Lourenswalsite is a rare potassium-barium niobium silicate mineral typically occurring as soft, pearly, micaceous flakes. It is most famous for its occurrences within the alkaline igneous rocks of the Magnet Cove complex in Arkansas. Collectors look for its distinctive platy habit and white color when inspecting microspecimens from rare-earth-bearing pegmatites.
Is this lourenswalsite?
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 lourenswalsite with a known reference. Lourenswalsite 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. Lourenswalsite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Lourenswalsite typically shows a pearly luster.
- 4Match the color rangeCompare against the expected color range: white, colorless.
- 5Look at form & habitCrystal system: hexagonal. Typical habit: platy crystals, micaceous aggregates.
Often confused with
Lourenswalsite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside lourenswalsite
Minerals reported to co-occur with lourenswalsite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- (K,Ba)₄(Nb,Ti)₅Si₄O₁₈(OH,F)·nH₂O
- Mohs hardness
- 2
- Density
- 2.33 g/cm³
- Streak
- White
- Luster
- Pearly
- Transparency
- Translucent
- Crystal system
- Hexagonal
- Crystal habit
- Platy Crystals, Micaceous Aggregates
- Cleavage
- Perfect Basal
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Nepheline Syenite
- Typical price
- $50-300 per specimen
Where rockhounds find lourenswalsite
Classic worldwide localities
- Magnet Cove, Arkansas, USA
Field-hunting tip
Look in nepheline syenite country — that is the host setting where lourenswalsite typically forms. If you start seeing potassium feldspar, aegirine, nepheline in float, you are in the right ground. Field specimens usually show a platy crystals, micaceous aggregates habit, so train your eye for that shape before scanning the outcrop.






