click below
click below
Normal Size Small Size show me how
Chapter 4
Mr. Trawinski
| Term | Definition |
|---|---|
| abrasion | physical weathering caused by friction between rock particles |
| agent of erosion | Wind, water or ice (glaciers) |
| bedrock | Solid layer of rock beneath the soil horizons |
| chemical weathering | changes the mineral composition of rock, forming new substances |
| deposition | Settling or release of sediments by agents of erosion |
| discharge | Quantity of water flowing past a certain point in the stream per unit of time |
| erosion | Transportation of weathered material (sediments) by wind water or ice away from thier place of origin |
| flotation | Transportation of particles along the surface of a stream |
| frost action | form of physical weathering in climates with seasonal weather changes above and below zero degrees |
| glacial erratic | Large rock that has been transported by a glacier |
| glacier | large mass of slowly flowing ice |
| graded bedding | Layers of sediment that change from course particles at the bottom of each layer to progressively finer particles toward the top |
| horizontal sorting | Gradual change in the size, density and shape of particles deposited when a stream slows on reaching calm water |
| humus | Organic remains on the top layer of soil - best for growing crops |
| ice age | Period when glacial ice covered large parts of the continents |
| leaching | Process by which groundwater carries dissolved minerals deeper into the soil as water infiltrates the ground |
| mass movement | Downhill movement of rock or sediment without being carried by wind, water or ice (same as mass wasting) |
| meander | Natural looping bend or S shaped curve in a stream |
| mass wasting | Downhill movement of rock or sediment without being carried by wind, water or ice (same as mass movement) |
| outcrop | bedrock exposed at the earth's surface |
| physical weathering | changes the size and/or shape of the rock without changing the chemical composition |
| precipitate | Salt crystals that form and settle out of a solution |
| precipitation | Process that involves substances substances settling out of a saturated solution |
| residual soil | Soil that remains on the top of the bedrock where it is formed |
| sediments | Rocks that have broken into fragments |
| soil | Weathered rock mixed with organic remains at the top of the lithosphere |
| soil horizon | Layers within the soil showing a particular stage of soil development - slow formation |
| solution | Mixture in which particles are so small they can't be filtered out of the water |
| sorted | Separated by particle size or other characteristics |
| stream discharge | Amount of water flowing in a stream |
| stream velocity | Speed at which a stream flows |
| striation | Parallel scratches on the surface of a rock caused by the movement of a glacier |
| suspension | Fluid in which particles that can can be filtered but they are too small to settle on their own |
| till | Unsorted sediments deposited directly by glacial ice |
| transported soil | Soil eroded and deposited AWAY from its parent bedrock |
| unsorted deposit | Sediment left by melting glacial ice (mixture of clay, sand, cobbles and boulders) |
| vertical sorting | Sorting of particles from bottom to top in a layer |
| weathering | breakdown of rock due to chemical or physical changes |
| What is usually required for chemical weathering? | Water |
| Give an example of chemical weathering | Rusting of iron |
| What speeds chemical weathering? | Heat |
| What happens to rock during frost action? | Water seeps into cracks in the rocks, water freezes and cracks in the rock get bigger each time |
| What controls the stream velocity? | The slope (gradient) and the stream discharge (amount of water flowing in a stream |