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Types of physical weathering
Freeze Thaw
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Incidents of Mass Wasting
Feb 17, 2006 - Southern Leyte
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Caused by rainwater reacting with the mineral grains in rocks to form new minerals (clays) and soluble salts.
Chemical Weathering
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is the process by which soil and rock particles are worn away and moved elsewhere by gravity, or by a moving transport agent – wind, water or ice.
Erosion
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Occurs when rocks are weakened by different biological agents like plants and animals. When plant roots grow through rocks, it creates fracture and cracks that result eventually to rock breakage.
Biological Weathering
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Types of Chemical Weathering
Carbonation
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examples of physical weathering
swiftly moving water
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the process in which the sediments is dropping in a new place.
Deposition
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the breakdown of rock by acidic water to produce clay and soluble salts. takes place when acid rain reacts with rock-forming minerals such as feldspar to produce clay and salts that are removed in solution.
Hydrolysis
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occurs in flat bare areas or dry, sandy and loose soils. It detaches soil particles and transports them by the wind.
Wind erosion
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the most common erosion agent. Millions of tons of sediments are picked up and transported everyday along rivers, coasts, and in deep oceans around the world.
Water Erosion
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Breakdown of rocks by oxygen and water often giving iron- rich rocks a rusty-colored weathered surface.
Biological Weathering by Chemical Compounds
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Caused by the effects of changing temperatures on rocks, causing rocks to break apart
physical weathering
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Types of Weathering
Physical Weathering
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Classification of Biological Weathering
biological weathering by physical means
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Factors of Mass Wasting
Increased Water
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the breakdown of rock by oxygen and water, often giving iron- rich rocks a rusty-colored weathered surface.
Oxidation
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The moving of glaciers, Change in shape of land, Entire rocks are moved due to an avalanche
Glacial Erosion
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Burrowing of animals like shrews, moles, and earthworms create holes on the ground by excavation and move the rock fragments to the surface
Biological Weathering by Physical Means
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carbon dioxide in the air dissolves in rainwater and becomes weakly acidic. This weak “carbonic acid” can dissolve limestone as it seeps into cracks and cavities.
carbonation
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Examples of Mass Wasting
Rock Fall
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breakdown of rocks at the earth’s surface by the action of water, ice, acids, salts, plants, anomals, gravity, and changing temperatures
Weathering
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a type of chemical weathering where water reacts chemically with the rocks, modifying its chemical structure.
Hydration
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or a mass movement, is the downslope movement of rock, soil, and ice due to gravity. It is also a natural hazard that can cause damage to life and property.
Mass wasting
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Exogenic Processes
Weathering
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It can happen as cracks develop parallel to the land surface as a consequence of the reduction in pressure during uplift and erosion. Heat Temperature
Exfoliation
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responsible for shaping the Earth’s surface and forming the geologic features seen on the earth’s surface
exogenic process
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Type of physical weathering wherein water continually seeps into cracks, freezes and expands, eventually breaking the rock apart
Freeze thaw
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Types of erosion
Wind erosion