1.8" Fossil Pine Cone Equicalastrobus Replaced By Agate Eocene Age Seeds Fruit Glyptodon preventing organic decay and enabling

preventing organic decay and enabling the formation of finely laminated limestone layers

As the quartz grows beyond this inclusion

melting and fusing sand into cool shapes that capture every grain’s little details

Members of Paralenorthis typically exhibit symmetrical

1.8" Fossil Pine Cone Equicalastrobus Replaced By Agate Eocene Age Seeds Fruit Glyptodon preventing organic decay and enablingLocation: Talsine, Morocco Weight: 0. 5 Ounces Dimensions: 1. 8 Inches Long, 0. 7 Inches Wide The item pictured is the one you will receive. Equicalastrobus petrified pine cones are fossilized conifer seed cones primarily found in the Western Sahara of Morocco, particularly near Talsine and west of Boujdour. These fossils date back to the Eocene epoch, approximately 33 to 55 million years ago. The preservation of Equicalastrobus pine cones occurs