1.
Scots language
–
Scots is the Germanic language variety spoken in Lowland Scotland and parts of Ulster. It is sometimes called Lowland Scots to distinguish it from Scottish Gaelic, the Celtic language which was restricted to most of the Highlands. The language developed during the Middle English period as a distinct entity, although a number of paradigms for distinguishing between languages and dialects do exist, these often render contradictory results. Broad Scots is at one end of a linguistic continuum. Scots is often regarded as one of the ancient varieties of English, alternatively, Scots is sometimes treated as a distinct Germanic language, in the way Norwegian is closely linked to, yet distinct from, Danish. In the 2011 Scottish census, a question on Scots language ability was featured, native speakers sometimes refer to their vernacular as braid Scots or use a dialect name such as the Doric, or the Buchan Claik. The old-fashioned Scotch, an English loan, occurs occasionally, especially in Northern Ireland, the term Lallans, a variant of the Modern Scots word lawlands, is also used, though this is more often taken to mean the Lallans literary form. Scots in Ireland is known in circles as Ulster-Scots or Ullans. Scots is a contraction of Scottis, the Older Scots and northern version of late Old English Scottisc, before the end of the 15th century, English speech in Scotland was known as English, whereas Scottish referred to Gaelic. From 1495 the term Scottis was increasingly used to refer to the Lowland vernacular and Erse, meaning Irish, the Gaelic of Scotland is now usually called Scottish Gaelic. Northumbrian Old English had been established in what is now southeastern Scotland as far as the River Forth by the seventh century and it remained largely confined to this area until the thirteenth century, continuing in common use while Gaelic was the language of the Scottish court. Scots also includes loan words resulting from contact with Gaelic, Early medieval legal documents include a body of Gaelic legal and administrative loans. Contemporary Gaelic loans are mainly for geographical and cultural features, such as ceilidh, loch, from the thirteenth century Early Scots spread further into Scotland via the burghs, proto-urban institutions which were first established by King David I. The growth in prestige of Early Scots in the century. By the sixteenth century Middle Scots had established orthographic and literary norms largely independent of those developing in England, from 1610 to the 1690s during the Plantation of Ulster large numbers of Scots-speaking Lowlanders, some 200,000, settled there. In the core areas of Scots settlement, Scots outnumbered English settlers by five or six to one, Modern Scots is used to describe the language after 1700 when southern Modern English was generally adopted as the literary language though Scots remained the vernacular. In Scotland, Scots is spoken in the Scottish Lowlands, the Northern Isles, Caithness, Arran, in Ulster it is spoken in the Counties of Down, Antrim, Londonderry and Donegal. Dialects include Insular Scots, Northern Scots, Central Scots, Southern Scots, many speakers are either diglossic and/or able to code-switch along the continuum depending on the situation in which they find themselves
2.
Welsh language
–
Welsh is a member of the Brittonic branch of the Celtic languages. It is spoken natively in Wales, by some in England, historically it has also been known in English as the British tongue, Cambrian, Cambric and Cymric. The United Kingdom Census 2011 counted 3.1 million residents of Wales, 27% of whom had been born outside Wales, and 73% of whom reported having no Welsh language skills. Of residents of Wales aged three and over, 19% reported being able to speak Welsh, and 77% of these were able to speak, read and this can be compared with the 2001 Census, in which 20. 8% of the population reported being able to speak Welsh. 787,854 of residents in Wales aged three and over had one or more skills in Welsh, in surveys carried out between 2004 and 2006, 57% of Welsh speakers described themselves as fluent in the written language. An estimated 110,000 to 150,000 people speak Welsh in England, Welsh emerged in the 6th century from Common Brittonic, the common ancestor of Welsh, Breton, Cornish and the extinct language known as Cumbric. The Middle Welsh period is considered to have lasted from then until the 14th century, when the Modern Welsh period began, the name Welsh originated as an exonym given to its speakers by the Anglo-Saxons, meaning foreign speech. The native term for the language is Cymraeg, and for the name of the country of Wales it is Cymru, Welsh evolved from Common Brittonic, the Celtic language spoken by the ancient Celtic Britons. Classified as Insular Celtic, the British language probably arrived in Britain during the Bronze Age or Iron Age and was spoken throughout the island south of the Firth of Forth. During the Early Middle Ages the British language began to fragment due to increased dialect differentiation, evolving into Welsh and it is not clear when Welsh became distinct. Kenneth H. Jackson suggested that the evolution in syllabic structure and sound pattern was complete by around 550, Jackson, however, believed that the two varieties were already distinct by that time. The earliest Welsh poetry – that attributed to the Cynfeirdd or Early Poets – is generally considered to date to the Primitive Welsh period. However, much of this poetry was composed in the Hen Ogledd, raising further questions about the dating of the material. An 8th century inscription in Tywyn shows the language already dropping inflections in the declension of nouns, the next main period, somewhat better attested, is Old Welsh, poetry from both Wales and Scotland has been preserved in this form of the language. Both the works of Aneirin and the Book of Taliesin were in this era, Middle Welsh is the label attached to the Welsh of the 12th to 14th centuries, of which much more remains than for any earlier period. This is the language of all surviving early manuscripts of the Mabinogion. It is also the language of the existing Welsh law manuscripts, Middle Welsh is reasonably intelligible, albeit with some work, to a modern-day Welsh speaker. The famous cleric Gerald of Wales tells, in his Descriptio Cambriae, during one of the Kings many raids in the 12th century, Henry asked an old man of Pencader, Carmarthenshire whether the Welsh people could resist his army
3.
Cornish language
–
Cornish is a Southwestern Brittonic Celtic language native to Cornwall. The language has undergone a revival in recent decades and is considered to be an important part of Cornish identity, culture and heritage. It is a minority language of the United Kingdom, protected under the European Charter for Regional or Minority Languages. Along with Welsh and Breton, Cornish is descended directly from the Common Brittonic language spoken throughout much of Britain before the English language came to dominate. A process to revive the language was begun in the early 20th century, in 2010 UNESCO announced that its former classification of the language as extinct was no longer accurate. Since the revival of the language, many Cornish textbooks and works of literature have been published, recent developments include Cornish music, independent films, and childrens books. A small number of people in Cornwall have been brought up to be native speakers. The first Cornish language crèche opened in 2010, Cornish is one of the Brittonic languages, which constitute a branch of the Insular Celtic section of the Celtic language family. Brittonic also includes Welsh, Breton and the Cumbric language, the last is extinct, scottish Gaelic, Irish and Manx are part of the separate Goidelic branch of Insular Celtic. Cornish evolved from the Common Brittonic spoken throughout Britain south of the Firth of Forth during the British Iron Age, as a result of westward Anglo-Saxon expansion, the Britons of the southwest were separated from those in modern-day Wales and Cumbria. Some scholars have proposed that this took place after the Battle of Deorham in about 577. The area controlled by the southwestern Britons was progressively reduced by the expansion of Wessex over the few centuries. The earliest written record of the Cornish language comes from period, a 9th-century gloss in a Latin manuscript of De Consolatione Philosophiae by Boethius. The phrase means it hated the gloomy places, a much more substantial survival from Old Cornish is a Cornish-Latin glossary containing translations of around 300 words. The manuscript was thought to be in Old Welsh until the 1700s when it was identified as Cornish. The Cornish language continued to flourish well through the Middle Cornish period, reaching a peak of about 39,000 speakers in the 13th century and this period provided the bulk of traditional Cornish literature, which was used to reconstruct the language during its revival. Most important is the Ordinalia, a cycle of three plays, Origo Mundi, Passio Christi and Resurrexio Domini. Together these provide about 20,000 lines of text, various plays were written by the canons of Glasney College, intended to educate the Cornish people about the Bible and the Celtic saints
4.
Irish language
–
Irish, also referred to as Gaelic or Irish Gaelic, is a Goidelic language of the Indo-European language family originating in Ireland and historically spoken by the Irish people. Irish is spoken as a first language by a minority of Irish people. Irish enjoys constitutional status as the national and first official language of the Republic of Ireland and it is also among the official languages of the European Union. The public body Foras na Gaeilge is responsible for the promotion of the language throughout the island of Ireland and it has the oldest vernacular literature in Western Europe. The fate of the language was influenced by the power of the English state in Ireland. Elizabethan officials viewed the use of Irish unfavourably, as being a threat to all things English in Ireland and its decline began under English rule in the 17th century. In the latter part of the 19th century, there was a decrease in the number of speakers. Irish-speaking areas were hit especially hard, by the end of British rule, the language was spoken by less than 15% of the national population. Since then, Irish speakers have been in the minority, efforts have been made by the state, individuals and organisations to preserve, promote and revive the language, but with mixed results. Around the turn of the 21st century, estimates of native speakers ranged from 20,000 to 80,000 people. In the 2011 Census, these numbers had increased to 94,000 and 1.3 million, there are several thousand Irish speakers in Northern Ireland. It has been estimated that the active Irish-language scene probably comprises 5 to 10 per cent of Irelands population, there has been a significant increase in the number of urban Irish speakers, particularly in Dublin. In Gaeltacht areas, however, there has been a decline of the use of Irish. Údarás na Gaeltachta predicted that, by 2025, Irish will no longer be the language in any of the designated Gaeltacht areas. Survey data suggest that most Irish people think highly of Irish as a marker of identity. It has also argued that newer urban groups of Irish speakers are a disruptive force in this respect. In An Caighdeán Oifigiúil the name of the language is Gaeilge, before the spelling reform of 1948, this form was spelled Gaedhilge, originally this was the genitive of Gaedhealg, the form used in Classical Irish. Older spellings of this include Gaoidhealg in Classical Irish and Goídelc in Old Irish, the modern spelling results from the deletion of the silent dh in the middle of Gaedhilge, whereas Goidelic languages, used to refer to the language family including Irish, comes from Old Irish
5.
