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Aleppo Plateau
The Aleppo plateau ( ar, هضبة حلب ) is a low, gently undulating plateau of northern Syria. It lies at the northern end of the junction between the Arabian Plate and the African Plate at the Dead Sea Rift. The plateau lies mostly in the Aleppo Governorate and Idlib Governorate. Aleppo is located in the north-center of the plateau. Boundaries The Aleppo plateau lies immediately north of the Palmyra mountain belt. To the east it is bounded by the Euphrates river valley, which separates it from the Jazirah plateau. To the west it is bounded by the northern half of the Dead Sea Rift, namely the Orontes river valley. The Aintab plateau forms a northern continuation of the plateau that leads to the Taurus Mountains. Description The average elevation of the plateau is 400 m. The surface gradually slopes down in north-south and west-east directions. The surface undulates gently with an amplitude of 10–30 m for each wave. The lowlands are covered with combined Paleozoic an ...
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PLATEAUS OF SYRIA
In geology and physical geography, a plateau (; ; ), also called a high plain or a tableland, is an area of a highland consisting of flat terrain that is raised sharply above the surrounding area on at least one side. Often one or more sides have deep hills or escarpments. Plateaus can be formed by a number of processes, including upwelling of volcanic magma, extrusion of lava, and erosion by water and glaciers. Plateaus are classified according to their surrounding environment as intermontane, piedmont, or continental. A few plateaus may have a small flat top while others have wide ones. Formation Plateaus can be formed by a number of processes, including upwelling of volcanic magma, extrusion of lava, Plate tectonics movements and erosion by water and glaciers. Volcanic Volcanic plateaus are produced by volcanic activity. The Columbia Plateau in the north-western United States is an example. They may be formed by upwelling of volcanic magma or extrusion of lava. The un ...
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Mesozoic
The Mesozoic Era ( ), also called the Age of Reptiles, the Age of Conifers, and colloquially as the Age of the Dinosaurs is the second-to-last era of Earth's geological history, lasting from about , comprising the Triassic, Jurassic and Cretaceous Period (geology), Periods. It is characterized by the dominance of archosaurian reptiles, like the dinosaurs; an abundance of conifers and ferns; a hot Greenhouse and icehouse earth, greenhouse climate; and the tectonic break-up of Pangaea. The Mesozoic is the middle of the three eras since Cambrian explosion, complex life evolved: the Paleozoic, the Mesozoic, and the Cenozoic. The era began in the wake of the Permian–Triassic extinction event, the largest well-documented mass extinction in Earth's history, and ended with the Cretaceous–Paleogene extinction event, another mass extinction whose victims included the non-avian dinosaurs, Pterosaur, pterosaurs, Mosasaur, mosasaurs, and Plesiosaur, plesiosaurs. The Mesozoic was a time of ...
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Limestone Massif
The Limestone Massif (from French ''Le Massif Calcaire'') or Belus Massif is the highlands on the western part of the Aleppo plateau in northwestern Syria. The Massif is famed for having the Dead Cities of Syria. The Massif includes three groups of highlands; the first is the northern group of Mount Simeon and Mount Kurd. The second middle group is the group of Harim Mountains. The third southern group is the group of Zawiya Mountain Mount Zāwiya ( ar, جبل الزاوية, Jabal az-Zāwiyah) or Mount Rīḥā ( ar, جبل ريحا, Jabal Rīḥā) (also in medieval times: Banī-ʻUlaym Mountain ( ar, جبل بني عليم, Jabal Banī-ʻUlaym) is a highland region in Idli .... See also * Aleppo plateau References *Darke, Diana (2006) ''Syria'' p.132 {{coord missing, Syria Aleppo Aleppo Governorate Idlib Governorate Mountains of Syria Geography of Syria de:Tote Städte#Geografie ...
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Ghab Plain
The Ghab Plain ( ar, سَهْلُ ٱلْغَابِ, Sahl al-Ġāb, literally: Forest Plain) is a fertile depression lying mainly in the Al-Suqaylabiyah District in northwest Syria. The Orontes River, flowing north, enters the Plain near Muhradah, around 25 km north-west of Hama.Federal Research Division, 2004, p. 74.Topography and Hydrology Map of the Orontes valley
water-security.org
The valley was flooded for centuries by the waters of the Orontes River, which rendered it a swamp.Sofer, 1999, p. 205. The "Ghab project", beginning in the ...
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Zawiya Mountain
Mount Zāwiya ( ar, جبل الزاوية, Jabal az-Zāwiyah) or Mount Rīḥā ( ar, جبل ريحا, Jabal Rīḥā) (also in medieval times: Banī-ʻUlaym Mountain ( ar, جبل بني عليم, Jabal Banī-ʻUlaym) is a highland region in Idlib Governorate in northwestern Syria. Around 36 towns and villages exist in the Mount Zawiya region. The biggest towns are Rīḥā (Arīḥā) and Maʻarrat an-Nuʻmān. It was the location of the December 2011 Jabal al-Zawiya massacres. It was bombed again as part of a Syrian government and Russian offensive in September 2017.Suleiman Al-KhalidRussia, Syria intensify bombing of rebel-held Idlib, witnesses say Reuters, 24 September 2017 Location and description Mount Zāwiya forms the southern group of the Limestone Massif of the western Aleppo plateau. To the north and northwest of the mountain lies the Rouge Plain. The Ghāb Plain is on the western side. South of the mountain are the plains of Ḥamā, and on the eastern side ...
