Schlegelite is a very rare lead arsenic molybdate mineral known primarily from the historic Schneeberg mining district in Germany. It typically forms small, clear to white tabular crystals that are difficult to distinguish from associated species like wulfenite without chemical analysis.
Is this schlegelite?
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 schlegelite with a known reference. Schlegelite sits at Mohs 3.5 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Schlegelite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Schlegelite typically shows a adamantine luster.
- 4Match the color rangeCompare against the expected color range: white, colorless, yellowish-white.
- 5Look at form & habitCrystal system: tetragonal. Typical habit: tabular crystals.
Often confused with
Schlegelite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside schlegelite
Minerals reported to co-occur with schlegelite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Pb₇(AsO₄)₂(MoO₄)₂
- Mohs hardness
- 3.5
- Density
- 5.68 g/cm³
- Streak
- White
- Luster
- Adamantine
- Transparency
- Transparent
- Crystal system
- Tetragonal
- Crystal habit
- Tabular Crystals
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector, Scientific Research
- Host rock
- Hydrothermal Veins
- Typical price
- $50-500 depending on specimen quality
Where rockhounds find schlegelite
Classic worldwide localities
- Schneeberg, Saxony, Germany
Field-hunting tip
Look in hydrothermal veins country — that is the host setting where schlegelite typically forms. If you start seeing wulfenite, mimetite, quartz in float, you are in the right ground. Field specimens usually show a tabular crystals habit, so train your eye for that shape before scanning the outcrop.



