Honey Calcite is a distinct, warm-hued variety of calcite characterized by its vibrant amber to golden yellow coloration. It typically forms as massive, translucent rhombohedral clusters and is highly prized by collectors for its strong fluorescence under ultraviolet light.
Is this honey 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 honey calcite with a known reference. Honey 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. Honey Calcite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Honey Calcite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: yellow, honey-yellow, amber, golden.
- 5Look at form & habitCrystal system: trigonal. Typical habit: rhombohedral.
Often confused with
Honey Calcite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside honey calcite
Minerals reported to co-occur with honey 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
- Cleavage
- Perfect Rhombohedral in 3 Directions
- Fluorescence
- Bright Yellow or Orange Under SW and LW UV
- Rarity
- Common
- Uses
- Collector, Decorative, Lapidary
- Host rock
- Sedimentary Limestone or Hydrothermal Veins
- Typical price
- $5-30 for small pieces, $50-200 for large decorative specimens
Where rockhounds find honey calcite
Classic worldwide localities
- Mexico
- USA
- Pakistan
- China
Field-hunting tip
Look in sedimentary limestone or hydrothermal veins country — that is the host setting where honey calcite typically forms. If you start seeing quartz, dolomite, siderite in float, you are in the right ground. Field specimens usually show a rhombohedral habit, so train your eye for that shape before scanning the outcrop.







