The official birthday of Queen Elizabeth II of United Kingdom of Great Britain and Northern Ireland

United Kingdom, island country located off the northwestern coast of mainland Europe. The United Kingdom comprises the whole of the island of Great Britain—which contains England, Wales, and Scotland—as well as the northern portion of the island of Ireland. The name Britain is sometimes used to refer to the United Kingdom as a whole. The capital is London, which is among the world’s leading commercial, financial, and cultural centres. Other major cities include Birmingham, Liverpool, and Manchester in England, Belfast and Londonderry in Northern Ireland, Edinburgh and Glasgow in Scotland, and Swansea and Cardiff in Wales. The origins of the United Kingdom can be traced to the time of the Anglo-Saxon king Athelstan, who in the early 10th century ce secured the allegiance of neighbouring Celtic kingdoms and became “the first to rule what previously many kings shared between them,” in the words of a contemporary chronicle. Through subsequent conquest over the following centuries, kingdoms lying farther afield came under English dominion. Wales, a congeries of Celtic kingdoms lying in Great Britain’s southwest, was formally united with England by the Acts of Union of 1536 and 1542. Scotland, ruled from London since 1603, formally was joined with England and Wales in 1707 to form the United Kingdom of Great Britain. (The adjective “British” came into use at this time to refer to all the kingdom’s peoples.) Ireland came under English control during the 1600s and was formally united with Great Britain through the Act of Union of 1800. The republic of Ireland gained its independence in 1922, but six of Ulster’s nine counties remained part of the United Kingdom as Northern Ireland. Relations between these constituent states and England have been marked by controversy and, at times, open rebellion and even warfare. These tensions relaxed somewhat during the late 20th century, when devolved assemblies were introduced in Northern Ireland, Scotland, and Wales. Nonetheless, even with the establishment of a power-sharing assembly after referenda in both Northern Ireland and the Irish republic, relations between Northern Ireland’s unionists (who favour continued British sovereignty over Northern Ireland) and nationalists (who favour unification with the republic of Ireland) remained tense into the 21st century. The United Kingdom has made significant contributions to the world economy, especially in technology and industry. Since World War II, however, the United Kingdom’s most prominent exports have been cultural, including literature, theatre, film, television, and popular music that draw on all parts of the country. Perhaps Britain’s greatest export has been the English language, now spoken in every corner of the world as one of the leading international mediums of cultural and economic exchange. The United Kingdom retains links with parts of its former empire through the Commonwealth. It also benefits from historical and cultural links with the United States and is a member of the North Atlantic Treaty Organization (NATO). Moreover, the United Kingdom became a member of the European Union in 1973. Many Britons, however, were sometimes reluctant EU members, holding to the sentiments of the great wartime prime minister Winston Churchill, who sonorously remarked, “We see nothing but good and hope in a richer, freer, more contented European commonalty. But we have our own dream and our own task. We are with Europe, but not of it. We are linked, but not comprised. We are interested and associated, but not absorbed.” Indeed, in June 2016, in a referendum on whether the United Kingdom should remain in the EU, 52 percent of British voters chose to leave. After much negotiation, several deadline extensions, prolonged domestic political discord, and two changes of prime minister, an agreement on “Brexit” (British exit from the EU) was reached that satisfied both the EU and the majority of Parliament. Thus, on January 31, 2020, the United Kingdom would become the first country to withdraw from the EU. Get a Britannica Premium subscription and gain access to exclusive content. Subscribe Now Ralph Charles Atkins The Editors of Encyclopaedia Britannica Land The United Kingdom comprises four geographic and historical parts—England, Scotland, Wales, and Northern Ireland. The United Kingdom contains most of the area and population of the British Isles—the geographic term for the group of islands that includes Great Britain, Ireland, and many smaller islands. Together England, Wales, and Scotland constitute Great Britain, the larger of the two principal islands, while Northern Ireland and the republic of Ireland constitute the second largest island, Ireland. England, occupying most of southern Great Britain, includes the Isles of Scilly off the southwest coast and the Isle of Wight off the southern coast. Scotland, occupying northern Great Britain, includes the Orkney and Shetland islands off the northern coast and the Hebrides off the northwestern coast. Wales lies west of England and includes the island of Anglesey to the northwest. Apart from the land border with the Irish republic, the United Kingdom is surrounded by sea. To the south of England and between the United Kingdom and France is the English Channel. The North Sea lies to the east. To the west of Wales and northern England and to the southeast of Northern Ireland, the Irish Sea separates Great Britain from Ireland, while southwestern England, the northwestern coast of Northern Ireland, and western Scotland face the Atlantic Ocean. At its widest the United Kingdom is 300 miles (500 km) across. From the northern tip of Scotland to the southern coast of England, it is about 600 miles (1,000 km). No part is more than 75 miles (120 km) from the sea. The capital, London, is situated on the tidal River Thames in southeastern England. The archipelago formed by Great Britain and the numerous smaller islands is as irregular in shape as it is diverse in geology and landscape. This diversity stems largely from the nature and disposition of the underlying rocks, which are westward extensions of European structures, with the shallow waters of the Strait of Dover and the North Sea concealing former land links. Northern Ireland contains a westward extension of the rock structures of Scotland. These common rock structures are breached by the narrow North Channel. On a global scale, this natural endowment covers a small area—approximating that of the U.S. state of Oregon or the African country of Guinea—and its internal diversity, accompanied by rapid changes of often beautiful scenery, may convey to visitors from larger countries a striking sense of compactness and consolidation. The peoples who, over the centuries, have hewed an existence from this Atlantic extremity of Eurasia have put their own imprint on the environment, and the ancient and distinctive palimpsest of their field patterns and settlements complements the natural diversity. Relief Great Britain is traditionally divided into a highland and a lowland zone. A line running from the mouth of the River Exe, in the southwest, to that of the Tees, in the northeast, is a crude expression of this division. The course of the 700-foot (213-metre) contour, or of the boundary separating the older rocks of the north and west from the younger southeastern strata, provides a more accurate indication of the extent of the highlands. More … Score: https://www.britannica.com/place/United-Kingdom

