Independence Day Ukraine

Ukraine, country located in eastern Europe, the second largest on the continent after Russia. The capital is Kyiv (Kiev), located on the Dnieper River in north-central Ukraine. A fully independent Ukraine emerged only late in the 20th century, after long periods of successive domination by Poland-Lithuania, Russia, and the Union of Soviet Socialist Republics (U.S.S.R.). Ukraine had experienced a brief period of independence in 1918–20, but portions of western Ukraine were ruled by Poland, Romania, and Czechoslovakia in the period between the two World Wars, and Ukraine thereafter became part of the Soviet Union as the Ukrainian Soviet Socialist Republic (S.S.R.). When the Soviet Union began to unravel in 1990–91, the legislature of the Ukrainian S.S.R. declared sovereignty (July 16, 1990) and then outright independence (August 24, 1991), a move that was confirmed by popular approval in a plebiscite (December 1, 1991). With the dissolution of the U.S.S.R. in December 1991, Ukraine gained full independence. The country changed its official name to Ukraine, and it helped to found the Commonwealth of Independent States (CIS), an association of countries that were formerly republics of the Soviet Union. Land Ukraine is bordered by Belarus to the north, Russia to the east, the Sea of Azov and the Black Sea to the south, Moldova and Romania to the southwest, and Hungary, Slovakia, and Poland to the west. In the far southeast, Ukraine is separated from Russia by the Kerch Strait, which connects the Sea of Azov to the Black Sea. Relief Ukraine occupies the southwestern portion of the Russian Plain (East European Plain). The country consists almost entirely of level plains at an average elevation of 574 feet (175 metres) above sea level. Mountainous areas such as the Ukrainian Carpathians and Crimean Mountains occur only on the country’s borders and account for barely 5 percent of its area. The Ukrainian landscape nevertheless has some diversity: its plains are broken by highlands—running in a continuous belt from northwest to southeast—as well as by lowlands. Get a Britannica Premium subscription and gain access to exclusive content. Subscribe Now The rolling plain of the Dnieper Upland, which lies between the middle reaches of the Dnieper (Dnipro) and Southern Buh (Pivdennyy Buh, or the Boh) rivers in west-central Ukraine, is the largest highland area; it is dissected by many river valleys, ravines, and gorges, some more than 1,000 feet (300 metres) deep. On the west the Dnieper Upland is abutted by the rugged Volyn-Podilsk Upland, which rises to 1,545 feet (471 metres) at its highest point, Mount Kamula. West of the Volyn-Podilsk Upland, in extreme western Ukraine, the parallel ranges of the Carpathian Mountains—one of the most picturesque areas in the country—extend for more than 150 miles (240 km). The mountains range in height from about 2,000 feet (600 metres) to about 6,500 feet (2,000 metres), rising to 6,762 feet (2,061 metres) at Mount Hoverla, the highest point in the country. The northeastern and southeastern portions of Ukraine are occupied by low uplands rarely reaching an elevation of 1,000 feet (300 metres). Among the country’s lowlands are the Pripet Marshes (Polissya), which lie in the northern part of Ukraine and are crossed by numerous river valleys. In east-central Ukraine is the Dnieper Lowland, which is flat in the west and gently rolling in the east. To the south, another lowland extends along the shores of the Black Sea and the Sea of Azov; its level surface, broken only by low rises and shallow depressions, slopes gradually toward the Black Sea. The shores of the Black Sea and the Sea of Azov are characterized by narrow, sandy spits of land that jut out into the water; one of these, the Arabat Spit, is about 70 miles (113 km) long but averages less than 5 miles (8 km) in width. The southern lowland continues in the Crimean Peninsula as the North Crimean Lowland. The peninsula—a large protrusion into the Black Sea—is connected to the mainland by the Perekop Isthmus. The Crimean Mountains form the southern coast of the peninsula. Mount Roman-Kosh, at 5,069 feet (1,545 metres), is the mountains’ highest point. Drainage Almost all the major rivers in Ukraine flow northwest to southeast through the plains to empty into the Black Sea and the Sea of Azov. The Dnieper River, with its hydroelectric dams, huge reservoirs, and many tributaries, dominates the entire central part of Ukraine. Of the total course of the Dnieper, 609 miles (980 km) are in Ukraine, making it by far the longest river in the country, of which it drains more than half. Like the Dnieper, the Southern Buh, with its major tributary, the Inhul, flows into the Black Sea. To the west and southwest, partly draining Ukrainian territory, the Dniester (Dnistro) also flows into the Black Sea; among its numerous tributaries, the largest in Ukraine are the Stryy and the Zbruch. The middle course of the Donets River, a tributary of the Don, flows through southeastern Ukraine and is an important source of water for the Donets Basin (Donbas). The Danube River flows along the southwestern frontier of Ukraine. Marshland, covering almost 3 percent of Ukraine, is found primarily in the northern river valleys and in the lower reaches of the Dnieper, Danube, and other rivers. The rivers are most important as a water supply, and for this purpose a series of canals has been built, such as the Donets–Donets Basin, the Dnieper–Kryvyy Rih, and the North Crimea. Several of the larger rivers are navigable, including the Dnieper, Danube, Dniester, Pripet (Pryp’yat), Donets, and Southern Buh (in its lower course). Dams and hydroelectric plants are situated on all the larger rivers. Ukraine has a few natural lakes, all of them small and most of them scattered over the river floodplains. One of the largest is Lake Svityaz, 11 square miles (28 square km) in area, in the northwest. Small saltwater lakes occur in the Black Sea Lowland and in Crimea. Larger saline lakes occur along the coast. Known as limans, these bodies of water form at the mouths of rivers or ephemeral streams and are blocked off by sandbars from the sea. Some artificial lakes have been formed, the largest of which are reservoirs at hydroelectric dams—e.g., the reservoir on the Dnieper upstream from Kremenchuk. The Kakhovka, Dnieper, Dniprodzerzhynsk, Kaniv, and Kyiv reservoirs make up the rest of the Dnieper cascade. Smaller reservoirs are located on the Dniester and Southern Buh rivers and on tributaries of the Donets River. Small reservoirs for water supply also are found near Kryvyy Rih, Kharkiv, and other industrial cities. Three large artesian basins—the Volyn-Podilsk, the Dnieper, and the Black Sea—are exceptionally important for municipal needs and agriculture as well. More … Score: https://www.britannica.com/place/Ukraine

