Beautiful Bangladesh

Bangladesh, a tourist attraction in south-central Asia with the world's largest beaches, historical monuments, resorts, picnic spots, forests and tribal ..

2025/03/28

Visit Greece

If you are looking for travel inspiration, visitgreece.gr has everything you need to know. Travel ideas, Events, guides, what to do, where to go in Greece.

2025/03/27

Bangladesh Independence Day

Bangladesh, country of South Asia, located in the delta of the Padma (Ganges [Ganga]) and Jamuna (Brahmaputra) rivers in the northeastern part of the Indian subcontinent. The riverine country of Bangladesh (“Land of the Bengals”) is one of the most densely populated countries in the world, and its people are predominantly Muslim. As the eastern portion of the historical region of Bengal, the area once formed, along with what is now the Indian state of West Bengal, the province of Bengal in British India. With the partition of India in 1947, it became the Pakistani province of East Bengal (later renamed East Pakistan), one of five provinces of Pakistan, separated from the other four by 1,100 miles (1,800 km) of Indian territory. In 1971 it became the independent country of Bangladesh, with its capital at Dhaka. Land Bangladesh is bordered by the Indian states of West Bengal to the west and north, Assam to the north, Meghalaya to the north and northeast, and Tripura and Mizoram to the east. To the southeast, it shares a boundary with Myanmar (Burma). The southern part of Bangladesh opens into the Bay of Bengal. Relief Stretching northward from the Bay of Bengal, Bangladesh constitutes roughly the eastern two-thirds of the deltaic plain of the Padma (Ganges [Ganga]) and Jamuna (Brahmaputra) rivers. Except for small higher areas of jungle-covered old alluvium (rising to about 100 feet [30 metres]) in the northwest and north-centre—in the Barind and the Madhupur Tract, respectively—the plain is a flat surface of recent alluvium, having a gentle slope and an elevation of generally less than 30 feet (9 metres) above sea level. In the northeast and southeast—in the Sylhet and Chittagong Hills areas, respectively—the alluvial plains give place to ridges, running mainly north-south, that form part of the mountains that separate Bangladesh from Myanmar and India. In its southern region, Bangladesh is fringed by the Sundarbans, a huge expanse of marshy deltaic forest. The Barind is a somewhat elevated triangular wedge of land that lies between the floodplains of the upper Padma and Jamuna rivers in northwestern Bangladesh. A depression called the Bhar Basin extends southeast from the Barind for about 100 miles (160 km) to the confluence of the Padma and Jamuna. This area is inundated during the summer monsoon season, in some places to a depth exceeding 10 feet (3 metres). The drainage of the western part of the basin is centred in the vast marshy area called the Chalan wetlands, also known as Chalan Lake. The floodplains of the Jamuna, which lie north of the Bhar Basin and east of the Barind, stretch from the border with Assam in the north to the confluence of the Padma and Jamuna in the south. The area is dominated by the Jamuna, which frequently overflows its banks in devastating floods. South of the Bhar Basin is the floodplain of the lower Padma. In north-central Bangladesh, east of the Jamuna floodplains, is the Madhupur Tract. It consists of an elevated plateau on which hillocks ranging in height from 30 to 60 feet (9 to 18 metres) give contour to cultivated valleys. The Madhupur Tract contains sal trees, whose hardwood is comparable in value and utility to teak. East of the Madhupur Tract, in northeastern Bangladesh, is a region called the Northeastern Lowland. It encompasses the southern and southwestern parts of the Sylhet area (including the valley plain of the Surma River) and the northern part of the Mymensingh area and has a large number of lakes. The Sylhet Hills in the far northeast of the region consist of a number of hillocks and hills ranging in elevation from about 100 feet (30 metres) to more than 1,100 feet (330 metres). In east-central Bangladesh the Brahmaputra River in its old course (the Old Brahmaputra River) built up the flood basin of the Meghna River, the region that includes the low and fertile Meghna-Sitalakhya Doab (the land area between those rivers). This area is enriched by the Titas distributary, and land areas are formed and changed by the deposition of silt and sand in the riverbeds of the Meghna River, especially between Bhairab Bazar and Daudkandi. Dhaka is located in this region. In southern Bangladesh the Central Delta Basins include the extensive lakes in the central part of the Bengal Delta, to the south of the upper Padma. The basin’s total area is about 1,200 square miles (3,100 square km). The belt of land in southwestern Bangladesh bordering the Bay of Bengal constitutes the Immature Delta. A lowland of some 3,000 square miles (7,800 square km), the belt contains, in addition to the vast mangrove forest known as the Sundarbans, the reclaimed and cultivated lands to the north of it. The area nearest the Bay of Bengal is crisscrossed by a network of streams that flow around roughly oblong islands. The Active Delta, located north of the Central Delta Basins and east of the Immature Delta, includes the Dhaleswari-Padma Doab and the estuarine islands of varying sizes that are found from the Pusur River in the southwest to the island of Sandwip near Chittagong in the southeast. Lying to the south of the Feni River in southeastern Bangladesh is the Chittagong region, which has many hills, hillocks, valleys, and forests and is quite different in aspect from other parts of the country. The coastal plain is partly sandy and partly composed of saline clay; it extends southward from the Feni River to the town of Cox’s Bazar and varies in width from 1 to 10 miles (1.6 to 16 km). The region has a number of offshore islands and one coral reef, St. Martin’s, off the coast of Myanmar. The hilly area known as the Chittagong Hill Tracts, in the far southeast, consists of low hills of soft rocks, mainly clay and shale. The north-south ranges are generally below 2,000 feet (600 metres) in elevation. More … Score: https://www.britannica.com/place/Bangladesh

