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Weathering Weathering  Process that breaks down and changes rock at or near earth’s surface   Mechanical – rock is broken into smaller pieces by physical means Chemical – rock undergoes changes due to a chemical change in composition Mechanical Weathering  Two factors that are important to mechanical weathering are temperature and pressure. Frost wedging Exfoliation  bedrock is under pressure within the earth; as it is exposed to the surface the pressure is reduced and the rock expands and long curved cracks form; layers of rock are stripped away  Root action Abrasion Chemical Weathering  Chemical reactions take place that alter the rocks composition     Water: can dissolve many kinds of minerals and rock Oxygen: can combine in chemical reactions with other substances – oxidation. Example: rust Carbon dioxide combines with water in the atmosphere to create carbonic acid which dissolves rocks Acid precipitation Factors affecting the rate of weathering     Climate Rock type and composition Surface area topography Erosion  The transport of weathered material form one place to another Forces that aid erosion   The force of gravity tends to pull materials downslope. http://www.youtube.com/watch?v=XC9AqJlaCj4&feature=related Running water Running water has greater erosional power than wind and can move more material greater distances.  As the slope of the land decreases, the water slows and larger particles are deposited.  http://www.youtube.com/watch?v=MFpCJsc_k64 Glacial erosion  Due to their high density glaciers carry huge rocks and piles of debris and scratch and grind over surfaces. Erosion by abrasion  http://www.youtube.com/watch?v=D5uDaEpJHjE  Wind erosion   Wind picks up and moves fine particles Prevalent in areas of low precipitation and high temperatures Wind erosion  http://www.youtube.com/watch?v=PQmo n7Rj6ns&feature=related Mass Movements   The downslope movement of loose sediment and weathered rock due to gravity Influenced by     weight of material materials resistance to sliding/flowing a trigger water Types of mass movement    Creep – slow, steady downhill movement Flows – materials flow as if thick liquid Slides – rapid, downslope movement of a thin layer of material that separates from underlying bedrock  Slumps –  Avalanches –  Rock falls – mass of material rotates and slides along a curved surface landslides that occur in mountainous areas with thick accumulations of snow rocks break loose and fall downward      Good Catch That's a Big Rock Washington Mudslide Glad I Wasn't Standing There Even More Thankful I Wasn't Driving
 
									 
									 
									 
									 
									 
									 
									 
									 
									 
									 
									 
									 
									 
									 
									 
									 
									 
									 
									 
									 
									 
                                             
                                             
                                             
                                             
                                             
                                             
                                             
                                             
                                             
                                             
                                            