Kozoite-(Nd) is an extremely rare rare-earth carbonate mineral typically found as tiny, needle-like acicular crystals or radiating sprays. It is most often discovered in cavities within alkaline pegmatites, where it is frequently associated with minerals like calcite and albite.
Is this kozoite-(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 kozoite-(nd) with a known reference. Kozoite-(Nd) sits at Mohs 4-4.5 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Kozoite-(Nd) leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Kozoite-(Nd) typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: white, colorless, pale pink.
- 5Look at form & habitCrystal system: orthorhombic. Typical habit: acicular crystals, radiating aggregates.
Often confused with
Kozoite-(Nd) vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside kozoite-(nd)
Minerals reported to co-occur with kozoite-(nd). Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Nd(CO₃)(OH,F)
- Mohs hardness
- 4-4.5
- Density
- 4.21 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Translucent
- Crystal system
- Orthorhombic
- Crystal habit
- Acicular Crystals, Radiating Aggregates
- Cleavage
- None Observed
- Rarity
- Rare
- Uses
- Collector, Research
- Host rock
- Alkaline Igneous Rocks, Specifically Pegmatites
- Typical price
- $50-300 per small specimen
Where rockhounds find kozoite-(nd)
Classic worldwide localities
- Hizen-cho, Saga Prefecture, Japan
- Kola Peninsula, Russia
Field-hunting tip
Look in alkaline igneous rocks, specifically pegmatites country — that is the host setting where kozoite-(nd) typically forms. If you start seeing calcite, albite, aegirine in float, you are in the right ground. Field specimens usually show a acicular crystals, radiating aggregates habit, so train your eye for that shape before scanning the outcrop.







