Oxyphlogopite is a rare member of the mica group characterized by the substitution of hydroxyl ions by oxygen, typically resulting from oxidation in high-temperature volcanic environments. It is physically similar to common phlogopite but can often be distinguished by its deeper reddish-brown hues and specific geological occurrence within volcanic ejecta.
Is this oxyphlogopite?
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 oxyphlogopite with a known reference. Oxyphlogopite sits at Mohs 2.5-3 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Oxyphlogopite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Oxyphlogopite typically shows a pearly luster.
- 4Match the color rangeCompare against the expected color range: brown, reddish-brown, dark-brown.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: tabular crystals, scaly aggregates, disseminated flakes.
Often confused with
Oxyphlogopite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside oxyphlogopite
Minerals reported to co-occur with oxyphlogopite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- K(Mg,Fe³⁺)₃(AlSi₃O₁₀)(OH,O)₂
- Mohs hardness
- 2.5-3
- Density
- 2.8-3.0 g/cm³
- Streak
- White
- Luster
- Pearly
- Transparency
- Translucent
- Crystal system
- Monoclinic
- Crystal habit
- Tabular Crystals, Scaly Aggregates, Disseminated Flakes
- Cleavage
- Perfect Basal
- Rarity
- Rare
- Uses
- Collector, Scientific Research
- Host rock
- Alkaline Igneous Rocks, Carbonatites
- Typical price
- $20-100 per specimen
Where rockhounds find oxyphlogopite
Classic worldwide localities
- Monte Somma, Italy
- Khibiny Massif, Russia
- Kola Peninsula, Russia
Field-hunting tip
Look in alkaline igneous rocks, carbonatites country — that is the host setting where oxyphlogopite typically forms. If you start seeing sanidine, nepheline, leucite in float, you are in the right ground. Field specimens usually show a tabular crystals, scaly aggregates, disseminated flakes habit, so train your eye for that shape before scanning the outcrop.







