WEATHERING AND MASS WASTING LECTURE NOTES
VOCABULARY: erosion; agents; base level; weathering; physical or mechanical; frost wedging; exfoliation; plant wedging; chemical; carbonation; oxidation; hydration; hydrolosis; solution; mass wasting; talus; talus cones; block falls; avalanches; rock glaciers; landslides; mudflows; slump; creep; solifluction
erosion--the wearing away of the earth's surface by natural processes
agents--gravity, wind, running water, ground water, glaciers, waves; acts to lower land to base level
weathering--the breakdown of existing surface and near surface material
2 classes of weathering
- Mechanical or Physical--disintegration--smaller pieces
• frost wedging--water freezes and expands in crack
• salt wedging--water evaporates and crystals grow
• exfoliation--rocks peel like an onion, especially intrusive igneous bodies; Stone Mountain,
Georgia (accelerated by chemical weathering)
• plant wedging--plant roots grow
• differential heating; (fire)
• granular disintegration
• animals
- Chemical--decomposition
• carbonation--CO2 + H2 yields H2CO3 (carbonic acid)
• oxidation
• hydration--water joins to cause expansion or swelling
• hydrolosis--water joins and weakens the rocks
•solution (leaching)
•plants and animals
factors affect rate
- nature of rock--material quartz, calcite, cement
- size of particles
- climate--greatest, warm humid
- topography--altitude, slope
erosion--involves an agent
One agent of erosion is gravity.
Agent = Gravity
Process = MASS WASTING
Mass Wasting--downslope movement of solid, solid and liquid material under the influence of gravity
3 variables:
- size of particles
- amount of moisture
- speed
Mass Movements
talus
solifluction--slow downslope movement of saturated soil at high latitudes
Go to the Weathering and Mass Wasting Review Questions.
Go to the Glossary of Landform Terms.
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