Tourism Australia: Travel to Australia - Australian Tourism ...

Looking for travel inspiration? Discover Australia's sparkling beaches, friendly wildlife and natural wonders. There's never been a better time to travel to

2025/01/28

Indian Republic Day

India, country that occupies the greater part of South Asia. Its capital is New Delhi, built in the 20th century just south of the historic hub of Old Delhi to serve as India’s administrative centre. Its government is a constitutional republic that represents a highly diverse population consisting of thousands of ethnic groups and likely hundreds of languages. With roughly one-sixth of the world’s total population, India is the second most populous country, after China. It is known from archaeological evidence that a highly sophisticated urbanized culture—the Indus civilization—dominated the northwestern part of the subcontinent from about 2600 to 2000 bce. From that period on, India functioned as a virtually self-contained political and cultural arena, which gave rise to a distinctive tradition that was associated primarily with Hinduism, the roots of which can largely be traced to the Indus civilization. Other religions, notably Buddhism and Jainism, originated in India—though their presence there is now quite small—and throughout the centuries residents of the subcontinent developed a rich intellectual life in such fields as mathematics, astronomy, architecture, literature, music, and the fine arts. Throughout its history, India was intermittently disturbed by incursions from beyond its northern mountain wall. Especially important was the coming of Islam, brought from the northwest by Arab, Turkish, Persian, and other raiders beginning early in the 8th century ce. Eventually, some of those raiders stayed; by the 13th century much of the subcontinent was under Muslim rule, and the number of Muslims steadily increased. Only after the arrival of the Portuguese navigator Vasco da Gama in 1498 and the subsequent establishment of European maritime supremacy in the region did India become exposed to major external influences arriving by sea, a process that culminated in the decline of the ruling Muslim elite and absorption of the subcontinent within the British Empire. Direct administration by the British, which began in 1858, effected a political and economic unification of the subcontinent. When British rule came to an end in 1947, the subcontinent was partitioned along religious lines into two separate countries—India, with a majority of Hindus, and Pakistan, with a majority of Muslims; the eastern portion of Pakistan later split off to form Bangladesh. Many British institutions stayed in place (such as the parliamentary system of government); English continued to be a widely used lingua franca; and India remained within the Commonwealth. Hindi became the official language (and a number of other local languages achieved official status), while a vibrant English-language intelligentsia thrived. India remains one of the most ethnically diverse countries in the world. Apart from its many religions and sects, India is home to innumerable castes and tribes, as well as to more than a dozen major and hundreds of minor linguistic groups from several language families unrelated to one another. Religious minorities, including Muslims, Christians, Sikhs, Buddhists, and Jains, still account for a significant proportion of the population; collectively, their numbers exceed the populations of all countries except China. Earnest attempts have been made to instill a spirit of nationhood in so varied a population, but tensions between neighbouring groups have remained and at times have resulted in outbreaks of violence. Yet social legislation has done much to alleviate the disabilities previously suffered by formerly “untouchable” castes, tribal populations, women, and other traditionally disadvantaged segments of society. At independence, India was blessed with several leaders of world stature, most notably Mohandas (Mahatma) Gandhi and Jawaharlal Nehru, who were able to galvanize the masses at home and bring prestige to India abroad. The country has played an increasing role in global affairs. Contemporary India’s increasing physical prosperity and cultural dynamism—despite continued domestic challenges and economic inequality—are seen in its well-developed