Osumilite

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Osumilite
Category Mineral
Chemical formula (K,Na)(Fe,Mg)2(Al,Fe)3(Si,Al)12O30·H2O
Identification
Color Rarely transparent to translucent, blue, brown, black, gray
Crystal habit Include prismatic crystals with a pinacoidal termination
Crystal system Hexagonal; 6/m 2/m 2/m.
Twinning Rarely
Cleavage None
Fracture Subconchoidal
Mohs Scale hardness 5 - 6
Luster Vitreous
Optical Properties Uniaxial (+), w=1.5406, e=1.543, bire=0.0024
Streak Blue-gray
Specific gravity 2.62 - 2.64
Other Characteristics Dana class: 63.2.1a.7

Osumilite a very rare hydrate potassium-sodium-iron-magnesium-aluminum silicate mineral. Osumilite is part of the of the milarite group (also known as the milarite-osumilite group) of cyclosilicates.

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[edit] Characteristics

Osumilite chemical formula is (K,Na)(Fe,Mg)2(Al,Fe)3(Si,Al)12O30·H2O. It is translucent and the typical coloring is either blue, black, brown, or gray. It displays no cleavage and has a vitreous luster. Osumilite has a hardness between 5-6 on the Mohs hardness scale.[1]

The hexagonal crystal structure of osumilite is an unusual molecular make-up. The primary unit is a double ring, with a formula of Si12O30. Normal cyclosilicate have rings composed of six silicate tetrahedrons; Si6O18. In a double ring structure, two normal rings are linked by sharing six oxygens, one from each tetrahedron in each six membered ring.[2]

[edit] Occurrence

Osumilite, was first discovered as grains in volcanic rocks near Osumi, Japan. It was confused with a similar mineral cordierite because of their similar coloring. It can be found in high-grade metamorphic rocks, xenoliths and in the groundmass of rhyolite and dacite.[3]

Osumilite is found in the Obsidian Cliffs, Oregon; Sardinia, Italy; Kagoshima and Yamanashi Prefecture, Japan; and the Eifel district in Germany.[3]

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