parent rock
The term that describes the area of bedrock from which soil forms is known as the "parent material". This bedrock is broken down over time through weathering and other processes to create the soil above it.
It can't
Bedrock is not a layer of mature residual soil. Bedrock is the solid rock underneath the soil layers that make up the Earth's crust. Residual soil forms from the weathering of bedrock over time.
Regolith
Soil typically forms first from bedrock through a process called weathering, where the bedrock is broken down by physical, chemical, or biological processes. Over time, weathering breaks down the bedrock into smaller particles that mix with organic material to form soil.
Residual soil forms from the weathering of the underlying bedrock in the same location. An example is clay soil derived from the weathering of granite bedrock.
The C horizon is the layer of a soil profile that forms first from the bedrock. It is the underlying layer that contains weathered rock fragments and shows the least amount of soil development.
The layer of solid rock under the soil is called bedrock. Bedrock is the hard, solid rock beneath the Earth's surface that forms the foundation for soil and other materials above it.
Bedrock is the solid rock underlying soil and other unconsolidated material on the Earth's surface. Soil, on the other hand, is a mixture of minerals, organic matter, gases, liquids, and organisms that support plant life. Bedrock is the solid foundation upon which soil forms and develops.
The layers of soil in an area are the topsoil, subsoil, weathered rock and bedrock.
Residual soil develops directly from the underlying bedrock through weathering processes. The characteristics of the bedrock, such as mineral composition and structure, influence the properties of the residual soil that forms above it. Over time, physical and chemical weathering break down the bedrock to produce a soil that retains some similarities to the parent material.
Soil forms from bedrock through a process called weathering, where the physical and chemical properties of the rock are broken down into smaller particles by factors like water, wind, and temperature changes. Over time, these particles accumulate and mix with organic matter to create soil. The type of bedrock, climate, and biological activity in the area all influence the specific composition and characteristics of the soil formed.