Anniversary of the Overthrow of the Derg Regime Federal Democratic Republic of Ethiopia

Ethiopia, country on the Horn of Africa. The country lies completely within the tropical latitudes and is relatively compact, with similar north-south and east-west dimensions. The capital is Addis Ababa (“New Flower”), located almost at the centre of the country. Ethiopia is the largest and most populated country in the Horn of Africa. With the 1993 secession of Eritrea, its former province along the Red Sea, Ethiopia became landlocked. Ethiopia is one of the world’s oldest countries, its territorial extent having varied over the millennia of its existence. In ancient times it remained centred on Aksum, an imperial capital located in the northern part of the modern state, about 100 miles (160 km) from the Red Sea coast. The present territory was consolidated during the 19th and 20th centuries as European powers encroached into Ethiopia’s historical domain. Ethiopia became prominent in modern world affairs first in 1896, when it defeated colonial Italy in the Battle of Adwa, and again in 1935–36, when it was invaded and occupied by fascist Italy. Liberation during World War II by the Allied powers set the stage for Ethiopia to play a more prominent role in world affairs. Ethiopia was among the first independent nations to sign the Charter of the United Nations, and it gave moral and material support to the decolonization of Africa and to the growth of Pan-African cooperation. These efforts culminated in the establishment of the Organization of African Unity (since 2002, the African Union) and the United Nations Economic Commission for Africa, both of which have their headquarters in Addis Ababa. … Relief of Ethiopia Ethiopia is bounded by Eritrea to the north, Djibouti to the northeast, Somalia to the east, Kenya to the south, and South Sudan and Sudan to the west. Ethiopia’s topography, one of the most rugged in Africa, is built on four geologic formations. Rocks of Precambrian origin (more than 540 million years in age) form the oldest basal complex of Ethiopia, as they do in most of Africa. The Precambrian layer is buried under more recent geologic formations—except in parts of northern, western, and southern Ethiopia, where there are exposed rock layers of granite and schist. Geologic processes of the Mesozoic Era (about 250 to 65 million years ago) contributed sedimentary layers of limestone and sandstone, most of which have been either eroded or covered by volcanic rocks. Younger sedimentary layers are found in northern Ethiopia and on the floors of the Rift Valley. Lava flows from the Cenozoic Era (i.e., the past 65 million years) have formed basaltic layers that now cover two-thirds of Ethiopia’s land surface with a thickness ranging from about 1,000 feet (300 metres) to almost 10,000 feet (3,000 metres). The Rift Valley forms a spectacular graben (a massive tectonic trough) running right down the middle of the country from the northern frontier with Eritrea to the southern border with Kenya. Although Ethiopia’s complex relief defies easy classification, five topographic features are discernible. These are the Western Highlands, the Western Lowlands, the Eastern Highlands, the Eastern Lowlands, and the Rift Valley. The Western Highlands are the most extensive and rugged topographic component of Ethiopia. The most spectacular portion is the North Central massifs; these form the roof of Ethiopia, with elevations ranging from 14,872 feet (4,533 metres) for Mount Ras Dejen (or Dashen), the highest point in Ethiopia, to the Blue Nile and Tekeze river channels 10,000 feet below. Lake Tana—Ethiopia’s largest inland lake and the main reservoir for the Blue Nile River—is located in this region, at an elevation of about 6,000 feet (1,800 metres). The Western Lowlands stretch north-south along the border with Sudan and South Sudan and include the lower valleys of the Blue Nile, Tekeze, and Baro rivers. With elevations of about 3,300 feet (1,000 metres), these lowlands become too hot to attract dense settlement. The Rift Valley is part of the larger East African Rift System. Hemmed in by the escarpments of the Western and Eastern Highlands, it has two distinct sections. The first part is in the northeast, where the valley floor widens into a funnel shape as it approaches the Red Sea and the Gulf of Aden. This is a relatively flat area interrupted only by occasional volcanic cones, some of which are active. The Denakil Plain, in which a depression known as the Kobar Sink drops as low as 380 feet (116 metres) below sea level, is found here. High temperatures and lack of moisture make the northeastern Rift Valley unattractive for settlement. The southwestern section, on the other hand, is a narrow depression of much higher elevation. It contains Ethiopia’s Lakes Region, an internal drainage basin of many small rivers that drain into Lakes Abaya, Abiyata, Awasa, Langano, Shala, Chamo, and Ziway. Together these lakes have more than 1,200 square miles (3,108 square km) of water surface. The upper Rift Valley is one of the most productive and most settled parts of Ethiopia. The Eastern Highlands are much smaller in extent than the Western Highlands, but they offer equally impressive contrast in topography. The highest peaks are Tullu Deemtu (Tulu Dīmtu), at 14,360 feet (4,377 metres), and Mount Batu, at 14,127 feet (4,305 metres). The Eastern Lowlands resemble the long train of a bridal gown suddenly dipping from the narrow band of the Eastern Highlands and gently rolling for hundreds of miles to the Somalian border. Two important regions here are the Ogaden and the Hawd. The Shebele and Genale rivers cross the lowlands, moderating the desert ecology. Drainage Ethiopia has three principal drainage systems. The first and largest is the western drainage system, which includes the watersheds of the Blue Nile (known as the Abay in Ethiopia), the Tekeze, and the Baro rivers. All three rivers flow west to the White Nile in South Sudan and Sudan. The second is the Rift Valley internal drainage system, composed of the Awash River, the Lakes Region, and the Omo River. The Awash flows northeast to the Denakil Plain before it dissipates into a series of swamps and Lake Abe at the border with Djibouti. The Lakes Region is a self-contained drainage basin, and the Omo flows south into Lake Turkana (Rudolf), on the border with Kenya. The third system is that of the Shebele and Genale rivers. Both of these rivers originate in the Eastern Highlands and flow southeast toward Somalia and the Indian Ocean. Only the Genale (known as the Jubba in Somalia) makes it to the sea; the Shebele (in Somali, Shabeelle) disappears in sand just inside the coastline. More … Score: https://www.britannica.com/place/Ethiopia

