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{{short description|desert in Africa}}{{other uses|Sahara (disambiguation)}}{{pp-vandalism|small=yes}}{{Use dmy dates|date=May 2014}}

| coordinates_ref =
| elevation =| elevation_m =| elevation_ft =| elevation_ref =| length =| length_mi =| length_km = 4800| length_orientation =| length_note =| width =| width_mi =| width_km = 1800| width_orientation =| width_note =| area =| area_mi2 =| area_km2 = 9200000| depth =| depth_ft =| depth_m =| type =| age =| border =| topo =| traversed =| river =
| footnotes =| embed =}}File:Evening Pass over the Sahara Desert and the Middle East.ogv|thumb|upright=1.35|This video over the Sahara and the Middle East was taken by the crew of Expedition 29 on board the International Space StationInternational Space StationFile:Libya 4985 Tadrart Acacus Luca Galuzzi 2007.jpg|thumb|Tadrart Acacus desert in western LibyaLibyaFile:SafsafOasis SAR comparison.jpg|thumb|The top image shows the Safsaf Oasis on the surface of the Sahara. The bottom (using radar) is the rock layer underneath, revealing black channels cut by the meandering of an ancient river that once fed the oasisoasisThe Sahara ({{IPAc-en|s|ə|ˈ|h|ɑːr|ə}}, {{IPAc-en|s|ə|ˈ|h|ær|ə}}; , {{transl|ar|ALA|aṣ-ṣaḥrāʼ al-kubrá}}, 'the Greatest Desert') is a desert located on the African continent. It is the largest hot desert in the world, and the third largest desert overall after Antarctica and the Arctic.WEB,weblink Largest Desert in the World, 30 December 2011, Its area of {{convert|9200000|km2}}JOURNAL, Cook, Kerry H., Vizy, Edward K., Detection and Analysis of an Amplified Warming of the Sahara Desert, Journal of Climate, 2015, 28, 16, 6560, 10.1175/JCLI-D-14-00230.1, 2015JCli...28.6560C, is comparable to the area of China or the United States.WEB, Is the World Full or Empty?,weblink Story Maps, Story Maps, 19 October 2018, The name 'Sahara' is derived from a dialectal Arabic word for "desert", {{transl|ar|ALA|ṣaḥra}} ( {{IPAc-ar|ˈ|S|a|H||r|a}}).[ "Sahara."] Online Etymology Dictionary. Douglas Harper, Historian. Retrieved 25 June 2007.WEB,weblink English-Arabic online dictionary,, 28 December 2006, 12 June 2010, BOOK, Wehr, Hans, A Dictionary of Modern Written Arabic (Arabic-English), 1994, Otto Harrassowitz, Wiesbaden, 978-0-87950-003-0, 4th, Hans Wehr, 589, BOOK, al-Ba'labakkī, Rūḥī, al-Mawrid: Qāmūs 'Arabī-Inklīzī, 2002, Dār al-‘Ilm lil-Malāyīn, Beirut, 16th, 689, Arabic, The desert comprises much of North Africa, excluding the fertile region on the Mediterranean Sea coast, the Atlas Mountains of the Maghreb, and the Nile Valley in Egypt and Sudan. It stretches from the Red Sea in the east and the Mediterranean in the north to the Atlantic Ocean in the west, where the landscape gradually changes from desert to coastal plains. To the south, it is bounded by the Sahel, a belt of semi-arid tropical savanna around the Niger River valley and the Sudan Region of Sub-Saharan Africa. The Sahara can be divided into several regions including: the western Sahara, the central Ahaggar Mountains, the Tibesti Mountains, the Aïr Mountains, the Ténéré desert, and the Libyan Desert.For several hundred thousand years, the Sahara has alternated between desert and savanna grassland in a 20,000 year cyclweblink caused by the precession of the Earth's axis as it rotates around the Sun, which changes the location of the North African Monsoon. The area is next expected to become green in about 15,000 years (17,000 AD).


(File:Africa satellite orthographic.jpg|thumb|A geographical map of Africa, showing the ecological break that defines the Saharan area)File:Hoggar8.jpg|thumb|An oasis in the Ahaggar MountainsAhaggar MountainsFile:Saharan Dust off West Africa.jpg|thumb|An intense Saharan dust storm sent an extensive dust plume northwestward over the Atlantic OceanAtlantic OceanFile:Algérie 2009.jpg|thumb|right|Butte naturally sculpted by the wind ]]The Sahara covers large parts of Algeria, Chad, Egypt, Libya, Mali, Mauritania, Niger, Western Sahara, Sudan and Tunisia. It covers {{convert|9|e6km2|sqmi}}, amounting to 31% of Africa. If all areas with a mean annual precipitation of less than 250 mm were included, the Sahara would be {{convert|11|e6km2|sqmi}}. It is one of three distinct physiographic provinces of the African massive physiographic division.The Sahara is mainly rocky hamada (stone plateaus); ergs (sand seas – large areas covered with sand dunes) form only a minor part, but many of the sand dunes are over {{convert|180|m}} high.Strahler, Arthur N. and Strahler, Alan H. (1987) Modern Physical Geography Third Edition. New York: John Wiley & Sons. {{ISBN|0-471-85064-0}}. p. 347 Wind or rare rainfall shape the desert features: sand dunes, dune fields, sand seas, stone plateaus, gravel plains (reg), dry valleys (wadi), dry lakes (oued), and salt flats (shatt or chott).{{WWF ecoregion|id=pa1327|name=Sahara desert|accessdate=30 December 2007}} Unusual landforms include the Richat Structure in Mauritania.Several deeply dissected mountains, many volcanic, rise from the desert, including the Aïr Mountains, Ahaggar Mountains, Saharan Atlas, Tibesti Mountains, Adrar des Iforas, and the Red Sea Hills. The highest peak in the Sahara is Emi Koussi, a shield volcano in the Tibesti range of northern Chad.The central Sahara is hyperarid, with sparse vegetation. The northern and southern reaches of the desert, along with the highlands, have areas of sparse grassland and desert shrub, with trees and taller shrubs in wadis, where moisture collects. In the central, hyperarid region, there are many subdivisions of the great desert: Tanezrouft, the Ténéré, the Libyan Desert, the Eastern Desert, the Nubian Desert and others. These extremely arid areas often receive no rain for years.To the north, the Sahara skirts the Mediterranean Sea in Egypt and portions of Libya, but in Cyrenaica and the Maghreb, the Sahara borders the Mediterranean forest, woodland, and scrub eco-regions of northern Africa, all of which have a Mediterranean climate characterized by hot summers and cool and rainy winters. According to the botanical criteria of Frank WhiteWickens, Gerald E. (1998) Ecophysiology of Economic Plants in Arid and Semi-Arid Lands. Springer, Berlin. {{ISBN|978-3-540-52171-6}} and geographer Robert Capot-Rey,JOURNAL, Grove, A.T., Nicole, 1958, 2007, The Ancient Erg of Hausaland, and Similar Formations on the South Side of the Sahara, The Geographical Journal, 124, 4, 528–533, 10.2307/1790942, 1790942, BOOK, Bisson, J., 2003, Mythes et réalités d'un désert convoité: le Sahara, L'Harmattan, fr, the northern limit of the Sahara corresponds to the northern limit of date palm cultivation and the southern limit of the range of esparto, a grass typical of the Mediterranean climate portion of the Maghreb and Iberia. The northern limit also corresponds to the {{convert|100|mm|in|abbr=on}} isohyet of annual precipitation.BOOK, Walton, K., 2007, The Arid Zones, Aldine, B008MR69VM, To the south, the Sahara is bounded by the Sahel, a belt of dry tropical savanna with a summer rainy season that extends across Africa from east to west. The southern limit of the Sahara is indicated botanically by the southern limit of Cornulaca monacantha (a drought-tolerant member of the Chenopodiaceae), or northern limit of Cenchrus biflorus, a grass typical of the Sahel. According to climatic criteria, the southern limit of the Sahara corresponds to the {{convert|150|mm|in|abbr=on}} isohyet of annual precipitation (this is a long-term average, since precipitation varies annually).Important cities located in the Sahara include Nouakchott, the capital of Mauritania; Tamanrasset, Ouargla, Béchar, Hassi Messaoud, Ghardaïa, and El Oued in Algeria; Timbuktu in Mali; Agadez in Niger; Ghat in Libya; and Faya-Largeau in Chad.


