Weathering Rates

Weathering rates refer to how quickly rocks and minerals break down or change due to natural processes like rain, wind, temperature changes, and chemical reactions. These rates vary depending on factors such as the type of rock, climate, presence of water, and biological activity. Faster weathering occurs in warm, moist environments or with softer rocks, while it slows in cold, dry, or harder rock conditions. Understanding weathering rates helps scientists study landscape evolution, soil formation, and the long-term stability of natural and built structures.