Volcanic ash soils of varying age occurring on the islands of the sout
hwestern Pacific were studied in terms of ferrallitization development
, which was shown to be specific by the mineralogy of newly formed pro
ducts (allophane-metahalloisite-oxide clay association) and by the geo
chemistry of the process: ferrallitized-ferrallitic products appear at
all the stages: their SiO2/Al2O3 ratio is close to 2.