Crystals of arsenic sulphide (reported as alacranite), coming from the burning dump of KateÏ rina Mine (Czech Republic), have been investigated by single crystal X-ray diffraction and chemical microanalysis.Both analytical data and unit-cell parameters strongly suggest the existence of a continuous series between the high-temperature polymorph ( -As 4 S 4 ) and the mineral alacranite (As 8 S 9 ). As the S content increases in the series, the unit-cell volume increases accordingly. The structural model has been obtained for two crystals, exhibiting different unit-cell volumes (ALA15: a = 9.940(2), b = 9.398(2), c = 9.033(2), =102.12(2), V = 825.0(3), R obs = 6.12 %; ALA2: a = 9.936(2), b = 9.458(2), c = 9.106(2), = 101.90(2), V = 837.3(3), R obs = 6.41 %). We found that the non-stoichiometric compounds crystallize as a disordered mixture of two kinds of cage-like molecules, packed together as in the -As 4 S 4 phase. The first one is identical to the As 4 S 4 molecule found in the structures of both realgar ( -As 4 S 4 ) and -As 4 S 4 . The second molecule is chemically and structurally identical to that found in the As 4 S 5 compound. The simultaneous presence of As 4 S 4 (C2/c) and As 8 S 9 (P2/c) microdomains could be a reason for the observed gradual change of the translation symmetry from the -phase to alacranite s.s..