Novákite is a rare copper-arsenic mineral typically found as massive or fine-grained aggregates within hydrothermal veins. It is visually similar to other copper arsenides and is usually identified through laboratory analysis or its occurrence in specific historical mining districts in the Czech Republic.
Is this novákite?
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 novákite with a known reference. Novákite 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: black.
- 3Read the lusterHold the specimen under a strong light. Luster: metallic.
- 4Match the color rangeCompare against the expected color range: steel gray, black.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: aggregates, botryoidal, tarnishes.
Often confused with
Novákite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside novákite
Minerals reported to co-occur with novákite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- (Cu,Ag)₂₁As₁₀
- Mohs hardness
- 3-3.5
- Density
- 6.7 g/cm³
- Colors
- Streak
- Black
- Luster
- Metallic
- Transparency
- Opaque
- Crystal system
- Monoclinic
- Crystal habit
- Aggregates, botryoidal, tarnishes
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- In hydrothermal carbonate veins up to 20 cm thick, cutting diopside hornfels lenses in pyroxene gneiss and less commonly in mica schist (Černý Důl mine, Czech Republic)
Where rockhounds find novákite
Classic worldwide localities
- Cashin mine, Montrose Co., Colorado, USA
- Černý Důl mine, Krkonoše (Giant Mountains), Czech Republic (type locality)
Field-hunting tip
Where it forms: In hydrothermal carbonate veins up to 20 cm thick, cutting diopside hornfels lenses in pyroxene gneiss and less commonly in mica schist (Černý Důl mine, Czech Republic). If you start seeing arsenic, arsenolamprite, koutekite in float, you are in the right ground. Typical habit: aggregates, botryoidal, tarnishes. Train your eye for that shape before scanning the outcrop.








