Ferrobustamite is a member of the wollastonite group characterized by its iron-rich composition. It typically occurs in skarn deposits formed through the contact metamorphism of impure limestones, often appearing as fibrous or granular masses that can be difficult to distinguish from common wollastonite without chemical testing.
Is this ferrobustamite?
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 ferrobustamite with a known reference. Ferrobustamite sits at Mohs 5.5-6 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Ferrobustamite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Ferrobustamite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: white, yellowish, brownish, colorless.
- 5Look at form & habitCrystal system: triclinic. Typical habit: fibrous, massive, or as tabular crystals.
Often confused with
Ferrobustamite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside ferrobustamite
Minerals reported to co-occur with ferrobustamite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- CaFeSi₂O₆
- Mohs hardness
- 5.5-6
- Density
- 3.5-3.6 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Translucent
- Crystal system
- Triclinic
- Crystal habit
- Fibrous, Massive, Or as Tabular Crystals
- Cleavage
- Perfect in Two Directions
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Metamorphosed Limestone or Skarn Deposits
- Typical price
- $20-100 per specimen depending on size
Where rockhounds find ferrobustamite
Classic worldwide localities
- Broken Hill, Australia
- Franklin, New Jersey, USA
- Kalkar Quarry, California, USA
- Vesuvius, Italy
Field-hunting tip
Look in metamorphosed limestone or skarn deposits country — that is the host setting where ferrobustamite typically forms. If you start seeing calcite, andradite, diopside in float, you are in the right ground. Field specimens usually show a fibrous, massive, or as tabular crystals habit, so train your eye for that shape before scanning the outcrop.






