Stevensite is a rare, magnesium-rich member of the smectite clay group, typically forming as a secondary alteration product. It is characterized by its soft, soapy feel and dense, compact massive habit rather than visible crystals. Collectors often find it in evaporite deposits or as a replacement product in ultramafic rocks.
Is this stevensite?
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 stevensite with a known reference. Stevensite 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. Stevensite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Stevensite typically shows a dull luster.
- 4Match the color rangeCompare against the expected color range: white, gray, yellowish, pinkish.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: massive.
Often confused with
Stevensite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside stevensite
Minerals reported to co-occur with stevensite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Na₀.₃Mg₃Si₄O₁₀(OH)₂·n(H₂O)
- Mohs hardness
- 1-2
- Density
- 2.0-2.2 g/cm³
- Streak
- White
- Luster
- Dull
- Transparency
- Opaque
- Crystal system
- Monoclinic
- Crystal habit
- Massive
- Cleavage
- None
- Rarity
- Uncommon
- Uses
- Collector, Scientific Research
- Host rock
- Sedimentary Basins and Alteration Zones of Magnesium-rich Rocks
- Typical price
- $10-40 per specimen
Where rockhounds find stevensite
Classic worldwide localities
- Stevens Canyon, New Jersey, USA
- Amargosa Valley, Nevada, USA
- Kizil-Dere, Azerbaijan
- Akhaten, Mongolia
Field-hunting tip
Look in sedimentary basins and alteration zones of magnesium-rich rocks country — that is the host setting where stevensite typically forms. If you start seeing calcite, dolomite, serpentine 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.






