GUINEA - Guinea - The Republic of Guinea Guinea Country

Guinea officially the Republic of Guinea is a west-coastal country in West Africa. Formerly known as French Guinea, the modern country is sometimes referred to as Guinea-Conakry to distinguish it from other countries with "Guinea" in the name and the eponymous region, such as Guinea-Bissau and Equatorial Guinea. Guinea has a population of 12.4 million and an area of 245,857 square kilometers (94,926 sq mi).

2023/10/01

Proclamation of the People's Republic of China

China, Chinese (Pinyin) Zhonghua or (Wade-Giles romanization) Chung-hua, also spelled (Pinyin) Zhongguo or (Wade-Giles romanization) Chung-kuo, officially People’s Republic of China or Chinese (Pinyin) Zhonghua Renmin Gongheguo or (Wade-Giles romanization) Chung-hua Jen-min Kung-ho-kuo, country of East Asia. It is the largest of all Asian countries and has the largest population of any country in the world. Occupying nearly the entire East Asian landmass, it covers approximately one-fourteenth of the land area of Earth. Among the major countries of the world, China is surpassed in area by only Russia and Canada, and it is almost as large as the whole of Europe. China has 33 administrative units directly under the central government; these consist of 22 provinces, 5 autonomous regions, 4 municipalities (Chongqing, Beijing, Shanghai, and Tianjin), and 2 special administrative regions (Hong Kong and Macau). The island province of Taiwan, which has been under separate administration since 1949, is discussed in the article Taiwan. Beijing (Peking), the capital of the People’s Republic, is also the cultural, economic, and communications centre of the country. Shanghai is the main industrial city; Hong Kong is the leading commercial centre and port. Within China’s boundaries exists a highly diverse and complex country. Its topography encompasses the highest and one of the lowest places on Earth, and its relief varies from nearly impenetrable mountainous terrain to vast coastal lowlands. Its climate ranges from extremely dry, desertlike conditions in the northwest to tropical monsoon in the southeast, and China has the greatest contrast in temperature between its northern and southern borders of any country in the world. The diversity of both China’s relief and its climate has resulted in one of the world’s widest arrays of ecological niches, and these niches have been filled by a vast number of plant and animal species. Indeed, practically all types of Northern Hemisphere plants, except those of the polar tundra, are found in China, and, despite the continuous inroads of humans over the millennia, China still is home to some of the world’s most exotic animals. Probably the single most identifiable characteristic of China to the people of the rest of the world is the size of its population. Some one-fifth of humanity is of Chinese nationality. The great majority of the population is Chinese (Han), and thus China is often characterized as an ethnically homogeneous country, but few countries have as wide a variety of indigenous peoples as does China. Even among the Han there are cultural and linguistic differences between regions; for example, the only point of linguistic commonality between two individuals from different parts of China may be the written Chinese language. Because China’s population is so enormous, the population density of the country is also often thought to be uniformly high, but vast areas of China are either uninhabited or sparsely populated. With more than 4,000 years of recorded history, China is one of the few existing countries that also flourished economically and culturally in the earliest stages of world civilization. Indeed, despite the political and social upheavals that frequently have ravaged the country, China is unique among nations in its longevity and resilience as a discrete politico-cultural unit. Much of China’s cultural development has been accomplished with relatively little outside influence, the introduction of Buddhism from India constituting a major exception. Even when the country was penetrated by such “barbarian” peoples as the Manchu, these groups soon became largely absorbed into the fabric of Han Chinese culture. This relative isolation from the outside world made possible over the centuries the flowering and refinement of the Chinese culture, but it also left China ill prepared to cope with that world when, from the mid-19th century, it was confronted by technologically superior foreign nations. There followed a century of decline and decrepitude, as China found itself relatively helpless in the face of a foreign onslaught. The trauma of this external challenge became the catalyst for a revolution that began in the early 20th century against the old regime and culminated in the establishment of a communist government in 1949. This event reshaped global political geography, and China has since come to rank among the most influential countries in the world. Central to China’s long-enduring identity as a unitary country is the province, or sheng (“secretariat”). The provinces are traceable in their current form to the Tang dynasty (618–907 ce). Over the centuries, provinces gained in importance as centres of political and economic authority and increasingly became the focus of regional identification and loyalty. Provincial power reached its peak in the first two decades of the 20th century, but, since the establishment of the People’s Republic, that power has been curtailed by a strong central leadership in Beijing. Nonetheless, while the Chinese state has remained unitary in form, the vast size and population of China’s provinces—which are comparable to large and midsize nations—dictate their continuing importance as a level of subnational administration. Land China stretches for about 3,250 miles (5,250 km) from east to west and 3,400 miles (5,500 km) from north to south. Its land frontier is about 12,400 miles (20,000 km) in length, and its coastline extends for some 8,700 miles (14,000 km). The country is bounded by Mongolia to the north; Russia and North Korea to the northeast; the Yellow Sea and the East China Sea to the east; the South China Sea to the southeast; Vietnam, Laos, Myanmar (Burma), India, Bhutan, and Nepal to the south; Pakistan to the southwest; and Afghanistan, Tajikistan, Kyrgyzstan, and