This document defines and describes the three main types of weathering: physical, chemical, and biological. Physical weathering breaks rocks into smaller pieces through temperature changes and water, such as exfoliation weathering caused by hot temperatures and freeze-thaw weathering caused by melting and freezing water. Chemical weathering occurs as acid in rainwater reacts with minerals in rocks, either slowly over time from carbonic acid or more rapidly from acid rain. Biological weathering results from plants and animals breaking rocks into fragments.