Sylvite is a primary source of potash and typically forms in salt deposits as a result of the evaporation of seawater. It is very similar to halite but can often be distinguished by its bitter, salty taste and its tendency to be slightly more brittle or have a different cleavage pattern when observed under magnification.
Is this sylvite?
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 sylvite with a known reference. Sylvite 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. Sylvite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Sylvite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: white, colorless, red, orange, blue.
- 5Look at form & habitCrystal system: cubic. Typical habit: cubic crystals, hoppered crystals, massive, granular.
Often confused with
Sylvite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside sylvite
Minerals reported to co-occur with sylvite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- KCl
- Mohs hardness
- 2
- Density
- 1.99 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Transparent
- Crystal system
- Cubic
- Crystal habit
- Cubic Crystals, Hoppered Crystals, Massive, Granular
- Cleavage
- Perfect Cubic
- Rarity
- Common
- Uses
- Fertilizer, Industrial, Collector
- Host rock
- Evaporite Deposits
- Typical price
- $10-50 per specimen
Where rockhounds find sylvite
5 mapped spotsClassic worldwide localities
- Stassfurt, Germany
- Carlsbad, USA
- Solikamsk, Russia
- Kalush, Ukraine
- Saskatchewan, Canada
Field-hunting tip
Look in evaporite deposits country — that is the host setting where sylvite typically forms. If you start seeing halite, carnallite, kieserite in float, you are in the right ground. Field specimens usually show a cubic crystals, hoppered crystals, massive, granular habit, so train your eye for that shape before scanning the outcrop. In the U.S., the densest reported localities are in Utah, Nevada — start trip planning there.





