Laterite soils are found in areas where the temperature is high and the rainfall is heavy. This type of soil is predominantly found in tropical regions with a wet climate. The high temperature and heavy rainfall promote the weathering of rocks, leading to the formation of laterite soils. The intense heat and frequent rainfall accelerate the process of chemical weathering, which breaks down the minerals in rocks and forms new compounds in the soil. This results in the characteristic red or orange color of laterite soils. The heavy rainfall also leaches out certain nutrients from the soil, making it relatively infertile. However, with proper techniques like irrigation and fertilization, laterite soils can be made suitable for agricultural purposes.