Australia The Ultimate Travel Guide | Best Places to Visit | Top Attractions

Australia is a wild and beautiful place, a land whose color palette of red outback sands and Technicolor reefs frames sophisticated cities and soulful Indigenous stories. Top Attractions: Sydney Opera House Sydney Harbor Bridge Great Ocean Road Melbourne

2024/01/25

Myanmar Welcomes You - Myanmar Travel Packages

Get your Tour infor & enjoy Myanmar. Express Service Available, Complimentary Consultation. Travel to Myanmar for Tourism & Business Traveling. Complete Solution for Travelers. Email Confirmation. 24/7 Customer Service. Support Available 24h.

2024/01/06

Malaysia Travel

Travel around to experience the remarkable treasures and the hidden gems in Malaysia. Each state offers a unique Malaysian experience for all. Terengganu ...

2024/01/03

The Official Travel Guide to Haiti · Visit Haiti

Haiti's official travel and tourist information web site. Everything about vacation in Haiti. Find inspiration and guides for your next trip to Haiti.

2024/01/03

Sudan Visit Online - All you need to visit Sudan

View Culture, View Experiences to Sudan, View Regions. Tourist Business, Trip Help. Travel..

2024/01/03

Slovakia.travel

Visit Slovakia.

2024/01/03

Cuba Travel | Tourism Portal

Cuba Travel has the best tourist guide for your trips to Cuba. Find tourist destinations, attractions, facts and all the right info for your Cuban vacation.

2024/01/03

Malaysia National Day

Malaysia, country of Southeast Asia, lying just north of the Equator, that is composed of two noncontiguous regions: Peninsular Malaysia (Semenanjung Malaysia), also called West Malaysia (Malaysia Barat), which is on the Malay Peninsula, and East Malaysia (Malaysia Timur), which is on the island of Borneo. The Malaysian capital, Kuala Lumpur, lies in the western part of the peninsula, about 25 miles (40 km) from the coast; the administrative centre, Putrajaya, is located about 16 miles (25 km) south of the capital. Malaysia, a member of the Commonwealth, represents the political marriage of territories that were formerly under British rule. When it was established on September 16, 1963, Malaysia comprised the territories of Malaya (now Peninsular Malaysia), the island of Singapore, and the colonies of Sarawak and Sabah in northern Borneo. In August 1965 Singapore seceded from the federation and became an independent republic. Land Peninsular Malaysia occupies most of the southern segment of the Malay Peninsula. To the north it is bordered by Thailand, with which it shares a land boundary of some 300 miles (480 km). To the south, at the tip of the peninsula, is the island republic of Singapore, with which Malaysia is connected by a causeway and also by a separate bridge. To the southwest, across the Strait of Malacca, is the island of Sumatra in Indonesia. East Malaysia consists of the country’s two largest states, Sarawak and Sabah, and is separated from Peninsular Malaysia by some 400 miles (640 km) of the South China Sea. These two states occupy roughly the northern fourth of the large island of Borneo and share a land boundary with the Indonesian portion (Kalimantan) of the island to the south. Surrounded by Sarawak is a small coastal enclave containing the sultanate of Brunei. Of the country’s total area, which includes about 265 square miles (690 square km) of inland water, Peninsular Malaysia constitutes about 40 percent and East Malaysia about 60 percent. Relief The long, narrow, and rugged Malay Peninsula extends to the south and southwest from Myanmar and Thailand. The Malaysian portion of it is about 500 miles (800 km) long and—at its broadest east-west axis—about 200 miles (320 km) wide. About half of Peninsular Malaysia is covered by granite and other igneous rocks, one-third is covered by stratified rocks older than the granite, and the remainder is covered by alluvium. At least half the land area lies more than 500 feet (150 metres) above sea level. Peninsular Malaysia is dominated by its mountainous core, which consists of a number of roughly parallel mountain ranges aligned north-south. The most prominent of these is the Main Range, which is about 300 miles (480 km) long and has peaks