Kottenheimite is a very rare hydrated calcium sulfate hydroxide mineral discovered in the volcanic fields of the Eifel region in Germany. It typically forms as delicate, white platy crystals or efflorescent crusts within cavities of volcanic rock. Due to its solubility and rarity, collectors should handle specimens with care and store them in stable, humidity-controlled conditions.
Is this kottenheimite?
4-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 kottenheimite with a known reference. Kottenheimite sits at Mohs 2-2.5, softer than the next harder reference, harder than the previous one.
- 2Read the lusterHold the specimen under a strong light. Luster: vitreous to silky (aggregates).
- 3Match the color rangeCompare against the expected color range: snow-white.
- 4Look at form & habitCrystal system: hexagonal. Typical habit: platy crystals, pseudohexagonal, efflorescent crusts.
Often confused with
Kottenheimite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside kottenheimite
Minerals reported to co-occur with kottenheimite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Ca₃Si(SO₄)₂(OH)₆·12H₂O
- Mohs hardness
- 2-2.5
- Density
- 1.92 g/cm³
- Colors
- Luster
- Vitreous to silky (aggregates)
- Transparency
- Translucent
- Crystal system
- Hexagonal
- Crystal habit
- Platy crystals, pseudohexagonal, efflorescent crusts
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- In miarolitic cavities in alkali basalt
Where rockhounds find kottenheimite
Classic worldwide localities
- Bellerberg, near Kottenheim, Eastern Eifel area, Rhineland-Palatinate (Rheinland-Pfalz), Germany
Field-hunting tip
Where it forms: In miarolitic cavities in alkali basalt. If you start seeing wollastonite, clinochlore, ellestadite in float, you are in the right ground. Typical habit: platy crystals, pseudohexagonal, efflorescent crusts. Train your eye for that shape before scanning the outcrop.






