    The geosphere is closely interconnected with the other Earth systems (atmosphere, hydrosphere, and biosphere) and plays a vital role in shaping the planet's surface and influencing life.

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