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MURCANYO MEDIA
Murcanyo ( so, Muranyo, ar, مورايو), also known as Bander Murcaayo (alternatively ''Bandar Murcaayo'' or ''Bunder Marayah''), is a coastal town in the northeastern Bari province of Somalia. It is situated in the autonomous Puntland region. Location Murcanyo is located at , in the Gulf of Aden. It lies 7 nautical miles (8 miles) southwest of Habo, 18 nautical miles (21 miles) southwest of Ras Filuk, and 38 nautical miles (44 miles) east of Qandala. Geography The town is situated along the beach of a long bay that borders the Gulf of Aden. Murcanyo lies at the foot of the Jebel Murcanyo mountains (''Jebel'' meaning mountain in Arabic), also known as ''Jebel Marayah''. This mountain range stretches across the Bari region to the Indian Ocean coastline at Bargal. The range consists of cream-coloured limestone, as well as sandstone, shale and quartz. History Murcanyo was historically an important port town along the northeastern Somalia littoral. It served as a stronghold of Be ...
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Administrative Divisions Of Somalia
Somalia is officially divided into 18 administrative regions (''gobollo'', singular ''gobol'') . These are in turn subdivided into seventy-two districts (plural ''degmooyin''; singular ''degmo'') On a ''de facto'' basis, northern Somalia is now divided up among the autonomous region of Puntland (which considers itself an autonomous state) and Somaliland (a self-declared but unrecognized sovereign state). In central Somalia, Galmudug is another regional entity that emerged south of Puntland. For these civil war divisions, see '' States and regions of Somalia''. Regions and districts Historical divisions Pre-independence In 1931, Italian Somaliland consisted of seven commissariats."Regions of Somalia"
''Statoids''. Retrieved 20 February 2011.
* Alto Giuba * Alto Uebi-Scebeli * Basso Giuba * Basso Uebi-Scebeli * Migiurtinia * Mogadi ...
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Limestone
Limestone ( calcium carbonate ) is a type of carbonate sedimentary rock which is the main source of the material lime. It is composed mostly of the minerals calcite and aragonite, which are different crystal forms of . Limestone forms when these minerals precipitate out of water containing dissolved calcium. This can take place through both biological and nonbiological processes, though biological processes, such as the accumulation of corals and shells in the sea, have likely been more important for the last 540 million years. Limestone often contains fossils which provide scientists with information on ancient environments and on the evolution of life. About 20% to 25% of sedimentary rock is carbonate rock, and most of this is limestone. The remaining carbonate rock is mostly dolomite, a closely related rock, which contains a high percentage of the mineral dolomite, . ''Magnesian limestone'' is an obsolete and poorly-defined term used variously for dolomite, for limes ...
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MURCANYO MEDIA
Murcanyo ( so, Muranyo, ar, مورايو), also known as Bander Murcaayo (alternatively ''Bandar Murcaayo'' or ''Bunder Marayah''), is a coastal town in the northeastern Bari province of Somalia. It is situated in the autonomous Puntland region. Location Murcanyo is located at , in the Gulf of Aden. It lies 7 nautical miles (8 miles) southwest of Habo, 18 nautical miles (21 miles) southwest of Ras Filuk, and 38 nautical miles (44 miles) east of Qandala. Geography The town is situated along the beach of a long bay that borders the Gulf of Aden. Murcanyo lies at the foot of the Jebel Murcanyo mountains (''Jebel'' meaning mountain in Arabic), also known as ''Jebel Marayah''. This mountain range stretches across the Bari region to the Indian Ocean coastline at Bargal. The range consists of cream-coloured limestone, as well as sandstone, shale and quartz. History Murcanyo was historically an important port town along the northeastern Somalia littoral. It served as a stronghold of Be ...
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Cape Guardafui
Cape Guardafui ( so, Gees Gardafuul, or Raas Caseyr, or Ras Asir, it, Capo Guardafui) is a headland in the autonomous Puntland region in Somalia. Coextensive with Puntland's Gardafuul administrative province, it forms the geographical apex of the Horn of Africa. Its shore at 51°27'52"E is the second easternmost point on mainland Africa after Ras Hafun. The offshore oceanic strait Guardafui Channel (or ''Marinka Gardafuul'') is named after it. Location Cape Guardafui is located at , next to the Guardafui Channel. The archipelago of Socotra lies off the cape in the north of the Somali Sea. Fifteen leagues (45 miles) west of Guardafui is Ras Filuk, a steep cliff jutting into the Gulf of Aden from flatland. The mountain is believed to correspond with the ancient ''Elephas Mons'' or ''Cape Elephant'' (''Ras Filuk'' in Arabic) described by Strabo. History Referred to as '' Aromata promontorium'' (Greek: Αρώματον ἄκρον) by the ancient Greeks, Guardafui was describ ...
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Mumbai
Mumbai (, ; also known as Bombay — the official name until 1995) is the capital city of the Indian state of Maharashtra and the ''de facto'' financial centre of India. According to the United Nations, as of 2018, Mumbai is the second-most populous city in India after Delhi and the eighth-most populous city in the world with a population of roughly 20 million (2 crore). As per the Indian government population census of 2011, Mumbai was the most populous city in India with an estimated city proper population of 12.5 million (1.25 crore) living under the Brihanmumbai Municipal Corporation. Mumbai is the centre of the Mumbai Metropolitan Region, the sixth most populous metropolitan area in the world with a population of over 23 million (2.3 crore). Mumbai lies on the Konkan coast on the west coast of India and has a deep natural harbour. In 2008, Mumbai was named an alpha world city. It has the highest number of millionaires and billionaires among all cities i ...
