Karasugite is a rare strontium calcium aluminum halide, typically colorless. It is a secondary mineral formed in fissures in the oxidation zone of veins of iron ores in tectonic breccias. It was first described from Tannu-Ola Mountains, Tuva, Siberia, Russia.
Is this karasugite?
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 karasugite with a known reference. Karasugite sits at Mohs 3-4, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Karasugite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Karasugite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: colorless.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: tabular crystals.
Often confused with
Karasugite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside karasugite
Minerals reported to co-occur with karasugite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- SrCaAlF₇
- Mohs hardness
- 3-4
- Density
- 3.06-3.11 g/cm³
- Colors
- Streak
- White
- Luster
- Vitreous
- Transparency
- Transparent
- Crystal system
- Monoclinic
- Crystal habit
- Tabular Crystals
- Cleavage
- Perfect On {100}, May Be A Parting
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Hydrothermal Iron Deposits
Where rockhounds find karasugite
Classic worldwide localities
- Karasug iron deposit, Tuva Republic, Russia
Field-hunting tip
Look in hydrothermal iron deposits country, the host setting where karasugite typically forms. If you start seeing baryte, fluorite, magnetite in float, you are in the right ground. Field specimens usually show a tabular crystals habit, so train your eye for that shape before scanning the outcrop.





