Towards a Sustainable Stability of Coastal Zone at Rosetta Promontory/ Mouth, Egypt

Seven major old deltaic branches of the Nile River are mentioned in various historical documents and in ancient maps. At the point of discharge of the Nile into the Mediterranean, the great Nile delta has formed and furnishes the most fertile area for cultivation in the Egyptian territory . Currently, the Nile delta is embraced by two large branches of the Nile (the Rosetta and Damietta branches and their promontories). Both the Rosetta and Damietta branches discharge some freshwater directly and indirectly into the Mediterranean Sea to form the Nile estuary (also known as the Nile delta coastal area).

Sustainable Stability of Coastal Zone
Fluctuations in both quantity and quality of the Nile water reaching the Mediterranean, especially as a result of the Aswan High Dam (AHD) construction in 1965, have profoundly influenced the ecological characteristics of the river and the surrounding marine environment. These two main branches developed the Rosetta and Damietta promontories which have pro-graded during Holocene times into the Mediterranean Sea. Rosetta Branch flows downstream Delta Barrage to the North-West where it ends with Edfina Barrage which releases excess water to the Mediterranean Sea. The Rosetta Branch water serves for a wide range of functions including tourism, trading and agricultural activities, industrial and domestic water supply, fisheries and recreation.

Comments