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, 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.






