Axinite-(Fe) is best identified by its distinctive sharp, wedge-shaped crystals that often look like axe blades. It is a calcium-iron borosilicate typically found in contact metamorphic zones where hydrothermal fluids have altered calcareous rocks.
Is this axinite-(fe)?
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-(fe) with a known reference. Axinite-(Fe) 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. Axinite-(Fe) leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Axinite-(Fe) typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: clove-brown, plum-blue, honey-brown.
- 5Look at form & habitCrystal system: triclinic. Typical habit: wedge-shaped, sharp-edged tabular crystals.
Often confused with
Axinite-(Fe) vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside axinite-(fe)
Minerals reported to co-occur with axinite-(fe). Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Ca₂Fe²⁺Al₂BSi₄O₁₅(OH)
- Mohs hardness
- 6.5-7
- Density
- 3.27-3.35 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Transparent
- Crystal system
- Triclinic
- Crystal habit
- Wedge-shaped, Sharp-edged Tabular Crystals
- Cleavage
- Distinct On {110}
- Rarity
- Uncommon
- Uses
- Collector, Gemstone
- Host rock
- Contact Metamorphic Rocks and Skarns
- Typical price
- $20-150 for small specimens, $200+ for large crystals
Where rockhounds find axinite-(fe)
Classic worldwide localities
- France
- Russia
- USA
- Brazil
- Mexico
Field-hunting tip
Look in contact metamorphic rocks and skarns country — that is the host setting where axinite-(fe) typically forms. If you start seeing quartz, calcite, epidote in float, you are in the right ground. Field specimens usually show a wedge-shaped, sharp-edged tabular crystals habit, so train your eye for that shape before scanning the outcrop.








