Eggletonite is a rare manganese silicate mineral that typically appears as brown to reddish-brown tabular crystals or massive grains. It is structurally related to the pyrosmalite group and is most famous for its occurrences in specific alkaline igneous environments. Collectors prize it primarily for its distinct crystal habits and association with rare-earth mineral assemblages.
Is this eggletonite?
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 eggletonite with a known reference. Eggletonite 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. Eggletonite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Eggletonite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: brown, reddish-brown.
- 5Look at form & habitCrystal system: trigonal. Typical habit: tabular crystals, massive, granular.
Often confused with
Eggletonite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside eggletonite
Minerals reported to co-occur with eggletonite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- (Na,Ca,K)₈(Mn,Fe,Mg,Zn)₈(Si,Al)₁₂O₃₀(OH,F)₁₀·4H₂O
- Mohs hardness
- 3-4
- Density
- 3.0-3.1 g/cm³
- Colors
- Streak
- White
- Luster
- Vitreous
- Transparency
- Translucent
- Crystal system
- Trigonal
- Crystal habit
- Tabular Crystals, Massive, Granular
- Cleavage
- Perfect Basal
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Nepheline Syenite Pegmatites, Hydrothermal Veins
- Typical price
- $50-300 per specimen depending on size and quality
Where rockhounds find eggletonite
Classic worldwide localities
- Big Rock Quarry, Arkansas, USA
- Franklin, New Jersey, USA
- Khibiny Massif, Russia
Field-hunting tip
Look in nepheline syenite pegmatites, hydrothermal veins country — that is the host setting where eggletonite typically forms. If you start seeing aegirine, microcline, pectolite 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.