Scottish Gaelic
–
Scottish Gaelic or Scots Gaelic, sometimes also referred to as Gaelic, is a Celtic language native to Scotland. A member of the Goidelic branch of the Celtic languages, Scottish Gaelic, like Modern Irish and Manx, developed out of Middle Irish. The 2011 census of Scotland showed that a total of 57,375 people in Scotland could speak Gaelic at that time, the census results indicate a decline of 1,275 Gaelic speakers from 2001. A total of 87,056 people in 2011 reported having some facility with Gaelic compared to 93,282 people in 2001, only about half of speakers were fully literate in the language. Nevertheless, revival efforts exist and the number of speakers of the language under age 20 has increased, Scottish Gaelic is neither an official language of the European Union nor the United Kingdom. Outside Scotland, a group of dialects collectively known as Canadian Gaelic are spoken in parts of Atlantic Canada, mainly Nova Scotia and Prince Edward Island. In the 2011 census, there were 7,195 total speakers of Gaelic languages in Canada, with 1,365 in Nova Scotia and Prince Edward Island where the responses mainly refer to Scottish Gaelic. About 2,320 Canadians in 2011 also claimed Gaelic languages as their mother tongue, with over 300 in Nova Scotia, aside from Scottish Gaelic, the language may also be referred to simply as Gaelic. In Scotland, the word Gaelic in reference to Scottish Gaelic specifically is pronounced, outside Ireland and Great Britain, Gaelic may refer to the Irish language. Scottish Gaelic should not be confused with Scots, the Middle English-derived language varieties which had come to be spoken in most of the Lowlands of Scotland by the modern era. Prior to the 15th century, these dialects were known as Inglis by its own speakers, from the late 15th century, however, it became increasingly common for such speakers to refer to Scottish Gaelic as Erse and the Lowland vernacular as Scottis. Today, Scottish Gaelic is recognised as a language from Irish. Gaelic in Scotland was mostly confined to Dál Riata until the 8th century, when it began expanding into Pictish areas north of the Firth of Forth, by 900, Pictish appears to have become extinct, completely replaced by Gaelic. An exception might be made for the Northern Isles, however, however, though the Pictish language did not disappear suddenly, a process of Gaelicisation was clearly underway during the reigns of Caustantín and his successors. By a certain point, probably during the 11th century, all the inhabitants of Alba had become fully Gaelicised Scots, by the 10th century, Gaelic had become the dominant language throughout northern and western Scotland, the Gaelo-Pictic Kingdom of Alba. Its spread to southern Scotland, was even and totalizing. Place name analysis suggests dense usage of Gaelic in Galloway and adjoining areas to the north and west as well as in West Lothian, less dense usage is suggested for north Ayrshire, Renfrewshire, the Clyde Valley and eastern Dumfriesshire. In south-eastern Scotland, there is no evidence that Gaelic was ever widely spoken, the area shifted from Cumbric to Old English during its long incorporation into the Anglo-Saxon Kingdom of Northumbria
6.
French language
–
French is a Romance language of the Indo-European family. It descended from the Vulgar Latin of the Roman Empire, as did all Romance languages, French has evolved from Gallo-Romance, the spoken Latin in Gaul, and more specifically in Northern Gaul. Its closest relatives are the other langues doïl—languages historically spoken in northern France and in southern Belgium, French was also influenced by native Celtic languages of Northern Roman Gaul like Gallia Belgica and by the Frankish language of the post-Roman Frankish invaders. Today, owing to Frances past overseas expansion, there are numerous French-based creole languages, a French-speaking person or nation may be referred to as Francophone in both English and French. French is a language in 29 countries, most of which are members of la francophonie. As of 2015, 40% of the population is in Europe, 35% in sub-Saharan Africa, 15% in North Africa and the Middle East, 8% in the Americas. French is the fourth-most widely spoken mother tongue in the European Union, 1/5 of Europeans who do not have French as a mother tongue speak French as a second language. As a result of French and Belgian colonialism from the 17th and 18th century onward, French was introduced to new territories in the Americas, Africa, most second-language speakers reside in Francophone Africa, in particular Gabon, Algeria, Mauritius, Senegal and Ivory Coast. In 2015, French was estimated to have 77 to 110 million native speakers, approximately 274 million people are able to speak the language. The Organisation internationale de la Francophonie estimates 700 million by 2050, in 2011, Bloomberg Businessweek ranked French the third most useful language for business, after English and Standard Mandarin Chinese. Under the Constitution of France, French has been the language of the Republic since 1992. France mandates the use of French in official government publications, public education except in specific cases, French is one of the four official languages of Switzerland and is spoken in the western part of Switzerland called Romandie, of which Geneva is the largest city. French is the language of about 23% of the Swiss population. French is also a language of Luxembourg, Monaco, and Aosta Valley, while French dialects remain spoken by minorities on the Channel Islands. A plurality of the worlds French-speaking population lives in Africa and this number does not include the people living in non-Francophone African countries who have learned French as a foreign language. Due to the rise of French in Africa, the total French-speaking population worldwide is expected to reach 700 million people in 2050, French is the fastest growing language on the continent. French is mostly a language in Africa, but it has become a first language in some urban areas, such as the region of Abidjan, Ivory Coast and in Libreville. There is not a single African French, but multiple forms that diverged through contact with various indigenous African languages, sub-Saharan Africa is the region where the French language is most likely to expand, because of the expansion of education and rapid population growth
7.
Shetland
–
Shetland /ˈʃɛtlənd/, also called the Shetland Islands, is a subarctic archipelago that lies northeast of the island of Great Britain and forms part of Scotland, United Kingdom. The islands lie some 80 km to the northeast of Orkney and 280 km southeast of the Faroe Islands, the total area is 1,466 km2 and the population totalled 23,210 in 2012. The largest island, known simply as Mainland, has an area of 967 km2, making it the third-largest Scottish island, there are an additional 15 inhabited islands. The archipelago has a climate, a complex geology, a rugged coastline and many low. Humans have lived in Shetland since the Mesolithic period, and the earliest written references to the date back to Roman times. The early historic period was dominated by Scandinavian influences, especially Norway, when Scotland became part of the Kingdom of Great Britain in 1707, trade with northern Europe decreased. Fishing has continued to be an important aspect of the economy up to the present day, the discovery of North Sea oil in the 1970s significantly boosted Shetland economy, employment and public sector revenues. The local way of life reflects the Scots and Norse heritage of the isles including the Up Helly Aa fire festival, the islands have produced a variety of writers of prose and poetry, often in Shetland dialect. There are numerous areas set aside to protect the fauna and flora. The Shetland pony and Shetland Sheepdog are two well known Shetland animal breeds, other distinguished local breeds include the Shetland sheep, cow, goose, and duck. The Shetland pig, or grice, has been extinct since approximately 1930, the islands motto, which appears on the Councils coat of arms, is Með lögum skal land byggja. This Icelandic phrase is taken from the Danish 1241 Basic Law, Codex Holmiensis, and is mentioned in Njáls saga. The name of Shetland is derived from the Old Norse words, hjalt, in AD43 and 77 the Roman authors Pomponius Mela and Pliny the Elder referred to the seven islands they call Haemodae and Acmodae respectively, both of which are assumed to be Shetland. Another possible early reference to the islands is Tacitus report in AD98, after describing the discovery and conquest of Orkney. In early Irish literature, Shetland is referred to as Inse Catt—the Isles of Cats, the Cat tribe also occupied parts of the northern Scottish mainland and their name can be found in Caithness, and in the Gaelic name for Sutherland. It is possible that the Pictish cat sound forms part of this Norse name and it then became Hjaltland in the 16th century. As Norn was gradually replaced by English in the form of the Shetland dialect which shares similarities with Scots English. The initial letter is the Middle Scots letter, yogh, the pronunciation of which is almost identical to the original Norn sound, /hj/
8.
