Danalite is a rare beryllium silicate that typically forms as reddish-brown to pinkish tetrahedral crystals. It is most frequently found in complex granite pegmatites and contact metamorphic zones, often requiring professional analysis to distinguish it from other members of the helvine group.
Is this danalite?
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 danalite with a known reference. Danalite 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. Danalite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Danalite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: red, reddish-brown, yellow, pink.
- 5Look at form & habitCrystal system: isometric. Typical habit: tetrahedral crystals, massive, granular.
Often confused with
Danalite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside danalite
Minerals reported to co-occur with danalite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- (Fe,Zn,Mn)₄Be₃(SiO₄)₃S
- Mohs hardness
- 5.5-6
- Density
- 3.3-3.4 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Translucent
- Crystal system
- Isometric
- Crystal habit
- Tetrahedral Crystals, Massive, Granular
- Cleavage
- Poor
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Granite Pegmatites, Contact Metamorphic Rocks
- Typical price
- $20-150 thumbnail, $200+ cabinet specimen
Where rockhounds find danalite
Classic worldwide localities
- Gloucester, Massachusetts, USA
- Iron Mountain, New Mexico, USA
- Sweden
- Russia
- Canada
Field-hunting tip
Look in granite pegmatites, contact metamorphic rocks country — that is the host setting where danalite typically forms. If you start seeing magnetite, fluorite, quartz in float, you are in the right ground. Field specimens usually show a tetrahedral crystals, massive, granular habit, so train your eye for that shape before scanning the outcrop.







