Here's why:
* Parent material is the fundamental source of the mineral and organic components of soil. It can be:
* Bedrock: Solid rock that has been weathered and broken down over time.
* Unconsolidated materials: Sediments like glacial till, alluvial deposits, or wind-blown sand.
* Weathering: The process of breaking down parent material into smaller particles, both physically and chemically. This is a crucial step in soil formation.
So, the bedrock is the parent material for the soil that forms above it.