erythrite

Erythrite crystallizes in the monoclinic system and forms prismatic crystals.

Erythrite and pharmacolite are common associated minerals.

The main ores of cobalt are cobaltite, erythrite, glaucodot and skutterudite.

It occurs with picropharmacolite, erythrite and aragonite.

It occurs in association with beudantite, carminite, dussertite, pharmacolite, pitticite, adamite and erythrite.

At the type locality, lavendulan occurs associated with erythrite and a cobalt molybdate originally called pateraite, but now discredited.

At San Juan, Chile, it is associated with erythrite, cuprite, malachite and cobaltian wad.

Associated minerals include: bismutite, smaltite, native bismuth, atelestite, erythrite, malachite and barite.

Erythrite occurs as a secondary mineral in the oxide zone of Co-Ni-As bearing mineral deposits.

More yellowish than green, the hypnotic, translucent autainite had come from France, and the purple erythrite from deep in the Atlas Mountains of Morocco.