Petrified Palm is a fossilized plant material characterized by the distinct, star-like vascular bundles (often appearing as 'dots' or 'fibers') seen in cross-section. It forms when minerals like silica replace the organic structure of palm wood over millions of years, often resulting in highly polished lapidary material.

Hardness
6.5-7
Mohs
Luster
Vitreous
Transparency
Opaque

Is this petrified palm?

5-step field check

Run through these checks against the specimen in your hand. The more boxes tick, the more confident the ID.

  • 1
    Test the hardness
    Try to scratch petrified palm with a known reference. Petrified Palm sits at Mohs 6.5-7, softer than the next harder reference, harder than the previous one.
  • 2
    Name the organism
    Decide 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).
  • 3
    Check the preservation
    Preservation: Replaced by silica, with prominent rod-like structures. That controls the weight, the hardness and how the piece takes a polish.
  • 4
    Read the luster
    Hold the specimen under a strong light. Luster: vitreous.
  • 5
    Match the color range
    Compare against the expected color range: brown, tan, black, red, white, gray.

Often confused with

Petrified Palm vs. its common look-alikes, and how to tell them apart in the field.

Often found alongside petrified palm

Minerals reported to co-occur with petrified palm. 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
Vitreous
Transparency
Opaque
Rarity
Common
Uses
Lapidary, Collector, Decorative
Host rock
sedimentary strata
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 petrified palm

3 mapped spots

Classic worldwide localities

  • Texas
  • Louisiana
  • Arizona
  • India
  • Indonesia

Field-hunting tip

Where it forms: sedimentary strata. If you start seeing quartz, chalcedony, opal in float, you are in the right ground. In the U.S., the densest reported localities are in New Mexico, Texas. Start trip planning there.

Common questions

How do you identify petrified palm?+
Mohs hardness is 6.5-7. Organism: Extinct palm (genus Palmoxylon). Preservation: Replaced by silica, with prominent rod-like structures. Luster: vitreous. Common colors include brown, tan, black, red.
Where is petrified palm found?+
Notable localities include Texas; Louisiana; Arizona; India; Indonesia.
Can I find petrified palm in the United States?+
RockHoundR maps 3 petrified palm rockhounding spots across 2 U.S. states. The top states are New Mexico, Texas.
What rocks look like petrified palm?+
Petrified Palm is most often confused with Petrified Wood, Chert, Agate. A quick hardness test and a streak check separate the look-alikes faster than color alone.
What minerals are found with petrified palm?+
Petrified Palm commonly co-occurs with Quartz, Chalcedony, Opal. Spotting any of these in float or country rock is a useful trip signal.
What kind of rock does petrified palm form in?+
Where it forms: sedimentary strata. Working float back to the host body is the standard way to chase a fresh occurrence.
What is petrified palm used for?+
Petrified Palm is used in lapidary, collector, decorative.

Find petrified palm on the map

RockHoundR shows mapped rockhounding spots, access rules, and lets you log every find.

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