The Sahara is the world's largest low-latitude hot desert. It is located in the horse latitudes under the subtropical ridge, a significant belt of semi-permanent subtropical warm-core high pressure where the air from upper levels of the troposphere tends to sink towards the ground. This steady descending airflow causes a warming and a drying effect in the upper troposphere. The sinking air prevents evaporating water from rising, and therefore prevents adiabatic cooling, which makes cloud formation extremely difficult to nearly impossible.WEB, Home – Institute Water for Africa,weblink, The permanent dissolution of clouds allows unhindered light and thermal radiation. The stability of the atmosphere above the desert prevents any convective overturning, thus making rainfall virtually non-existent. As a consequence, the weather tends to be sunny, dry and stable with a minimal chance of rainfall. Subsiding, diverging, dry air masses associated with subtropical high-pressure systems are extremely unfavorable for the development of convectional showers. The subtropical ridge is the predominant factor that explains the hot desert climate (Köppen climate classification BWh) of this vast region. The descending airflow is the strongest and the most effective over the eastern part of the Great Desert, in the Libyan Desert: this is the sunniest, driest and the most nearly "rainless" place on the planet, rivaling the Atacama Desert, lying in Chile and Peru.The rainfall inhibition and the dissipation of cloud cover are most accentuated over the eastern section of the Sahara rather than the western. The prevailing air mass lying above the Sahara is the continental tropical (cT) air mass, which is hot and dry. Hot, dry air masses primarily form over the North-African desert from the heating of the vast continental land area, and it affects the whole desert during most of the year. Because of this extreme heating process, a thermal low is usually noticed near the surface, and is the strongest and the most developed during the summertime. The Sahara High represents the eastern continental extension of the Azores High,{{citation needed|date=August 2016}} centered over the North Atlantic Ocean. The subsidence of the Sahara High nearly reaches the ground during the coolest part of the year, while it is confined to the upper troposphere during the hottest periods.The effects of local surface low pressure are extremely limited because upper-level subsidence still continues to block any form of air ascent. Also, to be protected against rain-bearing weather systems by the atmospheric circulation itself, the desert is made even drier by its geographical configuration and location. Indeed, the extreme aridity of the Sahara is not only explained by the subtropical high pressure: the Atlas Mountains of Algeria, Morocco and Tunisia also help to enhance the aridity of the northern part of the desert. These major mountain ranges act as a barrier, causing a strong rain shadow effect on the leeward side by dropping much of the humidity brought by atmospheric disturbances along the polar front which affects the surrounding Mediterranean climates.The primary source of rain in the Sahara is the Intertropical Convergence Zone, a continuous belt of low-pressure systems near the equator which bring the brief, short and irregular rainy season to the Sahel and southern Sahara. Rainfall in this giant desert has to overcome the physical and atmospheric barriers that normally prevent the production of precipitation. The harsh climate of the Sahara is characterized by: extremely low, unreliable, highly erratic rainfall; extremely high sunshine duration values; high temperatures year-round; negligible rates of relative humidity; a significant diurnal temperature variation; and extremely high levels of potential evaporation which are the highest recorded worldwide.BOOK, Griffiths, Ieuan L. l, The Atlas of African Affairs, Routledge, 978-1-135-85552-9,weblink en, 2013-06-17,


The sky is usually clear above the desert, and the sunshine duration is extremely high everywhere in the Sahara. Most of the desert has more than 3,600 hours of bright sunshine per year (over 82% of daylight hours), and a wide area in the eastern part has over 4,000 hours of bright sunshine per year (over 91% of daylight hours). The highest values are very close to the theoretical maximum value. A value of 4300 hours (98%) of the time would be{{clarify|date=January 2019}} recorded in Upper Egypt (Aswan, Luxor) and in the Nubian Desert (Wadi Halfa).BOOK, Oliver, John E., Encyclopedia of World Climatology, Springer Science & Business Media, 978-1-4020-3264-6,weblink en, 2008-04-23, The annual average direct solar irradiation is around 2,800 kWh/(m2 year) in the Great Desert. The Sahara has a huge potential for solar energy production.File:Algeria Sahara Desert Photo From Drone 5.jpg|thumb|Sand dunesSand dunesThe high position of the Sun, the extremely low relative humidity, and the lack of vegetation and rainfall make the Great Desert the hottest large region in the world, and the hottest place on Earth during summer in some spots. The average high temperature exceeds {{convert|38|to|40|C|F|1|disp=or}} during the hottest month nearly everywhere in the desert except at very high altitudes. The world's highest officially recorded average daily high temperature{{Clarify|reason=Average over what time period?|date=April 2017}} was {{convert|47|C|F|1|disp=or}} in a remote desert town in the Algerian Desert called Bou Bernous, at an elevation of {{convert|378|m|ft}} above sea level, and only Death Valley, California rivals it.BOOK, Griffiths, John F., Driscoll, Dennis M., Survey of Climatology, C.E. Merrill Publishing Company, 978-0-675-09994-3,weblink en, 1982, Other hot spots in Algeria such as Adrar, Timimoun, In Salah, Ouallene, Aoulef, Reggane with an elevation between {{convert|200|and|400|m|ft}} above sea level get slightly lower summer average highs, around {{convert|46|C|F|1|disp=or}} during the hottest months of the year. Salah, well known in Algeria for its extreme heat, has average high temperatures of {{convert|43.8|C|F|1|disp=or}}, {{convert|46.4|C|F|1|disp=or}}, {{convert|45.5|C|F|1|disp=or}} and {{convert|41.9|C|F|1|disp=or}} in June, July, August and September respectively. There are even hotter spots in the Sahara, but they are located in extremely remote areas, especially in the Azalai, lying in northern Mali. The major part of the desert experiences around three to five months when the average high strictly{{clarify|date=January 2019}} exceeds {{convert|40|C|F|disp=or}}; while in the southern central part of the desert, there are up to six or seven months when the average high temperature strictly{{clarify|date=January 2019}} exceeds {{convert|40|C|F|disp=or}}. Some examples of this are Bilma, Niger and Faya-Largeau, Chad. The annual average daily temperature exceeds {{convert|20|C|F|disp=or}} everywhere and can approach {{convert|30|C|F|disp=or}} in the hottest regions year-round. However, most of the desert has a value in excess of {{convert|25|C|F|disp=or}}.(File:Sunset in Sahara.jpg|thumb|Sunset in Sahara)Sand and ground temperatures are even more extreme. During daytime, the sand temperature is extremely high: it can easily reach {{convert|80|C|F|disp=or}} or more.BOOK, Nicholson, Sharon E., Dryland Climatology, Cambridge University Press, 978-1-139-50024-1,weblink en, 2011-10-27, A sand temperature of 83.5 Â°C (182.3 Â°F) has been recorded in Port Sudan. Ground temperatures of {{convert|72|C|F|1|disp=or}} have been recorded in the Adrar of Mauritania and a value of 75 Â°C (167 Â°F) has been measured in Borkou, northern Chad.Due to lack of cloud cover and very low humidity, the desert usually has high diurnal temperature variations between days and nights. However, it is a myth that the nights are cold after extremely hot days in the Sahara. The average diurnal temperature range is typically between {{convert|13|and|20|C-change|F-change|1|disp=or}}. The lowest values are found along the coastal regions due to high humidity and are often even lower than {{convert|10|C-change|F-change|disp=or}}, while the highest values are found in inland desert areas where the humidity is the lowest, mainly in the southern Sahara. Still, it is true that winter nights can be cold as it can drop to the freezing point and even below, especially in high-elevation areas. The frequency of subfreezing winter nights in the Sahara is strongly influenced by the North Atlantic Oscillation (NAO), with warmer winter temperatures during negative NAO events and cooler winters with more frosts when the NAO is positive.See Visbeck, Martin H.; Hurrell, James W.; Polvani, Lorenzo and Cullen, Heidi M.; ‘The North Atlantic Oscillation: Past, Present, and Future’; Proceedings of the National Academy of Sciences of the United States of America, vol. 98, no. 23 (2001); pp. 12876-12877 This is because the weaker clockwise flow around the eastern side of the subtropical anticyclone during negative NAO winters, although too dry to produce more than negligible precipitation, does reduce the flow of dry, cold air from higher latitudes of Eurasia into the Sahara significantly.Hurrell, James W.; Kushnir, Yochanan; Ottersen, Geir and Visbeck, Martin; An Overview of the North Atlantic Oscillation, pp. 17–19. Geophysical Monograph 134; published 2003 by the American Geophysical Union


