
Fossilized Mammal Molar
This specimen is a fossilized molar tooth, likely originating from a large prehistoric mammal such as an Ice Age mastodon or similar megafauna. The item measures approximately two to three inches across, featuring a robust, bulbous crown structure with distinct ridges and cusps characteristic of herbivorous grinding teeth. The coloration is primarily an off-white to creamy beige, showing heavy mineralization and calcification consistent with long-term burial. The surface texture is uneven with pit marks and deep fissures between the cusps, which are filled with dark sediment and mineral deposits. There is evidence of significant natural wear on the chewing surface, indicating the animal used the tooth extensively during its lifetime. The overall condition is remarkably intact for a fossil of this type, showing no major structural fractures, although the surface exhibits a natural patina of age. There are no man-made markings or signatures, as it is a biological remain. The preservation suggests it may date from the Pleistocene epoch, exhibiting high quality in terms of density and fossilization detail.
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Estimated Value
$450 - $650
Basic Information
Category
Paleontological Specimens / Fossils
Appraised On
April 7, 2026
Estimated Value
$450 - $650
Item Description
This specimen is a fossilized molar tooth, likely originating from a large prehistoric mammal such as an Ice Age mastodon or similar megafauna. The item measures approximately two to three inches across, featuring a robust, bulbous crown structure with distinct ridges and cusps characteristic of herbivorous grinding teeth. The coloration is primarily an off-white to creamy beige, showing heavy mineralization and calcification consistent with long-term burial. The surface texture is uneven with pit marks and deep fissures between the cusps, which are filled with dark sediment and mineral deposits. There is evidence of significant natural wear on the chewing surface, indicating the animal used the tooth extensively during its lifetime. The overall condition is remarkably intact for a fossil of this type, showing no major structural fractures, although the surface exhibits a natural patina of age. There are no man-made markings or signatures, as it is a biological remain. The preservation suggests it may date from the Pleistocene epoch, exhibiting high quality in terms of density and fossilization detail.
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