2025/06/11

iLove Philippines | Welcome to the Philippines

Officially the Republic of the Philippines (Filipino: Republika ng Pilipinas), is a sovereign island country in Southeast Asia situated in the western Pacific Ocean. It consists of about 7,641 islands that are categorized broadly under three main geographical divisions from north to south: Luzon, Visayas, and Mindanao. The capital city of the Philippines is Manila and the most populous city is Quezon City, both part of Metro Manila.

2025/06/11

Portuguese Republic Portugal Day

Portugal, officially Portuguese Republic, Portuguese República Portuguesa, country lying along the Atlantic coast of the Iberian Peninsula in southwestern Europe. Once continental Europe’s greatest power, Portugal shares commonalities—geographic and cultural—with the countries of both northern Europe and the Mediterranean. Its cold, rocky northern coast and mountainous interior are sparsely settled, scenic, and wild, while the country’s south, the Algarve, is warm and fertile. The rugged Estrela Mountains (Serra da Estrela, or “Star Mountain Range”), which lie between the Tagus and Mondego rivers, contain the highest point of mainland Portugal. In the 1st millennium bce the Celtic Lusitani entered the Iberian Peninsula and settled the land, and many traces of their influence remain. According to national legend, though, Lisbon, the national capital, was founded not by Celts but by the ancient Greek warrior Odysseus, who was said to have arrived at a rocky headland near what is the present-day city after leaving his homeland to wander the world and who, liking what he saw, stayed there for a while; his departure was said to have broken the heart of the nymph Calypso, who, the legend goes, turned herself into a snake, her coils becoming the seven hills of Lisbon. Of course, had Odysseus actually come to Portugal, he would have found the land already well settled by the Lusitani. Lusitani tribes battled the Romans for generations before acceding to empire, whereupon Rome established several important towns and ports; the Roman presence can be seen in the very name of the country, which derives from Portus Cale, a settlement near the mouth of the Douro River and the present-day city of Porto. Later, the descendants of Romans and the Lusitani would live under Moorish rule for several centuries until an independent kingdom was established. In constant battle and rivalry with Spain, its eastern neighbour, Portugal then turned to the sea and, after Henry the Navigator’s establishment of a school of navigation at Sagres, in time founded a vast overseas empire that would become Europe’s largest and richest. Much of that empire was quickly lost, but even then Portugal retained sizable holdings along the African coast, in southern and eastern Asia, and in South America. Portugal remained a colonial power until the mid-1970s, when a peaceful revolution transformed the country from a dictatorship into a democratic republic. Long among the poorest countries of Europe, Portugal modernized in the last decades of the 20th century, expanding its economy from one based primarily on textile manufacture and livestock raising to include a range of manufactures and services. Lisbon is Portugal’s capital and economic and cultural centre. The city clings to low but steep hills situated on the right bank of the Tagus and is a popular tourist destination. Lisbon is rather more tranquil and reserved than Madrid in neighbouring Spain, but it shares with it a reputation for great food, melancholy and romantic music, dance, and sport. Portuguese traditionally have prized a simple and unostentatious life, favouring the rural over the urban and the traditional to the modern, where a fine meal might consist of carne de porco à Alentejana (lean pork stuffed with clams), thick-crusted bread, and dark wine. Portuguese delight in the countryside, where they gather to hold family picnics, tend to their