Qandilite is a rare member of the spinel group characterized by its high titanium content. It is typically found as small, black, opaque octahedral crystals within contact-metamorphosed dolomitic limestones.
Is this qandilite?
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 qandilite with a known reference. Qandilite sits at Mohs 6 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Qandilite leaves a black streak.
- 3Read the lusterHold the specimen under a strong light. Qandilite typically shows a metallic luster.
- 4Match the color rangeCompare against the expected color range: black, dark brown.
- 5Look at form & habitCrystal system: cubic. Typical habit: octahedral crystals.
Often confused with
Qandilite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside qandilite
Minerals reported to co-occur with qandilite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Mg₂TiO₄
- Mohs hardness
- 6
- Density
- 4.41 g/cm³
- Colors
- Streak
- Black
- Luster
- Metallic
- Transparency
- Opaque
- Crystal system
- Cubic
- Crystal habit
- Octahedral Crystals
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Metamorphosed Limestone
- Typical price
- $50-300 per specimen
Where rockhounds find qandilite
Classic worldwide localities
- Qandil Mountains, Iraq
- Kola Peninsula, Russia
Field-hunting tip
Look in metamorphosed limestone country — that is the host setting where qandilite typically forms. If you start seeing forsterite, diopside, calcite in float, you are in the right ground. Field specimens usually show a octahedral crystals habit, so train your eye for that shape before scanning the outcrop.





