Soil Horizons
Soil is made comprised of distinct horizontal layers called soil horizons. Horizons in soil range from organic rich surface layers (humus and topsoil horizons) to underlying layers high in rock content (subsoil, regolith, and bedrock). Use the interactive graphic below to learn more about soil horizons.
Click each horizon to view its properties. (expand/collapse all)
Simple Definition
A surface horizon that is a mix of minerals and organic matter (leaf litter and humus). The organic matter is the dominant material in the O horizon.
Advanced Definition
This layer is dominated by a high content of organic matter. O horizon formation is favored by large inputs of vegetative materials and saturated soil conditions. Saturation reduces organic matter decomposition processes; wetlands soils often have thick O horizons due to saturation and high vegetative input. However, O horizons also form in soils that are not saturated (forest floors). (SSSA, 1996)
Simple Definition
A surface horizon that is a mix of mineral and organic matter. Unlike the O horizon, minerals are the dominant material.
Advanced Definition
Mineral horizons which have formed at the surface or below and O horizon. The exhibit obliteration of all or much of the original rock structure and show one or both of the following: (1) an accumulation of humified organic matter intimately mixed with the mineral fraction and not dominated by properties of E or B horizons (defined below), or (2) properties resulting from cultivation, pasture, or similar types of land disturbance. (SSSA, 1996)
Before the prairies were settled, the A-Horizon is estimated to have been 30 inches or more in depth. It is estimated that Missouri has only 10 inches of A-Horizon soil remaining in the prairie regions of the state since the settlement of the prairie. Over the same period, it is estimated that 1 foot of soil has accumulated along the streams.
Simple Definition
A subsurface horizon bleached in color (white or gray) due to loss of mineral coloring agents (iron and aluminum oxides).
Advanced Definition
Mineral horizons exhibiting a loss of silicate clays, iron, or aluminum, or some combination of these losses, resulting in a concentration of sand and silt size particles. These horizons are often bleached in appearance and they exhibit obliteration of all or much of the original rock structure. (SSSA, 1996)
Simple Definition
A subsoil horizon showing evidence of inorganic or organic material accumulation.
Advanced Definition
Horizons formed below the O, A, and E horizons. B horizons are dominated by the obliteration of all or much of the original rock structure and show one or more of the following: (1) illuvial (movement into a horizon usually through percolation of soils drainage water) concentration of silicate clay, iron, aluminum, humus, carbonates, gypsum, or silica alone or in combination; (2) evidence of removal of carbonates; (3) residual concentration of iron and aluminum oxides (sesquioxides); (4) coatings of sesquioxides that make the horizons lower in color value, higher in chroma, and redder in hue than overlying and underlying horizons; (5) alteration which forms silicate clays or liberates oxides or both, and which forms granular, blocky, or prismatic structure; or (6) brittleness. (SSSA, 1996)
Simple Definition
Unconsolidated parent material that has undergone little soil weathering.
Advanced Definition
Horizons, excluding hard bedrock, that are little affected by soil development processes and lack the properties of O, A, E, or B horizons. Most C horizons are mineral layers. The material of C horizons may be either like or unlike the material from which the solum has presumably formed. (SSSA, 1996)