exceeding 7,000 feet (2,100 metres). Karst landscapes—limestone hills with characteristically steep whitish gray sides, stunted vegetation, caves created by the dissolving action of water, and subterranean passages—are distinctive landmarks in central and northern Peninsular Malaysia. Bordering the mountainous core are the coastal lowlands, 10 to 50 miles (15 to 80 km) wide along the west coast of the peninsula but narrower and discontinuous along the east coast. East Malaysia is an elongated strip of land approximately 700 miles (1,125 km) long with a maximum width of about 170 miles (275 km). The coastline of 1,400 miles (2,250 km) is paralleled inland by a 900-mile (l,450-km) boundary with Kalimantan. For most of its length, the relief consists of three topographic features. The first is the flat coastal plain. In Sarawak, where the coastline is regular, the plain averages 20 to 40 miles (30 to 60 km) in width, while in Sabah, where the coastline is rugged and deeply indented, it is only 10 to 20 miles (15 to 30 km) wide. Inland from the coastal plain is the second topographic feature, the hill-and-valley region. Elevations there generally are less than 1,000 feet (300 metres), but isolated groups of hills reach heights of 2,500 feet (750 metres) or more. The terrain in this region is usually irregular, with steep-sided hills and narrow valleys. The third topographic feature is the mountainous backbone that forms the divide between East Malaysia and Kalimantan. This region, which is higher and nearer to the coast in Sabah than in Sarawak, is composed of an eroded and ill-defined complex of plateaus, ravines, gorges, and mountain ranges. Most of the summits of the ranges are between 4,000 and 7,000 feet (1,200 and 2,100 metres). Mount Kinabalu towers above this mountain complex; at 13,455 feet (4,101 metres), it is the highest peak in Malaysia and in the Southeast Asian archipelago as a whole. Drainage Peninsular Malaysia is drained by an intricate system of rivers and streams. The longest river—the Pahang—is only 270 miles (434 km) long. Streams flow year-round because of the constant rains, but the volume of water transported fluctuates with the localized and torrential nature of the rainfall. Prolonged rains often cause floods, especially in areas where the natural regimes of the rivers have been disrupted by uncontrolled mining or agricultural activities. As in Peninsular Malaysia, the drainage pattern of East Malaysia is set by the interior highlands, which also form the watershed between Malaysia and Indonesia. The rivers, also perennial because of the year-round rainfall, form a dense network covering the entire region. The longest river in Sarawak, the Rajang, is about 350 miles (563 km) long and is navigable by shallow-draft boats for about 150 miles (240 km) from its mouth; its counterpart in Sabah, the Kinabatangan, is of comparable length but is navigable only for about 120 miles (190 km) from its mouth. The rivers provide a means of communication between the coast and the interior, and historically, most settlement has taken place along the rivers. Soils The soils of both portions of Malaysia have been exposed for a long period of time to intense tropical weathering, with the result that most of their plant nutrients have been leached out. Soils typically are strongly acidic and coarse-textured and have low amounts of organic matter. Any organic matter is rapidly oxidized when exposed to weathering, and the soils consequently become even poorer. Soil erosion is always a danger on sloping ground, where such preventive measures as building contour embankments or planting protective cover crops are required. Only a small proportion of the soils of Peninsular Malaysia is fertile, necessitating regular application of fertilizer to sustain crop yields. Generally, soil conditions in Sarawak and Sabah do not differ greatly from those on the peninsula. Of these three regions, only Sabah has appreciable areas of fertile soils. These are found in the southeastern coastal areas, where the parent substance from which the soil is formed is composed of chemically basic volcanic materials. More … Score: https://www.britannica.com/place/Malaysia

