Lime, specifically quicklime or calcium oxide, is an industrially processed product derived primarily from heating limestone. It is rarely found as a naturally occurring mineral due to its high reactivity with water and carbon dioxide in the atmosphere. Collectors primarily interact with it in historical industrial contexts or as processed chemical samples.
Is this lime?
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 lime with a known reference. Lime sits at Mohs 3.5, 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: cubic. Typical habit: massive.
Often confused with
Lime vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside lime
Minerals reported to co-occur with lime. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- CaO
- Mohs hardness
- 3.5
- Density
- 3.345 g/cm³
- Colors
- Streak
- White
- Luster
- Vitreous
- Transparency
- Semitransparent
- Crystal system
- Cubic
- Crystal habit
- Massive
- Cleavage
- {001}, perfect; parting on {011} (synthetic)
- Rarity
- Common
- Uses
- Industrial, Construction, Agricultural
- Host rock
- In thermally metamorphosed calcareous ejecta (Vesuvius, Italy); in burning coal measures (Kopeysk, Russia)
Where rockhounds find lime
Classic worldwide localities
- Campbell mine, Bisbee, Cochise Co., Arizona, USA
- Vesuvius, Campania, Italy
- Kopeysk, Chelyabinsk coal basin, Southern Ural Mountains, Russia
- Northern Siwaqa complex, Tulul Al Hammam area, Dead Sea region, Central Jordan
Field-hunting tip
Where it forms: In thermally metamorphosed calcareous ejecta (Vesuvius, Italy); in burning coal measures (Kopeysk, Russia). If you start seeing calcite, fluorellestadite, periclase in float, you are in the right ground. Typical habit: massive. Train your eye for that shape before scanning the outcrop.