The average annual rainfall ranges from very low in the northern and southern fringes of the desert to nearly non-existent over the central and the eastern part. The thin northern fringe of the desert receives more winter cloudiness and rainfall due to the arrival of low pressure systems over the Mediterranean Sea along the polar front, although very attenuated by the rain shadow effects of the mountains and the annual average rainfall ranges from {{convert|100|mm|in|0}} to {{convert|250|mm|in|0}}. For example, Biskra, Algeria, and Ouarzazate, Morocco, are found in this zone. The southern fringe of the desert along the border with the Sahel receives summer cloudiness and rainfall due to the arrival of the Intertropical Convergence Zone from the south and the annual average rainfall ranges from {{convert|100|mm|in|0}} to {{convert|250|mm|in|0}}. For example, Timbuktu, Mali and Agadez, Niger are found in this zone. The vast central hyper-arid core of the desert is virtually never affected by northerly or southerly atmospheric disturbances and permanently remains under the influence of the strongest anticyclonic weather regime, and the annual average rainfall can drop to less than {{convert|1|mm|in|2}}. In fact, most of the Sahara receives less than {{convert|20|mm|in|1}}. Of the {{convert|9000000|km2|sqmi}} of desert land in the Sahara, an area of about {{convert|2800000|km2|sqmi}} (about 31% of the total area) receives an annual average rainfall amount of {{convert|10|mm|in|1}} or less, while some {{convert|1500000|km2|sqmi}} (about 17% of the total area) receives an average of {{convert|5|mm|in|sigfig=1}} or less.BOOK, Houérou, Henry N., Bioclimatology and Biogeography of Africa, Springer Science & Business Media, 978-3-540-85192-9,weblink en, 2008-12-10, The annual average rainfall is virtually zero over a wide area of some {{convert|1000000|km2|sqmi}} in the eastern Sahara comprising deserts of: Libya, Egypt and Sudan (Tazirbu, Kufra, Dakhla, Kharga, Farafra, Siwa, Asyut, Sohag, Luxor, Aswan, Abu Simbel, Wadi Halfa) where the long-term mean approximates {{convert|0.5|mm|in|sigfig=1}} per year. Rainfall is very unreliable and erratic in the Sahara as it may vary considerably year by year. In full contrast to the negligible annual rainfall amounts, the annual rates of potential evaporation are extraordinarily high, roughly ranging from {{convert|2500|mm|in|-1}} per year to more than {{convert|6,000|mm|in}} per year in the whole desert.BOOK, Brown, G.W., Desert Biology: Special Topics on the Physical and Biological Aspects of Arid Regions, Elsevier, 978-1-4832-1663-8,weblink en, 2013-09-17, Nowhere else on Earth has air been found as dry and evaporative as in the Sahara region. However, at least two instances of snowfall have been recorded in Sahara, in February 1979 and December 2016, both in the town of Ain Sefra.WEB,weblink Snow falls in Sahara for first time in 37 years, CNN, 21 December 2016, 22 December 2016,

