Rutile

Crystal system · Tetragonal

Rutile is an oxide mineral prized by collectors for its exceptional color range, with several world-class Chinese localities.

About Rutileextended article

Save to favoritesview your list
Crystal Structure
Tetragonal — Ti octahedrally coordinated, edge-sharing along c.
External databases provide CIF (Crystallographic Information File) downloads + interactive 3D viewers. AMCSD: American Mineralogist Crystal Structure Database (free, RRUFF-hosted). COD: open community-curated database.
Elemental Composition (by mass)
ElementMass %Visual
Ti Titanium59.93%
O Oxygen40.07%
Computed from simplified end-member formula. Solid-solution series, water content, and trace substitutions cause real-world variation.
IMA Abbreviation (Whitney-Evans 2010)
Rt
→ Rutile
TiO₂ tetragonal
Standard symbol from American Mineralogist (Whitney & Evans, 2010). Used in thin-section labeling, phase diagrams, and IMA-style species records.
Pronunciation
/ˈruːtiːl/
roo-TEEL
Latin rutilus (reddish)
Pseudomorph Relationships
Replaces — this mineral is often a pseudomorph after:
Ilmenite replacement
Ilmenite (FeTiO₃) weathers/exsolves to rutile (TiO₂) — important Ti ore process.
Heavy mineral sands.
A pseudomorph (Greek "false form") is a mineral with the external shape of another species — the chemistry has changed but the crystal habit is inherited. › Full catalogue
Luster
adamantine
Very high RI; brilliant brown-red shine.
Diaphaneity (Transparency)
translucent-to-opaque
Thin needles transparent in quartz host.
Type Locality
Boinik, Hungary — Slovakia
Described 1803 by Werner
Specific Gravity
4.20–4.30
g/cm³
heavy
TiO₂.
For comparison: water = 1.00, glass ≈ 2.5, quartz = 2.65, corundum ≈ 4.00, galena ≈ 7.50, gold ≈ 19.3.
Streak Test
pale brown
Tan streak from black-red crystals.
Streak = color of the powdered mineral. Drag specimen across unglazed white porcelain plate (Mohs 6.5). For minerals harder than the plate, crush a small flake into powder and observe color.
Twinning Laws
Knee twin (elbow)contact
Two prisms meeting at 114°36′ on {011}. Common in alpine cleft rutile.
Cyclic / sixlingcontact
Six crystals forming a star or wheel. Spectacular when complete.
Reticulated meshcontact
Lattice-like networks ("sagenite") in chlorite or in alpine quartz.
Collector tier: Solid Display
Reliable mid-tier display species. Easy to find in well-formed examples; broad locality diversity.
PolymorphsShares the formula TiO2 with: Anatase · Brookite — same chemistry, different crystal structure.
Often found withQuartz · Apatite · Ilmenite · Hematite
Mohs 6–6.5
Vickers (~) 820 HV
Knoop (~) 870 HK
Nickel–Strunz 4.DB.05
Dana 04.04.01.01
Geological setting
PegmatiteMetamorphic
Element composition by mass

Formula: TiO₂ · molar mass: 79.87 g/mol

Ti 59.93%
O 40.07%

Computed from atomic weights (IUPAC 2021). Site-occupancy groups (Fe,Mn) split equally.

Mohs Hardness 6–6.5

Rutile sits at 6–6.5 on the Mohs scale — just hard enough to scratch glass.

🔊 Read aloud
Colors:
Streak
Pale brown
Crystal system
Tetragonal
Type localityBoinik, Bohemia, Czech Republic
✓ I have this★ WishlistView my collection →

Discovery First described 1803 by Werner

📇 Print ID card

Oxides & HydroxidesOxides
TL;DR · 1 min read
Rutile (TiO₂) is the highest-temperature TiO₂ polymorph (with anatase low-T and brookite intermediate). Its name from Latin "rutilus" (red) reflects its diagnostic blood-red translucent crystals.
Text size:AAA

Rutile (TiO₂) is the highest-temperature TiO₂ polymorph (with anatase low-T and brookite intermediate). Its name from Latin “rutilus” (red) reflects its diagnostic blood-red translucent crystals. Rutile is the principal industrial source of titanium and a common accessory mineral in metamorphic and igneous rocks. Acicular needles in quartz produce “rutilated quartz” — a major collector variety.

More minerals to explore #

Identification & care

Rutile typically forms prismatic with vertical striations; twinned 'knee-shaped' twins (geniculated) and cyclic sixling 'wheel' twins; acicular in quartz (sagenite); massive, granular. Its color range is broad, including blood red, brownish yellow, brown-red, yellow, greyish-black, black, brown, and bluish or violet. The luster is adamantine, metallic, the streak is greyish black, pale brown, light yellow, and specimens range from transparent (red), to opaque (black). The cleavage is distinct/good on {110}, imperfect on {100}. The fracture is irregular/uneven, sub-conchoidal, which aids identification.

Collector context

How it forms

Rutile forms in accessory mineral in igneous and metamorphic rocks; pegmatites; hydrothermal veins; beach sand placers (with ilmenite, zircon); inclusions in quartz, garnet, corundum. It is commonly found in association with ilmenite, titanite, quartz (as inclusions), hematite, zircon, brookite, anatase.

Classic Chinese localities

Documented Chinese occurrences are recorded at Shangbao Mine, Jiama Cu-polymetallic deposit and Jinduicheng Mine, among others.

Why collectors care

Collectors pursue Rutile for the clarity of its crystal form and, in good material, saturated color that reads instantly across a display case. A well-terminated rutile on clean matrix photographs well, identifies quickly, and anchors a cabinet piece. Top Chinese specimens over the last two decades have reset the bar for what rutile looks like at collector grade.

What affects value

Value in Rutile is assessed, in typical order of weight, against: (1) locality provenance; (2) size relative to the species norm; (3) crystal form and termination sharpness; (4) color saturation and zoning; (5) transparency and internal clarity; (6) matrix quality and aesthetic balance; (7) condition (absence of damage, chips, or repair). Cleaning quality and verified locality documentation act as multipliers across the above.

Naming history

The name Rutile has a specific etymological and historical context — see Mindat's reference entry for provenance details. We have retained naming data at the record level; published prose is paraphrased from factual fields rather than copied from source.