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Al-Khor SC Managers
Al Khor (; also spelled ''Al Khawr''), officially Al Khor and Al Thakhira, is a municipality in northeastern Qatar. Al Khor City, the municipal seat, is located on the northeast coast of Qatar, around from the capital, Doha and is considered to be one of Qatar's the major cities. Al Thakhira is the second most significant settlement in the municipality after Al Khor City. The region was ruled by the Al Muhannadi tribe, which consists of seven Bedouin families, before Qatar gained its independence in 1971. Tourism has been increasing in recent years owing to the municipality's various resorts, natural areas and cultural attractions. Fishing was the historical mainstay of most of the municipality's inhabitants. Etymology Al Khor Municipality derives its name from the city of the same name. In Arabic, ''Al Khawr'' means bay; it was so named because Al Khor City was near a bay. Formerly, the city was known as "Khor Al-Shaqiq". History Al Khor Municipality was established in Jul ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Municipalities Of Qatar
Since 2015, Qatar has been divided into eight Municipality, municipalities. In 2004, a new municipality, Al Daayen, was created under Resolution No. 13, formed from parts of Umm Salal and Al Khawr; at the same time, Al Ghuwariyah was merged with Al Khawr; Al Jumaliyah was merged with Ar Rayyan; Jarayan al Batnah was split between Al Rayyan and Al Wakrah; and Mesaieed was merged with Al Wakrah. In 2014, the western city of Al-Shahaniya split off from Al Rayyan Municipality to form its own municipality. For statistical purposes, the municipalities are further subdivided into Zones of Qatar, 98 zones (as of 2015), which are in turn subdivided into districts and blocks, the latter being the lowest subdivision. History According to Ministry of Municipality and Urban Planning, in 1963, the first municipality was the Municipality of Qatar, created under Law No. 11. Later in the same year, its name was changed to Municipality of Doha by Law No. 15. Then, on 17 July 1972, Ar Rayyan, Al Wak ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Al-Shahaniya
Al Shahaniya () is a municipality (3299 km2) in Qatar, with its municipal seat being a city of the Al-Shahaniya (city), same name (39 km2). Formerly in the municipalities of Qatar, municipality of Al Rayyan, but now an independent municipality, the municipal seat was delimited in 1988 by Law No. 22. In 2014, the cabinet ratified a draft amending provisions to the 1988 law that formalized Al Shahaniya as Qatar's eighth municipality. Etymology Al-Shahaniya derives its name from a plant known locally as 'sheeh' which was valued for its anti-inflammatory properties. A variation of this name is ''Al-Sheehaniya''. The plant's Latin name is ''Artemisia inculta''; it is an aromatic perennial that frequently grows in the MENA, Middle East and North Africa region but which is scarce in Qatar due to its unsuitable soils. History In 2014, Al-Shahaniya split off from Al Rayyan Municipality to form its own municipality. Integrating approximately 35% of Al Rayyan's area into the new ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Madinat Al Kaaban
Madinat Al Kaaban () is a village in Qatar, located in the municipalities of Qatar, municipality of Ash Shamal. It lies close to the border with Al Khor, Al Khor Municipality. Etymology The 'madinat' portion translates to 'city' in English. 'Kaaban' refers to the Al-Kaabi tribe, who founded the village. Geography Madinat Al Kaaban has historically been inhabited by the Al-Kaabi tribe. To the north-east of the village is Waab Al Mashrab, a now-abandoned village. Waab Al Mashrab was likely built around the 1950s and was also mainly inhabited by the Al-Kaabi tribe, but the village was abandoned in 1976 amidst the government's efforts to resettle rural Qataris to urban areas. Some of its inhabitants moved to Madinat Al Kaaban. Now in ruins, Waab Al Mashrab has approximately 50 houses, a mosque, a school and several farms. Qatar's capital city, Doha, is about 65 km south from the village while Madinat ash Shamal is roughly 35 km to the north-west. Infrastructure After Qata ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Simaisma
