Olgite is a very rare phosphate mineral found primarily in the hyperalkaline pegmatites of the Kola Peninsula. It typically occurs as small tabular crystals embedded within nepheline syenite complexes and is highly valued by specialized collectors of Russian minerals.
Is this olgite?
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 olgite with a known reference. Olgite sits at Mohs 4.5, 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: blue, blue green.
- 5Look at form & habitCrystal system: trigonal. Typical habit: microscopic crystals, prismatic.
Often confused with
Olgite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside olgite
Minerals reported to co-occur with olgite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- (Ba,Sr)(Na,Sr,REE)₂Na(PO₄)₂
- Mohs hardness
- 4.5
- Density
- 3.94 g/cm³
- Colors
- Streak
- White
- Luster
- Vitreous
- Transparency
- Transparent
- Crystal system
- Trigonal
- Crystal habit
- Microscopic crystals, prismatic
- Cleavage
- Distinct on {0001}
- Rarity
- Rare
- Uses
- Collector
- Host rock
- In nepheline syenite pegmatite in a differentiated alkalic massif
Where rockhounds find olgite
Classic worldwide localities
- Mts. Karnasurt and Alluaiv, Lovozero massif, and in the Vuonnemiok River valley, Khibiny massif, Kola Peninsula, Russia
Field-hunting tip
Where it forms: In nepheline syenite pegmatite in a differentiated alkalic massif. If you start seeing natrosilite, analcime in float, you are in the right ground. Typical habit: microscopic crystals, prismatic. Train your eye for that shape before scanning the outcrop.