Kazakhstan to the west. In addition to the 14 countries that border directly on it, China also faces South Korea and Japan, across the Yellow Sea, and the Philippines, which lie beyond the South China Sea. Relief of China Broadly speaking, the relief of China is high in the west and low in the east; consequently, the direction of flow of the major rivers is generally eastward. The surface may be divided into three steps, or levels. The first level is represented by the Plateau of Tibet, which is located in both the Tibet Autonomous Region and the province of Qinghai and which, with an average elevation of well over 13,000 feet (4,000 metres) above sea level, is the loftiest highland area in the world. The western part of this region, the Qiangtang, has an average height of 16,500 feet (5,000 metres) and is known as the “roof of the world.” The second step lies to the north of the Kunlun and Qilian mountains and (farther south) to the east of the Qionglai and Daliang ranges. There the mountains descend sharply to heights of between 6,000 and 3,000 feet (1,800 and 900 metres), after which basins intermingle with plateaus. This step includes the Mongolian Plateau, the Tarim Basin, the Loess Plateau (loess is a yellow-gray dust deposited by the wind), the Sichuan Basin, and the Yunnan-Guizhou (Yungui) Plateau. The third step extends from the east of the Dalou, Taihang, and Wu mountain ranges and from the eastern perimeter of the Yunnan-Guizhou Plateau to the China Sea. Almost all of this area is made up of hills and plains lying below 1,500 feet (450 metres). The most remarkable feature of China’s relief is the vast extent of its mountain chains; the mountains, indeed, have exerted a tremendous influence on the country’s political, economic, and cultural development. By rough estimate, about one-third of the total area of China consists of mountains. China has the world’s tallest mountain and the world’s highest and largest plateau, in addition to possessing extensive coastal plains. The five major landforms—mountain, plateau, hill, plain, and basin—are all well represented. China’s complex natural environment and rich natural resources are closely connected with the varied nature of its relief. The topography of China is marked by many splendours. Mount Everest (Qomolangma Feng), situated on the border between China and Nepal, is the highest peak in the world, at an elevation of 29,035 feet (8,850 metres; see Researcher’s Note: Height of Mount Everest). By contrast, the lowest part of the Turfan Depression in the Uygur Autonomous Region of Xinjiang—Lake Ayding—is 508 feet (155 metres) below sea level. The coast of China contrasts greatly between South and North. To the south of the bay of Hangzhou, the coast is rocky and indented with many harbours and offshore islands. To the north, except along the Shandong and Liaodong peninsulas, the coast is sandy and flat. China is prone to intense seismic activity throughout much of the country. The main source of this geologic instability is the result of the constant northward movement of the Indian tectonic plate beneath southern Asia, which has thrust up the towering mountains and high plateaus of the Chinese southwest. Throughout its history China has experienced hundreds of massive earthquakes that collectively have killed millions of people. Two in the 20th century alone—in eastern Gansu province (1920) and in the city of Tangshan, eastern Hebei province (1976)—caused some 250,000 deaths each, and a quake in east-central Sichuan province in 2008 killed tens of thousands and devastated a wide area. China’s physical relief has dictated its development in many respects. The civilization of Han Chinese originated in the southern part of the Loess Plateau, and from there it extended outward until it encountered the combined barriers of relief and climate. The long, protruding corridor, commonly known as the Gansu, or Hexi, Corridor, illustrates this fact. South of the corridor is the Plateau of Tibet, which was too high and too cold for the Chinese to gain a foothold. North of the corridor is the Gobi Desert, which also formed a barrier. Consequently, Chinese civilization was forced to spread along the corridor, where melting snow and ice in the Qilian Mountains provided water for oasis farming. The westward extremities of the corridor became the meeting place of the ancient East and West. Thus, for a long time the ancient political centre of China was located along the lower reaches of the Huang He (Yellow River). Because of topographical barriers, however, it was difficult for the central government to gain complete control over the entire country, except when an unusually strong dynasty was in power. In many instances the Sichuan Basin—an isolated region in southwestern China, about twice the size of Scotland, that is well protected by high mountains and is self-sufficient in agricultural products—became an independent kingdom. A comparable situation often arose in the Tarim Basin in the northwest. Linked to the rest of China only by the Gansu Corridor, this basin is even remoter than the Sichuan, and, when the central government was unable to exert its influence, oasis states were established; only the three strong dynasties—the Han (206 bce–220 ce), the Tang (618–907ce), and the Qing, or Manchu (1644–1911/12)—were capable of controlling the region. Apart from the three elevation zones already mentioned, it is possible—on the basis of geologic structure, climatic conditions, and differences in geomorphologic development—to divide China into three major topographic regions: the eastern, northwestern, and southwestern zones. The eastern zone is shaped by the rivers, which have eroded landforms in some parts and have deposited alluvial plains in others; its climate is monsoonal (characterized by seasonal rain-bearing winds). The northwestern region is arid and eroded by the wind; it forms an inland drainage basin. The southwest is a cold, lofty, and mountainous region containing intermontane plateaus and inland lakes. The three basic regions may be further subdivided into second-order geographic divisions. The eastern region contains 10 of these, the southwest contains two, and the northwest contains three. Below is a brief description of each division. more … Score: https://www.britannica.com/place/China