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Harim Mountains
Harim Mountains ( ar, جبال حارم, Jabal Ḥārim ) are highlands in the north of Idlib Governorate in northwestern Syria. The mountains are located in the Harim and Jisr Shughur districts of Idlib Governorate. Location and description The Harim highlands are located between 36◦22′–36◦40′ E and 35◦46′–36◦14′ N on the westernmost part of the Aleppo plateau. They cover about 600 km2. The Orontes river valley forms the western boundary. Al-Ruj Plain ( ar, سهل الروج) is located to the south. The Ruj plain and the northern Idlib plain run along the eastern boundary. The Dana plain (part of the northern Idlib plain) separates the Harim mountains from Mount Simeon to the northwest. The valley of River Afrin and Lake Amiq surround Harim mountains from north. The mountains include three massifs Mount Halqa ( ar, جبل حلقة) and Mount Barisha ( ar, جبل باريشا) form the first massif from the east. Mount Halqa (meaning "circle mountain ...
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Kurd-Dagh
Kurd Mountain or Kurd Dagh ( ku, چیای کورمنج, Çiyayê Kurmênc; tr, Kürt Dağı, officially ; ar, جبل الأكراد) is a highland region in northwestern Syria and southeastern Turkey. It is located in the Aleppo Governorate of Syria and Kilis Province of Turkey. The Kurd Mountain should not be confused with the neighboring Jabal al Akrad, which is located further southwest towards the mediterranean coastline. Location and description Kurd Mountain is a part of the Limestone Massif of northwestern Syria. The mountain is a southern continuation into the Aleppo plateau of the highlands on the western part of the Aintab plateau. The valley of River Afrin surrounds Kurd Mountain from east and south and separates it from the plain of Aʻzāz and Mount Simeon to the east, and from Mount Harim to the south. The valley of River Aswad separates Mount Kurd from Mount Amanus to the west. In Syria, it is among the four "ethnic mountains" of western Syria, along with a ...
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Afrin River
The Afrin River ( ar, نهر عفرين ''Nahr ʻIfrīn''; ( ku, Çemê Efrînê; northern Syrian vernacular: ''Nahər ʻAfrīn''; tr, Afrin Çayı) is a tributary of the Orontes River in Turkey and Syria. It rises in the Kartal Mountains in Gaziantep Province, Turkey, flows south through the city of Afrin in Syria, then reenters Turkey. It joins the Karasu at the site of the former Lake Amik, and its waters flow to the Orontes by a canal. The total length of the river is , of which is in Syria. About of the annual flow of the river comes from the Hatay Province of Turkey, while about originates in Syria. The river is impounded by the Afrin Dam to the north of the city of Afrin. The Afrin was known as ''Apre'' to the Assyrians, ''Oinoparas'' in the Seleucid era, and as ''Ufrenus'' in the Roman era. Abu'l-Fida Ismāʿīl b. ʿAlī b. Maḥmūd b. Muḥammad b. ʿUmar b. Shāhanshāh b. Ayyūb b. Shādī b. Marwān ( ar, إسماعيل بن علي بن محمود ...
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Mount Simeon
Mount Simeon or Mount Simon ( ar, جبل سمعان Jabal Simʻān ), also called Mount Laylūn ( ar, جبل ليلون, is a highland region in Aleppo Governorate in northern Syria. The mountain is located in the Mount Simeon and Aʻzāz districts of Aleppo Governorate. It is named for Symeon the Stylite a Christian who lived atop a column in the region for 37 years and for whom a large monastery complex was established. Landscape Mount Simeon is part of the Limestone Massif in the western part of the Aleppo plateau. It is located about 20 km northwest of Aleppo. The mountain runs for 50 km from north to south with a width range of 20–40 km and average elevation of 500–600 m. The highest point is Sheikh Barakāt (876 m) in the southern part of the mountain. The valley of River ʻIfrīn runs between Mount Simeon and Mount Kurd to the west. Aʻzāz valley marks the northern boundary of the mountain, beyond which lies the Aʻzāz plain and Mount Barṣa ( ...
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Quwēq
The Queiq (Modern Standard Arabic: , ''Quwayq'', ; northern Syrian Arabic: ''ʾWēʾ'', ), with many variant spellings, known in antiquity as the Belus ( grc-gre, Βήλος, ''Bēlos''), Chalos and also known in English as the Aleppo River is a river and valley of the Aleppo Governorate, Syria and Turkey. It is a -long river that flows through the northern Syrian city of Aleppo. It arises from the southern Aintab plateau in southeastern Turkey. The Akpınar River in the Kilis plain is one of the headwaters of the Queiq. The former town of Qinnasrin lay on its banks. It partly flows along the western rim of the Matah Depression. The valley has been occupied for thousands of years and in ancient times the Queiq valley was noted for its flint industries and pottery. The river dried up completely in the late 1960s, due to irrigation projects on the Turkish side of the border. Recently, water from the Euphrates has been diverted to revive the dead river, and thus revive agricul ...
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Lake Jabboul
Sabkhat al-Jabbūl or Mamlahat al-Jabbūl or Lake Jabbūl ( ar, سبخة الجبول) is a large, traditionally seasonal, saline lake and concurrent salt flats (sabkha) 30 km southeast of Aleppo, Syria, in the Bāb District of Aleppo Governorate. It is the largest natural lake in Syria and the second largest lake after the artificial Lake Assad. In 2009 the lake covered about and was relatively stable. Today the Sabkhat al-Jabbul exists within a closed basin, but during the Pleistocene the basin filled, overflowed and formed a tributary of the Euphrates. The lake traditionally flooded in the spring, shrinking back during the summer and autumn. However, starting in 1988, irrigation projects on adjacent lands started discharging significant amounts of partially saline water into the basin, stabilizing the water table and creating a lake of . Resource use Primary uses of the area include tourism, waterfowl hunting, livestock grazing on the surrounding steppe and salt e ...
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