Pyrochlore is the niobium member of the pyrochlore supergroup and the main ore of niobium: the three largest niobium producers, led by the CBMM mine near Araxá, Brazil, all mine pyrochlore deposits. It usually forms well-shaped octahedra, brown to reddish brown with a vitreous to resinous luster, and it is characteristic of carbonatites and of pegmatites in alkalic rocks. It is commonly metamict, its structure damaged by radiation from included uranium and thorium. The name comes from the Greek for fire and green, the color it usually turns when heated.
Is this pyrochlore?
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 pyrochlore with a known reference. Pyrochlore sits at Mohs 5-5.5, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Streak: brown.
- 3Read the lusterHold the specimen under a strong light. Luster: vitreous to resinous.
- 4Match the color rangeCompare against the expected color range: black, brown, chocolate brown, reddish brown, amber orange, red orange.
- 5Look at form & habitCrystal system: cubic. Typical habit: octahedral crystals; granular, massive.
Often found alongside pyrochlore
Minerals reported to co-occur with pyrochlore. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- (Na,Ca)₂Nb₂O₆(OH,F)
- Mohs hardness
- 5-5.5
- Density
- 4.33 g/cm³
- Colors
- Streak
- Brown
- Luster
- Vitreous to resinous
- Transparency
- Translucent
- Crystal system
- Cubic
- Crystal habit
- Octahedral crystals; granular, massive
- Cleavage
- On {111}, may be a parting
- Uses
- Ore of niobium
- Host rock
- Carbonatites; pegmatites in nepheline syenites and other alkalic rocks; granite pegmatites and greisens
Where rockhounds find pyrochlore
Classic worldwide localities
- Fredriksvärn and Larvik, Norway (type locality)
- Araxá, Minas Gerais, Brazil
- Oka, Quebec, Canada
- Panda Hill, Mbeya, Tanzania
- Lovozero massif, Kola Peninsula, Russia
Field-hunting tip
Where it forms: Carbonatites; pegmatites in nepheline syenites and other alkalic rocks; granite pegmatites and greisens. If you start seeing zircon, aegirine, apatite in float, you are in the right ground. Typical habit: octahedral crystals; granular, massive. Train your eye for that shape before scanning the outcrop.







