Dypingite is a secondary magnesium carbonate mineral that typically forms as delicate white crusts or platy aggregates in weathered ultramafic environments. Collectors often find it as a fine-grained, chalky coating on serpentine rocks, where it is frequently misidentified as hydromagnesite.
Is this dypingite?
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 dypingite with a known reference. Dypingite 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. Dypingite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Dypingite typically shows a pearly luster.
- 4Match the color rangeCompare against the expected color range: white, colorless, pale blue.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: platy, foliated, or powdery crusts.
Often confused with
Dypingite vs. its common look-alikes, and how to tell them apart in the field.

How to tell apart: Hydromagnesite is the harder of the two (Mohs 3.5 vs. 2.5).

How to tell apart: Luster reads pearly on Dypingite and vitreous on Artinite.

How to tell apart: Magnesite is the harder of the two (Mohs 3.5-4.5 vs. 2.5); luster reads pearly on Dypingite and vitreous on Magnesite.
Often found alongside dypingite
Minerals reported to co-occur with dypingite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Mg₅(CO₃)₄(OH)₂·5H₂O
- Mohs hardness
- 2.5
- Density
- 2.16 g/cm³
- Streak
- White
- Luster
- Pearly
- Transparency
- Translucent
- Crystal system
- Monoclinic
- Crystal habit
- Platy, Foliated, Or Powdery Crusts
- Cleavage
- Perfect
- Fluorescence
- White to Light Blue Under SW UV
- Rarity
- Uncommon
- Uses
- Collector, Scientific Research
- Host rock
- Altered Ultramafic Rocks and Serpentinite
- Typical price
- $15-60 thumbnail
Where rockhounds find dypingite
Classic worldwide localities
- Dypingdal, Norway
- Sierra Nevada, Spain
- Woodsreef, Australia
- New Idria, USA
Field-hunting tip
Look in altered ultramafic rocks and serpentinite country, the host setting where dypingite typically forms. If you start seeing hydromagnesite, serpentine, brucite in float, you are in the right ground. Field specimens usually show a platy, foliated, or powdery crusts habit, so train your eye for that shape before scanning the outcrop.



