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Hassi Messaoud
Hassi Messaoud ( ar, حاسي مسعود) is a town in Ouargla Province, eastern Algeria, located southeast of Ouargla. As of 2008 it had a population of 45,147 people, up from 40,360 in 1998, and an annual population growth rate of 1.1%, the lowest in the province. Oil was discovered there in 1956 and the town's prominence has grown rapidly since then; it is considered as the First Energy town in Algeria where all the big oil and gas companies have offices and bases. It is an oil refinery town named after the first oil well. A water well, dug in 1917, can be found on the airport side of town. Today there are over 800 wells within a radius of the town. History The Name Hassi Messaoud means "the well of Messaoud" in Arabic, named after Messaoud Rouabeh, a well-digger in the region. Before the discovery of oil in the region, Hassi Messaoud was not very populated. After discovering oil in the region in the 1950s the French built two petroleum bases. After the nationalization of oi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Communes Of Algeria ...
The municipalities of Algeria (Arabic: بلدية (singular)) form the third level of administrative subdivisions of Algeria. As of 2002, there were 1,541 municipalities in the country. List This list is a copy from the Statoids page named Municipalities of Algeria'. The population data is from June 25, 1998. References See also * List of cities in Algeria * Cities of present-day nations and states {{DEFAULTSORT:Communes Of Algeria Subdivisions of Algeria Algeria 3 Communes, Algeria Communes An intentional community is a voluntary residential community which is designed to have a high degree of social cohesion and teamwork from the start. The members of an intentional community typically hold a common social, political, relig ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Köppen Climate Classification
The Köppen climate classification is one of the most widely used climate classification systems. It was first published by German-Russian climatologist Wladimir Köppen (1846–1940) in 1884, with several later modifications by Köppen, notably in 1918 and 1936. Later, the climatologist Rudolf Geiger (1894–1981) introduced some changes to the classification system, which is thus sometimes called the Köppen–Geiger climate classification system. The Köppen climate classification divides climates into five main climate groups, with each group being divided based on seasonal precipitation and temperature patterns. The five main groups are ''A'' (tropical), ''B'' (arid), ''C'' (temperate), ''D'' (continental), and ''E'' (polar). Each group and subgroup is represented by a letter. All climates are assigned a main group (the first letter). All climates except for those in the ''E'' group are assigned a seasonal precipitation subgroup (the second letter). For example, ''Af'' indi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Structural Basin
A structural basin is a large-scale structural formation of rock strata formed by tectonic warping of previously flat-lying strata. They are geological depressions, the inverse of domes. Elongated structural basins are also known as synclines. Some are sedimentary basins, aggregations of sediment that filled up a depression or accumulated in an area. Others were formed by tectonic events long after the sedimentary layers were deposited. Basins may appear on a geologic map as roughly circular or elliptical, with concentric layers. Because the strata dip toward the center, the exposed strata in a basin are progressively younger from the outside in, with the youngest rocks in the center. Basins are often large in areal extent, often hundreds of kilometers across. Structural basins are often important sources of coal, petroleum, and groundwater. Examples Europe * Hampshire Basin, United Kingdom * London Basin, United Kingdom * Paris Basin, France * Permian Basin, Poland, northern ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Dome
A dome () is an architectural element similar to the hollow upper half of a sphere. There is significant overlap with the term cupola, which may also refer to a dome or a structure on top of a dome. The precise definition of a dome has been a matter of controversy and there are a wide variety of forms and specialized terms to describe them. A dome can rest directly upon a Rotunda (architecture), rotunda wall, a Tholobate, drum, or a system of squinches or pendentives used to accommodate the transition in shape from a rectangular or square space to the round or polygonal base of the dome. The dome's apex may be closed or may be open in the form of an Oculus (architecture), oculus, which may itself be covered with a roof lantern and cupola. Domes have a long architectural lineage that extends back into prehistory. Domes were built in ancient Mesopotamia, and they have been found in Persian architecture, Persian, Ancient Greek architecture, Hellenistic, Ancient Roman architecture, ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sandstone
Sandstone is a clastic sedimentary rock composed mainly of sand-sized (0.0625 to 2 mm) silicate grains. Sandstones comprise about 20–25% of all sedimentary rocks. Most sandstone is composed of quartz or feldspar (both silicates) because they are the most resistant minerals to weathering processes at the Earth's surface. Like uncemented sand, sandstone may be any color due to impurities within the minerals, but the most common colors are tan, brown, yellow, red, grey, pink, white, and black. Since sandstone beds often form highly visible cliffs and other topographic features, certain colors of sandstone have been strongly identified with certain regions. Rock formations that are primarily composed of sandstone usually allow the percolation of water and other fluids and are porous enough to store large quantities, making them valuable aquifers and petroleum reservoirs. Quartz-bearing sandstone can be changed into quartzite through metamorphism, usually related to ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cambrian
