Kvanefjeldite is a rare phyllosilicate mineral found primarily in the unique agpaitic rocks of the Ilimaussaq complex in Greenland. It is highly valued by collectors for its brilliant white fluorescence under short-wave ultraviolet light and its tight association with other exotic alkaline minerals.
Is this kvanefjeldite?
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 kvanefjeldite with a known reference. Kvanefjeldite 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. Kvanefjeldite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Kvanefjeldite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: pink, brown, white.
- 5Look at form & habitCrystal system: orthorhombic. Typical habit: tabular crystals, massive, granular.
Often confused with
Kvanefjeldite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside kvanefjeldite
Minerals reported to co-occur with kvanefjeldite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Na₄(Mn,Fe)Si₄O₁₀·H₂O
- Mohs hardness
- 3-4
- Density
- 2.44 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Translucent
- Crystal system
- Orthorhombic
- Crystal habit
- Tabular Crystals, Massive, Granular
- Cleavage
- Perfect
- Fluorescence
- Bright White Under SW UV
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Agpaitic Nepheline Syenites
- Typical price
- $50-300 per specimen
Where rockhounds find kvanefjeldite
Classic worldwide localities
- Ilimaussaq Complex, Greenland
Field-hunting tip
Look in agpaitic nepheline syenites country — that is the host setting where kvanefjeldite typically forms. If you start seeing eudialyte, steenstrupine-(ce), arfvedsonite in float, you are in the right ground. Field specimens usually show a tabular crystals, massive, granular habit, so train your eye for that shape before scanning the outcrop.





