Carlosruizite is an extremely rare sulfate-iodate-selenate mineral found primarily in the hyper-arid regions of the Atacama Desert. It typically occurs as small, delicate, yellow needle-like crystals or radiating clusters within nitrate-rich evaporite deposits. Due to its scarcity and solubility, it is highly sought after by advanced mineral collectors specializing in rare species.
Is this carlosruizite?
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 carlosruizite with a known reference. Carlosruizite sits at Mohs 2-3, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Carlosruizite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Carlosruizite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: yellow, yellowish-orange.
- 5Look at form & habitCrystal system: hexagonal. Typical habit: acicular crystals, radiating sprays, crusts.
Often confused with
Carlosruizite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside carlosruizite
Minerals reported to co-occur with carlosruizite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- K₆(Na,K)₄Na₆Mg₂(SO₄)₃(IO₃)₄(SeO₄)₃·6H₂O
- Mohs hardness
- 2-3
- Density
- 2.36 g/cm³
- Colors
- Streak
- White
- Luster
- Vitreous
- Transparency
- Transparent
- Crystal system
- Hexagonal
- Crystal habit
- Acicular Crystals, Radiating Sprays, Crusts
- Cleavage
- Distinct
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Nitrate Deposits in Arid Desert Environments
- Typical price
- $50-300 thumbnail
Where rockhounds find carlosruizite
Classic worldwide localities
- Chuquicamata Mine, Chile
Field-hunting tip
Look in nitrate deposits in arid desert environments country, the host setting where carlosruizite typically forms. If you start seeing dietzeite, halite, gypsum in float, you are in the right ground. Field specimens usually show a acicular crystals, radiating sprays, crusts habit, so train your eye for that shape before scanning the outcrop.