The Cambrian Period ( ; sometimes symbolized C with bar, Ꞓ) was the first geological period of the Paleozoic Era, and of the Phanerozoic Eon. The Cambrian lasted 53.4 million years from the end of the preceding Ediacaran Period 538.8 million years ago (mya) to the beginning of the Ordovician Period mya. Its subdivisions, and its base, are somewhat in flux. The period was established as "Cambrian series" by Adam Sedgwick, who named it after Cambria, the Latin name for 'Cymru' (Wales), where Britain's Cambrian rocks are best exposed. Sedgwick identified the layer as part of his task, along with Roderick Murchison, to subdivide the large "Transition Series", although the two geologists disagreed for a while on the appropriate categorization. The Cambrian is unique in its unusually high proportion of sedimentary deposits, sites of exceptional preservation where "soft" parts of organisms are preserved as well as their more resistant shells. As a result, our understanding of the Ca ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Nezla
Nezla ( ar, ﻧﺰﻟﺔ) is a town and commune in Touggourt District, Touggourt Province, Algeria. According to the 2008 census it has a population of 51,674, up from 40,524 in 1998, and an annual population growth rate of 2.5%. Nezla is part of the urban area of Touggourt, and forms much of the southern area of that city. Agriculture is the main industry of the region, along with some tourism. The Sidi Madhi Airport is found in Nezla commune, and serves Touggourt and the surrounding areas. Localities The commune is composed of five localities: *Nezla *Boumerdès *Sidi Boudjenane *Aïn Sahra *Sidi Madhi See also * Bandar-e Anzali Bandar-e Anzali ( fa, بندرانزلی, also Romanized as Bandar-e Anzalī; renamed as Bandar-e Pahlavi during the Pahlavi dynasty) is a city of Gilan Province, Iran. At the 2011 census, its population was 144,664. Anzali is one of the mos ... References Neighbouring towns and cities Communes of Ouargla Province {{Ouargla-ge ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Gassi Touil
Gassi Touil is a large natural gas field in the Sahara Desert region of Grand Erg Oriental of Algeria, within the commune of Hassi Messaoud. It is an outlying part of the Berkine Basin, itself a region of the Ghadames Basin that extends into Tunisia. The land surface is dominated by extensive sand dune fields. Gassi Touil is the site of a major liquefied natural gas development project, in which natural gas extracted from the Gassi Touil field will be piped to a liquefaction plant at Djedid. The project was initially developed by Spanish firms Repsol and Gas Natural, but their contract was terminated in 2007 by the Algerian state oil company Sonatrach, which elected to pursue the project on its own. On November 6, 1961, a gas well fire broke out at Gassi Touil, becoming known as the Devil's Cigarette Lighter. It was finally extinguished on April 28, 1962, by well fire specialist Red Adair Paul Neal "Red" Adair (June 18, 1915 – August 7, 2004) [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Haoud El Hamra
Haoud El Hamra is a village in the commune of Hassi Messaoud, in Hassi Messaoud District, Ouargla Province, Algeria. The village is located north of Hassi Messaoud and east of the provincial capital Ouargla Ouargla ( Berber: Wargrən, ar, ورقلة) is the capital city of Ouargla Province in the Sahara Desert in southern Algeria. It has a flourishing petroleum industry and hosts one of Algeria's universities, the University of Ouargla. The commune .... References Neighbouring towns and cities Populated places in Ouargla Province {{Ouargla-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Djanet
Djanet ( ar, جانت) is an oasis city, and capital of Djanet District as well as of Djanet Province, southeast Algeria. It is located south of Illizi. According to the 2008 census it has a population of 14,655, up from 9,699 in 1998, and an annual population growth rate of 4.3%. It is inhabited by the Kel Ajjer Tuareg people. History The region of Djanet has been inhabited since Neolithic times. There were periods of ten thousand years at a time that the area was not desert. The flora and fauna were luxuriant as is seen in the numerous rock paintings of Tassili n'Ajjer around Djanet. Populations of hunter-gatherers lived there. Djanet was founded in the Middle Ages by the Tuareg. The Ottoman Empire, which had a nominal authority over the Fezzan region, reinforced their presence in the area at the beginning of the 20th century in reaction to the colonization of Africa by the Europeans. Geography Djanet, and the nearby towns of Azelouaz, El Mihan, Adjahil and Eferi, lie in ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Illizi
Illizi ( ar, إيليزي) is a town and commune, coextensive with Illizi District, situated in the south-eastern part of Algeria, and capital of Illizi Province. According to the 2008 census it is the largest commune by population in the province, with a population of 17,252, up from 10,163 in 1998, and an annual population growth rate of 5.5%, the highest in the province. It is one of the gates to the Tassili N'Ajjer National Park with caves situated under the sands containing prehistoric drawings dating from 6000 years BC. There is a hotel and two camping sites, as well as many local tourist agencies. Climate Illizi has a hot desert climate (Köppen climate classification ''BWh''), with long, extremely hot summers and short, very warm winters. The town is virtually rainless throughout the year as the average annual rainfall is around 10 mm (0.39 in), and summers are especially dry. The sky is always clear over Illizi all year long and the relative humidity is very l ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Biskra
Biskra ( ar, بسكرة ; ; Latin Vescera) is the capital city of Biskra Province, Algeria. In 2007, its population was recorded as 307,987. Biskra is located in northeastern Algeria, about 248 miles (400 km) from Algiers, 71 miles (115 km) southwest of Batna and 137 miles (222 km) north of Touggourt. It is nicknamed "The Queen of the Zibans", "The Door of the Desert" or "The Saharan Nice" because of its location at the beginning of the Sahara Desert. Due to its geographical location, its climate and natural resources, particularly farming, Biskra has always been a hub and a crossroad between the cities in the north and south. It has seen the passage of several civilizations, from the Romans and the Arabs to the French. In 1844, Biskra became a French garrison, which saw fighting during rebellions in 1849 and 1871. Currently the city of Biskra has 28 neighborhoods, including the three principal neighborhoods of, Korra, City 60 Logements, and Equipment Zones. I ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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