Hydroxylgugiaite is an extremely rare beryllium-bearing silicate primarily found in the volcanic ejecta of the Eifel region in Germany. It typically occurs as small, transparent prismatic crystals within cavities of metamorphosed limestone xenoliths. Due to its scarcity and association with complex mineral assemblages, it is highly sought after by specialized systematic mineral collectors.
Is this hydroxylgugiaite?
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 hydroxylgugiaite with a known reference. Hydroxylgugiaite 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: vitreous.
- 4Match the color rangeCompare against the expected color range: colorless, white, pale gray.
- 5Look at form & habitCrystal system: tetragonal. Typical habit: prismatic crystals.
Often confused with
Hydroxylgugiaite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside hydroxylgugiaite
Minerals reported to co-occur with hydroxylgugiaite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Ca₂BeSi₂O₇(OH)₂
- Mohs hardness
- ~5
- Density
- 2.79 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Transparent to translucent
- Crystal system
- Tetragonal
- Crystal habit
- Prismatic crystals
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- A replacement of Be silicate minerals in hydrothermally-altered syenite pegmatite
Where rockhounds find hydroxylgugiaite
Classic worldwide localities
- Larvik plutonic complex, at Blåfjell, Langangen and at the Saga I quarry, Mørje, Porsgrunn, Telemark, southern Norway, and on top of Mount Nakkaalaaq, Ilímaussaq alkaline complex, southern Greenland
Field-hunting tip
Where it forms: A replacement of Be silicate minerals in hydrothermally-altered syenite pegmatite. If you start seeing microcline, albite, biotite in float, you are in the right ground. Typical habit: prismatic crystals. Train your eye for that shape before scanning the outcrop.







