Tundrite-(Nd) is a rare silicate-carbonate mineral primarily found in the complex alkaline rocks of the Kola Peninsula in Russia. It typically occurs as small, tabular, or platy crystals associated with other rare earth minerals in pegmatite veins.
Is this tundrite-(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 tundrite-(nd) with a known reference. Tundrite-(Nd) sits at Mohs 3, 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: yellow, greenish yellow.
- 5Look at form & habitCrystal system: triclinic. Typical habit: tabular crystals, thin plates.
Often confused with
Tundrite-(Nd) vs. its common look-alikes, and how to tell them apart in the field.

How to tell apart: Streak differs, so Tundrite-(Nd) leaves white, Tundrite-(Ce) leaves yellowish gray to white.

How to tell apart: Lorenzenite is the harder of the two (Mohs 6 vs. 3); streak differs, so Tundrite-(Nd) leaves white, Lorenzenite leaves light brownish yellow.
Often found alongside tundrite-(nd)
Minerals reported to co-occur with tundrite-(nd). Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Na₂Nd₂TiO₂(SiO₄)(CO₃)₂
- Mohs hardness
- 3
- Density
- 4.02 g/cm³
- Colors
- Streak
- White
- Luster
- Vitreous
- Transparency
- Semitransparent
- Crystal system
- Triclinic
- Crystal habit
- Tabular crystals, thin plates
- Cleavage
- Good
- Rarity
- Rare
- Uses
- Collector
- Host rock
- In pegmatite veins associated with layered nepheline syenite
Where rockhounds find tundrite-(nd)
Classic worldwide localities
- Ilimaussaq intrusion, at Kringlerne, Kangerdluarssuk Plateau, southern Greenland (type locality)
Field-hunting tip
Where it forms: In pegmatite veins associated with layered nepheline syenite. If you start seeing microcline, arfvedsonite in float, you are in the right ground. Typical habit: tabular crystals, thin plates. Train your eye for that shape before scanning the outcrop.


