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Earth Science, Chapter 6: Erosion and Deposition

AB
WeatheringThe mechanical and chemical processes that break rock into smaller pieces over time
Mechanical weatheringPhysical processes – such as abrasion, growing plant roots, expanding ice, or burrowing animals – that naturally break rocks into smaller pieces
Chemical weatheringThe processes – such as dissolving by water, reaction with acids, or reaction with oxygen – that change the composition of rocks and minerals and cause them to wear away
ErosionThe movement of weathered material from one location to another by gravity, water, wind, and glaciers
DepositionThe laying down or settling of eroded material
MeanderA broad, C-shaped curve in a stream
Longshore currentA current that flows parallel to the shoreline
DeltaA large deposit of sediment that forms where a stream enters a large body of water
AbrasionThe grinding away of rock or other surfaces as particles carried by wind, water, or ice scrape against them
DuneA pile of windblown sand
Mass wastingThe downhill movement of a large mass of rocks or soil due to gravity
LandslideThe rapid, downhill movement of soil, loose rocks, and boulders
TalusA pile of angular rocks and sediment from a rockfall
GlacierA large mass of ice, formed by snow accumulation on land, that moves slowly across Earth’s surface
MoraineA mound or ridge of unsorted sediment deposited by a glacier



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