Norbergite is a member of the humite group typically found in contact-metamorphosed limestone or dolomitic marbles. It is most easily identified in the field by its distinct bright yellow fluorescence under shortwave ultraviolet light.
Is this norbergite?
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 norbergite with a known reference. Norbergite 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. Norbergite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Norbergite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: yellow, orange, brown, colorless.
- 5Look at form & habitCrystal system: orthorhombic. Typical habit: granular, massive, or small stubby prismatic crystals.
Often confused with
Norbergite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside norbergite
Minerals reported to co-occur with norbergite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Mg₃(SiO₄)(F,OH)₂
- Mohs hardness
- 6-6.5
- Density
- 3.15-3.20 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Transparent
- Crystal system
- Orthorhombic
- Crystal habit
- Granular, Massive, Or Small Stubby Prismatic Crystals
- Cleavage
- Poor in One Direction
- Fluorescence
- Bright Yellow Under SW UV
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Metamorphosed Limestones and Marbles
- Typical price
- $20-150 for specimens depending on size and quality
Where rockhounds find norbergite
Classic worldwide localities
- Norberg, Sweden
- Franklin, New Jersey, USA
- Amity, New York, USA
- Sahara Desert, Algeria
Field-hunting tip
Look in metamorphosed limestones and marbles country — that is the host setting where norbergite typically forms. If you start seeing calcite, dolomite, phlogopite in float, you are in the right ground. Field specimens usually show a granular, massive, or small stubby prismatic crystals habit, so train your eye for that shape before scanning the outcrop.








