Terminal Pleistocene lithic variability in the Western Negev (Israel): Is there any evidence for contacts with the Nile Valley?
At the end of the Pleistocene (25,000-15,000 BP), there is a shift to more arid conditions in the Negev and the Sinai corresponding to the Last Glacial Maximum. For the Nile Valley and the Levant, the lowering of the Mediterranean sea level, the expansion of the Sahara and the desiccation of some ma...
| Main Authors: | , |
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| Format: | Article |
| Language: | English |
| Published: |
University of Edinburgh
2018-03-01
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| Series: | Journal of Lithic Studies |
| Subjects: | |
| Online Access: | http://journals.ed.ac.uk/lithicstudies/article/view/2614 |