Friedelite is a rare manganese silicate that typically forms in metamorphosed manganese-rich deposits. It is most recognizable by its distinct pink to brownish-red color and perfect basal cleavage, often appearing as tabular crystals or in massive form alongside other manganese minerals.
Is this friedelite?
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 friedelite with a known reference. Friedelite 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. Friedelite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Friedelite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: pink, brown, red.
- 5Look at form & habitCrystal system: trigonal. Typical habit: tabular crystals, massive, granular.
Often confused with
Friedelite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside friedelite
Minerals reported to co-occur with friedelite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Mn₈Si₆O₁₅(OH,Cl)₁₀
- Mohs hardness
- 4-5
- Density
- 3.04-3.13 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Translucent
- Crystal system
- Trigonal
- Crystal habit
- Tabular Crystals, Massive, Granular
- Cleavage
- Perfect Basal
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Metamorphosed Manganese Deposits
- Typical price
- $50-500 thumbnail
Where rockhounds find friedelite
Classic worldwide localities
- Harstigen Mine, Sweden
- Franklin, New Jersey, USA
- Sterling Hill, New Jersey, USA
- Val d'Err, Switzerland
Field-hunting tip
Look in metamorphosed manganese deposits country — that is the host setting where friedelite typically forms. If you start seeing andradite, calcite, hematite in float, you are in the right ground. Field specimens usually show a tabular crystals, massive, granular habit, so train your eye for that shape before scanning the outcrop.






