Tinzenite is a member of the axinite group characterized by its significant manganese content, which gives it distinctive warm yellow to brownish-orange hues. It is typically found in manganese-rich silicate rocks formed through regional metamorphism. Collectors look for its wedge-shaped, triclinic crystal habits, which are rare and prized from classic localities like Switzerland and Franklin, New Jersey.
Is this tinzenite?
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 tinzenite with a known reference. Tinzenite sits at Mohs 6.5-7 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Tinzenite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Tinzenite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: yellow, orange, brown, reddish-brown.
- 5Look at form & habitCrystal system: triclinic. Typical habit: tabular to wedge-shaped crystals.
Often confused with
Tinzenite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside tinzenite
Minerals reported to co-occur with tinzenite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- (Ca,Mn)₃Al₂BSi₄O₁₅(OH)
- Mohs hardness
- 6.5-7
- Density
- 3.39-3.41 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Translucent
- Crystal system
- Triclinic
- Crystal habit
- Tabular to Wedge-shaped Crystals
- Cleavage
- Distinct
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Manganese-rich Metamorphic Rocks
- Typical price
- $50-300 per specimen
Where rockhounds find tinzenite
Classic worldwide localities
- Tinzen, Graubünden, Switzerland
- Franklin, New Jersey, USA
- Langban, Sweden
Field-hunting tip
Look in manganese-rich metamorphic rocks country — that is the host setting where tinzenite typically forms. If you start seeing braunite, rhodonite, calcite in float, you are in the right ground. Field specimens usually show a tabular to wedge-shaped crystals habit, so train your eye for that shape before scanning the outcrop.





