Silicified palm wood is a fossilized material formed when silica-rich water infiltrates organic plant matter, replacing cellular structures with chalcedony. Collectors prize it for the distinct 'starburst' or 'dot' patterns visible in cross-sections, which are actually the fossilized vascular bundles of the palm plant.
Is this silicified palm 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 silicified palm wood with a known reference. Silicified Palm 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: Extinct palm (genus Palmoxylon). Age: Late Cretaceous to Miocene (about 84.9 to 11.6 million years ago).
- 3Check the preservationPreservation: Replaced by silica, with prominent rod-like structures. 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, white, red.
Often confused with
Silicified Palm Wood vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside silicified palm wood
Minerals reported to co-occur with silicified palm 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
- Translucent
- Rarity
- Common
- Uses
- Lapidary, Collector, Decorative
- Host rock
- sedimentary deposits
- Organism
- Extinct palm (genus Palmoxylon)
- Age
- Late Cretaceous to Miocene (about 84.9 to 11.6 million years ago)
- Preservation
- Replaced by silica, with prominent rod-like structures
Where rockhounds find silicified palm wood
2 mapped spotsClassic worldwide localities
- Texas, USA
- Louisiana, USA
- Mississippi, USA
- Indonesia
Field-hunting tip
Where it forms: sedimentary deposits. If you start seeing quartz, chalcedony in float, you are in the right ground. In the U.S., the densest reported localities are in Louisiana. Start trip planning there.







