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.

Hardness
6
Mohs
Luster
Vitreous
Streak
White
Transparency
Semitransparent

Is this ferrobustamite?

5-step field check

Run through these checks against the specimen in your hand. The more boxes tick, the more confident the ID.

  • 1
    Test the hardness
    Try to scratch ferrobustamite with a known reference. Ferrobustamite sits at Mohs 6, softer than the next harder reference, harder than the previous one.
  • 2
    Check the streak
    Drag the specimen across an unglazed porcelain plate. Streak: white.
  • 3
    Read the luster
    Hold the specimen under a strong light. Luster: vitreous.
  • 4
    Match the color range
    Compare against the expected color range: green.
  • 5
    Look at form & habit
    Crystal system: triclinic. Typical habit: massive.

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
6
Density
3.09 g/cm³
Colors
Streak
White
Luster
Vitreous
Transparency
Semitransparent
Crystal system
Triclinic
Crystal habit
Massive
Cleavage
{100}, perfect; {110}, {110}, good
Rarity
Rare
Uses
Collector
Host rock
Surrounding chert nodules in a skarn in dolostone (Isle of Skye, Scotland)

Where rockhounds find ferrobustamite

Classic worldwide localities

  • Camas Malag, Isle of Skye, Scotland
  • Scawt Hill, near Larne, Co. Antrim, Ireland
  • Kagata, Ofuku, and Ohta mines, Yamaguchi Prefecture, Japan
  • Kasugayama and Tsuchiarashi deposits, near Iida, Nagano Prefecture, Japan
  • Kurodaké Peak, near Toyama, Yoyama Prefecture, Japan
  • Tsumo mine, Shimane Prefecture, Japan

Field-hunting tip

Where it forms: Surrounding chert nodules in a skarn in dolostone (Isle of Skye, Scotland). If you start seeing hedenbergite, grossular-andradite in float, you are in the right ground. Typical habit: massive. Train your eye for that shape before scanning the outcrop.

Common questions

How do you identify ferrobustamite?+
Mohs hardness is 6. Luster: vitreous. The streak is white. Common colors include green.
Where is ferrobustamite found?+
Notable localities include Camas Malag, Isle of Skye, Scotland; Scawt Hill, near Larne, Co. Antrim, Ireland; Kagata, Ofuku, and Ohta mines, Yamaguchi Prefecture, Japan; Kasugayama and Tsuchiarashi deposits, near Iida, Nagano Prefecture, Japan; Kurodaké Peak, near Toyama, Yoyama Prefecture, Japan.
What rocks look like ferrobustamite?+
Ferrobustamite is most often confused with Wollastonite, Pectolite, Pyroxferroite. A quick hardness test and a streak check separate the look-alikes faster than color alone.
What minerals are found with ferrobustamite?+
Ferrobustamite commonly co-occurs with Hedenbergite, Grossular-andradite. Spotting any of these in float or country rock is a useful trip signal.
What kind of rock does ferrobustamite form in?+
Where it forms: Surrounding chert nodules in a skarn in dolostone (Isle of Skye, Scotland). Working float back to the host body is the standard way to chase a fresh occurrence.
What is ferrobustamite used for?+
Ferrobustamite is used in collector.

Find ferrobustamite on the map

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