Answer: A
Correct answer: Hot and humid
Chemical weathering proceeds fastest in hot, humid conditions, because it depends on water and on chemical reactions, and reaction rates roughly double for every 10°C rise in temperature. Abundant rainfall supplies the water and carries the products away, exposing fresh surfaces. That is why tropical regions develop very deep weathering profiles - tens of metres in places - and soils such as laterite, in which prolonged leaching has removed the silica and left iron and aluminium oxides behind. Its main processes are hydrolysis, in which feldspar is converted to clay; oxidation, which rusts iron-bearing minerals; carbonation, in which slightly acidic rainwater dissolves limestone and produces caves and karst; and solution. Physical weathering has the opposite preference, dominating in cold and arid climates through frost shattering and the expansion and contraction of rock under large temperature swings. The two reinforce each other, since breaking rock apart exposes more surface for chemical attack.