Simaisma (; also spelled Sumaysimah) is a small seaside town located on the eastern coast of Qatar 30 km north of the capital Doha. The town features old houses and mosques from the days before the discovery of oil and natural gas in Qatar. It was demarcated in 1988. Small clusters of mangroves dot its coastline. Geographically, it is located in the municipality of Al Daayen, but administratively, it is a part of Al Khor. Etymology Simaisma is believed to derive from the diminutive form of the Arabic word ''simsim'' (), meaning "sesame". The term refers to the small sandy mounds constituting the area's natural landscape. History Simaisma was also the location of a battle fought in 1768 between Shaikh Mohamed bin Khalifa Al Khalifa the Chief of Zubarah and the Musalam clan who were based at Freiha. The cause of the Battle of Simaisma was Shaikh Mohamed's refusal to pay taxes to the Al Musalam after he built his castle. The Al Musalam were defeated and soon their power waned ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Avicennia Marina
''Avicennia marina'', commonly known as grey mangrove or white mangrove, is a species of mangrove tree classified in the plant family Acanthaceae (formerly in the Verbenaceae or Avicenniaceae). As with other mangroves, it occurs in the intertidal zones of estuarine areas. Description Grey mangroves grow as a shrub or tree to a height of , or up to in tropical regions. The habit is a gnarled arrangement of multiple branches. It has smooth light-grey bark made up of thin, stiff, brittle flakes. This may be whitish, a characteristic described in the common name. The leaves are thick, long, a bright, glossy green on the upper surface, and silvery-white, or grey, with very small matted hairs on the surface below. As with other ''Avicennia'' species, it has aerial roots (pneumatophores), which grow to a height of about , and a diameter of . These allow the plant to absorb oxygen, which is deficient in its habitat. These roots also anchor the plant during the frequent inundatio ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Coral Reef
A coral reef is an underwater ecosystem characterized by reef-building corals. Reefs are formed of colonies of coral polyps held together by calcium carbonate. Most coral reefs are built from stony corals, whose polyps cluster in groups. Coral belongs to the class Anthozoa in the animal phylum Cnidaria, which includes sea anemones and jellyfish. Unlike sea anemones, corals secrete hard carbonate exoskeletons that support and protect the coral. Most reefs grow best in warm, shallow, clear, sunny and agitated water. Coral reefs first appeared 485 million years ago, at the dawn of the Early Ordovician, displacing the microbial and sponge reefs of the Cambrian. Sometimes called ''rainforests of the sea'', shallow coral reefs form some of Earth's most diverse ecosystems. They occupy less than 0.1% of the world's ocean area, about half the area of France, yet they provide a home for at least 25% of all marine species, including fish, mollusks, worms, crustaceans, ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cape (geography)
In geography, a cape is a headland, peninsula or promontory extending into a body of water, usually a sea. A cape usually represents a marked change in trend of the Coast, coastline, often making them important landmarks in sea navigation. This also makes them prone to natural forms of erosion, mainly tidal actions, resulting in a relatively short geological lifespan. Formation Capes can be formed by Glacier, glaciers, Volcano, volcanoes, and changes in sea level. Erosion plays a large role in each of these methods of formation. Coastal erosion by waves and currents can create capes by wearing away softer rock and leaving behind harder rock formations. Movements of the Earth's crust can uplift land, forming capes. For example, the Cape of Good Hope was formed by tectonic forces. Volcanic eruptions can create capes by depositing lava that solidifies into new landforms. Cape Verde, (also known as Cabo Verde) is an example of a volcanic cape. Glaciers can carve out capes by erod ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sabkha
A sabkha () is a predominately coastal, supratidal mudflat or sandflat in which evaporite-saline minerals accumulate as the result of a semiarid to arid climate. Sabkhas are gradational between land and intertidal zone within restricted coastal plains just above normal high-tide level. Within a sabkha, evaporite-saline mineral sediments typically accumulate below the surface of mudflats or sandflats. Evaporite-saline minerals, tidal-flood, and aeolian deposits characterize many sabkhas found along modern coastlines. The accepted type locality for a sabkha is at the southern coast of the Persian Gulf, in the United Arab Emirates.Neuendorf, K.K.E., J.P. Mehl, Jr., and J.A. Jackson, eds. (2005) ''Glossary of Geology'' (5th ed.). Alexandria, Virginia, American Geological Institute. 779 pp. Tucker, M.E. and Wright, V.P., 2009. ''Carbonate sedimentology.'' John Wiley & Sons. and Warren, J.K., 2006. Evaporites: sediments, resources and hydrocarbons. Springer Science & Business Media ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Highland
