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Published byValerie Chambers Modified over 9 years ago
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Weathering is the breakdown and alteration of earth-forming materials by low pressure, temperature, water, air, and biological organisms.
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Weathering happens quicker on newly exposed rock because the minerals have not met their equilibrium state with their environment.
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Weathering surface are changed in color, texture, composition, firmness or form, with little or no transportation of the altered material
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Weathering is responsible for soil formation, nutrients used by marine organisms, fossil fuels and sedimentary ore deposits.
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Erosion is the transportation and removal of material produced by weathering.
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Erosion is caused by wind, water, currents, glaciers, humans, and animals.
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This type of weathering involves breaking down rocks into progressively smaller pieces. It increases the surface area exposed to the elements to increase the rate of chemical weathering.
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1. Pressure or Stress Release (Unloading) ◦ The removal of surface material by water, glacial erosion or human activities that could cause the minerals in the rock to spread further apart to create large voids.
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2. Frost Action ◦ The changes in pressure caused by the cycle of freezing and thawing of water in colder climates in joints and crevasses may cause the rocks to fracture.
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3. Salt Weathering ◦ The salt penetrates the rock’s surface and embeds itself in the pores and small cavities in the rock. ◦ The salt change size by either absorbing water or when the temperature changes.
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4. Heating and Cooling (Exfoliation) ◦ Rock is also a poor conductor of heat so the surface may be hot, but the interior might be cold. This difference in temperature may can the rock to break apart.
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Minerals in a rock undergo changes that make them more stable under their current environmental and biological conditions.
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1. Water ◦ Water serves as a medium for any chemical reaction to occur between a rock’s environment and it’s minerals. Flowing water prevents the chemical reaction to reach a state of equilibrium, thus allows it to continue indefinitely.
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2. Chemical Reactions ◦ the reaction between the ions in the water and the minerals. This decomposes igneous rock. Hydrolysis Ion Exchange
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Oxidation Carbonation
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The type of weathering that is the result of biochemical or biophysical processes associated with living matter.
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Worms increase a surface’s exposure to air and water.
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Bacteria break down chemicals and minerals and produce harmful by-products.
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Algae, lichen and fungus colonize rock surfaces reducing their contact with water and air and create ions that react chemically with the surface.
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