2023/10/01

Independence Day of the Federal Republic of Nigeria

Nigeria, country located on the western coast of Africa. Nigeria has a diverse geography, with climates ranging from arid to humid equatorial. However, Nigeria’s most diverse feature is its people. Hundreds of languages are spoken in the country, including Yoruba, Igbo, Fula, Hausa, Edo, Ibibio, Tiv, and English. The country has abundant natural resources, notably large deposits of petroleum and natural gas. The national capital is Abuja, in the Federal Capital Territory, which was created by decree in 1976. Lagos, the former capital, retains its standing as the country’s leading commercial and industrial city. Modern Nigeria dates from 1914, when the British Protectorates of Northern and Southern Nigeria were joined. The country became independent on October 1, 1960, and in 1963 adopted a republican constitution but elected to stay a member of the Commonwealth. Land Nigeria is bordered to the north by Niger, to the east by Chad and Cameroon, to the south by the Gulf of Guinea of the Atlantic Ocean, and to the west by Benin. Nigeria is not only large in area—larger than the U.S. state of Texas—but also Africa’s most populous country. Relief In general, the topography of Nigeria consists of plains in the north and south interrupted by plateaus and hills in the centre of the country. The Sokoto Plains lie in the northwestern corner of the country, while the Borno Plains in the northeastern corner extend as far as the Lake Chad basin. The Lake Chad basin and the coastal areas, including the Niger River delta and the western parts of the Sokoto region in the far northwest, are underlain by soft, geologically young sedimentary rocks. Gently undulating plains, which become waterlogged during the rainy season, are found in these areas. The characteristic landforms of the plateaus are high plains with broad, shallow valleys dotted with numerous hills or isolated mountains, called inselbergs; the underlying rocks are crystalline, although sandstones appear in river areas. The Jos Plateau rises almost in the centre of the country; it consists of extensive lava surfaces dotted with numerous extinct volcanoes. Other eroded surfaces, such as the Udi-Nsukka escarpment (see Udi-Nsukka Plateau), rise abruptly above the plains at elevations of at least 1,000 feet (300 metres). The most mountainous area is along the southeastern border with Cameroon, where the Cameroon Highlands rise to the highest points in the country, Chappal Waddi (7,936 feet [2,419 metres]) in the Gotel Mountains and Mount Dimlang (6,699 feet [2,042 metres]) in the Shebshi Mountains. Drainage The major drainage areas in Nigeria are the Niger-Benue basin, the Lake Chad basin, and the Gulf of Guinea basin. The Niger River, for which the country is named, and the Benue, its largest tributary, are the principal rivers. The Niger has many rapids and waterfalls, but the Benue is not interrupted by either and is navigable throughout its length, except during the dry season. Rivers draining the area north of the Niger-Benue trough include the Sokoto, the Kaduna, the Gongola, and the rivers draining into Lake Chad. The coastal areas are drained by short rivers that flow into the Gulf of Guinea. River basin development projects have created many large man-made lakes, including Lake Kainji on the Niger and Lake Bakolori on the Rima River. The Niger delta is a vast low-lying region through which the waters of the Niger River drain into the Gulf of Guinea. Characteristic landforms in this region include oxbow lakes, river meander belts (see meander), and prominent levees. Large freshwater swamps give way to brackish mangrove thickets near the seacoast. Soils Soils in Nigeria, and in Africa generally, are usually of a poorer quality than those in other regions of the world. However, over the centuries Nigerians have utilized agricultural techniques such as slash and burn, intercropping, and the use of shallow planting implements to cope with the shortcomings of the soil. In the precolonial period the country normally produced enough agricultural commodities to feed its population, and it even maintained a surplus for export. Nigeria’s major soil zones conform to geographic location. Loose sandy soils consisting of wind-borne deposits and riverine sands are found in the northern regions, although, in areas where there is a marked dry season, a dense surface layer of laterite develops, making these soils difficult to cultivate. The soils in the northern states of Kano and Sokoto, however, are not subject to leaching and are therefore easily farmed. South of Kano the mixed soils contain locally derived granite and loess (wind-borne deposits). The middle two-thirds of the country, the savanna regions, contain reddish, laterite soils; they are somewhat less fertile than those of the