Darapskite

darapskite

blodite

mirabilite

nitratine

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Formula: Na3(SO4)(NO3).H2O
Compound nitrate
Crystal System: Monoclinic
Specific gravity: 2.201 measured, 2.202 calculated
Hardness: 2½
Streak: White
Colour: Colourless
Solubility: Readily soluble in water
Environments

Evaporite deposits

Darapskite occurs in nitrate deposits rich in sulphates. Common associates include anhydrite, blödite, halite and nitratine (Mindat).

Localities

At the Roberts Massif, Queen Maud Land, Eastern Antarctica, Antarctica, and supposedly darapskite has been reported in saline arid soil (AM 55.1500-1517).

At the type locality, Pampa del Toro, Oficina Lautaro, Taltal, Antofagasta Province, Antofagasta, Chile, darapskite occurs in the nitrate ore as discrete crystals in cavities, as platy masses in veins, and as granular material admixed with other saline minerals in veins, pods, and cementing material. Delicate tabular crystals are by far the most abundant and widespread; prismatic crystals were found at only a few localities. Veins of darapskite, found at a few localities only, consist of imperfect tabular crystals as much as 10 cm long and 1 cm thick. Granular darapskite is found associated with halite and nitratine in veins, in encrustations in cavities, and in small pods or blebs as well as in finely disseminated saline cement.
It appears that darapskite formed between 7 and 74oC. (AM 55.1500-1517).
Associated minerals include niter, blödite, mirabilite, epsomite and anhydrite, as well as halite and nitratine (HOM).

At the Chuquicamata Mine, Chuquicamata District, Calama, El Loa Province, Antofagasta, Chile, darapskite occurs in veins, as much as 6 inches wide, associated with kröhnkite, blödite, mirabilite and epsomite (AM 55.1500-1517).

At the Funeral Mts, Amargosa Range, Inyo county, California, USA, darapskite occurs in saline material from caves in limestone (AM 55.1500-1517).

At the Death Valley National Park, USA, darapskite occurs in the nitrate deposits of California, where it is associated with nitratine and niter (AM 55.1500-1517).

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