Merrill Earth Science
Chapter 6: Erosion and Deposition
6-1 Gravity
Erosion- is the process that moves weathered sediments from one location to another.
4 major types or agents:
1. Gravity
2. Running water
3. Glaciers
4. Wind
Deposition- the dropping or depositing their load of sediments when their motion decreases.
Gravity: causes materials to move downslope at a variety of speeds.
Slump: is a type of mass movement that takes place on steep slopes. It occurs because the material under the slumped material weakens.
Creep: as the ground freezes, small sediments are pushed up by the expanding water in the soil. Then, when the soil thaws, the sediments fall downslope, often less than a millimeter at a time.
Rockslides: Page 145
Mudflows: occur in dry areas after a heavy rainstorm(s). Steep slopes.
6-2 Running Water:
Water erodes more sediments than any other agent of erosion.
Rill Erosion- begins when a small stream forms during a heavy rain.
Rills may evolve into gullies- thus creating gully erosion.
Sheet erosion- happens when this rainwater flows into lower elevations, carrying sediments with it.
Types of Deposits:
Alluvial Fan: shaped like a triangle, occurs when a stream slows down rapidly due to the leveling of the slope.
Deltas: an area of deposit where streams or rivers flow into lakes or oceans.
6-4 Glaciers
Glaciers: a slowly moving mass of snow-moves downhill. Movement is what separates glaciers from snowfields.
Continental Glaciers: very large cover the earth’s polar regions.
Valley or Mountain Glaciers: smaller, found in mountain regions where the climate is temperate or colder with a high annual snowfall.
Glacial Erosion:
Most powerful type of erosion.
Plucking- movement of rocks fragments by the ice itself. See
page 157
Glacial Deposition: Page 159
Moraines:
Till:
Outwash Plain:
6-5 Wind
Wind erodes in 2 ways: by deflation and by abrasion.
Deflation: wind picking up small particles.
Abrasion: a type of sandblasting. The moving air with rock particles acts like sandpaper.
Wind Deposition:
Loess:
Dunes: