Houn Jau De!
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Houn Jau De!
Hun or Houn () () is an oasis town in the northern Fezzan region of southwest Libya. The town is the capital of the Jufra District. The "International Autumn Tourism Festival" is an annual festival usually held at the end of September. History During the colonial Italian Libya period, Hun was the administrative capital of the Italian Fezzan region, called '' Territorio del Sahara Libico''. Hun was the Italian military center of southern Italian Libya, and was not part of the national Fourth Shore territory of the Kingdom of Italy as Italian Tripolitania and Italian Cyrenaica. In the 1939 census Italians were 3% of the total population of 35,316 in the city. They disappeared from Hun after Italy's loss of Libya in World War II. An important Libyan Italian born in Hun was the internationally renowned painter Mario Schifano (1934–1998). In the 1930s the Italian government made some important improvements to the small town, including a connection to the coast via the new Fezzan Ro ...
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Fezzan
Fezzan ( , ; ; ; ) is the southwestern region of modern Libya. It is largely desert, but broken by mountains, uplands, and dry river valleys (wadis) in the north, where oases enable ancient towns and villages to survive deep in the otherwise inhospitable Sahara Desert. The term originally applied to the land beyond the coastal strip of Africa proconsularis, including the Nafusa and extending west of modern Libya over Ouargla Province, Ouargla and Illizi Province, Illizi. As these Berber people, Berber areas came to be associated with the regions of Tripoli, Libya, Tripoli, Cirta or Algiers, the name was increasingly applied to the arid areas south of Tripolitania. After the 1934 formation of Libya, the Fezzan province was designated as one of the three primary Provinces of Libya, provinces of the country, alongside Tripolitania (region), Tripolitania province to the north and Cyrenaica province to the northeast. Etymology In Berber languages, ''Fezzan'' (or ''ifezzan'') means " ...
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Fezzan Road
Fezzan Road is an asphalt road in central Libya, running from Abu Qurayn near the coast to Sabha in the Sahara Desert. It is long. History Fezzan Road was constructed in the early 1960s. It was the largest road project in Libya since the Italian colonial Libyan Coastal Highway. It was probably the most important transportation project in Libya prior to the petroleum era. The importance of Fezzan Road was reduced after paving the Mizda–Brak Road in the 1980s. It reduced the full Tripoli-Sabha route length from to . References *Abdel Aziz Tarih Sharaf, "Jughrafia Libia", Munsha'at al Ma'arif, Alexandria, 2nd ed., 1971. *Mustapha Ben Halim, "Libia: Inbe'ath Omma.. wa Soqout Dawla", Manshurat al Jamal, Cologne, Germany Germany, officially the Federal Republic of Germany, is a country in Central Europe. It lies between the Baltic Sea and the North Sea to the north and the Alps to the south. Its sixteen States of Germany, constituent states have a total popu ..., 2003. ...
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Spring (hydrosphere)
A spring is a natural exit point at which groundwater emerges from an aquifer and flows across the ground surface as surface water. It is a component of the hydrosphere, as well as a part of the water cycle. Springs have long been important for humans as a source of fresh water, especially in arid regions which have relatively little annual rainfall. Springs are driven out onto the surface by various natural forces, such as gravity and Hydrostatics#Hydrostatic pressure, hydrostatic pressure. A spring produced by the emergence of Geothermal activity, geothermally heated groundwater is known as a hot spring. The yield (hydrology), yield of spring water varies widely from a volumetric flow rate of nearly zero to more than for the biggest springs. Formation Springs are formed when groundwater flows onto the surface. This typically happens when the water table reaches above the surface level, or if the terrain depression (geology), depresses sharply. Springs may also be formed ...
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Mosque
A mosque ( ), also called a masjid ( ), is a place of worship for Muslims. The term usually refers to a covered building, but can be any place where Salah, Islamic prayers are performed; such as an outdoor courtyard. Originally, mosques were simple places of prayer for the early Muslims, and may have been open spaces rather than elaborate buildings. In the first stage of Islamic architecture (650–750 CE), early mosques comprised open and closed covered spaces enclosed by walls, often with minarets, from which the Adhan, Islamic call to prayer was issued on a daily basis. It is typical of mosque buildings to have a special ornamental niche (a ''mihrab'') set into the wall in the direction of the city of Mecca (the ''qibla''), which Muslims must face during prayer, as well as a facility for ritual cleansing (''wudu''). The pulpit (''minbar''), from which public sermons (''khutbah'') are delivered on the event of Friday prayer, was, in earlier times, characteristic of the central ...
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Ksar
Ksar or qṣar (), in plural ksour or qsour (), is a type of fortified village in North Africa, usually found in the regions predominantly or traditionally inhabited by Berbers (Amazigh). The equivalent Berber languages, Berber term used is ' (singular) or (plural). Etymology The Arabic ''qaṣr'' () was probably borrowed from the Latin word . Architecture Ksour in the Maghreb typically consist of attached houses, often having a Fortified Granaries of Aures, fortified communal granary like those in Algeria, or the ghorfa and agadir (granary), agadir types known in Tunisia and Morocco respectively, beside other structures like a mosque, hammam, oven, and shops. Ksur or igherman are widespread among the oasis populations of North Africa. Ksars are sometimes situated in mountain locations to make defense easier; they often are entirely within a single, continuous wall. The building material of the entire structure usually is adobe, or cut stone and adobe. The idea of the ks ...
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Sokna, Libya
Sokna (, IPA ['so:kna], also transliterated as Socna or Sawknah, Tamazight: IsuknenAghali Zakara, M., Allati, A., Amaoui, M., Baldi, S., Boukerrouf, R., Bouzakhar, M., ... & Fedikhi, R. (2015). La lingua nella vita e la vita della lingua. Itinerari e percorsi degli studi berberi. Miscellanea per il Centenario di studi berberi a «L’Orientale» di Napoli. Scritti in onore di Francesco Beguinot. URL :https://unora.unior.it/retrieve/handle/11574/164317/34753/SB4.pdf) is a Saharan desert oasis town in the Fezzan region of southwest Libya. The Eastern Berber language Sokna language, Sokna is native to the town. This local pre-arabized dialect, which fell out of use by the end of the 20th century, is retained in place names. Presently, the population speaks Arabic. Geography Sokna is located southwest of the district capital Hun, Libya, Hun, in the Jufra District. The Spring (hydrosphere), natural springs support native date palm (''Phoenix dactylifera'') groves. Due to its reliable ...
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Waddan, Libya
Waddan (, ) is an oasis town of the Sahara Desert in the northeast Fezzan region of southwest Libya, in the Jufra District. It was an important town on the ancient trade routes across the Sahara. Geography Waddan is the oldest city in Jufra District located south of Sirte, and northeast of Hun. The town is at the crossroads of the Sirte-Waddan Road and the Fezzan Road. The natural springs support native date palm (''Phoenix dactylifera'') groves. History In the Seventh Century C.E., Waddan was the primary town among the oasis settlements in the al-Jufra area. It was captured for Islam during the southern excursion of Amr ibn al-As in 642 C.E. by commander Busr ibn Artat, although he only extracted tribute and didn't garrison the town. However, the nephew of Amr ibn al-As, Uqba ibn Nafi, reconquered Waddan in 666-667, and established a military post there. During the Libyan Civil War, NATO forces bombed an ammunition store in the town. On 8 September 2011, the tow ...
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Oases
In ecology, an oasis (; : oases ) is a fertile area of a desert or semi-desert environmentBattesti, Vincent (2005) Jardins au désert: Évolution des pratiques et savoirs oasiens: Jérid tunisien. Paris: IRD éditions.
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that sustains plant life and provides habitat for animals. Surface water may be present, or water may only be accessible from wells or underground channels created by humans. In geography, an oasis may be a current or past rest stop on a transportation route, or less-than-verdant location that nonetheless provides access to underground water through deep wells created and maintained by humans. Although they depend on a natural condition, such as the presence of water that may be stored in reservoirs and us ...
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Phoenix Dactylifera
''Phoenix dactylifera'', commonly known as the date palm, is a flowering-plant species in the palm family Arecaceae, cultivated for its edible sweet #Fruits, fruit called dates. The species is widely cultivated across North Africa, northern Africa, the Middle East, the Horn of Africa, Australia, South Asia, and the desert regions of Southern California in the United States. It is Naturalisation (biology), naturalized in many Tropics, tropical and Subtropics, subtropical regions worldwide. ''P. dactylifera'' is the type species of genus ''Phoenix (plant), Phoenix'', which contains 12–19 species of wild date palms. Date palms reach up to 60–110 feet in height, growing singly or forming a Clumping (biology), clump with several stems from a single root system. Slow-growing, they can reach over 100years of age when maintained properly. Date fruits (dates) are oval-cylindrical, long, and about in diameter, with colour ranging from dark brown to bright red or yellow, depen ...
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Basalt
Basalt (; ) is an aphanite, aphanitic (fine-grained) extrusive igneous rock formed from the rapid cooling of low-viscosity lava rich in magnesium and iron (mafic lava) exposed at or very near the planetary surface, surface of a terrestrial planet, rocky planet or natural satellite, moon. More than 90% of all volcanic rock on Earth is basalt. Rapid-cooling, fine-grained basalt is chemically equivalent to slow-cooling, coarse-grained gabbro. The eruption of basalt lava is observed by geologists at about 20 volcanoes per year. Basalt is also an important rock type on other planetary bodies in the Solar System. For example, the bulk of the plains of volcanism on Venus, Venus, which cover ~80% of the surface, are basaltic; the lunar mare, lunar maria are plains of flood-basaltic lava flows; and basalt is a common rock on the surface of Mars. Molten basalt lava has a low viscosity due to its relatively low silica content (between 45% and 52%), resulting in rapidly moving lava flo ...
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Sahara Desert
The Sahara (, ) is a desert spanning across North Africa. With an area of , it is the largest hot desert in the world and the list of deserts by area, third-largest desert overall, smaller only than the deserts of Antarctica and the northern Arctic. The name "Sahara" is derived from , a broken plural form of ( ), meaning "desert". The desert covers much of North Africa, excluding the fertile region on the Mediterranean Sea coast, the Atlas Mountains of the Maghreb, and the Nile, Nile Valley in Egypt and the 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 Tropical and subtropical grasslands, savannas, and shrublands, semi-arid tropical savanna around the Niger River valley and the Sudan (region), Sudan region of sub-Saharan Africa. The Sahara can be divided into several regions, including ...
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Mediterranean
The Mediterranean Sea ( ) is a sea connected to the Atlantic Ocean, surrounded by the Mediterranean basin and almost completely enclosed by land: on the east by the Levant in West Asia, on the north by Anatolia in West Asia and Southern Europe, on the south by North Africa, and on the west almost by the Morocco–Spain border. The Mediterranean Sea covers an area of about , representing 0.7% of the global ocean surface, but its connection to the Atlantic via the Strait of Gibraltar—the narrow strait that connects the Atlantic Ocean to the Mediterranean Sea and separates the Iberian Peninsula in Europe from Morocco in Africa—is only wide. Geological evidence indicates that around 5.9 million years ago, the Mediterranean was cut off from the Atlantic and was partly or completely desiccated over a period of some 600,000 years during the Messinian salinity crisis before being refilled by the Zanclean flood about 5.3 million years ago. The sea was an important rout ...
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