Solution:The typical arrangement of soil horizons in a well-developed soil profile, starting from the top, is as follows:
O Horizon: This is the topmost layer comprised mainly of organic matter such as decomposing leaves, plants, and other materials. It's dark in color due to the organic content.
A Horizon: Known as the topsoil, this horizon is rich in minerals and organic matter. It's generally dark in color and is where most plant roots grow.
E Horizon: This is the eluviation or leaching layer where minerals and organic matter are leached to lower layers. It's often lighter in color.
B Horizon: Known as the subsoil, this horizon accumulates minerals and organic matter from above layers. It can be richer in clay and may have different colors based on its composition.
C Horizon: This is the parent material, which can be partially disintegrated rock or unweathered rock. The soil properties here are less influenced by the soil-forming processes.
This sequence reflects the natural processes of soil development, with organic matter accumulation at the top and mineral accumulation and leaching occurring as you move deeper.