Fluorophlogopite is a fluorine-rich member of the mica group, characterized by its flexible, thin lamellae and pearly luster. It commonly appears in metamorphosed carbonate rocks and is visually indistinguishable from standard phlogopite without advanced chemical analysis. Collectors typically find it in contact metamorphic zones alongside other high-temperature silicates.
Is this fluorophlogopite?
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 fluorophlogopite with a known reference. Fluorophlogopite 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. Fluorophlogopite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Fluorophlogopite typically shows a pearly luster.
- 4Match the color rangeCompare against the expected color range: colorless, white, yellow, brown, green.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: tabular crystals, scaly aggregates, micaceous flakes.
Often confused with
Fluorophlogopite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside fluorophlogopite
Minerals reported to co-occur with fluorophlogopite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- KMg₃(AlSi₃O₁₀)F₂
- Mohs hardness
- 2.5-3
- Density
- 2.7-2.9 g/cm³
- Streak
- White
- Luster
- Pearly
- Transparency
- Transparent
- Crystal system
- Monoclinic
- Crystal habit
- Tabular Crystals, Scaly Aggregates, Micaceous Flakes
- Cleavage
- Perfect Basal
- Rarity
- Uncommon
- Uses
- Industrial, Collector
- Host rock
- Metamorphosed Limestones, Skarns, Alkaline Igneous Rocks
- Typical price
- $10-60 thumbnail
Where rockhounds find fluorophlogopite
Classic worldwide localities
- Kola Peninsula, Russia
- Franklin, New Jersey, USA
- Monte Somma, Italy
- Kilimanjaro, Tanzania
Field-hunting tip
Look in metamorphosed limestones, skarns, alkaline igneous rocks country — that is the host setting where fluorophlogopite typically forms. If you start seeing calcite, diopside, forsterite in float, you are in the right ground. Field specimens usually show a tabular crystals, scaly aggregates, micaceous flakes habit, so train your eye for that shape before scanning the outcrop.







