Optical calcite, known as Iceland spar, is a high-purity, transparent variety of calcite that exhibits strong double refraction. When a single line or image is viewed through a clean rhombohedral cleavage piece, it appears doubled, making it a classic specimen for physical optics study. Collectors should look for large, clear, and perfectly shaped rhombohedrons free of internal clouding or heavy twinning.
Is this optical calcite?
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 optical calcite with a known reference. Optical Calcite sits at Mohs 3, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Optical Calcite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Optical Calcite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: colorless, white.
- 5Look at form & habitCrystal system: trigonal. Typical habit: rhombohedral crystals.
Often confused with
Optical Calcite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside optical calcite
Minerals reported to co-occur with optical calcite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- CaCO₃
- Mohs hardness
- 3
- Density
- 2.71 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Transparent
- Crystal system
- Trigonal
- Crystal habit
- Rhombohedral Crystals
- Cleavage
- Perfect Rhombohedral in 3 Directions
- Fluorescence
- Often Fluorescent Under UV
- Rarity
- Common
- Uses
- Collector, Scientific, Optical
- Host rock
- Sedimentary Environments and Hydrothermal Veins
- Typical price
- $10-100 per specimen
Where rockhounds find optical calcite
Classic worldwide localities
- Helgustadir, Iceland
- Chihuahua, Mexico
- Sonora, Mexico
- Tennessee, USA
Field-hunting tip
Look in sedimentary environments and hydrothermal veins country, the host setting where optical calcite typically forms. If you start seeing quartz, fluorite, dolomite in float, you are in the right ground. Field specimens usually show a rhombohedral crystals habit, so train your eye for that shape before scanning the outcrop.





