Aspidolite is a rare sodium-dominant member of the trioctahedral mica group, chemically analogous to phlogopite. It typically occurs as small, transparent, platy crystals in metamorphosed dolomitic marbles, often difficult to distinguish from common phlogopite without chemical analysis.
Is this aspidolite?
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 aspidolite with a known reference. Aspidolite sits at Mohs 2.5 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Aspidolite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Aspidolite typically shows a pearly luster.
- 4Match the color rangeCompare against the expected color range: colorless, pale yellow, brown, greenish.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: platy, micaceous, tabular crystals.
Often confused with
Aspidolite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside aspidolite
Minerals reported to co-occur with aspidolite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- NaMg₃(AlSi₃O₁₀)(OH)₂
- Mohs hardness
- 2.5
- Density
- 2.9-3.0 g/cm³
- Streak
- White
- Luster
- Pearly
- Transparency
- Transparent
- Crystal system
- Monoclinic
- Crystal habit
- Platy, Micaceous, Tabular Crystals
- Cleavage
- Perfect Basal
- Rarity
- Rare
- Uses
- Collector, Scientific Research
- Host rock
- Metamorphosed Dolomite Rocks
- Typical price
- $20-150 thumbnail to miniature
Where rockhounds find aspidolite
Classic worldwide localities
- Ticino, Switzerland
- Val Malenco, Italy
- Khibiny Massif, Russia
Field-hunting tip
Look in metamorphosed dolomite rocks country — that is the host setting where aspidolite typically forms. If you start seeing tremolite, diopside, calcite in float, you are in the right ground. Field specimens usually show a platy, micaceous, tabular crystals habit, so train your eye for that shape before scanning the outcrop.







