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2,800 km Total LengthDrainage Basin: 879,790 km²

Tigris & Euphrates Basin

Ancient Appellations: Idigna & Buranun (Sumerian) • Diklat & Purattu (Akkadian) • Dijla & Furat (Arabic)

The storied Fertile Crescent river system where humanity first invented agriculture, urban city-states, the wheel, and cuneiform writing.

5.0
Source: Taurus Mountains Mouth: Shatt al-Arab into the Persian GulfWikidata: Q3608991 ↗
Tigris
Tigris. Image via Wikimedia Commons (author and licence on the file page).

Hydrological Influence & Ancient Statecraft

Between the twin currents of the Tigris and Euphrates arose Mesopotamia ("the land between the rivers"). Unlike the gentle, predictable Nile, the Tigris and Euphrates flooded violently and unpredictably in late spring when mountain snows melted, necessitating complex communal canal engineering, dykes, and legal codes (such as Hammurabi’s Code) to manage water rights and combat soil salinization.

Agricultural Surplus & Flood Pulse Ecology

Large-scale gravity-fed canal networks turned arid alluvium into bountiful fields of date palms, barley, sesame, and grazing pastures for livestock.

Hydrological Anatomy

  • ✓Euphrates: Slower flowing, 2,800 km in length, highly vulnerable to evaporation in the Syrian desert
  • ✓Tigris: Faster flowing, carrying twice the water volume of the Euphrates, with steep gorge downcuts
  • ✓Convergence into the Shatt al-Arab marshlands before debouching into the Persian Gulf
  • ✓Extensive alluvial plains with shifting river beds over millennia

About the Tigris

The Tigris ( TY-griss; see below) is the eastern of the two great rivers that define Mesopotamia, the other being the Euphrates. The river flows south from the mountains of the Armenian Highlands through the Syrian and Arabian Deserts, before merging with the Euphrates and reaching to the Persian Gulf.

The Tigris passes through historical cities such as Mosul, Tikrit, Samarra and Baghdad. It is also home to archaeological sites and ancient religious communities, including the Mandaeans, who use it for baptism. In ancient times the Tigris nurtured the Assyrian Empire, with remnants such as the relief of King Tiglath-Pileser.

Today, the Tigris faces modern threats from geopolitical instability, dam projects, poor water management, and climate change, raising concerns about its sustainability. Efforts to protect and preserve the river's legacy are ongoing, with local archaeologists and activists working to safeguard its future.

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

Tigris in Depth

Geography

The Tigris is 1,750 km (1,090 mi) long, rising in the Taurus Mountains of eastern Turkey about 25 km (16 mi) southeast of the city of Elazığ and about 30 km (19 mi) south of the valley of the Euphrates. The river then flows for 400 km (250 mi) through Southeastern Turkey before forming part of the Syria-Turkey border. This stretch of 44 km (27 mi) is the only part of the river that is located in Syria. Some of its affluences are Garzan, Anbarçayi, Batman, and the Great and the Little Zab.

Close to its confluence with the Euphrates, the Tigris splits into several channels. First, the artificial Shatt al-Hayy branches off, to join the Euphrates near Nasiriyah. Second, the Shatt al-Muminah and Majar al-Kabir branch off to feed the Central Marshes.

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

Tigris: Key Facts

Key facts about Tigris
Length1,850 km
Average discharge1,014 m³/s
Drainage basin375,000 km²
SourceLake Hazar
MouthShatt al-Arab
Drainage systemPersian Gulf Basin
TributariesLittle Zab, Great Zab, Botan River, Khabur, 'Adhaim

Facts from Wikidata Q35591 (CC0).

About the Euphrates

The Euphrates ( yoo-FRAY-teez; see below) is the longest and one of the most historically important rivers of West Asia. Together with the Tigris, it is one of the two defining rivers of Mesopotamia (lit. 'the land between the rivers'). Originating in Turkey, the Euphrates flows through Syria and Iraq to join the Tigris in the Shatt al-Arab in Iraq, which empties into the Persian Gulf.

The Euphrates is the fifteenth-longest river in Asia and the longest in West Asia, at about 2,780 km (1,730 mi), with a drainage area of 440,000 km2 (170,000 mi2) that covers six countries.

