Andychristyite

andychristyite

timroseite

khinite

hematite

Images

Formula: PbCu2+Te6+O5(H2O)
Tellurate
Crystal System: Triclinic
Specific gravity: 6.304 calculated
Hardness: 2 to 3
Streak: Very pale bluish green
Colour: Bluish green
Luminescence: No fluorescence under UV
Solubility: Decomposes rapidly in dilute hydrochloric acid at room temperature
Environments

Hydrothermal environments

Localities

At the type locality, the Aga Mine, Otto Mountain, Baker, Soda Mountains, Silver Lake Mining District, San Bernardino County, California, USA, andychristyite occurs in vugs in quartz in association with timroseite. It is thought to have formed from the partial oxidation of primary sulphides and tellurides during or following brecciation of quartz veins. It forms as small transparent, tabular crystals up to ∼50 µm across, in sub-parallel aggregates, with adamantine lustre. The colour is bluish green and the streak is very pale bluish green (MM 80.6.1055-1065).
As well as quartz and timroseite, other associated minerals include khinite, hematite and goethite (Mindat).

Back to Minerals