Fluorescent calcite is a popular collector's mineral prized for its intense, vivid response under long-wave and short-wave ultraviolet light. It commonly occurs in rhombohedral or scalenohedral crystal habits and is most frequently found in limestone cavities or as a gangue mineral in ore deposits.
Is this fluorescent 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 fluorescent calcite with a known reference. Fluorescent 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. Streak: white.
- 3Read the lusterHold the specimen under a strong light. Luster: vitreous.
- 4Match the color rangeCompare against the expected color range: white, colorless, yellow, orange, pink, blue.
- 5Look at form & habitCrystal system: trigonal. Typical habit: rhombohedral, scalenohedral, massive, or stalactitic.
Often confused with
Fluorescent Calcite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside fluorescent calcite
Minerals reported to co-occur with fluorescent 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
- Translucent
- Crystal system
- Trigonal
- Crystal habit
- Rhombohedral, scalenohedral, massive, or stalactitic
- Cleavage
- Perfect rhombohedral
- Fluorescence
- Bright red, orange, or pink under UV light
- Rarity
- Common
- Uses
- Collector, Lapidary
- Host rock
- sedimentary limestones, hydrothermal veins, and metamorphic marbles
Where rockhounds find fluorescent calcite
7 mapped spotsClassic worldwide localities
- Franklin, New Jersey, USA
- Terlingua, Texas, USA
- Mexico
- China
- Pakistan
Field-hunting tip
Where it forms: sedimentary limestones, hydrothermal veins, and metamorphic marbles. If you start seeing willemite, fluorite, barite in float, you are in the right ground. Typical habit: rhombohedral, scalenohedral, massive, or stalactitic. Train your eye for that shape before scanning the outcrop. In the U.S., the densest reported localities are in Indiana, Arizona, Missouri. Start trip planning there.









