Rocks may decompose or dissolve and, at the same time, changes in composition through a certain chemical process to form residual materials. This change is called chemical weathering. Three ordinary chemical processes are involved in chemical weathering: dissolution or dissolving from water or rain, oxidation or rusting from oxygen, and hydrolysis when certain minerals and water form another product like clay.
On the other hand, mechanical weathering transpires when rocks disintegrate or break down into smaller pieces through physical forces, including exfoliation, abrasion, and freeze and thaw weathering. Exfoliation occurs when rock sheds off sheets that form by putting pressure on the rock through natural causes such as tectonic activities.
Abrasion occurs when rock surfaces weather and removes layers of it through friction, and the rock breaks down, which causes it to decrease in size. In freeze and thaw weathering, water thaws, and it allows for more space water to sink inside the aperture, and then it freezes again until the time that rock breaks along such fracture, causing the rock to diminish into smaller fragments.