Klebelsbergite is a rare secondary antimony mineral that typically forms as delicate, acicular crystals or radiating sprays in the oxidation zones of antimony deposits. It is best identified by its adamantine luster and association with other secondary antimony minerals like valentinite. Due to its fragility and rarity, it is highly sought after by advanced systematic collectors.
Is this klebelsbergite?
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 klebelsbergite with a known reference. Klebelsbergite sits at Mohs 3.5-4, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Streak: white to yellow.
- 3Read the lusterHold the specimen under a strong light. Luster: vitreous to silky.
- 4Match the color rangeCompare against the expected color range: colorless, yellow orange, white, light yellow, dark yellow.
- 5Look at form & habitCrystal system: orthorhombic. Typical habit: acicular crystals, radiating clusters, crusts.
Often confused with
Klebelsbergite vs. its common look-alikes, and how to tell them apart in the field.

How to tell apart: Luster reads vitreous to silky on Klebelsbergite and adamantine, pearly on cleavages on Valentinite.

How to tell apart: Klebelsbergite is noticeably harder (Mohs 3.5-4 vs. 2-2.5); luster reads vitreous to silky on Klebelsbergite and resinous to subadamantine on Senarmontite.
How to tell apart: Stibiconite is the harder of the two (Mohs 5.5-7 vs. 3.5-4); streak differs, so Klebelsbergite leaves white to yellow, Stibiconite leaves light yellow; luster reads vitreous to silky on Klebelsbergite and pearly, opaline, glassy to earthy on Stibiconite.
Often found alongside klebelsbergite
Minerals reported to co-occur with klebelsbergite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Sb₄O₄(OH)₂SO₄
- Mohs hardness
- 3.5-4
- Density
- 4.62 g/cm³
- Colors
- Streak
- White to yellow
- Luster
- Vitreous to silky
- Transparency
- Semitransparent
- Crystal system
- Orthorhombic
- Crystal habit
- Acicular crystals, radiating clusters, crusts
- Cleavage
- Perfect
- Rarity
- Rare
- Uses
- Collector
- Host rock
- An alteration product of stibnite in antimony deposits
Where rockhounds find klebelsbergite
Classic worldwide localities
- Baia Sprie (Felsőbánya), Romania
- Tuscany, at the Cetine mine, 20 km southwest of Siena, Italy
- Pereta mine, Scansano, Italy
- Micciano, near Larderello, Italy
Field-hunting tip
Where it forms: An alteration product of stibnite in antimony deposits. If you start seeing stibnite, valentinite, cervantite in float, you are in the right ground. Typical habit: acicular crystals, radiating clusters, crusts. Train your eye for that shape before scanning the outcrop.