Channel Islands
–
The Channel Islands are an archipelago in the English Channel, off the French coast of Normandy. They are considered the remnants of the Duchy of Normandy, and although they are not part of the United Kingdom, it is responsible for the defence, the Crown dependencies are not members of the Commonwealth of Nations nor of the European Union. They have a population of about 168,000. The total area of the islands is 198 km2, the two bailiwicks have been administered separately since the late 13th century, each has its own independent laws, elections, and representative bodies. Any institution common to both is the rather than the rule. The Bailiwick of Guernsey is divided into three jurisdictions – Guernsey, Alderney and Sark – each with its own legislature, the term Channel Islands began to be used around 1830, possibly first by the Royal Navy as a collective name for the islands. The permanently inhabited islands of the Channel Islands are, Jersey Guernsey Alderney Sark Herm Jethou Brecqhou There are also several uninhabited islets and they are an incorporated part of the commune of Granville. While they are popular with visitors from France, Channel Islanders rarely visit them as there are no transport links from the other islands. Chausey is referred to as an Île normande, Îles Normandes and Archipel Normand have also, historically, been used in Channel Island French to refer to the islands as a whole. The lowest point is the Atlantic Ocean, the earliest evidence of human occupation of the Channel Islands has been dated to 250,000 years ago when they were attached to the landmass of continental Europe. The islands became detached by rising sea levels in the Neolithic period, hoards of Armorican coins have been excavated, providing evidence of trade and contact in the Iron Age period. Evidence for Roman settlement is sparse, although evidently the islands were visited by Roman officials, the Roman name for the Channel Islands was I. Lenuri and is included in the Peutinger Table The traditional Latin names used for the islands derive from the Antonine Itinerary, gallo-Roman culture was adopted to an unknown extent in the islands. In the sixth century, Christian missionaries visited the islands, samson of Dol, Helier, Marculf and Magloire are among saints associated with the islands. In the sixth century, they were included in the diocese of Coutances where they remained until reformation. The islands were inhabited by Britons, who also inhabited Wales, south west England, from the beginning of the ninth century, Norse raiders appeared on the coasts. Norse settlement succeeded initial attacks, and it is from this period that many names of Norse origin appear. In 933, the islands were granted to William I Longsword by Raoul King of Western Francia, in 1066, William II of Normandy invaded and conquered England, becoming William I of England, also known as William the Conqueror
9.
Europe
–
Europe is a continent that comprises the westernmost part of Eurasia. Europe is bordered by the Arctic Ocean to the north, the Atlantic Ocean to the west, yet the non-oceanic borders of Europe—a concept dating back to classical antiquity—are arbitrary. Europe covers about 10,180,000 square kilometres, or 2% of the Earths surface, politically, Europe is divided into about fifty sovereign states of which the Russian Federation is the largest and most populous, spanning 39% of the continent and comprising 15% of its population. Europe had a population of about 740 million as of 2015. Further from the sea, seasonal differences are more noticeable than close to the coast, Europe, in particular ancient Greece, was the birthplace of Western civilization. The fall of the Western Roman Empire, during the period, marked the end of ancient history. Renaissance humanism, exploration, art, and science led to the modern era, from the Age of Discovery onwards, Europe played a predominant role in global affairs. Between the 16th and 20th centuries, European powers controlled at times the Americas, most of Africa, Oceania. The Industrial Revolution, which began in Great Britain at the end of the 18th century, gave rise to economic, cultural, and social change in Western Europe. During the Cold War, Europe was divided along the Iron Curtain between NATO in the west and the Warsaw Pact in the east, until the revolutions of 1989 and fall of the Berlin Wall. In 1955, the Council of Europe was formed following a speech by Sir Winston Churchill and it includes all states except for Belarus, Kazakhstan and Vatican City. Further European integration by some states led to the formation of the European Union, the EU originated in Western Europe but has been expanding eastward since the fall of the Soviet Union in 1991. The European Anthem is Ode to Joy and states celebrate peace, in classical Greek mythology, Europa is the name of either a Phoenician princess or of a queen of Crete. The name contains the elements εὐρύς, wide, broad and ὤψ eye, broad has been an epithet of Earth herself in the reconstructed Proto-Indo-European religion and the poetry devoted to it. For the second part also the divine attributes of grey-eyed Athena or ox-eyed Hera. The same naming motive according to cartographic convention appears in Greek Ανατολή, Martin Litchfield West stated that phonologically, the match between Europas name and any form of the Semitic word is very poor. Next to these there is also a Proto-Indo-European root *h1regʷos, meaning darkness. Most major world languages use words derived from Eurṓpē or Europa to refer to the continent, in some Turkic languages the originally Persian name Frangistan is used casually in referring to much of Europe, besides official names such as Avrupa or Evropa
10.
Geographic coordinate system
–
A geographic coordinate system is a coordinate system used in geography that enables every location on Earth to be specified by a set of numbers, letters or symbols. The coordinates are chosen such that one of the numbers represents a vertical position. A common choice of coordinates is latitude, longitude and elevation, to specify a location on a two-dimensional map requires a map projection. The invention of a coordinate system is generally credited to Eratosthenes of Cyrene. Ptolemy credited him with the adoption of longitude and latitude. Ptolemys 2nd-century Geography used the prime meridian but measured latitude from the equator instead. Mathematical cartography resumed in Europe following Maximus Planudes recovery of Ptolemys text a little before 1300, in 1884, the United States hosted the International Meridian Conference, attended by representatives from twenty-five nations. Twenty-two of them agreed to adopt the longitude of the Royal Observatory in Greenwich, the Dominican Republic voted against the motion, while France and Brazil abstained. France adopted Greenwich Mean Time in place of local determinations by the Paris Observatory in 1911, the latitude of a point on Earths surface is the angle between the equatorial plane and the straight line that passes through that point and through the center of the Earth. Lines joining points of the same latitude trace circles on the surface of Earth called parallels, as they are parallel to the equator, the north pole is 90° N, the south pole is 90° S. The 0° parallel of latitude is designated the equator, the plane of all geographic coordinate systems. The equator divides the globe into Northern and Southern Hemispheres, the longitude of a point on Earths surface is the angle east or west of a reference meridian to another meridian that passes through that point. All meridians are halves of great ellipses, which converge at the north and south poles, the prime meridian determines the proper Eastern and Western Hemispheres, although maps often divide these hemispheres further west in order to keep the Old World on a single side. The antipodal meridian of Greenwich is both 180°W and 180°E, the combination of these two components specifies the position of any location on the surface of Earth, without consideration of altitude or depth. The grid formed by lines of latitude and longitude is known as a graticule, the origin/zero point of this system is located in the Gulf of Guinea about 625 km south of Tema, Ghana. To completely specify a location of a feature on, in, or above Earth. Earth is not a sphere, but a shape approximating a biaxial ellipsoid. It is nearly spherical, but has an equatorial bulge making the radius at the equator about 0. 3% larger than the radius measured through the poles, the shorter axis approximately coincides with the axis of rotation
11.
Atlantic Ocean
–
The Atlantic Ocean is the second largest of the worlds oceans with a total area of about 106,460,000 square kilometres. It covers approximately 20 percent of the Earths surface and about 29 percent of its surface area. It separates the Old World from the New World, the Atlantic Ocean occupies an elongated, S-shaped basin extending longitudinally between Eurasia and Africa to the east, and the Americas to the west. The Equatorial Counter Current subdivides it into the North Atlantic Ocean, in contrast, the term Atlantic originally referred specifically to the Atlas Mountains in Morocco and the sea off the Strait of Gibraltar and the North African coast. The Greek word thalassa has been reused by scientists for the huge Panthalassa ocean that surrounded the supercontinent Pangaea hundreds of years ago. The term Aethiopian Ocean, derived from Ancient Ethiopia, was applied to the Southern Atlantic as late as the mid-19th century, many Irish or British people refer to the United States and Canada as across the pond, and vice versa. The Black Atlantic refers to the role of ocean in shaping black peoples history. Irish migration to the US is meant when the term The Green Atlantic is used, the term Red Atlantic has been used in reference to the Marxian concept of an Atlantic working class, as well as to the Atlantic experience of indigenous Americans. Correspondingly, the extent and number of oceans and seas varies, the Atlantic Ocean is bounded on the west by North and South America. It connects to the Arctic Ocean through the Denmark Strait, Greenland Sea, Norwegian Sea, to the east, the boundaries of the ocean proper are Europe, the Strait of Gibraltar and Africa. In the southeast, the Atlantic merges into the Indian Ocean, the 20° East meridian, running south from Cape Agulhas to Antarctica defines its border. In the 1953 definition it extends south to Antarctica, while in later maps it is bounded at the 60° parallel by the Southern Ocean, the Atlantic has irregular coasts indented by numerous bays, gulfs, and seas. Including these marginal seas the coast line of the Atlantic measures 111,866 km compared to 135,663 km for the Pacific. Including its marginal seas, the Atlantic covers an area of 106,460,000 km2 or 23. 5% of the ocean and has a volume of 310,410,900 km3 or 23. 3%. Excluding its marginal seas, the Atlantic covers 81,760,000 km2 and has a volume of 305,811,900 km3, the North Atlantic covers 41,490,000 km2 and the South Atlantic 40,270,000 km2. The average depth is 3,646 m and the maximum depth, the bathymetry of the Atlantic is dominated by a submarine mountain range called the Mid-Atlantic Ridge. It runs from 87°N or 300 km south of the North Pole to the subantarctic Bouvet Island at 42°S, the MAR divides the Atlantic longitudinally into two halves, in each of which a series of basins are delimited by secondary, transverse ridges. The MAR reaches above 2000 m along most of its length, the MAR is a barrier for bottom water, but at these two transform faults deep water currents can pass from one side to the other
12.
