Monday, 4 March 2013

Weathering and Erosion

Weathering is the process whereby rocks exposed to the atmosphere atomic number 18 broken drop into soil.
Erosion is the process by which the land is sculpted or worn out-of-door by agents of erosion (wind, rivers etc) and material is transported and deposited away from its source.
What is the difference between weathering and erosion?
When a rock or particle is loose it is weathering and once that particle starts moving from its sure place it is erosion.
The main types of Weathering
1. mechanical / Physical weathering is the disintegration/ crack-up of rocks into smaller fragments.
2. Chemical weathering is the decomposition/ decay of minerals in rocks or organic materials.
3. Biological / Biotic weathering- is the crumbling of rocks through the work of plants and animals.
Mechanical / Physical Weathering
Mechanical weathering break-dances up rocks but does not lurch its mineral composition. The rock particles are not softened, and do not change their colour.
Rock particles created by physical weathering can be further altered and broken downhearted by chemic weathering.
Physical weathering takes place mostly in regions where there is right smart daily range of temperature.
Some rocks that are jointed break up into blocks and this is known as block disintegration.

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Some rocks dismantle off into layers, like onions this process is called exfoliation.
Abrasion -physical wearing down of rocks as they rub or bounce against each other--most greens in windy areas, under glaciers, or in well out channels.
Process of Mechanical weathering:
Frost action - Weathering occurs in places with temperatures alter above and below 0ºC. During the day water from rain, dew or melting snow seeps into cracks in rocks. At night the temperatures wane and the water in the rocks is turned into ice. When the ice freezes it expands creating pressure and the cracks are forced wider, spitting rocks apart. The rocks then form heaps of run off these are called screes.

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