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. Streak: light brown.
- 3Read the lusterHold the specimen under a strong light. Luster: vitreous.
- 4Match the color rangeCompare against the expected color range: golden brown.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: acicular, prismatic, radial.
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,K,Ca)₂Mn₆(Si,Al)₁₀O₂₄(OH)₄·7-11H₂O
- Mohs hardness
- 3-4
- Density
- 2.76 g/cm³
- Colors
- Streak
- Light brown
- Luster
- Vitreous
- Transparency
- Semitransparent
- Crystal system
- Monoclinic
- Crystal habit
- Acicular, prismatic, radial
- Cleavage
- Perfect on {001}
- Rarity
- Rare
- Uses
- Collector
- Host rock
- In miarolitic pockets in nepheline syenite pegmatite
Where rockhounds find eggletonite
Classic worldwide localities
- Big Rock quarry, Granite Mountain, near Little Rock, Pulaski Co., Arkansas, USA
Field-hunting tip
Where it forms: In miarolitic pockets in nepheline syenite pegmatite. If you start seeing albite, natrolite, apophyllite in float, you are in the right ground. Typical habit: acicular, prismatic, radial. Train your eye for that shape before scanning the outcrop.






