3.3.2 Selected trace elements
Soils of Anak Krakatau had high contents of Ti, Pb, and Ag, while soils
of Sebesi had high contents of Mn, Cl, Ti, Cr compared to the other
studied soils (Table 3). As described in previous sections, soils of
Anak Krakatau were distinct from those of Rakata and Sebesi. This
finding shows that a clear distinction can be made between the origins
of the tephra deposits from the 1883 Krakatau and those from the Anak
Krakatau.