Laterization represents the most rapid cycling of nutrients of all soil-forming processes.

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Laterization is a soil-forming process that occurs in tropical regions characterized by intense rainfall and high temperatures. It involves the rapid leaching of nutrients and the accumulation of iron and aluminum oxides. As a result, lateritic soils are typically low in fertility, but they can be very productive when managed properly. Because of the intense weathering and nutrient cycling that occurs during laterization, it is considered one of the most rapid soil-forming processes.

Laterization Represents the Most Rapid Cycling of Nutrients of All