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Mountains Of Arta
The Arta Mountains, also known as the Great Mountains of Arta ( so, Buuraha Carta) are a mountain range in Djibouti. They sit at an average elevation of above sea level, is the tenth highest point in Djibouti. The mountains lie to the south of the Gulf of Tadjoura, in the Arta Region. They are situated approximately 35 kilometres (21 mi) west of the capital Djibouti City, and 69 kilometres (43 mi) by road from Ali Sabieh. Climate Arta Mountains has a hot semi-arid climate (Köppen BSh) surrounded by a hot desert climate (BWh). So it has a mild fresh weather, The climate is greatly affected by its varying geographic features. Due to its location at 755 metres (2,477 ft) above sea level, Arta Mountains climate is very warm summers and cool winters. See also *Arta Region Arta Region ( ar, إقليم عرتا, so, Gobolka Carta) is one of the six regions of Djibouti. It was officially created in 2003 by the regrouping of districts of the regions of Dikhil and Djibouti. ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Gulf Of Tadjoura
The Gulf of Tadjoura (; ) is a gulf or basin of the Indian Ocean in the Horn of Africa. It lies south of the straits of Bab-el-Mandeb, or the entrance to the Red Sea, at . The gulf has many fishing grounds, extensive coral reefs, and abundant pearl oysters. Most of its coastline is the territory of Djibouti, except for a short stretch on the southern shore, which is part of the territory of Somaliland. The Gulf’s other marine habitats include sea grass beds, salt pans and mangroves. History In August 1840, the conclusion of a treaty of friendship and commerce between the Sultan Mohammed bin Mohammed of Tadjoura and Commander Robert Moresby of the Indian Navy is tracking the sale of Moucha Island to Great Britain for ten sacks of rice. The sale will however follow any occupation. In 1887, Britain cedes sovereignty of the island to France at the same time it recognizes the French sphere of influence in the Gulf of Tadjoura, in exchange for the abandonment by France of any right ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Arta Region
Arta Region ( ar, إقليم عرتا, so, Gobolka Carta) is one of the six regions of Djibouti. It was officially created in 2003 by the regrouping of districts of the regions of Dikhil and Djibouti. It is situated in the south-central of the country, bordering the Tadjoura Region to the north, and the Djibouti Region to the north-east, and Dikhil Region the Ali Sabieh Region to the south, the country of Somaliland lies to the east. The capital of Arta Region is Arta. Other towns include We`a, Damerjog and Loyada. The Hemed mountain is the highest point in the region of Arta. History Nomadic life in the Arta Region dates back at least 2,000 years. During the Middle Ages, the Arta Region was ruled by the Ifat Sultanate and the Adal Sultanate. It later formed a part of the French Somaliland protectorate in the first half of the 20th century. Loyada village has a beautiful beach and a picturesque palm grove and the tombs of great historical leaders of this region. Halfway bet ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Arta, Djibouti
Arta ( so, Carta, ar, عرته) is a town in southeastern Djibouti. The center of the Arta Region, it is the country's sixth-largest city. , the population was 11,043. Arta is situated on the Mountains of Arta and is famous for its mild climate. It is located some west of the national capital, Djibouti City. History The Arta settlement is several centuries old. During the Middle Ages, it was ruled by the Ifat and Adal sultanates. Arta later formed a part of the French Somaliland protectorate in the first half of the 20th century. In the December 1942 British invasion of French Somaliland, about 700 British troops and Free French troops occupied the town. Under French colonial rule in 1946, a new housing estate and hill station was built. Arta's climate lent itself to becoming the prime sanctuary of the French civil servants in Djibouti. The region of Arta is inhabited of the popular ethnic group of Djibouti, the Issa, formulated the "Declaration of Arta", in which they p ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mountain Range
A mountain range or hill range is a series of mountains or hills arranged in a line and connected by high ground. A mountain system or mountain belt is a group of mountain ranges with similarity in form, structure, and alignment that have arisen from the same cause, usually an orogeny. Mountain ranges are formed by a variety of geological processes, but most of the significant ones on Earth are the result of plate tectonics. Mountain ranges are also found on many planetary mass objects in the Solar System and are likely a feature of most terrestrial planets. Mountain ranges are usually segmented by highlands or mountain passes and valleys. Individual mountains within the same mountain range do not necessarily have the same geologic structure or petrology. They may be a mix of different orogenic expressions and terranes, for example thrust sheets, uplifted blocks, fold mountains, and volcanic landforms resulting in a variety of rock types. Major ranges Most geolo ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Djibouti
Djibouti, ar, جيبوتي ', french: link=no, Djibouti, so, Jabuuti officially the Republic of Djibouti, is a country in the Horn of Africa, bordered by Somalia to the south, Ethiopia to the southwest, Eritrea in the north, and the Red Sea and the Gulf of Aden to the east. The country has an area of . In antiquity, the territory, together with Ethiopia, Eritrea and Somaliland, was part of the Land of Punt. Nearby Zeila, now in Somaliland, was the seat of the medieval Adal and Ifat Sultanates. In the late 19th century, the colony of French Somaliland was established following treaties signed by the ruling Dir Somali sultans with the French, and its railroad to Dire Dawa (and later Addis Ababa) allowed it to quickly supersede Zeila as the port for southern Ethiopia and the Ogaden. It was renamed the French Territory of the Afars and the Issas in 1967. A decade later, the Djiboutian people voted for independence. This officially marked the establishment of the ''Rep ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Djibouti City