north because they are not subject to as much seasonal drying, nor do they receive the greater rainfall that occurs in the more southerly regions. The forest soils represent the third zone. There the vegetation provides humus and protects it from erosion by heavy rainfall. Although these soils can readily be leached and lose their fertility, they are the most productive agriculturally. Hydromorphic and organic soils, confined largely to areas underlain by sedimentary rocks along the coast and river floodplains, are the youngest soil types. Climate of Nigeria Nigeria has a tropical climate with variable rainy and dry seasons, depending on location. It is hot and wet most of the year in the southeast but dry in the southwest and farther inland. A savanna climate, with marked wet and dry seasons, prevails in the north and west, while a steppe climate with little precipitation is found in the far north. In general, the length of the rainy season decreases from south to north. In the south the rainy season lasts from March to November, whereas in the far north it lasts only from mid-May to September. A marked interruption in the rains occurs during August in the south, resulting in a short dry season often referred to as the “August break.” Precipitation is heavier in the south, especially in the southeast, which receives more than 120 inches (3,000 mm) of rain a year, compared with about 70 inches (1,800 mm) in the southwest. Rainfall decreases progressively away from the coast; the far north receives no more than 20 inches (500 mm) a year. Temperature and humidity remain relatively constant throughout the year in the south, while the seasons vary considerably in the north; during the northern dry season the daily temperature range becomes great as well. On the coast the mean monthly maximum temperatures are steady throughout the year, remaining about 90 °F (32 °C) at Lagos and about 91 °F (33 °C) at Port Harcourt; the mean monthly minimum temperatures are approximately 72 °F (22 °C) for Lagos and 68 °F (20 °C) for Port Harcourt. In general, mean maximum temperatures are higher in the north, while mean minimum temperatures are lower. In the northeastern city of Maiduguri, for example, the mean monthly maximum temperature may exceed 100 °F (38 °C) during the hot months of April and May, while in the same season frosts may occur at night. The humidity generally is high in the north, but it falls during the harmattan (the hot, dry northeast trade wind), which blows for more than three months in the north but rarely for more than two weeks along the coast. Plant and animal life The main vegetation patterns run in broad east-west belts, parallel to the Equator. Mangrove and freshwater swamps occur along the coast and in the Niger delta. A short way inland, the swamps give way to dense tropical rainforests. Economically valuable, the oil palm grows wild and is usually preserved when forest is cleared for cultivation. In the more densely populated parts of the southeast, the original forest vegetation has been replaced by open palm bush. In the southwest large areas of forest have been replaced by cacao and rubber plantations. Tropical grassland occupies the area north of the forest belt and is studded with baobab, tamarind, and locust bean trees. The savanna becomes more open in the far north and is characterized by scattered stunted trees and short grasses. Semidesert conditions exist in the Lake Chad region, where various species of acacia and the doum species of palm are common. Gallery forests (narrow forest zones along rivers) are also characteristic of the open savanna in the north. In densely populated areas of the savanna, such as those around the towns of Sokoto, Kano, and Katsina, the vegetation has been removed by continuous cropping, overgrazing, and bush burning. In the far northern areas the nearly total disappearance of plant life has facilitated a gradual southward advance of the Sahara. Camels, antelopes, hyenas, lions, baboons, and giraffes once inhabited the entire savanna region, and red river hogs, forest elephants, and chimpanzees lived in the rainforest belt. Animals found in both forest and savanna included leopards, golden cats, monkeys, gorillas, and wild pigs. Today these animals can be found only in such protected places as the Yankari National Park in Bauchi state, Gashaka Gumti National Park in Taraba state, Kainji Lake National Park in Kwara state (see Kainji Lake), and Cross River National Park in Cross River state. Rodents such as squirrels, porcupines, and cane rats constitute the largest family of mammals. The northern savanna abounds in guinea fowl. Other common birds include quail, vultures, kites, bustards, and gray parrots. The rivers contain crocodiles, hippopotamuses, and a great variety of fishes. More … Score: https://www.britannica.com/place/Nigeria

