Weathering breaks down rocks into smaller pieces through physical or chemical processes. Physical weathering mechanically breaks rocks apart through frost wedging, friction, or animal burrowing. Chemical weathering uses chemical reactions to break rocks down, aided by water, oxygen, carbon dioxide, living organisms, and acid rain. Carbon dioxide dissolves in water to form carbonic acid, which chemically weathers limestone. Biological weathering also contributes through plant roots penetrating rocks and animal burrowing.