An enhydro is a quartz nodule or crystal containing a trapped pocket of ancient water, often with an air bubble that moves when the specimen is tilted. It is found within agate geodes or sedimentary deposits where silica-rich fluid was sealed in during crystal growth. Collectors prize it as a portable, prehistoric reservoir.
Is this enhydro?
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 enhydro with a known reference. Enhydro sits at Mohs 7, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Streak: white.
- 3Read the lusterHold the specimen under a strong light. Luster: vitreous.
- 4Match the color rangeCompare against the expected color range: colorless, white, brown, yellow.
- 5Look at form & habitCrystal system: trigonal. Typical habit: nodular.
Often confused with
Enhydro vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside enhydro
Minerals reported to co-occur with enhydro. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- SiO₂
- Mohs hardness
- 7
- Density
- 2.65 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Transparent
- Crystal system
- Trigonal
- Crystal habit
- Nodular
- Cleavage
- None
- Rarity
- Uncommon
- Uses
- Collector
- Host rock
- hydrothermal veins
Where rockhounds find enhydro
1 mapped spotsClassic worldwide localities
- Uruguay
- Brazil
- China
- United States
Field-hunting tip
Where it forms: hydrothermal veins. If you start seeing quartz, calcite, chalcedony in float, you are in the right ground. Typical habit: nodular. Train your eye for that shape before scanning the outcrop. In the U.S., the densest reported localities are in Florida. Start trip planning there.




