Eifelite is an exceptionally rare member of the osumilite group, typically found as microscopic prismatic crystals within volcanic rocks. It is most recognized from its type locality in the Eifel volcanic region of Germany, often occurring alongside sanidine and other volcanic minerals.
Is this eifelite?
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 eifelite with a known reference. Eifelite sits at Mohs 5-6, 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: vitreous.
- 4Match the color rangeCompare against the expected color range: colorless, light green, light greenish yellow, light yellow.
- 5Look at form & habitCrystal system: hexagonal. Typical habit: prismatic crystals.
Often confused with
Eifelite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside eifelite
Minerals reported to co-occur with eifelite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- KNa₂(MgNa)(Mg₃Si₁₂)O₃₀
- Mohs hardness
- 5-6
- Density
- 2.67 g/cm³
- Colors
- Streak
- White
- Luster
- Vitreous
- Transparency
- Transparent
- Crystal system
- Hexagonal
- Crystal habit
- Prismatic crystals
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- In vesicles in contact metamorphosed basement gneiss xenoliths in leucite tephrite
Where rockhounds find eifelite
Classic worldwide localities
- Bellerberg volcano, two km north of Mayen, Eifel district, Germany
Field-hunting tip
Where it forms: In vesicles in contact metamorphosed basement gneiss xenoliths in leucite tephrite. If you start seeing tridymite, hematite, pseudobrookite in float, you are in the right ground. Typical habit: prismatic crystals. Train your eye for that shape before scanning the outcrop.