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Jeddah
Jeddah ( ), also spelled Jedda, Jiddah or Jidda ( ; ar, , Jidda, ), is a city in the Hejaz region of the Kingdom of Saudi Arabia (KSA) and the country's commercial center. Established in the 6th century BC as a fishing village, Jeddah's prominence grew in 647 when the Caliph Osman made it a major port for Indian Ocean trade routes, channelling goods to Mecca, and to serve Muslim travelers for Islamic pilgrimage. Since those times, Jeddah has served as the gateway for millions of pilgrims who have arrived in Saudi Arabia, traditionally by sea and recently by air. With a population of about 4,697,000 people as of 2021, Jeddah is the largest city in Makkah Province, the largest city in Hejaz, the second-largest city in the Saudi Arabia (after the capital Riyadh), and the ninth-largest in the Middle East. It also serves as the administrative centre of the OIC. Jeddah Islamic Port, on the Red Sea, is the thirty-sixth largest seaport in the world and the second-largest and s ...
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Mukalla
Mukalla ( ar, ٱلْمُكَلَّا, ') is a seaport and the capital city of Yemen's largest governorate, Hadhramaut. The city is in the southern part of the Arabian Peninsula on the Gulf of Aden, on the shores of the Arabian Sea, about east of Aden. It is the most important port in the Hadhramaut and the fifth-largest city in Yemen, with a population of approximately 500,000. The city is served by the nearby Riyan International Airport. History Mukalla is not far from Cane or Qana, the ancient principal Hadrami trading post between India and Africa, with incense producing areas in its hinterland. Mukalla was founded in 1035 as a fishing settlement. This area was part of Oman until the middle of the 11th century, and later this area became part of Yemen. After witnessing a struggle for control by the Kathiri and Qu'aiti Sultanates in the 19th and 20th centuries, it became the capital of the Qu'aiti State of Hadhramaut, and then in 1967, it became a part of South Yemen. The Qu ...
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Dhow
Dhow ( ar, داو, translit=dāwa; mr, script=Latn, dāw) is the generic name of a number of traditional sailing vessels with one or more masts with settee or sometimes lateen sails, used in the Red Sea and Indian Ocean region. Typically sporting long thin hulls, dhows are trading vessels primarily used to carry heavy items, such as fruit, fresh water, or other heavy merchandise, along the coasts of Eastern Arabia, East Africa, Yemen and coastal South Asia (Pakistan, India, Bangladesh). Larger dhows have crews of approximately thirty, smaller ones typically around twelve. History The exact origins of the dhow are lost to history. Some claim that the sambuk, a type of dhow, may be derived from the Portuguese caravel. The dhow was the ship of trade used by the Swahili. It was a dhow that transported a giraffe to Chinese Emperor Yong Le's court, in 1414. Another source suggests the ship that carried the giraffe to China was part of a large Chinese fleet led by Zheng He. Ships ...
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Majeerteen
The Majeerteen ( so, Majeerteen, ar, ماجرتين; also spelled Majerteen, Macherten, Majertain, or Mijurtin) is a sub-clan. It is one of the major Somali groups, with a vast traditional territory spanning 3 major regions of Somalia: Bari, Nugaal and Mudug. From Bosaso down to Garacad, the Majerteen settle in what is literally considered to be the 'Horn of Africa'. They can also be found in Kismayo in southern Somalia. Its members form a part of the Harti Darod clan family, and primarily inhabit the Puntland state of northern Somalia. Overview The Majeerteen Sultanates played an important role in the pre-independence era of Somalia. The Majeerteen also held many other significant government posts in the 1960s and 1970s, and continue to play a key role in Puntland state and Somalia as a whole. For the treaty between the Majeerteen and colonial powers, see "treaties". Distribution The Majeerteen are traditionally settled in Somalia's northern regions of Bari, Nugal and ...
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Quartz
Quartz is a hard, crystalline mineral composed of silica (silicon dioxide). The atoms are linked in a continuous framework of SiO4 silicon-oxygen tetrahedra, with each oxygen being shared between two tetrahedra, giving an overall chemical formula of SiO2. Quartz is the second most abundant mineral in Earth's continental crust, behind feldspar. Quartz exists in two forms, the normal α-quartz and the high-temperature β-quartz, both of which are chiral. The transformation from α-quartz to β-quartz takes place abruptly at . Since the transformation is accompanied by a significant change in volume, it can easily induce microfracturing of ceramics or rocks passing through this temperature threshold. There are many different varieties of quartz, several of which are classified as gemstones. Since antiquity, varieties of quartz have been the most commonly used minerals in the making of jewelry and hardstone carvings, especially in Eurasia. Quartz is the mineral defining the val ...
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Shale
Shale is a fine-grained, clastic sedimentary rock formed from mud that is a mix of flakes of clay minerals (hydrous aluminium phyllosilicates, e.g. kaolin, Al2 Si2 O5( OH)4) and tiny fragments (silt-sized particles) of other minerals, especially quartz and calcite.Blatt, Harvey and Robert J. Tracy (1996) ''Petrology: Igneous, Sedimentary and Metamorphic'', 2nd ed., Freeman, pp. 281–292 Shale is characterized by its tendency to split into thin layers ( laminae) less than one centimeter in thickness. This property is called '' fissility''. Shale is the most common sedimentary rock. The term ''shale'' is sometimes applied more broadly, as essentially a synonym for mudrock, rather than in the more narrow sense of clay-rich fissile mudrock. Texture Shale typically exhibits varying degrees of fissility. Because of the parallel orientation of clay mineral flakes in shale, it breaks into thin layers, often splintery and usually parallel to the otherwise indistinguishable beddin ...
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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 ...
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