Lüneburgite is a rare magnesium borophosphate mineral typically found in saline evaporite deposits. Collectors should look for its characteristic clear, tabular crystals or radial clusters embedded in salt-bearing sediments.
Is this lüneburgite?
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 lüneburgite with a known reference. Lüneburgite sits at Mohs 2, 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: colorless, white, brownish white, green.
- 5Look at form & habitCrystal system: triclinic. Typical habit: tabular crystals, radial aggregates, crusts.
Often confused with
Lüneburgite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside lüneburgite
Minerals reported to co-occur with lüneburgite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Mg₃[B₂(OH)₆(PO₄)₂](H₂O)₆
- Mohs hardness
- 2
- Density
- 2.05 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Translucent
- Crystal system
- Triclinic
- Crystal habit
- Tabular crystals, radial aggregates, crusts
- Cleavage
- On {010}, fair
- Rarity
- Rare
- Uses
- Collector
- Host rock
- In marine evaporite sequences
Where rockhounds find lüneburgite
Classic worldwide localities
- Permian Basin, around Carlsbad, Eddy Co., New Mexico and into Culbertson Co., Texas, USA
- Liineburg, 40 km south-southeast of Hannover, Lower Saxony, Germany
- Bela Stena, Serbia
- Kerch, Crimean Peninsula, Ukraine
- Kara-Bogaz-Gol and Uzun-Su, Turkmenistan
- Mejillones, Tarapaca, Chile
Field-hunting tip
Where it forms: In marine evaporite sequences. If you start seeing boracite, gypsum, colemanite in float, you are in the right ground. Typical habit: tabular crystals, radial aggregates, crusts. Train your eye for that shape before scanning the outcrop.







