Bronze Age sea salt production in Northwestern Iberia
The neo-glaciation, characterized by a cooling and a decrease in humidity, despite the existence of several episodes of slight climatic improvement, which occurred between the middle of the 4th and the end of the 2nd millennia BCE in the Iberian Northwest, is a well-known reality. The effects of thi...
| Autor principal: | |
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| Outros Autores: | , , , |
| Formato: | conferenceObject |
| Idioma: | eng |
| Publicado em: |
2019
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| Assuntos: | |
| Texto completo: | http://hdl.handle.net/1822/72736 |
| País: | Portugal |
| Oai: | oai:repositorium.sdum.uminho.pt:1822/72736 |