Hadrosaurid Dinosaur Bone Fragment

Hadrosauridae gen. et sp. indet. (Possibly Edmontosaurus cf. annectens based on typical regional matrix)Body fossil; Vertebrate remains; Petrified osteological material

Hadrosaurid Dinosaur Bone Fragment

Geological Period

Upper Cretaceous

Estimated Age

66 to 75 million years

Preservation Type

Permineralization with significant iron-oxide replacement, leading to the characteristic reddish-brown coloration.

Condition Assessment

Fair; the specimen is an isolated, weathered fragment with high levels of erosion and lack of diagnostic articular surfaces.

Taxonomic Classification

Phylum: Chordata, Class: Reptilia, Order: Ornithischia, Family: Hadrosauridae

Morphological Description

Fragmentary limb bone or vertebral process showing distinct cancellous (spongy) internal bone structure. Surface exhibits longitudinal striations and vascular pitting characteristic of dinosaurian cortical bone.

Rock Matrix

Ferruginous sandstone/siltstone matrix; heavily oxidized mudstone indicative of terrestrial fluvial or floodplain depositional environments.

Formation & Location

Likely Hell Creek Formation (USA) or Judith River Group (USA/Canada); common in the Badlands of Montana, Wyoming, or Alberta.

Size & Dimensions

Approximately 5-8 cm in length; representing a small fragment of a much larger skeletal element.

Value & Rarity

Estimated Market Value

$15 - $40 USD

Auction Estimate

$20 - $50 USD

Rarity Assessment

Common; isolated fragments such as this ('dinosaur chunks') are frequently found in Late Cretaceous terrestrial lag deposits.

Scientific Significance

Provides evidence of Late Cretaceous herbivorous megafauna distribution; contributes to paleoecological mapping of terrestrial environments prior to the K-Pg extinction event.

Preparation Recommendations

Requires minimal preparation; stabilize with a reversible consolidant like Paraloid B-72 if crumbling occurs; keep in a low-humidity environment to prevent further oxidation.

Notable Features

The specimen displays highly visible trabecular bone structure on the cross-section, which is a key diagnostic feature distinguishing it from ordinary rock.

Identified on 3/29/2026