Amesite is a relatively rare member of the chlorite group, typically occurring as small, pearly, pseudohexagonal plates. It is best identified by its association with altered ultramafic rocks and its distinct micaceous habit compared to more common chlorite species.
Is this amesite?
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 amesite with a known reference. Amesite 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. Amesite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Amesite typically shows a pearly luster.
- 4Match the color rangeCompare against the expected color range: white, green, pink, red.
- 5Look at form & habitCrystal system: triclinic. Typical habit: pseudohexagonal platy crystals, micaceous aggregates.
Often confused with
Amesite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside amesite
Minerals reported to co-occur with amesite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Mg₂Al(SiAl)O₅(OH)₄
- Mohs hardness
- 2.5-3
- Density
- 2.7-2.9 g/cm³
- Streak
- White
- Luster
- Pearly
- Transparency
- Translucent
- Crystal system
- Triclinic
- Crystal habit
- Pseudohexagonal Platy Crystals, Micaceous Aggregates
- Cleavage
- Perfect Basal
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Metamorphic Rocks, Specifically Contact Metamorphic Zones and Hydrothermal Veins
- Typical price
- $20-150 thumbnail specimens
Where rockhounds find amesite
Classic worldwide localities
- Chester, Massachusetts, USA
- Sarany, Ural Mountains, Russia
- Val di Vizze, Italy
- Lac Nicolet, Quebec, Canada
Field-hunting tip
Look in metamorphic rocks, specifically contact metamorphic zones and hydrothermal veins country — that is the host setting where amesite typically forms. If you start seeing magnetite, calcite, diopside in float, you are in the right ground. Field specimens usually show a pseudohexagonal platy crystals, micaceous aggregates habit, so train your eye for that shape before scanning the outcrop.







