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External Forces Shaping the Earth
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Weathering Weathering refers to physical and chemical processes that change the characteristics of rock on or near the earth’s surface.
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Weathering processes create smaller and smaller pieces of rock called sediment.
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Mechanical Weathering
Processes that break rock into smaller pieces are referred to as mechanical weathering. Agents that can break apart rocks include: running water, plant roots, ice (glaciers), and temperature.
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Chemical Weathering Occurs when rock is changed into a new substance as a result of interaction between elements in the air or water and the minerals in the rock.
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Erosion Occurs when weathered material is moved by the action of wind, water, ice, or gravity. For erosion to occur, a transporting agent, such as water or wind must be present. When a river enters the ocean, the sediment is deposited in a fan like landform called a delta.
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Wind Erosion Wind can also transport and eposit sediment in other locations. Loess is windblown silt and clay sediment that produces very fertile soil.
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Glacial Erosion A glacier is a large, long lasting mass of ice that moves because of gravity. Glaciation is the changing of landforms by slowly moving glaciers. Rocks left behind by a glacier may form a ridge called a moraine.
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Building Soil Organic material in the soil is called humus.
Soil has parent material or the chemical composition of the rock it is made of. The relief is a factor in soil production as steeper slopes erode more quickly The organisms in the area provide material for soil. Warmer climates produce different soil. The amount of time is also a factor in soil production.
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