Pyroaurite is a member of the hydrotalcite group typically found as pearly, platy crystals or foliated masses in metamorphic environments. It is often distinguished by its characteristic waxy to pearly luster and soft, flexible flakes when found in thin, hexagonal plates.
Is this pyroaurite?
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 pyroaurite with a known reference. Pyroaurite 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. Pyroaurite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Pyroaurite typically shows a pearly luster.
- 4Match the color rangeCompare against the expected color range: yellow, brown, white, orange, colorless.
- 5Look at form & habitCrystal system: trigonal. Typical habit: platy crystals, foliated masses, or hexagonal plates.
Often confused with
Pyroaurite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside pyroaurite
Minerals reported to co-occur with pyroaurite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Mg₆Fe₃⁺₂(OH)₁₆(CO₃)·4H₂O
- Mohs hardness
- 2.5
- Density
- 2.1-2.2 g/cm³
- Streak
- White
- Luster
- Pearly
- Transparency
- Translucent
- Crystal system
- Trigonal
- Crystal habit
- Platy Crystals, Foliated Masses, Or Hexagonal Plates
- Cleavage
- Perfect Basal
- Rarity
- Uncommon
- Uses
- Collector, Scientific Research
- Host rock
- Metamorphosed Limestones and Altered Mafic Rocks
- Typical price
- $10-60 for small specimens
Where rockhounds find pyroaurite
Classic worldwide localities
- Långban, Sweden
- Magnet Cove, USA
- Khibiny Massif, Russia
- Königsberg, Norway
Field-hunting tip
Look in metamorphosed limestones and altered mafic rocks country — that is the host setting where pyroaurite typically forms. If you start seeing brucite, calcite, aragonite in float, you are in the right ground. Field specimens usually show a platy crystals, foliated masses, or hexagonal plates habit, so train your eye for that shape before scanning the outcrop.