2023/10/01

Independence day of the Republic of Cyprus

Cyprus, Greek Kípros, Turkish Kıbrıs, an island in the eastern Mediterranean Sea renowned since ancient times for its mineral wealth, superb wines and produce, and natural beauty. A “golden-green leaf thrown into the Sea” and a land of “wild weather and volcanoes,” in the words of the Greek Cypriot poet Leonidas Malenis, Cyprus comprises tall mountains, fertile valleys, and wide beaches. Settled for more than 10 millennia, Cyprus stands at a cultural, linguistic, and historic crossroads between Europe and Asia. Its chief cities—the capital of Nicosia, Limassol, Famagusta, and Paphos—have absorbed the influences of generations of conquerors, pilgrims, and travelers and have an air that is both cosmopolitan and provincial. Today Cyprus is a popular tourist destination for visitors from Europe, favoured by honeymooners (as befits the legendary home of Aphrodite, the ancient Greek goddess of love), bird-watchers drawn by the island’s diversity of migratory species, and other vacationers.In 1960 Cyprus became independent of Britain (it had been a crown colony since 1925) as the Republic of Cyprus. The long-standing conflict between the Greek Cypriot majority and the Turkish Cypriot minority and an invasion of the island by Turkish troops in 1974 produced an actual—although internationally unrecognized—partition of the island and led to the establishment in 1975 of a de facto Turkish Cypriot state in the northern third of the country. The Turkish Cypriot state made a unilateral declaration of independence in 1983 and adopted the name Turkish Republic of Northern Cyprus. Its independence was recognized only by Turkey. Land Cyprus lies about 40 miles (65 km) south of Turkey, 60 miles (100 km) west of Syria, and 480 miles (770 km) southeast of mainland Greece. Its maximum length, from Cape Arnauti in the west to Cape Apostolos Andreas at the end of the northeastern peninsula, is 140 miles (225 km); the maximum north-south extent is 60 miles (100 km). It is the third largest Mediterranean island, after Sicily and Sardinia. Relief The rugged island of Cyprus resembles a saucepan, with the handle extending northeastward from the main part. The general pattern of its roughly 400-mile (640-km) coastline is indented and rocky, with long, sandy beaches. The Kyrenia Mountains—the western portion of which is also known as the Pentadaktylos for its five-fingered peak—extend for 100 miles (160 km) parallel to and just inland from the northern coast. It is the southernmost range of the great Alpine-Himalayan chain in the eastern Mediterranean; like much of that extensive mountain belt, it is formed largely of deformed masses of Mesozoic limestone. The Troodos Mountains in the south and southwest are of great interest to geologists, who have concluded that the range, made up of igneous rock, was formed from molten rock beneath the deep ocean (Tethys) that once separated the continents of Eurasia and Afro-Arabia. The range stretches eastward about 50 miles (80 km) from near the island’s west coast to the 2,260-foot (689-metre) Stavrovouni peak, about 12 miles (19 km) from the southeastern coast. The range’s summit, Mount Olympus (also called Mount Troodos), reaches an elevation of 6,401 feet (1,951 metres) and is the island’s highest point. Between the two ranges lies the Mesaoria Plain (its name means “Between the Mountains”), which is flat and low-lying and extends from Morphou Bay in the west to Famagusta Bay in the east. Roughly in the centre of the plain is Nicosia. The plain is the principal cereal-growing area in the island. Drainage and soils The major rivers in Cyprus originate in the Troodos Mountains. The Pedieos, which is the largest, flows eastward toward Famagusta Bay; the Serakhis flows northwestward and the Karyotis northward to Morphou Bay; and the Kouris flows southward to Episkopi Bay. The rivers are fed entirely from the runoff of winter precipitation; in summer