Stavelotite-(La) is an extremely rare copper-lanthanum silicate mineral first identified in the Stavelot Massif of Belgium. It typically occurs as small, brownish platy crystals associated with manganese-rich mineral assemblages. Due to its rarity and limited locality, it is highly sought after by advanced systematic mineral collectors.
Is this stavelotite-(la)?
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 stavelotite-(la) with a known reference. Stavelotite-(La) sits at Mohs 5 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Stavelotite-(La) leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Stavelotite-(La) typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: yellowish-brown, brown.
- 5Look at form & habitCrystal system: trigonal. Typical habit: platy crystals, granular aggregates.
Often found alongside stavelotite-(la)
Minerals reported to co-occur with stavelotite-(la). Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- CuLa₄Al₃(Si₂O₇)(SiO₄)₃(OH)₃
- Mohs hardness
- 5
- Density
- 4.21 g/cm³
- Colors
- Streak
- White
- Luster
- Vitreous
- Transparency
- Translucent
- Crystal system
- Trigonal
- Crystal habit
- Platy Crystals, Granular Aggregates
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Metamorphic Rocks, Specifically Manganese-rich Deposits in The Stavelot Massif
- Typical price
- $100-500+ for rare micro specimens
Where rockhounds find stavelotite-(la)
Classic worldwide localities
- Stavelot Massif, Belgium
Field-hunting tip
Look in metamorphic rocks, specifically manganese-rich deposits in the stavelot massif country — that is the host setting where stavelotite-(la) typically forms. If you start seeing quartz, chlorite, hematite in float, you are in the right ground. Field specimens usually show a platy crystals, granular aggregates habit, so train your eye for that shape before scanning the outcrop.



