Bohseite

bohseite

phenakite

helvite

lepidolite

Images

Formula: Ca4Be3+xAl1-xSi9O25-x(OH)3+x (x = 0 to 1)
Inosilicate (chain silicate), forms a series with bavenite, beryllium-bearing mineral
Crystal System: Orthorhombic
Specific gravity: 2.719 calculated
Hardness: 5 to 6
Streak: White
Colour: White
Environments

Pegmatites

Localities

At the type locality, the Piława Górna Quarry, Piława Górna, Dzierżoniów County, Lower Silesian Voivodeship, Poland, bohseite occurs in a zoned anatectic pegmatite dyke in close association with microcline, cesium-rich beryl, phenakite, helvine, lepidolite and probably bertrandite, as alteration products after a primary beryllium mineral, probably beryl. Bohseite forms fan-like or parallel aggregates up to 0.7 cm of white, platy crystals up to 2 mm long, with characteristic striations (MM 81.35-46).

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