Nile Delta

Nile Delta

The Nile Delta is the area formed in Lower Egypt, where the Nile River spreads out and drains into the Mediterranean Sea. It is one of the world’s largest river deltas—from Alexandria in the west to Port Said in the east. It covers 240 km (150 mi) of the Mediterranean coastline and is a rich agricultural region. From north to south, the Delta is approximately 160 km (99 mi) in length. The Delta begins slightly downriver from Cairo.

From north to south, the Delta is approximately 160 km (99 mi) in length. It covers some 240 km (150 mi) of coastline from west to east. The Delta is sometimes divided into sections, with the Nile dividing into two main distributaries, the Damietta and the Rosetta, flowing into the Mediterranean at port cities with the same name. In the past, the Delta had several distributaries, but these have been lost due to flood control, silting and changing relief. One such defunct distributary is Wadi Tumilat.


The Suez Canal is east of the Delta and enters the coastal Lake Manzala northeast of the Delta. To the northwest are three other coastal lakes or lagoons: Lake Burullus, Lake Idku and Lake Mariout.

The Nile is considered an “arcuate” delta (arc-shaped), as it resembles a triangle or flower when seen from above. Some scholars, such as Aristotle, have written that the Delta was constructed for agricultural purposes due to the drying of the region of Egypt.

In the modern-day, the outer edges of the Nile Delta are eroding, and some coastal lagoons have seen increasing salinity levels as their connection to the Mediterranean Sea increases. Since the Delta no longer receives an annual supply of nutrients and sediments from upstream due to the construction of the Aswan Dam, the soils of the floodplains have become poorer, and large amounts of fertilizers are now used. Topsoil in the Delta can be as much as 21 m (70 ft) in depth.


People have lived in the Nile Delta region for thousands of years, and it has been intensively farmed for at least the last five thousand years. The Delta was a principal constituent of Lower Egypt, and many archaeological sites exist in and around the Delta. Artefacts belonging to ancient sites have been found on the Delta’s coast. The Rosetta Stone was found in the Delta in 1799 in the port city of Rosetta (an anglicized version of the name Rashid). In July 2019, a small Greek temple, ancient granite columns, treasure-carrying ships, and bronze coins from the reign of Ptolemy II, dating back to the third and fourth centuries BC, were found at the sunken city of Heracleion, colloquially known as Egypt’s Atlantis. The investigations by Egyptian and European divers were led by the underwater archaeologist Franck Goddio. They also uncovered a devastating historic temple (the city’s main temple) underwater off Egypt’s north coast.

In January 2019, archaeologists led by Mostafa Waziri working in the Kom Al-Khelgan area of the Nile Delta discovered tombs from the Second Intermediate Period and burials from the Naqada II era. The burial site contained the remains of animals, amulets and scarabs carved from faience, round and oval pots with handles, flint knives, and broken and burned pottery. All burials included skulls and skeletons in the bending position and were not remarkably well-preserved.

Ancient branches of the Nile

Records from ancient times (such as by Ptolemy) show that the Delta had seven distributaries or branches (from east to west):

  • the Pelusiac,
  • the Tanitic,
  • the Mendesian,
  • the Phatnitic (or Phatmetic),
  • the Sebennytic,
  • the Bolbitine, and
  • the Canopic (also called the Herakleotic and the Agathodaemon

Due to flood control, there are now only two main branches, silting and changing relief: the Damietta (corresponding to the Phatnitic) to the east and the Rosetta (comparing to the Bolbitine) in the western part of the Delta. The Delta used to flood annually, but this ended with the construction of the Aswan Dam.


About 39 million people live in the Delta region. Outside of major cities, population density in the delta averages 1,000/km2 (2,600/sq mi) or more. Alexandria is the largest city in the Delta, with an estimated population of more than 4.5 million. Other large cities in the Delta include Shubra El Kheima, Port Said, El Mahalla El Kubra, Mansura, Tanta, and Zagazig.


During autumn, parts of the Nile River are red with lotus flowers. The Lower Nile (North) and the Upper Nile (South) have plants that grow in abundance. The Upper Nile plant is the Egyptian lotus, and the Lower Nile plant is the Papyrus Sedge (Cyperus papyrus), although it is not nearly as plentiful as it once was and is becoming quite rare.

Several hundred thousand water birds winter in the Delta, including the world’s largest concentrations of little gulls and whiskered terns. Other birds making their homes in the Delta include grey herons, Kentish plovers, shovelers, cormorants, egrets and ibises.

Fish found in the Delta include the flathead grey mullet and soles. Frogs, turtles, tortoises, mongooses, and the Nile monitor are other animals in the Delta. Nile crocodiles and hippopotamus, two widespread animals in the Delta during antiquity, are no longer found there.


The Delta has a hot desert climate (Köppen: BWh) like the rest of Egypt, but its northernmost part, as is the case with the rest of the northern coast of Egypt, which is the wettest region in the country, has relatively moderate temperatures, with highs usually not surpassing 31 °C (88 °F) in the summer. The Delta experiences its hottest temperatures in July and August, with a maximum average of 34 °C (93 °F). Winter temperatures are generally in the range of 9 °C (48 °F) at night to 19 °C (66 °F) in the daytime. The Nile Delta region becomes humid during the winter with cooler temperatures and rain. Only 100–200 mm (4–8 in) of rain falls on the delta area during an average year, most of which falls in winter.

Sea level rise

Egypt’s Mediterranean coastline experiences significant loss of land to the sea, sometimes amounting to 90 m (100 yds) a year. The low-lying Nile Delta area, in particular, is vulnerable to sea-level rise associated with global warming. This effect is exacerbated by the lack of sediments deposited since the Aswan Dam’s construction. If the polar ice caps were to melt, much of the northern Delta, including the ancient port city of Alexandria, could disappear under the Mediterranean. A 30 cm (12 in) rise in sea level could affect about 6.6% of the total land cover area in the Nile Delta region. At 1 m (3 ft 3 in) sea-level rise, an estimated 887 thousand people could be at risk of flooding and displacement. About 100 km2 (40 sq mi) of vegetation, 16 km2 (10 sq mi) of wetland, 402 km2 (160 sq mi) cropland, and 47 km2 (20 sq mi) of urban area land could be destroyed, flooding approximately 450 km2 (170 sq mi). Some areas of the Nile Delta’s agricultural land have been rendered saline due to sea-level rise; farming has been abandoned in some places, while sand has been brought in from elsewhere to reduce the effect. In addition to agriculture, the Delta’s ecosystems and tourist industry could be negatively affected by global warming. Food shortages resulting from climate change could lead to seven million “climate refugees” by the end of the 21st century. Nevertheless, environmental damage to the Delta is not currently one of Egypt’s priorities.

The Delta’s coastline has also undergone significant changes in geomorphology due to the reclamation of coastal dunes and lagoons to form new agricultural land and fish farms, as well as the expansion of coastal urban areas.