Highlands or uplands are areas of high elevation such as a mountainous region, elevated mountainous plateau or high hills. Generally, ''upland'' refers to a range of hills, typically from up to , while ''highland'' is usually reserved for ranges of low mountains. However, the two terms are interchangeable and also include regions that are transitional between hilly and mountainous terrain. Highlands internationally Probably the best-known area officially or unofficially referred to as ''highlands'' in the Anglosphere is the Scottish Highlands in northern Scotland, the mountainous region north and west of the Highland Boundary Fault. The Highland (council area), Highland council area is a local government (Scotland), local government area in the Scottish Highlands and Britain's largest local government area. Other highland or upland areas reaching 400 m or higher in the United Kingdom include the Southern Uplands in Scotland, the Pennines, North York Moors, Dartmoor and Exmoor ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Plain
In geography, a plain, commonly known as flatland, is a flat expanse of land that generally does not change much in elevation, and is primarily treeless. Plains occur as lowlands along valleys or at the base of mountains, as coastal plains, and as plateaus or Highland, uplands. Plains are one of the major landforms on earth, being present on all continents and covering more than one-third of the world's land area. Plains in many areas are important for agriculture. There are various types of plains and biomes on them. Description A plain or flatland is a flat expanse of land with a layer of grass that generally does not change much in elevation, and is primarily treeless. Plains occur as lowlands along valleys or at the base of mountains, as coastal plains, and as plateaus or Highland, uplands. Plains are one of the major landforms on earth, where they are present on all continents, and cover more than one-third of the world's land area. In a valley, a plain is enclosed on tw ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Stream
A stream is a continuous body of water, body of surface water Current (stream), flowing within the stream bed, bed and bank (geography), banks of a channel (geography), channel. Depending on its location or certain characteristics, a stream may be referred to by a variety of local or regional names. Long, large streams are usually called rivers, while smaller, less voluminous and more intermittent river, intermittent streams are known, amongst others, as brook, creek, rivulet, rill, run, tributary, feeder, freshet, narrow river, and streamlet. The flow of a stream is controlled by three inputs – surface runoff (from precipitation or meltwater), daylighting (streams), daylighted subterranean river, subterranean water, and surfaced groundwater (Spring (hydrology), spring water). The surface and subterranean water are highly variable between periods of rainfall. Groundwater, on the other hand, has a relatively constant input and is controlled more by long-term patterns of pr ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Wadi
Wadi ( ; ) is a river valley or a wet (ephemerality, ephemeral) Stream bed, riverbed that contains water only when heavy rain occurs. Wadis are located on gently sloping, nearly flat parts of deserts; commonly they begin on the distal portions of alluvial fans and extend to inland sabkhas or dry lakes. Permanent channels do not exist, due to lack of continual water flow. Water percolates down into the stream bed, causing an abrupt loss of energy and resulting in vast deposition. Wadis may develop dams of sediment that change the stream patterns in the next flash flood. Wadis tend to be associated with centers of human population because sub-surface water is sometimes available in them. Nomadic and pastoral desert peoples will rely on seasonal vegetation found in wadis, even in regions as dry as the Sahara, as they travel in complex transhumance routes. The centrality of wadis to water – and human life – in desert environments gave birth to the distinct sub-field of wadi h ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
