Alumoklyuchevskite

alumoklyuchevskite

fedotovite

piypite

langbeinite

Images

Collecting from the Tolbachik fumeroles is not for the faint-hearted. The fumerole temperature may be 500oC to 800oC, but the ambiant temperature may be as low as 10oC in summer, with rain, or a daunting -30oC in winter, with snow that may last as long as six months. The latitude is just short of 60o N (the Arctic Cicle is just over 66o N), and the highest point is at an altitude of 3682 m (high enough to begin to feel its effect on your breathing). Nevertheless, standing on a rough scree slope in these conditions, scientists have collected no fewer than 270 different mineral species, and for 133 of them this is the type locality.

Formula: K3Cu2+3AlO2(SO4)4
Anhydrous sulphate
Crystal System: Triclinic
Specific gravity: 3.1 measured, 2.95 calculated (HOM)
Hardness: 2 to 2½
Streak: Light green
Colour: Dark Green, turns white on exposure to air, possibly from hydration (HOM)
Environments

Fumeroles

Alumoklyuchevskite was approved in 1993, but to date (July 2023) it has been reported only from the second scoria cone of the Great Fissure eruption at Tolbachik, in three different fumeroles.

Localities

At the type locality, the Great Fissure eruption, Tolbachik Volcanic field, Milkovsky District, Kamchatka Krai, Russia, alumoklyuchevskite is deposited by fumarolic gases as aggregates of prismatic to needle-like crystals, up to 1 mm long and less than 0.1 mm thick. Associated minerals include fedotovite, tenorite, lammerite, averievite, piypite and langbeinite (HOM, Mindat).

Back to Minerals