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Add natural flair to your walls with authentic fossils and minerals.
Xiphactinus audax 87 and 82 million years ago during the Coniacian, Santonian, and Campanian stages of the Late Cretaceous Niobrara Chalk Formatio...
View full detailsSabalites powellii, an extinct species of palm frond in the family Arcaceae. Plate approx. size: 67" tall x 44.75" wide Specimen approx. size: ...
View full detailsSabalites powellii, an extinct species of palm frond in the family Arcaceae. Dimensions approx: 44.5" x 34.25" Due to the size of this specime...
View full detailsNotogoneus osculus Natural Specimen, zero restoration with full skin intact Eocene (52.3 Million Years Ago) Green River Formation, Wyoming, USA ...
View full detailsKnightia unrestored specimen 100% Natural Eocene (51.98 Million Years Ago) Green River Formation, Wyoming, USA In Stone Fossils Private Quarry Twe...
View full detailsKnightia unrestored specimen 100% Natural Eocene (51.98 Million Years Ago) Green River Formation, Wyoming, USA In Stone Fossils Private Quarry Plat...
View full detailsKnightia unrestored specimen 100% Natural Eocene (51.98 Million Years Ago) Green River Formation, Wyoming, USA In Stone Fossils Private Quarry Plat...
View full detailsKnightia eocaena mortality layer, unrestored specimen Eocene (52.3 Million Years Ago) Green River Formation, Wyoming, USA In Stone Fossils Privat...
View full detailsBeautiful and unique copper splash butterfly art measuring approx. 4" x 5" x 0.5cm Copper is heated to a high temperature then splashed for the sha...
View full detailsBeautiful and unique copper splash butterfly art measuring approx 4" x 5" x .5cm Copper is heated to a high temperature then splashed for the shape...
View full detailsBeautiful copper splash measuring approx: 3.75" x 3" Copper is heated to a high temperature then splashed for the shape. It is then cleaned and re...
View full detailsSold as a pair for top and bottom. 4.5" polycarbonate in black. Take your fossils from out of the cabinet and securely fit them to any wall for a ...
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