Taramellite is a rare barium iron silicate that typically forms dark brown, elongated prismatic crystals. It is most frequently found in metamorphic environments rich in barium, particularly in skarns and localized hydrothermal occurrences. Collectors prize it for its unique chemical composition and association with other rare barium minerals.
Is this taramellite?
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 taramellite with a known reference. Taramellite sits at Mohs 5.5, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Streak: brown.
- 3Read the lusterHold the specimen under a strong light. Luster: vitreous to silky.
- 4Match the color rangeCompare against the expected color range: reddish brown, bronze purple, brownish violet.
- 5Look at form & habitCrystal system: orthorhombic. Typical habit: fibrous.
Often confused with
Taramellite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside taramellite
Minerals reported to co-occur with taramellite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Ba₄(Fe,Ti)₄O₂[B₂Si₈O₂₇]Cl₁
- Mohs hardness
- 5.5
- Density
- 3.92 g/cm³
- Colors
- Streak
- Brown
- Luster
- Vitreous to silky
- Transparency
- Semitransparent
- Crystal system
- Orthorhombic
- Crystal habit
- Fibrous
- Rarity
- Rare
- Uses
- Collector
- Host rock
- In metamorphic rocks rich in barium silicates, in contact with granitic rocks (Candoglia, Italy); in a metamorphosed Fe{Mn orebody (Långban, Sweden)
Where rockhounds find taramellite
Classic worldwide localities
- Candoglia, Valle de Toce, Piedmont, Italy
- Långban, Värmland, Sweden
Field-hunting tip
Where it forms: In metamorphic rocks rich in barium silicates, in contact with granitic rocks (Candoglia, Italy); in a metamorphosed Fe{Mn orebody (Långban, Sweden). If you start seeing calcite, diopside, actinolite in float, you are in the right ground. Typical habit: fibrous. Train your eye for that shape before scanning the outcrop.








