Betpakdalite-CaCa is a rare secondary molybdenum arsenate mineral typically occurring in the oxidation zones of ore deposits. It is often found as small, fragile, yellow platy crystals or as earthy, powdery coatings on host rocks.
Is this betpakdalite-caca?
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 betpakdalite-caca with a known reference. Betpakdalite-CaCa 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: pale yellow.
- 3Read the lusterHold the specimen under a strong light. Luster: dull to waxy.
- 4Match the color rangeCompare against the expected color range: rarely brownish, tint.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: platy crystals, powdery aggregates.
Often confused with
Betpakdalite-CaCa vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside betpakdalite-caca
Minerals reported to co-occur with betpakdalite-caca. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- [Ca₂(H₂O)₁₇Ca(H₂O)₆][Mo₈As₂Fe₃O₃₆(OH)]
- Mohs hardness
- ~3
- Density
- 2.98-3.05 g/cm³
- Colors
- Rarely brownishTint
- Streak
- Pale yellow
- Luster
- Dull to waxy
- Transparency
- Transparent
- Crystal system
- Monoclinic
- Crystal habit
- Platy crystals, powdery aggregates
- Cleavage
- {001}, very good
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Filling cracks in leached pyrite in the oxidized zone of a mineral deposit (Kara-Oba deposit, Kazakhstan); on vein quartz (Krupka, Czech Republic)
Where rockhounds find betpakdalite-caca
Classic worldwide localities
- Kara-Oba Mo-W deposit, Bet-Pak-Dal Desert, central Kazakhstan
- Descubridora mine, Pampa Larga district, Copiapó, Chile, Norway
- Bajan Cogto, Mongolia, Norway
- Rustler mine, Gold Hill district, Tooele County, Utah, USA, Norway
- Nedre Kvartsen quarry, Drag, Tysfjord, Nordland, Norway
- Krupka, Krušné hory Mountains, Czech Republic
Field-hunting tip
Where it forms: Filling cracks in leached pyrite in the oxidized zone of a mineral deposit (Kara-Oba deposit, Kazakhstan); on vein quartz (Krupka, Czech Republic). If you start seeing ferrimolybdite, gypsum, jarosite in float, you are in the right ground. Typical habit: platy crystals, powdery aggregates. Train your eye for that shape before scanning the outcrop.