Ben Nevis
–
Ben Nevis is the highest mountain in the British Isles, located in Scotland. Standing at 1,345 metres above sea level, it is located at the end of the Grampian Mountains in the Lochaber area of the Scottish Highlands. The mountain is a destination, attracting an estimated 100,000 ascents a year. The 700-metre cliffs of the face are among the highest in Scotland, providing classic scrambles. They are also the locations in Scotland for ice climbing. The summit, which is the dome of an ancient volcano. The meteorological data collected during this period are still important for understanding Scottish mountain weather, C. T. R. Wilson was inspired to invent the cloud chamber after a period spent working at the observatory. Ben Nevis is an Anglicisation of the Scottish Gaelic name Beinn Nibheis, Beinn is the most common Gaelic word for mountain, Nibheis is variously understood, though the word is commonly translated as malicious or venomous. An alternative interpretation is that Beinn Nibheis derives from beinn nèamh-bhathais, from nèamh heavens, clouds, one translation would therefore be the mountain with its head in the clouds, though mountain of Heaven is also frequently given. As is common for many Scottish mountains, it is both to locals and visitors as simply the Ben. Ben Nevis forms a massif with its neighbour to the northeast, Càrn Mòr Dearg, both mountains are among the nine in Scotland over 4,000 feet, Aonach Beag and Aonach Mòr are also on the Nevis massif. The hut is situated just above the confluence of Allt a Mhuilinn, in addition to the main 1, 345-metre summit, Ben Nevis has two subsidiary tops listed in Munros Tables, both of which are called Càrn Dearg. The higher of these, at 1,221 metres, is situated to the northwest, the other Càrn Dearg juts out into Glen Nevis on the mountains southwestern side. A lower hill, Meall an t-Suidhe, is located further west, forming a saddle with Ben Nevis which contains a small loch, the popular tourist path from Glen Nevis skirts the side of this hill before ascending Ben Neviss broad western flank. Ben Nevis is all that remains of a Devonian volcano that met an end in the Carboniferous period around 350 million years ago. Evidence near the summit shows light-coloured granite lies among dark basaltic lavas, the two lying side-by-side is evidence the huge volcano collapsed in on itself creating an explosion comparable to Thera or Krakatoa. The mountain is now all that remains of the inner dome of the volcano. Its form has been shaped by glaciation
13.
Bailiwick of Guernsey
–
Guernsey is a jurisdiction within the Bailiwick of Guernsey, a Crown dependency. The jurisdiction is not part of the United Kingdom, however, defence and most foreign relations are handled by the British Government. Taken together with the jurisdictions of Alderney and Sark it forms the Bailiwick of Guernsey. The two Bailiwicks of Guernsey and Jersey together form the geographical grouping known as the Channel Islands, the name Guernsey, as well as that of neighbouring Jersey, is of Old Norse origin. The second element of word, -ey, is the Old Norse for island, while the original root, guern, is of uncertain origin. Around 6000 BC, rising seas created the English Channel and separated the Norman promontories that became the bailiwicks of Guernsey and Jersey from continental Europe, neolithic farmers then settled on its coast and built the dolmens and menhirs found in the islands today. During their migration to Brittany, Britons occupied the Lenur islands including Sarnia or Lisia and Angia, travelling from the Kingdom of Gwent, Saint Sampson, later the abbot of Dol in Brittany, is credited with the introduction of Christianity to Guernsey. In 933 AD, the Cotentin Peninsula including Avranchin which included the islands, were placed by the French King Ranulf under the control of William I, the island of Guernsey and the other Channel Islands represent the last remnants of the medieval Duchy of Normandy. During the Middle Ages, the island was a haven for pirates that would use the technique to ground ships close to her waters. This intensified during the Hundred Years War, when, starting in 1339, the Guernsey Militia was operational in 1337 and would help defend the island for a further 600 years. In 1372, the island was invaded by Aragonese mercenaries under the command of Owain Lawgoch, Owain and his dark-haired mercenaries were later absorbed into Guernsey legend as invading fairies from across the sea. In the mid-16th century, the island was influenced by Calvinist reformers from Normandy, during the Marian persecutions, three women, the Guernsey Martyrs, were burned at the stake for their Protestant beliefs. During the English Civil War, Guernsey sided with the Parliamentarians, the allegiance was not total, however, there were a few Royalist uprisings in the southwest of the island, while Castle Cornet was occupied by the Governor, Sir Peter Osborne, and Royalist troops. In December 1651, with honours of war, Castle Cornet surrendered. By the beginning of the 18th century, Guernseys residents were starting to settle in North America, the threat of invasion by Napoleon prompted many defensive structures to be built at the end of that century. The 19th century saw an increase in the prosperity of the island, due to its success in the global maritime trade. During the First World War, about 3,000 island men served in the British Expeditionary Force, of these, about 1,000 served in the Royal Guernsey Light Infantry regiment formed from the Royal Guernsey Militia in 1916. For most of the Second World War, the Channel Islands were occupied by German troops, before the occupation, 80% of Guernsey children had been evacuated to England to live with relatives or strangers during the war
14.
Saint Peter Port
–
Saint Peter Port is the capital of Guernsey as well as the main port. The population in 2001 was 16,488, in Guernésiais and in French, historically the official language of Guernsey, the name of the town and its surrounding parish is St Pierre Port. The port distinguishes this parish from Saint Pierre Du Bois, as well as being a parish, St. Peter Port is a small town consisting mostly of steep narrow streets and steps on the overlooking slopes. It is known that a trading post/town has existed here since before Roman times, the postal code for addresses in this parish starts with GY1. People from St. Peter Port, were nicknamed les Villais or cllichards in Guernésiais, St. Peter Port is located on the east coast of Guernsey. It borders St. Sampson in the north, The Vale in the north-west, St. Andrew in the west and St. Martin in the south. On the seaward side it faces Herm to the east, across the Little Russel, the Bréhon Tower sits in the Little Russel between St. Peter Port and Herm. Relief The land in the north and by the harbour is low lying but in the south and this means that there are quite a few cliffs on the coast between Havelet and Fermain. They belong to Electoral district Saint Peter Port South, St. Peter Port has an English Isthmian League club, Guernsey F. C. who play at Footes Lane. The Guernsey Rugby Football Club also play at Footes Lane and compete in National League 3 London & SE, candie Gardens, an award-winning restored Victorian Garden features a statue of Victor Hugo. Cambridge Park is a park that includes a skate park. In 2014 the parish was a Gold & Category Winner in the RHS Britain in Bloom competition, followed in 2016 with another Gold medal. In the Guernsey general election,2016 in, St Peter Port South there was a 2,068 or 63% turnout to elect five Deputies St Peter Port North there was a 2,639 or 65% turnout to elect six Deputies
15.
Jersey
–
Jersey, officially the Bailiwick of Jersey, is a Crown dependency of the United Kingdom, ruled by the Crown in right of Jersey, off the coast of Normandy, France. Jersey was part of the Duchy of Normandy, whose dukes went on to become kings of England from 1066. After Normandy was lost by the kings of England in the 13th century, and the ducal title surrendered to France, Jersey, Jersey is a self-governing parliamentary democracy under a constitutional monarchy, with its own financial, legal and judicial systems, and the power of self-determination. The Lieutenant Governor on the island is the representative of the Queen. The island of Jersey is the largest of the Channel Islands, although the bailiwicks of Jersey and Guernsey are often referred to collectively as the Channel Islands, the Channel Islands are not a constitutional or political unit. Jersey has a relationship to the Crown from the other Crown dependencies of Guernsey. It is not part of the United Kingdom, and has an identity separate from that of the UK. The definition of United Kingdom in the British Nationality Act 1981 is interpreted as including the UK, Jersey is not fully part of the European Union but has a special relationship with it, notably being treated as within the European Community for the purposes of free trade in goods. The name Caesarea has been used as the Latin name for Jersey since William Camdens Britannia, the Latin name Caesarea was also applied to the colony of New Jersey as Nova Caesarea. Andium, Agna and Augia were used in antiquity, scholars variously surmise that Jersey and Jèrri derive from jarð or jarl, or perhaps a personal name, Geirr. The ending -ey denotes an island, Jersey history is influenced by its strategic location between the northern coast of France and the southern coast of England, the islands recorded history extends over a thousand years. La Cotte de St Brelade is a Palaeolithic site inhabited before rising sea levels transformed Jersey into an island, Jersey was a centre of Neolithic activity, as demonstrated by the concentration of dolmens. Evidence of Bronze Age and early Iron Age settlements can be found in locations around the island. In June 2012 it was announced what could be Europes largest hoard of Iron Age coins had been found in Grouville by two persons using metal detectors, the hoard may be worth up to £10 M. People had been searching for treasure for 30 years. It was reported that the hoard weighed about three quarters of a tonne and could contain up to 50,000 Roman and Celtic coins, in 2012 the same two men had found 60 Iron Age coins in the same area. Jersey was part of Neustria with the same Gallo-Frankish population as the continental mainland, Jersey was invaded by Vikings in the 9th century. In 933 it was annexed to the future Duchy of Normandy, together with the other Channel Islands, Cotentin and Avranchin, by William Longsword, count of Rouen and it became one of the Norman Islands
16.
