Step 1: Understanding the Concept:
The soil profile is organized into master genetic horizons (O, A, E, B, C, R) formed through pedogenic soil development processes.
Step 2: Detailed Explanation:
In standard soil taxonomy and pedology:
- The A Horizon (topsoil surface mineral horizon) forms at the surface or below an O horizon.
- It is characterized by the humification and accumulation of decomposed organic matter intimately mixed with the mineral soil fraction.
- It is the primary zone of biological activity, root proliferation, and nutrient cycling.
Step 3: Final Answer:
Therefore, the A horizon is Rich in organic matter and intimately mixed with mineral matter, corresponding to option (A).