Great Zab in the context of "Kalhu"

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⭐ Core Definition: Great Zab

The Great Zab or Upper Zab (Arabic: الزَّاب الْكَبِيْر, romanizedez-Zâb el-Kebîr; Kurdish: Zêy Badînan or Zêyê Mezin; Turkish: Zap; Syriac: ܙܒܐ ܥܠܝܐ, romanizedzāba ʻalya) is an approximately 400-kilometre (250 mi) long river flowing through Turkey and Iraq. It rises in Turkey near Lake Van and joins the Tigris in Iraq south of Mosul. During its course, the river collects water from many tributaries and the drainage basin of the Great Zab covers approximately 40,300 square kilometres (15,600 sq mi). The river and its tributaries are primarily fed by rainfall and snowmelt – as a result of which discharge fluctuates highly throughout the year. At least six dams have been planned on the Great Zab and its tributaries, but construction of only one, the Bekhme Dam, has commenced but was halted after the Gulf War.

The Zagros Mountains have been occupied since at least the Lower Palaeolithic, and Neanderthal occupation of the Great Zab basin has been testified at the archaeological site of Shanidar Cave. Historical records for the region are available from the end of the third millennium BCE onward. In the Neo-Assyrian period, the Great Zab provided water for irrigation for the lands around the capital city of Nimrud. The Battle of the Zab – which ended the Umayyad Caliphate – took place near a tributary of the Great Zab, and the valleys of the river provided shelter for refugees from the Mongol conquest of Iraq. During the 19th and 20th centuries, the Great Zab basin saw frequent uprisings of local Kurdish tribes striving for autonomy.

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👉 Great Zab in the context of Kalhu

Nimrud (/nɪmˈrd/; Syriac: ܢܢܡܪܕ Arabic: النمرود) is an ancient Assyrian city (original Assyrian name Kalḫu, biblical name Calah) located in Iraq, 30 kilometres (20 mi) south of the city of Mosul, and 5 kilometres (3 mi) south of the village of Selamiyah (Arabic: السلامية), in the Nineveh Plains in Upper Mesopotamia. It was a major Assyrian city between approximately 1350 BC and 610 BC. The city is located in a strategic position 10 kilometres (6 mi) north of the point that the river Tigris meets its tributary the Great Zab. The city covered an area of 360 hectares (890 acres). The ruins of the city were found within one kilometre (1,100 yd) of the modern-day Assyrian village of Noomanea in Nineveh Governorate, Iraq.

By 800 BCE, the city of Nimrud had expanded to a population of approximately 75,000, establishing it as the most populous urban center in the world at that time.

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Great Zab in the context of Urartian language

Urartian or Vannic is an extinct Hurro-Urartian language which was spoken by the inhabitants of the ancient kingdom of Urartu (Biaini or Biainili in Urartian), which was centered on the region around Lake Van and had its capital, Tushpa, near the site of the modern town of Van in the Armenian highlands, now in the Eastern Anatolia region of Turkey. Its past prevalence is unknown. While some believe it was probably dominant around Lake Van and in the areas along the upper Zab valley, others believe it was spoken by a relatively small population who comprised a ruling class.

First attested in the 9th century BCE, Urartian ceased to be written after the fall of the Urartian state in 585 BCE and presumably became extinct due to the fall of Urartu. It must have had long contact with, and been gradually totally replaced by, an early form of Armenian.

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Great Zab in the context of Lake Urmia

Lake Urmia is an endorheic salt lake in Iran. The lake is located in the Armenian Highlands, between the provinces of Azerbaijan in Iran, and west of the southern portion of the Caspian Sea. At its greatest extent, it was the largest lake in the Middle East. It is the sixth-largest saltwater lake on Earth, with a surface area of approximately 6,000 km (2,300 sq mi), a length of 140 km (87 mi), a width of 70 km (43 mi), and a maximum depth of 20 m (66 ft).

By late 2017, the lake had shrunk to 10% of its former size (and 1/60 of water volume in 1998) due to persistent general drought in Iran, but also the damming of the local rivers that flow into it, and the pumping of groundwater from the surrounding area. This dry spell was broken in 2019 and the lake began filling up once again, due to both increased rain and water diversion from the Zab River under the Urmia Lake Research Programme. The trend reversed again in early 2020s, and a combination of drought and administrative mismanagement caused a renewed acute drop in water levels. Based on NASA's satellite imagery, the lake has almost entirely dried up by September 2025.

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Great Zab in the context of Nimrud

Nimrud (/nɪmˈrd/; Syriac: ܢܢܡܪܕ Arabic: النمرود) is an ancient Assyrian city (original Assyrian name Kalḫu, biblical name Calah) located in Iraq, 30 kilometres (20 mi) south of the city of Mosul, and 5 kilometres (3 mi) south of the village of Selamiyah (Arabic: السلامية), in the Nineveh Plains in Upper Mesopotamia. It was a major Assyrian city between approximately 1350 BC and 610 BC. The city is located in a strategic position 10 kilometres (6 mi) north of the point that the river Tigris meets its tributary the Great Zab. The city covered an area of 360 hectares (890 acres). The ruins of the city were found within one kilometre (1,100 yd) of the modern-day Assyrian village of Noomanea in Nineveh Governorate, Iraq.

The name Nimrud was recorded as the local name by Carsten Niebuhr in the mid-18th century. In the mid 19th century, biblical archaeologists proposed the Assyrian name Kalḫu (the Biblical Calah), based on a description of the travels of Nimrod in Genesis 10.

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Great Zab in the context of Battle of the Zab

The Battle of the Zab (Arabic: معركة الزاب), also referred to in scholarly contexts as Battle of the Great Zāb River, took place on January 25, 750, on the banks of the Great Zab in what is now the modern country of Iraq. It spelled the end of the Umayyad Caliphate and the rise of the Abbasid Caliphate, which would last from 750 to 1258.

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Great Zab in the context of Adiabene

Adiabene (Greek: Αδιαβηνή, Classical Syriac: ܚܕܝܐܒ) was an ancient kingdom in northern Mesopotamia, corresponding to the northwestern part of ancient Assyria. The size of the kingdom varied over time; initially encompassing an area between the Zab Rivers, it eventually gained control of Nineveh and starting at least with the rule of Monobazos I (late 1st-century BCE), Gordyene became an Adiabenian dependency. It reached its zenith under Izates II, who was granted the district of Nisibis by the Parthian king Artabanus II (r. 12–40) as a reward for helping him regain his throne. Adiabene's eastern borders stopped at the Zagros Mountains, adjacent to the region of Media. Arbela served as the capital of Adiabene.

The formation of the kingdom is obscure. The first instance of a recorded Adiabenian ruler is in 69 BCE, when an unnamed king of Adiabene participated in the battle of Tigranocerta as an ally of the Armenian king Tigranes the Great (r. 95–55 BCE). However, coinage implies the establishment of a kingdom in Adiabene around 164 BCE, following the disintegration of Greek Seleucid rule in the Near East. Adiabene was conquered by the Parthian king Mithridates I (r. 171–132 BCE) between 145–141 BCE, and served at least from the reign of Mithridates II (r. 124–91 BCE) as an integral part of the Parthian realm.

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Great Zab in the context of Bradost (mountain)

Bradost or Chia-y Bradost (Nawakhin), a mountain range over 5,000 feet above sea level and about 25 miles long, stretches northwest from the Rawanduz river opposite the town of Rawanduz in Erbil Governorate, Kurdistan Region,Iraq, to Rubari kuchuk, a tributary of the Great Zab.

The Shanidar Cave, a Neanderthal archaeological site, lies about 15 km N-W from its peak.

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