Hingganite-(Nd) is a rare beryllium silicate mineral belonging to the gadolinite group, named after its type locality in the Hinggan Mountains. It typically forms as small, brownish prismatic crystals in alkaline pegmatites and is highly sought after by advanced collectors for its distinct REE-rich composition.
Is this hingganite-(nd)?
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-(nd) with a known reference. Hingganite-(Nd) 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-(Nd) leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Hingganite-(Nd) typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: yellowish-brown, brown, black.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: prismatic crystals.
Often confused with
Hingganite-(Nd) vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside hingganite-(nd)
Minerals reported to co-occur with hingganite-(nd). Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- ☐Be₂(Nd,Ca,REE)₂(SiO₄)₂(OH)₂
- Mohs hardness
- 6.5-7
- Density
- 4.4-4.8 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Translucent
- Crystal system
- Monoclinic
- Crystal habit
- Prismatic Crystals
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Alkaline Pegmatites
- Typical price
- $50-300 per thumbnail specimen
Where rockhounds find hingganite-(nd)
Classic worldwide localities
- Hinggan League, Inner Mongolia, China
- Tvedalen, Norway
- Kola Peninsula, Russia
Field-hunting tip
Look in alkaline pegmatites country — that is the host setting where hingganite-(nd) typically forms. If you start seeing albite, microcline, aegirine 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.





