Soil is closely related to bedrock as it is formed from the weathering and breakdown of the underlying bedrock. Bedrock refers to the solid rock layer that lies beneath the soil. Over time, physical, chemical, and biological weathering processes act on the bedrock, breaking it down into smaller mineral particles. These particles are then mixed with organic matter, such as decaying plant and animal material, to form soil. Therefore, soil can be considered as the result of the gradual transformation of bedrock and represents the uppermost layer in which plants grow and many terrestrial organisms reside.
Soil is directly related to bedrock as it is formed from the weathering and decomposition of bedrock over time. Bedrock refers to the solid, unweathered rock layer that underlies the soil. Through physical, chemical, and biological processes, bedrock is gradually broken down into smaller particles, which then mix with organic matter and minerals to form soil. In other words, soil is the result of the ongoing breakdown and transformation of bedrock.
