Fossilized Dinosaur Bone Fragment
Paleontological Specimens

Fossilized Dinosaur Bone Fragment

This specimen is a significant fragment of fossilized dinosaur bone, specifically sourced from the Morrison Formation, dating to the Late Jurassic period (approximately 150 million years ago). The piece measures roughly 3 to 4 inches across and displays a characteristic sub-triangular, tabular shape. The surface exhibits a distinct 'honeycomb' or porous texture, which is the permineralized cancellous (spongy) bone structure. Coloration is a mottled combination of creamy whites, light grays, and yellowish-tan mineral staining, likely due to iron or silica replacement during the fossilization process. One edge shows a smoother, denser cortical bone layer, while the broken faces reveal the internal vascular architecture. There are visible stress fractures and minor chipping along the periphery, consistent with natural weathering and excavation. The specimen lacks specific diagnostic features to identify a genus, but the size and density suggest a large vertebrate, potentially a sauropod or large theropod common to the Morrison strata. The craftsmanship of nature is evident in the preservation of the microscopic pore spaces, indicating high-quality permineralization.

Estimated Value

$125-$225

Basic Information

Category

Paleontological Specimens

Appraised On

May 13, 2026

Estimated Value

$125-$225

Additional Details Provided By Owner

User Provided Information

Fossil from Morrison formation

Item Description

This specimen is a significant fragment of fossilized dinosaur bone, specifically sourced from the Morrison Formation, dating to the Late Jurassic period (approximately 150 million years ago). The piece measures roughly 3 to 4 inches across and displays a characteristic sub-triangular, tabular shape. The surface exhibits a distinct 'honeycomb' or porous texture, which is the permineralized cancellous (spongy) bone structure. Coloration is a mottled combination of creamy whites, light grays, and yellowish-tan mineral staining, likely due to iron or silica replacement during the fossilization process. One edge shows a smoother, denser cortical bone layer, while the broken faces reveal the internal vascular architecture. There are visible stress fractures and minor chipping along the periphery, consistent with natural weathering and excavation. The specimen lacks specific diagnostic features to identify a genus, but the size and density suggest a large vertebrate, potentially a sauropod or large theropod common to the Morrison strata. The craftsmanship of nature is evident in the preservation of the microscopic pore spaces, indicating high-quality permineralization.

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