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

Euphrates in Depth

Course

The Euphrates is the longest river of West Asia. It emerges from the confluence of the Kara Su or Western Euphrates (450 kilometres (280 mi)) and the Murat Su or Eastern Euphrates (650 kilometres (400 mi)) 10 kilometres (6.2 mi) upstream from the town of Keban in southeastern Turkey. Daoudy and Frenken put the length of the Euphrates from the source of the Murat River to the confluence with the Tigris at 3,000 kilometres (1,900 mi), of which 1,230 kilometres (760 mi) is in Turkey, 710 kilometres (440 mi) in Syria and 1,060 kilometres (660 mi) in Iraq. The same figures are given by Isaev and Mikhailova. The length of the Shatt al-Arab, which connects the Euphrates and the Tigris with the Persian Gulf, is given by various sources as 145–195 kilometres (90–121 mi).

History

The early occupation of the Euphrates basin was limited to its upper reaches; that is, the area that is popularly known as the Fertile Crescent. Acheulean stone artifacts have been found in the Sajur basin and in the El Kowm oasis in the central Syrian steppe; the latter together with remains of Homo erectus that were dated to 450,000 years old. In the Taurus Mountains and the upper part of the Syrian Euphrates valley, early permanent villages such as Abu Hureyra – at first occupied by hunter-gatherers but later by some of the earliest farmers, Jerf el Ahmar, Mureybet and Nevalı Çori became established from the eleventh millennium BCE onward.

Natural history

The Euphrates flows through a number of distinct vegetation zones. Although millennia-long human occupation in most parts of the Euphrates basin has significantly degraded the landscape, patches of original vegetation remain. The steady drop in annual rainfall from the sources of the Euphrates toward the Persian Gulf is a strong determinant for the vegetation that can be supported. In its upper reaches the Euphrates flows through the mountains of Southeast Turkey and their southern foothills which support a xeric woodland. Plant species in the moister parts of this zone include various oaks, pistachio trees, and Rosaceae (rose/plum family). The drier parts of the xeric woodland zone supports less dense oak forest and Rosaceae.

Economy

Throughout history, the Euphrates has been of vital importance to those living along its course. With the construction of large hydropower stations, irrigation schemes, and pipelines capable of transporting water over large distances, many more people now depend on the river for electricity and drinking water than in the past. Syria's Euphrates Lake is the most important source of drinking water for the city of Aleppo, 75 kilometres (47 mi) to the west of the river valley. The lake also supports a modest state-operated fishing industry. Through a newly restored power line, the Haditha Dam in Iraq provides electricity to Baghdad.

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

Euphrates: Key Facts

Key facts about Euphrates
Length2,800 km
Average discharge818 m³/s
Drainage basin673,000 km²
MouthShatt al-Arab
Drainage systemPersian Gulf Basin
TributariesKhabur River, Balikh River

Facts from Wikidata Q34589 (CC0).

Dams of the Tigris and Euphrates

4 dams of the Tigris and Euphrates, ordered by structural height, with their reservoirs and generating capacity.

Dams of the Tigris and Euphrates
DamHeightCapacityCompleted
Atatürk Dam169 m2,400 MW1992
Ilısu Dam135 m1,200 MW2020
Mosul Dam (Saddam Dam)113 m1,052 MW1986
Tabqa Dam (al-Thawra)60 m824 MW1973

Atatürk Dam

Zoned Rock-fill dam · Şanlıurfa, Turkey

Atatürk Dam is a zoned rock-fill dam on the Euphrates in Şanlıurfa, Turkey, standing 169 m (554 ft) high and completed in 1992. It carries an installed hydroelectric capacity of 2,400 MW. The structure impounds Lake Atatürk.

The Atatürk Dam (Turkish: Atatürk Barajı), originally the Karababa Dam, is the fourth largest dam in the world and it is a zoned rock-fill dam with a central core on the Euphrates River on the border of Adıyaman Province and Şanlıurfa Province in the Southeastern Anatolia Region of Turkey. Built both to generate electricity and to irrigate the plains in the region, it was renamed in honour of Mustafa Kemal Atatürk (1881–1938), the founder of the Turkish Republic. The construction began in 1983 and was completed in 1990. The dam and the hydroelectric power plant, which went into service after the upfilling of the reservoir was completed in 1992, are operated by the State Hydraulic Works (DSİ). The reservoir created behind the dam, called Atatürk Reservoir (Turkish: Atatürk Baraj Gölü), is the third largest in Turkey.

