Wöhlerite is a rare sorosilicate mineral primarily found in alkaline igneous environments like nepheline syenite pegmatites. It is prized by collectors for its distinctive honey-yellow to orange tabular crystals, often occurring in complex alkaline massifs associated with rare zirconium minerals.
Is this wöhlerite?
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 wöhlerite with a known reference. Wöhlerite sits at Mohs 5.5-6, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Wöhlerite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Wöhlerite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: yellow, brown, orange, colorless.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: tabular crystals, prismatic, bladed.
Often confused with
Wöhlerite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside wöhlerite
Minerals reported to co-occur with wöhlerite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- NaCa₂Zr(Si₂O₇)(F,O)₂
- Mohs hardness
- 5.5-6
- Density
- 3.4 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Translucent
- Crystal system
- Monoclinic
- Crystal habit
- Tabular Crystals, Prismatic, Bladed
- Cleavage
- Distinct On {100}
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Alkaline Igneous Rocks, Nepheline Syenites, Pegmatites
- Typical price
- $20-150 for micro to thumbnail specimens
Where rockhounds find wöhlerite
Classic worldwide localities
- Langesundsfjord, Norway
- Khibiny Massif, Russia
- Mont Saint-Hilaire, Canada
- Ilimaussaq Complex, Greenland
Field-hunting tip
Look in alkaline igneous rocks, nepheline syenites, pegmatites country, the host setting where wöhlerite typically forms. If you start seeing nepheline, aegirine, eudialyte in float, you are in the right ground. Field specimens usually show a tabular crystals, prismatic, bladed habit, so train your eye for that shape before scanning the outcrop.