they become dry courses. The island’s major soil types consist of imperfect, gravelly lithosols found in the Troodos and Kyrenia mountains and agriculturally productive vertisols located in the Mesaoria Plain and along the southeastern coast. Other, less-productive soils include solonchaks and solonetz soils. These latter are found only in isolated saline pockets throughout the island. Climate Cyprus has an intense Mediterranean climate, with a typically strongly marked seasonal rhythm. Hot, dry summers (June to September) and rainy winters (November to March) are separated by short autumn and spring seasons (October and April to May, respectively) of rapid change. Autumn and winter precipitation, on which agriculture and water supply depend, is variable. Average annual precipitation is about 20 inches (500 mm). The lowest average precipitation of 14 inches (350 mm) occurs at Nicosia, and the highest, 41 inches (1,050 mm), is on Mount Olympus. Summer temperatures in Nicosia range between an average daily maximum of 98 °F (37 °C) and an average daily minimum of 70 °F (21 °C); in winter the range is between 59 °F (15 °C) and 41 °F (5 °C). From December to March the Troodos range experiences several weeks of below-freezing night temperatures, and snowfall is considerable. Plant and animal life There is a narrow fertile plain along the northern coast, where the vegetation is largely evergreen and includes olive, carob, and citrus trees. The Troodos range has pine, dwarf oak, cypress, and cedar forest coverings. The southern and western slopes are extensively planted with vineyards. Between autumn and spring the Mesaoria Plain is green and colourful, with an abundance of wildflowers, flowering bushes, and shrubs; there are also patches of woodland in which eucalyptus and various types of acacia, cypress, and lowland pine are found. Orange plantations dot the island’s northwestern end in the area around Morphou. Fossil remains of elephants and hippopotamuses have been found in the Kyrenia area, and in ancient times there were large numbers of deer and boar. The only large wild animal now surviving is the agrino, a subspecies of wild sheep related to the mouflon of the western Mediterranean; it is under strict protection in a small forested area of the Troodos range. Small game is abundant but keenly hunted. Snakes were widespread in ancient times, giving the island the name Ophiussa, “the Abode of Snakes”; they are now relatively rare. Green and loggerhead turtles, which are protected by law, breed on the beaches along the coast. Cyprus lies on major migration routes for birds. In spring and autumn millions pass over the island, while many species winter there. Among the numerous resident species are francolin and chukar partridges. People of Cyprus - Ethnic groups and languages The people of Cyprus represent two main ethnic groups, Greek and Turkish. The Greek Cypriots, who constitute nearly four-fifths of the population, descended from a mixture of aboriginal inhabitants and immigrants from the Peloponnese who colonized Cyprus starting about 1200 bc and assimilated subsequent settlers up to the 16th century. Roughly one-fifth of the population are Turkish Cypriots, descendants of the soldiers of the Ottoman army that conquered the island in 1571 and of immigrants from Anatolia brought in by the sultan’s government. Since 1974 additional immigrants from Turkey have been brought in to work vacant land and increase the total labour force. The language of the majority is Greek and of the minority, Turkish. There are also a small number of Arabic-speaking Maronite Christians, as well as a small group who speak Armenian. These groups each total only a few thousand speakers, and they are mostly bilingual, with either Turkish or Greek their second language. English is widely spoken and understood. Illiteracy is extremely low, the result of an excellent educational system. More: Score: https://www.britannica.com/place/Cyprus  

