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6,650 km Total LengthDrainage Basin: 3,254,555 km²

The Nile River Basin

Ancient Appellations: Iteru (Ancient Egyptian) • Nilus (Latin) • Bahr an-Nil (Arabic)

The longest river in Africa and the hydrological cradle of Egyptian civilization, providing predictable inundation and vital transport through the Sahara.

5.0
Source: Lake Victoria Mouth: Mediterranean Sea Wikidata: Q3392 ↗

Hydrological Influence & Ancient Statecraft

For over five millennia, the Nile has sustained dense human settlement amidst one of the hyper-arid deserts on Earth. The annual flooding cycle (Akhet), fed by monsoon rains in the Ethiopian Highlands via the Blue Nile, deposited millions of tons of nutrient-rich volcanic silt (kemet) upon the floodplains, yielding crop surpluses that funded the monumental pyramids, temples, and standing armies of the Pharaohs.

Agricultural Surplus & Flood Pulse Ecology

Predictable inundation permitted basin irrigation, three seasonal agricultural rotations, and the cultivation of emmer wheat, barley, flax, and papyrus reeds used for global writing materials.

Hydrological Anatomy

  • ✓Confluence of the White Nile (steady flow) and Blue Nile (seasonal flood pulse) at Khartoum
  • ✓Six historic rocky cataracts that formed natural defensive boundaries for Upper Egypt
  • ✓Vast triangular Delta fan with seven ancient distributary branches emptying into the Mediterranean

About the Nile

The Nile is a major north-flowing river in northeast Africa which empties into the Mediterranean Sea. At 7,088 kilometers (4,404 mi) long, it is the longest river in the world, although the volume of water it carries is much smaller than other major rivers such as the Amazon or the Congo. The Nile has played a central role in the environmental, economic, and cultural history of Africa for millennia.

The Nile has two major tributaries: the White Nile and the Blue Nile. The White Nile is longer and is considered to be the headwaters, yet the Blue Nile contributes over twice the water volume of the White Nile. The White Nile begins near Lake Victoria and flows through Uganda and South Sudan, while the Blue Nile begins near Lake Tana in Ethiopia and flows into Sudan from the southeast. The two rivers meet at the Sudanese capital, Khartoum. From there, the Nile flows north through the Nubian Desert to Egypt's capital, Cairo, and finally empties into the Mediterranean Sea near Alexandria, where it has formed a large river delta.

Geologically, the Nile is a young river, having followed its present course for about 15,000 years. Its drainage basin extends across eleven countries.

Encyclopedic summary adapted from Wikipedia: Nile (CC BY-SA 4.0).

Nile in Depth

Geography

The Nile is a major river in northeast Africa which flows into the Mediterranean Sea. The Nile Basin is all land that drains into the Nile, and it covers 2,927,843 km2 – about 10% of the African continent (see adjacent map). Eleven countries are wholly or partially within the basin: Burundi, Democratic Republic of the Congo, Egypt, Eritrea, Ethiopia, Kenya, Rwanda, South Sudan, Sudan, Tanzania, and Uganda. The basin covers a wide variety of climates, ecosystems, and topographies – ranging from arid, sandy deserts in the north, to flat, swampy wetlands in the middle, to rainy, forested mountains in the south.

The basin can be divided into seven regions; five of these regions encompass the longest course of the Nile.

Hydrology

Although the Nile is the longest river in the world, it does not have the largest discharge. Its flow – about 87 km3 per year – is small compared to other major rivers. The Nile's discharge is only about 1% of the Amazon, 6% of the Congo, and 12% of the Yangtze.

The annual contributions to the main Nile from the three primary tributaries are: 54% from the Blue Nile, 32% from the White Nile (including contributions from the Bahr el Ghazal and Sobat tributaries), and 14% from the Atbarah.

The highlands of the White Nile and Blue Nile both experience seasonal rain, but the White Nile's flow into the main Nile is much more constant than the Blue Nile. This is due to the many lakes and wetlands on the White Nile, which moderate the cyclic effects of seasonal rainfall.

Geological history

The Nile – like most rivers – evolved from ancestral river systems that followed significantly different courses. Over millions of years, tectonic and environmental forces shifted, separated, and merged rivers. The river assumed its current form relatively recently, about 15,000 years ago. One hypothesis describes the Nile's geological history as a sequence of five evolutionary periods.

Around 20 million years ago (mya), the west flank of the East African Rift System began to uplift, separating the African Great Lakes region from the Congo basin. About 6 mya, the ancestral Nile in Egypt was a relatively short river, originating near the modern Wadi Howar and flowing north into the Mediterranean Sea.