gardens and orchards, and relax. It is from the countryside that the fado, a form of romantic ballad, is thought to have come (though it is now clearly associated with the cities of Lisbon and Coimbra), and it is in the countryside that the country’s traditional sport of bullfighting takes its finest form, though in Portuguese bullfighting the bull is not killed but rather is retired to the countryside for the rest of its life. Land of Portugal Portugal occupies one-sixth of the Iberian Peninsula at Europe’s southwestern perimeter. To its north and east is Spain, which makes up the rest of the peninsula; to the south and the west is the Atlantic Ocean; and to the west and southwest lie the Azores (Açores) and the Madeira Islands, which are part of metropolitan Portugal. Portugal is not a large country, but it offers a great diversity of physical geography, ranging from low-lying coasts and plains to the Estrela Mountains, which rise to nearly 6,500 feet (2,000 metres). With Spanish Galicia, northern Portugal comprises the mountainous border of the Meseta (the block of ancient rock that forms the core of the Iberian Peninsula); southern Portugal also contains extensive areas of limestone and other sedimentary strata, mostly plateaus or plains. Other physical features link Portugal with Spain: its major rivers—Douro, Tagus (Rio Tejo), Guadiana—rise in the central Meseta before draining west (or, in the case of the Guadiana, south) to the Atlantic, while the proximity of the Meseta affects the climate and increases the rainfall of the northern Portuguese interior, contributing to that region’s verdant vegetation. Southern Portugal, however, is predominantly Mediterranean both in vegetation and in climate. Despite Portugal’s remarkable scenic diversity, the essence of its relief and underlying geology can be described under three headings: the north, the northern interior, and the south. The old coastal provinces of Beira Litoral and Estremadura are transitional in cultural landscape, vegetation, and climate but southern in relief and geology. In order to discuss Portugal’s physiographic regions, however, it is necessary to consider the provincial divisions of the country that no longer exist as administrative entities but that survive as important geographical designations. Although superseded by several planning regions and districts (see below Local government) that now organize Portugal, six provinces have traditionally divided the country since the Middle Ages (though these never served as administrative units): Minho, located between the Minho and Douro rivers; Trás-os-Montes, bounded by Spain (north and east), by the gorges of the Douro River (south), and by the mountains (west); Beira, extending from the Douro River in the north to the Tagus in the southeast and from the border with Spain to the Atlantic Ocean; Estremadura, containing Lisbon; the Alentejo, covering south-central Portugal; and the Algarve, in southern Portugal. From 1933 to 1959, mainland Portugal also was officially further divided into 11 new provinces that were created on a geographic and economic basis: the Algarve, the Alto (Upper) Alentejo, the Baixo (Lower) Alentejo, Beira Alta (Upper Beira), Beira Baixa (Lower Beira), Beira Litoral, Douro Litoral, Estremadura, Minho, Ribatejo, and Trás-os-Montes e Alto (Upper) Douro. More … Score: https://www.britannica.com/place/Portugal

2025/06/10

Welcome to GREAT

The GREAT Britain Campaign gratefully acknowledges the help provided by the following organisations:

2025/06/10

The beauty of Portugal

Portugal is an amazing country and I would like to thank everyone, who made me feel great over there. During 2 weeks, I was able to travel from the North to the South, where I stayed in Lisbon. In this video, you will visit: Porto, Braga, Guimaraes, Coimbra, Fátima, Nazare, Lisbon, Cascais and Sintra. I had so many beautiful shots, unfortunately, not all of them made it into the final cut.