2026/08/24

Amazing Ukraine - Open for Tourism

It combines centuries-old traditions and contemporary art, fascinating urban architecture and unique nature, loud festivals and warm home holidays, as well as food, color, and hospitality, which is a decisive feature of the character of any Ukrainian.

2026/08/23

Visit Hungary

Act now and visit Hungary and its capital, Budapest! Add to your list the lake Balaton, and the world famous hungarian thermal bathes. Apply our website to ...

2026/08/22

Invest in Afghanistan

Afghanistan has a fast growing economy acting as a bridge, connecting south Asia-central Asia with the Middle East & Europe ultimately. As a World Trade Organization (WTO) member, the country is committed to enable business environment for domestic as well as foreign investors.

2026/08/21

Feast of the Establishment of the Hungarian State

Hungary, Hungarian Magyarország, landlocked country of central Europe. The capital is Budapest. At the end of World War I, defeated Hungary lost 71 percent of its territory as a result of the Treaty of Trianon (1920). Since then, grappling with the loss of more than two-thirds of their territory and people, Hungarians have looked to a past that was greater than the present as their collective psyche suffered from the so-called “Trianon Syndrome.” The syndrome was widespread prior to 1945; it was suppressed during Soviet domination (1945–90); and it reemerged during independence in 1990, when it took on a different form. The modern country appears to be split into two irreconcilable factions: those who are still concerned about Trianon and those who would like to forget it. This split is evident in most aspects of Hungarian political, social, and cultural life. Hungarians, who know their country as Magyarország, “Land of Magyars,” are unique among the nations of Europe in that they speak a language that is not related to any other major European language. Linguistically surrounded by alien nations, Hungarians felt isolated through much of their history. This may be the reason why after Christianization they became attached to Latin, which became the language of culture, scholarship, and state administration—and even the language of the Hungarian nobility until 1844. Cast adrift in a Slavic-Germanic sea, Hungarians are proud to have been the only people to establish a long-lasting state in the Carpathian Basin. Only after six centuries of independent statehood (896–1526) did Hungary become part of two other political entities: the Habsburg and Ottoman empires. But even then Hungarians retained much of their separate political identity and near-independence, which in 1867 made them a partner in Austria-Hungary (1867–1918). This was much more than the other nations of the Carpathian Basin were able to achieve before 1918.By accepting Catholicism in 1000 ce, the Hungarians joined the Christianized nations of the West, but they still remained on the borderlands of that civilization. This made them eager to prove themselves and also defensive about lagging behind Western developments elsewhere. Their geographical position often forced them to fight various Eastern invaders, and, as a result, they viewed themselves as defenders of Western Christianity. In that role, they felt that the West owed them something, and when, in times of crisis, special treatment was not forthcoming (e.g., Trianon in 1920), they judged the West as ungrateful.Today Hungary is wholly Budapest-centred. The capital dominates the country both by the size of its population—which dwarfs those of Hungary’s other cities—and by the concentration within its borders of most of the country’s scientific, scholarly, and artistic institutions. Budapest is situated on both banks of the Danube (Hungarian: Duna) River, a few