Ecology

The total number of fish species found in the Nile Basin is estimated at over 800. In the river alone, 128 species are found, belonging to 27 families. The majority of species belong to four families: Cichlidae (cichlids), Cyprinidae (carp), Mormyridae (elephantfish), and Mochokidae (catfish). A number of Cichlid species are found in the African Great Lakes.

In addition to fish, animals that sometimes reside in the Nile's waters include hippos, crocodiles, and African buffalo. Other water dwellers include molluscs, crabs, and shrimp.

Sections adapted from Wikipedia: Nile (CC BY-SA 4.0).

Nile: Key Facts

Key facts about Nile
Average discharge2,830 m³/s
Drainage systemNile basin
TributariesWhite Nile, Blue Nile

Facts from Wikidata Q3392 (CC0).

Dams of the Nile River

2 dams of the Nile River, ordered by structural height, with their reservoirs and generating capacity.

Dams of the Nile River
DamHeightCapacityCompleted
Aswan High Dam111 m2,100 MW1970
Merowe Dam67 m1,250 MW2009
Aswan High Dam
Image via Wikimedia Commons (author and licence on the file page).

Aswan High Dam

Rock-fill / Clay Core dam · Aswan, Egypt

Aswan High Dam is a rock-fill / clay core dam on the Nile in Aswan, Egypt, standing 111 m (364 ft) high and completed in 1970. It carries an installed hydroelectric capacity of 2,100 MW. The structure impounds Lake Nasser, about 3,575 km² on the map.

The Aswan High Dam, often called simply Aswan Dam, was built between 1960 and 1970 across the Nile in Aswan, Egypt. One of the world's largest embankment dams, it was developed by the Egyptian government with the help of the Soviet Union to control flooding, increase water storage for irrigation, and generate hydroelectricity. The dam was seen as pivotal to the country's industrialization plans. Like the Aswan Low Dam, which had been completed in 1902, the High Dam has changed the economy and culture of Egypt.

When the Aswan High Dam was completed, it was the tallest earthen dam in the world, surpassing the Chatuge Dam in the United States. It created the Lake Nasser reservoir.

It was built 7 km (4.3 mi) upstream of the Low Dam, which was built in 1902 to regulate the annual flooding of the Nile during late summer. These floods brought high water with natural nutrients and minerals that annually enriched the fertile soil along its floodplain and delta; this predictability had made the Nile valley ideal for farming since ancient times.

Adapted from Wikipedia: Aswan High Dam (CC BY-SA 4.0).

Dam type
Rock-fill / Clay Core
Structural height
111 m (364 ft)
Installed capacity
2,100 MW
Impounded river
Nile
Reservoir
Lake Nasser
Location
Aswan, Egypt
Year completed
1970
Height rank
#46 of 115 indexed
Output rank
#30 of 102 indexed
Coordinates
23.9703°, 32.8797°

Notable: Ended the historic annual Nile inundations; flooded Nubian monuments requiring UNESCO relocation.

Among the 115 dams indexed in YearMaps, Aswan High Dam ranks #46 by structural height, behind Jinping-I Dam (305 m). By installed generating capacity it ranks #30, behind Three Gorges Dam (22,500 MW).

Impounded reservoir: Lake Nasser (3,575 km², impounded 1970).

Nearest cities: Aswan (13 km), Kom Ombo (56 km), Isna (151 km).

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More about Aswan High Dam

Construction history

The earliest recorded attempt to build a dam near Aswan was in the 11th century, when the Arab polymath and engineer Ibn al-Haytham (known as Alhazen in the West) was summoned to Egypt by the Fatimid Caliph Al-Hakim bi-Amr Allah to regulate the flooding of the Nile, a task requiring an early attempt at an Aswan Dam. After his field work convinced him of the impracticality of this scheme, and fearing the Caliph's anger, he feigned madness. He was kept under house arrest from 1011 until al-Hakim's death in 1021, during which time he wrote his influential Book of Optics.

The British began construction of the first dam across the Nile in 1898. Construction lasted until 1902 and the dam was opened on 10 December 1902.

Sections adapted from Wikipedia: Aswan High Dam (CC BY-SA 4.0).

Merowe Dam
Image via Wikimedia Commons (author and licence on the file page).

Merowe Dam

Concrete-faced Rock-fill dam · Northern State, Sudan

Merowe Dam is a concrete-faced rock-fill dam on the Nile in Northern State, Sudan, standing 67 m (220 ft) high and completed in 2009. It carries an installed hydroelectric capacity of 1,250 MW. The structure impounds Merowe Reservoir.