2025/06/09

Welcome to Denmark, the Land of Everyday Wonder

Get ready for simple pleasures and unexpected delights. We're here to make your visit to Denmark the most wonder-full experience. Before you pack your bags be sure to check out all of our updates on safe travel to Denmark. Ready? Let’s get exploring.

2025/06/07

Flag day of Kingdom of Sweden

Sweden, country located on the Scandinavian Peninsula in northern Europe. The name Sweden was derived from the Svear, or Suiones, a people mentioned as early as 98 ce by the Roman author Tacitus. The country’s ancient name was Svithiod. Stockholm has been the permanent capital since 1523. Sweden occupies the greater part of the Scandinavian Peninsula, which it shares with Norway. The land slopes gently from the high mountains along the Norwegian frontier eastward to the Baltic Sea. Geologically, it is one of the oldest and most stable parts of the Earth’s crust. Its surface formations and soils were altered by the receding glaciers of the Pleistocene Epoch (about 2,600,000 to 11,700 years ago). Lakes dot the fairly flat landscape, and thousands of islands form archipelagoes along more than 1,300 miles (2,100 km) of jagged, rocky coastline. Like all of northwestern Europe, Sweden has a generally favourable climate relative to its northerly latitude owing to moderate southwesterly winds and the warm North Atlantic Current. The country has a 1,000-year-long continuous history as a sovereign state, but its territorial expanse changed often until 1809. Today it is a constitutional monarchy with a well-established parliamentary democracy that dates from 1917. Swedish society is ethnically and religiously very homogeneous, although recent immigration has created some social diversity. Historically, Sweden rose from backwardness and poverty into a highly developed postindustrial society and advanced welfare state with a standard of living and life expectancy that rank among the highest in the world. Sweden long ago disavowed the military aggressiveness that once involved its armies deeply in Europe’s centuries of dynastic warfare. It has chosen instead to play a balancing role among the world’s conflicting ideological and political systems. It is for this reason that Swedish statesmen have often been sought out to fill major positions in the United Nations. At peace since 1814, Sweden has followed the doctrine, enunciated in every document on foreign policy since World War II, of “nonalignment in peace aiming at neutrality in war.” Land Sweden lies to the southwest of Finland. A long coastline forms the country’s eastern border, extending along the Gulf of Bothnia and the Baltic Sea; a narrow strait, known as The Sound (Öresund), separates Sweden from Denmark in the south. A shorter coastline along the Skagerrak and Kattegat straits forms Sweden’s border to the southwest, and Norway lies to the west. Sweden extends some 1,000 miles (1,600 km) to the north and south and 310 miles (500 km) to the east and west. The country is traditionally divided into three regions: to the north is Norrland, the vast mountain and forest region; in central Sweden is Svealand, an expanse of lowland in the east and highland in the west; and in the south is Götaland, which includes the Småland highlands and, at the southern extremity, the small but rich plains of Skåne. In the far north the region of Lappland overlaps Norrland and northern Finland. Relief Norrland is the largest and most sparsely populated of the regions, covering some three-fifths of the country. The region features an undulating surface of rounded hills and mountains, large lakes, and extensive river valleys. To the