2025/03/26

Independence Day Greek Republic

Greece, the southernmost of the countries of the Balkan Peninsula. Geography has greatly influenced the country’s development. Mountains historically restricted internal communications, but the sea opened up wider horizons. The total land area of Greece (one-fifth of which is made up of the Greek islands) is comparable in size to England or the U.S. state of Alabama. Greece has more than 2,000 islands, of which about 170 are inhabited; some of the easternmost Aegean islands lie just a few miles off the Turkish coast. The country’s capital is Athens, which expanded rapidly in the second half of the 20th century. Attikí (ancient Greek: Attica), the area around the capital, is now home to about one-third of the country’s entire population. A Greek legend has it that God distributed soil through a sieve and used the stones that remained to build Greece. The country’s barren landscape historically caused the people to migrate. The Greeks, like the Jews and the Armenians, traditionally have been a people of diaspora, and several million people of Greek descent live in various parts of the world. Xeniteia, or sojourning in foreign lands, with its strong overtones of nostalgia for the faraway homeland, has been a central element in the historical experience of the Greek people. Greece is a country that is at once European, Balkan, Mediterranean, and Near Eastern. It lies at the juncture of Europe, Asia, and Africa and is heir to the heritages of Classical Greece, the Byzantine Empire, and nearly four centuries of Ottoman Turkish rule. Get a Britannica Premium subscription and gain access to exclusive content. Subscribe Now Land Greece is bordered to the east by the Aegean Sea, to the south by the Mediterranean Sea, and to the west by the Ionian Sea. Only to the north and northeast does it have land borders (totaling some 735 miles [1,180 km]), with, from west to east, Albania, the Republic of North Macedonia (see Researcher’s Note: Macedonia: the provenance of the name), Bulgaria, and Turkey. The Greek landscape is conspicuous not only for its rugged beauty but also for its complexity and variety. Three elements dominate: the sea, the mountains, and the lowland. The Greek mainland is sharply indented; arms and inlets of the sea penetrate so deeply that only a small, wedge-shaped portion of the interior is more than 50 miles (80 km) from the coast. The rocky headlands and peninsulas extend outward to the sea where there are many island arcs and archipelagoes. The southernmost part of mainland Greece, the Pelopónnisos (ancient Greek: Peloponnese) peninsula, connects to the mainland only by the narrow isthmus at the head of the Gulf of Korinthiakós (Corinth). Greece’s mountainous terrain covers some four-fifths of the country, much of which is deeply dissected. A series of mainland mountain chains running northwest-southeast enclose narrow parallel valleys and numerous small basins that once held lakes. With riverine plains and thin, discontinuous strips of coastal plain, these interior valleys and basins constitute the lowland. Although it accounts for only about one-fifth of the country’s land area, the lowland has played an important role in the life of the country. Relief Three characteristics of geology and structure underlie these landscape elements. First, northeastern Greece is occupied by a stable block of ancient (Hercynian) hard rock. Second, younger and weaker rocks, the majority of which are of limestone origin, make up western and southern Greece. These were heavily folded during the Alp-building phase of the Paleogene and Neogene periods (about 66 to 2.6 million years ago), when Earth movements thrust the softer sediments east-northeast against the unyielding Hercynian block and produced a series of roughly parallel tectonic zones that gave rise to the mountain-and-valley relief. Third, both the Hercynian block and the Hellenidic (Alpine) ranges were subsequently raised and fractured by tectonic movements. These dislocations created the sunken basins of the Ionian and Aegean seas as well as the jagged edges so typical of Greece’s landscape. Earthquakes are frequent reminders that similar earth movements continue, particularly along the major fault lines. One result of the region’s geologic instability is the widespread presence of marble, which is limestone that has been altered by pressure and heat. Seismic disturbances are sometimes associated with volcanic explosions, especially those involving the island of Thíra (ancient Greek: Thera; also called Santoríni), which was virtually destroyed by a major eruption in the 2nd millennium bce. The vents of the Kaméni islands in the sea-filled explosion crater of Thíra remain active. The island of Mílos (Melos), which rises to 2,465 feet (751 metres) above sea level, is composed of young volcanic rocks. Relief and geology provide the basis for describing the Greek landscape in terms of six major regions: central, northeastern, eastern, southern, and western mainland Greece, along with the islands. More … Score: https://www.britannica.com/place/Greece

2025/03/25

Welcome to Pakistan

The Principal objective of the corporation is to promote and develop tourism in Pakistan.

