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Published byNicholas Harris Modified over 9 years ago
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2 Weathering, Erosion, Deposition, and Landscapes Weathering – the breakdown of rocks into smaller pieces, called sediments. Erosion – the process where the sediments are transported by wind, gravity, glaciers, and running water. Deposition – the process whereby these sediments are dropped by their transporting agents. Weathering breaks down the rocks, erosion moves the particles, and deposition drops the sediments in another location.
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Erosion: Gravity is the main force causing erosion Deposition: Can be moved by wind or flowing water Weathering Χ Can be physical or chemical Χ Has to happen before erosion. The rocks have to be broken into smaller pieces before they can erode away.
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1. Release of Pressure 2. Freezing & Thawing 3. Animal Actions 4. Plant Growth
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Root/Plant Wedging/Action Ice/Frost Wedging/Action Rusting Action WEATHERING
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Release of Pressure Χ As the surface of a rock is eroded, the rock begins to release pressure. Χ Causes top layers of the rock to crack and flake off.
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Freezing & Thawing When water in the cracks of rocks freezes it expands causing the crack to enlarge or get bigger. The ice melts & refreezes over & over, breaking the rock apart.
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Animals dig (burrow) through the ground to make their homes. This loosens the soil & breaks apart rocks.
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Plants roots can grow into cracks in the rock, slowly breaking them apart.
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Moving water causes much of the erosion that shapes the Earth’s surface Sediments that have been transported through running water appear rounded and smooth and are deposited in sorted piles. Water can deposit materials in other places to create new landforms. Sediments are deposited in sorted piles.
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Can loosen sediments and carry them away Can cause flooding Damages soil, roads, and buildings
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Cause erosion along coastlines Sand in the waves acts like sandpaper Weathers away rock Grasses and plants can help hold soil in place
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Gravity pulls glaciers down along a valley Grind rocks beneath them into sediments Over a long time, creates a U shaped valley
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Gravity causes rivers to flow Carry sediments Rock, sand, and soil Deposited materials found at the bottom of cliffs or steep slopes Can form deltas Appear angular and unsorted.
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Caused by wind blowing dust, soil, or sand from one place to another Sediments appear pitted (random holes) and frosted (glazed look) and are deposited in sorted piles Only very small particles can be transported by wind. Changes sand dunes and fields Sediments are deposited in sorted piles.
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Large, loose deposits of sand Size and shape depend on speed and direction that winds are blowing More common in drier landscapes Easier for particles to move through the air Less plant life to hold down soil
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Bare, plowed fields can become dry Winds blow topsoil off fields Farmers plant trees along edges of fields to stop wind Less they plow, less erosion
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