Jasmundite is a rare calcium-iron silicate mineral discovered in the combustion metamorphic rocks of the Jasmund cliff on Rügen Island. It typically occurs as minute anhedral grains within rocks formed by the burning of bituminous marls, making it a highly localized curiosity for advanced mineral collectors.
Is this jasmundite?
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 jasmundite with a known reference. Jasmundite sits at Mohs ~5, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Streak: white.
- 3Read the lusterHold the specimen under a strong light. Luster: resinous.
- 4Match the color rangeCompare against the expected color range: brownish green, greenish brown, dark brown.
- 5Look at form & habitCrystal system: tetragonal. Typical habit: anhedral grains.
Often confused with
Jasmundite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside jasmundite
Minerals reported to co-occur with jasmundite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Ca₁₁O₂(SiO₄)₄S
- Mohs hardness
- ~5
- Density
- 3.03 g/cm³
- Streak
- White
- Luster
- Resinous
- Transparency
- Semitransparent
- Crystal system
- Tetragonal
- Crystal habit
- Anhedral grains
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- In metamorphosed limestone inclusions in basalt
Where rockhounds find jasmundite
Classic worldwide localities
- Bellerberg volcano, two km north of Mayen, Eifel district, Germany
Field-hunting tip
Where it forms: In metamorphosed limestone inclusions in basalt. If you start seeing mayenite, brownmillerite, larnite in float, you are in the right ground. Typical habit: anhedral grains. Train your eye for that shape before scanning the outcrop.





