
Kyanite Schist
Mica schist with kyanite (Al2SiO5)
A mica schist containing bladed blue kyanite crystals, a marker of medium- to high-grade metamorphism of aluminous rocks.
- Mohs hardness
- Variable (kyanite 4.5 along blade, 6.5-7 across)
- Color
- Silvery-grey with blue blades
- Type
- metamorphic
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Overview
Kyanite schist is a foliated metamorphic rock in which bladed crystals of blue kyanite are set in a matrix of mica and quartz. The striking blue blades, sometimes streaked white or grey, make it a visually distinctive and collectible schist.
Kyanite is one of three aluminosilicate polymorphs (with andalusite and sillimanite) and is the form stable at relatively high pressure, so kyanite schist records deeper or higher-pressure metamorphism than its low-pressure cousins.
The rock is both a geologic indicator and a source of industrial kyanite, used to make heat-resistant refractory materials.
Formation & geology
Kyanite schist develops by regional metamorphism of aluminum-rich (pelitic) sediments such as shale under medium- to high-grade conditions at relatively high pressure. The alumina liberated from breaking-down clay minerals crystallizes as kyanite, frequently alongside garnet, staurolite, and mica.
Because kyanite is the high-pressure aluminosilicate polymorph, its presence implies metamorphism at greater depth than andalusite-bearing rocks; with increasing temperature kyanite eventually converts to sillimanite.
Notable occurrences include the Appalachians (Virginia's Willis Mountain, a major commercial deposit), the Alps, Brazil, India, and Scotland.
How to identify it
Identify kyanite schist by its silvery, foliated mica-quartz matrix containing elongate, bladed crystals of sky-blue to grey-blue kyanite. The hallmark test is kyanite's anisotropic hardness: it can be scratched along the length of a blade (~4.5) but not across it (~6.5-7).
Kyanite has a pearly to vitreous luster, perfect cleavage along the blade, and a white streak. Distinguish the blue blades from blue tourmaline (harder, prismatic, no anisotropic hardness) and from sillimanite (fibrous, not bladed). Garnet and staurolite often accompany it.
Uses & significance
Industrially, kyanite extracted from kyanite schist is a key raw material for refractories: when heated it converts to mullite, producing materials that withstand very high temperatures, used in furnace linings, kiln furniture, and ceramics.
Gem-quality blue kyanite blades are faceted or set as collector jewelry, though their cleavage and variable hardness make cutting challenging. Attractive specimens of the schist are popular with mineral collectors.
Geologically the rock is valuable for indicating high-pressure metamorphic conditions. Metaphysically blue kyanite is associated with communication and alignment, a cultural rather than scientific use.
Frequently asked questions
Why does kyanite have two different hardnesses?
Kyanite is anisotropic: its crystal structure is much softer along the length of a blade (about 4.5) than across it (about 6.5-7), a diagnostic property.
What is kyanite schist used for industrially?
Its kyanite is mined for refractories; on heating it transforms to mullite, giving heat-resistant materials for furnaces, kilns, and high-temperature ceramics.
What does kyanite tell us about metamorphism?
Kyanite is the high-pressure aluminosilicate polymorph, so kyanite schist indicates medium- to high-grade metamorphism at relatively high pressure or depth.
How do I distinguish kyanite from blue tourmaline?
Kyanite forms flat blades with anisotropic hardness and perfect cleavage; tourmaline forms striated prisms, is uniformly hard, and lacks easy cleavage.
Kyanite Schist guides
In-depth guides for identifying, valuing, and understanding Kyanite Schist.
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