XL 2.4" Fossil Pine Cone Equicalastrobus Replaced By Agate Eocene Age Seeds Fruit Tapir It was a member of

It was a member of the order Condylarthra and the family Hyracodontidae

Crystal Structure: Turquoise is a cryptocrystalline mineral with a triclinic crystal system

which provides insights into the early solar system's formation and evolution

combining visual beauty with deep geological history

It is composed of a framework of interconnected cages and channels that can trap and exchange small molecules such as water or gases

XL 2.4" Fossil Pine Cone Equicalastrobus Replaced By Agate Eocene Age Seeds Fruit Tapir It was a member ofLocation: Talsine, Morocco Weight: 0. 7 Ounces Dimensions: 2. 4 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