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

Welcome to Pakistan - Tourism Promotional Video

Welcome to Pakistan If you ever decide to travel to Pakistan, I promise you that you will have the adventure of your lifetime. This Pakistan travel guide contains everything you need to know, including all travel information regarding visas, transportation, cultural etiquette, cultural behavior, costs and more!

2025/03/22

Visit Tunisia DMC | Official Website

Visit Tunisia is a full service Destination Management Company that has a long experience to help You to design, plan and deliver memorable events ..

2025/03/22

Independence Day the Republic of Namibia

Namibia, officially Republic of Namibia, also called (internationally until 1968) South West Africa, Afrikaans Namibië or Suidwesafrica, country located on the southwestern coast of Africa. It is bordered by Angola to the north, Zambia to the northeast, Botswana to the east, South Africa to the southeast and south, and the Atlantic Ocean to the west. It ranges from arid in the north to desert on the coast and in the east. The landscape is spectacular, but the desert, mountains, canyons, and savannas are perhaps better to see than to occupy. The only permanent rivers are the Kunene (Cunene), the Okavango (Cubango), the Mashi (Kwando), and the Zambezi on the northern border and the Orange on the southern. Only the northern frontier—and not all of it—is readily passable. The coastal Namib desert, the treacherous reefs and shoals of the coast (half aptly named the “Skeleton Coast”), the near deserts along the Orange River, and the dry Kalahari region to the east explain the late conquest of Namibia and form a geographic frame around the country. Roughly rectangular (600 by 300 to 450 miles [965 by 480 to 725 kilometres]), Namibia has a long, narrow eastern extension (the Caprivi Strip) based on a German misconception that access to the Zambezi—despite the Victoria Falls—meant access to the Indian Ocean. After 106 years of German and South African rule, Namibia became independent on March 21, 1990, under a democratic multiparty constitution. The capital of the country is Windhoek. Land - Relief Namibia is divided from west to east into three main topographic zones: the coastal Namib desert, the Central Plateau, and the Kalahari. The Namib is partly rocky and partly (in the central stretch) dunes. While having complex flora and fauna, it is a fragile and sparsely covered environment unsuitable for pastoral or agricultural activities. Diamonds (probably washed down from the Basotho highlands by the Orange River) and uranium are found at Oranjemund in the south and Arandis in the centre. The Namib, 50 to 80 miles wide over most of its length, is constricted in the north where the Kaokoveld, the western mountain scarp of the Central Plateau, abuts on the sea. The Central Plateau, which varies in altitude from 3,200 to 6,500 feet (975 to 1,980 metres), is the core of the agricultural life of Namibia. In the north it abuts on the Kunene and Okavango river valleys and in the south on the Orange. Largely savanna and scrub, it is somewhat more wooded in parts of the north and is broken throughout by hills, mountains, ravines (including the massive Fish River Canyon), and salt pans (notably the Etosha Pan). Brandberg, also known as Mount Brand (8,442 feet [2,573 metres]), is Namibia’s highest mountain and is located along the plateau’s western escarpment. In the east, Namibia slopes gradually downward, and the savanna merges into the Kalahari. In the north, hardpan and rock beneath the sand, in addition to more abundant river water and rainfall, make both herding and cultivation possible. Drainage and soils As noted, only the border rivers are permanent. The Swakop and Kuiseb rivers rise on the plateau, descend the western escarpment, and die out in the Namib (except in rare flood years, when they reach the sea at Swakopmund and Walvis Bay, respectively). The Fish (Vis) River rises in the Central Plateau and (seasonally) flows south to the Orange. Various lesser rivers rise on the plateau and die out downstream in the Namib or Kalahari desert. Namibia’s soils range from barren sand and rock to low-quality sand-dominated to relatively fertile soils. The best soils are in the north, in the Otavi Mountains, in parts of the central and southern portions of the plateau, and in the Caprivi Strip. Water—not soil fertility—is the primary constraint on agriculture. Both in the densely populated Ovambo region in the north and in the commercial farming areas, overuse of land has reduced tree and bush cover, compacted soils, led to serious erosion, and lowered the water table by as much as 100 feet in the 20th century. Climate of Namibia Namibia is located on the southern margin of the tropics and has distinct seasons. The coast is cooled by the Benguela Current (which carries with it the country’s rich and recovering fish stocks) and averages less than 2 inches (50 millimetres) of rainfall annually. The Central Plateau and the Kalahari have wide diurnal temperature ranges, more than 50 °F (30 °C) on summer days and less than 20 °F (10 °C) in winter. In Windhoek, on the plateau, the average temperature for December is 75 °F (24 °C), and the average maximum 88 °F (31 °C). In July these averages are 55 °F (13 °C) and 68 °F (20 °C), respectively. Humidity is normally low, and rainfall increases from about 10 inches (250 millimetres) on the southern and western parts of the plateau to about 20 inches in the north-central part and more than 24 inches on the Caprivi Strip and Otavi Mountains. However, rainfall is highly variable, and multiyear droughts are common. In the north and adjacent to mountains, groundwater is as important as—but only slightly less variable than—rainfall. Kalahari rainfall—in its Namibian portion—is not radically different from that of the plateau, but, except in the northern Karstveld and isolated artesian areas, groundwater is less available. More … Score: https://www.britannica.com/place/Namibia