The dam is situated 23 km (14 mi) northwest of Bozova, Şanlıurfa Province, on state road D-875 from Bozova to Adıyaman. Centerpiece of the 22 dams on the Euphrates and the Tigris, which comprise the integrated, multi-sector, Southeastern Anatolia Project (Turkish: Güney Doğu Anadolu Projesi, known as GAP), it is one of the world's largest dams.

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

Dam type
Zoned Rock-fill
Structural height
169 m (554 ft)
Installed capacity
2,400 MW
Impounded river
Euphrates
Reservoir
Lake Atatürk
Location
Şanlıurfa, Turkey
Year completed
1992
Height rank
#21 of 115 indexed
Output rank
#28 of 102 indexed
Coordinates
37.4789°, 38.5175°

Notable: Centerpiece of the Southeastern Anatolia Project (GAP); key to Tigris-Euphrates water diplomacy.

Among the 115 dams indexed in YearMaps, Atatürk Dam ranks #21 by structural height, behind Jinping-I Dam (305 m). By installed generating capacity it ranks #28, behind Three Gorges Dam (22,500 MW).

Nearest cities: Adıyaman (39 km), Şanlıurfa (42 km), Malatya (101 km).

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Atatürk Dam: Key Facts

Key facts about Atatürk Dam
Crest length1,820 m
Officially opened1992

Facts from Wikidata Q753776 (CC0).

Ilısu Dam

Concrete-face rock-fill dam · Mardin / Şırnak, Turkey

Ilısu Dam is a concrete-face rock-fill dam on the Tigris in Mardin / Şırnak, Turkey, standing 135 m (443 ft) high and completed in 2020. It carries an installed hydroelectric capacity of 1,200 MW. The structure impounds Ilısu Reservoir.

The Ilısu Dam (Turkish pronunciation: [ɯɫɯˈsu]) is a concrete-face rock-fill dam on the Tigris near the village of Ilısu and along the border of Mardin and Şırnak Provinces in Turkey. It is one of the 22 dams of the Southeastern Anatolia Project and its purpose is hydroelectric power production, flood control and water storage. When operational, the dam will support a 1,200 MW power station and will form a 10.4 billion m3 reservoir. Construction of the dam began in 2006 and was originally expected to be completed by 2016. As part of the project, the much smaller Cizre Dam is to be constructed downstream for irrigation and power. The dam has drawn international controversy, because it will flood portions of ancient Hasankeyf and necessitate the relocation of people living in the region. Because of this, the dam lost international funding in 2008. Most historical structures in Hasankeyf were moved to the new Hasankeyf prior to the filling of the dam. The dam began to fill its reservoir in late July 2019.

Due to rainfall, the dam has achieved water levels up to 100m above the river bed and stored 5 billion cubic meters of water.

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

Dam type
Concrete-face rock-fill
Structural height
135 m (443 ft)
Installed capacity
1,200 MW
Impounded river
Tigris
Reservoir
Ilısu Reservoir
Location
Mardin / Şırnak, Turkey
Year completed
2020
Height rank
#38 of 115 indexed
Output rank
#47 of 102 indexed
Coordinates
37.5317°, 41.8350°

Notable: Crown jewel of Turkey's Southeastern Anatolia Project (GAP), impounding 10.4 billion cubic meters.

Among the 115 dams indexed in YearMaps, Ilısu Dam ranks #38 by structural height, behind Jinping-I Dam (305 m). By installed generating capacity it ranks #47, behind Three Gorges Dam (22,500 MW).

Nearest cities: Siirt (47 km), Batman (73 km), Nusaybin (75 km).

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Background

Beginning in 1954 the Turkish government surveyed 53 kilometres (33 miles) of the Tigris river downstream of Diyarbakır with the aim of identifying suitable locations for a hydroelectric power plant at an elevation below 550 metres (1,800 ft). Turkey's Electric Power Resources Survey and Development Administration (EIE) included 10 potential sites in its 1971 Tigris River Pre-Investigation Report. By 1975, the EIE had completed a technical and economic evaluation of the sites. Ilısu was selected as the preferred site for geological reasons. A feasibility study and final design by international consultants (1980–82) resulted in a recommendation to construct both the Ilısu Dam and the Cizre Dam downstream.

