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  • Physical Weathering of Rocks and Minerals: Processes & Examples
    Physical weathering breaks down rocks and minerals without changing their chemical composition. It's like taking a big rock and smashing it into smaller pieces. Here's what happens:

    1. Frost Wedging:

    - Water seeps into cracks in rocks.

    - When the water freezes, it expands, putting pressure on the rock.

    - Repeated freezing and thawing cycles widen the cracks, eventually breaking the rock apart.

    2. Abrasion:

    - Rocks and minerals are rubbed against each other by wind, water, or ice.

    - This grinding action wears them down, creating smaller particles.

    - Think of sandblasting, but with nature doing the work!

    3. Exfoliation:

    - Rocks that have formed deep underground are exposed to the surface.

    - The pressure from the overlying rock is released, causing the rock to expand and peel away in layers, like an onion.

    4. Thermal Expansion and Contraction:

    - Rocks are exposed to extreme temperature changes, like hot days and cold nights.

    - The different minerals in the rock expand and contract at different rates.

    - This stress can cause cracks to form and eventually break the rock.

    5. Root Wedging:

    - Tree roots grow into cracks in rocks.

    - As the roots grow larger, they put pressure on the rock, eventually breaking it apart.

    6. Salt Wedging:

    - Saltwater evaporates, leaving salt crystals behind in rock cracks.

    - The crystals grow larger and put pressure on the rock, widening the cracks.

    Important Note: Physical weathering doesn't change the chemical makeup of the rocks and minerals, only their size and shape.

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