2025/03/25

Beautiful Bangladesh - Land Of Stories

Bangladesh Tourism Board

2025/03/25

Visit Greece | A 365 Day Destination (Narrative) (English)

Bustling cities, small traditional villages, breathtaking nature, rich culture, imposing archaeological sites, mesmerising islands, savoury culinary treats and recipes form a fascinating destination. Enjoy Greece all year round, as each season has something special to offer. Uncover Greece's hidden treasures!

2025/03/24

Republic Day of Islamic Republic Of Pakistan

Pakistan, populous and multiethnic country of South Asia. Having a predominately Indo-Iranian speaking population, Pakistan has historically and culturally been associated with its neighbours Iran, Afghanistan, and India. Since Pakistan and India achieved independence in 1947, Pakistan has been distinguished from its larger southeastern neighbour by its overwhelmingly Muslim population (as opposed to the predominance of Hindus in India). Pakistan has struggled throughout its existence to attain political stability and sustained social development. Its capital is Islamabad, in the foothills of the Himalayas in the northern part of the country, and its largest city is Karachi, in the south on the coast of the Arabian Sea. Pakistan was brought into being at the time of the partition of British India, in response to the demands of Islamic nationalists: as articulated by the All India Muslim League under the leadership of Mohammed Ali Jinnah, India’s Muslims would receive just representation only in their own country. From independence until 1971, Pakistan (both de facto and in law) consisted of two regions—West Pakistan, in the Indus River basin in the northwestern portion of the Indian subcontinent, and East Pakistan, located more than 1,000 miles (1,600 km) to the east in the vast delta of the Ganges-Brahmaputra river system. In response to grave internal political problems that erupted in civil war in 1971, East Pakistan was proclaimed the independent country of Bangladesh. Pakistan encompasses a rich diversity of landscapes, starting in the northwest, from the soaring Pamirs and the Karakoram Range through a maze of mountain ranges, a complex of valleys, and inhospitable plateaus, down to the remarkably even surface of the fertile Indus River plain, which drains southward into the Arabian Sea. It contains a section of the ancient Silk Road and the Khyber Pass, the famous passageway that has brought outside influences into the otherwise isolated subcontinent. Lofty peaks such as K2 and Nanga Parbat, in the Pakistani-administered region of Kashmir, present a challenging lure to mountain climbers. Along the Indus River, the artery of the country, the ancient site of Mohenjo-daro marks one of the cradles of civilization. Yet, politically and culturally, Pakistan has struggled to define itself. Established as a parliamentary democracy that espoused secular ideas, the country has experienced repeated military coups, and religion—that is to say, adherence to the values of Sunni Islam—has increasingly become a standard by which political leaders are measured. In addition, northern Pakistan—particularly the Federally Administered Tribal Areas—has become a haven for members of neighbouring Afghanistan’s ousted Taliban regime and for members of numerous other Islamic extremist groups. In various parts of the country, instances of ethnic, religious, and social conflict have flared up from time to time, often rendering those areas virtually ungovernable by the central authorities, and acts of violence against religious minorities have increased. At the time of partition in 1947, as many as 10 million Muslim refugees fled their homes in India and sought refuge in Pakistan—about 8 million in West Pakistan. Virtually an equal number of Hindus and Sikhs were uprooted from their land and familiar surroundings in what became Pakistan, and they fled to India. Unlike the earlier migrations, which took centuries to unfold, these chaotic population transfers took hardly one year. The resulting impact on the life of the subcontinent has reverberated ever since in the rivalries between the two countries, and each has continued to seek a lasting modus vivendi with the other. Pakistan and India have fought four wars, three of which (1948–49, 1965, and 1999) were over Kashmir. Since 1998 both countries have also possessed nuclear weapons, further heightening tensions between them. Land Pakistan is bounded by Iran to the west, Afghanistan to the northwest and north, China to the northeast, and India to the east and southeast. The coast of the Arabian Sea forms its southern border. Since 1947 the Kashmir region, along the western Himalayas, has been disputed, with Pakistan, India, and China each controlling sections of the territory. Part of the Pakistani-administered territory comprises the so-called Azad Kashmir (“Free Kashmir”) region—which Pakistan nonetheless considers an independent state, with its capital at Muzaffarabad. The remainder of Pakistani-administered Kashmir consists of Gilgit and Baltistan, known collectively as the Northern Areas. More … Score: https://www.britannica.com/place/Pakistan

2025/03/23

Home - Visit Namibia

DID YOU KNOW Interesting facts to know before visiting Namibia. Houses the Oldest Desert Only desert in the world where you can find large mammals like

2025/03/23