soil formation: When parent material, such as lava or volcanic ash, rock or sediment left behind by glaciers, wind-blown dunes, sediments left behind by rivers, lakes, or the ocean, or any type of bedrock, is exposed to the impacts of the atmosphere, hydrosphere, and biosphere and eventually turns into soil.
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Soil Layers: Different soil layers begin to form once weathering, erosion, and decomposition have created a large number of tiny particles. Each soil layer is referred to as a horizon.
O horizon:Composed of a litter layer with leaves, branches, mosses, and animal waste.
B horizon:Minerals and organic matter leached (a process in which materials suspended or dissolved in liquid are transported through the subsurface)
A horizon :Contains inorganic mineral components with organic matter and humus; often called topsoil (part of the soil that has most nutrients and is most important for ecosystems and agriculture)
C horizon:If present, this layer consists of broken-up rock material and contains rock particles that are larger and less weathered than the layers above.
R horizon:Unaltered rock material, parent material or bedrock is found in this layer
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