is the living skin of Earth which is a result of the dynamic interaction among the atmosphere, biosphere, geosphere, and hydrosphere.
pedosphere
This is the ideal soil for agricultural use
Loam
The sequence of soil horizons from the surface down to the underlying bedrock
soil profile.
This horizon is composed of loose or partly decayed organic matter
Organic Horizon (O Horizon)
This horizon is composed of mineral matter mixed with some dark organic humus.
Surface Horizon (A Horizon)
This horizon is the accumulated clay and other nutrients from the layer above it.
Subsoil (B Horizon)
This horizon is composed of partially altered parent material.
Substratum (C Horizon)
This horizon is characterized by a significant loss of minerals (eluviation) and leaching.
Eluviation (E Horizon)
This horizon is not soil, while the layer of loose, heterogenous, and superficial material covering the bedrock is collectively called regolith
Bedrock (R Horizon)
the smallest particle of soil texture
clay (<0.002mm)
the second smallest particle of soil texture
slit (0.002-0.005mm)
the third smallest particle of soil texture
sand (0.005-2.00mm)
particles larger than coarse grained sand are called
gravel and rock >75.00mm