Hloušekite

hlousekite

vesevloskyite

pradetite

lavendulan

Images

Formula: (Ni,Co)Cu4(AsO4)2(AsO3OH)2.9H2O
Arsenate, lindackerite group, nickel- and cobalt- bearing mineral
Crystal System: Triclinic
Specific gravity: 3.295 calculated
Hardness: 2 to 3
Streak: Greyish white
Colour: Pale green
Luminescence: Does not fluoresce under short wave or long wave UV
Environments

Hydrothermal environments

Hloušekite is a secondary mineral derived from highly oxidised, hydrothermal quartz veins containing disseminated tennantite, chalcopyrite, and nickel - cobalt arsenides. Associated minerals include veselovskýite, pradetite, lavendulan, arsenolite, babánekite and gypsum (HOM).

Localities

At the type locality, the Geister vein, Rovnost Mine, Jáchymov, Karlovy Vary District, Karlovy Vary Region, Czech Republic, hloušekite was found on the surface of strongly altered ore fragments containing dominant tennantite and chalcopyrite. Associated minerals include veselovskýite, pradetite, lavendulan, arsenolite, babánekite and gypsum. Hloušekite forms thin, lath-like transparent, pale green crystals, locally elongated reaching up to 3 mm across (MM 78.1341-1353).

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