Djibouti (also called Djibouti City and in many early English texts and on many early maps, Jibuti; so, Magaalada Jabuuti, french: link=no, Ville de Djibouti, ar, مدينة جيبوتي, aa, Gabuutî Magaala) is the eponymous capital of Djibouti, and has more people than the rest of Djibouti combined. It is located in the coastal Djibouti Region on the Gulf of Tadjoura. Djibouti has a population of around 600,000 inhabitants, which counts for 54% of the country's population. The settlement was founded in 1888 by the French, on land leased from the ruling Somali and Afar Sultans. During the ensuing period, it served as the capital of French Somaliland and its successor the French Territory of the Afars and Issas. Known as the ''Pearl of the Gulf of Tadjoura'' due to its location, Djibouti is strategically positioned near the world's busiest shipping lanes and acts as a refueling and transshipment center. The Port of Djibouti is the principal maritime port for imports to and ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ali Sabieh
Ali Sabieh ( so, Cali Sabiix, ar, علي صبيح) is the second largest city in Djibouti. It is situated about Southwest of Djibouti City and north of the border with Ethiopia. It sprawls on a wide basin surrounded by granitic mountains on all sides. The famous landmark of Ali Sabieh is located near the city. History The Ali Sabieh settlement is several centuries old. During the Middle Ages, it was ruled by the Ifat and Adal sultanates. According to an old legend, the present-day territory of Ali Sabieh was covered by some trees and wadis. Where the nomadics use to stopping here for water on the way to the town of Zeila and after the signing treaties in 1894 with the then ruling Issa Somali Sultans, to established a protectorate in the region referred to as French Somaliland. Ali Sabieh became an administrative and commercial centre in the 1900s after the construction of the Ethio-Djibouti Railways, the first railway in French Somaliland. In 1904, a report notes that "when t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Semi-arid Climate
A semi-arid climate, semi-desert climate, or steppe climate is a dry climate sub-type. It is located on regions that receive precipitation below potential evapotranspiration, but not as low as a desert climate. There are different kinds of semi-arid climates, depending on variables such as temperature, and they give rise to different biomes. Defining attributes of semi-arid climates A more precise definition is given by the Köppen climate classification, which treats steppe climates (''BSk'' and ''BSh'') as intermediates between desert climates (BW) and humid climates (A, C, D) in ecological characteristics and agricultural potential. Semi-arid climates tend to support short, thorny or scrubby vegetation and are usually dominated by either grasses or shrubs as it usually can't support forests. To determine if a location has a semi-arid climate, the precipitation threshold must first be determined. The method used to find the precipitation threshold (in millimeters): *multiply by ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Desert Climate
The desert climate or arid climate (in the Köppen climate classification ''BWh'' and ''BWk''), is a dry climate sub-type in which there is a severe excess of evaporation over precipitation. The typically bald, rocky, or sandy surfaces in desert climates are dry and hold little moisture, quickly evaporating the already little rainfall they receive. Covering 14.2% of earth's land area, hot deserts are the second most common type of climate on earth after the polar climate. There are two variations of a desert climate according to the Köppen climate classification: a hot desert climate (''BWh''), and a cold desert climate (''BWk''). To delineate "hot desert climates" from "cold desert climates", there are three widely used isotherms: most commonly a mean annual temperature of , or sometimes the coldest month's mean temperature of , so that a location with a ''BW'' type climate with the appropriate temperature above whichever isotherm is being used is classified as "hot arid sub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
National Oceanic And Atmospheric Administration
The National Oceanic and Atmospheric Administration (abbreviated as NOAA ) is an United States scientific and regulatory agency within the United States Department of Commerce that forecasts weather, monitors oceanic and atmospheric conditions, charts the seas, conducts deep sea exploration, and manages fishing and protection of marine mammals and endangered species in the U.S. exclusive economic zone. Purpose and function NOAA's specific roles include: * ''Supplying Environmental Information Products''. NOAA supplies to its customers and partners information pertaining to the state of the oceans and the atmosphere, such as weather warnings and forecasts via the National Weather Service. NOAA's information services extend as well to climate, ecosystems, and commerce. * ''Providing Environmental Stewardship Services''. NOAA is a steward of U.S. coastal and marine environments. In coordination with federal, state, local, tribal and international authorities, NOAA manages the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mountains Of Djibouti
A mountain is an elevated portion of the Earth's crust, generally with steep sides that show significant exposed bedrock. Although definitions vary, a mountain may differ from a plateau in having a limited summit area, and is usually higher than a hill, typically rising at least 300 metres (1,000 feet) above the surrounding land. A few mountains are isolated summits, but most occur in mountain ranges. Mountains are formed through tectonic forces, erosion, or volcanism, which act on time scales of up to tens of millions of years. Once mountain building ceases, mountains are slowly leveled through the action of weathering, through slumping and other forms of mass wasting, as well as through erosion by rivers and glaciers. High elevations on mountains produce colder climates than at sea level at similar latitude. These colder climates strongly affect the ecosystems of mountains: different elevations have different plants and animals. Because of the less hospitable terrain and ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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