Hingganite-(Yb) is a very rare beryllium silicate mineral belonging to the gadolinite group, distinguished by its high ytterbium content. Collectors typically look for small, sharp, prismatic crystals occurring within alkaline pegmatites or hydrothermal veins associated with rare-earth element deposits.
Is this hingganite-(yb)?
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 hingganite-(yb) with a known reference. Hingganite-(Yb) sits at Mohs 6.5-7 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Hingganite-(Yb) leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Hingganite-(Yb) typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: colorless, white, pale yellow, brownish.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: prismatic crystals.
Often confused with
Hingganite-(Yb) vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside hingganite-(yb)
Minerals reported to co-occur with hingganite-(yb). Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Yb₂Be₂Si₂O₁₀
- Mohs hardness
- 6.5-7
- Density
- 4.57 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Transparent
- Crystal system
- Monoclinic
- Crystal habit
- Prismatic Crystals
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector, Scientific Study
- Host rock
- Alkaline Pegmatites
- Typical price
- $100-500 for small crystals
Where rockhounds find hingganite-(yb)
Classic worldwide localities
- Hinggan League, Inner Mongolia, China
- Tvedalen, Norway
- Zagi Mountains, Pakistan
Field-hunting tip
Look in alkaline pegmatites country — that is the host setting where hingganite-(yb) typically forms. If you start seeing quartz, microcline, albite in float, you are in the right ground. Field specimens usually show a prismatic crystals habit, so train your eye for that shape before scanning the outcrop.







