Kyanite is an aluminum silicate mineral with the formula Al2SiO5, belonging to the nesosilicate (orthosilicate) class of minerals, in which isolated SiO4 tetrahedra are linked by aluminum in octahedral coordination. It crystallizes in the triclinic system, most commonly forming elongated, bladed or tabular crystals, exactly the habit displayed by the crystals in this cluster.
One of the most distinctive scientific features of Kyanite is its directional, anisotropic hardness: crystals typically measure around 4.5 to 5 on the Mohs scale along the length of the crystal, but rise to roughly 6.5 to 7 when measured across it, a rare property caused by the internal atomic bonding pattern of the mineral, and the reason for its historical alternative name Disthene, meaning 'two strengths'.
The vivid blue color seen in specimens from Coronel Murta, Minas Gerais, is caused by trace amounts of iron and titanium substituting for aluminum within the crystal structure. Specifically, the color arises from intervalence charge transfer, an optical process in which an electron is transferred between adjacent Fe2+ and Ti4+ ions (and, to a lesser extent, between Fe2+ and Fe3+ ions) when the crystal absorbs light, the same fundamental mechanism responsible for the blue color of sapphire. Higher iron content generally produces a deeper, richer blue hue.
Geologically, the Kyanite of Barra do Salinas forms within granite pegmatites, often found in association with quartz, a setting that has produced some of the most gemmy and well-formed blue Kyanite crystals known, distinguishing this locality from many others where the mineral occurs as dull, opaque material embedded in schist.
- Formula: Al2SiO5
- Key chemical elements: Aluminum, Silicon, Oxygen
- Hardness (Mohs scale): 4.5-5 along crystal length, 6.5-7 across it (directional/anisotropic)
- Mineral class: Silicates (Nesosilicates)
- Crystal system: Triclinic
- Crystal habit: Bladed, prismatic, intergrown in clusters
- Formation: Granite pegmatites
- Color: Blue, caused by Fe2+/Ti4+ and Fe2+/Fe3+ intervalence charge transfer