Rock Identifier
Fossilized Plant or Tree Bark (Lepidodendron or Sigillaria (example genera)) — sedimentary
sedimentary

Fossilized Plant or Tree Bark

Lepidodendron or Sigillaria (example genera)

Hardness: 3-4 (matrix usually shale or siltstone), Color: Grey to dark charcoal, Luster: Dull/Earthy, Crystal Structure: Amorphous/Organic, Texture: Imprinted or carbonized surface.

Identified More sedimentary

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Physical properties

Hardness: 3-4 (matrix usually shale or siltstone), Color: Grey to dark charcoal, Luster: Dull/Earthy, Crystal Structure: Amorphous/Organic, Texture: Imprinted or carbonized surface.

Formation & geological history

Formed during the Carboniferous period (approx. 300-360 million years ago) in swampy forest environments through rapid burial in anaerobic conditions.

Uses & applications

Paleontological study, educational tools, and private geological collections.

Geological facts

These giant lycopsids grew up to 30 meters tall and are major components of the coal seams found across the Northern Hemisphere.

Field identification & locations

Identified by symmetrical patterns or scale-like impressions on flat sedimentary layers. Common in coal-mining regions like the Appalachians or the UK.