
2.8.5 Mineralogical Composition of Laterite
The mineralogical and composition of laterite are dependent on their parent rocks. Laterites consist mainly of quartz and oxides of titanium, zircon, iron, tin, aluminum, and magnesium which remain during the course of weathering (Tardy, 2000). Quartz is the most abundant rock mineral from the parent rock. Laterites very significantly accordingly to their location, climate and depth. The main host materials for nickel and cobalt can be either iron oxides or clay mineral or manganese oxides, iron oxides are derived from mafic igneous rock and other iron – rich rocks, bauxite are derived from granitic igneous rock and other iron –poor rock (Yamaguchi, 2010). Nickel laterites occur in zone of the earth which experienced prolonged tropical weathering of ultramafic rocks containing the ferro-magnetic mineral olivine, pyroxene and amphibole (Dalvi et al, 2004).