Hydrotalcite is a layered double hydroxide mineral typically forming soft, waxy or pearly masses and thin hexagonal plates. It is most commonly identified by its low hardness and association with serpentinite or contact-metamorphosed carbonate rocks. Collectors look for its characteristic micaceous habit and smooth, greasy feel.
Is this hydrotalcite?
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 hydrotalcite with a known reference. Hydrotalcite sits at Mohs 2 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Hydrotalcite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Hydrotalcite typically shows a pearly luster.
- 4Match the color rangeCompare against the expected color range: white, gray, pale green, pale yellow.
- 5Look at form & habitCrystal system: trigonal. Typical habit: tabular crystals, micaceous aggregates, massive.
Often confused with
Hydrotalcite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside hydrotalcite
Minerals reported to co-occur with hydrotalcite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Mg₆Al₂CO₃(OH)₁₆·4H₂O
- Mohs hardness
- 2
- Density
- 2.06-2.10 g/cm³
- Streak
- White
- Luster
- Pearly
- Transparency
- Translucent
- Crystal system
- Trigonal
- Crystal habit
- Tabular Crystals, Micaceous Aggregates, Massive
- Cleavage
- Perfect Basal
- Rarity
- Common
- Uses
- Collector, Scientific Research
- Host rock
- Metamorphosed Limestones and Dolomites, Ultramafic Rocks
- Typical price
- $10-50 thumbnail
Where rockhounds find hydrotalcite
Classic worldwide localities
- Snarum, Norway
- Bergslagen, Sweden
- Ural Mountains, Russia
- Val di Susa, Italy
- Amity, New York, USA
Field-hunting tip
Look in metamorphosed limestones and dolomites, ultramafic rocks country — that is the host setting where hydrotalcite typically forms. If you start seeing brucite, dolomite, calcite in float, you are in the right ground. Field specimens usually show a tabular crystals, micaceous aggregates, massive habit, so train your eye for that shape before scanning the outcrop.







