Abstract:Raman spectroscopy has been used to characterise four natural halotrichites: halotrichite FeSO 4 .Al 2 (SO 4 ) 3 4 . Raman bands at around 474, 460 and 423 cm -1 are attributed to the ν 2 (A g ) SO 4 mode. The band at 618 cm -1 is assigned to the ν 4 (B g ) SO 4 mode. The splitting of the ν 2 , ν 3 and ν 4 modes is attributed to the reduction of symmetry of the SO 4 and it is proposed that the sulphate coordinates to water in the hydrated aluminium in bidentate chelation.Key words: apjohnite, pickingerite, halotrichite, wupatkiite, jarosite, sulphate, Raman spectroscopy Introduction Sulphate efflorescences have been known for some considerable time 1-3 . These often occur in tailings impoundments (see Jambour et al. p322) 4 . The sulphate formation results from the oxidation of pyrite. Halotrichites are formed close to pyrite and are often found with copiapites and related minerals 5 . The minerals are found in efflorescences of geothermal fields 6 . Halotrichite has a formula• Author for correspondence (r.frost@qut.edu.au)