west lie the Kölen (Kjølen; Scandinavian) Mountains, through which runs the border demarcating Sweden and Norway. This range is characterized by numerous glaciers, the southernmost of which is on Helags Mountain (Helagsfjället), near the Norwegian border. At the region’s far northern edge, north of the Arctic Circle, are Sweden’s highest peaks: Mount Kebne (Kebnekaise), which is 6,926 feet (2,111 metres) in elevation, and Mount Sarek (Sarektjåkkå), which rises 6,854 feet (2,089 metres), in the magnificent Sarek National Park. The interior of southern Sweden, Småland, is a wooded upland with elevations of 980 to 1,300 feet (300 to 400 metres). A region of poor and stony soils, Småland has been cultivated through the ages with some difficulty, as evidenced by the enormous mounds of stone cleared from the land. More recently the area has been characterized by flourishing small factories. Except for a stretch of scenic “high coast,” the Bothnian coastal plain is low-lying and stretches from Norrland into Svealand. Most of the fairly level surface of eastern Svealand and northern Götaland was pressed below sea level by glaciers, leaving a landscape of fragmented bedrock, fertile clayey plains, numerous lakes, and sandy ridges. Today these are intermingled with mixed forests and farmland. Sweden’s landscape changes from the hills of Småland to the fertile plains of Skåne, which is physiographically and economically more similar to Denmark than to the rest of Sweden. This is Sweden’s oldest settled and most densely populated agricultural area. The Swedish coastline is typically rocky, with hundreds of small, sometimes wooded islands. Ground by glacial ice in the same direction, they have a common rounded shape. This type of coast, known as skärgård, is found in both the east and the west, especially around Stockholm and Gothenburg. Off the southern coast in the Baltic, the large, flat islands of Öland and Gotland are outcropping layers of sandstone and limestone. Drainage The country’s chief rivers originate in the mountains of Norrland, mostly flowing southeastward with many falls and rapids and emptying into the Gulf of Bothnia or the Baltic Sea. The longest, however, is the Klar-Göta River, which rises in Norway and flows 447 miles (719 km), reaching Lake Väner (Vänern) and continuing southward out of the lake’s southern end to the North Sea; along its southernmost course are the famous falls of Trollhättan. The Muonio and Torne rivers form the frontier with Finland, and in the south the Dal River marks the transition to Svealand. The rivers, except in the far north, where they are protected, are sources of hydroelectric power. In Svealand are Sweden’s largest lakes, including Lakes Väner, 2,181 square miles (5,650 square km); Vätter (Vättern), 738 square miles (1,911 square km); and Mälar (Mälaren), 440 square miles (1,139 square km). The shores of Lakes Siljan and Storsjön and the river valleys support agriculture. Soils The dominant soil of Sweden is till, formed under glacial ice. Till that comes from the archaic bedrock of granites and gneisses forms a poor soil, and forestry and polluted (acid) rain add to its acidification. On the other hand, small areas of clayey till from younger sedimentary limestone, scattered mainly in southern Sweden, form brown earth, providing agricultural soils of high fertility. In addition, vast areas of central Sweden are covered by heavy and fertile sea-bottom clays raised out of the sea by postglacial land uplift. One-fifth of the country, especially in rainy southwestern Sweden and the cold far north, is covered by marshland and peat. https://www.britannica.com/place/Sweden