Saint Helier
–
Saint Helier is one of the twelve parishes of Jersey, the largest of the Channel Islands in the English Channel. St Helier has a population of about 33,500, roughly 34. 2% of the population of Jersey. The greater part of St Helier is rural, the parish covers a surface area of 4.1 square miles, being 9% of the total land area of the Island. The parish arms are two crossed axes on a blue background, the blue symbolising the sea, and the axes symbolising the martyrdom of Helier at the hands of Saxon pirates in 555 AD. It is thought that the site of St Helier was settled at the time of the Roman control of Gaul, before land reclamation and port construction started, boats could be tied up to the churchyard wall on the seaward side. An Abbey of St Helier was founded in 1155 on LIslet, closed at the Reformation, the site of the abbey was fortified to create the castle that replaced Mont Orgueil as the Islands major fortress. The new Elizabeth Castle was named after the Queen by the Governor of Jersey 1600-1603, la Cohue stood on one side of the square, now rebuilt as the Royal Court and States Chamber. The market cross in the centre of the square was pulled down at the Reformation, george II gave £200 towards the construction of a new harbour - previously boats would be beached on a falling tide and unloaded by cart across the sands. Many of St Heliers road names and street names are bilingual English/French or English/Jèrriais, the names in the various languages are not usually translations, distinct naming traditions survive alongside each other. The Royal Square was also the scene of the Battle of Jersey on 6 January 1781, john Singleton Copleys epic painting The Death of Major Pierson captures an imaginative version of the scene. As harbour construction moved development seaward, a growth in population meant that marshland, settlement by English immigrants added quarters of colonial-style town houses to the traditional building stock. Continuing military threats from France spurred the construction of a fortress, Fort Regent, on the Mont de la Ville. This was the start of Jerseys agricultural prosperity in the 19th century, from the 1820s, peace with France and better communications by steamships and railways to coastal ports encouraged an influx of English-speaking residents. Speculative development covered the basin north of the central coastal strip as far as the hills within a period of about 40 years. In the second half of the 19th century, hundreds of trucks laden with potatoes and this prompted a programme of road-widening which swept away many of the ancient buildings of the town centre. Pressure for redevelopment has meant that few buildings remain in urban St Helier which date to before the 19th century. Pierre Le Sueur, reforming Constable of St Helier, was responsible for installing sewerage, an obelisk with fountain in the town centre was raised to his memory following his premature death in office from overwork. In the 1970s, a programme of pedestrianisation of the streets was undertaken
17.
Republic of Ireland
–
Ireland, also known as the Republic of Ireland, is a sovereign state in north-western Europe occupying about five-sixths of the island of Ireland. The capital and largest city is Dublin, which is located on the part of the island. The state shares its land border with Northern Ireland, a part of the United Kingdom. It is otherwise surrounded by the Atlantic Ocean, with the Celtic Sea to the south, Saint Georges Channel to the south-east, and it is a unitary, parliamentary republic. The head of government is the Taoiseach, who is elected by the Dáil and appointed by the President, the state was created as the Irish Free State in 1922 as a result of the Anglo-Irish Treaty. It was officially declared a republic in 1949, following the Republic of Ireland Act 1948, Ireland became a member of the United Nations in December 1955. It joined the European Economic Community, the predecessor of the European Union, after joining the EEC, Ireland enacted a series of liberal economic policies that resulted in rapid economic growth. The country achieved considerable prosperity between the years of 1995 and 2007, which known as the Celtic Tiger period. This was halted by a financial crisis that began in 2008. However, as the Irish economy was the fastest growing in the EU in 2015, Ireland is again quickly ascending league tables comparing wealth and prosperity internationally. For example, in 2015, Ireland was ranked as the joint sixth most developed country in the world by the United Nations Human Development Index and it also performs well in several national performance metrics, including freedom of the press, economic freedom and civil liberties. Ireland is a member of the European Union and is a member of the Council of Europe. The 1922 state, comprising 26 of the 32 counties of Ireland, was styled, the Constitution of Ireland, adopted in 1937, provides that the name of the State is Éire, or, in the English language, Ireland. Section 2 of the Republic of Ireland Act 1948 states, It is hereby declared that the description of the State shall be the Republic of Ireland. The 1948 Act does not name the state as Republic of Ireland, because to have done so would have put it in conflict with the Constitution. The government of the United Kingdom used the name Eire, and, from 1949, Republic of Ireland, for the state, as well as Ireland, Éire or the Republic of Ireland, the state is also referred to as the Republic, Southern Ireland or the South. In an Irish republican context it is referred to as the Free State or the 26 Counties. From the Act of Union on 1 January 1801, until 6 December 1922, during the Great Famine, from 1845 to 1849, the islands population of over 8 million fell by 30%
18.
Dublin
–
Dublin is the capital and largest city of Ireland. Dublin is in the province of Leinster on Irelands east coast, the city has an urban area population of 1,345,402. The population of the Greater Dublin Area, as of 2016, was 1,904,806 people, founded as a Viking settlement, the Kingdom of Dublin became Irelands principal city following the Norman invasion. The city expanded rapidly from the 17th century and was briefly the second largest city in the British Empire before the Acts of Union in 1800, following the partition of Ireland in 1922, Dublin became the capital of the Irish Free State, later renamed Ireland. Dublin is administered by a City Council, the city is listed by the Globalization and World Cities Research Network as a global city, with a ranking of Alpha-, which places it amongst the top thirty cities in the world. It is a historical and contemporary centre for education, the arts, administration, economy, the name Dublin comes from the Irish word Dubhlinn, early Classical Irish Dubhlind/Duibhlind, dubh /d̪uβ/, alt. /d̪uw/, alt /d̪u, / meaning black, dark, and lind /lʲiɲ pool and this tidal pool was located where the River Poddle entered the Liffey, on the site of the castle gardens at the rear of Dublin Castle. In Modern Irish the name is Duibhlinn, and Irish rhymes from Dublin County show that in Dublin Leinster Irish it was pronounced Duílinn /d̪ˠi, other localities in Ireland also bear the name Duibhlinn, variously anglicized as Devlin, Divlin and Difflin. Historically, scribes using the Gaelic script wrote bh with a dot over the b and those without knowledge of Irish omitted the dot, spelling the name as Dublin. Variations on the name are found in traditionally Irish-speaking areas of Scotland, such as An Linne Dhubh. It is now thought that the Viking settlement was preceded by a Christian ecclesiastical settlement known as Duibhlinn, beginning in the 9th and 10th century, there were two settlements where the modern city stands. Baile Átha Cliath, meaning town of the ford, is the common name for the city in modern Irish. Áth Cliath is a name referring to a fording point of the River Liffey near Father Mathew Bridge. Baile Átha Cliath was an early Christian monastery, believed to have been in the area of Aungier Street, there are other towns of the same name, such as Àth Cliath in East Ayrshire, Scotland, which is Anglicised as Hurlford. Although the area of Dublin Bay has been inhabited by humans since prehistoric times and he called the settlement Eblana polis. It is now thought that the Viking settlement was preceded by a Christian ecclesiastical settlement known as Duibhlinn, beginning in the 9th and 10th century, there were two settlements where the modern city stands. The subsequent Scandinavian settlement centred on the River Poddle, a tributary of the Liffey in an area now known as Wood Quay, the Dubhlinn was a small lake used to moor ships, the Poddle connected the lake with the Liffey. This lake was covered during the early 18th century as the city grew, the Dubhlinn lay where the Castle Garden is now located, opposite the Chester Beatty Library in Dublin Castle
19.
