Morenosite is a secondary nickel sulfate mineral that typically forms as a dehydration product or efflorescence in the oxidation zones of nickel-bearing sulfide ores. It is highly unstable in dry air and can quickly dehydrate to form retgersite, so collectors should store it in sealed containers with humidity control.
Is this morenosite?
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 morenosite with a known reference. Morenosite sits at Mohs 2-2.5 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Morenosite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Morenosite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: apple-green, light green, white.
- 5Look at form & habitCrystal system: tetragonal. Typical habit: acicular, fibrous, crusts, efflorescent.
Often confused with
Morenosite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside morenosite
Minerals reported to co-occur with morenosite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- NiSO₄·7H₂O
- Mohs hardness
- 2-2.5
- Density
- 1.97 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Translucent
- Crystal system
- Tetragonal
- Crystal habit
- Acicular, Fibrous, Crusts, Efflorescent
- Cleavage
- Perfect
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Oxidized Zones of Nickel-rich Sulfide Deposits
- Typical price
- $20-150 per specimen
Where rockhounds find morenosite
Classic worldwide localities
- Spain
- Germany
- Greece
- USA
Field-hunting tip
Look in oxidized zones of nickel-rich sulfide deposits country — that is the host setting where morenosite typically forms. If you start seeing annabergite, retgersite, millerite in float, you are in the right ground. Field specimens usually show a acicular, fibrous, crusts, efflorescent habit, so train your eye for that shape before scanning the outcrop.






