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Index >> Microbes and Lithosphere>> Expansion of Rocks

Expansion of Rocks

Expansion of Rocks

During the day, heat is conducted very slowly from the outer to the inner layer of the rock. Hence outer layer is at a higher temperature (expands more than the inner layer during the day) than the inner layers. The same experiences greater temperature drop during the night (i.e. surface layers are cooler than inner layers at night). This process of warming and cooling continues till the outer layer gets separated from the inner layer (exfoliation). During winter, water freezes in the cracks to form ice leading to tremendous pressure exertion on the rock (due to expansion of ice). Cracks widen due to this pressure.

When ice melts (warm season) and again freezes (cold season), it leads to widening of cracks and ultimately causes the rocks to gradually break down to smaller and smaller pieces. Rocks can also be disintegrated by the abrasive action of glaciers--water running down the rocks carry away small pieces of rocks with them causing cutting of these rocks (water loaded with rocks have tremendous cutting power). Wind action also takes part in mechanical weathering by scraping rocks and carrying away fine particles.

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