Fluorotetraferriphlogopite is a rare mica-group mineral occurring primarily in carbonatites and alkaline igneous environments. Collectors identify it by its characteristic platy, micaceous habit and distinctive iron-rich brown coloration typical of the phlogopite-annite series.
Is this fluorotetraferriphlogopite?
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 fluorotetraferriphlogopite with a known reference. Fluorotetraferriphlogopite 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. Fluorotetraferriphlogopite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Fluorotetraferriphlogopite typically shows a pearly luster.
- 4Match the color rangeCompare against the expected color range: brown, yellowish-brown, dark brown.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: platy crystals, micaceous masses.
Often confused with
Fluorotetraferriphlogopite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside fluorotetraferriphlogopite
Minerals reported to co-occur with fluorotetraferriphlogopite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- KFe²⁺₃(Si₃Fe³⁺)O₁₀F₂
- Mohs hardness
- 2.5-3
- Density
- 2.8-3.0 g/cm³
- Streak
- White
- Luster
- Pearly
- Transparency
- Translucent
- Crystal system
- Monoclinic
- Crystal habit
- Platy Crystals, Micaceous Masses
- Cleavage
- Perfect Basal
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Alkaline Igneous Rocks, Carbonatites
- Typical price
- $20-100 per specimen
Where rockhounds find fluorotetraferriphlogopite
Classic worldwide localities
- Kovdor Massif (Russia)
- Iron Mountain (USA)
Field-hunting tip
Look in alkaline igneous rocks, carbonatites country — that is the host setting where fluorotetraferriphlogopite typically forms. If you start seeing magnetite, apatite, calcite in float, you are in the right ground. Field specimens usually show a platy crystals, micaceous masses habit, so train your eye for that shape before scanning the outcrop.







