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Forces that Change the Earth’s Surface
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Earth’s Systems Lithosphere(troposphere) – rocks and land
Atmosphere - gases Hydrosphere – water on the ground and in the atmosphere
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External Forces Weathering – The breakdown of rocks into smaller pieces. Physical Weathering – changes size and shape Ex. Frost Action Chemical Weathering – changes chemical composition Ex.Acid Rain and rusting Erosion – Transporting material from its original location Ex. Water, Wind, Gravity, Glaciers
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Landforms Mountains – Formed by folding and faulting.
Also by volcanic lava cooling. Plains – broad flat regions at low elevations Plateaus – layers of rock at higher elevations Built similar to mountains.
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Earthquakes Earthquakes are the sudden sliding movement along a fault.
The vibrations travel in waves Primary (p-waves), secondary (s-waves), and longitudinal (l-waves) P – waves travel all through the earth S – waves cannot travel through liquids like the outer core. L –waves travel on the surface
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Structure of the Earth Crust – outer layer made of rock, 5-50km thick.
Mantle – 2900 km thick, dense iron and magnesium rock Outer Core – 2300 km thick made of liquid iron and nickel Inner Core – 1200 km thick, made of solid iron and nickel
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Plate Tectonics and Continental Drift
The Earth’s crust is broken up into 12 large plates and many smaller ones. These plates slowly move and interact……mountains, earthquakes etc. A theory was proposed that they are separating. At one time they were all together as one big continent called Pangea. Evidence – ancient mountain ranges line up Continents fit like puzzles. Fossils
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Pangea Plates
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Sea Floor Spreading New rock is made at the center of the ocean
Old rock is destroyed near the continents Ex. Mid Atlantic Ridge
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