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  • Understanding Lee Slopes: Formation and Wind Erosion
    When sediment is blown against an obstacle and settles behind it, it forms a lee slope.

    Here's a breakdown:

    * Lee: Refers to the side of an object that is sheltered from the wind.

    * Slope: Indicates an inclined surface.

    How it happens:

    1. Wind Erosion: Wind picks up loose sediment, carrying it along.

    2. Obstacle Encounter: The wind encounters an obstacle like a rock, hill, or building.

    3. Sediment Deposition: The wind slows down behind the obstacle, causing the sediment to settle.

    4. Lee Slope Formation: The accumulated sediment forms a slope on the leeward (downwind) side of the obstacle.

    Examples:

    * Sand Dunes: Sand dunes are classic examples of lee slopes. The wind blows sand up the windward side of the dune, then deposits it on the leeward side.

    * Rock Formations: Wind can erode rock formations and deposit sediment on the leeward side, creating unique shapes.

    * Artificial Structures: Buildings and fences can also create lee slopes, especially in areas with high wind and loose sediment.

    Key Takeaway:

    Lee slopes are a common feature in areas with strong winds and loose sediment. They demonstrate the powerful role of wind in shaping landscapes.

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