sedimentary
Calamites (Fossil Plant)
Calamites (Genus), belonging to the class Equisetopsida
Hardness: 2-3 (surrounding matrix), Color: Light gray to tan, Luster: Dull/Earthy, Structure: Characterized by vertical ribs and horizontal nodes similar to modern bamboo
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Physical properties
Hardness: 2-3 (surrounding matrix), Color: Light gray to tan, Luster: Dull/Earthy, Structure: Characterized by vertical ribs and horizontal nodes similar to modern bamboo
Formation & geological history
Formed through the carbonization or cast-and-mold fossilization of giant horsetail plants during the Carboniferous Period (approx. 300-360 million years ago) in swampy forest environments.
Uses & applications
Primarily used for educational purposes, scientific research, and as a collector's item in the paleontology community.
Geological facts
Calamites were treelike plants that could grow up to 100 feet tall. They are the ancestors of the small modern horsetails (Equisetum) we see today.
Field identification & locations
Identify by the distinctive parallel longitudinal ribbing on the surface. Commonly found in coal-bearing shale or sandstone layers in the Appalachian region of the US and parts of Europe.
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