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 2-2.5 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Klebelsbergite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Klebelsbergite typically shows a adamantine luster.
- 4Match the color rangeCompare against the expected color range: yellow, yellowish-green, colorless.
- 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.
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
- 2-2.5
- Density
- 4.67 g/cm³
- Streak
- White
- Luster
- Adamantine
- Transparency
- Transparent
- Crystal system
- Orthorhombic
- Crystal habit
- Acicular Crystals, Radiating Clusters, Crusts
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Oxidized Zones of Antimony Deposits
- Typical price
- $50-300 per specimen
Where rockhounds find klebelsbergite
Classic worldwide localities
- Antimony Mine, Hungary
- Pereta mine, Italy
- Tuscany, Italy
Field-hunting tip
Look in oxidized zones of antimony deposits country — that is the host setting where klebelsbergite typically forms. If you start seeing stibnite, valentinite, senarmontite in float, you are in the right ground. Field specimens usually show a acicular crystals, radiating clusters, crusts habit, so train your eye for that shape before scanning the outcrop.




