Ice is a naturally occurring crystalline solid formed by the freezing of water. While often overlooked, it is recognized as a valid mineral species by the IMA due to its stable, ordered crystalline structure under specific planetary conditions.
Is this cubo-ice?
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 cubo-ice with a known reference. Cubo-ice sits at Mohs 1.5 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Cubo-ice leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Cubo-ice typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: colorless, white, blue.
- 5Look at form & habitCrystal system: cubic. Typical habit: hexagonal plates, needles, or massive.
Often confused with
Cubo-ice vs. its common look-alikes — and how to tell them apart in the field.
All properties
- Chemical formula
- H₂O
- Mohs hardness
- 1.5
- Density
- 0.917 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Transparent
- Crystal system
- Cubic
- Crystal habit
- Hexagonal Plates, Needles, Or Massive
- Cleavage
- None
- Rarity
- Common
- Uses
- Scientific Study, Cryology, Collector
- Host rock
- Glaciers and Permafrost Environments
- Typical price
- n/a (lab-grown/environmental)
Where rockhounds find cubo-ice
Classic worldwide localities
- Antarctica
- Greenland
- Alpine glaciers
- Earth polar regions
Field-hunting tip
Look in glaciers and permafrost environments country — that is the host setting where cubo-ice typically forms. If you start seeing air, gases, impurities in float, you are in the right ground. Field specimens usually show a hexagonal plates, needles, or massive habit, so train your eye for that shape before scanning the outcrop.



