Aklimaite is a rare calcium silicate mineral typically found in metamorphic environments involving limestone. It most often presents as white, fibrous, or radiating crystalline masses that can be easily mistaken for other fibrous silicates.
Is this aklimaite?
4-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 aklimaite with a known reference. Aklimaite sits at Mohs 3-4, softer than the next harder reference, harder than the previous one.
- 2Read the lusterHold the specimen under a strong light. Luster: vitreous.
- 3Match the color rangeCompare against the expected color range: colorless.
- 4Look at form & habitCrystal system: monoclinic. Typical habit: fibrous aggregates, radiating clusters.
Often confused with
Aklimaite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside aklimaite
Minerals reported to co-occur with aklimaite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Ca₄[Si₂O₅(OH)₂](OH)₄·5H₂O
- Mohs hardness
- 3-4
- Density
- 2.20 g/cm³
- Colors
- Luster
- Vitreous
- Transparency
- Transparent
- Crystal system
- Monoclinic
- Crystal habit
- Fibrous aggregates, radiating clusters
- Cleavage
- On {001}, perfect
- Rarity
- Rare
- Uses
- Collector
- Host rock
- In a metasomatically altered limestone xenolith in ignimbrite
Where rockhounds find aklimaite
Classic worldwide localities
- Upper Chegem (Verkhnechegemskaya) Caldera, near Mount Lakargi, Kabardino-Balkaria, Northern Caucasus, Russia
Field-hunting tip
Where it forms: In a metasomatically altered limestone xenolith in ignimbrite. If you start seeing larnite, hydrogarnets, bultfonteinite in float, you are in the right ground. Typical habit: fibrous aggregates, radiating clusters. Train your eye for that shape before scanning the outcrop.





