carbon dioxide and oxygen
yes
Chemical weathering
Weathering of rocks can involve both chemical and physical changes. Physical weathering involves the breakdown of rocks without changing their chemical composition, while chemical weathering involves the alteration of a rock's chemical composition through reactions with water, air, or other substances.
Chemical weathering is primarily started by the presence of water and acidic substances, such as carbon dioxide in the atmosphere, which can react with minerals in rocks to break them down. Other factors, like temperature changes, biological activity, and the presence of certain minerals, can also influence the rate of chemical weathering.
Chemical weathering is the type of weathering that involves a chemical change in some of the minerals in a rock. This process breaks down the rock into smaller pieces by altering its mineral composition through chemical reactions with substances like water, oxygen, or acids.
Decomposition is a type of chemical weathering, where rocks and minerals break down into smaller particles through chemical reactions with substances like water, oxygen, and acids.
Chemical weathering is the process that breaks down rocks by altering their chemical composition through reactions with substances like water, oxygen, and acids. This process can result in the transformation of minerals within the rock, leading to its decomposition and eventual disintegration.
Both chemical and physical weathering processes break down rocks into smaller pieces. While physical weathering involves the physical breakdown of rocks without changing their chemical composition, chemical weathering involves the transformation of rocks through chemical reactions with substances like water or acids.
Chemical weathering is the main producer of sediment. In chemical weathering, the compounds in rock decompose into substances that are more stable in the surface nvironment.
acid rain probably
Warm, wet, tropical climates speed chemical weathering of rock.
false;by kaleb owens