Ussingite is a rare sodium aluminosilicate mineral known primarily for its distinct violet to lavender coloration. It is most often found in alkaline igneous complexes, occurring as massive veins or granular aggregates that fluoresce strikingly under short-wave UV light.
Is this ussingite?
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 ussingite with a known reference. Ussingite sits at Mohs 6-7 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Ussingite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Ussingite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: violet, pink, lavender, colorless, white.
- 5Look at form & habitCrystal system: triclinic. Typical habit: massive, granular, or rarely as platy crystals.
Often confused with
Ussingite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside ussingite
Minerals reported to co-occur with ussingite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Na₂AlSi₃O₈(OH)
- Mohs hardness
- 6-7
- Density
- 2.56 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Translucent
- Crystal system
- Triclinic
- Crystal habit
- Massive, Granular, Or Rarely as Platy Crystals
- Cleavage
- Good in One Direction
- Fluorescence
- Bright Orange Under UV Light
- Rarity
- Rare
- Uses
- Collector, Mineralogical Study
- Host rock
- Alkaline Pegmatites
- Typical price
- $20-150 per specimen depending on size and intensity of color
Where rockhounds find ussingite
Classic worldwide localities
- Ilimaussaq Complex, Greenland
- Mont Saint-Hilaire, Canada
- Kola Peninsula, Russia
Field-hunting tip
Look in alkaline pegmatites country — that is the host setting where ussingite typically forms. If you start seeing sodalite, eudialyte, aegirine in float, you are in the right ground. Field specimens usually show a massive, granular, or rarely as platy crystals habit, so train your eye for that shape before scanning the outcrop.







