Hydrombobomkulite is a rare hydrated nickel-aluminum nitrate sulfate carbonate mineral belonging to the layered double hydroxide group. It typically occurs as small, delicate platy crystals or thin crusts in the oxidation zones of nickel-bearing mineral deposits.
Is this hydrombobomkulite?
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 hydrombobomkulite with a known reference. Hydrombobomkulite 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. Hydrombobomkulite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Hydrombobomkulite typically shows a pearly luster.
- 4Match the color rangeCompare against the expected color range: white, pale blue, pale green.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: platy crystals, crusts, or aggregates.
Often confused with
Hydrombobomkulite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside hydrombobomkulite
Minerals reported to co-occur with hydrombobomkulite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- (Ni,Al)₄(NO₃,SO₄,CO₃)₂(OH)₁₂·3H₂O
- Mohs hardness
- 2
- Density
- 2.28 g/cm³
- Colors
- Streak
- White
- Luster
- Pearly
- Transparency
- Translucent
- Crystal system
- Monoclinic
- Crystal habit
- Platy Crystals, Crusts, Or Aggregates
- Cleavage
- Perfect Basal
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Weathered Nickel Ore Zones and Hydrothermal Environments
- Typical price
- n/a
Where rockhounds find hydrombobomkulite
Classic worldwide localities
- Bobomkul deposit, Tajikistan
- various nickel-bearing ore occurrences
Field-hunting tip
Look in weathered nickel ore zones and hydrothermal environments country — that is the host setting where hydrombobomkulite typically forms. If you start seeing bunsenite, violarite, nickel-rich clays in float, you are in the right ground. Field specimens usually show a platy crystals, crusts, or aggregates habit, so train your eye for that shape before scanning the outcrop.



