Sanguite is a very rare potassium chloride mineral that typically forms as red crusts around volcanic fumaroles. It is named for its blood-red color and is primarily found in the Vesuvius volcanic complex. Collectors should note it is highly water-soluble, similar to sylvite, and requires storage in a humidity-controlled environment.
Is this sanguite?
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 sanguite with a known reference. Sanguite sits at Mohs ~3, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Streak: reddish orange.
- 3Read the lusterHold the specimen under a strong light. Luster: vitreous.
- 4Match the color rangeCompare against the expected color range: bright red, dark, brownish red with alteration.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: granular, massive, crystalline crusts.
Often confused with
Sanguite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside sanguite
Minerals reported to co-occur with sanguite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- KCuCl₃
- Mohs hardness
- ~3
- Density
- 2.96 g/cm³
- Colors
- Bright redDarkBrownish red with alteration
- Streak
- Reddish orange
- Luster
- Vitreous
- Transparency
- Transparent
- Crystal system
- Monoclinic
- Crystal habit
- Granular, massive, crystalline crusts
- Cleavage
- Perfect on {010}, distinct on {102̄}
- Rarity
- Rare
- Uses
- Collector
- Host rock
- As sublimates on scoria around an active fumarole
Where rockhounds find sanguite
Classic worldwide localities
- Glavnaya Tenoritovaya (“Major Tenorite”) fumarole, Second scoria cone, Northern Breakthrough of the Great Tolbachik Fissure Eruption, Tolbachik volcano, Kamchatka, Russia
Field-hunting tip
Where it forms: As sublimates on scoria around an active fumarole. If you start seeing belloite, avdoninite, eriochalcite in float, you are in the right ground. Typical habit: granular, massive, crystalline crusts. Train your eye for that shape before scanning the outcrop.





