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29-632: El Oued Province lies in the Sahara desert in northeast Algeria. The mostly uninhabited southern half of the province is covered by the Grand Erg Oriental , a vast region of uninterrupted sand dunes . The northern half of the province is a mixture of sandy desert with scarce vegetation, scattered oases , and salt lakes . The most notable oases are the Oued Souf region, upon which the capital El Oued and neighbouring towns are built, as well as oases located near

58-464: A hot desert climate . Winters are mild, with average temperatures around 11 °C (52 °F) in January, but summers are hot with average temperatures around 32 °C (90 °F), average maxima around 40 °C (104 °F) and the hottest days approaching 50 °C (122 °F). Precipitation is very low throughout the province, but somewhat more rain does fall in the north, particularly during

87-533: Is a desert, a natural region receiving very little rainfall. It is the largest Erg in Algeria, the next in size being the much smaller Grand Erg Occidental ('Western Sand Sea'). The largest erg of the Sahara is probably As-Sahra al-Libiyah , which straddles the inland border of Libya and Egypt. Erg is a Tamachek Berber word, and also a geographic term of art . The Grand Erg Oriental used to be associated with

116-523: Is also sometimes called alluvial deposit . Alluvium is typically geologically young and is not consolidated into solid rock. Sediments deposited underwater, in seas, estuaries , lakes, or ponds, are not described as alluvium. Floodplain alluvium can be highly fertile, and supported some of the earliest human civilizations. The present consensus is that "alluvium" refers to loose sediments of all types deposited by running water in floodplains or in alluvial fans or related landforms . However,

145-539: Is now served by an international airport. A desert road going east from Hassi Messaoud continues through the Grand Erg , passing by a well named Bordj Sif Fatima ["Fatima's River Tower" perhaps], on its way to the small but ancient settlement of Ghadames at the Libyan frontier. Another and better road from Hassi Messaoud goes south, also crossing the grand erg where it passes a well called Hassi Tartrat , before reaching

174-619: Is situated directly adjacent to the Grand Erg's southeast edge. Tuareg Berbers (a people sourced in the central Sahara) compose the majority in Ghadames. This oasis was known by ancient Egypt , and later by Carthage and by Rome , as Cydamus. A Libyan road from Tarabulus on the Mediterranean coast now leads to present-day Ghadames. The historic Saharan architecture found in its Old Town has received international recognition . In Algeria Oued Irara Airport at Hassi Messaoud (located in

203-565: The Aurès mountains, then salt lakes by the city of Biskra . Next the road skirts the western edge of the erg. After about 500 km. in all, it reaches the ancient oasis of Ouargla [Wargla]. Since late antiquity Wargla was a stop for the Saharan trade , being situated along a caravan route of several thousand kilometers, stretching from the Mediterranean to the Sahel . In the process such caravans crossed

232-492: The Grand Erg Oriental . In addition to oil in Wargla and Hassi Messaoud (see above), other Algerian hydrocarbon sites include In Salah , a city (pop: 44,000) to the erg's southwest, yielding natural gas , and also El Adeb Larache, Edjelé, Tingentourine, and Zarzaïtine (south of the erg, close to Libya). One of Algeria's largest field of natural gas is near Ghardaïa , west of Touggourt. Gas pipelines have been constructed north to

261-500: The great desert ( Ar : aṣ-ṣaḥrā´ al-kubra). Wargla was the capital of late medieval M'zab , an Ibadi political entity descended from the earlier Rustamid polity. Wargla is today a mid-sized modern city ( pop : 129,000) and provincial capital, with a focus on the oil industry. The above north-south Algerian road from Constantine passes through other oases . North of Wargla [Ouargla] lies Touggourt [Tuggurt, Taghit] (pop: 153,000), where date palms are grown commercially. Touggourt