infrastructure and a highly diversified industrial base, in its pool of scientific and engineering personnel (one of the largest in the world), in the pace of its agricultural expansion, and in its rich and vibrant cultural exports of music, literature, and cinema. Though the country’s population remains largely rural, India has three of the most populous and cosmopolitan cities in the world—Mumbai (Bombay), Kolkata (Calcutta), and Delhi. Three other Indian cities—Bengaluru (Bangalore), Chennai (Madras), and Hyderabad—are among the world’s fastest-growing high-technology centres, and most of the world’s major information technology and software companies now have offices in India. Land India’s frontier, which is roughly one-third coastline, abuts six countries. It is bounded to the northwest by Pakistan, to the north by Nepal, China, and Bhutan; and to the east by Myanmar (Burma). Bangladesh to the east is surrounded by India to the north, east, and west. The island country of Sri Lanka is situated some 40 miles (65 km) off the southeast coast of India across the Palk Strait and Gulf of Mannar. The land of India—together with Bangladesh and most of Pakistan—forms a well-defined subcontinent, set off from the rest of Asia by the imposing northern mountain rampart of the Himalayas and by adjoining mountain ranges to the west and east. In area, India ranks as the seventh largest country in the world. Much of India’s territory lies within a large peninsula, surrounded by the Arabian Sea to the west and the Bay of Bengal to the east; Cape Comorin, the southernmost point of the Indian mainland, marks the dividing line between those two bodies of water. India has two union territories composed entirely of islands: Lakshadweep, in the Arabian Sea, and the Andaman and Nicobar Islands, which lie between the Bay of Bengal and the Andaman Sea. Relief It is now generally accepted that India’s geographic position, continental outline, and basic geologic structure resulted from a process of plate tectonics—the shifting of enormous, rigid crustal plates over the Earth’s underlying layer of molten material. India’s landmass, which forms the northwestern portion of the Indian-Australian Plate, began to drift slowly northward toward the much larger Eurasian Plate several hundred million years ago (after the former broke away from the ancient southern-hemispheric supercontinent known as Gondwana, or Gondwanaland). When the two finally collided (approximately 50 million years ago), the northern edge of the Indian-Australian Plate was thrust under the Eurasian Plate at a low angle. The collision reduced the speed of the oncoming plate, but the underthrusting, or subduction, of the plate has continued into contemporary times. The effects of the collision and continued subduction are numerous and extremely complicated. An important consequence, however, was the slicing off of crustal rock from the top of the underthrusting plate. Those slices were thrown back onto the northern edge of the Indian landmass and came to form much of the Himalayan mountain system. The new mountains—together with vast amounts of sediment eroded from them—were so heavy that the Indian-Australian Plate just south of the range was forced downward, creating a zone of crustal subsidence. Continued rapid erosion of the Himalayas added to the sediment accumulation, which was subsequently carried by mountain streams to fill the subsidence zone and cause it to sink more. India’s present-day relief features have been superimposed on three basic structural units: the Himalayas in the north, the Deccan (peninsular plateau region) in the south, and the Indo-Gangetic Plain (lying over the subsidence zone) between the two. Further information on the geology of India is found in the article Asia. The Himalayas of India The Himalayas (from the Sanskrit words hima, “snow,” and alaya, “abode”), the loftiest mountain system in the world, form the northern limit of India. That great, geologically young mountain arc is about 1,550 miles (2,500 km) long, stretching from the peak of Nanga Parbat (26,660 feet [8,126 metres]) in the Pakistani-administered portion of the Kashmir region to the Namcha Barwa peak in the Tibet Autonomous Region of China. Between those extremes the mountains fall across India, southern Tibet, Nepal, and Bhutan. The width of