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The Zagros Mountains [a] are a mountain range in Iran, northern Iraq, and southeastern Turkey.The mountain range has a total length of 1,600 km (990 miles). The Zagros range begins in northwestern Iran and roughly follows Iran's western border while covering much of southeastern Turkey and northeastern Iraq.
Relief of Western, Central, and Southeastern Taurus Mountains. The Western Taurus Mountains form an arc around the Gulf of Antalya. It includes the Akdağlar, Bey Mountains, Katrancık Mountain, Kuyucak Mountains, and Geyik Mountains. The East Taşeli Plateau and Goksu River divide it from the Central Taurus Mountains. It has many peaks rising ...
The area pertaining to the hilly flanks is predominantly characterised as the foothills of the Zagros Mountains.Intercepting through the modern-day borders of Turkey, Iraq, and Iran, the region spans over 1000 miles from the lower central area of the Turkish peninsula, curling around the northern sector of the Tigris river, then running along the foothills of the Zagros Mountain range.
The Zagros are home to many threatened and endangered animals, including the Persian leopard (Panthera pardus tulliana), Syrian brown bear (Ursus arctos syriacus), mouflon (Ovis orientalis orientalis), wolf (Canis lupus), striped hyena (Hyena hyena), Blanford's fox (Vulpes cana), and Zagros Mountains mouse-like hamster (Calomyscus bailwardi).
The Amadiya valley within the Great Zab drainage basin is the third-largest valley in the Iraqi Zagros, after the Shahrazor and the Ranya Plain. [12] [13] The Great Zab rises in the highlands of the Zagros Mountains, where a climate with cold winter and annual precipitation in excess of 1,000 millimetres (39 in) prevails.
The northwestern Iranian plateau, where the Pontic and Taurus Mountains converge, is rugged country with higher elevations, a more severe climate, and greater precipitation than are found on the Anatolian sub-plateau. The region is known as the Anti-Taurus, and the average elevation of its peaks exceeds 3,000 m (9,800 ft).
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The process of collision continues to the present and as the Arabian plate is being pushed against the Iranian plate, the Zagros Mountains and the Iranian plateau are getting higher and higher. The Zagros mountain range, itself, has a totally sedimentary origin and is made primarily of limestone. In the Elevated Zagros or the Higher Zagros, the ...