miles downstream from the Danube Bend. It is a magnificent city, even compared with the great pantheon of European capitals, and it has been an anchor of Hungarian culture since its inception. In spite of many national tragedies during the last four centuries, Hungarians remain confident and are proud of their achievements in the sciences, scholarship, and the arts. During the 20th century, many talented Hungarians emigrated, particularly to the United States. Among them were leading scientists who played a defining role in the emergence of American atomic discovery and the computer age. The abundance of these scientists, mathematicians, economists, anthropologists, musicians, and artists—among them a dozen Nobel laureates—prompted Laura Fermi, writer and wife of Italian American physicist Enrico Fermi, to speculate about “the mystery of the Hungary talent.” Land Landlocked and lying approximately between latitudes 45° and 49° N and longitudes 16° and 23° E, Hungary shares a border to the north with Slovakia, to the northeast with Ukraine, to the east with Romania, to the south with Serbia (specifically, the Vojvodina region) and Croatia, to the southwest with Slovenia, and to the west with Austria. Relief Dominating the relief are the great lowland expanses that make up the core of Hungary. The Little Alfold (Little Hungarian Plain, or Kisalföld) lies in the northwest, fringed to the west by the easternmost extension of the sub-Alps along the border with Austria and bounded to the north by the Danube. The Little Alfold is separated from the Great Alfold (Great Hungarian Plain, or Nagy Magyar Alföld) by a low mountain system extending across the country from southwest to northeast for a distance of 250 miles (400 km). This system, which forms the backbone of the country, is made up of Transdanubia (Dunántúl) and the Northern Mountains, separated by the Visegrád Gorge of the Danube. Transdanubia is dominated by the Bakony Mountains, with dolomite and limestone plateaus at elevations between 1,300 and 2,300 feet (400 and 700 metres) above sea level. Volcanic peaks comprise the Mátra Mountains in the north, reaching an elevation of 3,327 feet (1,014 metres) at Mount Kékes, Hungary’s highest peak. Regions of hills reaching elevations of 800 to 1,000 feet (250 to 300 metres) lie on either side of the mountain backbone, while to the south and west of Lake Balaton is an upland region of more-subdued loess-covered topography. The Great Alfold covers most of central and southeastern Hungary. Like its northwestern counterpart, it is a basinlike structure filled with fluvial and windblown deposits. Four types of surface may be distinguished: floodplains, composed of river alluvium; alluvial fans, wedge-shaped features deposited at the breaks of slopes where rivers emerge from the mountain rim; alluvial fans overlain by sand dunes; and plains buried under loess, deposits of windblown material derived from the continental interior. These lowlands range in elevation from about 260 to 660 feet (80 to 200 metres) above sea level, with the lowest point at 256 feet (78 metres), on the southern edge of Szeged, along the Tisza River. In the northeast, bordering Slovakia, is Aggtelek National Park; characterized by karst terrain and featuring hundreds of caves, the area was designated a UNESCO World Heritage site in the late 20th century. More … Score: https://www.britannica.com/place/Hungary 

2026/08/20

Introducing Hungary

Start exploring Hungary with Lonely Planet’s video guide to getting around, when to go and the top things to do while you're there.

2026/08/19

Gabon | Travel and Ecotourism

The beautiful landscape in Gabon has many facets conducive to tourism. As part of the Congo basin, Gabon has flora and fauna that are among the most ...

