Atlas Mountains
| Atlas Mountains | |
|---|---|
 Toubkal Mountain in Toubkal National Park in the High Atlas | |
| Highest point | |
| Peak | Toubkal |
| Elevation | 4,165 m (13,665 ft) |
| Geography | |
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| |
| Countries | Algeria, Morocco and Tunisia |
| Geology | |
| Age of rock | Precambrian |
The Atlas Mountains (Berber: ⵉⴷⵓⵔⴰⵔ ⵏ ⵓⴰⵟⵍⴰⵙ - idurar n Waṭlas, Arabic: جبال الأطلس, Classical Arabic: Daran; Dyrin) is a mountain range across the northwestern stretch of Africa extending about 2,500 km (1,600 mi) through Algeria, Morocco and Tunisia. The highest peak is Toubkal, with an elevation of 4,165 metres (13,665 ft) in southwestern Morocco. The Atlas ranges separate the Mediterranean and Atlantic coastlines from the Sahara Desert. The population of the Atlas Mountains is mainly Berbers. The terms for 'mountain' in some Berber languages are adrar and adras, believed to be cognate with the toponym.
The mountains have been home to a number of plant and animal species unique in Africa, often more like those of Europe; many of them are endangered and some have already gone extinct. Examples include the Barbary Macaque, the Atlas Bear (Africa's only species of bear; now extinct), the Barbary Leopard, the Barbary stag, Barbary Sheep, the Barbary Lion (extinct in the wild), the Atlas Mountain Badger, the North African Elephant (extinct), the African Aurochs (extinct), Cuvier's Gazelle, the Northern Bald Ibis, Dippers, the Atlas mountain viper, the Atlas Cedar, the European Black Pine, and the Algerian Oak.
Geology
The basement rock of most of Africa was formed in the Precambrian (approximately 4.54 - 0.57 billion years ago) and is much older than the Atlas mountains lying in Africa. The Atlas formed during three subsequent phases of Earth's history.
The first tectonic deformation phase involves only the Anti-Atlas, which was formed in the Paleozoic Era (~300 million years ago) as the result of continental collisions. North America, Europe and Africa were connected millions of years ago.
The Anti-Atlas mountains are believed to have originally been formed as part of Alleghenian orogeny. These mountains were formed when Africa and America collided, and were once a chain rivaling today's Himalayas. Today, the remains of this chain can be seen in the Fall line in the eastern United States. Some remnants can also be found in the later formed Appalachians in North America.
A second phase took place during the Mesozoic Era (before ~65 My) and consisted of a widespread extension of the Earth's crust that rifted and separated the continents mentioned above. This extension was responsible for the formation of many thick intracontinental sedimentary basins including the present Atlas. Most of the rocks forming the surface of the present High Atlas were deposited under the ocean at that time.
Finally, in the Tertiary Period (~65 million to ~1.8 million years ago), the mountain chains that today comprise the Atlas were uplifted as the land masses of Europe and Africa collided at the southern end of the Iberian peninsula. Such convergent tectonic boundaries occur where two plates slide towards each other forming a subduction zone (if one plate moves underneath the other) and/or a continental collision (when the two plates contain continental crust). In the case of the Africa-Europe collision, it is clear that tectonic convergence is partially responsible for the formation of the High Atlas, as well as for the closure of the Strait of Gibraltar and the formation of the Alps and the Pyrenees. However, there is a lack of evidence for the nature of the subduction in the Atlas region, or for the thickening of the Earth's crust generally associated with continental collisions. In fact, one of the most striking features of the Atlas to geologists is the relative small amount of crustal thickening and tectonic shortening despite the important altitude of the mountain range. Recent studies suggest that deep processes rooted in the Earth's mantle may have contributed to the uplift of the High and Middle Atlas.[1][2]
Natural resources
The Atlas are rich in natural resources. There are deposits of iron ore, lead ore, copper, silver, mercury, rock salt, phosphate, marble, anthracite coal, and natural gas among other resources.
Subranges of the Atlas Mountains
The range can be divided into four general regions:
- Tell Atlas (Algeria, Tunisia).
- Saharan Atlas (Algeria).
- Aurès Mountains (Algeria, Tunisia).
- Middle Atlas, High Atlas, and Anti-Atlas (Morocco).
Middle Atlas range
The Middle Atlas is a portion of the Atlas mountain range lying completely in Morocco. The Middle Atlas is the westernmost of three Atlas Mountains chains that define a large, plateaued basin extending eastward into Algeria. South of the Middle Atlas and separated by the Moulouya and Oum Er-Rbia rivers, the High Atlas stretches for 700 kilometres (430 mi) with a succession of peaks among which ten reach above 4,000 metres (13,000 ft). North of the Middle Atlas and separated by the Sebou River, the Rif mountains are an extension of the Baetic Cordillera (Baetic mountains, which include the Sierra Nevada) in the south of Spain.
High Atlas
The High Atlas in central Morocco rises in the west at the Atlantic coast and stretches in an eastern direction to the Moroccan-Algerian border. At the Atlantic and to the southwest the range drops abruptly and makes an impressive transition to the coast and the Anti-Atlas range. To the north, in the direction of Marrakech, the range descends less abruptly.
On the heights of Ouarzazate the massif is cut through by the Draa valley which opens southward. Here, water runs in some places, forming clear basins. It is mainly inhabited by Berber people, who live in small villages and cultivate the high plains of Ourika Valley.
Near Barrage Cavagnac, there is a hydroelectric dam that has created the artificial lake Lalla Takerkoust. The lake serves also as a source for fish for the local fishermen.
The largest villages and towns of the area are Ouarzazate, Tahanaoute, Amizmiz, Imlil, Tin Mal and Ijoukak.
Anti-Atlas ranges
The Anti-Atlas extends from the Atlantic Ocean in the southwest of Morocco toward the northeast to the heights of Ouarzazate and further east to the city of Tafilalt (altogether a distance of approximately 500 kilometres or 310 miles). In the south it borders the Sahara. The easternmost point of the anti-Atlas is the Djebel Sarhro mountains and its eastern boundary is set by sections of the High Atlas range.
Saharan Atlas range
The Saharan Atlas of Algeria is the eastern portion of the Atlas mountain range. Though not as high as the Grand Atlas, they are far more imposing than the Tell Atlas range that runs to the north of them and closer to the coast. The highest peak in the range is the 2,236 m (7,336 ft) high Djebel Aissa. They mark the northern edge of the Sahara Desert. The mountains see some rainfall and are better suited to agriculture than the plateau region to the north. Today most of the population of the region are Berbers (Imazighen).
Tell Atlas range
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The Tell Atlas is a mountain chain over 1,500 kilometres (930 mi) in length, belonging to the Atlas mountain ranges and stretching from Morocco, through Algeria to Tunisia. It parallels the Mediterranean coast. Together with the Saharan Atlas to the south it forms the northernmost of two more or less parallel ranges which gradually approach one another towards the east, merging in Eastern Algeria. At the western ends at the Middle Atlas range in Morocco. The area immediately to the south of this range is high plateau, with lakes in the wet season and salt flats in the dry.
Aurès mountain range
The Aurès Mountains of Algeria and Tunisia are the farthest eastern portion of the Atlas mountain range.
See also
References and notes
- ^ UAB.es Potential field modelling of the Atlas lithosphere
- ^ UAB.es Crustal structure under the central High Atlas Mountains (Morocco) from geological and gravity data, P. Ayarza, et al., 2005, Tectonophysics, 400, 67-84
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