Tube Agate is a variety of chalcedony characterized by distinctive, hollow, tube-like formations that often radiate within the stone. These tubes, which can be clear or filled with contrasting minerals, are created during the deposition process in volcanic cavities. Collectors prize them for their unique structural patterns which reveal intricate details when sliced and polished.
Is this tube agate?
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 tube agate with a known reference. Tube Agate sits at Mohs 6.5-7 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Tube Agate leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Tube Agate typically shows a waxy luster.
- 4Match the color rangeCompare against the expected color range: white, gray, blue, yellow, brown.
- 5Look at form & habitCrystal system: trigonal. Typical habit: botryoidal.
Often confused with
Tube Agate vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside tube agate
Minerals reported to co-occur with tube agate. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- SiO₂
- Mohs hardness
- 6.5-7
- Density
- 2.6-2.7 g/cm³
- Streak
- White
- Luster
- Waxy
- Transparency
- Translucent
- Crystal system
- Trigonal
- Crystal habit
- Botryoidal
- Cleavage
- None
- Rarity
- Common
- Uses
- Lapidary, Collector, Decorative
- Host rock
- Rhyolite Cavities
- Typical price
- $5-50 thumbnail, $50-200 cabinet specimen
Where rockhounds find tube agate
Classic worldwide localities
- Ojo Laguna, Mexico
- Montana, USA
- Agua Nueva, Mexico
- Patagonia, Argentina
Field-hunting tip
Look in rhyolite cavities country — that is the host setting where tube agate typically forms. If you start seeing quartz, calcite, goethite in float, you are in the right ground. Field specimens usually show a botryoidal habit, so train your eye for that shape before scanning the outcrop.




