Minerals & Crystals Codexery

Brookite

Orthorhombic titanium dioxide polymorph, rare and photocatalytic.

Brookite

Brookite is the orthorhombic polymorph of titanium dioxide (TiO2), one of four known natural forms of the mineral, alongside akaogiite, anatase, and rutile. It is named after English crystallographer and mineralogist Henry James Brooke, and is noted for its rarity compared to anatase and rutile, as well as its photocatalytic activity. Brookite crystals are typically brown, tabular, and elongated, with a submetallic luster and high refractive indices exceeding that of diamond.

crystal_system
Orthorhombic
formula
TiO2
hardness
5+1⁄2 to 6 (Mohs)
specific_gravity
4.08 to 4.18
refractive_index
Above 2.5 (biaxial positive)
common_impurities
Iron, tantalum, niobium
type_locality
Twll Maen Grisial, Fron Olau, Prenteg, Gwynedd, Wales

Lore & Background

The mineral occurs as an accessory in alpine veins in gneiss and schist, and is also a common detrital mineral.

Reader's Guide

Brookite is significant as a rare polymorph of titanium dioxide, exhibiting photocatalytic activity similar to anatase and rutile but with a larger unit cell volume (8 TiO2 groups per cell). Its structure consists of distorted octahedra sharing three edges, forming an orthorhombic lattice. The mineral's high refractive indices (above 2.5) and biaxial positive optical character make it distinctive among minerals. Brookite is typically brown, with weak pleochroism, and is brittle with a hardness of 5+1⁄2 to 6. Common impurities include iron, tantalum, and niobium. A variety known as arkansite occurs in Magnet Cove, Arkansas, and the Murun Massif in Eastern Siberia. Associated minerals include anatase, rutile, titanite, quartz, and hematite.

Did You Know?

More in Minerals & Crystals 1-24

Elsewhere in the Minerals & Crystals universe

Spotted an error? Know more?

This is a living reference — every entry is fact-audited, and reader corrections feed straight into our audit queue. Suggest an edit · See this site's audit record

Comments

Loading…
Open in the interactive codex →