the system varies between 125 and 250 miles (200 and 400 km). Within India the Himalayas are divided into three longitudinal belts, called the Outer, Lesser, and Great Himalayas. At each extremity there is a great bend in the system’s alignment, from which a number of lower mountain ranges and hills spread out. Those in the west lie wholly within Pakistan and Afghanistan, while those to the east straddle India’s border with Myanmar (Burma). North of the Himalayas are the Plateau of Tibet and various Trans-Himalayan ranges, only a small part of which, in the Ladakh union territory (in the Indian-administered portion of Kashmir), are within the territorial limits of India. Because of the continued subduction of the Indian peninsula against the Eurasian Plate, the Himalayas and the associated eastern ranges remain tectonically active. As a result, the mountains are still rising, and earthquakes—often accompanied by landslides—are common. Several since 1900 have been devastating, including one in 1934 in what is now Bihar state that killed more than 10,000 people. In 2001 another tremor (the Bhuj earthquake), farther from the mountains, in Gujarat state, was less powerful but caused extensive damage, taking the lives of more than 20,000 people and leaving more than 500,000 homeless. Still others—notably the 2005 quake in Pakistani-administered Kashmir and the 2015 temblor in Nepal—principally affected those regions but also caused widespread damage and hundreds of deaths in adjacent parts of India. The relatively high frequency and wide distribution of earthquakes likewise have generated controversies about the safety and advisability of several hydroelectric and irrigation projects. The Outer Himalayas (the Siwalik Range) The southernmost of the three mountain belts are the Outer Himalayas, also called the Siwalik (or Shiwalik) Range. Crests in the Siwaliks, averaging from 3,000 to 5,000 feet (900 to 1,500 metres) in elevation, seldom exceed 6,500 feet (2,000 metres). The range narrows as it moves east and is hardly discernible beyond the Duars, a plains region in West Bengal state. Interspersed in the Siwaliks are heavily cultivated flat valleys (duns) with a high population density. To the south of the range is the Indo-Gangetic Plain. Weakly indurated, largely deforested, and subject to heavy rain and intense erosion, the Siwaliks provide much of the sediment transported onto the plain. The Lesser Himalayas To the north of the Siwaliks and separated from them by a fault zone, the Lesser Himalayas (also called the Lower or Middle Himalayas) rise to heights ranging from 11,900 to 15,100 feet (3,600 to 4,600 metres). Their ancient name is Himachal (Sanskrit: hima, “snow,” and acal, “mountain”). The mountains are composed of both ancient crystalline and geologically young rocks, sometimes in a reversed stratigraphic sequence because of thrust faulting. The Lesser Himalayas are traversed by numerous deep gorges formed by swift-flowing streams (some of them older than the mountains themselves), which are fed by glaciers and snowfields to the north. The Great Himalayas The northernmost Great, or Higher, Himalayas (in ancient times, the Himadri), with crests generally above 16,000 feet (4,900 metres) in elevation, are composed of ancient crystalline rocks and old marine sedimentary formations. Between the Great and Lesser Himalayas are several fertile longitudinal vales; in India the largest is the Vale of Kashmir, an ancient lake basin with an area of about 1,700 square miles (4,400 square km). The Great Himalayas, ranging from 30 to 45 miles (50 to 75 km) wide, include some of the world’s highest peaks. The highest in the range, Mount Everest (at 29,035 feet [8,850 metres]; see Researcher’s Note: Height of Mount Everest), is on the China-Nepal border, but India also has many lofty peaks. Notable among those is Kanchenjunga (28,169 feet [8,586 metres]) on the border of Nepal and the state of Sikkim, which is the world’s third tallest peak and India’s highest point. Other high mountains in India include Nanda Devi (25,646 feet [7,817 metres]), Kamet (25,446 feet [7,755 metres]), and Trisul (23,359 feet [7,120]) in Uttarakhand. The Great Himalayas lie mostly above the line of perpetual snow and thus contain most of the Himalayan glaciers. More …. Source: https://www.britannica.com/place/India

