Montmorillonite is a soft clay mineral formed by the weathering of volcanic ash. It is widely known for its significant swelling properties when exposed to water, making it a primary component of bentonite clay.
Is this montmorillonite?
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 montmorillonite with a known reference. Montmorillonite sits at Mohs 1-2 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Montmorillonite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Montmorillonite typically shows a dull luster.
- 4Match the color rangeCompare against the expected color range: white, gray, yellow, pink, blue.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: massive.
Often confused with
Montmorillonite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside montmorillonite
Minerals reported to co-occur with montmorillonite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- (Na,Ca)₀.₃₃(Al,Mg)₂Si₄O₁₀(OH)₂·nH₂O
- Mohs hardness
- 1-2
- Density
- 2.0-2.7 g/cm³
- Streak
- White
- Luster
- Dull
- Transparency
- Opaque
- Crystal system
- Monoclinic
- Crystal habit
- Massive
- Cleavage
- Perfect
- Rarity
- Common
- Uses
- Industrial, Scientific, Cosmetic, Drilling Mud
- Host rock
- Altered Volcanic Ash Beds
- Typical price
- $5-20 per specimen
Where rockhounds find montmorillonite
Classic worldwide localities
- France
- USA
- Italy
- Greece
- Japan
Field-hunting tip
Look in altered volcanic ash beds country — that is the host setting where montmorillonite typically forms. If you start seeing calcite, gypsum, quartz in float, you are in the right ground. Field specimens usually show a massive habit, so train your eye for that shape before scanning the outcrop.







