Quadruphite is a rare phosphate-silicate mineral found predominantly in the hyper-alkaline environments of the Kola Peninsula in Russia. It typically appears as yellowish or colorless tabular crystals embedded within nepheline syenite pegmatites, often associated with other rare alkaline minerals.
Is this quadruphite?
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 quadruphite with a known reference. Quadruphite 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, resinous on fractures, pearly to adamantine on cleavages.
- 4Match the color rangeCompare against the expected color range: yellow, brown, colorless.
- 5Look at form & habitCrystal system: triclinic. Typical habit: tabular crystals, massive, granular.
Often confused with
Quadruphite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside quadruphite
Minerals reported to co-occur with quadruphite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Na₆Na₂(CaNa)₂Na₂Ti₂Na₂Ti₂(Si₂O₇)₂(PO₄)₄O₄F₂
- Mohs hardness
- 5
- Density
- 3.12 g/cm³
- Streak
- White
- Luster
- Vitreous, resinous on fractures, pearly to adamantine on cleavages
- Transparency
- Translucent to transparent
- Crystal system
- Triclinic
- Crystal habit
- Tabular crystals, massive, granular
- Cleavage
- {001}, perfect; {110} and {100}, less perfect
- Rarity
- Rare
- Uses
- Collector
- Host rock
- In ultra-agpaitic pegmatites in a differentiated alkalic massif
Where rockhounds find quadruphite
Classic worldwide localities
- Mt. Alluaiv, Lovozero massif, Kola Peninsula, Russia
Field-hunting tip
Where it forms: In ultra-agpaitic pegmatites in a differentiated alkalic massif. If you start seeing nepheline, sodalite, analcime in float, you are in the right ground. Typical habit: tabular crystals, massive, granular. Train your eye for that shape before scanning the outcrop.








