What describes laterites?

Laterites are characterized primarily by their reddish-orange color, which results from the oxidation of iron compounds in the soil. This distinctive coloration is a key indicator of laterites. These soils typically form in hot, wet tropical climates where the significant rainfall leads to intense weathering of rocks and minerals. The high temperatures and moisture levels contribute to the leaching process, removing nutrients and resulting in a soil structure that is rich in iron and aluminum oxides. This environmental context helps to establish the defining characteristics of laterites, making them unique compared to soils found in other regions or climates.