Axinite-(Mg) is a rare magnesium-rich member of the axinite group, highly prized by collectors for its distinctive wedge-shaped, blade-like crystals. It is most commonly found in contact metamorphic rocks, often displaying a range of brownish to violet hues and exceptional brilliance when facet-cut.
Is this axinite-(mg)?
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-(mg) with a known reference. Axinite-(Mg) 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-(Mg) leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Axinite-(Mg) typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: brown, violet, yellow, gray.
- 5Look at form & habitCrystal system: triclinic. Typical habit: wedge-shaped or tabular crystals with sharp edges.
Often confused with
Axinite-(Mg) vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside axinite-(mg)
Minerals reported to co-occur with axinite-(mg). Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Ca₂MgAl₂BSi₄O₁₅OH
- Mohs hardness
- 6.5-7
- Density
- 3.18-3.24 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Transparent
- Crystal system
- Triclinic
- Crystal habit
- Wedge-shaped or Tabular Crystals with Sharp Edges
- Cleavage
- Good in One Direction
- Rarity
- Rare
- Uses
- Collector, Gemstone
- Host rock
- Contact Metamorphic Zones and Hydrothermal Veins
- Typical price
- $20-200 for specimens depending on crystal clarity and size
Where rockhounds find axinite-(mg)
Classic worldwide localities
- Loma Larga, Baja California, Mexico
- Merelani Hills, Tanzania
- Madagascar
- France
Field-hunting tip
Look in contact metamorphic zones and hydrothermal veins country — that is the host setting where axinite-(mg) typically forms. If you start seeing calcite, quartz, dolomite in float, you are in the right ground. Field specimens usually show a wedge-shaped or tabular crystals with sharp edges habit, so train your eye for that shape before scanning the outcrop.







