The parent material of a soil is the

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The parent material of a soil is the underlying geologic material (i.e., bedrock) from which the soil is formed. This material can influence the characteristics of the soil, such as its texture, pH, and mineral content. Organic matter from vegetation and erosion can also contribute to soil formation, but they are not considered the parent material. The transportation of soil from one area to another is not a factor in the parent material of a soil.

The Parent Material of a Soil Is the