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  • Rock Weathering: Two Key Processes Shaping Earth's Surface
    Here are two ways rocks on the surface change:

    1. Weathering: This is the breakdown of rocks, soil, and minerals through direct contact with the Earth's atmosphere, water, and biological organisms.

    * Physical weathering: Mechanical breakdown of rocks into smaller pieces, such as from:

    * Frost wedging: Water freezing in cracks and expanding, breaking the rock.

    * Abrasion: Rocks rubbing against each other, such as in a river.

    * Root wedging: Plant roots growing into cracks and splitting the rock.

    * Chemical weathering: Breakdown of rocks through chemical reactions, such as:

    * Dissolution: Acids in rainwater dissolving minerals in rocks.

    * Oxidation: Minerals reacting with oxygen, like the rusting of iron.

    * Hydrolysis: Water reacting with minerals to form new substances.

    2. Erosion: This is the process of moving weathered rock and sediment from one place to another.

    * Wind erosion: Wind picks up and carries away loose sediments.

    * Water erosion: Rivers, streams, and waves carry away eroded material.

    * Glacial erosion: Massive ice sheets carve out valleys and transport rocks.

    * Gravity erosion: Landslides and mudflows move material downhill.

    These processes work together to change the landscape over time, shaping mountains, creating valleys, and shaping the Earth's surface as we know it.

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