Agatized picture wood is a fossilized material formed when silica-rich fluids replace the organic structure of ancient wood, preserving the cellular pattern. Collectors look for distinct 'landscape' or 'picture' patterns caused by differential staining from mineral impurities like iron and manganese. It is highly sought after by lapidary enthusiasts for its ability to take a high polish and display striking scenic motifs.
Is this agatized picture wood?
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 agatized picture wood with a known reference. Agatized Picture Wood sits at Mohs 6.5-7, softer than the next harder reference, harder than the previous one.
- 2Name the organismDecide what left the fossil before worrying about the rock. Organism: Trees and tree-like plants.
- 3Check the preservationPreservation: Cell walls replicated by silica, here as agate (chalcedony). That controls the weight, the hardness and how the piece takes a polish.
- 4Read the lusterHold the specimen under a strong light. Luster: waxy.
- 5Match the color rangeCompare against the expected color range: brown, tan, black, red, yellow, cream.
Often confused with
Agatized Picture Wood vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside agatized picture wood
Minerals reported to co-occur with agatized picture wood. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Mohs hardness
- 6.5-7
- Density
- 2.6-2.7 g/cm³
- Luster
- Waxy
- Transparency
- Opaque
- Rarity
- Common
- Uses
- Lapidary, Cabochons, Decorative, Collector
- Host rock
- sedimentary deposits
- Organism
- Trees and tree-like plants
- Preservation
- Cell walls replicated by silica, here as agate (chalcedony)
Where rockhounds find agatized picture wood
1 mapped spotsClassic worldwide localities
- Arizona, USA
- Madagascar
- Oregon, USA
- Indonesia
- Wyoming, USA
Field-hunting tip
Where it forms: sedimentary deposits. If you start seeing quartz, chalcedony, goethite in float, you are in the right ground. In the U.S., the densest reported localities are in New Mexico. Start trip planning there.