Desertification and prehistoric climate

One theory for the formation of the Sahara is that the monsoon in Northern Africa was weakened because of glaciation during the Quaternary period, starting two or three million years ago. Another theory is that the monsoon was weakened when the ancient Tethys Sea dried up during the Tortonian period around 7 million years.JOURNAL, Yan, Qing, Contoux, Camille, Camille Li, Schuster, Mathieu, Ramstein, Gilles, Zhang, Zhongshi, September 17, 2014, Aridification of the Sahara desert caused by Tethys Sea shrinkage during the Late Miocene, Nature, en, 513, 7518, 401–404, 10.1038/nature13705, 25230661, 1476-4687, 2014Natur.513..401Z, The climate of the Sahara has undergone enormous variations between wet and dry over the last few hundred thousand years,JOURNAL, Ancient Lakes of the Sahara, American Scientist, 94, 2006, 58–65, Kevin White, David J. Mattingly, 1, believed to be caused by long-term changes in the North African climate cycle that alters the path of the North African Monsoon – usually southward. The cycle is caused by a 41000-year cycle in which the tilt of the earth changes between 22° and 24.5°. At present (2000 AD), we are in a dry period, but it is expected that the Sahara will become green again in 15000 years (17000 AD). When the North African monsoon is at its strongest annual precipitation and subsequent vegetation in the Sahara region increase, resulting in conditions commonly referred to as the "green Sahara". For a relatively weak North African monsoon, the opposite is true, with decreased annual precipitation and less vegetation resulting in a phase of the Sahara climate cycle known as the "desert Sahara".JOURNAL, Foley, Jonathan A., Coe, Michael T., Scheffer, Marten, Wang, Guiling, Regime Shifts in the Sahara and Sahel: Interactions between Ecological and Climatic Systems in Northern Africa, Ecosystems, 1 October 2003, 6, 6, 524–539, 10.1007/s10021-002-0227-0,, The idea that changes in insolation (solar heating) caused by long-term changes in the Earth's orbit are a controlling factor for the long-term variations in the strength of monsoon patterns across the globe was first suggested by Rudolf Spitaler in the late nineteenth century,BOOK, Ruddiman, William F., Earth's Climate: Past and Future, 2001, W.H. Freeman and Company, New York, 978-0-7167-3741-4, The hypothesis was later formally proposed and tested by the meteorologist John Kutzbach in 1981.JOURNAL, Kutzbach, J.E., Monsoon Climate of the Early Holocene: Climate Experiment with the Earth's Orbital Parameters for 9000 Years Ago, Science, 2 October 1981, 214, 4516, 59–61, 10.1126/science.214.4516.59, 17802573, 1981Sci...214...59K, Kutzbach's ideas about the impacts of insolation on global monsoonal patterns have become widely accepted today as the underlying driver of long term monsoonal cycles. Kutzbach never formally named his hypothesis and as such it is referred to here as the "Orbital Monsoon Hypothesis" as suggested by Ruddiman in 2001.File:Village Telly in Mali.jpg|thumb|SahelSahelDuring the last glacial period, the Sahara was much larger than it is today, extending south beyond its current boundaries.Christopher Ehret. The Civilizations of Africa. University Press of Virginia, 2002. The end of the glacial period brought more rain to the Sahara, from about 8000 BCE to 6000 BCE, perhaps because of low pressure areas over the collapsing ice sheets to the north.Fezzan Project â€” Palaeoclimate and environment. Retrieved March 15, 2006. {{webarchive |url= |date=June 7, 2009 }} Once the ice sheets were gone, the northern Sahara dried out. In the southern Sahara, the drying trend was initially counteracted by the monsoon, which brought rain further north than it does today. By around 4200 BCE, however, the monsoon retreated south to approximately where it is today,Sahara's Abrupt Desertification Started by Changes in Earth's Orbit, Accelerated by Atmospheric and Vegetation Feedbacks. leading to the gradual desertification of the Sahara.JOURNAL, Kröpelin, Stefan, Stefan Kröpelin, 2008, Climate-Driven Ecosystem Succession in the Sahara: The Past 6000 Years, Science, 320, 5877, 765–768, 10.1126/science.1154913,weblink 18467583, etal, 2008Sci...320..765K, The Sahara is now as dry as it was about 13,000 years ago.The Sahara pump theory describes this cycle. During periods of a wet or "Green Sahara", the Sahara becomes a savanna grassland and various flora and fauna become more common. Following inter-pluvial arid periods, the Sahara area then reverts to desert conditions and the flora and fauna are forced to retreat northwards to the Atlas Mountains, southwards into West Africa, or eastwards into the Nile Valley. This separates populations of some of the species in areas with different climates, forcing them to adapt, possibly giving rise to allopatric speciation.It is also proposed that humans accelerated the drying out period from 6,000–2,500 BCE by pastoralists overgrazing available grassland.NEWS,weblink What Really Turned the Sahara Desert From a Green Oasis Into a Wasteland?, Boissoneault, Lorraine, 2017-03-24, Smithsonian, 2017-08-15, en,

Evidence for cycles

The growth of speleothems (which requires rainwater) was detected in Hol-Zakh, Ashalim, Even-Sid, Ma'ale-ha-Meyshar, Ktora Cracks, Nagev Tzavoa Cave, and elsewhere, and has allowed tracking of prehistoric rainfall. The Red Sea coastal route was extremely arid before 140 and after 115 kya. Slightly wetter conditions appear at 90–87 kya, but it still was just one tenth the rainfall around 125 kya. In the southern Negev Desert speleothems did not grow between 185–140 kya (MIS 6), 110–90 (MIS 5.4–5.2), nor after 85 kya nor during most of the interglacial period (MIS 5.1), the glacial period and Holocene. This suggests that the southern Negev was arid to hyper-arid in these periods.JOURNAL
, 10.1130/G23794A.1
, Desert speleothems reveal climatic window for African exodus of early modern humans
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, 2011-07-21
, During the Last Glacial Maximum (LGM) the Sahara desert was more extensive than it is now with the extent of the tropical forests being greatly reduced,WEB,weblink Africa during the last 150,000 years, Jonathan, Adams, Environmental Sciences Division, ORNL Oak Ridge National Laboratory, dead,weblink" title="">weblink 2006-05-01, and the lower temperatures reduced the strength of the Hadley Cell. This is a climate cell which causes rising tropical air of the Inter-Tropical Convergence Zone (ITCZ) to bring rain to the tropics, while dry descending air, at about 20 degrees north, flows back to the equator and brings desert conditions to this region. It is associated with high rates of wind-blown mineral dust, and these dust levels are found as expected in marine cores from the north tropical Atlantic. But around 12,500 BCE the amount of dust in the cores in the Bølling/Allerød phase suddenly plummets and shows a period of much wetter conditions in the Sahara, indicating a Dansgaard-Oeschger (DO) event (a sudden warming followed by a slower cooling of the climate). The moister Saharan conditions had begun about 12,500 BCE, with the extension of the ITCZ northward in the northern hemisphere summer, bringing moist wet conditions and a savanna climate to the Sahara, which (apart from a short dry spell associated with the Younger Dryas) peaked during the Holocene thermal maximum climatic phase at 4000 BCE when mid-latitude temperatures seem to have been between 2 and 3 degrees warmer than in the recent past. Analysis of Nile River deposited sediments in the delta also shows this period had a higher proportion of sediments coming from the Blue Nile, suggesting higher rainfall also in the Ethiopian Highlands. This was caused principally by a stronger monsoonal circulation throughout the sub-tropical regions, affecting India, Arabia and the Sahara.{{Citation needed|date=August 2009}} Lake Victoria only recently became the source of the White Nile and dried out almost completely around 15 kya.JOURNAL, 10.1007/s10750-007-9158-2, The late Pleistocene desiccation of Lake Victoria and the origin of its endemic biota, 2008, Stager, J.C., Hydrobiologia, 596, 5–16, Johnson, T.C., The sudden subsequent movement of the ITCZ southwards with a Heinrich event (a sudden cooling followed by a slower warming), linked to changes with the El Niño-Southern Oscillation cycle, led to a rapid drying out of the Saharan and Arabian regions, which quickly became desert. This is linked to a marked decline in the scale of the Nile floods between 2700 and 2100 BCE.Burroughs, William J. (2007) "Climate Change in Prehistory: the end of the reign of chaos" (Cambridge University Press)


