Sharp intense Raman bands for the German sample, are observed at 972 and 814 cm鈭? attributed to the 谓1 PO43鈭?/sup> and AsO43鈭?/sup> symmetric stretching modes. Raman bands at 1014, 1057, 1148 and 1160 cm鈭? are attributed to the 谓1 PO2 symmetric stretching mode and 谓3 PO43鈭?/sup> antisymmetric stretching vibrations. Raman bands at 764 and 776 cm鈭? and 758 and 756 cm鈭? are assigned to the 谓3 AsO43鈭?/sup> antisymmetric stretching vibrations. For the Australian mineral, the 谓1 PO43鈭?/sup> band is found at 973 cm鈭?. The intensity of the arsenate bands observed at 814, 838 and 870 cm鈭? is greatly enhanced. Two low intensity Raman bands at 1307 and 1332 cm鈭? are assigned to hydroxyl deformation modes. The intense Raman band at 441 cm鈭? with a shoulder at 462 cm鈭? is assigned to the 谓2 PO43鈭?/sup> bending mode. Raman bands at 318 and 340 cm鈭? are attributed to the (AsO4)3鈭?/sup> 谓2 bending. The broad band centred at 3301 cm鈭? is assigned to water stretching vibrations and the sharper peak at 3473 cm鈭? is assigned to the OH stretching vibrations. The observation of strong water stretching vibrations brings into question the actual formula of arsenogorceixite. It is proposed the formula is better written as BaAl3AsO3(OH)(AsO4,PO4)(OH,F)6路xH2O. The observation of both phosphate and arsenate bands provides a clear example of solid solution formation.