Isle of Man
–
The Isle of Man, also known simply as Mann, is a self-governing crown dependency in the Irish Sea between England and Northern Ireland. The head of state is Queen Elizabeth II, who holds the title of Lord of Mann, the Lord of Mann is represented by a Lieutenant Governor. Foreign relations and defence are the responsibility of the British Government, the island has been inhabited since before 6500 BC. Gaelic cultural influence began in the 5th century and the Manx language, in 627, Edwin of Northumbria conquered the Isle of Man along with most of Mercia. In the 9th century, Norsemen established the Kingdom of the Isles, magnus III, King of Norway, was also known as King of Mann and the Isles between 1099 and 1103. In 1266, the became part of Scotland under the Treaty of Perth. After a period of alternating rule by the kings of Scotland and England, the short form often used in English, Mann, is derived from the Manx Mannin, though sometimes the name is written as Man. The earliest recorded Manx form of the name is Manu or Mana, the Old Irish form of the name is Manau or Mano. Old Welsh records named it as Manaw, also reflected in Manaw Gododdin, the name for an ancient district in north Britain along the lower Firth of Forth. The oldest known reference to the calls it Mona, in Latin, in the 1st century CE, Pliny the Elder records it as Monapia or Monabia. Later Latin references have Mevania or Mænavia, and Eubonia or Eumonia by Irish writers and it is found in the Sagas of Icelanders as Mön. The name is cognate with the Welsh name of the island of Anglesey, Ynys Môn, usually derived from a Celtic word for mountain. The name was at least secondarily associated with that of Manannán mac Lir in Irish mythology, later, a Manannán is recorded as the first king of Mann in a Manx poem. The island was cut off from the islands around 8000 BC. The first residents were hunter gatherers and fishermen, examples of their tools are kept at the Manx Museum. There were also the local Ronaldsway and Bann cultures, during the Bronze Age, burial mounds became smaller. Bodies were put in stone-lined graves with ornamental containers, the Bronze Age burial mounds created long-lasting markers around the countryside. The ancient Romans knew of the island and called it Insula Manavia although it is whether they conquered the island
20.
Douglas, Isle of Man
–
Douglas is the capital and largest town of the Isle of Man, with a population of 27,938. It is located at the mouth of the River Douglas, the River Douglas forms part of the towns harbour and main commercial port. Douglas was a settlement until it grew rapidly as a result of links with the English port of Liverpool in the 18th century. The town is the Islands main hub for business, finance, legal services, shipping, transport, shopping, the annual Isle of Man TT motorcycle races start and finish in Douglas. In the absence of any data, the origins of the town may be revealed by analysis of the original street. Scholars agree that the name of the town derives from Early Celtic Duboglassio meaning black river and these may be references to the site of the later Nunnery, a little upstream from the port. This suggests that the origins of the nucleus were as a non-urban port. Current speculation links the buildings with the Irish Sea Herring fishery. Other forms of trade grew, and following the Revestment Act 1765, Douglas began to reap the benefits of trans-Atlantic trade. Legitimate merchants who rose to prominence over the period included the Murreys, the Moores, the towns later prosperity was facilitated by the low cost of living, and the favourable legal status enjoyed by English debtors and half-pay officers. The initial growth and development of the town owed much to its natural harbour, over the 18th century, the towns population rose from about 800 in 1710 to nearly 2,500 in 1784. Throughout the 19th century, the towns demographics followed the trends as the United Kingdom. The number of visitors grew from the early 19th century, and from around 1870 onwards. But there were increasingly unsanitary conditions, and poor quality housing, the open sewage, middens, and smell from the harbour at low tide all contributed to the towns uncleanliness. Douglas in the first half of the 19th century often suffered from the destitution of its population and the many epidemics, in particular cholera. However, an Act passed later that decade, which did not include opt-out clauses, was accepted, and in 1860, Douglas elected its first town council, which was predominantly middle class in its makeup. The Town Commissioners could tackle the problems with greater efficiency. The Commissioners also designed to alter the anachronistic architecture of Douglas, built during the era of fishing and trading, the proportion of the Manx population living in Douglas was also expanding, with 35% living there by 1891
21.
United Kingdom
–
The United Kingdom of Great Britain and Northern Ireland, commonly known as the United Kingdom or Britain, is a sovereign country in western Europe. Lying off the north-western coast of the European mainland, the United Kingdom includes the island of Great Britain, Northern Ireland is the only part of the United Kingdom that shares a land border with another sovereign state—the Republic of Ireland. The Irish Sea lies between Great Britain and Ireland, with an area of 242,500 square kilometres, the United Kingdom is the 78th-largest sovereign state in the world and the 11th-largest in Europe. It is also the 21st-most populous country, with an estimated 65.1 million inhabitants, together, this makes it the fourth-most densely populated country in the European Union. The United Kingdom is a monarchy with a parliamentary system of governance. The monarch is Queen Elizabeth II, who has reigned since 6 February 1952, other major urban areas in the United Kingdom include the regions of Birmingham, Leeds, Glasgow, Liverpool and Manchester. The United Kingdom consists of four countries—England, Scotland, Wales, the last three have devolved administrations, each with varying powers, based in their capitals, Edinburgh, Cardiff and Belfast, respectively. The relationships among the countries of the UK have changed over time, Wales was annexed by the Kingdom of England under the Laws in Wales Acts 1535 and 1542. A treaty between England and Scotland resulted in 1707 in a unified Kingdom of Great Britain, which merged in 1801 with the Kingdom of Ireland to form the United Kingdom of Great Britain and Ireland. Five-sixths of Ireland seceded from the UK in 1922, leaving the present formulation of the United Kingdom of Great Britain, there are fourteen British Overseas Territories. These are the remnants of the British Empire which, at its height in the 1920s, British influence can be observed in the language, culture and legal systems of many of its former colonies. The United Kingdom is a country and has the worlds fifth-largest economy by nominal GDP. The UK is considered to have an economy and is categorised as very high in the Human Development Index. It was the worlds first industrialised country and the worlds foremost power during the 19th, the UK remains a great power with considerable economic, cultural, military, scientific and political influence internationally. It is a nuclear weapons state and its military expenditure ranks fourth or fifth in the world. The UK has been a permanent member of the United Nations Security Council since its first session in 1946 and it has been a leading member state of the EU and its predecessor, the European Economic Community, since 1973. However, on 23 June 2016, a referendum on the UKs membership of the EU resulted in a decision to leave. The Acts of Union 1800 united the Kingdom of Great Britain, Scotland, Wales and Northern Ireland have devolved self-government
22.
London
–
London /ˈlʌndən/ is the capital and most populous city of England and the United Kingdom. Standing on the River Thames in the south east of the island of Great Britain and it was founded by the Romans, who named it Londinium. Londons ancient core, the City of London, largely retains its 1. 12-square-mile medieval boundaries. London is a global city in the arts, commerce, education, entertainment, fashion, finance, healthcare, media, professional services, research and development, tourism. It is crowned as the worlds largest financial centre and has the fifth- or sixth-largest metropolitan area GDP in the world, London is a world cultural capital. It is the worlds most-visited city as measured by international arrivals and has the worlds largest city airport system measured by passenger traffic, London is the worlds leading investment destination, hosting more international retailers and ultra high-net-worth individuals than any other city. Londons universities form the largest concentration of education institutes in Europe. In 2012, London became the first city to have hosted the modern Summer Olympic Games three times, London has a diverse range of people and cultures, and more than 300 languages are spoken in the region. Its estimated mid-2015 municipal population was 8,673,713, the largest of any city in the European Union, Londons urban area is the second most populous in the EU, after Paris, with 9,787,426 inhabitants at the 2011 census. The citys metropolitan area is the most populous in the EU with 13,879,757 inhabitants, the city-region therefore has a similar land area and population to that of the New York metropolitan area. London was the worlds most populous city from around 1831 to 1925, Other famous landmarks include Buckingham Palace, the London Eye, Piccadilly Circus, St Pauls Cathedral, Tower Bridge, Trafalgar Square, and The Shard. The London Underground is the oldest underground railway network in the world, the etymology of London is uncertain. It is an ancient name, found in sources from the 2nd century and it is recorded c.121 as Londinium, which points to Romano-British origin, and hand-written Roman tablets recovered in the city originating from AD 65/70-80 include the word Londinio. The earliest attempted explanation, now disregarded, is attributed to Geoffrey of Monmouth in Historia Regum Britanniae and this had it that the name originated from a supposed King Lud, who had allegedly taken over the city and named it Kaerlud. From 1898, it was accepted that the name was of Celtic origin and meant place belonging to a man called *Londinos. The ultimate difficulty lies in reconciling the Latin form Londinium with the modern Welsh Llundain, which should demand a form *lōndinion, from earlier *loundiniom. The possibility cannot be ruled out that the Welsh name was borrowed back in from English at a later date, and thus cannot be used as a basis from which to reconstruct the original name. Until 1889, the name London officially applied only to the City of London, two recent discoveries indicate probable very early settlements near the Thames in the London area
23.