(File:Saharan topographic elements map.png|thumb|upright=1.75|The major topographic features of the Saharan region)The Sahara comprises several distinct ecoregions. With their variations in temperature, rainfall, elevation, and soil, these regions harbor distinct communities of plants and animals.The Atlantic coastal desert is a narrow strip along the Atlantic coast where fog generated offshore by the cool Canary Current provides sufficient moisture to sustain a variety of lichens, succulents, and shrubs. It covers an area of {{convert|39,900|km2|sqmi|sp=us}} in the south of Morocco and Mauritania.{{WWF ecoregion|id=pa1304|name=Atlantic coastal desert|accessdate=29 December 2007}}The North Saharan steppe and woodlands is along the northern desert, next to the Mediterranean forests, woodlands, and scrub ecoregions of the northern Maghreb and Cyrenaica. Winter rains sustain shrublands and dry woodlands that form a transition between the Mediterranean climate regions to the north and the hyper-arid Sahara proper to the south. It covers {{convert|1,675,300|km2|sqmi|sp=us|sigfig=5}} in Algeria, Egypt, Libya, Mauritania, Morocco, and Tunisia.{{WWF ecoregion|id=pa1321|name=North Saharan steppe and woodlands|accessdate=29 December 2007}}The Sahara Desert ecoregion covers the hyper-arid central portion of the Sahara where rainfall is minimal and sporadic. Vegetation is rare, and this ecoregion consists mostly of sand dunes (erg, chech, raoui), stone plateaus (hamadas), gravel plains (reg), dry valleys (wadis), and salt flats. It covers {{convert|4639900|km2|sqmi}} of: Algeria, Chad, Egypt, Libya, Mali, Mauritania, Niger, and Sudan.The South Saharan steppe and woodlands ecoregion is a narrow band running east and west between the hyper-arid Sahara and the Sahel savannas to the south. Movements of the equatorial Intertropical Convergence Zone (ITCZ) bring summer rains during July and August which average {{convert|100|to|200|mm|abbr=on|sigfig=1|in}} but vary greatly from year to year. These rains sustain summer pastures of grasses and herbs, with dry woodlands and shrublands along seasonal watercourses. This ecoregion covers {{convert|1101700|km2|sqmi}} in Algeria, Chad, Mali, Mauritania, and Sudan.{{WWF ecoregion|id=pa1329|name=South Saharan steppe and woodlands|accessdate=29 December 2007}}In the West Saharan montane xeric woodlands, several volcanic highlands provide a cooler, moister environment that supports Saharo-Mediterranean woodlands and shrublands. The ecoregion covers {{convert|258100|km2|sqmi|sigfig=4}}, mostly in the Tassili n'Ajjer of Algeria, with smaller enclaves in the Aïr of Niger, the Dhar Adrar of Mauritania, and the Adrar des Iforas of Mali and Algeria.{{WWF ecoregion|id=pa1332|name=West Saharan montane xeric woodlands|accessdate=29 December 2007}}The Tibesti-Jebel Uweinat montane xeric woodlands ecoregion consists of the Tibesti and Jebel Uweinat highlands. Higher and more regular rainfall and cooler temperatures support woodlands and shrublands of date palm, acacias, myrtle, oleander, tamarix, and several rare and endemic plants. The ecoregion covers {{convert|82,200|km2|sqmi}} in the Tibesti of Chad and Libya, and Jebel Uweinat on the border of Egypt, Libya, and Sudan.{{WWF ecoregion|id=pa1331|name=Tibesti-Jebel Uweinat montane xeric woodlands|accessdate=29 December 2007}}The Saharan halophytics is an area of seasonally flooded saline depressions which is home to halophytic (salt-adapted) plant communities. The Saharan halophytics cover {{convert|54,000|km2|sqmi}} including: the Qattara and Siwa depressions in northern Egypt, the Tunisian salt lakes of central Tunisia, Chott Melghir in Algeria, and smaller areas of Algeria, Mauritania, and the southern part of Morocco.{{WWF ecoregion|id=pa0905|name=Saharan halophytics|accessdate=29 December 2007}}The Tanezrouft is one of the harshest regions on Earth as well as one of the hottest and driest parts of the Sahara, with no vegetation and very little life. It is along the borders of Algeria, Niger, and Mali, west of the Hoggar mountains.

Flora and fauna

The flora of the Sahara is highly diversified based on the bio-geographical characteristics of this vast desert. Floristically, the Sahara has three zones based on the amount of rainfall received – the Northern (Mediterranean), Central and Southern Zones. There are two transitional zones – the Mediterranean-Sahara transition and the Sahel transition zone.BOOK, Mares, Michael A., Encyclopedia of Deserts,weblink 1999, University of Oklahoma Press, 978-0-8061-3146-7, 490, The Saharan flora comprises around 2800 species of vascular plants. Approximately a quarter of these are endemic. About half of these species are common to the flora of the Arabian deserts.BOOK, Houérou, Henry N., Bioclimatology and Biogeography of Africa,weblink 2008, Springer, 978-3-540-85192-9, 82, File:GueltaCamels.jpg|thumb|Camels in the Guelta d'Archei, in north-eastern ChadChadThe central Sahara is estimated to include five hundred species of plants, which is extremely low considering the huge extent of the area. Plants such as acacia trees, palms, succulents, spiny shrubs, and grasses have adapted to the arid conditions, by growing lower to avoid water loss by strong winds, by storing water in their thick stems to use it in dry periods, by having long roots that travel horizontally to reach the maximum area of water and to find any surface moisture, and by having small thick leaves or needles to prevent water loss by evapotranspiration. Plant leaves may dry out totally and then recover.Several species of fox live in the Sahara including: the fennec fox, pale fox and Rüppell's fox. The addax, a large white antelope, can go nearly a year in the desert without drinking. The dorcas gazelle is a north African gazelle that can also go for a long time without water. Other notable gazelles include the rhim gazelle and dama gazelle.The Saharan cheetah (northwest African cheetah) lives in Algeria, Togo, Niger, Mali, Benin, and Burkina Faso. There remain fewer than 250 mature cheetahs, which are very cautious, fleeing any human presence. The cheetah avoids the sun from April to October, seeking the shelter of shrubs such as balanites and acacias. They are unusually pale.NEWS,weblink Rare cheetah captured on camera, BBC News, 24 February 2009, 12 June 2010, WEB,weblink Acinonyx jubatus ssp. hecki (Northwest African Cheetah, Saharan Cheetah),, 2018-10-23, The other cheetah subspecies (northeast African cheetah) lives in Chad, Sudan and the eastern region of Niger. However, it is currently extinct in the wild in Egypt and Libya. There are approximately 2000 mature individuals left in the wild.File:Libya 5391 Ubari Lakes Luca Galuzzi 2007.jpg|thumb|left|An Idehan Ubari oasis lake, with native grasses and date palms ]]Other animals include the monitor lizards, hyrax, sand vipers, and small populations of African wild dog,{{IUCN2008|assessor=McNutt|assessor-link=Tico McNutt|display-assessors=etal|year=2008|id=12436|title=Lycaon pictus|downloaded=6 May 2008}} in perhaps only 14 countriesMAGAZINE,weblink Endangered in South Africa: Those Doggone Conservationists, Brendan, Borrell, Slate, 19 August 2009, dead,weblink" title="">weblink 30 April 2011, and red-necked ostrich. Other animals exist in the Sahara (birds in particular) such as African silverbill and black-faced firefinch, among others. There are also small desert crocodiles in Mauritania and the Ennedi Plateau of Chad."Desert-Adapted Crocs Found in Africa", National Geographic News, 18 June 2002The deathstalker scorpion can be {{convert|10|cm|in|abbr=on}} long. Its venom contains large amounts of agitoxin and scyllatoxin and is very dangerous; however, a sting from this scorpion rarely kills a healthy adult. The Saharan silver ant is unique in that due to the extreme high temperatures of their habitat, and the threat of predators, the ants are active outside their nest for only about ten minutes per day.JOURNAL, Wehner, R., Marsh, A.C., Wehner, S., 1992, Desert ants on a thermal tightrope, Nature, 357, 6379, 586–87, 10.1038/357586a0, 1992Natur.357..586W, Dromedary camels and goats are the domesticated animals most commonly found in the Sahara. Because of its qualities of endurance and speed, the dromedary is the favourite animal used by nomads.Human activities are more likely to affect the habitat in areas of permanent water (oases) or where water comes close to the surface. Here, the local pressure on natural resources can be intense. The remaining populations of large mammals have been greatly reduced by hunting for food and recreation. In recent years development projects have started in the deserts of Algeria and Tunisia using irrigated water pumped from underground aquifers. These schemes often lead to soil degradation and salinization.Researchers from Hacettepe University (Yücekutlu, N. et al., 2011) have reported that Saharan soil may have bio-available iron and also some essential macro and micro nutrient elements suitable for use as fertilizer for growing wheat.JOURNAL, Yücekutlu, Nihal, Terzioğlu, Serpil, Saydam, Cemal, Bildacı, Işık, Organic Farming By Using Saharan Soil: Could It Be An Alternative To Fertilizers?, Hacettepe Journal of Biology and Chemistry, 2011, 39, 1, 29–38,weblink 23 March 2015, {{dead link|date=January 2018 |bot=InternetArchiveBot |fix-attempted=yes }}


