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, 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.





