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. Streak: yellow.
- 3Read the lusterHold the specimen under a strong light. Luster: pearly.
- 4Match the color rangeCompare against the expected color range: yellow, greenish-yellow.
- 5Look at form & habitCrystal system: triclinic. Typical habit: platy crystals, micaceous aggregates.
Often confused with
Hydronováčekite vs. its common look-alikes, and how to tell them apart in the field.

How to tell apart: Luster reads pearly on Hydronováčekite and waxy on Nováčekite.

How to tell apart: Streak differs, so Hydronováčekite leaves yellow, Autunite leaves pale yellow; luster reads pearly on Hydronováčekite and vitreous, pearly on {001} on Autunite.

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
- Colors
- Streak
- Yellow
- Luster
- Pearly
- Transparency
- Transparent
- Crystal system
- Triclinic
- 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
Where rockhounds find hydronováčekite
Classic worldwide localities
- Jáchymov, Czech Republic
- Schneeberg, Germany
- Wölsendorf, Germany
Field-hunting tip
Where it forms: hydrothermal uranium-bearing veins. If you start seeing uraninite, schröckingerite, heinrichite in float, you are in the right ground. Typical habit: platy crystals, micaceous aggregates. Train your eye for that shape before scanning the outcrop.