2024/01/01

Independence day of the Republic of Haiti

Haiti, country in the Caribbean Sea that includes the western third of the island of Hispaniola and such smaller islands as Gonâve, Tortue (Tortuga), Grande Caye, and Vache. The capital is Port-au-Prince. Haiti, whose population is almost entirely descended from African slaves, won independence from France in 1804, making it the second country in the Americas, after the United States, to free itself from colonial rule. Over the centuries, however, economic, political, and social difficulties as well as a number of natural disasters have beset Haiti with chronic poverty and other serious problems. Land Haiti is bordered to the east by the Dominican Republic, which covers the rest of Hispaniola, to the south and west by the Caribbean, and to the north by the Atlantic Ocean. Cuba lies some 50 miles (80 km) west of Haiti’s northern peninsula, across the Windward Passage, a strait connecting the Atlantic to the Caribbean. Jamaica is some 120 miles (190 km) west of the southern peninsula, across the Jamaica Channel, and Great Inagua Island (of The Bahamas) lies roughly 70 miles (110 km) to the north. Haiti claims sovereignty over Navassa (Navase) Island, an uninhabited U.S.-administered islet about 35 miles (55 km) to the west in the Jamaica Channel. Relief and drainage The generally rugged topography of central and western Hispaniola is reflected in Haiti’s name, which derives from the indigenous Arawak place-name Ayti (“Mountainous Land”); about two-thirds of the total land area is above 1,600 feet (490 metres) in elevation. Haiti’s irregular coastline forms a long, slender peninsula in the south and a shorter one in the north, separated by the triangular-shaped Gulf of Gonâve. Within the gulf lies Gonâve Island, which has an area of approximately 290 square miles (750 square km). Haiti’s shores are generally rocky, rimmed with cliffs, and indented by a number of excellent natural harbours. The surrounding seas are renowned for their coral reefs. Plains, which are quite limited in extent, are the most productive agricultural lands and the most densely populated areas. Rivers are numerous but short, and most are not navigable. The backbone of the island of Hispaniola consists of four major mountain ranges that extend from west to east. The most northerly range, known as the Cordillera Septentrional in the Dominican Republic, occurs in Haiti only on Tortue Island, off the northern coast. Tortue Island has an area of about 70 square miles (180 square km). In the 17th century it was a stronghold of privateers and pirates from various countries. The second major range, Haiti’s Massif du Nord (“Northern Massif”), is a series of parallel chains known in the Dominican Republic as the Cordillera Central. It has an average elevation of some 4,000 feet (1,200 metres). The Citadel (Citadelle Laferrière), a fortress built by Haitian ruler Henry Christophe in the early 19th century, stands atop one of the peaks overlooking the city of Cap-Haïtien and the narrow coastal plain. An interior basin, known as the Central Plateau in Haiti and the San Juan Valley in the Dominican Republic, occupies about 150 square miles (390 square km) in the centre of the country. The plateau has an average elevation of about 1,000 feet (300 metres), and access to it is difficult through winding roads. It is bounded by two minor mountain ranges on the west and south—respectively, the Cahos Mountains and the Noires Mountains. The Artibonite River—the island’s longest, approximately 175 miles (280 km) long—rises in the western Dominican Republic in the Cordillera Central and follows a southwestward course along the border with Haiti. Its tributaries flow eastward and southward through Haiti’s Central Plateau to a point near the Dominican border, where they join the river proper as it turns westward. The Artibonite then skirts the Noires Mountains as it flows to the Gulf of Gonâve. In eastern Haiti the river was impounded as Lake Péligre in the mid-20th century; a hydroelectric complex began operating at Péligre in 1971, but its power output has been unreliable during the dry season. Just upstream from the Artibonite’s delta in the Gulf of Gonâve, some of its waters are used to irrigate the triangular Artibonite Plain. The third major range, known as the Matheux Mountains (Chaîne des Matheux) in west-central Haiti and the Trou d’Eau Mountains (Chaîne du Trou d’Eau) farther east, corresponds to the Sierra de Neiba in the Dominican Republic. The range forms the northern boundary to the narrow Cul-de-Sac Plain, which is immediately adjacent to Port-au-Prince and includes the brackish Lake Saumâtre on the Dominican border. South of the Cul-de-Sac Plain is the fourth major range, called the Massif de la Selle in Haiti and the Sierra de Baoruco in the Dominican Republic. It rises to 8,773 feet (2,674 metres) at Mount Selle, the highest point in the country. The range’s western extension on the southern peninsula is called the Massif de la Hotte (Massif du Sud), which rises to 7,700 feet (2,345 metres) at Macaya Peak. The Cayes Plain lies on the coast to the southeast of the peak. Haiti’s mountains are mainly limestone, although some volcanic formations can be found, particularly in the Massif du Nord. Karstic features, such as limestone caves, grottoes, and subterranean rivers, are present in many parts of the country. A long fault line crosses the southern peninsula and passes just south of Port-au-Prince. Haiti is subject to periodic seismic activity; earthquakes destroyed Cap-Haïtien in 1842 and Port-au-Prince in 1751 and 1770. In January 2010 another catastrophic earthquake and its aftershocks resulted in severe damage to Port-au-Prince. Buildings collapsed throughout the capital and surrounding region, including many homes as well as large public structures such as the National Palace, the city’s cathedral, and hospitals. Estimates of the number of people killed ranged upward of 200,000, and several hundred thousand others were injured. More than a million people were made homeless. To the west of the capital, near the quake’s epicentre, the city of Léogâne was almost completely ruined. Soils The soils in the mountains are thin and lose fertility quickly when cultivated. The lower hills are covered with red clays and loams. The alluvial soils of the plains and valleys are fertile but overcultivated, owing to high population densities in those areas. Deforestation has caused much soil erosion, and as much as one-third of Haiti’s land may have eroded beyond recovery. Climate of Haiti Haiti has a warm, humid tropical climate characterized by diurnal temperature variations that are greater than the annual variations; temperatures are modified by elevation. Average temperatures range from the high 70s F (about 25 °C) in January and February to the mid-80s F (about 30 °C) in July and August. The village of Kenscoff, at some 4,700 feet (1,430 metres), has an average temperature of about 60 °F (16 °C), whereas Port-au-Prince, at sea level, has an average of 79 °F (26 °C). In winter, frost can occur at high elevations. Haiti is located on the leeward side of the island, which means that the influence of humid trade winds is not as great as in the Dominican Republic. The more humid districts are found on the northern and eastern slopes of the mountains. Some portions of the island receive less than 28 inches (700 mm) of rainfall per year. The northwestern peninsula and Gonâve Island are particularly dry. Some regions have two rainy seasons, lasting from April to June and from August to October, whereas other regions experience rainfall from May to November. Annual variations of precipitation can cause droughts, widespread crop failures, and famine. The southern peninsula, which is more vulnerable to hurricanes (tropical cyclones) than other parts of Haiti, suffered heavy damage from Hurricanes Allen (1980), Gilbert (1988), and Georges (1998). All parts of the country, however, can be hit by tropical storms and hurricanes. During August and September 2008 a series of severe storms that included Hurricanes Hanna and Ike caused widespread damage and the loss of some 800 lives. More … Source: https://www.britannica.com/place/Haiti  

2024/01/01