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Soil Formation
| Term | Definition |
|---|---|
| Soil | A loose mixture of rock fragments, organic material, water, and air that can support the growth of vegetation. |
| Parent Rock | The rock formation that is the source of mineral fragments in the soil. |
| Bedrock | The layer of rock beneath the soil. |
| Residual Soil | The soil that remains above its parent rock. |
| Transported Soil | Soil that is blown, washed away, or moved by glaciers. |
| Soil Composition | The mixture of rock particles, minerals, decayed organic material, water, and air. |
| Humus | A dark-colored substance that forms as plant and animal remains decay. (Litter) |
| Decomposition | The process in which humus forms. |
| Fertile Soil | Fertile soil is rich in the nutrients that plants need to grow. |
| Soil Texture | The soil quality that is based on the proportions of soil particles. |
| Loam | Soil that is made up of about equal parts of clay, sand, and silt. |
| Infiltration | The ability of water to move through soil. |
| Soil Structure | The arrangement of soil particles. |
| Soil Horizons | Layers that soil develops over time. |
| Horizon A (topsoil) | A crumbly, dark brown soil that is a mixture of humus, clay, and other minerals. |
| Litter | Leaves and other organic material that fall to the ground. |
| Horizon B (Subsoil) | Usually consists of clay and other particles washed down from the Horizon A, but little humus. |
| Horizon C (bedrock) | |
| Soil Mixers | Earthworms and burrowing animals, such as mice, moles, prairie dogs, and gophers break up hard compacted soil and mix humus through it. |