290-579: The Mediterranean port of Bourgie, and later northeast through Tunisia. Along the north rim of the Grand Erg Oriental , both the physical ecology and the human culture surviving there since ancient times are said to form a continuum. From Biskra (pop: 200,000) in Algeria by the Aurès mountains, this region extends east to the Djerid of Tunisia. It is a low-lying area of chotts (salt pans), and occasional oases, where exists intensive cultivation of date palms in

319-640: The Wadi Igharghar, a mostly dry and buried river with a sizable network of tributaries which, should it possess any water, would flow north into the erg from the Ahaggar mountains of the central Sahara . Yet such dry, anciently-made river beds, lying seemingly useless beneath the desert sands, can preserve the infrequent rain water, by carrying it off underground and so rescue the moisture from an otherwise "intense and almost instantaneous" evaporation. A buried river bed "not only serves in certain cases to carry into

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348-406: The east and southeast slopes" toward Ghadames at the Libyan border. Winds over time will sweep desert sand into heaps which, given enough sand, form into a series of hills. In some types of dunes the slope on the windward side is gradual, on the leeward steep, and such dunes may "roll" forward being blown in the direction of the wind is taking. These dunes tend to be perpendicular to

377-446: The edge of the Grand Erg Oriental . 30°00′N 6°00′E  /  30.000°N 6.000°E  / 30.000; 6.000 Alluvial Alluvium (from Latin alluvius , from alluere  'to wash against') is loose clay , silt , sand , or gravel that has been deposited by running water in a stream bed, on a floodplain , in an alluvial fan or beach , or in similar settings. Alluvium

406-432: The erg's far side. Further south lies the Ahaggar mountains. The cities of Wargla and Touggourt lie outside the western limits of the erg. Nearby, within the accepted boundaries of the Grand Erg Oriental , the landscape is described as being "practically free from [sand] dunes" evidently due to strong, persistent winds. Petroleum and other hydrocarbons have been extracted in Algeria , from areas in and surrounding

435-426: The erg) serves a few international flights and also national flights. Ouargla Airport (OGX) has limited international and national flights. North of the erg Guemar Airport , 20 km. from El Oued , has only national flights. In Libya Ghadames Airport schedules only national flights. In Tunisia Djerba – Zarzis Airport (DJE/DTTJ) serves international and national flights, it being over 100 km. north of

464-609: The fruits of "some buried wadi". To the north of the erg, the Aurès mountains provide abundant runoff. These waters feed the artesian aquifer of the Jerid , despite its surface covering of salt lakes . These geographic conditions lie adjacent to the Grand Erg Oriental. Here grow "the finest dates of all the Maghrib ". In winter, winds blow from the northwest and the north. The Grand Erg Oriental "appears to have been pushed forward on

493-449: The heart of the desert the waters of distant rains which have fallen outside the desert domain, but in it the waters of the local storms are concentrated and carried swiftly to the alluvial basins where they are imbibed by the lighter earth and form lasting reserves within its depths. The result is that what vegetation survives is localized along the wadi beds or in their basins; in fact the words wadi and pasturage are interchangeable in

522-471: The language of the nomads , who habitually reside in such places." For these and similar reasons concerning the desert ecology of water, the geographer and historian of the Sahara E.-F. Gautier once wrote referring to the Grand Erg Oriental as "the great Igharghar Erg". Accordingly, surface moisture, seasonal pastures, and wells may reflect unseen conditions beneath the sands. What appears as an entirely inhospitable erg can elsewhere, in stark contrast, offer

551-408: The late 19th century. "Colluvium" is now generally understood as sediments produced by gravity-driven transport on steep slopes. At the same time, the definition of "alluvium" has switched back to an emphasis on sediments deposited by river action. There continues to be disagreement over what other sediment deposits should be included under the term "alluvium". Most alluvium is Quaternary in age and

580-498: The meaning of the term has varied considerably since it was first defined in the French dictionary of Antoine Furetière , posthumously published in 1690. Drawing upon concepts from Roman law , Furetière defined alluvion (the French term for alluvium) as new land formed by deposition of sediments along rivers and seas. By the 19th century, the term had come to mean recent sediments deposited by rivers on top of older diluvium , which

