Minerale caratterizzato da un colore giallo pallido, lucentezza vitrea, frattura concoide, sfaldatura perfetta ma spesso difficile da osservare, traslucido, tenacità molto fragile. L’abito cristallino del minerale risulta essere prismatico allungato con cristalli aggregati. Minerale associato ad emimorfite.
ZONA DI PROVENIENZA
Mapimi, Durango
NAZIONE DI PROVENIENZA
Messico
ORIGINE
Minerale che si origina nelle zone di ossidazione di giacimenti di zinco contenenti minerali primari di arsenico
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