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  • Understanding Soil Layers: A Comprehensive Guide to Soil Horizons
    The layers of soil, also known as soil horizons, are:

    O Horizon (Organic Layer):

    * The uppermost layer, composed of decomposed plant and animal matter (humus).

    * Rich in nutrients and organic matter.

    * Usually dark in color.

    A Horizon (Topsoil):

    * A mix of mineral particles (sand, silt, clay) and organic matter.

    * Supports plant growth and is most fertile.

    * Often darker in color than the layers below.

    E Horizon (Eluviated Layer):

    * Found in some soils, especially those in humid climates.

    * Lighter in color than the A horizon due to the leaching of minerals and organic matter.

    * Contains mostly sand and silt.

    B Horizon (Subsoil):

    * Rich in minerals, but less organic matter than the topsoil.

    * Often denser and more compact than the layers above.

    * Can have a variety of colors depending on the minerals present.

    C Horizon (Parent Material):

    * Consists of partially weathered rock fragments that form the basis of the soil.

    * Less weathered than the layers above.

    * May contain large rock fragments.

    R Horizon (Bedrock):

    * The solid, unweathered rock that lies beneath the soil.

    * Not technically considered part of the soil profile.

    Note: Not all soils have all these layers. The presence and development of specific layers depend on factors like climate, vegetation, and parent material.

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