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Weathering And Erosion Weathering And Erosion
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Weathering The breaking down of the Earth’s crust into smaller pieces
Weathering The breaking down of the Earth’s crust into smaller pieces. It is caused by physical, chemical, or biological means.
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The Different Types of Weathering
Physical Weathering The Different Types of Weathering Process by which rocks are broken down into smaller pieces by external conditions. Types of Physical Weathering Frost heaving and frost wedging Plant roots Friction and impact Burrowing of animals Temperature changes
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Frost Wedging
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Frost Heaving
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Frost Action or ice wedging slowly breaks up this sedimentary rock into unusual shapes.
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Root Pry The tree is growing in the rock and soon the rock will break apart because of the tree roots.
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Plant Roots
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Friction and Repeated Impact
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Burrowing of Animals
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Temperature Temperature can produce mechanical weathering. During the day, the sun’s energy heats a rock’s surface. During the night, the rock’s surface cools. The repeated change from hot to cold may cause the rock to peel or flake layers that are parallel to the rock’s surface. This peeling or flaking is known as exfoliation.
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Temperature Changes
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This is a picture of the Half Dome
This is a picture of the Half Dome. The rock is peeling away from the mountain in layers just like an onion. This is exfoliation.
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These rocks have been blasted by wind and sand causing them to become rounded.
WIND ABRASION
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Chemical Weathering The process that breaks down rock through chemical changes. The agents of chemical weathering Water Oxygen Carbon dioxide Living organisms Acid rain
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Water Water weathers rock by dissolving it
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Oxygen Iron combines with oxygen in the presence of water in a processes called oxidation The product of oxidation is rust
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This rock is red because of the oxidation of iron in the sediment when the rock was being formed.
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Carbon Dioxide CO2 dissolves in rain water and creates carbonic acid
Carbonic acid easily weathers limestone and marble
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Living Organisms Lichens that grow on rocks produce weak acids that chemically weather rock
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Acid Rain Compounds from burning coal, oil and gas react chemically with water forming acids. Acid rain causes very rapid chemical weathering
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Acid rain has eaten away this limestone statue.
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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: Caves
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Features of Karst: Disappearing Streams
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Features of Karst: Sinkholes
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Erosion The process by which water, ice, wind or gravity moves fragments of rock and soil. Erosion loosens & transports sediment formed by weathering.
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There are many kinds of Erosion.
Here are a few: Wave Action Running Water Landslides Avalanche Glaciers Slump Creep Rock Fall Mud Flow
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Erosion Moving water & wind cause changes to
existing land forms & create new landforms such as valleys, plateaus, flood plains, canyons, caves or dunes
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Colorado River as it winds its way through the Grand Canyon.
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Grand Falls, near Leup, Arizona
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Water Erosion Rivers, streams, and runoff
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Wave action is when waves hit the rocks and pieces of rock break off.
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In this picture the running water eroded the sides of this canyon and created the V-shaped valleys.
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Ice Erosion Glaciers
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This is a picture of a glacier which carves out a U-shaped valley where it flows dragging rocks and boulders along the way.
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Wind Erosion
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Mass Movements Landslides, mudslides, slump and creep
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This is a picture of a landslide. A type of mass wasting.
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This is a picture of an avalanche
This is a picture of an avalanche. It is similar to a landslide with ice and snow instead of rock.
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Mudslide
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This is a diagram of creep
This is a diagram of creep. The hillside slowly slips over many years from temperature or water.
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Creep
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In this picture the land has slumped
into the road below.
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