609-431: The slope being steep on both sides. Seif dunes generally form long rows whose parallel ridge lines follow the wind's direction. There are other types of dunes , as well as "complex" dunes. Saharan winds are also known to clear an area of sand altogether, leaving bare rock ( hamada ) or gravel (reg). The Grand Erg Oriental is accessible overland by an Algerian road, which goes south from Constantine . It passes through

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638-512: The tens of thousands. Between Biskra and the Djerid, but a little to the south, lies El Oued , a mid-sized Algerian city (pop: 139,000), graced with domes and arches of Saharan architecture. Also an oasis, it's located about 100 km. east of Touggourt and by the northern frontier of the erg. The thirst of El Oued is quenched by a subterranean river . South of the Tunisian sea port of Gabès , in

667-509: The towns of El M'Ghair and Djamaa , both of which support extensive palm plantations. Chott Melrhir , a large endorheic salt lake, lies in the north-central part of the province, while Chott Felrhir is a smaller salt lake to its southwest, near El M'Ghair. These salt lakes, and the surrounding areas, lie as much as 30 metres (98 ft) below sea level; nearby towns and villages including Hamraia , Méguibra , Dendouga and Aïn Cheikh are also below sea level. El Oued Province experiences

696-535: The vicinity of the Grand Erg's northeast edge, there are a number of Berber villages, among them Tataouine . From here a bleak Tunisian paved road leads south along the Libyan border, by sand dunes of the Grand Erg's eastern limits, terminating at Borj El Khadra, an oasis, near Ghadames. The ancient oasis town of Ghadames (pop: 7,000) in Libya is located by where the frontiers of Algeria, Tunisia, and Libya meet. The city

725-404: The wind's direction. Vegetation does not survive in such spreads of hot dry sand. Only in rare areas where moisture can endure is there life. Common in the Sahara desert are seif dunes : here the air currents form sand dunes parallel to the prevailing direction of the wind. These dunes have long, sharp ridge lines. Cross-winds, however, may alter the height or width of such lengthy dunes, with

754-405: The winter and adjacent months. El Oued Province is bordered to the northeast by Tébessa Province , to the north by Khenchela Province , to the northwest by Biskra Province , to the west by El M'Ghair Province to the south and southwest by Ouargla Province , to the southeast by Tunisia 's Tataouine Governorate , and to the east by Tunisia 's Tozeur and Kebili Governorates . The province

783-619: Was created from Biskra Province in 1984. The province is made up of 10 districts , which are divided into 22 communes or municipalities. Grand Erg Oriental The Grand Erg Oriental (English: 'Great Eastern Sand Sea') is a large erg or "field of sand dunes" in the Sahara Desert . Situated for the most part in Saharan lowlands of northeast Algeria , the Grand Erg Oriental covers an area some 600 km wide by 200 km north to south. The erg's northeastern edge spills over into neighbouring Tunisia . The Grand Erg Oriental

812-434: Was formerly a medieval Sultanate and a northern oasis on a Trans-Saharan trade route. South of Wargla on this road, lies Hassi Messaoud ["blessed well"], which is located within the Grand Erg . Until recently Hassi Messaoud was a small Saharan village, but has grown substantially on account of the local discovery of oil in 1956. An oil refinery has since been built, and the city (current population estimated at 60,000)

841-528: Was similar in character but interpreted as sediments deposited by Noah's flood . With the rejection by geologists of the concept of a primordial universal flood, the term "diluvium" fell into disfavor and was replaced with "older alluvium". At the same time, the term "alluvium" came to mean all sediment deposits due to running water on plains. The definition gradually expanded to include deposits in estuaries, coasts, and young rock of marine and fluvial origin. Alluvium and diluvium were grouped as colluvium in

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