Hejtmanite is a rare manganese-bearing silicate mineral belonging to the bafertisite group. It typically occurs as small brown lamellar or tabular crystals within alkaline syenite pegmatites, often identified by its distinct cleavage and associations with other rare-earth minerals.
Is this hejtmanite?
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 hejtmanite with a known reference. Hejtmanite 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: brownish yellow.
- 3Read the lusterHold the specimen under a strong light. Luster: vitreous.
- 4Match the color rangeCompare against the expected color range: golden yellow, orange brown.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: lamellar to tabular crystals.
Often confused with
Hejtmanite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside hejtmanite
Minerals reported to co-occur with hejtmanite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Ba₂Mn₄Ti(Si₂O₇)₂O₂(OH,F)₂
- Mohs hardness
- 4.5
- Density
- 3.97-4.06 g/cm³
- Streak
- Brownish yellow
- Luster
- Vitreous
- Transparency
- Transparent to translucent
- Crystal system
- Monoclinic
- Crystal habit
- Lamellar to tabular crystals
- Cleavage
- Perfect on {100}; poor parting on f0klg
- Rarity
- Rare
- Uses
- Collector
- Host rock
- In arfvedsonite veins in pegmatite cutting alkalic granite and syenite (Mbolwe Hill, Zambia)
Where rockhounds find hejtmanite
Classic worldwide localities
- Mbolwe Hill, Mkushi River area, Central Province, Zambia
- Dara-i-Pioz massif, Alai Range, Tien Shan, Tajikistan
Field-hunting tip
Where it forms: In arfvedsonite veins in pegmatite cutting alkalic granite and syenite (Mbolwe Hill, Zambia). If you start seeing manganoan arfvedsonite, albite, bastnäsite in float, you are in the right ground. Typical habit: lamellar to tabular crystals. Train your eye for that shape before scanning the outcrop.






