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, 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.







