Ephesite is a rare brittle mica that typically occurs as thin, platy crystals or foliated masses. It is primarily identified by its occurrence in specific metamorphic environments like emery deposits and its distinct association with corundum and diaspore.
Is this ephesite?
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 ephesite with a known reference. Ephesite sits at Mohs 3.5-4 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Ephesite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Ephesite typically shows a pearly luster.
- 4Match the color rangeCompare against the expected color range: white, pink, pale red, colorless.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: platy crystals, micaceous aggregates.
Often confused with
Ephesite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside ephesite
Minerals reported to co-occur with ephesite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- NaLiAl₂(Al₂Si₂)O₁₀(OH)₂
- Mohs hardness
- 3.5-4
- Density
- 3.06 g/cm³
- Streak
- White
- Luster
- Pearly
- Transparency
- Translucent
- Crystal system
- Monoclinic
- Crystal habit
- Platy Crystals, Micaceous Aggregates
- Cleavage
- Perfect Basal
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Metamorphic Rocks, Specifically Emery Deposits and Metamorphosed Limestones
- Typical price
- $20-150 for thumbnail to small cabinet specimens
Where rockhounds find ephesite
Classic worldwide localities
- Ephesus, Turkey
- Franklin, New Jersey, USA
- Jacupiranga, Brazil
- Sar-e-Sang, Afghanistan
Field-hunting tip
Look in metamorphic rocks, specifically emery deposits and metamorphosed limestones country — that is the host setting where ephesite typically forms. If you start seeing corundum, diaspore, chlorite in float, you are in the right ground. Field specimens usually show a platy crystals, micaceous aggregates habit, so train your eye for that shape before scanning the outcrop.







