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 5.5-6, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Streak: white.
- 3Read the lusterHold the specimen under a strong light. Luster: vitreous, pearly on {010} cleavage.
- 4Match the color rangeCompare against the expected color range: violet pink.
- 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
- Na₄CaSi₆O₁₄(OH)₂
- Mohs hardness
- 5.5-6
- Density
- 2.55 g/cm³
- Colors
- Violet pink
- Streak
- White
- Luster
- Vitreous, pearly on {010} cleavage
- Transparency
- Transparent
- Crystal system
- Orthorhombic
- Crystal habit
- Tabular crystals, massive, granular
- Cleavage
- Good on {010}; poor on {101}, intersecting at 83°
- Fluorescence
- Bright white under SW UV
- Rarity
- Rare
- Uses
- Collector
- Host rock
- As patches, streaks, and veinlets cutting arfvedsonite-bearing nepheline syenite; probably of late-stage hydrothermal origin
Where rockhounds find kvanefjeldite
Classic worldwide localities
- On the Kvanefjeld Plateau, in the Ilimaussaq intrusion, southern Greenland (type locality)
Field-hunting tip
Where it forms: As patches, streaks, and veinlets cutting arfvedsonite-bearing nepheline syenite; probably of late-stage hydrothermal origin. If you start seeing villiaumite, analcime in float, you are in the right ground. Typical habit: tabular crystals, massive, granular. Train your eye for that shape before scanning the outcrop.