2026/08/19

Independence Day of the Islamic Republic of Afghanistan

Afghanistan, landlocked multiethnic country located in the heart of south-central Asia. Lying along important trade routes connecting southern and eastern Asia to Europe and the Middle East, Afghanistan has long been a prize sought by empire builders, and for millennia great armies have attempted to subdue it, leaving traces of their efforts in great monuments now fallen to ruin. The country’s forbidding landscape of deserts and mountains has laid many imperial ambitions to rest, as has the tireless resistance of its fiercely independent peoples—so independent that the country has failed to coalesce into a nation but has instead long endured as a patchwork of contending ethnic factions and ever-shifting alliances. The modern boundaries of Afghanistan were established in the late 19th century in the context of a rivalry between imperial Britain and tsarist Russia that Rudyard Kipling termed the “Great Game.” Modern Afghanistan became a pawn in struggles over political ideology and commercial influence. In the last quarter of the 20th century, Afghanistan suffered the ruinous effects of civil war greatly exacerbated by a military invasion and occupation by the Soviet Union (1979–89). In subsequent armed struggles, a surviving Afghan communist regime held out against Islamic insurgents (1989–92), and, following a brief rule by mujahideen groups, an austere movement of religious students—the Taliban—rose up against the country’s governing parties and warlords and established a theocratic regime (1996–2001) that soon fell under the influence of a group of well-funded Islamists led by an exiled Saudi Arabian, Osama bin Laden. The Taliban regime collapsed in December 2001 in the wake of a sustained U.S.-dominated military campaign aimed at the Taliban and fighters of bin Laden’s al-Qaeda organization. Soon thereafter, anti-Taliban forces agreed to a period of transitional leadership and an administration that would lead to a new constitution and the establishment of a democratically elected government.The capital of Afghanistan is its largest city, Kabul. A serene city of mosques and gardens during the storied reign of the emperor Bābur (1526–30), founder of the Mughal dynasty, and for centuries an important entrepôt on the Silk Road, Kabul lay in ruins following the long and violent Afghan War. So, too, fared much of the country, its economy in shambles and its people scattered and despondent. By the early 21st century an entire generation of Afghans had come to adulthood knowing nothing but war. Land Afghanistan is completely landlocked—the nearest coast lies along the Arabian Sea, about 300 miles (480 km) to the south—and, because of both its isolation and its volatile political history, it remains one of the most poorly surveyed areas of the world. It is bounded to the east and south by Pakistan (including those areas of Kashmir administered by Pakistan but claimed by India), to the west by Iran, and to the north by the Central Asian states of Turkmenistan, Uzbekistan, and Tajikistan. It also has a short border with Xinjiang, China, at the end of the long, narrow Vākhān (Wakhan Corridor), in the extreme northeast. Its overall area is roughly twice that of Norway. Relief - The Hindu Kush Afghanistan’s shape has been compared to a leaf, of which the Vākhān strip, nestled high in the Pamirs, forms the stem. The outstanding geographic feature of Afghanistan is its mountain range, the Hindu Kush. This formidable range creates the major pitch of Afghanistan from northeast to southwest and, along with its subsidiary ranges, divides Afghanistan into three distinct geographic regions, which roughly can be designated as the central highlands, the northern plains, and the southwestern plateau. When the Hindu Kush itself reaches a point some 100 miles (160 km) north of Kabul, it spreads out and continues westward as a series of ranges under the names of Bābā, Bāyan, Sefīd Kūh (Paropamisus), and others, and each section in turn sends spurs in different directions. One of these spurs is the Torkestān Mountains, which extend northwestward. Other important ranges include the Sīāh Kūh, south of the Harīrūd, and the Ḥeṣār Mountains, which stretch northward. A number of other ranges, including the Mālmand and Khākbād, extend to the southwest. On the eastern frontier with Pakistan, several mountain ranges effectively isolate the interior of the country from the moisture-laden winds that blow from the Indian Ocean. This accounts for the dryness of the climate. Physiographic regions The central highlands—actually a part of the Himalayan chain—include the main Hindu Kush range. Its area of about 160,000 square miles (414,000 square km) is a region of deep, narrow valleys and lofty mountains, some peaks of which rise above 21,000 feet (6,400 metres). High mountain passes, generally situated between 12,000 and 15,000 feet (3,600 to 4,600 metres) above sea level, are of great strategic importance and include the Shebar Pass, located northwest of Kabul where the Bābā Mountains branch out from the Hindu Kush, and the storied Khyber Pass, which leads to the Indian subcontinent, on the Pakistan border southeast of Kabul. The Badakhshān area in the northeastern part of the central highlands is the location of the epicentres for many of the 50 or so earthquakes that occur in the country each year. The northern plains region, north of the central highlands, extends eastward from the Iranian border to the foothills of the Pamirs, near the border with Tajikistan. It comprises some 40,000 square miles (103,000 square km) of plains and fertile foothills sloping gently toward the Amu Darya (the ancient Oxus River). This area is a part of the much larger Central Asian Steppe, from which it is separated by the Amu Darya. The average elevation is about 2,000 feet (600 metres). The northern plains region is intensively cultivated and densely populated. In addition to fertile soils, the region possesses rich mineral resources, particularly deposits of natural gas. The southwestern plateau, south of the central highlands, is a region of high plateaus, sandy deserts, and semideserts. The average elevation is about 3,000 feet (900 metres). The southwestern plateau covers about 50,000 square miles (130,000 square km), one-fourth of which forms the sandy Rīgestān region. The smaller Mārgow Desert of salt flats and desolate steppe lies west of Rīgestān. Several large rivers cross the southwestern plateau; among them are the Helmand River and its major tributary, the Arghandāb. Most of Afghanistan lies between 2,000 and 10,000 feet (600 and 3,000 metres) in elevation. Along the Amu Darya in the north and the delta of the Helmand River in the southwest, the elevation is about 2,000 feet (600 metres). The Sīstān depression of the southwestern plateau is roughly 1,500 to 1,700 feet (450 to 500 metres) in elevation. More … Score: https://www.britannica.com/place/Afghanistan

2026/08/19

A Tourist in Afghanistan 2021

A video journey of a recent trip to Afghanistan in January 2021 as a tourist. Visiting sites around Kabul & Panjshir Valley with Jared Hauck & friends Marilyn & Jim Collins.

2026/08/18