Charmarite is a rare member of the hydrotalcite group, typically orange-brown to pale brown. It occurs in silicate and carbonate cavities and in pegmatites cutting nepheline syenite, and is the manganese-dominant analogue of quintinite. It is prized by advanced collectors of microminerals.
Is this charmarite?
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 charmarite with a known reference. Charmarite sits at Mohs ~3, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Streak: white.
- 3Read the lusterHold the specimen under a strong light. Luster: adamantine.
- 4Match the color rangeCompare against the expected color range: colorless, yellow.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: platy crystals, granular aggregates.
Often confused with
Charmarite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside charmarite
Minerals reported to co-occur with charmarite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Mn²⁺₄Al₂(CO₃)(OH)₁₂·3H₂O
- Mohs hardness
- ~3
- Density
- 6.30-6.49 g/cm³
- Streak
- White
- Luster
- Adamantine
- Transparency
- Transparent
- Crystal system
- Monoclinic
- Crystal habit
- Platy crystals, granular aggregates
- Cleavage
- {100} and {010}
- Rarity
- Rare
- Uses
- Collector
- Host rock
- In the oxidized zone of a lead-bearing U–V deposit (Mounana mine, Gabon)
Where rockhounds find charmarite
Classic worldwide localities
- Mounana uranium mine, Franceville, Gabon
- Kusu deposit, 85 km south of Kinshasa, Bas-Congo Province, Congo (Bas-Zaire Province, Zaire)
- St. Andreasberg, Harz Mountains, Germany
- Found at Vrančice, near Příbram, Czech Republic
Field-hunting tip
Where it forms: In the oxidized zone of a lead-bearing U–V deposit (Mounana mine, Gabon). If you start seeing francevillite, wulfenite in float, you are in the right ground. Typical habit: platy crystals, granular aggregates. Train your eye for that shape before scanning the outcrop.



