Deloneite is a rare phosphate mineral member of the apatite group characterized by its strontium and sodium content. It primarily occurs as anhedral grains within alkaline igneous rock complexes and is predominantly known from the Kovdor Massif in Russia. Identification typically requires laboratory analysis due to its visual similarity to common apatite group minerals.
Is this deloneite?
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 deloneite with a known reference. Deloneite sits at Mohs 5, 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: white, colorless, yellowish.
- 5Look at form & habitCrystal system: trigonal. Typical habit: anhedral grains, massive.
Often confused with
Deloneite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside deloneite
Minerals reported to co-occur with deloneite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- (Na₀.₅REE₀.₂₅Ca₀.₂₅)(Ca₀.₇₅REE₀.₂₅)Sr₁.₅(CaNa₀.₂₅REE₀.₂₅)(PO₄)₃F₀.₅(OH)₀.₅
- Mohs hardness
- 5
- Density
- 5.69 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Translucent
- Crystal system
- Trigonal
- Crystal habit
- Anhedral grains, massive
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- alkaline igneous rocks
Where rockhounds find deloneite
Classic worldwide localities
- Kovdor Massif, Kola Peninsula, Russia
Field-hunting tip
Where it forms: alkaline igneous rocks. If you start seeing kovdorskite, magnetite, forsterite in float, you are in the right ground. Typical habit: anhedral grains, massive. Train your eye for that shape before scanning the outcrop.






