Kuzelite is a rare layered double hydroxide mineral typically found in environments associated with the hydration of industrial waste like blast furnace slag or concrete. Collectors should look for delicate, white to colorless hexagonal plates or radiating rosettes in cavities of anthropogenic materials. It is a scientifically significant mineral for understanding mineral crystallization in artificial geological settings.
Is this kuzelite?
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 kuzelite with a known reference. Kuzelite 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. Kuzelite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Kuzelite typically shows a pearly luster.
- 4Match the color rangeCompare against the expected color range: white, colorless, pale yellow.
- 5Look at form & habitCrystal system: trigonal. Typical habit: platy hexagonal crystals, rosettes, or incrustations.
Often confused with
Kuzelite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside kuzelite
Minerals reported to co-occur with kuzelite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Ca₄Al₂(OH)₁₂(SO₄)·6H₂O
- Mohs hardness
- 2
- Density
- 2.05 g/cm³
- Streak
- White
- Luster
- Pearly
- Transparency
- Translucent
- Crystal system
- Trigonal
- Crystal habit
- Platy Hexagonal Crystals, Rosettes, Or Incrustations
- Cleavage
- Perfect Basal
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Altered Calcium-rich Industrial Waste Sites, Cement Hydration Zones
- Typical price
- $20-100 per specimen
Where rockhounds find kuzelite
Classic worldwide localities
- Kuzel mine, Germany
- Cava del Ferro, Italy
- Upper Merion Township, USA
Field-hunting tip
Look in altered calcium-rich industrial waste sites, cement hydration zones country — that is the host setting where kuzelite typically forms. If you start seeing ettringite, portlandite, gypsum in float, you are in the right ground. Field specimens usually show a platy hexagonal crystals, rosettes, or incrustations habit, so train your eye for that shape before scanning the outcrop.





