The number of linkages in silicon tetrahedra varies among silicate types. Tectosilicates have all four oxygen atoms shared (maximum linkages), followed by phyllosilicates (three shared), then inosilicates (two shared), and nesosilicates have isolated tetrahedra (no shared oxygens). Thus, the order is: Tectosilicates > Phyllosilicates > Inosilicates > Nesosilicates.