OBJECTIVE FORESTRY

Detailed explanation-1: -The horizons are: O (humus or organic): Mostly organic matter such as decomposing leaves. The O horizon is thin in some soils, thick in others, and not present at all in others. A (topsoil): Mostly minerals from parent material with organic matter incorporated.

Detailed explanation-2: -The C horizon is a mineral horizon, excluding strongly cemented and hard bedrock, and the horizon is little affected by pedogenic processes and, by definition, lacks the properties of O, A, E, or B horizons (Soil Survey Staff, 2014).

Detailed explanation-3: -The B horizon lies underneath the A horizon and is commonly called the subsoil. It is the horizon of maximum accumulation, or illuviation, of clay, iron, aluminum, or other compounds leached from the A horizon. In some soils the B horizon forms through alteration of material in place rather than by illuviation.

Detailed explanation-4: -The A horizon, called topsoil by most growers, is the surface mineral layer where organic matter accumulates.