fossil

Fossil bone fragment, likely mammalian

Fossilized bone; exact taxon indeterminate from image

AI-generated identification · may be incorrect

Tan, porous, irregular fragment with apparent cortical bone and internal vascular cavities; hardness typically about 3–5 Mohs, earthy to dull luster, and specific gravity commonly 1.8–2.5 after mineralization. The texture appears mineral-replaced rather than ordinary limestone or modern bone.

Identified August 24, 2026More fossil →

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Physical properties

Formation & geological history

Formed when buried bone was permineralized by groundwater carrying silica, calcite, or iron minerals; age cannot be determined visually and may range from thousands to millions of years. Common in sedimentary deposits, especially river gravels, deserts, caves, and badlands.

Uses & applications

Primarily a collecting, educational, and decorative specimen; scientifically useful for paleontology. Value depends heavily on diagnostic anatomy, preservation, provenance, and legal collecting status.

Geological facts

The honeycomb-like pores and dense outer cortex are characteristic of bone, though weathered limestone can look similar. A thin section or laboratory analysis is needed for confident identification and dating.

Field identification & locations

Look for a dense outer cortical layer surrounding porous or channelled interior, unlike uniformly granular rock; avoid destructive tests. Common fossil-bone regions include the western United States, Mongolia, Patagonia, and parts of Africa.