
sedimentary
Fossil / Permineralized Bone
Tyrannosaurus rex fossil (Hydroxylapatite replaced by various minerals)
Hardness: 5 (variable based on mineral replacement); Color: Dark brown to black (likely iron or manganese staining); Luster: Dull to sub-metallic; Structure: Porous micro-structure of original bone; Specific gravity: Varies by mineral content.
- Hardness
- 5 (variable based on mineral replacement)
- Color
- Dark brown to black (likely iron or manganese staining)
- Luster
- Dull to sub-metallic
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Physical properties
Hardness: 5 (variable based on mineral replacement); Color: Dark brown to black (likely iron or manganese staining); Luster: Dull to sub-metallic; Structure: Porous micro-structure of original bone; Specific gravity: Varies by mineral content.
Formation & geological history
Formed via permineralization where minerals like silica or calcite fill the pores of bone buried in sediment. This specimen originates from the Late Cretaceous period (approx. 66-68 million years ago).
Uses & applications
Predominantly used for scientific research, museum exhibitions, and high-end private collections.
Geological facts
This appears to be a Tyrannosaurus rex skull. The most complete T. rex ever found, 'Sue', is housed at the Field Museum. T. rex fossils are found exclusively in the Hell Creek, Lance, and Ferris formations of North America.
Field identification & locations
Identify in the field by looking for 'bone texture' (the spongy appearance of cancellous bone) in sedimentary layers. Usually found in floodplains or river channel sandstone. Professional excavation is required for preservation.
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