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  • Understanding Soil Horizons: Identifying the E Horizon
    The second layer in a soil profile is called the E horizon, also known as the zone of eluviation.

    Here's a breakdown of the typical soil profile layers:

    * O horizon: This is the topmost layer, composed of organic matter like leaves, twigs, and decomposing plant and animal material.

    * A horizon: Also known as topsoil, this layer is a mix of mineral soil and organic matter. It's where most plant roots grow.

    * E horizon: This layer is characterized by the loss of minerals and organic matter due to leaching. It's typically lighter in color than the A horizon.

    * B horizon: This is the subsoil, where minerals and organic matter from the A and E horizons accumulate.

    * C horizon: This layer consists of weathered bedrock and is the transition zone between soil and parent rock.

    * R horizon: This is the bedrock layer.

    Note: Not all soil profiles have all of these layers. The presence and development of each layer depend on factors like climate, vegetation, and parent material.

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