How does erosion differ from weathering?
Erosion removes and moves rock, soil, or sediment; weathering breaks down or alters rock in place.
Study 2 Erosion and Sediment Transport with 12 free online flashcards. Review key terms, definitions, and concepts with this interactive flashcard deck.
How does erosion differ from weathering?
Erosion removes and moves rock, soil, or sediment; weathering breaks down or alters rock in place.
What can happen when a transporting force weakens?
When the force transporting sediment weakens, sediment may be deposited, building or reshaping landforms.
What is traction in sediment transport?
Traction moves particles by rolling or sliding them along the ground or a channel bed.
What is mass wasting?
Mass wasting is the downhill movement of loosened material under gravity; examples include rockfalls, landslides, slumps, and debris flows.
How can runoff erode a slope?
Runoff can remove soil in a thin layer; as it gathers into channels, it cuts small channels and gullies.
How do erosion and deposition shape a river bend?
Faster flow on the outside of a river bend tends to erode a cut bank, while slower flow on the inside deposits sediment to form a point bar.
How does a river form an alluvial fan?
An alluvial fan may form when a river leaves steep terrain, spreads onto flatter ground, slows, and deposits sediment.
How does wind move different sediment sizes?
Wind commonly carries dust and silt in suspension, moves sand by saltation, and pushes larger grains along the surface by creep.
What are two ways glaciers erode bedrock?
Glaciers erode by abrasion, as rock fragments frozen in ice scrape and grind bedrock, and by plucking, which loosens pieces of bedrock.
How do till and outwash differ?
Till is an unsorted deposit left by melting ice; meltwater can sort and carry sediment onward, forming deposits such as outwash plains.
What is longshore drift?
Longshore drift is the movement of beach sediment roughly parallel to the coastline by waves and currents.
What is saltation?
Saltation moves sand-sized particles in short hops; bouncing grains may knock other grains into motion.
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