Håleniusite-(La) is an extremely rare lanthanum-dominant fluoride mineral belonging to the fluorite group. It typically occurs as minute octahedral crystals within alkaline pegmatite environments, often requiring micro-analysis for definitive identification.
Is this håleniusite-(la)?
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 håleniusite-(la) with a known reference. Håleniusite-(La) 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. Håleniusite-(La) leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Håleniusite-(La) typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: yellow, colorless.
- 5Look at form & habitCrystal system: cubic. Typical habit: small octahedra.
Often confused with
Håleniusite-(La) vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside håleniusite-(la)
Minerals reported to co-occur with håleniusite-(la). Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- LaF₃
- Mohs hardness
- 3-4
- Density
- 5.68 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Transparent
- Crystal system
- Cubic
- Crystal habit
- Small Octahedra
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Alkaline Pegmatites
- Typical price
- $200-1000+ per specimen
Where rockhounds find håleniusite-(la)
Classic worldwide localities
- Khibiny Massif, Russia
- Narssârssuk, Greenland
Field-hunting tip
Look in alkaline pegmatites country — that is the host setting where håleniusite-(la) typically forms. If you start seeing khibinskite, aegirine, nepheline in float, you are in the right ground. Field specimens usually show a small octahedra habit, so train your eye for that shape before scanning the outcrop.



