Lemmleinite-Ba is a rare silicate mineral belonging to the labuntsovite group, typically occurring as small, honey-yellow to brownish prismatic crystals. It is primarily found in complex alkaline pegmatites where it forms as a late-stage crystallization product. Collectors prize it for its association with rare mineral suites found in sites like the Kola Peninsula and Mont Saint-Hilaire.
Is this lemmleinite-ba?
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 lemmleinite-ba with a known reference. Lemmleinite-Ba sits at Mohs 5.5, 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: vitreous.
- 4Match the color rangeCompare against the expected color range: bright orange, reddish orange, light coffee brown.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: aggregates, prismatic.
Often confused with
Lemmleinite-Ba vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside lemmleinite-ba
Minerals reported to co-occur with lemmleinite-ba. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Na₄K₄BaxTi₈(Si₄O₁₂)₄(O,OH)₈·8H₂O
- Mohs hardness
- 5.5
- Density
- 3.03 g/cm³
- Colors
- Streak
- White
- Luster
- Vitreous
- Transparency
- Transparent
- Crystal system
- Monoclinic
- Crystal habit
- Aggregates, prismatic
- Cleavage
- Imperfect
- Rarity
- Rare
- Uses
- Collector
- Host rock
- In alkaline pegmatites in an alkaline massif
Where rockhounds find lemmleinite-ba
Classic worldwide localities
- Kirovskii mine, Mt. Kukisvumchorr (type locality), Khibiny alkaline massif and at Mt. Karnasurt and Mt. Maly Punkaruaiv, Lovozero massif, Kola Peninsula, Russia
Field-hunting tip
Where it forms: In alkaline pegmatites in an alkaline massif. If you start seeing calcite, strontianite, aegirine in float, you are in the right ground. Typical habit: aggregates, prismatic. Train your eye for that shape before scanning the outcrop.