File:Mathendous giraffes.jpg|thumb|Saharan rock art in the FezzanFezzanPeople lived on the edge of the desert thousands of years ago,Discover Magazine, 2006-Oct. since the end of the last glacial period. The Sahara was then a much wetter place than it is today. Over 30,000 petroglyphs of river animals such as crocodilesNational Geographic News, 17 June 2006. survive, with half found in the Tassili n'Ajjer in southeast Algeria. Fossils of dinosaurs,NEWS, Near-perfect fossils of Egyptian dinosaur discovered in the Sahara desert, Nature Middle East, 29 January 2018, 10.1038/nmiddleeast.2018.7, including Afrovenator, Jobaria and Ouranosaurus, have also been found here. The modern Sahara, though, is not lush in vegetation, except in the Nile Valley, at a few oases, and in the northern highlands, where Mediterranean plants such as the olive tree are found to grow. It was long believed that the region had been this way since about 1600 BCE, after shifts in the Earth's axis increased temperatures and decreased precipitation, which led to the abrupt desertification of North Africa about 5,400 years ago.


The Kiffian culture is a prehistoric industry, or domain, that existed between 10,000 and 8,000 years ago in the Sahara, during the Neolithic Subpluvial. Human remains from this culture were found in 2000 at a site known as Gobero, located in Niger in the Ténéré Desert.WEB,weblink Stone Age Graveyard Reveals Lifestyles Of A 'Green Sahara', Science Daily, 2008-08-15, 2008-08-15, The site is known as the largest and earliest grave of Stone Age people in the Sahara desert.NEWS,weblink Graves Found From Sahara's Green Period, John Noble, Wilford, New York Times, 2008-08-14, 2008-08-15, The Kiffians were skilled hunters. Bones of many large savannah animals that were discovered in the same area suggest that they lived on the shores of a lake that was present during the Holocene Wet Phase, a period when the Sahara was verdant and wet. The Kiffian people were tall, standing over six feet in height. Craniometric analysis indicates that this early Holocene population was closely related to the Late Pleistocene Iberomaurusians and early Holocene Capsians of the Maghreb, as well as mid-Holocene Mechta groups.JOURNAL, Sereno PC, ((Garcea EAA)), Jousse H, Stojanowski CM, ((Saliège J-F)), Maga A, Lakeside Cemeteries in the Sahara: 5000 Years of Holocene Population and Environmental Change, PLoS ONE, 2008, 3, 8, 10.1371/journal.pone.0002995, etal, 18701936, 2515196, e2995, 2008PLoSO...3.2995S, Traces of the Kiffian culture do not exist after 8,000 years ago, as the Sahara went through a dry period for the next thousand years.MAGAZINE,weblink Stone Age mass graves reveal green Sahara, Nora, Schultz, New Scientist, 2008-08-14, 2008-08-15, After this time, the Tenerian culture colonized the area.


Gobero was discovered in 2000 during an archaeological expedition led by Paul Sereno, which sought dinosaur remains. Two distinct prehistoric cultures were discovered at the site: the early Holocene Kiffian culture, and the middle Holocene Tenerian culture. The Kiffians were a prehistoric people who preceded the Tenerians and vanished approximately 8000 years ago, when the desert became very dry. The desiccation lasted until around 4600 BCE, when the earliest artefacts associated with the Tenerians have been dated to. Some 200 skeletons have been discovered at Gobero. The Tenerians were considerably shorter in height and less robust than the earlier Kiffians. Craniometric analysis also indicates that they were osteologically distinct. The Kiffian skulls are akin to those of the Late Pleistocene Iberomaurusians, early Holocene Capsians, and mid-Holocene Mechta groups, whereas the Tenerian crania are more like those of Mediterranean groups.JOURNAL, Sereno PC, Garcea EA, Jousse H, Stojanowski CM, Saliège JF, Maga A, Lakeside Cemeteries in the Sahara: 5000 Years of Holocene Population and Environmental Change, PLoS ONE, 2008, 3, 8, 10.1371/journal.pone.0002995, etal, 18701936, 2515196, e2995, 2008PLoSO...3.2995S, NEWS, Wilford, John Noble, In the Sahara, Stone Age graves from greener days,weblink 10 June 2016, New York Times, 14 August 2008, Graves show that the Tenerians observed spiritual traditions, as they were buried with artifacts such as jewelry made of hippo tusks and clay pots. The most interesting find is a triple burial, dated to 5300 years ago, of an adult female and two children, estimated through their teeth as being five and eight years old, hugging each other. Pollen residue indicates they were buried on a bed of flowers. The three are assumed to have died within 24 hours of each other, but as their skeletons hold no apparent trauma (they did not die violently) and they have been buried so elaborately – unlikely if they had died of a plague – the cause of their deaths is a mystery.File:Vue de Taghit.jpg|thumb|Oued Zouzfana and village of TaghitTaghit

Tashwinat Mummy

Uan Muhuggiag appears to have been inhabited from at least the 6th millennium BCE to about 2700 BCE, although not necessarily continuously.BOOK, Mori, F., 1998, The Great Civilisations of the ancient Sahara: Neolithisation and the earliest evidence of anthropomorphic religions, Rome, L'Erma di Bretschneider, 88-7062-971-6, The most noteworthy find at Uan Muhuggiag is the well-preserved mummy of a young boy of approximately {{frac|2|1|2}} years old. The child was in a fetal position, then embalmed, then placed in a sack made of antelope skin, which was insulated by a layer of leaves.AV MEDIA, Hooke, C. (Director), & Mosely, G. (Producer), 2003, Black Mummy of the Green Sahara, Discovery Channel, The boy's organs were removed, as evidenced by incisions in his stomach and thorax, and an organic preservative was inserted to stop his body from decomposing.BOOK, Cockburn, A., 1980, Mummies, Disease and Ancient Cultures, Cambridge, Cambridge University Press, 0-521-23020-9, An ostrich eggshell necklace was also found around his neck. Radiocarbon dating determined the age of the mummy to be approximately 5600 years old, which makes it about 1000 years older than the earliest previously recorded mummy in ancient Egypt.WEB, Wan Muhuggiag, November 16, 2015,weblink In 1958–59, an archaeological expedition led by Antonio Ascenzi conducted anthropological, radiological, histological and chemical analyses on the Uan Muhuggiag mummy. The specimen was determined to be that of a 30-month old child of uncertain sex, who possessed Negroid features. A long incision on the specimen's abdominal wall also indicated that the body had been initially mummified by evisceration and later underwent natural desiccation.JOURNAL, V. Giuffra, etal, Antonio Ascenzi (1915–2000), a Pathologist devoted to Anthropology and Paleopathology, Pathologica, 2010, 102, 1, 1–5,weblink 24 November 2016, 20731247, One other individual, an adult, was found at Uan Muhuggiag, buried in a crouched position. However, the body showed no evidence of evisceration or any other method of preservation. The body was estimated to date from about 7500 BP.BOOK, Soukopova, J., 2012, Round Heads: The Earliest Rock Paintings in the Sahara, Newcastle upon Tyne, Cambridge Scholars Publishing, 978-1-4438-4007-1,


