Formicaite is an extremely rare calcium formate mineral typically found in environments containing decomposing organic matter and limestone. It usually appears as small, thin, tabular crystals in cavities of sedimentary rocks, often requiring micro-analysis for definitive identification.
Is this formicaite?
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 formicaite with a known reference. Formicaite 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, light blue.
- 5Look at form & habitCrystal system: tetragonal. Typical habit: aggregates, microscopic crystals, tabular.
Often confused with
Formicaite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside formicaite
Minerals reported to co-occur with formicaite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Ca(HCOO)₂
- Mohs hardness
- 1
- Density
- 1.9 g/cm³
- Colors
- Streak
- White
- Luster
- Vitreous
- Transparency
- Semitransparent
- Crystal system
- Tetragonal
- Crystal habit
- Aggregates, microscopic crystals, tabular
- Cleavage
- {100}, perfect
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Rare in hydrothermal veinlets cutting kurchatovite-sakhaite ore (Solongo deposit, Russia); in a veinlet in skarnitized marble (Novofrolovskoye deposit, Russia)
Where rockhounds find formicaite
Classic worldwide localities
- Solongo boron deposit, Buryatia, and the Novofrolovskoye copper deposit, near Krasnoturinsk, Turinsk district, Northern Ural Mountains, Russia
Field-hunting tip
Where it forms: Rare in hydrothermal veinlets cutting kurchatovite-sakhaite ore (Solongo deposit, Russia); in a veinlet in skarnitized marble (Novofrolovskoye deposit, Russia). If you start seeing calcite, lizardite, frolovite in float, you are in the right ground. Typical habit: aggregates, microscopic crystals, tabular. Train your eye for that shape before scanning the outcrop.







