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Mauritania is almost 100% Muslim, with most inhabitants adhering to the Sunni denomination. The Sufi orders, the Tijaniyah and the Qadiriyyah, have great influence not only in the country, but in Morocco, Algeria, Senegal and other neighboring countries as well.
- Slavery in Mauritania
Mauritania ratified in 1961 the Forced Labour Convention,...
- Beidane
Beidane or Bidān, also spelled Baydan or Beydan (Arabic:...
- Flag
The flag of Mauritania (Arabic: علم موريتانيا, French:...
- Seal
The Seal of Mauritania (Arabic: شعار الجمهورية الإسلامية...
- Nouakchott
Nouakchott (/ n w æ k ˈ ʃ ɒ t, n w ɑː-/; French:; Arabic:...
- Religion in Mauritania
Qur'an collection in a library in Chinguetti. The people of...
- Mauritania–Senegal Border War
The Mauritania–Senegal Border War was a conflict fought...
- National Anthem of Mauritania
Also known as " Bilāda l-ʾubāti l-hudāti l-kirām " (English:...
- Slavery in Mauritania
- Overview
- Land
- Relief
- Drainage
- Soils
- Climate
Mauritania, country on the Atlantic coast of Africa. Mauritania forms a geographic and cultural bridge between the North African Maghrib (a region that also includes Morocco, Algeria, and Tunisia) and the westernmost portion of sub-Saharan Africa. Culturally, it forms a transitional zone between the Arab-Amazigh (Berber) populations of North Africa and the African peoples in the region to the south of the Tropic of Cancer known as the Sudan (a name derived from Arabic bilād al-sūdān, “land of the Blacks”). Much of Mauritania encompasses part of the Sahara desert, and, until the drought conditions that affected most of that zone of Africa in the 1970s, a large proportion of the population was nomadic. The country’s mineral wealth includes large reserves of iron ore, copper, and gypsum, all of which are now being exploited, as well as some oil resources.
Mauritania was administered as a French colony during the first half of the 20th century and became independent on November 28, 1960. By the terms of the constitution, Islam is the official state religion, but the republic guarantees freedom of conscience and religious liberty to all. Arabic is the official language; Fula, Soninke, and Wolof are national languages. The capital, Nouakchott, is located in the southwestern part of the country.
Mauritania is bounded to the northwest by Western Sahara (formerly the Spanish Sahara), to the northeast by Algeria, to the east and southeast by Mali, and to the southwest by Senegal. Its Atlantic Ocean coastline, to the west, extends for 435 miles (700 km) from the delta of the Sénégal River northward to Cape Nouâdhibou (Cape Blanco) Peninsula.
Both Mauritania’s relief and its drainage are influenced by the aridity that characterizes the greater part of the country. The impression of immensity given by the landscape is reinforced by its flatness. The coastal plains are lower than 150 feet (45 metres), while the higher plains of the interior vary from 600 to 750 feet (180 to 230 metres). The interior plains form a plateau of which the culminating heights, occurring at different levels, form many tablelands joined to one another by very long, gentle slopes of about 2°. The topography is relieved by vestiges of cliffs (generally cuestas); by sloping plains that terminate at one end of the slope with a steep cliff or faulted scarp, which may reach heights of 900 feet (275 metres); or by inselbergs (steep-sided residual hills), of which the highest is Mount Ijill at 3,002 feet (915 metres), an enormous block of hematite.
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Mauritania may be divided into three principal geologic zones. The first of these, located in the north and northwest, consists of underlying Precambrian rock (about 2.7 billion years old), which emerges to form not only the backbone of northern Mauritania’s Reguibat ridge region but also the Akjoujt rock series that forms a vast peneplain (a land surface worn down by erosion to a nearly flat plain) studded with inselbergs. The second zone is located partly in the extreme north but mostly in the centre and east. In the north it consists of primary sandstone, which covers the Tindouf Syncline (a fold in the rocks in which the strata dip inward from both sides toward the axis); in the centre is the vast synclinal basin of Taoudeni, bounded by the Adrar, Tagant, and ʿAçâba (Assaba) plateaus. The basin is scarcely indented to the south by the Hodh Depression, with the Affollé Anticline (a fold in which the rock strata incline downward on both sides from a central axis) lying in its centre. The third zone is formed by the Senegalese-Mauritanian sedimentary basin, which includes coastal Mauritania and the lower Sénégal River valley of the southwest.
