Hyalite is a clear, colorless variety of opal often found as bubbly or globular botryoidal crusts. It is most famous among collectors for its spectacular, intense neon-green fluorescence under ultraviolet light, which is caused by trace amounts of uranium impurities. It typically forms as a coating on rocks within volcanic environments or pegmatites.
Spotting hyalite in the field
Field marks- 1
Colorless, glassy, botryoidal crusts that look like drops of clear glue on rock
- 2
Glows a strong green under shortwave ultraviolet light
- 3
Very light in the hand, soft, and often quite thin
Hyalite is the best reason to carry a UV light. Trace uranium makes it fluoresce a vivid green that is unmistakable and visible from several feet away in the dark, so a night sweep of a known outcrop finds material that is nearly invisible by day. It forms as glassy botryoidal coatings in volcanic rock and pegmatite. Bring a shortwave lamp, wear UV-blocking glasses, and never look into the lamp.
Before you collect
Shortwave UV lamps damage eyes and skin. Wear UV-rated eye protection, keep the beam off skin, and never point it at another person.
Straight answers
- Is it worth cutting?
- Rarely cut. It is a specimen mineral, and its value is the fluorescence and the botryoidal form.
- What is it really worth?
- Modest. Bright fluorescence and well-formed clear botryoidal crusts on attractive matrix carry the value.
- Can you legally keep it?
- Ordinary personal-use collecting rules apply. The trace uranium is far too low to raise handling or transport concerns.
Often confused with
Hyalite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside hyalite
Minerals reported to co-occur with hyalite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- SiO₂·nH₂O
- Mohs hardness
- 5.5-6.5
- Density
- 2.0-2.1 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Transparent
- Crystal system
- Amorphous
- Crystal habit
- Botryoidal, crusts, globular, stalactitic
- Cleavage
- None
- Fluorescence
- Intense bright green under SW and LW UV
- Rarity
- Common
- Uses
- Collector, Specimen
- Host rock
- volcanic rhyolite, pegmatites, hydrothermal cavities
Where rockhounds find hyalite
2 mapped spotsClassic worldwide localities
- Zacatecas, Mexico
- San Luis Potosi, Mexico
- Karlovarský, Czech Republic
- Georgia, USA
- North Carolina, USA
Field-hunting tip
Where it forms: volcanic rhyolite, pegmatites, hydrothermal cavities. If you start seeing quartz, topaz, cassiterite in float, you are in the right ground. Typical habit: botryoidal, crusts, globular, stalactitic. Train your eye for that shape before scanning the outcrop. In the U.S., the densest reported localities are in Utah. Start trip planning there.





