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This text explores the layers that make up topsoil, specifically horizon O and A, which are rich in organic material known as humus. It discusses horizon C, which consists of partly weathered rock from unweathered parent rock, and horizon R, the unweathered base layer. The process of leaching is described as a means of material movement from horizon A to B. Additionally, it highlights the importance of horizon A for plant growth due to its nutrient-rich composition. Understanding these layers is essential for soil health and agriculture.
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The process of leaching moves material from horizon A to horizon B.
Both horizon A and horizon B have decayed organic material called humus.
The partly weathered rock in horizon C comes from unweathered parent rock.
Horizon O is composed of leaf litter and other organic matieral.
Horizon A is rich in organic material and horizon C has very little organic mateial.
Plants grow well in horizon A because it is rich in organic material and nutrients.