Flinkite is a rare manganese arsenate mineral typically found as tabular crystals or radial clusters. It is almost exclusively found in the famous manganese mines of Långban, Sweden, where it occurs within metamorphic manganese-rich formations.
Is this flinkite?
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 flinkite with a known reference. Flinkite sits at Mohs 5 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Flinkite leaves a light brown streak.
- 3Read the lusterHold the specimen under a strong light. Flinkite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: brown, brownish-red, yellowish-brown.
- 5Look at form & habitCrystal system: orthorhombic. Typical habit: tabular to prismatic crystals, often in radial or sheaflike aggregates.
Often confused with
Flinkite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside flinkite
Minerals reported to co-occur with flinkite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Mn²⁺₂Mn³⁺(AsO₄)(OH)₄
- Mohs hardness
- 5
- Density
- 3.84 g/cm³
- Streak
- Light Brown
- Luster
- Vitreous
- Transparency
- Translucent
- Crystal system
- Orthorhombic
- Crystal habit
- Tabular to Prismatic Crystals, Often in Radial or Sheaflike Aggregates
- Cleavage
- Distinct On {010}
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Metamorphosed Manganese Ore Deposits
- Typical price
- $50-300 thumbnail
Where rockhounds find flinkite
Classic worldwide localities
- Långban, Värmland, Sweden
- Jakobsberg, Värmland, Sweden
- Pajsberg, Värmland, Sweden
Field-hunting tip
Look in metamorphosed manganese ore deposits country — that is the host setting where flinkite typically forms. If you start seeing hausmannite, jakobsite, barite in float, you are in the right ground. Field specimens usually show a tabular to prismatic crystals, often in radial or sheaflike aggregates habit, so train your eye for that shape before scanning the outcrop.





