Armenite is a rare barium-calcium cyclosilicate that typically occurs as pseudo-hexagonal prismatic crystals. It is primarily sought by advanced collectors for its complex twinning patterns and rarity in hydrothermal environments.
Is this armenite?
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 armenite with a known reference. Armenite sits at Mohs 7-8, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Streak: white.
- 3Read the lusterHold the specimen under a strong light. Luster: vitreous.
- 4Match the color rangeCompare against the expected color range: colorless, gray green, white.
- 5Look at form & habitCrystal system: orthorhombic. Typical habit: prismatic crystals, often forming pseudo-hexagonal cyclic twins.
Often confused with
Armenite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside armenite
Minerals reported to co-occur with armenite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- BaCa₂Al₆Si₉O₃₀·2H₂O
- Mohs hardness
- 7-8
- Density
- 2.74-2.76 g/cm³
- Colors
- Streak
- White
- Luster
- Vitreous
- Transparency
- Translucent
- Crystal system
- Orthorhombic
- Crystal habit
- Prismatic crystals, often forming pseudo-hexagonal cyclic twins
- Cleavage
- Perfect prismatic, one pinacoidal distinct; partings along sector boundaries
- Rarity
- Rare
- Uses
- Collector
- Host rock
- In calcite veins (Kongsberg, Norway); in manganese-metasomatized diorite included in later granodiorite (Rémigny, Canada)
Where rockhounds find armenite
Classic worldwide localities
- Armen mine, near Kongsberg, Norway
- Su Zurfuru mine, Fluminese, Sardinia, Italy
- Wasenalp, near Simplon, Valais, Switzerland
- Coire Loch Kander, 11 km south-southeast of Braemar, Scotland
- Chvaletice, Czech Republic
- Rémigny, Quebec, Canada
Field-hunting tip
Where it forms: In calcite veins (Kongsberg, Norway); in manganese-metasomatized diorite included in later granodiorite (Rémigny, Canada). If you start seeing axinite, pyrrhotite, quartz in float, you are in the right ground. Typical habit: prismatic crystals, often forming pseudo-hexagonal cyclic twins. Train your eye for that shape before scanning the outcrop.









