Sanguite | |
---|---|
General | |
Category | Halides |
Formula (repeating unit) | KCuCl₃ |
IMA symbol | Sgu |
Crystal system | monoclinic |
Crystal class | 2/m |
Space group | 2/ m - prismatic |
Unit cell | V = 481.38 ų |
Identification | |
Color | bright red |
Twinning | polysynthetic twinning has been observed. |
Cleavage | Perfect |
Fracture | staggered, step-like |
Tenacity | fragile |
Luster | Vitreous |
Streak | reddish orange |
Density | 2.86(1) g/cm³ (measured); 2.88 g/cm³ (calculated) |
Optical properties | biaxial |
Refractive index | n α = 1.653(3) n β = 1.780(6) n γ = 1.900(8) |
Birefringence | δ = 0.247 |
Pleochroism | strong |
2V angle | Measured: 85° (5) Calculated: 82° |
Dispersion | very strong |
References | [1] |
Sanguite is a halide mineral. It is named after the Latin word sanguis, meaning blood, due to its bright red colouration. It was approved as a valid species by the International Mineralogical Association in 2013.
Sanguite is a chloride with the chemical formula KCuCl3. It crystallizes in the monoclinic system and has a Mohs scale hardness of 3.
Sanguite was discovered in the Glavnaya Tenoritovaya fumarole on the Tolbachik Volcano in Kamchatka Krai, Russia, the only place on Earth where it is known to form. [1] There it forms in clusters or crusts as fine prismatic crystals up to 1 mm long and 0.2 mm thick.
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Chrysothallite is a rare thallium-bearing chloride mineral with the formula K6Cu6Tl3+Cl17(OH)4•H2O. Chrysothallite is unique in being only the second mineral with essential trivalent thallium, a feature shared with natural thallium(III) oxide, avicennite. Another examples of natural thallium chlorides are steropesite, Tl3BiCl6, and lafossaite, TlCl. Chrysothallite is one of numerous fumarolic minerals discovered among fumarolic sites of the Tolbachik volcano, Kamchatka, Russia The mineral is named in allusion to its colour and thallium content.
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: CS1 maint: url-status (link)The map of localities is at the bottom of the page, showing it is only known to form on Tolbachik.