{{further|Sahara pump theory|Neolithic Subpluvial}}File:Beni-Izguen.jpg|thumb|Beni Isguen, a holy city surrounded by thick walls in the Algerian Sahara]]During the Neolithic Era, before the onset of desertification around 9500 BCE, the central Sudan had been a rich environment supporting a large population ranging across what is now barren desert, like the Wadi el-Qa'ab. By the 5th millennium BCE, the people who inhabited what is now called Nubia, were full participants in the "agricultural revolution", living a settled lifestyle with domesticated plants and animals. Saharan rock art of cattle and herdsmen suggests the presence of a cattle cult like those found in Sudan and other pastoral societies in Africa today.WEB,weblink History of Nubia,, 12 June 2010, Megaliths found at Nabta Playa are overt examples of probably the world's first known archaeoastronomy devices, predating Stonehenge by some 2,000 years.weblink" title="">The History of Astronomy. PlanetQuest This complexity, as observed at Nabta Playa, and as expressed by different levels of authority within the society there, likely formed the basis for the structure of both the Neolithic society at Nabta and the Old Kingdom of Egypt.Wendorf, Fred (1998) weblink" title="">Late Neolithic megalithic structures at Nabta Playa.


By 6000 BCE predynastic Egyptians in the southwestern corner of Egypt were herding cattle and constructing large buildings. Subsistence in organized and permanent settlements in predynastic Egypt by the middle of the 6th millennium BCE centered predominantly on cereal and animal agriculture: cattle, goats, pigs and sheep. Metal objects replaced prior ones of stone. Tanning of animal skins, pottery and weaving were commonplace in this era also. There are indications of seasonal or only temporary occupation of the Al Fayyum in the 6th millennium BCE, with food activities centering on fishing, hunting and food-gathering. Stone arrowheads, knives and scrapers from the era are commonly found.Fayum, Qarunian (Fayum B, about 6000–5000 BCE?), Digital Egypt. Burial items included pottery, jewelry, farming and hunting equipment, and assorted foods including dried meat and fruit. Burial in desert environments appears to enhance Egyptian preservation rites, and the dead were buried facing due west.Predynastic (5,500–3,100 BCE), Tour Egypt.By 3400 BCE, the Sahara was as dry as it is today, due to reduced precipitation and higher temperatures resulting from a shift in the Earth's orbit. As a result of this aridification, it became a largely impenetrable barrier to humans, with the remaining settlements mainly being concentrated around the numerous oases that dot the landscape. Little trade or commerce is known to have passed through the interior in subsequent periods, the only major exception being the Nile Valley. The Nile, however, was impassable at several cataracts, making trade and contact by boat difficult.


{{Further|History of Western Sahara}}File:Bilma-Salzkarawane1.jpg|thumb|AzalaiAzalaiThe people of Phoenicia, who flourished from 1200–800 BCE, created a confederation of kingdoms across the entire Sahara to Egypt. They generally settled along the Mediterranean coast, as well as the Sahara, among the people of ancient Libya, who were the ancestors of people who speak Berber languages in North Africa and the Sahara today, including the Tuareg of the central Sahara.The Phoenician alphabet seems to have been adopted by the ancient Libyans of north Africa, and Tifinagh is still used today by Berber-speaking Tuareg camel herders of the central Sahara.Sometime between 633 BCE and 530 BCE, Hanno the Navigator either established or reinforced Phoenician colonies in Western Sahara, but all ancient remains have vanished with virtually no trace.


By 500 BCE, Greeks arrived in the desert. Greek traders spread along the eastern coast of the desert, establishing trading colonies along the Red Sea. The Carthaginians explored the Atlantic coast of the desert, but the turbulence of the waters and the lack of markets caused a lack of presence further south than modern Morocco. Centralized states thus surrounded the desert on the north and east; it remained outside the control of these states. Raids from the nomadic Berber people of the desert were of constant concern to those living on the edge of the desert.

Urban civilization

File:Ghardaia01.jpg|thumb|Market on the main square of GhardaïaGhardaïaAn urban civilization, the Garamantes, arose around 500 BCE in the heart of the Sahara, in a valley that is now called the Wadi al-Ajal in Fezzan, Libya. The Garamantes achieved this development by digging tunnels far into the mountains flanking the valley to tap fossil water and bring it to their fields. The Garamantes grew populous and strong, conquering their neighbors and capturing many slaves (who were put to work extending the tunnels). The ancient Greeks and the Romans knew of the Garamantes and regarded them as uncivilized nomads. However, they traded with them, and a Roman bath has been found in the Garamantes' capital of Garama. Archaeologists have found eight major towns and many other important settlements in the Garamantes' territory. The Garamantes' civilization eventually collapsed after they had depleted available water in the aquifers and could no longer sustain the effort to extend the tunnels further into the mountains.MAGAZINE, Keys, David, 2004, Kingdom of the Sands, Archaeology, 57, 2,weblink


File:Marabutto-Taghirt.JPG|thumb|Zawiya at the entrance of TaghitTaghitFile:Hoggar caravane2.jpg|thumb|upright|The Tuareg once controlled the central Sahara and its trade.]]The Berber people occupied (and still occupy with Arabs) much of the Sahara. The Garamantes Berbers built a prosperous empire in the heart of the desert.Mattingly et al. (2003). Archaeology of Fazzan, Volume 1 The Tuareg nomads continue to inhabit and move across wide Sahara surfaces to the present day.

Islamic and Arabic expansion

The Byzantine Empire ruled the northern shores of the Sahara from the 5th to the 7th centuries. After the Muslim conquest of Arabia, specifically the Arabian peninsula, the Muslim conquest of North Africa began in the mid-7th to early 8th centuries and Islamic influence expanded rapidly on the Sahara. By the end of 641 all of Egypt was in Muslim hands. Trade across the desert intensified, and a significant slave trade crossed the desert. It has been estimated that from the 10th to 19th centuries some 6,000 to 7,000 slaves were transported north each year.Fage, J.D. (2001) A History of Africa. Routledge, 4th ed. {{ISBN|0-415-25248-2}}. p. 256

Ottoman Turkish era

In the 16th century the northern fringe of the Sahara, such as coastal regencies in present-day Algeria and Tunisia, as well as some parts of present-day Libya, together with the semi-autonomous kingdom of Egypt, were occupied by the Ottoman Empire. From 1517 Egypt was a valued part of the Ottoman Empire, ownership of which provided the Ottomans with control over the Nile Valley, the east Mediterranean and North Africa. The benefit of the Ottoman Empire was the freedom of movement for citizens and goods. Traders exploited the Ottoman land routes to handle the spices, gold and silk from the East, manufactured goods from Europe, and the slave and gold traffic from Africa. Arabic continued as the local language and Islamic culture was much reinforced. The Sahel and southern Sahara regions were home to several independent states or to roaming Tuareg clans.

