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Weathering• The process that breaks down rocks and
other materials of Earth’s crust into smaller pieces.
4. Friction and impactRiver rocks are rounded and smoothed due to the repeated tumbling along the river bed as they roll downstream
5. Temperature Changes
Rocks expand (get bigger) when they are hot, and contract (get smaller) when they are cold.
2. Oxygen• Iron combines with
oxygen in the presence of water in a processes called oxidation
• The product of oxidation is rust
3. Carbon Dioxide
• CO2 dissolves in rain water and creates carbonic acid
• Carbonic acid easily weathers limestone and marble
5. Acid Rain• Chemicals from burning coal, oil and gas
react chemically with water forming acids.
• Acid rain causes very rapid chemical weathering
Formation of Devil’s Tower, Wyoming
http://www.youtube.com/watch?v=Hsh3_ZMKq-A
Karst Topography• A type of
landscape in rainy regions where there is limestone near the surface
• Created by chemical weathering of limestone
1. Water Erosion
• Rivers, streams, and runoff
http://www.youtube.com/watch?v=ReCt2AcydCg&feature=related
2. Ice Erosion
• Glaciers
http://www.youtube.com/watch?v=XOGbOOaPHsw&feature=related
3. Wind Erosion
http://www.youtube.com/watch?v=mecKnkc9qMk
4. Gravity
• Landslides, mudslides, slump and creep
http://www.youtube.com/watch?v=ZVjr4mii3cE&feature=player_embedded#!
Summary
• Weathering breaks down rocks– It can be physical (ice, plants, animals,
friction, temperature change) or chemical (water, oxidation, acid rain, carbon dioxide, living organisms)
• Erosion moves the rocks
• Together they produce soil
http://www.youtube.com/watch?v=HjVSiuj7Lxk
Soil
• Soil is made from rocks, minerals (mostly sand and clay), and organic materials
• Soil forms layers of different characteristics called horizons
What is soil?
• Soil is a material that forms the crust of the earth.
• It comes from the weathering of rocks and decomposition of organisms.
• It is formed very slowly.
O horizon(green)
• O = Organic
• The top, organic layer made up mostly of leaf litter and humus.
• Humus is decomposed organic matter.
A horizon(dark brown)
• A = Topsoil.
• Dark colored
• Where seeds germinate and roots grow. This is generally the most productive layer of soil.
B horizon(light brown)
• B = Subsoil
• Lighter colored
• Contains clay and mineral deposits (iron, aluminum, etc)
C horizon(tan)
• C = Parent Material
• Layer of large unbroken rocks
Weak humus-mineral mixture
Mosaicof closelypackedpebbles,boulders
Dry, brown toreddish-brown, with variable accumulationsof clay, calciumcarbonate, andsoluble salts
Desert Soil(hot, dry climate)
Grassland Soil(semiarid climate)
Alkaline,dark,and richin humus
Clay,calciumcompounds
Acidiclight-coloredhumus
Iron andaluminumcompoundsmixed withclay
Forest litterleaf mold
Humus-mineralmixture
Light, grayish-brown, silt loam
Dark brownfirm clay
Acid litterand humus
Humus andiron andaluminumcompounds
Light-coloredand acidic
Tropical Rain Forest Soil(humid, tropical climate)
Deciduous Forest Soil(humid, mild climate)
Coniferous Forest Soil(humid, cold climate)
Soil lab online
• Tomorrow you will meet in the computer lab (123) and compare rainfall amounts to topsoil depths.
• You will learn how rainfall affects topsoil depth.