Wermlandite is a rare layered double hydroxide mineral typically found as small, thin, yellow-to-brownish platy crystals. It is primarily known from the historic manganese mines of Långban, Sweden, where it forms in the metamorphic mineral assemblages. Collectors should look for its characteristic pearly luster and perfect basal cleavage, though it is often found as tiny inclusions or crusts on other manganese-bearing minerals.
Is this wermlandite?
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 wermlandite with a known reference. Wermlandite sits at Mohs 2 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Wermlandite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Wermlandite typically shows a pearly luster.
- 4Match the color rangeCompare against the expected color range: yellow, brownish-yellow.
- 5Look at form & habitCrystal system: trigonal. Typical habit: platy crystals, tabular aggregates.
Often confused with
Wermlandite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside wermlandite
Minerals reported to co-occur with wermlandite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- [Mg₇(Al,Fe³⁺)₂(OH)₁₈][Ca(H₂O)₆(SO₄)₂]
- Mohs hardness
- 2
- Density
- 2.23 g/cm³
- Colors
- Streak
- White
- Luster
- Pearly
- Transparency
- Translucent
- Crystal system
- Trigonal
- Crystal habit
- Platy Crystals, Tabular Aggregates
- Cleavage
- Perfect Basal
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Metamorphic Manganese Deposits
- Typical price
- $50-300 per specimen
Where rockhounds find wermlandite
Classic worldwide localities
- Långban, Sweden
- Jakobsberg, Sweden
Field-hunting tip
Look in metamorphic manganese deposits country — that is the host setting where wermlandite typically forms. If you start seeing calcite, barite, hausmannite in float, you are in the right ground. Field specimens usually show a platy crystals, tabular aggregates habit, so train your eye for that shape before scanning the outcrop.






