Kerimasite is a rare member of the garnet group characterized by its high zirconium and iron content. It typically forms sharp dodecahedral crystals in alkaline igneous environments and is primarily sought after by advanced systematic mineral collectors.
Is this kerimasite?
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 kerimasite with a known reference. Kerimasite sits at Mohs 6.5-7 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Kerimasite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Kerimasite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: black.
- 5Look at form & habitCrystal system: cubic. Typical habit: dodecahedral crystals.
Often confused with
Kerimasite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside kerimasite
Minerals reported to co-occur with kerimasite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Ca₃Zr₂(Fe³⁺SiO₄)₃
- Mohs hardness
- 6.5-7
- Density
- 3.8-3.9 g/cm³
- Colors
- Streak
- White
- Luster
- Vitreous
- Transparency
- Opaque
- Crystal system
- Cubic
- Crystal habit
- Dodecahedral Crystals
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Alkaline Igneous Rocks
- Typical price
- $50-500 depending on crystal size and quality
Where rockhounds find kerimasite
Classic worldwide localities
- Kovdor Massif (Russia)
- Uncompahgre Uplift (USA)
Field-hunting tip
Look in alkaline igneous rocks country — that is the host setting where kerimasite typically forms. If you start seeing calcite, forsterite, magnetite in float, you are in the right ground. Field specimens usually show a dodecahedral crystals habit, so train your eye for that shape before scanning the outcrop.






