The breakdown of rocks through mechanical or chemical processes is called weathering.
When exposed rocks, minerals, soil, wood, and man-made structures are subjected to weathering factors such temperature changes, frost actions, plant, animal, and human activity, these materials break down and deteriorate.
It is described as the chemical and mechanical degradation of rocks caused by weather and climate change. Rocks disintegrate due to mechanical weathering, also known as physical weathering and disaggregation. Rocks and soil undergo chemical weathering, which modifies their molecular composition. Quartz and clay minerals are some of the most typical results of chemical weathering. In all sedimentary rocks on Earth, clays make up around 40% of the chemical composition. Carbonic acid is created when plants and some fungi decompose. This process, known as biological weathering, can weaken and dissolve rock.
Wind, water, ice, plants, gravity, and temperature fluctuations can all contribute to weathering.
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