Hydroscarbroite is a rare aluminum carbonate mineral typically found as white, chalky, or botryoidal coatings within clay-rich sedimentary environments. It is most easily identified by its soft, porcelain-like appearance and its association with other aluminum-rich secondary minerals in coastal cliff settings.
Is this hydroscarbroite?
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 hydroscarbroite with a known reference. Hydroscarbroite sits at Mohs 2-3 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Hydroscarbroite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Hydroscarbroite typically shows a dull luster.
- 4Match the color rangeCompare against the expected color range: white.
- 5Look at form & habitCrystal system: orthorhombic. Typical habit: massive, chalky, or botryoidal crusts.
Often confused with
Hydroscarbroite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside hydroscarbroite
Minerals reported to co-occur with hydroscarbroite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Al₁₄(CO₃)₃(OH)₃₆·n H₂O
- Mohs hardness
- 2-3
- Density
- 2.1-2.2 g/cm³
- Colors
- Streak
- White
- Luster
- Dull
- Transparency
- Opaque
- Crystal system
- Orthorhombic
- Crystal habit
- Massive, Chalky, Or Botryoidal Crusts
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Sedimentary Clay Beds and Fissures in Sandstone
- Typical price
- $20-100 per specimen
Where rockhounds find hydroscarbroite
Classic worldwide localities
- Scarborough, North Yorkshire, England
- Various clay-rich sedimentary deposits
Field-hunting tip
Look in sedimentary clay beds and fissures in sandstone country — that is the host setting where hydroscarbroite typically forms. If you start seeing kaolinite, gibbsite, allophane in float, you are in the right ground. Field specimens usually show a massive, chalky, or botryoidal crusts habit, so train your eye for that shape before scanning the outcrop.




