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greater precipitation in the summer
greater precipitation in summer
increasing temperature and increasing precipitation
Chemical Weathering.
Regional Climate
greater precipitation in the summer
greater precipitation in summer
increasing temperature and increasing precipitation
Chemical Weathering.
Regional Climate
Bcjjg
it is an example of chemical reaction/weathering and erosion!!
large caves in limestone bedrock
yes
well it is very hard to break up bedrock, but the main process that does is weathering. You have two seperit kinds of weathering. The first one is Chemical Weathering. Chemical weathering is when weathering effects the exterior. two examples are rust and leaching. The second type of weathering is Mechanical Weathering. This effects rocks physically. two examples are abrasion and erosion.SO THE MAIN ANSWER WOULD BE WEATHERING. THE TYPE OF WEATHERING, MECHANICAL WEATHERING, THE PROCESS, ABRASION (well there is more than that but that is the most common situation)
Unloading acts as a weathering agent by breaking bedrock into smaller pieces. This increases the surface area along which chemical reactions can occur, which eventually leads to weathering.
A bare mountain peak may be exposed to freeze/ thaw cycles, harsh sunlight, surface erosion by wind blown and water carried particles, and chemical weathering from acid rain. Bedrock under soil is not exposed to most weathering forces.