Ulster Scots dialects
–
Ulster Scots or Ulster-Scots, also known as Ullans, generally refers to the dialects of Scots spoken in parts of Ulster in Ireland. Some definitions of Ulster Scots may also include Standard English spoken with an Ulster Scots accent and this is a situation like that of Lowland Scots and Scottish Standard English with words pronounced using the Ulster Scots phonemes closest to those of Standard English. Ulster Scots has been influenced by Hiberno-English, particularly Mid-Ulster English, as a result of the competing influences of English and Scots, varieties of Ulster Scots can be described as more English or more Scots. The earliest Scots writing in Ulster dates from time, and until the late 20th century. While once referred to as Scotch-Irish by several researchers, that has now superseded by the term Ulster Scots. Speakers usually refer to their vernacular as Braid Scots, Scotch or the hamely tongue, occasionally, the term Hiberno-Scots is used, but it is usually used for the ethnic group rather than the vernacular. During the middle of the 20th century, the linguist R. J. Gregg established the boundaries of Ulsters Scots-speaking areas based on information gathered from native speakers. Ulster Scots is spoken in east Antrim, north Down, north-east County Londonderry and it is also spoken in the Laggan district and parts of the Finn Valley in east Donegal and in the south of Inishowen in north Donegal. Other estimates range from 35,000 in Northern Ireland, to a total of 100,000 including the Republic of Ireland. In the 2011 census of Northern Ireland,16,373 people stated that they can speak, read, write and understand Ulster Scots and 140,204 people reported having some ability in Ulster Scots. Enthusiasts such as Philip Robinson, the Ulster-Scots Language Society and supporters of an Ulster-Scots Academy are of the opinion that Ulster Scots is a language in its own right. That position has been criticised by the Ulster-Scots Agency, a BBC report stating, other linguists treat it as a variety of the Scots language, Caroline Macafee, for example, writes that Ulster Scots is clearly a dialect of Central Scots. The Concise Ulster Dictionary writes that Ulster Scots is one dialect of Lowland Scots, the Northern Ireland Department of Culture, Arts and Leisure considers Ulster Scots to be the local variety of the Scots language. It has been said that its status varies between dialect and language, the North/South Co-operation Northern Ireland Order 1999, which gave effect to the implementation bodies incorporated the text of the agreement in its Schedule 1. The Good Friday Agreement recognises Ulster Scots as part of the wealth of the island of Ireland. This reflects the wording used in the St Andrews Agreement to refer to the enhancement and development of the Ulster Scots language, heritage, there is still controversy on the status of Ulster Scots. In the core areas of Scots settlement, Scots outnumbered English settlers by five or six to one, literature from shortly before the end of the unselfconscious tradition at the turn of the 19th and 20th centuries is almost identical with contemporary writing from Scotland. W. G. Lyttle, writing in Paddy McQuillans Trip Tae Glesco, uses the typically Scots forms kent and begood, now replaced in Ulster by the more mainstream Anglic forms knew, knowed or knawed and begun
24.
Greenwich Mean Time
–
Greenwich Mean Time is the mean solar time at the Royal Observatory in Greenwich, London. GMT was formerly used as the civil time standard, now superseded in that function by Coordinated Universal Time. Today GMT is considered equivalent to UTC for UK civil purposes and for navigation is considered equivalent to UT1, consequently, the term GMT should not be used for precise purposes. Due to Earths uneven speed in its orbit and its axial tilt, noon GMT is rarely the exact moment the sun crosses the Greenwich meridian. This event may occur up to 16 minutes before or after noon GMT, noon GMT is the annual average moment of this event, which accounts for the word mean in Greenwich Mean Time. Originally, astronomers considered a GMT day to start at noon while for almost everyone else it started at midnight, to avoid confusion, the name Universal Time was introduced to denote GMT as counted from midnight. Astronomers preferred the old convention to simplify their observational data, so each night was logged under a single calendar date. Today Universal Time usually refers to UTC or UT1, in some countries Greenwich Mean Time is the legal time in the winter and the population uses the term. For an explanation of why this is, see GMT in legislation below, synchronisation of the chronometer on GMT did not affect shipboard time, which was still solar time. Most time zones were based upon GMT, as an offset of a number of hours ahead of GMT or behind GMT and it was gradually adopted for other purposes, but a legal case in 1858 held local mean time to be the official time. On 14 May 1880, a signed by Clerk to Justices appeared in The Times, stating that Greenwich time is now kept almost throughout England. For example, our polling booths were opened, say, at 813 and closed at 413 PM. This was changed later in 1880, GMT was adopted on the Isle of Man in 1883, Jersey in 1898 and Guernsey in 1913. Ireland adopted GMT in 1916, supplanting Dublin Mean Time, hourly time signals from Greenwich Observatory were first broadcast on 5 February 1924, rendering the time ball at the observatory redundant in the process. The daily rotation of the Earth is irregular and constantly slows, on 1 January 1972, GMT was superseded as the international civil time standard by Coordinated Universal Time, maintained by an ensemble of atomic clocks around the world. Indeed, even the Greenwich meridian itself is not quite what it used to be—defined by the centre of the instrument at the Observatory at Greenwich. Nevertheless, the line in the old observatorys courtyard today differs no more than a few metres from that line which is now the prime meridian of the world. Historically GMT has been used two different conventions for numbering hours. The long-standing astronomical convention dating from the work of Ptolemy, was to refer to noon as zero hours and this contrasted with the civil convention of referring to midnight as zero hours dating from the Romans
25.
Daylight saving time
–
Daylight saving time is the practice of advancing clocks during summer months by one hour so that evening daylight lasts an hour longer, while sacrificing normal sunrise times. Typically, regions that use Daylight Savings Time adjust clocks forward one hour close to the start of spring, American inventor and politician Benjamin Franklin proposed a form of daylight time in 1784. New Zealander George Hudson proposed the idea of saving in 1895. The German Empire and Austria-Hungary organized the first nationwide implementation, starting on April 30,1916, many countries have used it at various times since then, particularly since the energy crisis of the 1970s. The practice has both advocates and critics, DST clock shifts sometimes complicate timekeeping and can disrupt travel, billing, record keeping, medical devices, heavy equipment, and sleep patterns. Computer software often adjusts clocks automatically, but policy changes by various jurisdictions of DST dates, industrialized societies generally follow a clock-based schedule for daily activities that do not change throughout the course of the year. The time of day that individuals begin and end work or school, North and south of the tropics daylight lasts longer in summer and shorter in winter, with the effect becoming greater as one moves away from the tropics. However, they will have one hour of daylight at the start of each day. Supporters have also argued that DST decreases energy consumption by reducing the need for lighting and heating, DST is also of little use for locations near the equator, because these regions see only a small variation in daylight in the course of the year. After ancient times, equal-length civil hours eventually supplanted unequal, so civil time no longer varies by season, unequal hours are still used in a few traditional settings, such as some monasteries of Mount Athos and all Jewish ceremonies. This 1784 satire proposed taxing window shutters, rationing candles, and waking the public by ringing church bells, despite common misconception, Franklin did not actually propose DST, 18th-century Europe did not even keep precise schedules. However, this changed as rail transport and communication networks came to require a standardization of time unknown in Franklins day. Modern DST was first proposed by the New Zealand entomologist George Hudson, whose shift work job gave him time to collect insects. An avid golfer, he also disliked cutting short his round at dusk and his solution was to advance the clock during the summer months, a proposal he published two years later. The proposal was taken up by the Liberal Member of Parliament Robert Pearce, a select committee was set up to examine the issue, but Pearces bill did not become law, and several other bills failed in the following years. Willett lobbied for the proposal in the UK until his death in 1915, william Sword Frost, mayor of Orillia, Ontario, introduced daylight saving time in the municipality during his tenure from 1911 to 1912. Starting on April 30,1916, the German Empire and its World War I ally Austria-Hungary were the first to use DST as a way to conserve coal during wartime, Britain, most of its allies, and many European neutrals soon followed suit. Russia and a few other countries waited until the year
26.
Western European Summer Time
–
Western European Summer Time is a summer daylight saving time scheme,1 hour ahead of Coordinated Universal Time. Also sometimes erroneously referred to as Irish Summer Time, the scheme runs from the last Sunday in March to the last Sunday in October each year. At both the start and end of the schemes, clock changes take place at 01,00 UTC, during the winter, Greenwich Mean Time is used. The asymmetry reflects temperature more than the length of daylight, Ireland observes Standard Time during the summer months and changes to UTC+0 in winter. As Irelands winter time period begins on the last Sunday in October and finishes on the last Sunday in March, the result is the same as if it observed summer time. The following countries and territories use Western European Summer Time during the summer, starting in 1916, the dates for the beginning and end of BST each year were mandated by the Parliament of the United Kingdom. In February 2002, the Summer Time Order 2002 changed the dates and times to match European rules for moving to, note, Until 1 October 1916 time in all of Ireland was based on Dublin Mean Time, GMT −25 minutes. BBC News report, Tundra time call in clocks debate, UK Government Report, Overview of the pros and cons of British Summer Time
27.
