fossil

Fossilized bone or tooth fragment

Mineralized vertebrate bone; exact taxon indeterminate from image

AI-generated identification · may be incorrect

Tan, porous, irregular fragment with a dense outer surface and hollow/cancellous interior; likely mineralized apatite and calcite. Hardness is approximately 4–6 Mohs, with earthy to dull luster; visible texture is consistent with bone rather than a crystalline mineral.

Identified September 22, 2026More fossil →

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Physical properties

Formation & geological history

A vertebrate bone or tooth was buried, then progressively mineralized as groundwater replaced or filled its original tissues, commonly during the Cenozoic or Mesozoic. Exact age requires geological context and laboratory testing.

Uses & applications

Primarily a paleontological or educational collectible; not generally used in industry, construction, or jewelry.

Geological facts

The porous internal structure resembles trabecular bone, but the small size and damage prevent reliable species identification. A professional paleontologist can distinguish bone from tooth using cross-section, density, and microscopic structure.

Field identification & locations

Commonly found in sedimentary deposits, especially river gravels, caves, deserts, and marine or lake beds. Look for repeating porous architecture, mineral infill, and a heavier feel than modern bone; avoid destructive testing.