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Erosion and deposition

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AB
Explain diff. b/t erosion and depositionerosion is when weathered rock & soil particles move from one place to another. deposition is when sediments are laid in new locations
give 2 ex. of each erosion and depositionerosion - landslide, mudflow deposition - sand dunes, earthflow
Explain how the five agents of erosion change the Earth's surfaceGravity - pulls down rocks and slopes Wind - loose material gets picked up and moved Running Water - carries sediments which can cause abrasian Glaciers - abrasian and plucking the rock beneath it Waves - shapes the shoreline
how does gravity help erosion on a mountain slope covered with rocks and soilit pulls the rocks and soil down
at the bottom of a slope, huges sediment deposits orrur. they're known aslandslides
what is deflationwhen wind removes loose materials such as clay, silt, and sand from the land
how does a sand dune form?when particles of sand is deposited and the mounds of sand keep moving
why are windbreaks importantdecreases wind erosion and aid in wind deposition protects plants
how does water erode sedimentsediments collide with rocks chipping away pieces of the rocks
what mode of erosion causes the most change in the Earth's surface?running water
how does surface runoff form a streamnetwork of surface runoff form gullies --> rills --> streams
describe development of river systemrunoff --> rills--> gullies --> streams --> rivers
alluvial fanwhen a river leaves the mountains and slows down as it runs out onto a plain
meanderloop in a river
oxbow lakeformed when a meander is cut off from the rest of the river
deltawhen large amts of sediments are deposited at the mouth of a large river that flows into a lake
leveewhen particles are deposited along the sides of a river the larger particles accumulate to form levees
flood plainafter heavy rain, a river over flows and covers a flood plain
compare valley glacier to a continental glaciervalley glaciers are long, narrow glaciers that move downhill b/t steep sides of a mtn valley. continental glaciers are thicker sheets of ice.
tillrocks and debris deposited directly by a glacier
moraineridge of till left behind be a retreating glacier
drumlinoveal shaped mound of glaciel till
meltwaterwater from melting ice or snow
kettle lakeround, deep lake formed by a huge block of ice left by a glacier
outwash plainflat fan shaped area in from of terminal moraines formed by sediments deposited by rivers of glaciel meltwater
glaciel terminusthe place where a glacier ends

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