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Where does the weathered material go? How does it get there?
Ch. 9 – Erosion Where does the weathered material go? How does it get there?
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Changing Earth’s Surface
Review: What is the difference between weathering and erosion? Weathering: breakdown of rocks and other substances on earth’s surface (destructive) Erosion: movement of weathered material to new places Sediment: pieces of weathered rock
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Weathering and Erosion cause CONSTANT, SLOW change on earth’s surface over time, creating a cycle:
DEPOSITION Deposition: when sediment gets laid down or dropped (deposited) in new places, it piles up and creates new land forms (constructive process)
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But, new landforms are also carved out where rock has weathered and the sediment eroded away (destructive). Slowly, over time, the shape of earth’s surface changes – mountains weather, and the sediment gets eroded, which lowers elevation and makes them less steep – but that sediment piles up somewhere else – creates new landforms where the sediment weathered, and new landforms where the sediment gets eroded to.
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So what forces move (erode) the weathered sediment?
Gravity – causes mass movement Moving Water Ice Wind Coastal Waves
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Sierra Nevada Mountains, CA
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Appalachian Mountains, NC
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Mass movement; also called mass wasting is when a large mass of weathered sediment moves at the same time, due to force of gravity, the force that pulls things down toward earth’s center; sediment moves downhill
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Landslides mixed rock and soil (weathered materials) move downhill quickly; RAPID and DESTRUCTIVE
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Mudslides water rapidly accumulates in the ground, such as during heavy rainfall or rapid snow melt, changing the earth into a flowing river of mud as water mixes with loose soil and rocks; moves downhill. Usually occurs in a normally dry area, that all of a sudden gets a huge amount of rain; RAPID and DESTRUCTIVE
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Colluvium, San Bernardino Mountains, California
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Slump a large mass of soil or other material moves downhill in one large chunk; due to underground weathering; FAST and DESTRUCTIVE.
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Creep Slow movement downhill of soil and surface materials results in tree trunks that are curved at the base, tilted utility poles, fence posts, and tombstones; caused mostly by repeated underground freezing and thawing of water; SLOW, and ongoing.
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Soil Creep
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