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Layers of Soil

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O Horizon

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The topmost layer of soil, primarily composed of organic materials including decomposed leaves, twigs, and other plant materials, humus.

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C Horizon

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Consists of slightly broken-up bedrock, lacks the properties of O, A, and B horizons since it is influenced less by the soil-forming processes; contains rock fragments, very little organic material.

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A Horizon

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Known as the topsoil; rich in humus and minerals, typically darker than lower layers, and has a high concentration of organic matter and microorganisms.

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E Horizon

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Characterized by the leaching of organic acids, clay, iron, or aluminum oxides, which leaves a concentration of sand and silt particles of quartz or other resistant materials - known as eluviation.

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B Horizon

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Commonly known as the subsoil; rich in minerals that leached (moved down) from the A or E Horizons and were redeposited within this layer, known as illuviation.

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