Axinite is highly prized by collectors for its distinctive wedge-shaped, blade-like crystal habits that often appear sharp and flattened. It is most commonly found in contact metamorphic rocks, specifically in calc-silicate skarns and hydrothermal veins.
Is this axinite?
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 axinite with a known reference. Axinite 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. Streak: white.
- 3Read the lusterHold the specimen under a strong light. Luster: vitreous.
- 4Match the color rangeCompare against the expected color range: brown, violet-brown, plum-blue, grayish-brown.
- 5Look at form & habitCrystal system: triclinic. Typical habit: wedge-shaped crystals, tabular, massive.
Often confused with
Axinite vs. its common look-alikes, and how to tell them apart in the field.

How to tell apart: Axinite is noticeably harder (Mohs 6.5-7 vs. 5-5.5); luster reads vitreous on Axinite and adamantine on Sphene.

How to tell apart: Streak differs, so Axinite leaves white, Epidote leaves grayish white.

Often found alongside axinite
Minerals reported to co-occur with axinite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Ca₂(Fe,Mg,Mn)Al₂BSi₄O₁₅(OH)
- Mohs hardness
- 6.5-7
- Density
- 3.27-3.35 g/cm³
- Colors
- Streak
- White
- Luster
- Vitreous
- Transparency
- Transparent
- Crystal system
- Triclinic
- Crystal habit
- Wedge-shaped crystals, tabular, massive
- Cleavage
- Good in one direction
- Rarity
- Uncommon
- Uses
- Collector, Lapidary
- Host rock
- metamorphic contact zones
Where rockhounds find axinite
6 mapped spotsClassic worldwide localities
- Bourg-d'Oisans, France
- Cornwall, England
- Baja California, Mexico
- New Jersey, USA
- Russia
Field-hunting tip
Where it forms: metamorphic contact zones. If you start seeing calcite, quartz, epidote in float, you are in the right ground. Typical habit: wedge-shaped crystals, tabular, massive. Train your eye for that shape before scanning the outcrop. In the U.S., the densest reported localities are in New Jersey, California. Start trip planning there.





