The layered structure of mature soil
Soil is not a uniform material; it develops distinct layers called horizons over thousands of years. The O horizon is organic matter (leaf litter, decomposing plants). The A horizon (topsoil) is dark and rich with organic material and minerals leached from above. The E horizon is pale and leached of minerals. The B horizon (subsoil) is where minerals accumulate. The C horizon is weathered parent rock, and R is solid bedrock.
Climate and soil development
Soils develop faster in warm, wet climates where decomposition is rapid. Tropical soils are deeply weathered and leached, often nutrient-poor despite their appearance. Cold soils develop slowly and retain nutrients better. Arid soils skip many horizons entirely, lacking the water flow needed for leaching. Reading soil profiles tells the story of past and present climate, vegetation, and drainage.