European colonialism

European colonialism in the Sahara began in the 19th century. France conquered the regency of Algiers from the Ottomans in 1830, and French rule spread south from Algeria and eastwards from Senegal into the upper Niger to include present-day Algeria, Chad, Mali then French Sudan including Timbuktu, Mauritania, Morocco (1912), Niger, and Tunisia (1881). By the beginning of the 20th century, the trans-Saharan trade had clearly declined because goods were moved through more modern and efficient means, such as airplanes, rather than across the desert.Trans-Saharan Africa in World History, Ch. 6, Ralph AustinThe French Colonial Empire was the dominant presence in the Sahara. It established regular air links from Toulouse (HQ of famed Aéropostale), to Oran and over the Hoggar to Timbuktu and West to Bamako and Dakar, as well as trans-Sahara bus services run by La Compagnie Transsaharienne (est. 1927).WEB,weblink Wauthier Bréard 1933, 22 February 2013, French, A remarkable film shot by famous aviator Captain René Wauthier documents the first crossing by a large truck convoy from Algiers to Tchad, across the Sahara.WEB, Wauthier, René, Reconnaissance saharienne,weblink French Cinema Archives, 22 February 2013, french, Egypt, under Muhammad Ali and his successors, conquered Nubia in 1820–22, founded Khartoum in 1823, and conquered Darfur in 1874. Egypt, including the Sudan, became a British protectorate in 1882. Egypt and Britain lost control of the Sudan from 1882 to 1898 as a result of the Mahdist War. After its capture by British troops in 1898, the Sudan became an Anglo-Egyptian condominium.Spain captured present-day Western Sahara after 1874, although Rio del Oro remained largely under Sahrawi influence. In 1912, Italy captured parts of what was to be named Libya from the Ottomans. To promote the Roman Catholic religion in the desert, Pope Pius IX appointed a delegate Apostolic of the Sahara and the Sudan in 1868; later in the 19th century his jurisdiction was reorganized into the Vicariate Apostolic of Sahara.

Breakup of the empires and afterwards

(File:Libya 5101 Fozzigiaren Arch Tadrart Acacus Luca Galuzzi 2007.jpg|thumb|A natural rock arch in south western Libya)(File:Hoggar Desert (Algerie).jpg|left|thumb|The Sahara today)Egypt became independent of Britain in 1936, although the Anglo-Egyptian treaty of 1936 allowed Britain to keep troops in Egypt and to maintain the British-Egyptian condominium in the Sudan. British military forces were withdrawn in 1954.Most of the Saharan states achieved independence after World War II: Libya in 1951; Morocco, Sudan, and Tunisia in 1956; Chad, Mali, Mauritania, and Niger in 1960; and Algeria in 1962. Spain withdrew from Western Sahara in 1975, and it was partitioned between Mauritania and Morocco. Mauritania withdrew in 1979; Morocco continues to hold the territory.In the post–World War II era, several mines and communities have developed to utilize the desert's natural resources. These include large deposits of oil and natural gas in Algeria and Libya, and large deposits of phosphates in Morocco and Western Sahara.A number of Trans-African highways have been proposed across the Sahara, including the Cairo–Dakar Highway along the Atlantic coast, the Trans-Sahara Highway from Algiers on the Mediterranean to Kano in Nigeria, the Tripoli – Cape Town Highway from Tripoli in Libya to N'Djamena in Chad, and the Cairo – Cape Town Highway which follows the Nile. Each of these highways is partially complete, with significant gaps and unpaved sections.

People, culture, and languages

{{See|Saharan languages|Saharan rock art|Rock art#Sahara}}File:Arabslavers.jpg|thumb|A 19th-century engraving of an Arab slave-trading caravan transporting black African slaves across the Sahara]]The people of the Sahara are of various origins. Among them the Amazigh including the Tuareg, various Arabized Amaziɣ groups such as the Hassaniya-speaking Sahrawis, whose populations include the Znaga, a tribe whose name is a remnant of the pre-historic Zenaga language. Other major groups of people include the: Toubou, Nubians, Zaghawa, Kanuri, Hausa, Songhai, Beja, and Fula/Fulani (; ).Arabic dialects are the most widely spoken languages in the Sahara. Arabic, Berber and its variants now regrouped under the term Amazigh (which includes the Guanche language spoken by the original Berber inhabitants of the Canary Islands) and Beja languages are part of the Afro-Asiatic or Hamito-Semitic family.{{citation needed|date=February 2013}} Unlike neighboring West Africa and the central governments of the states that comprise the Sahara, the French language bears little relevance to inter-personal discourse and commerce within the region, its people retaining staunch ethnic and political affiliations with Tuareg and Berber leaders and culture.Jane E. Goodman (2010) [2005]). Berber Culture on the World Stage: From Village to Video. Indiana University Press, {{ISBN|978-0-253-21784-4}} pp. 49–68 The legacy of the French colonial era administration is primarily manifested in the territorial reorganization enacted by the Third and Fourth republics, which engendered artificial political divisions within a hitherto isolated and porous region.Ralph A. Austen. Trans-Saharan Africa in World History. Oxford University Press, 2010. {{ISBN|0-19-979883-4}} Diplomacy with local clients was conducted primarily in Arabic, which was the traditional language of bureaucratic affairs. Mediation of disputes and inter-agency communication was served by interpreters contracted by the French government, who, according to Keenan, "documented a space of intercultural mediation," contributing much to preserving the indigenous cultural identities in the region.Jeremy Keenan, ed. (2013). The Sahara: Past, Present and Future. Routledge, {{ISBN|1-317-97001-2}}

See also




  • BOOK, Brett, Michael, Prentess, Elizabeth, The Berbers, Blackwell Publishers, 1996,
  • BOOK, Bulliet, Richard W., The Camel and the Wheel, Harvard University Press, 1975, Republished with a new preface Columbia University Press, 1990.
  • BOOK, Gearon, Eamonn, Eamonn Gearon, The Sahara: A Cultural History, Signal Books (UK), Oxford University Press (US), 2011,
  • BOOK, Julien, Charles-Andre, History of North Africa: From the Arab Conquest to 1830, Praeger, 1970,
  • BOOK, Kennedy, Hugh, Hugh N. Kennedy, Muslim Spain and Portugal: A Political History of al-Andalus, Longman, 1996,
  • BOOK, Laroui, Abdallah Laroui, The History of the Maghrib: An Interpretive Essay, Princeton, 1977,
  • BOOK, Scott, Chris, Sahara Overland, Trailblazer Guides, 2005,
  • JOURNAL, Wade, Lizzie,weblink Drones and Satellites Spot Lost Civilizations in Unlikely Places, Science, 2015, 10.1126/science.aaa7864,

External links

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Eastern Philosophy
History of Philosophy
M.R.M. Parrott