Abstract: | Pedological Examination of “Covering Layers” (Deckschichten) in Northern Togo “Covering layers” (Deckschichten) in northern Togo occur regularly and are widespread. Their composition varies according to the morphological situation. Only covering layers of the same morphological position are comparable. The uppermost covering layer is a product of subrecent geomorphodynamic activity. The origin of the material is still unknown. The contribution of termites to the genesis of covering layers in N-Togo is insignificant. The covering layer is the parent material of recent soil forming processes. The soils are generally stratified with polycyclic genesis. The composition, the thickness and the number of covering layers are causing the agronomic potential of these soils. |