Eastonite is a rare magnesium-rich mica belonging to the biotite group, often appearing as platy or foliated dark-colored crystals. It is predominantly found in contact-metamorphosed limestone or marble environments. Collectors prize it for its specific chemical composition which distinguishes it from more common phlogopite specimens.
Is this eastonite?
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 eastonite with a known reference. Eastonite sits at Mohs 2.5-3, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Eastonite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Eastonite typically shows a pearly luster.
- 4Match the color rangeCompare against the expected color range: dark brown, black, greenish-brown.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: platy crystals, foliated masses, micaceous aggregates.
Often confused with
Eastonite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside eastonite
Minerals reported to co-occur with eastonite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- KMg₃AlSi₃O₁₀(OH)₂
- Mohs hardness
- 2.5-3
- Density
- 2.9-3.2 g/cm³
- Streak
- White
- Luster
- Pearly
- Transparency
- Translucent
- Crystal system
- Monoclinic
- Crystal habit
- Platy Crystals, Foliated Masses, Micaceous Aggregates
- Cleavage
- Perfect Basal
- Rarity
- Rare
- Uses
- Collector, Research
- Host rock
- Metamorphosed Limestones and Marbles
- Typical price
- $10-50 per specimen
Where rockhounds find eastonite
Classic worldwide localities
- Monroe, New York, USA
- Grenville Province, Canada
- Kola Peninsula, Russia
Field-hunting tip
Look in metamorphosed limestones and marbles country, the host setting where eastonite typically forms. If you start seeing calcite, diopside, spinel in float, you are in the right ground. Field specimens usually show a platy crystals, foliated masses, micaceous aggregates habit, so train your eye for that shape before scanning the outcrop.







