Kalistrontite is a rare potassium-strontium sulfate primarily found in saline evaporite deposits. Collectors should look for its characteristic tabular crystal habit or white crusts, often associated with other salt minerals like halite and sylvite.
Is this kalistrontite?
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 kalistrontite with a known reference. Kalistrontite sits at Mohs 2-2.5, 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.
- 5Look at form & habitCrystal system: trigonal. Typical habit: tabular crystals, massive, crusts.
Often confused with
Kalistrontite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside kalistrontite
Minerals reported to co-occur with kalistrontite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- K₂Sr(SO₄)₂
- Mohs hardness
- 2-2.5
- Density
- 3.30 g/cm³
- Colors
- Streak
- White
- Luster
- Vitreous
- Transparency
- Transparent
- Crystal system
- Trigonal
- Crystal habit
- Tabular crystals, massive, crusts
- Cleavage
- On {0001}, perfect
- Rarity
- Rare
- Uses
- Collector
- Host rock
- In a drillhole into anhydrite beds, probably formed by the reaction of sylvite with strontium-bearing solutions (Alshtan, Russia); an alteration product of celestine (Pleismar, Germany)
Where rockhounds find kalistrontite
Classic worldwide localities
- Alshtan, Sterlitamak district, southwestern Ural Mountains, Russia
- Bohrung, near Pleismar, Saxony-Anhalt, and from Kalkberg, near Lüneburg, Lower Saxony, Germany
- Stebnyk, Ukraine
- Cesano geothermal field, Latium, Italy
- Omongwa Pan, southwestern Kalahari, Namibia
Field-hunting tip
Where it forms: In a drillhole into anhydrite beds, probably formed by the reaction of sylvite with strontium-bearing solutions (Alshtan, Russia); an alteration product of celestine (Pleismar, Germany). If you start seeing halite, anhydrite, dolomite in float, you are in the right ground. Typical habit: tabular crystals, massive, crusts. Train your eye for that shape before scanning the outcrop.