2025/01/26

Australian Union Day

Australia, the smallest continent and one of the largest countries on Earth, lying between the Pacific and Indian oceans in the Southern Hemisphere. Australia’s capital is Canberra, located in the southeast between the larger and more important economic and cultural centres of Sydney and Melbourne. The Australian mainland extends from west to east for nearly 2,500 miles (4,000 km) and from Cape York Peninsula in the northeast to Wilsons Promontory in the southeast for nearly 2,000 miles (3,200 km). To the south, Australian jurisdiction extends a further 310 miles (500 km) to the southern extremity of the island of Tasmania, and in the north it extends to the southern shores of Papua New Guinea. Australia is separated from Indonesia to the northwest by the Timor and Arafura seas, from Papua New Guinea to the northeast by the Coral Sea and the Torres Strait, from the Coral Sea Islands Territory by the Great Barrier Reef, from New Zealand to the southeast by the Tasman Sea, and from Antarctica in the far south by the Indian Ocean. Australia has been called “the Oldest Continent,” “the Last of Lands,” and “the Last Frontier.” Those descriptions typify the world’s fascination with Australia, but they are somewhat unsatisfactory. In simple physical terms, the age of much of the continent is certainly impressive—most of the rocks providing the foundation of Australian landforms were formed during Precambrian and Paleozoic time (some 4.6 billion to 252 million years ago)—but the ages of the cores of all the continents are approximately the same. On the other hand, whereas the landscape history of extensive areas in Europe and North America has been profoundly influenced by events and processes that occurred since late in the last Ice Age—roughly the past 25,000 years—in Australia scientists use a more extensive timescale that takes into account the great antiquity of the continent’s landscape. Australia is the last of lands only in the sense that it was the last continent, apart from Antarctica, to be explored by Europeans. At least 60,000 years before European explorers sailed into the South Pacific, the first Aboriginal explorers had arrived from Asia, and by 20,000 years ago they had spread throughout the mainland and its chief island outlier, Tasmania. When Captain Arthur Phillip of the British Royal Navy landed with the First Fleet at Botany Bay in 1788, there may have been between 250,000 and 500,000 Aboriginals, though some estimates are much higher. Largely nomadic hunters and gatherers, the Aboriginals had already transformed the primeval landscape, principally by the use of fire, and, contrary to common European perceptions, they had established robust, semipermanent settlements in well-favoured localities. The American-style concept of a national “frontier” moving outward along a line of settlement is also inappropriate. There was, rather, a series of comparatively independent expansions from the margins of the various colonies, which were not joined in an independent federated union until 1901. Frontier metaphors were long employed to suggest the existence of yet another extension of Europe and especially of an outpost of Anglo-Celtic culture in the distant “antipodes.” The most striking characteristics of the vast country are its global isolation, its low relief, and the aridity of much of its surface. If, like the English novelist D.H. Lawrence, visitors from the Northern Hemisphere are at first overwhelmed by “the vast, uninhabited land and by the grey charred bush…so phantom-like, so ghostly, with its tall, pale trees and many dead trees, like corpses,” they should remember that to Australians the bush—that sparsely populated Inland or Outback beyond the Great Dividing Range of mountains running along the Pacific coast and separating it from the cities in the east—is familiar and evokes nostalgia. It still retains some of the mystical quality it had for the first explorers searching for inland seas and great rivers, and it remains a symbol of Australia’s strength and independence; the Outback poem by A.B. (“Banjo”) Paterson, “Waltzing Matilda,” is the unofficial national anthem of Australia known the world over. Australia’s isolation from other continents explains much of the singularity of its plant and animal life. Its unique flora and fauna include hundreds of kinds of eucalyptus trees and the only egg-laying mammals on Earth, the platypus and echidna. Other plants and animals associated with Australia are various acacias (Acacia pycnantha [golden wattle] is the national flower) and dingoes, kangaroos, koalas, and kookaburras. The Great Barrier Reef, off the east coast of Queensland, is the greatest mass of coral in the world and one of the world’s foremost tourist attractions. The country’s low relief results from the long and extensive erosive action of the forces of wind, rain, and the heat of the sun during the great periods of geologic time when the continental mass was elevated well above sea level. Isolation is also a pronounced characteristic of much of the social landscape beyond the large coastal cities. But an equally significant feature of modern Australian society is the representation of a broad spectrum of cultures drawn from many lands, a development stemming from immigration that is transforming the strong Anglo-Celtic orientation of Australian culture. Assimilation, of course, is seldom a quick and easy process, and minority rights, multiculturalism, and race-related issues have played a large part in contemporary Australian politics. In the late 1990s these issues sparked a conservative backlash. Australia has a federal form of government, with a national government