Caryochroite is a rare phyllosilicate mineral typically found in the alkaline rock environments of the Kola Peninsula. It often occurs as small, brownish, platy crystals that resemble chlorite but can be distinguished through analytical testing of its unique sodium and strontium content.
Is this caryochroite?
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 caryochroite with a known reference. Caryochroite 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. Caryochroite leaves a light brown streak.
- 3Read the lusterHold the specimen under a strong light. Caryochroite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: brown, reddish-brown.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: platy crystals, granular, massive.
Often found alongside caryochroite
Minerals reported to co-occur with caryochroite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- (Na,Sr,K)₂(Fe³⁺,Mn³⁺,Mg)₂Si₄O₁₀(OH)₂·H₂O
- Mohs hardness
- 3-4
- Density
- 2.9-3.0 g/cm³
- Colors
- Streak
- Light Brown
- Luster
- Vitreous
- Transparency
- Translucent
- Crystal system
- Monoclinic
- Crystal habit
- Platy Crystals, Granular, Massive
- Cleavage
- Perfect
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Alkaline Igneous Complexes
- Typical price
- $50-300 per specimen
Where rockhounds find caryochroite
Classic worldwide localities
- Kola Peninsula, Russia
Field-hunting tip
Look in alkaline igneous complexes country — that is the host setting where caryochroite typically forms. If you start seeing aegirine, nepheline, eudialyte in float, you are in the right ground. Field specimens usually show a platy crystals, granular, massive habit, so train your eye for that shape before scanning the outcrop.




