Haapalaite is a rare layered sulfide-hydroxide mineral that typically forms as small, platy bronze-yellow crystals. It is most frequently identified in nickel-copper sulfide ore bodies where it occurs as an alteration product of primary sulfide minerals like pentlandite.
Is this haapalaite?
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 haapalaite with a known reference. Haapalaite sits at Mohs 1, 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, strong.
- 4Match the color rangeCompare against the expected color range: bronze red.
- 5Look at form & habitCrystal system: hexagonal. Typical habit: scaly, thin.
Often confused with
Haapalaite vs. its common look-alikes, and how to tell them apart in the field.


How to tell apart: Pyrrhotite is the harder of the two (Mohs 3.5-4.5 vs. 1); streak differs, so Haapalaite leaves black, Pyrrhotite leaves dark grayish black.

How to tell apart: Pentlandite is the harder of the two (Mohs 3.5-4 vs. 1); streak differs, so Haapalaite leaves black, Pentlandite leaves pale bronze-brown.
Often found alongside haapalaite
Minerals reported to co-occur with haapalaite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- 2[(Fe,Ni)S]·1.61[(Mg,Fe)(OH)₂]
- Mohs hardness
- 1
- Density
- 3.576 g/cm³
- Colors
- Bronze red
- Streak
- Black
- Luster
- Metallic, strong
- Transparency
- Opaque
- Crystal system
- Hexagonal
- Crystal habit
- Scaly, thin
- Cleavage
- Good
- Rarity
- Rare
- Uses
- Collector
- Host rock
- As thin scales in the Kokka serpentine and in carbonate; rarely in chrysotile
Where rockhounds find haapalaite
Classic worldwide localities
- Kokka serpentinite body, about 33 km north-northwest from the Outokumpu mine, Tapiola, Finland (type locality)
Field-hunting tip
Where it forms: As thin scales in the Kokka serpentine and in carbonate; rarely in chrysotile. If you start seeing pentlandite, maucherite, chalcopyrite in float, you are in the right ground. Typical habit: scaly, thin. Train your eye for that shape before scanning the outcrop.