2025/03/21

This is Namibia

This is Namibia. Video courtesy: Travel News Namibia

2025/03/20

Independence Day of Tunisian Republic

Tunisia, country of North Africa. Tunisia’s accessible Mediterranean Sea coastline and strategic location have attracted conquerors and visitors throughout the ages, and its ready access to the Sahara has brought its people into contact with the inhabitants of the African interior. According to Greek legend, Dido, a princess of Tyre, was the first outsider to settle among the native tribes of what is now Tunisia when she founded the city of Carthage in the 9th century bce. Although the story is certainly apocryphal, Carthage nonetheless grew into one of the great cities and preeminent powers of antiquity, and its colonies and entrepôts were scattered throughout the western Mediterranean region. Carthage fought a series of wars with its rival, Rome. Rome prevailed in the mid-2nd century bce, razed Carthage, and ruled the region for the following 500 years. In the 7th century Arab conquerors converted the native Berber (Amazigh) population of North Africa to Islam. The area was ruled by a succession of Islamic dynasties and empires until coming under French colonial rule in the late 19th century. After achieving independence in 1956, Tunisia pursued a progressive social agenda and sought to modernize its economy under two long-serving presidents, Habib Bourguiba and Zine al-Abidine Ben Ali. However, Tunisia remained an authoritarian state with an all-powerful ruling party and no significant institutions of representative government. (For a discussion of political changes in Tunisia in 2011, see Jasmine Revolution.) Tunisia’s culture is highly diverse, in part because of long periods of Ottoman and then French rule but also because populations of Jews and Christians have lived among a Muslim majority for centuries. Similarly, the capital, Tunis, blends ancient Arab souks and mosques and modern-style office buildings into one of the most handsome and lively cities in the region. Other cities include Sfax (Ṣafāqis), Sousse (Sūsah), and Gabès (Qābis) on the fertile coast and Kairouan (Al-Qayrawān) and El-Kef (Al-Kāf) in the arid interior. We shared the ground floor of a shapeless old building, a sort of two-room apartment. The kitchen, half of it roofed over and the rest an open courtyard, was a long vertical passage toward the light. But before reaching this square of pure blue sky, it received, from a multitude of windows, all the smoke, the smells, and the gossip of our neighbours. At night, each locked himself in his room, but in the morning, life was always communal. This warmth, joined with the country’s renowned hospitality and cuisine, has contributed greatly to Tunisia’s growing popularity as a destination for tourists from throughout Europe and the Americas. Land Tunisia is bounded by Algeria to the west and southwest, by Libya to the southeast, and by the Mediterranean Sea to the east and north. Relief Tunisia is characterized by moderate relief. The Tunisian Dorsale, or High Tell, a southwest-northeast–trending mountain range that is an extension of the Saharan Atlas (Atlas Saharien) of Algeria, tapers off in the direction of the Sharīk (Cape Bon) Peninsula in the northeast, south of the Gulf of Tunis. The highest mountain, Mount Chambi (Al-Shaʿnabī), located near the centre of the Algerian border, rises to 5,066 feet (1,544 metres), while Mount Zaghwān (Zaghouan), about 30 miles (50 km) southwest of Tunis, reaches 4,249 feet (1,295 metres). Between the limestone peaks of the central Tunisian Dorsale and the mountains of the Northern Tell—which include the sandstone ridges of the Kroumirie Mountains in the northwest that reach elevations of 3,000 feet (900 metres)—and the Mogods, a mountain range running along the deeply indented coastline to the north, lies the Majardah (Medjerda) River valley, formed by a series of ancient lake basins covered with alluvium. This valley was once the granary of ancient Rome and has remained to this day the richest grain-producing region of Tunisia. To the south of the Tunisian Dorsale lies a hilly region known as the Haute Steppe (High Steppes) in the west and the Basse Steppe (Low Steppes) in the east. These have elevations ranging from about 600 to 1,500 feet (180 to 460 metres) and are crossed by secondary ranges trending north-south. Farther south there is a series of chott (or shaṭṭ; salty lake) depressions. Large plains border the eastern coasts; south of Sousse lies Al-Sāḥil (Sahel) and south of Gabès is Al-Jifārah (Gefara) Plain. The extreme south is largely sandy desert, much of it part of the Great Eastern Erg of the Sahara. Drainage The major drainage feature of the north is the Majardah River, the country’s only perennially flowing stream, which cuts the Majardah valley before emptying into the Gulf of Tunis, near the site of ancient Carthage. Farther south, streams are intermittent and largely localized in the form of wadis, which are subject to seasonal flooding and terminate inland in chotts. In the country’s most southerly regions, within the Sahara, even these seasonal streams are rare. As in other countries of this arid region, access to water is a major concern. During the 1990s the government sponsored the construction of a number of dams to control flooding, preserve runoff, and recharge the water table. Soils Tunisia’s most fertile soils are found in the well-watered intermontane valleys in the north, where rich sandy clay soils formed from alluvium or soils high in lime content cover the valley bottoms and plains. Aside from these and from the plains of the Haute Steppe region, where some clay soils of medium fertility may be found, soils in the rest of the country tend to be rocky or sandy. In the dry south, moreover, they are often also saline because of excessive evaporation. The humid coastal plain in the east, running between the Gulf of Hammamet and the Gulf of Gabes, where Tunisia’s thriving olive plantations are found, is the most agriculturally productive of these coarse-textured soil areas. more … Score: https://www.britannica.com/place/Tunisia

2025/03/20

Tunisia 2020 - the official film

Tunisia 2020 - Invest In Tunisia

2025/03/19