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, 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.