2025/06/06

Introducing Sweden

Start exploring Sweden with Lonely Planet’s video guide to getting around, when to go and the top things to do while you're there. For more travel tips, head to https://www.lonelyplanet.com/sweden

2025/06/05

Feast of the Constitution of Kingdom of Denmark

Denmark, country occupying the peninsula of Jutland (Jylland), which extends northward from the centre of continental western Europe, and an archipelago of more than 400 islands to the east of the peninsula. Jutland makes up more than two-thirds of the country’s total land area; at its northern tip is the island of Vendsyssel-Thy (1,809 square miles [4,685 square km]), separated from the mainland by the Lim Fjord. The largest of the country’s islands are Zealand (Sjælland; 2,715 square miles [7,031 square km]), Vendsyssel-Thy, and Funen (Fyn; 1,152 square miles [2,984 square km]). Along with Norway and Sweden, Denmark is a part of the northern European region known as Scandinavia. The country’s capital, Copenhagen (København), is located primarily on Zealand; the second largest city, Århus, is the major urban centre of Jutland. Though small in territory and population, Denmark has nonetheless played a notable role in European history. In prehistoric times, Danes and other Scandinavians reconfigured European society when the Vikings undertook marauding, trading, and colonizing expeditions. During the Middle Ages, the Danish crown dominated northwestern Europe through the power of the Kalmar Union. In later centuries, shaped by geographic conditions favouring maritime industries, Denmark established trading alliances throughout northern and western Europe and beyond, particularly with Great Britain and the United States. Making an important contribution to world culture, Denmark also developed humane governmental institutions and cooperative, nonviolent approaches to problem solving. This article covers principally the land and people of continental Denmark. However, the Kingdom of Denmark also encompasses the Faroe Islands and the island of Greenland, both located in the North Atlantic Ocean. Each area is distinctive in history, language, and culture. Home rule was granted to the Faroes in 1948 and to Greenland in 1979, though foreign policy and defense remain under Danish control. Land Denmark is attached directly to continental Europe at Jutland’s 42-mile (68-km) boundary with Germany. Other than this connection, all the frontiers with surrounding countries are maritime, including that with the United Kingdom to the west across the North Sea. Norway and Sweden lie to the north, separated from Denmark by sea lanes linking the North Sea to the Baltic Sea. From west to east, these passages are called the Skagerrak, the Kattegat, and The Sound (Øresund). Eastward in the Baltic Sea lies the Danish island of Bornholm. Relief Denmark proper is a lowland area that lies, on average, not more than 100 feet (30 metres) above sea level. The country’s highest point, reaching only 568 feet (173 metres), is Yding Forest Hill (Yding Skovhøj) in east-central Jutland. The basic contours of the Danish landscape were shaped at the end of the Pleistocene Epoch (i.e., about 2,600,000 to 11,700 years ago) by the so-called Weichsel glaciation. This great glacial mass withdrew temporarily during several warmer interstadial periods, but it repeatedly returned to cover the land until it retreated to the Arctic north for the last time about 10,000 years ago. As a result, the barren layers of chalk and limestone that earlier constituted the land surface acquired a covering of soil that built up as the Weichsel retreated, forming low, hilly, and generally fertile moraines that diversify the otherwise flat landscape. A scenic boundary representing the extreme limit reached by the Scandinavian and Baltic ice sheets runs from Nissum Fjord on the western coast of Jutland eastward toward Viborg, from there swinging sharply south down the spine of the peninsula toward Åbenrå and the German city of Flensburg, just beyond the Danish frontier. The ice front is clearly marked in the contrast between the flat western Jutland region, composed of sands and gravels strewn by meltwaters that poured west from the shrinking ice sheet, and the fertile loam plains and hills of eastern and northern Denmark, which become markedly sandier toward the prehistoric ice front. (See also Scandinavian Ice Sheet.) In northern Jutland, where the long Lim Fjord separates the northern tip (Vendsyssel-Thy) from the rest of the peninsula, there are numerous flat areas of sand and gravel, some of which became stagnant bogs. Burials and ritual deposits interred in these bogs in antiquity—especially during the Bronze Age and the Iron Age—have been recovered by archaeologists. In more recent centuries these bogs were a valued source of peat for fuel. In the 20th century they were drained to serve as grazing areas for livestock. In places along the northern and southwestern coasts of Jutland, salt marshes were formed by the evaporation of an inland sea that existed during the late Permian Epoch (approximately 260 to 250 million years ago). Senonian chalk, deposited about 100 million years ago, is exposed in southeastern Zealand, at the base of Stevns Cliff (Stevns Klint) and Møns Cliff (Møns Klint), and at Bulbjerg, in northwestern Jutland. Younger limestone of the Danian Age (about 65 million years old) is quarried in southeastern Zealand. On Bornholm, outcroppings reveal close affinities with geologic formations in southern Sweden. Precambrian granites more than 570 million years old—among the oldest on the Earth’s surface—are exposed across extensive areas on the northern half of the island. On the southern half, sandstone and shales of the Cambrian Period (about 540 to 490 million years ago) overlie the older granites. Drainage The longest river in Denmark is the Gudenå. It flows a distance of 98 miles (158 km) from its source just northwest of Tørring, in east-central Jutland, through the Silkeborg Lakes (Silkeborg Langsø) and then northeast to empty in the Randers Fjord on the east coast. There are many small lakes; the largest is Arresø on Zealand. Large lagoons have formed behind the coastal dunes in the west, such as at the Ringkøbing and Nissum fjords. More … Score: https://www.britannica.com/place/Denmark

2025/06/05