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, 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: yellow, orange red.
- 5Look at form & habitCrystal system: triclinic. Typical habit: columnar.
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
- Density
- 3.355-3.433 g/cm³
- Colors
- Streak
- White
- Luster
- Vitreous
- Transparency
- Translucent
- Crystal system
- Triclinic
- Crystal habit
- Columnar
- Cleavage
- {100} good; {001}, {110}, {011}, poor (by analogy to the axinite group)
- Rarity
- Rare
- Uses
- Collector
- Host rock
- In metamorphosed manganese-bearing ophiolites (Liguria, Italy); in quartz veins in cherts of the greenschist facies (Akatore, New Zealand)
Where rockhounds find tinzenite
Classic worldwide localities
- Tinzen, in the Val d'Err, Graubünden, Switzerland
- Cassagna and Gambatesa mines, Val Graveglia, near Chiavari, Liguria, Italy
- Akatore, New Zealand
Field-hunting tip
Where it forms: In metamorphosed manganese-bearing ophiolites (Liguria, Italy); in quartz veins in cherts of the greenschist facies (Akatore, New Zealand). If you start seeing braunite, quartz in float, you are in the right ground. Typical habit: columnar. Train your eye for that shape before scanning the outcrop.



