Schüllerite is a rare barium sodium titanium silicate, typically brown. It is a late pneumatolitic mineral in miarolitic cavities in alkaline basalt. Associated minerals include nepheline, leucite, augite and phlogopite. It was first described from the Löhley quarry near Üdersdorf, Eifel volcanic region, Rheinland-Pfalz, Germany.
Is this schüllerite?
4-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 schüllerite with a known reference. Schüllerite sits at Mohs 3-4, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Schüllerite leaves a white streak.
- 3Match the color rangeCompare against the expected color range: brown.
- 4Look at form & habitCrystal system: triclinic. Typical habit: flattened crystals to 2 mm.
Often confused with
Schüllerite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside schüllerite
Minerals reported to co-occur with schüllerite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Ba₂Na(Mn,Ca)(Fe³⁺,Mg,Fe²⁺)₂Ti₂(Si₂O₇)₂(O,F)₄
- Mohs hardness
- 3-4
- Density
- 3.974 g/cm³
- Colors
- Streak
- White
- Transparency
- Translucent
- Crystal system
- Triclinic
- Crystal habit
- Flattened Crystals to 2 Mm
- Cleavage
- Perfect On {001}
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Skarn Deposits
Where rockhounds find schüllerite
Classic worldwide localities
- Schwarzenberg, Germany
- Kola Peninsula, Russia
- San Benito County, California
Field-hunting tip
Look in skarn deposits country, the host setting where schüllerite typically forms. If you start seeing calcite, diopside, epidote in float, you are in the right ground. Field specimens usually show a flattened crystals to 2 mm habit, so train your eye for that shape before scanning the outcrop.





