Hydronováčekite is a rare uranyl arsenate mineral characterized by its distinctive bright yellow, platy crystals. It is typically found in the oxidized zones of uranium deposits and is highly prized by collectors for its strong fluorescence under ultraviolet light.
Is this hydronováčekite?
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 hydronováčekite with a known reference. Hydronováčekite 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. Hydronováčekite leaves a yellow streak.
- 3Read the lusterHold the specimen under a strong light. Hydronováčekite typically shows a pearly luster.
- 4Match the color rangeCompare against the expected color range: yellow, greenish-yellow.
- 5Look at form & habitCrystal system: tetragonal. Typical habit: platy crystals, micaceous aggregates.
Often confused with
Hydronováčekite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside hydronováčekite
Minerals reported to co-occur with hydronováčekite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- H₂Mg(UO₂)₂(AsO₄)₂·n H₂O
- Mohs hardness
- 2-2.5
- Density
- 3.32 g/cm³
- Colors
- Streak
- Yellow
- Luster
- Pearly
- Transparency
- Transparent
- Crystal system
- Tetragonal
- Crystal habit
- Platy Crystals, Micaceous Aggregates
- Cleavage
- Perfect Basal
- Fluorescence
- Bright Yellow-green Under UV Light
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Hydrothermal Uranium-bearing Veins
- Typical price
- $50-300 per thumbnail/small specimen
Where rockhounds find hydronováčekite
Classic worldwide localities
- Jáchymov, Czech Republic
- Schneeberg, Germany
- Wölsendorf, Germany
Field-hunting tip
Look in hydrothermal uranium-bearing veins country — that is the host setting where hydronováčekite typically forms. If you start seeing uraninite, schröckingerite, heinrichite in float, you are in the right ground. Field specimens usually show a platy crystals, micaceous aggregates habit, so train your eye for that shape before scanning the outcrop.






