Brookite

TiO2
IMA status
  • Approved
  • Grandfathered
IMA symbol
Brk
Discovered
1825
Also known as
  • Arkansit
  • Arkansita
  • Jurinit
  • +3 more

History

The name brookite honors a wool merchant who, in his spare hours, became one of England's most respected crystallographers. Henry James Brooke (1771–1857) trained no microscope on minerals professionally — his living came from textiles — yet he described twelve new species and wrote two foundational books on the subject.

In 1825 the French mineralogist Armand Lévy attached Brooke's name to a brown titanium oxide he was describing from north Wales. The type specimen came from Twll Maen Grisial, a crevice in the diabase — a dark, fine-grained volcanic rock — of Fron Olau near Prenteg in Gwynedd. Through the 19th century that Welsh locality produced some of the finest brookite ever found.

Brooke himself was a fellow of the Royal Society, the Geological Society of London and the Linnean Society. He authored A Familiar Introduction to Crystallography and co-authored An Elementary Introduction to Mineralogy in 1852. The twelve minerals he described include several still familiar to collectors today — annabergite, autunite, caledonite, childrenite, linarite and thomsonite among them.

The mineral itself filled in a chemical puzzle. Titanium dioxide (TiO₂) had already been recognised in two crystal forms — rutile (tetragonal, the common type) and anatase (also tetragonal, but built differently). Brookite gave the trio a third member, this one orthorhombic — a crystal class in which the three axes are all of different lengths and meet at right angles. A fourth natural polymorph, the monoclinic akaogiite, was identified much later under high-pressure conditions.

Beyond Wales, brookite became a classic mineral of the alpine clefts — narrow fractures in metamorphic rock where slow-growing crystals line the walls. The species is widespread in such veins through the Alps and turns up more locally in gneiss and schist, two banded metamorphic rocks formed under heat and pressure. The American collecting tradition centres on Magnet Cove in Arkansas, where the dark variety once called arkansite is in fact brookite.

Industrial & practical applications

Brookite has no industrial use of its own. It is also the least thermally stable of the common titanium dioxide polymorphs — minerals sharing one chemistry but built on different crystal frameworks. Heat brookite past about 750 °C and it converts to rutile, one of its two cousins in the polymorph family.
What remains is collector demand and a small research literature. Sharp brown crystals from the alpine clefts of Europe, and the dark arkansite variety from Magnet Cove in Arkansas, are sought after on the specimen market. Laboratory work on synthetic brookite continues to probe its photocatalytic activity — its ability to drive chemical reactions under light.

Where it forms, where it's found

Geological setting

Hydrothermal vein

An accessory mineral in alpine veins in gneiss and schist; in contact metamorphic zones and hydrothermal veinlets; a common detrital mineral.

Type locality
Twll Maen Grisial
  1. Fron Olau
  2. Prenteg
  3. Dolbenmaen
  4. Gwynedd
  5. Wales
  6. UK

52.9481°, -4.1131°

702recorded occurrences
Source · OpenStreetMap

Varieties

Physical

Hardness
123456789105.5 – 6/ 10 MOHS
  1. 1Talc
  2. 2Gypsum
  3. 3Calcite
  4. 4Fluorite
  5. 5Apatite
  6. 6Orthoclase
  7. 7Quartz
  8. 8Topaz
  9. 9Corundum
  10. 10Diamond
Lustre
Metallic · Adamantine
Transparency
Transparent · Translucent · Opaque
Colour
Brown · yellowish brown · reddish brown · dark brown to iron-black · yellowish brown to dark brown in transmitted light
Streak
White to greyish white or yellowish white
Tenacity
brittle
Cleavage
Poor/Indistinct

on (120), in traces on (001)

Fracture
Irregular/Uneven · Sub-Conchoidal
Density
4.08 g/cm³

Optical

Optical type
Biaxial (+) · 2V measured = 28° · 2V calc = 12 – 20°
Refractive index
2.5831 – 2.7004
Surface relief
Very high
Principal indices
nα 2.5831 · nβ 2.5843 · nγ 2.7004
Birefringence
0.1173
Pleochroism
Weak

