Tetraferriphlogopite is a rare member of the mica group characterized by the substitution of Fe³⁺ for silicon in the tetrahedral site of the crystal lattice. Collectors typically look for its distinct dark brown to reddish-brown platy, pseudo-hexagonal crystals embedded in carbonatite or alkaline silicate rocks.
Is this tetraferriphlogopite?
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 tetraferriphlogopite with a known reference. Tetraferriphlogopite 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. Tetraferriphlogopite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Tetraferriphlogopite typically shows a pearly luster.
- 4Match the color rangeCompare against the expected color range: brown, dark brown, yellowish-brown, reddish-brown.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: platy crystals, pseudo-hexagonal flakes.
Often confused with
Tetraferriphlogopite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside tetraferriphlogopite
Minerals reported to co-occur with tetraferriphlogopite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- KMg₃(Fe³⁺Si₃O₁₀)(OH)₂
- Mohs hardness
- 2.5-3
- Density
- 2.7-2.9 g/cm³
- Streak
- White
- Luster
- Pearly
- Transparency
- Translucent
- Crystal system
- Monoclinic
- Crystal habit
- Platy Crystals, Pseudo-hexagonal Flakes
- Cleavage
- Perfect Basal
- Rarity
- Uncommon
- Uses
- Collector
- Host rock
- Alkaline Igneous Rocks, Carbonatites
- Typical price
- $10-50 per specimen
Where rockhounds find tetraferriphlogopite
Classic worldwide localities
- Kovdor Massif, Russia
- Magnet Cove, USA
- Jacupiranga, Brazil
- Tapira, Brazil
Field-hunting tip
Look in alkaline igneous rocks, carbonatites country — that is the host setting where tetraferriphlogopite typically forms. If you start seeing magnetite, apatite, calcite in float, you are in the right ground. Field specimens usually show a platy crystals, pseudo-hexagonal flakes habit, so train your eye for that shape before scanning the outcrop.







