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, 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.






