Wilhelmgümbelite is a rare secondary phosphate mineral typically found as a result of the alteration of triphylite in granitic pegmatites. Collectors should look for small, delicate platy crystals or radiating sprays in the cavities of weathered phosphate zones. It is named in honor of the German geologist Wilhelm von Gümbel.
Is this wilhelmgümbelite?
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 wilhelmgümbelite with a known reference. Wilhelmgümbelite sits at Mohs 3-4 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Wilhelmgümbelite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Wilhelmgümbelite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: colorless, white, pale yellow.
- 5Look at form & habitCrystal system: triclinic. Typical habit: platy crystals, radial aggregates, crusts.
Often confused with
Wilhelmgümbelite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside wilhelmgümbelite
Minerals reported to co-occur with wilhelmgümbelite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- ZnFe²⁺(PO₄)₂·4H₂O
- Mohs hardness
- 3-4
- Density
- 3.1-3.2 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Transparent
- Crystal system
- Triclinic
- Crystal habit
- Platy Crystals, Radial Aggregates, Crusts
- Cleavage
- Perfect On {010}
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Phosphate-rich Granitic Pegmatites
- Typical price
- $50-500 thumbnail specimens
Where rockhounds find wilhelmgümbelite
Classic worldwide localities
- Hagendorf-South Pegmatite, Germany
- Tip Top Mine, South Dakota, USA
Field-hunting tip
Look in phosphate-rich granitic pegmatites country — that is the host setting where wilhelmgümbelite typically forms. If you start seeing triphylite, sicklerite, hureaulite in float, you are in the right ground. Field specimens usually show a platy crystals, radial aggregates, crusts habit, so train your eye for that shape before scanning the outcrop.





