Ferrotychite is a rare member of the Tychite group, characterized by its isometric, octahedral crystals. It is primarily found in alkaline igneous environments and is notably associated with its magnesium-dominant analogue, Tychite.
Is this ferrotychite?
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 ferrotychite with a known reference. Ferrotychite sits at Mohs 4, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Streak: white.
- 3Read the lusterHold the specimen under a strong light. Luster: vitreous.
- 4Match the color rangeCompare against the expected color range: colorless, light yellow.
- 5Look at form & habitCrystal system: cubic. Typical habit: octahedral crystals.
Often confused with
Ferrotychite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside ferrotychite
Minerals reported to co-occur with ferrotychite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Na₆Fe₂(SO₄)(CO₃)₄
- Mohs hardness
- 4
- Density
- 2.79 g/cm³
- Colors
- Streak
- White
- Luster
- Vitreous
- Transparency
- Semitransparent
- Crystal system
- Cubic
- Crystal habit
- Octahedral crystals
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- A rare constituent of a vein cutting ijolite-urtite in an alkaline igneous complex, from a drill core
Where rockhounds find ferrotychite
Classic worldwide localities
- Olenii Ruchei (Reindeers Stream), Khibiny massif, Kola Peninsula, Russia (type locality)
Field-hunting tip
Where it forms: A rare constituent of a vein cutting ijolite-urtite in an alkaline igneous complex, from a drill core. If you start seeing shortite, bonshtedtite, analcime in float, you are in the right ground. Typical habit: octahedral crystals. Train your eye for that shape before scanning the outcrop.




