
Fossilized Dinosaur Bone Fragment in Sandstone Matrix
This specimen is a fossilized fragment of a dinosaur bone encased in a light-colored sandstone matrix, originating from the Late Jurassic Morrison Formation (approximately 150 million years old). The piece measures roughly 3 to 4 inches in width and fits within a human hand, exhibiting a consistent buff or tan coloration throughout both the matrix and the fossilized material. The bone structure is visible as a relatively smooth, linear impressions and mineralized surface that contrasts with the coarser, granular texture of the surrounding sedimentary rock. Notable features include longitudinal grain patterns indicative of cortical bone, though the specimen is heavily weathered with indistinct margins. The condition is raw and unprepared, with significant natural erosion and missing sections where the bone once extended. There are no visible maker's marks, as it is a natural specimen, but it possesses the diagnostic 'pitted' texture often found in permineralized dinosaur remains from this famous geological unit. The craftsmanship is entirely natural, resulting from millions of years of mineralization and geological pressure. Quality is considered fair for a field-found fragment, suitable for study or as a representative geologic sample rather than a museum-quality display piece.
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Estimated Value
$35.00 - $60.00
Basic Information
Category
Paleontological Specimens / Fossils
Appraised On
May 13, 2026
Estimated Value
$35.00 - $60.00
Additional Details Provided By Owner
User Provided Information
Fossil from Morrison formation
Item Description
This specimen is a fossilized fragment of a dinosaur bone encased in a light-colored sandstone matrix, originating from the Late Jurassic Morrison Formation (approximately 150 million years old). The piece measures roughly 3 to 4 inches in width and fits within a human hand, exhibiting a consistent buff or tan coloration throughout both the matrix and the fossilized material. The bone structure is visible as a relatively smooth, linear impressions and mineralized surface that contrasts with the coarser, granular texture of the surrounding sedimentary rock. Notable features include longitudinal grain patterns indicative of cortical bone, though the specimen is heavily weathered with indistinct margins. The condition is raw and unprepared, with significant natural erosion and missing sections where the bone once extended. There are no visible maker's marks, as it is a natural specimen, but it possesses the diagnostic 'pitted' texture often found in permineralized dinosaur remains from this famous geological unit. The craftsmanship is entirely natural, resulting from millions of years of mineralization and geological pressure. Quality is considered fair for a field-found fragment, suitable for study or as a representative geologic sample rather than a museum-quality display piece.
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