Margarite is a brittle mica that forms typically as platy, pearly aggregates in metamorphic environments. Unlike common micas, its sheets are brittle and do not flex or elasticize when bent, a key characteristic for field identification.
Is this margarite?
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 margarite with a known reference. Margarite 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. Margarite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Margarite typically shows a pearly luster.
- 4Match the color rangeCompare against the expected color range: pink, white, yellow, gray.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: tabular, micaceous plates.
Often confused with
Margarite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside margarite
Minerals reported to co-occur with margarite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- CaAl₂(Al₂Si₂)O₁₀(OH)₂
- Mohs hardness
- 3.5-4
- Density
- 3.0-3.1 g/cm³
- Streak
- White
- Luster
- Pearly
- Transparency
- Translucent
- Crystal system
- Monoclinic
- Crystal habit
- Tabular, Micaceous Plates
- Cleavage
- Perfect Basal
- Rarity
- Uncommon
- Uses
- Collector, Scientific Research
- Host rock
- Metamorphosed Limestone, Mica Schists, Chlorite Schists
- Typical price
- $10-60 per specimen
Where rockhounds find margarite
Classic worldwide localities
- Chester, Massachusetts, USA
- Sterzing, Italy
- Naxos, Greece
- Zillertal, Austria
Field-hunting tip
Look in metamorphosed limestone, mica schists, chlorite schists country — that is the host setting where margarite typically forms. If you start seeing corundum, diaspore, chlorite in float, you are in the right ground. Field specimens usually show a tabular, micaceous plates habit, so train your eye for that shape before scanning the outcrop.







