- Soil is formed by the weathering of rocks and decomposition of dead plants and animals over long periods of time. - Soil has different layers with varying compositions - the topsoil at the surface contains more organic matter like humus while the subsoil and bedrock below contain fewer nutrients. - Soils also differ in texture depending on the size of their particles - sandy soil has large particles and drains quickly, silt soil has medium sized particles, and clay soil has the smallest particles and holds the most water.