Construction

As part of early and ongoing construction, 52 km (32 mi) of roads are subject to raising and repairing work. A 110 m (361 ft) long temporary bridge was constructed upstream of the dam site which is supported by 30 sections of steel pipe. Additionally, a 250 m (820 ft) permanent steel-girder bridge with concrete supports was constructed just downstream of the dam. Construction of new Ilısu and Koçtepe villages were underway as well as the relocation of major portions of Hasankeyf. Excavations for the main body of the dam began in May 2011 and the first loads of fill were laid in January 2012. Diversion of the Tigris River began during a ceremony on 29 August 2012. As of April 2014, the project is 60% complete while the resettlement of Hasankeyf is 73% complete.

Design

The Ilısu Dam will be a 135 m (443 ft) high and 1,820 m (5,971 ft) wide rock-fill embankment dam with a structural volume of 43,900,000 m3 (35,590 acre⋅ft). It will be 15 m (49 ft) wide at its crest and 610 m (2,001 ft) wide at its base. The dam will have an overflow spillway on its right bank which will be controlled by eight radial gates which will pour into four chutes before the water reaches a plunge pool. Its power station will be above ground and will contain 6 x 200 MW Francis turbine-generators with an expected annual generation of 3,833 GWh and gross hydraulic head of 122.6 m (402 ft).

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

Ilısu Dam: Key Facts

Key facts about Ilısu Dam
Crest length1,820 m

Facts from Wikidata Q1659316 (CC0).

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

Mosul Dam (Saddam Dam)

Earth-fill embankment dam · Nineveh, Iraq

Mosul Dam (Saddam Dam) is an earth-fill embankment dam on the Tigris in Nineveh, Iraq, standing 113 m (371 ft) high and completed in 1986. It carries an installed hydroelectric capacity of 1,052 MW. The structure impounds Lake Mosul.

Mosul Dam (Arabic: سد الموصل), formerly known as Saddam Dam (سد صدام), is the largest dam in Iraq. It is located on the Tigris river in the western governorate of Nineveh, upstream of the city of Mosul. The dam serves to generate hydroelectricity and provide water for downstream irrigation. At full capacity, the structure holds about 11.1 cubic kilometres (2.7 cu mi) of water and provides electricity to the 1.7 million residents of Mosul.

The dam's main 750-megawatt (1,010,000 hp) power station contains four 187.5-megawatt (251,400 hp) Francis turbine–generators. A pumped-storage hydroelectricity power plant with a capacity of 250 megawatts (340,000 hp) and a run-of-the-river dam downstream with a 62-megawatt (83,000 hp) capacity also belong to the Mosul Dam scheme. It is the fourth largest dam in the Middle East, as measured by reserve capacity, capturing snowmelt from Turkey, some 70 miles (110 km) north.

Built in the 1980s on a karst foundation, concerns over the dam's instability have led to major remediation and rehabilitation efforts since the 2003 U.S. invasion of Iraq.

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

Dam type
Earth-fill embankment
Structural height
113 m (371 ft)
Installed capacity
1,052 MW
Impounded river
Tigris
Reservoir
Lake Mosul
Location
Nineveh, Iraq
Year completed
1986
Height rank
#45 of 115 indexed
Output rank
#48 of 102 indexed
Coordinates
36.6303°, 42.8231°

Notable: Largest dam in Iraq with a 3.2-km crest; built on soluble gypsum karst requiring continuous grouting.

Among the 115 dams indexed in YearMaps, Mosul Dam (Saddam Dam) ranks #45 by structural height, behind Jinping-I Dam (305 m). By installed generating capacity it ranks #48, behind Three Gorges Dam (22,500 MW).

Nearest cities: Dahuk (31 km), Mosul (43 km), Tall Afar (44 km).

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History

To ensure as many of the archeological sites were inspected before being submerged under the lake that would form behind the dam, the Iraqi government invited several foreign delegations to participate. This rescue operation included the British Archaeological Expedition to Iraq as a prominent participant. In 1985, one of their sites, Tell Deir Situn garnered an Assyrian fibula, some Hellenic oil lamps, and a Seleucid coin of Alexander Balas.

In 2010, following a massive drought, the ruins of an ancient palace were discovered in the reservoir. The palace, which is approximately 3,400 years old, is believed to have belonged to the Mitanni. The first excavation occurred in 2019 by a joint Kurdish-German team.

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

Mosul Dam (Saddam Dam): Key Facts

Key facts about Mosul Dam (Saddam Dam)
Crest length3,400 m

Facts from Wikidata Q606561 (CC0).

Tabqa Dam (al-Thawra)
Image via Wikimedia Commons (author and licence on the file page).