for the Commonwealth of Australia and individual state governments (those of New South Wales, Victoria, Queensland, South Australia, Western Australia, and Tasmania). Each state has a constitution, and its government exercises a limited degree of sovereignty. There are also two internal territories: Northern Territory, established as a self-governing territory in 1978, and the Australian Capital Territory (including the city of Canberra), which attained self-governing status in 1988. The federal authorities govern the external territories of Norfolk Island, the Cocos (Keeling) Islands, Christmas Island, Ashmore and Cartier islands, the Coral Sea Islands, and Heard Island and McDonald Islands and claim the Australian Antarctic Territory, an area larger than Australia itself. Papua New Guinea, formerly an Australian external territory, gained its independence in 1975. Historically part of the British Empire and now a member of the Commonwealth, Australia is a relatively prosperous independent country. Australians are in many respects fortunate in that they do not share their continent—which is only a little smaller than the United States—with any other country. Extremely remote from their traditional allies and trading partners—it is some 12,000 miles (19,000 km) from Australia to Great Britain via the Indian Ocean and the Suez Canal and about 7,000 miles (11,000 km) across the Pacific Ocean to the west coast of the United States—Australians have become more interested in the proximity of huge potential markets in Asia and in the highly competitive industrialized economies of China, Japan, South Korea, and Taiwan. Australia, the continent and the country, may have been quite isolated at the beginning of the 20th century, but it entered the 21st century a culturally diverse land brimming with confidence, an attitude encouraged by the worldwide fascination with the land “Down Under” and demonstrated when Sydney hosted the 2000 Olympic Games. Geologic history The earliest known manifestations of the geologic record of the Australian continent are 4.4-billion-year-old detrital grains of zircon in metasedimentary rocks that were deposited from 3.7 to 3.3 billion years ago. Based on that and other findings, the Precambrian rocks in Australia have been determined to range in age from about 3.7 billion to 541 million years (i.e., to the end of Precambrian time). They are succeeded by rocks of the Paleozoic Era, which extended to about 252 million years ago; of the Mesozoic Era, which lasted until about 66 million years ago; and of the Cenozoic Era, the past 66 million years. For millions of years Australia was part of the supercontinent of Pangaea and subsequently its southern segment, Gondwanaland (or Gondwana). Its separate existence was finally assured by the severing of the last connection between Tasmania and Antarctica, but it has been drifting toward the Southeast Asian landmass. As a continent, Australia thus encompasses two extremes: on the one hand, it contains the oldest known earth material while, on the other, it has stood as a free continent only since about 35 million years ago and is in the process—in terms of geologic time—of merging with Asia, so that its life span as a continent will be of relatively short duration. (See also geochronology: Geologic history of the Earth.) General considerations - Tectonic framework The map of the structural features of Australia and the surrounding region shows the distribution of the main tectonic units. The primary distinction is between the plates of oceanic lithosphere, generated within the past 160 million years by seafloor spreading at the oceanic ridges, and the continental lithosphere, accumulated over the past 4 billion years. (The lithosphere is the outer rock shell of the Earth that consists of the crust and the uppermost portion of the underlying mantle; see plate tectonics.) The largest area of oldest rocks is the Western Shield, comprising the western half of the continent, which has been eroded to a low relief. The youngest rocks are found in the growing fold belt of the Banda arcs and in New Guinea at the boundary between the Indian-Australian plate and the Eurasian and Pacific plates. The modern fold belts are separated from Australia by a “moat” (the Timor Trough) and a wide shelf (the Timor and Arafura seas). The northern half of the Australian margin is completed by the North West Shelf and the Exmouth Plateau on the west and by the Great Barrier Reef and the Queensland Plateau on the east. Precambrian rocks occupy three tectonic environments. The first is in shields, such as the Yilgarn and Pilbara blocks of the Western Shield, enclosed by later orogenic (mountain) belts. The second is as the basement to a younger cover of Phanerozoic sediment (deposited during the past 541 million years); for example, all the sedimentary basins west of the Tasman Line are underlain by Precambrian basement. The third is as relicts in younger orogenic belts, as in the Georgetown Inlier of northern Queensland and in the western half of Tasmania. Rocks of Paleozoic age occur either in flat-lying sedimentary basins, such as the Canning Basin, or within belts, such as the east–west-trending Amadeus Transverse Zone and north-trending Tasman Fold Belt. Mesozoic and Cenozoic rocks occur in widely distributed (though poorly exposed) basins onshore (the Great Artesian Basin in the eastern centre). Offshore they occur on the western, southern, and eastern margins, including beneath Bass Strait, which separates Australia from Tasmania, and to the north in the submerged ground between the Banda arcs/New Guinea and the mainland. More … Source: https://www.britannica.com/place/Australia

