Weathering consists of physical and chemical processes that work together to break down rocks into smaller fragments and alter their mineral composition, creating essential products like sedimentary clasts. Chemical weathering is more prominent in warm, humid conditions.
Weathering involves two main processes: physical weathering (mechanical breakdown of rock into smaller fragments) and chemical weathering (chemical change of minerals within rock). These processes work together, with chemical weathering weakening rocks for physical weathering, creating important products like sedimentary clasts and soil. Chemical weathering dominates in warm, humid environments, accelerated by higher temperatures.
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