The Merowe Dam, also known as Merowe High Dam, Merowe Multi-Purpose Hydro Project or Hamdab Dam, is a large dam near Merowe Town in northern Sudan, about 350 kilometres (220 mi) north of the capital Khartoum. Its dimensions make it the largest contemporary hydropower project in Africa. It is situated on the river Nile, close to and inundating the 4th Cataract where the river divides into multiple smaller branches with large islands in between. Merowe is a city about 40 kilometres (25 mi) downstream from the construction site at Hamdab. The main purpose for building the dam was the generation of electricity.

Adapted from Wikipedia: Merowe Dam (CC BY-SA 4.0).

Dam type
Concrete-faced Rock-fill
Structural height
67 m (220 ft)
Installed capacity
1,250 MW
Impounded river
Nile
Reservoir
Merowe Reservoir
Location
Northern State, Sudan
Year completed
2009
Height rank
#63 of 115 indexed
Output rank
#45 of 102 indexed
Coordinates
18.6678°, 32.0500°

Notable: Largest contemporary hydroelectric development in Sudan, constructed on the Fourth Cataract of the Nile.

Among the 115 dams indexed in YearMaps, Merowe Dam ranks #63 by structural height, behind Jinping-I Dam (305 m). By installed generating capacity it ranks #45, behind Three Gorges Dam (22,500 MW).

Nearest cities: Dongola (174 km), Berber (216 km), Atbara (230 km).

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More about Merowe Dam

Planning and construction

The idea of a Nile dam at the 4th cataract is quite old. The authorities of the Anglo-Egyptian Sudan proposed it several times during the first half of the 20th century. It was supposed to equalize the large annual Nile flow fluctuations, create the possibility of growing cotton and provide flood protection for the lower Nile valley. After Sudan achieved independence in 1956, Egypt decided to control the flow of Nile water that reached its own territory by building a dam and creating a reservoir —the Aswan Dam and Nasser Lake.

The Sudan military government under President Nimeiri revived the plan in 1979, now with the intention of producing hydroelectricity for Sudan's rising demand.

Environmental impact

The resettlement area is a vast area with an expected 50,000–70,000 inhabitants who would be going through a transitional period for a few years before the get acclimatised and psychologically adapted to their new life. Governing by the two eminent health impact experiences of New Halfa resettlement projects and Aswan Dam in Egypt, strategic health planning ought to start early to foresee what water born diseases and other ecological health problems (such as bilharziasis, malaria) are likely to prevail and to plan how to guard against that.

The creation of the reservoir lake will increase the surface area of the Nile by about 700 km2. Under the climatic conditions at the site, additional evaporation losses of up to 1,500,000,000 m3 per year can be expected.

Sections adapted from Wikipedia: Merowe Dam (CC BY-SA 4.0).

Merowe Dam: Key Facts

Key facts about Merowe Dam
Crest length9,280 m

Facts from Wikidata Q1921988 (CC0).

Major Dams & Engineering Projects

Monumental hydraulic infrastructure and hydroelectric stations on this basin

1 Megaproject
Height145 m
Generation5,150 MW
💧 Reservoir:Millennium Reservoir

Africa's largest hydroelectric installation built on the Blue Nile headwaters.

Nile River: Quick Answers

Which countries does the Nile River flow through?
The mapped course of the Nile River runs through or along Burundi, Tanzania, Rwanda, Uganda, South Sudan, Sudan, Egypt and Ethiopia.
Where does the Nile River begin and end?
Source: Lake Victoria / Nyungwe Forest (White Nile) & Lake Tana (Blue Nile). Mouth: Mediterranean Sea (Nile Delta, Egypt).
How long is the Nile River?
About 6,650 km (4,132 miles), draining a basin of about 3,254,555 km².
What is the tallest dam on the Nile River?
Aswan High Dam is the tallest dam recorded on the Nile River, at 111 m (364 ft), completed in 1970.
Which civilizations grew up along the Nile River?
Among them: Ancient Egypt, Kingdom of Kush / Nubia, Ptolemaic Kingdom and Fatimid Caliphate.

Countries Along the River

The main stream from source to mouth, then any country only a tributary or delta branch reaches.

  1. 1Burundi
  2. 2Tanzania
  3. 3Rwanda
  4. 4Uganda
  5. 5South Sudan
  6. 6Sudan
  7. 7Egypt
  8. 8Ethiopia

Historic Cities on the Banks

AlexandriaCairo / MemphisLuxor / ThebesAswanKhartoumJuba