Dashkovaite is a very rare magnesium formate dihydrate mineral primarily found in the ultra-alkaline rocks of the Khibiny Massif. Collectors should look for its tabular, colorless to white crystals that are typically associated with secondary minerals in pegmatite cavities.
Is this dashkovaite?
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 dashkovaite with a known reference. Dashkovaite sits at Mohs 1, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Streak: white.
- 3Read the lusterHold the specimen under a strong light. Luster: vitreous.
- 4Match the color rangeCompare against the expected color range: white.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: aggregates, fibrous.
Often confused with
Dashkovaite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside dashkovaite
Minerals reported to co-occur with dashkovaite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Mg(HCOO)₂·2H₂O
- Mohs hardness
- 1
- Density
- 1.74 g/cm³
- Colors
- Streak
- White
- Luster
- Vitreous
- Transparency
- Semitransparent
- Crystal system
- Monoclinic
- Crystal habit
- Aggregates, fibrous
- Cleavage
- Perfect
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Rare, in hydrothermal veinlets in serpentine in dolomite marble
Where rockhounds find dashkovaite
Classic worldwide localities
- Korshunovskoye iron–boron skarn deposit, Irkutsk district, Siberia, Russia
Field-hunting tip
Where it forms: Rare, in hydrothermal veinlets in serpentine in dolomite marble. If you start seeing shabynite, iowaite, ekaterinite in float, you are in the right ground. Typical habit: aggregates, fibrous. Train your eye for that shape before scanning the outcrop.








