Cuatrocapaite-(K) is an extremely rare sulfate mineral discovered in evaporitic environments in Mexico. It is typically found as fragile, pale yellow platy crystals or foliated masses associated with gypsum and other evaporite minerals. Due to its scarcity and delicate nature, it is highly sought after by systematic mineral collectors.
Is this cuatrocapaite-(k)?
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 cuatrocapaite-(k) with a known reference. Cuatrocapaite-(K) 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. Cuatrocapaite-(K) leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Cuatrocapaite-(K) typically shows a pearly luster.
- 4Match the color rangeCompare against the expected color range: yellow, pale yellow.
- 5Look at form & habitCrystal system: trigonal. Typical habit: platy crystals, pseudohexagonal, foliated aggregates.
Often confused with
Cuatrocapaite-(K) vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside cuatrocapaite-(k)
Minerals reported to co-occur with cuatrocapaite-(k). Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- K₂Na₃(H₂O)₁₀[Ce₂(SO₄)₄(OH)₂]·nH₂O
- Mohs hardness
- 2
- Density
- 2.7 g/cm³
- Colors
- Streak
- White
- Luster
- Pearly
- Transparency
- Translucent
- Crystal system
- Trigonal
- Crystal habit
- Platy Crystals, Pseudohexagonal, Foliated Aggregates
- Cleavage
- Perfect Basal
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Evaporitic Deposits
- Typical price
- $50-300+ per specimen depending on size and rarity
Where rockhounds find cuatrocapaite-(k)
Classic worldwide localities
- Cuatro Ciénegas, Coahuila, Mexico
Field-hunting tip
Look in evaporitic deposits country — that is the host setting where cuatrocapaite-(k) typically forms. If you start seeing gypsum, anhydrite, halite in float, you are in the right ground. Field specimens usually show a platy crystals, pseudohexagonal, foliated aggregates habit, so train your eye for that shape before scanning the outcrop.




