Weathering Rate

Weathering Rate refers to the speed at which rocks and minerals break down or change due to environmental processes. Factors like temperature, moisture, and plant activity influence how quickly this happens. For example, warmer, wetter conditions often accelerate weathering, while cold, dry conditions slow it down. Understanding weathering rates helps scientists learn how landscapes evolve over time, how soils develop, and the long-term effects of climate change. Overall, it measures the pace of natural rock and mineral transformation driven by surface environmental conditions.