Limb casts are natural molds formed when molten volcanic debris buries a tree limb and the wood eventually rots away, leaving a hollow cavity that is later filled by silica-rich minerals. Collectors often find these as tubular or bark-textured rocks that can be broken open to reveal druzy quartz or colorful chalcedony linings. They are highly prized for their unique internal textures which preserve the shape of the original ancient vegetation.
Is this limb cast?
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 limb cast with a known reference. Limb Cast 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. Limb Cast leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Limb Cast typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: clear, white, gray, brown, red, yellow.
- 5Look at form & habitCrystal system: trigonal. Typical habit: botryoidal.
Often confused with
Limb Cast vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside limb cast
Minerals reported to co-occur with limb cast. 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
- 2.6-2.7 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Translucent
- Crystal system
- Trigonal
- Crystal habit
- Botryoidal
- Cleavage
- None
- Rarity
- Common
- Uses
- Lapidary, Collector, Decorative
- Host rock
- Volcanic Ash Beds
- Typical price
- $10-200 depending on size and internal crystallization
Where rockhounds find limb cast
Classic worldwide localities
- Oregon, USA
- Washington, USA
- Idaho, USA
- Patagonia, Argentina
Field-hunting tip
Look in volcanic ash beds country — that is the host setting where limb cast typically forms. If you start seeing chalcedony, quartz, opal 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.





