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Published byAbner Sanders Modified over 6 years ago
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Types of Weathering © Copyright M. J. Krech. All rights reserved.
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Mechanical Weathering
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Disintegration – breaks down into smaller pieces, no new substance
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Frost Action or Ice Wedging
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Frost Action Ice expands when frozen and cracks rocks
Causes pot holes in winter Happens where the temperature goes both above and below the freezing point of water Called Ice Wedging
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Abrasion
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Wind blows sand which wears away cliffs
Wind Abrasion Wind blows sand which wears away cliffs
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Water Abrasion Water carries rocks along in streams & rivers which collide and become smoothed into rounded river rocks
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Gravity
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Landslides Gravity pulls rocks loose
They break apart as they fall downhill
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Organic Activity: Root Pry
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Root Pry Roots expand as they grow and crack rocks.
Other organic activity Ants, woodchucks, and worms dig holes that let in water that causes weathering.
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Wetting and Drying
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Rocks that contain CLAY swell and shrink as they absorb water then dry out, thus cracking the rocks
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Joint Sheeting
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As top soil erodes, rock layers below expand and crack into layers
Called EXFOLIATION when large sheets of rock break away at the surface
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Chemical Weathering
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Decomposition – breakdown into new substances
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Hydrolysis
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The chemical action of water with other substances
Example: Feldspar turns into clay
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Feldspar +Water = Clay Feldspar A Clay Cliff
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Plant Acids
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Acids given off by lichens and mosses eat at rocks
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Sulfuric Acid
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ACID RAIN: Sulfuric acid causes blurred words on gravestones and monuments
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Photo taken 100 years ago Photo taken recently
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Both of these are Civil War headstones.
Why has one weathered more? 1865 1862
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Oxidation
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RUST caused by oxygen combining with iron-bearing minerals in rocks causes red bands on limestone cliffs
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Carbonation
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Carbon dioxide combines with water to form carbonic acid which eats away layers of limestone rock
Forms CAVES; KARST TOPOGRAPHY
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Karst Topography A type of landscape in rainy regions where there is limestone near the surface, characterized by caves, sinkholes, and disappearing streams. Created by chemical weathering of limestone
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Features of Karst: Sinkholes
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Features of Karst: Caves
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Features of Karst: Disappearing Streams
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The end. © Copyright M. J. Krech. All rights reserved.
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