Khademite

khademite

copiapite

butlerite

amarantite

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Formula: Al(SO4)F(H2O)5
Hydrated sulphate containing halogen
Crystal System: Orthorhombic
Specific gravity: 1.925 measured, 1.942 calculated
Hardness: 1 to 2
Streak: White
Colour: Colourless
Environments

Hydrothermal environments

Khademite occurs as a post-mine efflorescence (Webmin), and, rarely, it is formed in the oxidised zone of hydrothermal base-metal deposits (HOM).

Localities

At the type locality, Kavir-e-Sagand, Saghand, Ardakan County, Yazd Province, Iran, khademite was found associated with copiapite, butlerite, parabutlerite, jarosite, amarantite and alunogen (AM 60.486).

At Mine no. 2, Byk Mountain, Lermontovskoe U Deposit, Pyatigorsk, Stavropol Krai, Russia, gurzhiite occurs as fine-grained aggregates forming veinlets up to 50 cm long in cracks of the brecciated rock. Gurzhiite aggregates are composed of small bladed crystals up to 0.1 mm across. Associated minerals include khademite and quartz. (MM 86.3.412–421).

At the Lone Pine mine, Lone Pine Hill area, Wilcox Mining District, Catron County, New Mexico, USA, khademite has been found associated with with wilcoxite, lannonite and gypsum (HOM).

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