Periglacial deformations of bear long bones
DOI:
https://doi.org/10.26485/BP/1957/5/8Keywords:
periglacial climate, Pleistocene deposits, Torell LandAbstract
In 1934, the author found a deformed bear bone on Torell Land. The bone's bending and cracking were caused by differences in the conditions of its buried and exposed parts. This example demonstrates the potential for long bone fractures in periglacial climates.
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Published
2025-12-17
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