2023/05/28

Anniversary of the Proclamation of the Azerbaijani Republic

Azerbaijan, also spelled Azerbaidzhan, officially Azerbaijani Republic, Azerbaijani Azärbayjan Respublikasi, country of eastern Transcaucasia. Occupying an area that fringes the southern flanks of the Caucasus Mountains, it is bounded on the north by Russia, on the east by the Caspian Sea, on the south by Iran, on the west by Armenia, and on the northwest by Georgia. The exclave of Naxçıvan (Nakhichevan) is located southwest of Azerbaijan proper, bounded by Armenia, Iran, and Turkey. Azerbaijan includes within its borders the predominantly Armenian enclave of Nagorno-Karabakh, which from 1988 was the focus of intense conflict between Azerbaijan and Armenia. The capital of Azerbaijan is the ancient city of Baku (Bakı), whose harbour is the best on the Caspian Sea. In addition to its variegated and often beautiful terrain, Azerbaijan offers a blend of traditions and modern development. The people of its remoter areas retain many distinctive folk traditions, but the lives of its inhabitants have been much influenced by accelerating modernization, characterized by industrialization, the development of power resources, and the growth of the cities, in which more than half the people now live. Industry dominates the economy, and more-diversified pursuits have supplemented the exploitation of oil, of which Azerbaijan was the world’s leading producer at the beginning of the 20th century. Fine horses and caviar continue as some of the more distinctive traditional exports of the republic. Azerbaijan was an independent nation from 1918 to 1920 but was then incorporated into the Soviet Union. It became a constituent (union) republic in 1936. Azerbaijan declared sovereignty on September 23, 1989, and independence on August 30, 1991. Land - Relief, drainage, and soils As a result of its broken relief, drainage patterns, climatic differences, and sharply defined altitudinal zoning of vegetation, Azerbaijan is characterized by a wide variety of landscapes. More than two-fifths of its territory is taken up by lowlands, about half lies at 1,300 to 4,900 feet (400 to 1,500 metres), and areas above 4,900 feet occupy a little more than one-tenth of the total area. The highest peaks are Bazardyuzyu (Bazardüzü; 14,652 feet [4,466 metres]), Shakhdag, and Tufan, all part of the Greater Caucasus range, the crest of which forms part of Azerbaijan’s northern boundary. Magnificent spurs and ridges, cut into by the deep gorges of mountain streams, make this part of Azerbaijan a region of great natural beauty. At the same time, it lies within a region characterized by a high degree of seismic activity. The spurs of the Lesser Caucasus, in southwestern Azerbaijan, form the second important mountain system, which includes the Shakhdag, Murovdag, and Zangezur ranges, their summits rising to nearly 13,000 feet, and also the Karabakh Upland. The large and scenic Lake Geygyol lies at an altitude of 5,138 feet. The southeastern part of Azerbaijan is bordered by the Talish (Talysh) Mountains, consisting of three longitudinal ranges, with Mount Kyumyurkyoy as the highest peak (8,176 feet), and the Länkäran Lowland, along the Caspian coast. This lowland, an extension of the Kura-Aras Lowland, reaches the Iranian border near Astara. The Kura-Aras Lowland is named for the main river, the Kura (Kür), and its tributary the Aras (Araz). The Shirvan, Milskaya, and Mugan plains are part of this lowland and have similar soils and climate. Gray soils and saline solonchaks (aridisols) and, in higher regions, gray alkaline solonetz and chestnut soils (mollisols) prevail. A well-developed network of canals between the Kura and Aras rivers makes it possible to irrigate a major part of the lowland. The Upper Karabakh Canal, 107 miles (172 kilometres) long, provides a vital link between the Aras River and the Mingäçevir Reservoir on the Kura River. The reservoir has a surface area of 234 square miles and a maximum depth of 246 feet. The Upper Karabakh Canal alone irrigates more than 250,000 acres (100,000 hectares) of fertile land and in addition supplies the Aras River with water during dry summer periods. The Upper Shirvan Canal, the second most important canal, is 76 miles in length and also irrigates about 250,000 acres. Climate The dry subtropical climate of central and eastern Azerbaijan is characterized by a mild winter and a long (four to five months) and very hot summer, with temperatures averaging about 81 °F (27 °C) and maximum temperatures reaching 109 °F (43 °C). Southeastern Azerbaijan is characterized by a humid subtropical climate with the highest precipitation in the country, some 47 to 55 inches (1,200 to 1,400 millimetres) a year, most of it falling in the cold months. A dry continental climate, with a cold winter and a dry, hot summer, prevails in Naxçıvan at altitudes of 2,300 to 3,300 feet. Moderately warm, dry, or humid types of climate are to be found in other parts of Azerbaijan. The mountain forest zone has a moderately cold climate, while an upland tundra climate characterizes elevations of 10,000 feet and above. Frosts and heavy snowfalls make the passes at such altitudes inaccessible for three or four months of the year. Plant and animal life Natural vegetation zones vary according to altitude. Steppe and semidesert conditions prevail in the lowlands and the foothills of the mountain regions. The slopes of the mountains are covered with beech, oak, and pine forests. Higher up there is a zone of alpine meadows. The Länkäran region of southern Azerbaijan has evergreen vegetation and thick beech and oak forests. In the lowlands the animal life includes gazelles, jackals, and hyenas as well as reptile and rodent species. The mountain regions are inhabited by Caucasian deer, roe deer, wild boar, brown bear, lynx, European bison (wisent), chamois, and leopard, though the latter is rare. Mild winters draw many birds to the Caspian coast, and nature reserves provide a resting home for flamingos, swans, pelicans, herons, egrets, sandpipers, and partridges. More … Score: https://www.britannica.com/place/Azerbaijan

