Ivsite is an extremely rare sulfate mineral found exclusively at the historic cryolite deposit in Ivigtut, Greenland. It typically occurs as small, delicate colorless platy crystals or crusts associated with other secondary minerals in the cryolite mine environment.
Is this ivsite?
4-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 ivsite with a known reference. Ivsite sits at Mohs 2, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Streak: white.
- 3Match the color rangeCompare against the expected color range: colorless.
- 4Look at form & habitCrystal system: monoclinic. Typical habit: platy crystals, crusts.
Often confused with
Ivsite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside ivsite
Minerals reported to co-occur with ivsite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Na₃H(SO₄)₂
- Mohs hardness
- 2
- Density
- 2.406 g/cm³
- Colors
- Streak
- White
- Transparency
- Transparent
- Crystal system
- Monoclinic
- Crystal habit
- Platy crystals, crusts
- Rarity
- Rare
- Uses
- Collector
- Host rock
- A sublimate at an active volcanic fumarole (Kamchatka); secondary in the post-mining oxidation zone of asphaltum-rich sandstone beds laced with uraninite and sulfides in a damp underground environment (Utah)
Where rockhounds find ivsite
Classic worldwide localities
- Blue Lizard mine, Red Canyon, San Juan County, Utah, USA
- A fumarole on the Naboko outburst, Tolbachik fissure eruption, Kamchatka Peninsula, Russia (type locality)
Field-hunting tip
Where it forms: A sublimate at an active volcanic fumarole (Kamchatka); secondary in the post-mining oxidation zone of asphaltum-rich sandstone beds laced with uraninite and sulfides in a damp underground environment (Utah). If you start seeing copiapite, ferrinatrite, metavoltine in float, you are in the right ground. Typical habit: platy crystals, crusts. Train your eye for that shape before scanning the outcrop.






