Krutovite is a rare nickel arsenide mineral that occurs primarily as metallic grains or small aggregates within hydrothermal vein systems. It is notoriously difficult to identify without chemical analysis due to its similarity to other nickel and cobalt arsenides.
Is this krutovite?
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 krutovite with a known reference. Krutovite sits at Mohs 5.5, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Streak: black.
- 3Read the lusterHold the specimen under a strong light. Luster: metallic.
- 4Match the color rangeCompare against the expected color range: gray white.
- 5Look at form & habitCrystal system: cubic. Typical habit: grains, inclusions in other minerals.
Often confused with
Krutovite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside krutovite
Minerals reported to co-occur with krutovite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- NiAs₂
- Mohs hardness
- 5.5
- Density
- 7.08-7.12 g/cm³
- Colors
- Streak
- Black
- Luster
- Metallic
- Transparency
- Opaque
- Crystal system
- Cubic
- Crystal habit
- Grains, inclusions in other minerals
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- In Co–Ni–As sulfide veins of hydrothermal origin
Where rockhounds find krutovite
Classic worldwide localities
- Geshiber vein, Jáchymov (Joachimsthal), Czech Republic (type locality)
- Khovu-Aksy Ni–Co deposit, Tuva, Siberia, Russia
Field-hunting tip
Where it forms: In Co–Ni–As sulfide veins of hydrothermal origin. If you start seeing nickel-skutterudite, tennantite, nickeline in float, you are in the right ground. Typical habit: grains, inclusions in other minerals. Train your eye for that shape before scanning the outcrop.