Yellow, red, orange to brown

Dispersion
r > v, very strong, with crossed axial dispersion
Extinction
Parallel
UV response
Not fluorescent in ultraviolet
Michel-Lévy diagramhighlighted lineδ = 0.1173
Attainable Michel-Lévy rangeΔ ∈ [0, t·δmax]1173 nm3rd order
Δ = 0Δmax
Thin-section mosaic70 grains · random 3D orientations
PPLpleochroism per grain
XPLindependent extinctions · rotate the stage
Interference simulatorsingle grain · PPL ↔ XPL
PPLpleochroism only · colour blends on rotation
XPLinterference colour · extinct every 90°
Retardation1173 nm
Order3rd order
XPL colour

Crystallography

Crystal system
Orthorhombic
Cell parameters
a = 5.4558 Å · b = 9.1819 Å · c = 5.1429 Å
Ratio a:b:c
1 : 1.683 : 0.943
Z
8
Morphology

Crystals typically tabular on (010), striated parallel to [001] and elongated; pyramidal (111) or pseudohexagonal with (120) and (111) equally developed; also prismatic on [001] with (120) prominent; rarely tabular on (001) or pseudo-pyramidal.

Twinning

On (120), uncertain

Epitaxy

Rutile (110) [001] parallel to brookite (120) [001]. Rutile (110) [001] parallel to brookite (111) [001].

Type-locality form

Bladed red to brown transparent to translucent bladed crystals with longitudinal striations.

Comment

Space Group: Pcab

Crystal structure

Chemical composition

Constituent elements
Mass composition breakdown
ElementAtoms At. mass g/mol Mass g/molMass share
22TiTitaniumTitanium147.86747.867
59.93%
8OOxygenOxygen215.99931.998
40.07%
Total79.865100.00%

Mass share = atoms × atomic mass ÷ molar mass × 100

From IMA formula

Impurities
  • Fe
  • Ta
  • Nb

Synonyms

  • Arkansit
  • Arkansita
  • Jurinit
  • Jurinita
  • Jurinite
  • Pyromelane

In other languages

French
arkansite · brookite · eumanite · jurinite · pyromélane
German
Arkansit · Brookit
Spanish
Brookita
Italian
Brookite
Portuguese
brookita · Brookite
Japanese
ブルカイト · ブルッカイト · 板チタン石
Chinese
板鈦礦 · 板钛矿
Russian
Брукит
Arabic
بروكيت

Classification

Strunz
10th ed.

4.DD.10

  • 4OxidesClass
  • 4.DMetal: Oxygen = 1:2 and similarDivision
  • 4.DDWith medium-sized cations; frameworks of edge-sharing octahedraGroup
  • 4.DD.10BrookiteSpecies
Dana
8th ed.

04.04.05.01

  • 04Simple OxidesClass
  • 04.04AX2Type
  • 04.04.05— unnamed intermediate level —Group
  • 04.04.05.01BrookiteSpecies
CIM

7.9.4

  • 7Oxides and HydroxidesClass
  • 7.9Oxides of TiGroup
  • 7.9.4BrookiteSpecies

Group, growth & confusion

Often grow together
3 minerals
Commonly confused with
4 minerals

Literature, links & citation

Citations
  1. 1825Levy, M. (1825) An account of a new mineral. The Annals of Philosophy: 9: 140-142.
  2. 1825Haidinger, W. (1825) Beschreibung mehrerer neuer oder bisher nur unvollkommen bekannter Mineralien. Annalen der Physik, 5, 157-177 (162).
  3. 1850Kokscharow, N. (1850) Ueber Brookit-Krystalle vom Ural. Annalen der Physik, 155(3), 454-464.
  4. 1858Des Cloizeaux (1858) Annales minéralogiques: 14: 361.
  5. 1884Zepharovich, V. von (1884) Ueber Brookit, Wulfenit und Skolezit. Zeitschrift für Krystallographie, Mineralogie und Petrographie, 8 (1-6). 577-592 doi:10.1524/zkri.1884.8.1.577DOI: 10.1524/zkri.1884.8.1.577
Cite this entry
@misc{mineral2026,
  author    = {Mineral Index editorial board},
  title     = {Brookite — Mineral Index},
  year      = {2026},
  url       = {https://mineralindex.org/minerals/brookite-787},
  note      = {Accessed 2026-05-11}
}