5+ , was found at the KriĆŸnica deposit near Pernek (Male Karpaty Mountains, Slovak Republic); it is the third occurrence of this mineral phase worldwide. Crystals and crusts of brand holzite occur as surface coatings on altered shales mineralized with stibnite and pyrite. Associated minerals include romeiteÂlike phases, sulphur, aragonite, gypsum, senarmontite and SbÂrich FeÂhydroxides. Brandholzite forms euhedral tabular crystals of hexagonal habit, typically 0.5 to 0.8 mm across, exceptionally up to 2 mm long. The crystals occur as isolated, or randomly grouped individuals, creating inconspicuous crusts up to several cm 2 . Brandholzite crystals are colourless, transparent or showing white clouding. No fluorescence was observed under either short or longÂwave UV radiation. The average electron microprobe analysis gave 6.11 MgO, 0.52 CaO, 0.16 FeO, 55.89 Sb 2 O 5 and (37.32) H 2 O if recast to 100 wt. %. The calculated formula is (Mg 0.88 Ca 0.05 Fe 0.01 ) ÎŁ0.94 (H 2 O) 6.00 [Sb(OH) 6 ] 2.00 . The XRD pattern was indexed in a trigonal setting (space group P3), with refined unitÂcell parameters a = 16.1076(9), c = 9.8628(9) A and V = 2216.1(2) A 3 . The thermogravimetric curve shows total weight loss of 34.6 wt. % (over the interval of 20â800 °C), caused by H 2 O release. The initial rapid weight decrease (20â140 °C) was followed by a minor continuous weight loss up to 800 °C. Brandholzite from Pernek and its mineral association were probably formed by subÂrecent weathering processes in an abandoned mines environment.