The oxygen in the air combines with the minerals and the rocks change because the minerals are oxidizing. Oxidation can cause new chemical compounds such as iron oxide to form in the rocks.
Minerals combine to form rocks through processes such as crystallization, cooling of magma, or precipitation from water. Rocks can also undergo weathering and erosion to release minerals back into the environment.
Physical weathering is a type of weathering in which minerals react with dissolved oxygen in water. This causes chemical changes to take place in the minerals.
Weathering takes place the most in regions with high humidity and precipitation, such as tropical rainforests or coastal areas. This is because moisture accelerates chemical weathering processes by promoting the breakdown of rocks and minerals.
Chemical weathering is most likely to occur in areas with high temperatures, abundant moisture, and exposure to oxygen. This is because these environmental conditions accelerate chemical reactions that break down minerals in rocks. Areas with tropical climates or high levels of rainfall are prime locations for chemical weathering to take place.
Chemical weathering often refers to the chemical reactions that take place between acidic rain or ground water and various rock types. It can also refer to the gradual oxidation of minerals by exposure to air and water. The chemical reaction usually results in the gradual dissolution of the rock.
Water
Minerals combine to form rocks through processes such as crystallization, cooling of magma, or precipitation from water. Rocks can also undergo weathering and erosion to release minerals back into the environment.
Physical weathering is a type of weathering in which minerals react with dissolved oxygen in water. This causes chemical changes to take place in the minerals.
Chemical weathering is the phenomenon which contributes to the destroying of rocks with chemical agents; the chemicals may be natural or man made.Examples are water, carbon dioxide, organic acids, acid rains etc.
Weathering takes place the most in regions with high humidity and precipitation, such as tropical rainforests or coastal areas. This is because moisture accelerates chemical weathering processes by promoting the breakdown of rocks and minerals.
Chemical weathering is most likely to occur in areas with high temperatures, abundant moisture, and exposure to oxygen. This is because these environmental conditions accelerate chemical reactions that break down minerals in rocks. Areas with tropical climates or high levels of rainfall are prime locations for chemical weathering to take place.
Water facilitates chemical weathering by dissolving minerals and carrying them away, leading to the breakdown of rocks. It also allows chemical reactions to occur more readily by providing a medium for reactions to take place. Water can also contribute to the formation of new minerals through hydration and hydrolysis reactions.
Chemical weathering often refers to the chemical reactions that take place between acidic rain or ground water and various rock types. It can also refer to the gradual oxidation of minerals by exposure to air and water. The chemical reaction usually results in the gradual dissolution of the rock.
Shale is a clastic sedimentary rock formed of clay and silt sized eroded particles that are a result of both physical and chemical weathering. The clay minerals, however are the result of chemical weathering of feldspars.
Warm and wet climates are best for chemical weathering to occur because moisture and heat accelerate the breakdown of minerals in rocks. The presence of water allows for chemical reactions to happen more easily, while higher temperatures speed up these reactions.
Humidity and temperature are the keys to chemical weathering (and to answer a previous poster, chemical weathering is a natural process, though human activity can affect it. Chemical weathering needs water, to act as a solvent and to transport corrosive ions so chemical weathering in arid climates, and in arctic climates (where water is frozen, and so not available) have little if any chemical weathering. Chemical processes are also (mostly) accelerated by higher temperature so the high humidity and high temperature of the tropics is the place where chemical weathering predominates . Contribution of humic acids from soils is also important, and the high rate of growth of plants in tropical climates is also a factor. While the solution of Limestones by acidified water is the most commonly quoted example, many minerals break down chemically, feldspar breaking down to clay minerals would be another important example.
Chemical weathering is acid rain. If it rains onto carbonate rocks e.g. limestone, they undergo a chemical reaction. This breaks down the rock.Biological weathering is animals and plants. Rabbits burrow under rocks which weakens them. Tree roots grow through rocks and weaken them. Weak rock breaks up easily.Hope this helps x