2025/01/26

This is India in 4K | Incredible India | Soul and Fuel |

There is so much to experience in Incredible India that one life time is just not enough. No wonder we Indians believe in reincarnation so that we can visit India again and again to cherish the billion things India has to offer from the Great Himalayas to the beaches of Goa and the Colors of Rajasthan to the fragrance of spices in Gods own country Kerala.

2025/01/25

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

2025/01/25

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.

2025/01/06

Independence Day of the Republic of the Union of Myanmar

Myanmar, also called Burma, country, located in the western portion of mainland Southeast Asia. In 1989 the country’s official English name, which it had held since 1885, was changed from the Union of Burma to the Union of Myanmar; in the Burmese language the country has been known as Myanma (or, more precisely, Mranma Prañ) since the 13th century. The English name of the city that served as the country’s capital from 1948 to 2006, Rangoon, also was dropped in 1989 in favour of the common Burmese name, Yangon. In 2005 the government began to shift its administrative centre, first to the city of Pyinmana (some 200 miles [320 km] north of Yangon) and then to Nay Pyi Taw (Naypyidaw), a newly constructed city near Pyinmana. Nay Pyi Taw was proclaimed the capital of Myanmar in 2006. Land Stretching from latitude 10° N to about 28° 30′ N, Myanmar is the northernmost country of Southeast Asia; it is shaped like a kite with a long tail that runs south along the Malay Peninsula. The country is bordered by China to the north and northeast, Laos to the east, Thailand to the southeast, the Andaman Sea and Bay of Bengal to the south and southwest, Bangladesh to the west, and India to the northwest. Its total length from north to south is about 1,275 miles (2,050 km), and its width at the widest part, across the centre of the country at about the latitude of the city of Mandalay, is approximately 580 miles (930 km) from east to west. Relief Myanmar slopes from north to south, from an elevation of 19,296 feet (5,881 metres) at Mount Hkakabo (the country’s highest peak) in the extreme north to sea level at the Irrawaddy (Ayeyarwady) and Sittang (Sittoung) river deltas. The mountain ranges generally run from north to south. The country as a whole can be divided into five physiographic regions—the northern mountains, the western ranges, the eastern plateau, the central basin and lowlands, and the coastal plains. The northern mountains consist of a series of ranges that form a complex knot at Mount Hkakabo. In terms of plate tectonics, this knot marks the northeastern limit of the encroaching Indian-Australian Plate, which has been colliding with the southern edge of the Eurasian Plate for roughly the past 50 million years and thrusting up the mountain ranges of Myanmar and beyond. This region contains the sources of several of Asia’s great rivers, including the Irrawaddy, which rises and flows wholly within Myanmar, and the Salween (Thanlwin), which rises to the north in China. The upper courses of these rivers all flow through deep gorges within a short distance of each other, separated by steep, sheer peaks. The western ranges traverse the entire western side of Myanmar, from the northern mountains to the southern tip of the Rakhine (Arakan) Peninsula, where they run under the sea and reappear as the Indian territory of the Andaman and Nicobar Islands. Their average elevation is about 6,000 feet (1,800 metres), although some peaks rise to 10,000 feet (3,000 metres) or higher. The mountains consist of old crystalline rocks surrounded by hard, tightly folded sedimentary rocks on either side. From north to south, the Patkai Range, Naga Hills, and Chin Hills form the border between India and Myanmar. To the south of these are the Rakhine Mountains (Arakan Mountains), which lie entirely within Myanmar and separate the coastal strip from the central basin. The Shan Plateau to the east rises abruptly from the central basin, often in a single step of some 2,000 feet (600 metres). Occupying the eastern half of the country, it is deeply dissected, with an average elevation of about 3,000 feet (900 metres). The plateau was formed during the Mesozoic Era (about 250 to 65 million years ago) and thus is a much older feature than the western mountains, but the plateau also shows more-recent and intensive folding, with north-south longitudinal ranges rising steeply to elevations of 6,000 to 8,600 feet (1,800 to 2,600 metres) above the plateau surface. Northward, the plateau merges into the northern mountains, and southward it continues into the Dawna Range and the peninsular Tenasserim Mountains (Tanintharyi Mountains), each a series of parallel ranges with narrow valleys. The central basin and lowlands, lying between the Rakhine Mountains and the Shan Plateau, are structurally connected with the folding of the western ranges. The basin was deeply excavated by the predecessors of the Irrawaddy, Chindwin, and Sittang rivers; the valleys are now occupied by these rivers, which cover the ancient soft sandstones, shales, and clays with alluvial deposits. In the deltaic regions formed by the Irrawaddy and Sittang rivers, the landscape is absolutely flat, and the monotony is relieved only by a few blocks of erosion-resistant rocks that are never more than 60 feet (18 metres) high. The basin is divided into two unequal parts, the larger Irrawaddy valley and the smaller Sittang valley, by the Bago Mountains. In