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  • Creep: Understanding Slow Soil and Rock Movement
    The very slow downhill movement of rock and soil is called creep.

    Here's a breakdown:

    * Creep: This is a type of mass wasting, where gravity slowly pulls soil, rock, and other debris downslope. It's a very slow process, often only moving a few centimeters or inches per year.

    * Causes: Creep is caused by:

    * Freezing and thawing: Water expands when it freezes, pushing soil particles apart. When it thaws, the soil particles settle, causing them to move downhill slightly.

    * Wetting and drying: Similar to freezing and thawing, the expansion and contraction of soil due to wetting and drying can also cause slow downslope movement.

    * Animal activity: Burrowing animals and even plant roots can disrupt the soil structure and contribute to creep.

    Signs of creep:

    * Tilted fence posts or trees

    * Curved or bent retaining walls

    * Terraced slopes

    While creep is slow, it can have significant long-term impacts on the landscape, causing landslides and other forms of mass wasting over time.

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