Krinovite is an extremely rare silicate mineral first identified in the remains of the Tunguska meteorite. It typically appears as dark green, anhedral grains within meteoritic material, requiring professional chemical analysis to distinguish from other pyroxene-group minerals.
Is this krinovite?
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 krinovite with a known reference. Krinovite sits at Mohs 6-7 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Krinovite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Krinovite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: dark green, emerald green.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: granular.
Often confused with
Krinovite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside krinovite
Minerals reported to co-occur with krinovite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- NaMg₂CrSi₃O₁₀
- Mohs hardness
- 6-7
- Density
- 3.85 g/cm³
- Colors
- Streak
- White
- Luster
- Vitreous
- Transparency
- Translucent
- Crystal system
- Monoclinic
- Crystal habit
- Granular
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Iron-rich Meteorites
- Typical price
- $100-500 per micro-mount or small specimen
Where rockhounds find krinovite
Classic worldwide localities
- Krasnoyarsk Krai, Russia
- Tunguska meteorite fall area, Russia
Field-hunting tip
Look in iron-rich meteorites country — that is the host setting where krinovite typically forms. If you start seeing forsterite, enstatite, chromite in float, you are in the right ground. Field specimens usually show a granular habit, so train your eye for that shape before scanning the outcrop.







