Witherite is a barium carbonate mineral best recognized by its characteristic pseudohexagonal twinned crystals that appear as rounded, six-sided pyramids. Collectors should look for its distinctive bright fluorescence under ultraviolet light and its notably high specific gravity compared to similar carbonate minerals.
Is this witherite?
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 witherite with a known reference. Witherite sits at Mohs 3-3.5, 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, resinous on fractures.
- 4Match the color rangeCompare against the expected color range: white, gray, yellow, brown, colorless, milky white, grayish white, pale yellowish white, pale brownish white.
- 5Look at form & habitCrystal system: orthorhombic. Typical habit: columnar, pseudo hexagonal, reniform.
Often confused with
Witherite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside witherite
Minerals reported to co-occur with witherite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- BaCO₃
- Mohs hardness
- 3-3.5
- Density
- 4.22-4.31 g/cm³
- Colors
- Streak
- White
- Luster
- Vitreous, resinous on fractures
- Transparency
- Transparent to translucent
- Crystal system
- Orthorhombic
- Crystal habit
- Columnar, pseudo hexagonal, reniform
- Cleavage
- On {010}, distinct; on {110}, {012}, poor
- Fluorescence
- Bluish white under SW and LW UV
- Rarity
- Uncommon
- Uses
- Collector, Industrial source of barium
- Host rock
- Usually in minor amounts in low-temperature hydrothermal veins, typically an alteration product of barite; may be of anoxic sedimentary origin, barium supplied by volcanic hot-spring activity; uncommon in coal measures
Where rockhounds find witherite
2 mapped spotsClassic worldwide localities
- Fine several mines around Rosiclare, as in the Minerva #2 mine, Cave-in-Rock, Hardin Co., Illinois, USA
- Pigeon Roost, Montgomery Co., Arkansas, USA
- England, from Alston Moor, Cumbria
- Settlingstones mine, near Fourstones, and at Fallowfield, near Hexham, Northumberland
- Leogang and at Peggau, north of Graz, Styria, Austria
- Příbram, Czech Republic
Field-hunting tip
Where it forms: Usually in minor amounts in low-temperature hydrothermal veins, typically an alteration product of barite; may be of anoxic sedimentary origin, barium supplied by volcanic hot-spring activity; uncommon in coal measures. If you start seeing barite, fluorite, calcite in float, you are in the right ground. Typical habit: columnar, pseudo hexagonal, reniform. Train your eye for that shape before scanning the outcrop. In the U.S., the densest reported localities are in Illinois, Ohio. Start trip planning there.







