Triceratops Frill Fossil Value Guide

- Period
- 66-68 Million Years Ago
- Origin
- United States
- Materials
- Fossilized Bone, Mineralized Calcium Phosphate
- Category
- Fossil
This specimen is a genuine fragment of the iconic bony frill from a Triceratops, recovered from the renowned Hell Creek Formation in the United States. These fossils are highly collectible as they represent the final era of the dinosaurs and showcase the unique vascular structure used for defense and thermal regulation.
What Is Triceratops Frill Fossil Worth?
The typical price range for Triceratops Frill Fossil is $150 - $165 based on recent sales. However, values can vary depending on the item's condition, rarity, and other factors such as:
- The presence of clear surface details, such as distinct vascular channels, significantly increases the specimen's market value.
- Size and thickness of the fragment, with larger or more robust sections of the frill commanding higher prices within the $150-$165 range.
- The quality of preservation and the lack of excessive restoration or chemical stabilizers.
- Provenance linking the piece specifically to the Hell Creek Formation, a premier site for Late Cretaceous fossils.
How to Identify Triceratops Frill Fossil?
- Look for the characteristic 'honeycomb' or porous internal texture unique to fossilized dinosaur bone marrow.
- Verify the presence of distinct vascular grooves on the surface where blood vessels once nourished the frill.
- Check for the heavy mineralization and dark coloration typical of specimens sourced from the Hell Creek Formation's Cretaceous sediment.
- Ensure the specimen is composed of mineralized calcium phosphate rather than modern bone or resin casts.
History of Triceratops Frill Fossil
This specimen originates from the Hell Creek Formation, a world-famous geological site that preserves the final days of the dinosaur era. The frill of a Triceratops served multiple purposes, including defense, thermal regulation, and species recognition. Finding fragments like this is a direct link to the Late Cretaceous period, approximately 66 to 68 million years ago.
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Tuff | Geology 1501 | ECU
geology.ecu.edu
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