2023/10/01

Travel to Tuvalu A land of Coral and Beauty

Tuvalu is a beautiful group of tiny atolls in the south pacific. The unique culture and isolation makes this place what it is. The people here are like the sun, they are warm, spread light, and and energize you with their light.

2023/09/30

On Location: Palau

Growing up on the beautiful tropical islands of Palau in the Pacific Ocean, Rondy is used to living between reef and rainforest. Rondy takes us on an adventure by boat through the rock islands, experiences world class diving and marine wildlife as well as relaxes in the natural spa called the milky way. On land he visit a local Arai village to teach us Palauan traditions and customs but above all shows us, why Palau is known as a pristine paradise.

2023/09/30

Xinjiang Tourism Promotional Video | China's largest province & One Belt One Road

China’s Xinjiang Uygur Autonomous Region, the capital city of Urumqi, is located in Northwest China and is one of China’s five ethnic minority autonomous regions. Covering an area of ​​1.66 million square kilometers, it is the provincial administrative region with the largest land area in China, accounting for 1/6 of China's total land area.

2023/09/30

Lagos Nigeria - fly Victoria Island & Eko Atlantic

Lagos Nigeria VICTORIA ISLAND, EKO ATLANTIC CITY, Eko hotel, eko roundabout... I hope you will enjoy this flight upon the biggest city of Africa. Around sunset, Lagos population is leaving Victoria Island to go back home. You will observe the great traffic jam in lagos, also called "LAGOS GO SLOW" and the beautifull light of the tours in the night.

2023/09/30

Cyprus welcomes the world!

2023/09/30