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PHS ES 5
Weathering, Soil and Mass Movement
| Question | Answer |
|---|---|
| weathering | The chemical and physical processes that break down rock at Earth's surface. |
| erosion | The process by which water, ice, wind or gravity moves weathered rock and soil. |
| mechanical weathering | The type of weathering in which rock is physically broken into smaller pieces. |
| abrasion | The grinding away of rock by other rock particles carried in water, ice, or wind. |
| Frost wedging | Process that splits rock when water seeps into cracks, then freezes and expands. |
| chemical weathering | The process that breaks down rock through chemical changes. |
| permeable | Characteristic of a material that is full of tiny, connected air spaces that water can seep through. |
| soil | The loose, weathered material on Earth's surface in which plants can grow. |
| bedrock | The solid layer of rock beneath the soil. |
| humus | Dark-colored organic material in soil. |
| loam | Rich, fertile soil that is made up of about equal parts of clay, sand, and silt. |
| soil horizon | a layer of soil that differs in color and texture from the layers above or below it. |
| topsoil | Mixture of humus, clay, and other minerals that forms the crumbly, topmost layer of soil. |
| subsoil | The layer of soil beneath the topsoil that contains mostly clay and other minerals. |
| litter | The loose layer of dead plant leaves and stems on the surface of the soil. |
| decomposers | Soil organism that breaks down the remains of organisms and digests them. |
| soil profile | a vertical section through a soil showing its succession of horizons and the underlying parent material. |
| pedalfer | soil of humid regions characterized by the accumulation of iron oxides and alumnium rich clays in the B horizon. |
| soil conservation | The management of soil to prevent its destruction. |
| contour plowing | Plowing fields along the curves of a slope to prevent soil loss. |
| conservation plowing | Soil conservation method in which the dead stalks from the previous year's crop are left in the ground to hold the soil in place. |
| pedocal | soil associated with drier regions and characterized by an accumulation of calcium carbonate in the upper horizons. |
| sediment | Earth materials deposited by erosion. |
| deposition | Process in which sediment is laid down in new locations. |
| mass movement | Any one of several processes by which gravity moves sediment downhill. |
| laterite | a red, highly leached soil type found in the tropics that is rich in oxides of iron and aluminum. |
| exfoliation | Type of weathering caused by reducing pressure on a rock surface, allowing slabs of outer rock to break off in layers. |
| talus | an accumulation of rock debris at the base of a cliff. |
| regolith | the layer of rock and mineral fragments that nearly everywhere covers Earth's surface. |
| Rock fall | occurs when rocks or rock fragments fall freely through the air; common on steep slopes. |
| Rockslide | occurs when a mass of rock slides rapidly downslope along planes of weakness. |
| slump | movement of a mass of rock and soil, move down together as one, occurs on a curved surface. |
| mudflow | rapid downhill movement of a mixture of water, rock and sand ¬タモ consistency of wet concrete - often occur after heavy rains but like landslides can be triggered by earthquakes. |
| earthflow | most destructive, rapid form of erosion ¬タモ may not only move rock and sediments but trees, plants, roads, whatever is in the way. |
| creep | very slow downhill movement of rock and soil (regolith). Only noticeable by looking at objects such as trees, telephone poles ¬タモ all at a tilt. |
| Slides | Rockslides occur when a block of bedrock suddenly slides down a flat, inclined surface |