Indialite is the high-temperature polymorph of cordierite, structurally analogous to beryl. It is typically found in paralavas and buchites formed by the extreme heating of sediments by igneous intrusions, appearing as small blue to colorless hexagonal crystals.
Is this indialite?
5-step field checkRun through these checks against the specimen in your hand. The more boxes tick, the more confident the ID.
- 1Test the hardnessTry to scratch indialite with a known reference. Indialite sits at Mohs 7-7.5, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Streak: white.
- 3Read the lusterHold the specimen under a strong light. Luster: vitreous.
- 4Match the color rangeCompare against the expected color range: colorless, pale mauve.
- 5Look at form & habitCrystal system: hexagonal. Typical habit: hexagonal, prismatic.
Often confused with
Indialite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside indialite
Minerals reported to co-occur with indialite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Mg₂Al₄Si₅O₁₈
- Mohs hardness
- 7-7.5
- Density
- 2.512 g/cm³
- Colors
- ColorlessPale mauve
- Streak
- White
- Luster
- Vitreous
- Transparency
- Transparent
- Crystal system
- Hexagonal
- Crystal habit
- Hexagonal, prismatic
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector, Scientific research
- Host rock
- Formed by fusion and recrystallization of sedimentary rocks as a result of the burning of underlying coal seams (Bokaro coalfield, India); in cordierite veins in a polymetamorphosed pelitic rock (Unazuki, Japan)
Where rockhounds find indialite
Classic worldwide localities
- Pyramid Lake, Washoe Co., Nevada, USA
- Bokaro coal seam, southwest of Hazaribagh, Bihar, India
- Unazuki area, Toyama Prefecture, Japan
- Bellerberg volcano, two km north of Mayen, Eifel district, Germany
Field-hunting tip
Where it forms: Formed by fusion and recrystallization of sedimentary rocks as a result of the burning of underlying coal seams (Bokaro coalfield, India); in cordierite veins in a polymetamorphosed pelitic rock (Unazuki, Japan). If you start seeing enstatite, magnetite, labradorite in float, you are in the right ground. Typical habit: hexagonal, prismatic. Train your eye for that shape before scanning the outcrop.







