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 6-6.5, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Streak: pale yellow.
- 3Read the lusterHold the specimen under a strong light. Luster: vitreous, inclining to resinous, dull, and greasy.
- 4Match the color rangeCompare against the expected color range: yellow, dark yellow, gray, brown.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: granular, prismatic, tabular.
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
- Na₂Ca₄Zr(Nb,Ti)(Si₂O₇)₂(O,F)₄
- Mohs hardness
- 6-6.5
- Density
- 3.40-3.44 g/cm³
- Streak
- Pale yellow
- Luster
- Vitreous, inclining to resinous, dull, and greasy
- Transparency
- Transparent to translucent
- Crystal system
- Monoclinic
- Crystal habit
- Granular, prismatic, tabular
- Cleavage
- {010}, distinct; {100} and {110}, poor
- Rarity
- Rare
- Uses
- Collector
- Host rock
- A late phase in alkalic pegmatites; an accessory mineral in nepheline syenites; in fenites associated with alkaline intrusives; and in carbonatites
Where rockhounds find wöhlerite
Classic worldwide localities
- Red Hill, Moultonborough, Carroll Co., New Hampshire, and Magnet Cove, Hot Spring Co., Arkansas, USA
- A number of islands in the Langesundsfjord, around Brevik, and at Tvedalen, Norway
- Khibiny and Lovozero massifs, Kola Peninsula, Russia
- Siberia, in the Burpala massif, about 120 km north of Lake Baikal, at Zaangar'ya, Yenisei Ridge, and in the Sangilene massif, Russia
- Kruft and Mendig, Eifel district, Germany
- Mont Saint-Hilaire and Oka, Quebec, Canada
Field-hunting tip
Where it forms: A late phase in alkalic pegmatites; an accessory mineral in nepheline syenites; in fenites associated with alkaline intrusives; and in carbonatites. If you start seeing cancrinite, ferro-hornblende, aegirine in float, you are in the right ground. Typical habit: granular, prismatic, tabular. Train your eye for that shape before scanning the outcrop.







