Abstract
Wadi El-Natrun depression lies about 100 km north-west of Cairo, just south of the ‘desert road’ between Cairo and Alexandria. The depression has a longitudinal morphology extending from the southeast to the northwest with average dimensions of about 60 km × 15 km. Bani Salama site lies in the eastern part of the depression, to the east of Fasda Lake, which is located at -27 m below sea level. Based on a geomorphological survey and local archaeology, we found that the site has been occupied by human societies since at least around 4000 years before the present. The site contains ruins of a temple and a castle dating back to the 12th Dynasty of the Pharaonic period (1985-1773 BC). The site also contains workshops of raw glass production dating back to Egypt’s Roman period (31 BC – AD 395). The aim of this study is to investigate the Holocene marsh deposits of Bani Salama, which are located between the Pliocene plateau and Fasda Lake. A sediment core (NAT-11) was taken from the site in June 2015. This core is investigated to understand the Holocene palaeo-geography, palaeoclimates and human impacts.
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