Tabqa Dam (al-Thawra)

Earth-fill dam · Raqqa, Syria

Tabqa Dam (al-Thawra) is an earth-fill dam on the Euphrates in Raqqa, Syria, standing 60 m (197 ft) high and completed in 1973. It carries an installed hydroelectric capacity of 824 MW. The structure impounds Lake Assad, about 675 km² on the map.

The Euphrates Dam (Arabic: سَدُّ الْفُرَاتِ, romanized: Sadd al-Furāt; Kurdish: Bendava Firatê; Classical Syriac: ܣܟܪܐ ܕܦܪܬ, romanized: Sekro d'Frot), most commonly known as Tabqa Dam; formerly known as al-Thawra Dam during the Ba'athist era, is an embankment dam on the Euphrates, located 40 kilometres (25 mi) upstream from the city of Raqqa in Raqqa Governorate, Syria. The city of Al-Thawrah is located immediately south of the dam. The dam is 60 metres (200 ft) high and 4.5 kilometres (2.8 mi) long and is the largest dam in Syria. Its construction led to the creation of Euphrates Lake, Syria's largest water reservoir. The dam was constructed between 1968 and 1973 with help from the Soviet Union. At the same time, an international effort was made to excavate and document as many archaeological remains as possible in the area of the future lake before they would be flooded by the rising water. When the flow of the Euphrates was reduced in 1974 to fill the lake behind the dam, a dispute broke out between Syria and Iraq (which is downstream) that was settled by intervention from Saudi Arabia and the Soviet Union.

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

Dam type
Earth-fill
Structural height
60 m (197 ft)
Installed capacity
824 MW
Impounded river
Euphrates
Reservoir
Lake Assad
Location
Raqqa, Syria
Year completed
1973
Height rank
#73 of 115 indexed
Output rank
#54 of 102 indexed
Coordinates
35.8814°, 38.5683°

Notable: Largest dam in Syria; creates Lake Assad (610 km²), Syria's primary freshwater reservoir.

Among the 115 dams indexed in YearMaps, Tabqa Dam (al-Thawra) ranks #73 by structural height, behind Jinping-I Dam (305 m). By installed generating capacity it ranks #54, behind Three Gorges Dam (22,500 MW).

The Reservoir: Buhayrat al-Assad

Buhayrat al-Assad is the water body held back by Tabqa Dam (al-Thawra), with a mapped surface of about 675 km², impounded in 1974. The area is computed from the mapped outline and is approximate.

Nearest cities: Madinat ath Thawrah (5 km), Ar Raqqah (41 km), Manbij (90 km).

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Project history

In 1927, when Syria was a French mandate, it was proposed to build a dam in the Euphrates near the Syria–Turkey border. After Syria became independent in 1946, the feasibility of the project was studied and shelved. In 1957, the Syrian government reached an agreement with the Soviet Union to build a dam in the Euphrates. In 1960, as part of the United Arab Republic, Syria signed an agreement with West Germany for a financing loan. In 1965, after Syria left the UAR, a new agreement was reached with the Soviet Union. A special government department was created to oversee the construction. In the early 1960s Swedish geomorphologist Åke Sundborg worked as an advisor on the dam project with the task of estimating the amount and fate of sediment entering the dam.

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

Tabqa Dam (al-Thawra): Key Facts

Key facts about Tabqa Dam (al-Thawra)
Crest length4,500 m

Facts from Wikidata Q372823 (CC0).

Tigris and Euphrates: Quick Answers

Which countries does the Tigris and Euphrates flow through?
The mapped course of the Tigris and Euphrates runs through or along Turkey, Syria, Iraq and Iran.
Where does the Tigris and Euphrates begin and end?
Source: Taurus Mountains / Armenian Highlands (Eastern Turkey). Mouth: Shatt al-Arab into the Persian Gulf.
What is the tallest dam on the Tigris and Euphrates?
Atatürk Dam is the tallest dam recorded on the Tigris and Euphrates, at 169 m (554 ft), completed in 1992.
Which civilizations grew up along the Tigris and Euphrates?
Among them: Sumer, Akkadian Empire, Babylonian Empire, Assyrian Empire and Abbasid Caliphate.

Countries Along the River

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

  1. 1Turkey
  2. 2Syria
  3. 3Iraq
  4. 4Iran

Historic Cities on the Banks

UrBabylonNinevehBaghdadBasraCtesiphon