Final answer:
Weathering is most intense in hot and wet climates because higher temperatures and moisture accelerate both chemical and physical weathering processes, contributing to rapid soil formation and the development of nutrient-rich soil horizons.
Step-by-step explanation:
The effects of weathering would be greatest in environments that are both hot and wet. This is because higher temperatures accelerate chemical reactions, including those involved in chemical weathering, while moisture provides the necessary medium for these reactions and also promotes physical weathering through freeze-thaw cycles in less extreme temperatures. Furthermore, moisture fosters the growth of organisms which can contribute to biological weathering. Hot and wet climates support the most vigorous weathering processes, leading to rapid soil formation, with a higher likelihood of developing thick, nutrient-rich soil horizons due to the intense breakdown of parent material.
In contrast, extremely cold and dry or hot and dry environments slow down weathering processes. Low temperatures reduce the rate of chemical reactions while dry conditions limit the amount of water available to facilitate both chemical and physical weathering processes. Something of a middle ground is struck in areas of medium temperature and moisture, where weathering occurs at a more moderate pace.