Ertixiite is an extremely rare sodium silicate mineral known almost exclusively from its type locality at the Koktokay pegmatite in China. It typically occurs as small, clear, equant crystals associated with lithium-bearing pegmatite minerals. Due to its extreme rarity, it is highly sought after by advanced systematic mineral collectors.
Is this ertixiite?
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 ertixiite with a known reference. Ertixiite sits at Mohs 5.8-6.5, 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, white.
- 5Look at form & habitCrystal system: cubic. Typical habit: granular.
Often confused with
Ertixiite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside ertixiite
Minerals reported to co-occur with ertixiite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Na₂Si₄O₉
- Mohs hardness
- 5.8-6.5
- Density
- 2.35 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Transparent
- Crystal system
- Cubic
- Crystal habit
- Granular
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- As linings of miarolitic cavities in a Ta-Nb-Be-bearing granite pegmatite
Where rockhounds find ertixiite
Classic worldwide localities
- Altay pegmatite mine, Fuyun Co., 600 km northeast of Urumchi, Sinkiang Uighur Autonomous Region, China
Field-hunting tip
Where it forms: As linings of miarolitic cavities in a Ta-Nb-Be-bearing granite pegmatite. If you start seeing topaz, albite, muscovite in float, you are in the right ground. Typical habit: granular. Train your eye for that shape before scanning the outcrop.






