Argandite is an exceptionally rare member of the garnet group, specifically a manganese vanadate. It is primarily found as small, yellow, dodecahedral crystals in highly specific metamorphic manganese deposits, most notably the Långban mines in Sweden.
Is this argandite?
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 argandite with a known reference. Argandite sits at Mohs 7 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Argandite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Argandite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: yellow, brownish-yellow, orange-yellow.
- 5Look at form & habitCrystal system: cubic. Typical habit: dodecahedral crystals, granular.
Often confused with
Argandite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside argandite
Minerals reported to co-occur with argandite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Mn₃(VO₄)₂
- Mohs hardness
- 7
- Density
- 3.80-3.90 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Translucent
- Crystal system
- Cubic
- Crystal habit
- Dodecahedral Crystals, Granular
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Metamorphosed Manganese Ore Deposits
- Typical price
- $100-500 per specimen
Where rockhounds find argandite
Classic worldwide localities
- Långban, Sweden
Field-hunting tip
Look in metamorphosed manganese ore deposits country — that is the host setting where argandite typically forms. If you start seeing hausmannite, jakobsite, manganosite in float, you are in the right ground. Field specimens usually show a dodecahedral crystals, granular habit, so train your eye for that shape before scanning the outcrop.




