Pyrosmalite-(Fe) is a rare manganese-iron silicate typically found in skarn environments. Collectors prize it for its distinct, mica-like pearly luster on its perfect cleavage planes and its characteristic tabular hexagonal crystal habit.
Is this pyrosmalite-(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 pyrosmalite-(fe) with a known reference. Pyrosmalite-(Fe) sits at Mohs 4.5, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Streak: light green.
- 3Read the lusterHold the specimen under a strong light. Luster: vitreous.
- 4Match the color rangeCompare against the expected color range: green blackish, pale liver brown, gray.
- 5Look at form & habitCrystal system: hexagonal. Typical habit: massive, prismatic.
Often confused with
Pyrosmalite-(Fe) vs. its common look-alikes, and how to tell them apart in the field.

How to tell apart: Pyrosmalite-(Fe) is noticeably harder (Mohs 4.5 vs. 2.5-3); streak differs, so Pyrosmalite-(Fe) leaves light green, Biotite leaves white; luster reads vitreous on Pyrosmalite-(Fe) and splendent to submetallic, vitreous, pearly on cleavage on Biotite.

How to tell apart: Pyrosmalite-(Fe) is noticeably harder (Mohs 4.5 vs. 2-3); streak differs, so Pyrosmalite-(Fe) leaves light green, Phlogopite leaves white; luster reads vitreous on Pyrosmalite-(Fe) and pearly to submetallic on cleavage on Phlogopite.
Often found alongside pyrosmalite-(fe)
Minerals reported to co-occur with pyrosmalite-(fe). Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Fe₈Si₆O₁₅(OH)₁₀
- Mohs hardness
- 4.5
- Density
- 3.06-3.19 g/cm³
- Colors
- Streak
- Light green
- Luster
- Vitreous
- Transparency
- Semitransparent
- Crystal system
- Hexagonal
- Crystal habit
- Massive, prismatic
- Cleavage
- {0001}, good
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Intergrown with sulfdes, formed during metamorphism of a stratiform Pb-Zn deposit; a retrograde reaction product derived from clinopyroxene in saline fluid inclusions in contact metamorphic rocks
Where rockhounds find pyrosmalite-(fe)
Classic worldwide localities
- Pegmont lead-zinc deposit, 175 km southeast of Mt. Isa, Queensland, Australia
- Sudbury, Ontario and the PGE-Au-As deposits of the Thomson nickel belt, Manitoba
- Banská Štiavnica district, Slovakia
Field-hunting tip
Where it forms: Intergrown with sulfdes, formed during metamorphism of a stratiform Pb-Zn deposit; a retrograde reaction product derived from clinopyroxene in saline fluid inclusions in contact metamorphic rocks. If you start seeing fayalite, greenalite, galena in float, you are in the right ground. Typical habit: massive, prismatic. Train your eye for that shape before scanning the outcrop.






