Carbonatite is a rare igneous rock composed of more than 50% carbonate minerals rather than the typical silicate minerals found in most igneous rocks. They are of significant interest to collectors and geologists because they are the world's primary source of rare earth elements, niobium, and apatite.
Is this carbonatite?
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 carbonatite with a known reference. Carbonatite sits at Mohs 3-4 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Carbonatite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Carbonatite typically shows a vitreous to dull luster.
- 4Match the color rangeCompare against the expected color range: white, gray, tan, pink, brown.
- 5Look at form & habitTypical habit: massive to granular.
Often confused with
Carbonatite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside carbonatite
Minerals reported to co-occur with carbonatite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Mohs hardness
- 3-4
- Density
- 2.7-3.0 g/cm³
- Streak
- White
- Luster
- Vitreous to Dull
- Transparency
- Opaque
- Crystal habit
- Massive to Granular
- Rarity
- Rare
- Uses
- Industrial, Scientific Research
- Host rock
- Intrusive Igneous Complexes
- Typical price
- $10-100 per specimen
Where rockhounds find carbonatite
Classic worldwide localities
- Fen Complex, Norway
- Kola Peninsula, Russia
- Mount Weld, Australia
- Palabora, South Africa
- Mountain Pass, USA
Field-hunting tip
Look in intrusive igneous complexes country — that is the host setting where carbonatite typically forms. If you start seeing calcite, dolomite, apatite in float, you are in the right ground. Field specimens usually show a massive to granular habit, so train your eye for that shape before scanning the outcrop.