The drainage system is characterized by a lack of pattern. Normal drainage is limited to inland southwestern Mauritania, where tributaries of the Sénégal River, which forms the frontier between Mauritania and Senegal, flow southward and are subject to ephemeral flooding in summer. In the greater part of the country, however, the plateaus are cut into by wadis (dry riverbeds), where the rare floods that occur dissipate their waters into a few permanent drainage basins called guelt (singular guelta). In the wastes of the north and the east, precipitation is so rare and slight that there is practically no runoff.
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As a result of the arid phases it underwent during the Quaternary Period (2.58 million years ago to the present), the Mauritanian landscape in general presents three different aspects; these are represented by skeletal soils, regs (desert surfaces consisting of small, rounded, tightly packed pebbles), and dunes.
Skeletal soils are formed where outcrops of the underlying rock have been slightly weathered or where they have been covered with a patina or chalky crust. To these may be added the saline soils of the salt flats, formed from the caking of gypsum or of salt derived from the evaporation of former lakes. The regs form plains often of great extent, carpeted with pebbles and boulders. The dunes cover about half of the total area of the country. They are stretched out, often for several dozen miles, in long ridges known as ʿalâb, which are sometimes 300 feet (90 metres) high; they frequently overlap with one another, forming a network of domes and basins.
The climate owes its aridity to the northeastern trade winds, which blow constantly in the north and throughout most of the year in the rest of the country; the drying effect produced by these winds is increased by the harmattan, a hot, dry wind that blows from the northeast or east. With the exception of the few winter rains that occur as a result of climatic disturbances originating in the mid-latitude regions, precipitation essentially results from the rain-bearing southwesterly winds, which progressively extend throughout the southern half of the country at the height of the summer. The duration of the rainy season, as well as the total annual amount of precipitation, diminishes progressively from south to north. Thus, Sélibabi in the extreme south receives about 25 inches (635 mm) between June and October; Kiffa, farther north, receives about 14 inches (355 mm) between mid-June and mid-October; Tidjikdja receives about 7 inches (180 mm) between July and September; Atar receives 7 inches between mid-July and September; and Nouâdhibou (formerly Port-Étienne) receives between 1 and 2 inches (between 25 and 50 mm), usually between September and November. Because of opposition between the wet southwesterlies and the harmattan, precipitation often takes the form of stormy showers or squalls.
The strength of the sun and the lack of haze in these latitudes result in high temperatures. In the summer months, afternoon temperatures may reach the low 100s F (high 30s C) in most areas, and daily highs in the 110s F (40s C) are not uncommon in the interior. The average temperature in the coldest month at most stations is in the high 60s F (low 20s C), while the average temperature during the hottest month rises to the mid-70s F (mid-20s C) at Nouakchott in September, to the high 70s F (mid-20s C) at Kiffa in May, to the low 80s F (high 20s C) at Atar in July, and to the mid-80s F (high 20s C) at Néma in May.
Apr 17, 2024 · A former French colony, Mauritania achieved independence from France in 1960. Mauritania initially began as a single-party, authoritarian regime and experienced 49 years of dictatorships, flawed elections, failed attempts at democracy, and military coups. Ould Abdel AZIZ led the last coup in 2008, was elected president in 2009, and was ...
May 22, 2023 · 22 May 2023. One of Africa's newest oil producers, the Islamic Republic of Mauritania bridges the Arab Maghreb and western sub-Saharan Africa. The largely-desert country presents a cultural...
Dec 28, 2021 · Mauritanian Armed Forces: Army, Mauritanian Navy (Marine Mauritanienne), Islamic Republic of Mauritania Air Group (Groupement Aerienne Islamique de Mauritanie, GAIM); Gendarmerie (Ministry of Defense); Ministry of Interior and Decentralization: National Guard, General Group for Road Safety (2021)
The Islamic Republic of Mauritania was declared an independent state on November 28, 1960; it became a member of the United Nations in October 1961. Hubert Jules Deschamps. Struggle for postindependence stability.
Learn about the Islamic Republic of Mauritania, a vast, ethnically diverse, and arid country with an expansive coastline on the Atlantic Ocean. Find out how USAID works with Mauritania to address humanitarian, democracy, human rights, education, health, and youth challenges.
