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Ch.6. Geomorphic Processes
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Exogenic forces Endogenic Forces Geomorphic processes
Originate on the earth surface- Weathering, Mass movement, erosion and deposition Endogenic Forces Originate below the surface- Orogenic, Epirogenic, Volcanism and earthquakes
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Diastrophic forces Slow Movements Sudden forces
These include two type of movements: Orogenic or mountain building force. Epirogenic or continent building forces Slow Movements Volcanism Earthquakes Sudden forces
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Exogenic forces Weathering Mass wasting Erosion
It includes breaking of rocks on its place. It does not involves any movement of eth weathered material. Mass wasting It include movement of earth material down the slope. It is caused by gravity Erosion It involves breaking, transporting and deposition of weathered material It s done by various agents like river, glacier, wind etc
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Mechanical weathering
Chemical Weathering Mechanical weathering Biological Weathering
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Chemical weathering Carbonation-Carbonation is the mixing of water with carbon dioxide to make carbonic acid. Carbonation takes place when the rock minerals react with weak carbonic acid formed when water combines with carbon dioxide in the atmosphere. Carbonic acid acts on the rock by breaking down and dissolving its mineral contents. The dissolved materials are washed away by ground water, and the soluble ions are stored in the groundwater supply. Rocks such as limestone and feldspar experience this type of chemical weathering more. This type of weathering is important in the formation of caves. Solution- Removal of soluble minerals from the rock 3. Hydration-Hydration is the chemical reactions caused by water. Water reacts with the rock and alters the size and chemical compositions of the minerals. 4. Oxidation or Reduction- Reaction of atmospheric oxygen with minerals of the rock, eg, rusting of iron
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Physical or Mechanical weathering
Unloading : It results in exfoliation or onion weathering.
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Freezing and Thawing and frost wedging
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Expansion and Contraction
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Salt Weathering
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Biological Weathering
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Mass movements
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Land Slide
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Earth Flow
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Creep- Very slow movement
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Slump
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Rock Slide
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Soil Profile
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