2023/05/28

Ethiopia by HandZaround

'Ehtiopia' is a personal project of travellers HandZaround.com funded in majority by them and created in their free time. 'Green highlands, barren deserts, impassable lowlands, sparkling waterfalls, glistening lakes, bustling towns. We can’t describe Ethiopia with one word, unless we reach for ‘diversity’.

2023/05/27

Azerbaijan promo video 2018

Travel to Azerbaijan. You may contact me with any queries if you come :)

2023/05/27

Welcome to Jordan Tourism Board

The Official Tourism Website. Kingdom of time. Discover experiences. Plan your trip. Explore attractions. Highlights: A Large Insurance Company, A Technical Support Team, We Offer Various Insurance Solutions.

2023/05/27

Argentina.gob.ar: Inicio

Portal oficial del Estado argentino. Conocé cómo hacer trámites en organismos públicos, tramitalos en línea y recibí servicios digitales y beneficios.

2023/05/27

Festival de Cinema de Língua Portuguesa

Temos o prazer de convidá-los para o II Festival de Cinema de Língua Portuguesa MARÉ, que acontecerá nos dias de 26 e 27 de maio, em Varsóvia (no Kino Muranów) e nos dias 26 a 28 de maio, em Wrocław (no Kino Nowe Horizonty).Para mais informações, acesse às programações:

2023/05/26

Promoting actions, projects and cooperation programmes of the Republic of Trinidad and Tobago

On Friday 12 May 2023, Senator the Honourable Dr. Amery Browne, Minister of Foreign and CARICOM Affairs of the Republic of Trinidad and Tobago addressed the Ninth ACS Summit in Antigua, Guatemala. The Summit was held under the theme “Innovating Integration Through the Sustainable Development of the Greater Caribbean” and sought to reinvigorate the commitment of ACS Member States in promoting actions, projects and cooperation programmes that contribute to the sustainable development of the peoples and nations of the Greater Caribbean.

2023/05/26

KU Leuven, największy i najstarszy uniwersytet w Belgii

Dla KU Leuven, największego i najstarszego uniwersytetu w Belgii, absolwenci są nieocenioną częścią "kapitału społecznego" tego miejsca. Aby utrzymać z nimi kontakt, umożliwić nawiązywanie relacji i śledzenie ich osiągnięć, 19 maja w Warszawie utworzono KU Leuven Alumni Chapter Poland

2023/05/26