the centre of the basin and structurally connected with the Bago Mountains and their northern extension is a line of extinct volcanoes with small crater lakes and eroded cones, the largest being Popa Hill, at 4,981 feet (1,518 metres). The coastal areas consist of the narrow Rakhine and Tenasserim plains, which are backed by the high ranges of the Rakhine and Tenasserim mountains and are fringed with numerous islands of varying sizes. Drainage and soils Like the mountains, Myanmar’s main rivers run from north to south. About three-fifths of Myanmar’s surface is drained by the Irrawaddy and its tributaries. Flowing entirely through Myanmar, it is navigable for nearly 1,000 miles (1,600 km). At the apex of its delta, the Irrawaddy breaks up into a vast network of streams and empties into the Andaman Sea through multiple mouths. Its great tributary, the Chindwin, drains the western region. The Bassein River (Pathein River) drains the southern Rakhine Mountains, and the Yangon River (Rangoon River) drains the Bago Mountains; both enter the Irrawaddy at the delta. The Sittang flows into the Gulf of Martaban of the Andaman Sea, and, for a comparatively short river, it has a large valley and delta. The Shan Plateau is drained by the Salween River, which enters Myanmar from southern China and empties into the Gulf of Martaban southeast of the Sittang. It is deeply entrenched and crosses the plateau in a series of deep gorges. Many of its tributaries are more than 300 miles (480 km) long and join the Salween in cascades. The Rakhine coastal plains are drained by short, rapid streams, which, after forming broad deltas, flow into the Bay of Bengal. The Tenasserim plains also are drained by short and rapid rivers, which enter the Gulf of Martaban. Myanmar has two major lakes. Indawgyi Lake, in the northern hills, runs some 15 miles (24 km) from north to south and 8 miles (13 km) from east to west; it is one of the largest natural inland lakes of Southeast Asia. Somewhat smaller is Inle Lake, stretching about 14 miles (22 km) from north to south and 7 miles (11 km) from east to west, on the Shan Plateau. Inle Lake is fed by dozens of streams. The highland regions of Myanmar are covered with highly leached, iron-rich, dark red and reddish brown soils. When protected by forest cover, these soils absorb the region’s heavy rain, but they erode quickly once the forest has been cleared. The lowland regions are covered with alluvial soils—mainly silt and clay. Low in nutrients and organic matter, they are improved by fertilizers. In the dry belt of the central region are found red-brown soils rich in calcium and magnesium. In the same region, however, when the soil has a low clay content, it becomes saline under high evaporation and is recognizable by its yellow or brown colour. Climate of Myanmar Although Myanmar is located in the monsoon region of Asia, its climate is greatly modified by its geographic position and its relief. The cold air masses of Central Asia bring snow to the northern mountains for two months of the year, but this mountain wall prevents the cold air from moving farther south, so that Myanmar lies primarily under the influence of the monsoon winds. The north-south alignment of ranges and valleys creates a pattern of alternate zones of heavy and scanty precipitation during both the northeast and southwest monsoons. Most of the precipitation, however, comes from the southwest monsoon. The west coast is subject to occasional tropical cyclones. Myanmar has three seasons: the cool, relatively dry northeast monsoon (late October to mid-February), the hot, dry intermonsoonal season (mid-February to mid-May), and the rainy southwest monsoon (mid-May to late October). The coastal regions and the western and southeastern ranges receive more than 200 inches (5,000 mm) of precipitation annually, while the delta regions receive about 100 inches (2,500 mm). The central region is not only away from the sea but also on the drier, lee side—in the rain shadow—of the Rakhine Mountains. Precipitation gradually decreases northward until in the region’s dry zone it amounts to only 20 to 40 inches (500 to 1,000 mm) per year. The Shan Plateau, because of its elevation, usually receives between 75 and 80 inches (1,900 and 2,000 mm) annually. Elevation and distance from the sea affect temperature as well. Although Myanmar generally is a tropical country, temperatures are not uniformly high throughout the year. The daily temperature range is greater than that in nearly all other parts of Southeast Asia, but no locality has a continental type of climate (i.e., one characterized by large seasonal differences in average temperature). Mandalay, in the centre of the dry zone, has some of the greatest daily temperature ranges, which span about 22 °F (12 °C) annually. In broader perspective, however, average daily temperatures show little variation, ranging from 79 °F (26 °C) to 82 °F (28 °C) between Sittwe (Akyab) in the Rakhine region, Yangon near the coast, and Mandalay in the northern part of the central basin. At Lashio, on the Shan Plateau, the average daily temperature is somewhat cooler, around 71 °F (22 °C). More … Source: https://www.britannica.com/place/Myanmar  

2025/01/04

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 ...

2025/01/03

Travel to Morocco - Official website of tourism in Morocco ...

The largest oasis in the world is in Morocco Oases are part of the natural wealth of Morocco. With an area of 77,000 km2, the region of Tafilalet, in the south of the country, is home to the

2025/01/03