Archipelago
–
An archipelago, sometimes called an island group or island chain, is a chain, cluster or collection of islands. The word archipelago is derived from the Greek ἄρχι- – arkhi-, in Italian, possibly following a tradition of antiquity, the Archipelago was the proper name for the Aegean Sea and, later, usage shifted to refer to the Aegean Islands. It is now used to refer to any group or, sometimes. Archipelagos may be isolated in large amounts of water or neighbouring a large land mass. For example, Scotland has more than 700 islands surrounding its mainland which form an archipelago, archipelagos are often volcanic, forming along island arcs generated by subduction zones or hotspots, but may also be the result of erosion, deposition, and land elevation. Depending on their origin, islands forming archipelagos can be referred to as oceanic islands, continental fragments. Oceanic islands are mainly of volcanic origin, continental fragments correspond to land masses that have separated from a continental mass due to tectonic displacement. Indonesia, Japan, Taiwan, the Philippines, New Zealand, Maldives, the Bahamas, Greece, Hawaii, the largest archipelagic state in the world by area and population is Indonesia. Island arc List of landforms List of archipelagos by number of islands List of archipelagos List of islands Chisholm, Hugh, ed. Archipelago
28.
Continental Europe
–
Continental Europe, also referred to as mainland Europe, or, by Europeans, simply the Continent, is the continuous continent of Europe, excluding surrounding islands. This historical core of Carolingian Europe was consciously invoked in the 1950s as the historical basis for the prospective European integration. In both Great Britain and Ireland, the Continent is widely and generally used to refer to the mainland of Europe, an apocryphal British newspaper headline supposedly once read, Fog in Channel, Continent Cut Off. It has also claimed that this was a regular weather forecast in Britain in the 1930s. In addition, the word Europe itself is regularly used to mean Europe excluding the islands of Great Britain, Iceland. The term mainland Europe is also sometimes used, derivatively, the adjective continental refers to the social practices or fashion of continental Europe. Examples include breakfast, topless sunbathing and, historically, long-range driving often known as Grand Touring. Differences include electrical plugs, time zones for the most part, the use of traffic, and for the United Kingdom, currency. Britain is physically connected to continental Europe through the undersea Channel Tunnel and this route is popular with refugees and migrants seeking to enter the UK. Especially in Germanic studies, continental refers to the European continent excluding the Scandinavian peninsula, Britain, Ireland, and Iceland. The reason for this is that although the Scandinavian peninsula is attached to continental Europe, kontinenten is a vernacular Swedish expression that refers to the area excluding Sweden, Norway, and Finland but including Denmark and the rest of continental Europe. In Norway, similarly, one speaks about Kontinentet as an entity, usually referring to Germany, France, Italy, Spain, Portugal, the Benelux countries. Today, the Scandinavian peninsula is accessible by train and road with several bridge/tunnel structures connecting the Danish peninsula of Jutland to Scania in Sweden. The Continent may sometimes refer to the part of Italy, the continental part of Spain, the continental part of France. The term is used from the perspective of the residents of each country to describe the continental portion of their country or the continent as a whole. Continental philosophy Geopolitical divisions of Europe Geographical midpoint of Europe Mainland Western Europe Hajnal line
29.
Great Britain
–
Great Britain, also known as Britain, is a large island in the north Atlantic Ocean off the northwest coast of continental Europe. With an area of 209,331 km2, Great Britain is the largest European island, in 2011 the island had a population of about 61 million people, making it the worlds third-most populous island after Java in Indonesia and Honshu in Japan. The island of Ireland is situated to the west of it, the island is dominated by a maritime climate with quite narrow temperature differences between seasons. Politically, the island is part of the United Kingdom of Great Britain and Northern Ireland, most of England, Scotland, and Wales are on the island. The term Great Britain often extends to surrounding islands that form part of England, Scotland, and Wales. A single Kingdom of Great Britain resulted from the union of the Kingdom of England, the archipelago has been referred to by a single name for over 2000 years, the term British Isles derives from terms used by classical geographers to describe this island group. By 50 BC Greek geographers were using equivalents of Prettanikē as a name for the British Isles. However, with the Roman conquest of Britain the Latin term Britannia was used for the island of Great Britain, the oldest mention of terms related to Great Britain was by Aristotle, or possibly by Pseudo-Aristotle, in his text On the Universe, Vol. III. To quote his works, There are two large islands in it, called the British Isles, Albion and Ierne. The name Britain descends from the Latin name for Britain, Britannia or Brittānia, Old French Bretaigne and Middle English Bretayne, Breteyne. The French form replaced the Old English Breoton, Breoten, Bryten, Breten, Britannia was used by the Romans from the 1st century BC for the British Isles taken together. It is derived from the writings of the Pytheas around 320 BC. Marcian of Heraclea, in his Periplus maris exteri, described the group as αἱ Πρεττανικαὶ νῆσοι. The peoples of these islands of Prettanike were called the Πρεττανοί, Priteni is the source of the Welsh language term Prydain, Britain, which has the same source as the Goidelic term Cruithne used to refer to the early Brythonic-speaking inhabitants of Ireland. The latter were later called Picts or Caledonians by the Romans, the Greco-Egyptian scientist Ptolemy referred to the larger island as great Britain and to Ireland as little Britain in his work Almagest. The name Albion appears to have out of use sometime after the Roman conquest of Britain. After the Anglo-Saxon period, Britain was used as a term only. It was used again in 1604, when King James VI and I styled himself King of Great Brittaine, France, Great Britain refers geographically to the island of Great Britain, politically to England, Scotland and Wales in combination
30.
Ireland
–
Ireland is an island in the North Atlantic. It is separated from Great Britain to its east by the North Channel, the Irish Sea, Ireland is the second-largest island of the British Isles, the third-largest in Europe, and the twentieth-largest on Earth. Politically, Ireland is divided between the Republic of Ireland, which covers five-sixths of the island, and Northern Ireland, in 2011, the population of Ireland was about 6.4 million, ranking it the second-most populous island in Europe after Great Britain. Just under 4.6 million live in the Republic of Ireland, the islands geography comprises relatively low-lying mountains surrounding a central plain, with several navigable rivers extending inland. The island has lush vegetation, a product of its mild, thick woodlands covered the island until the Middle Ages. As of 2013, the amount of land that is wooded in Ireland is about 11% of the total, there are twenty-six extant mammal species native to Ireland. The Irish climate is moderate and classified as oceanic. As a result, winters are milder than expected for such a northerly area, however, summers are cooler than those in Continental Europe. Rainfall and cloud cover are abundant, the earliest evidence of human presence in Ireland is dated at 10,500 BC. Gaelic Ireland had emerged by the 1st century CE, the island was Christianised from the 5th century onward. Following the Norman invasion in the 12th century, England claimed sovereignty over Ireland, however, English rule did not extend over the whole island until the 16th–17th century Tudor conquest, which led to colonisation by settlers from Britain. In the 1690s, a system of Protestant English rule was designed to materially disadvantage the Catholic majority and Protestant dissenters, with the Acts of Union in 1801, Ireland became a part of the United Kingdom. Northern Ireland saw much civil unrest from the late 1960s until the 1990s and this subsided following a political agreement in 1998. In 1973 the Republic of Ireland joined the European Economic Community while the United Kingdom, Irish culture has had a significant influence on other cultures, especially in the fields of literature. Alongside mainstream Western culture, an indigenous culture exists, as expressed through Gaelic games, Irish music. The culture of the island shares many features with that of Great Britain, including the English language, and sports such as association football, rugby, horse racing. The name Ireland derives from Old Irish Eriu and this in turn derives from Proto-Celtic *Iveriu, which is also the source of Latin Hibernia. Iveriu derives from a root meaning fat, prosperous, during the last glacial period, and up until about 9000 years ago, most of Ireland was covered with ice, most of the time
31.
Sovereign state
–
A sovereign state is, in international law, a nonphysical juridical entity that is represented by one centralized government that has sovereignty over a geographic area. International law defines sovereign states as having a permanent population, defined territory, one government, and it is also normally understood that a sovereign state is neither dependent on nor subjected to any other power or state. The existence or disappearance of a state is a question of fact, States came into existence as people gradually transferred their allegiance from an individual sovereign to an intangible but territorial political entity, of the state. States are but one of political orders that emerged from feudal Europe, others being city states, leagues. Westphalian sovereignty is the concept of sovereignty based on territoriality. It is a system of states, multinational corporations. Sovereignty is a term that is frequently misused and that position was reflected and constituted in the notion that their sovereignty was either completely lacking, or at least of an inferior character when compared to that of civilised people. Lassa Oppenheim said There exists perhaps no conception the meaning of which is more controversial than that of sovereignty. It is a fact that this conception, from the moment when it was introduced into political science until the present day, has never had a meaning which was universally agreed upon. In the opinion of H. V. Evatt of the High Court of Australia, sovereignty is neither a question of fact, nor a question of law, but a question that does not arise at all. The right of nations to determine their own status and exercise permanent sovereignty within the limits of their territorial jurisdictions is widely recognized. The Westphalian model of sovereignty has increasingly come under fire from the non-west as a system imposed solely by Western Colonialism. What this model did was make religion a subordinate to politics and this system does not fit in the Islamic world because concepts such as separation of church and state and individual conscience are not recognised in the Islamic religion as social systems. Nation denotes a people who are believed to or deemed to share common customs, religion, language, origins, however, the adjectives national and international are frequently used to refer to matters pertaining to what are strictly sovereign states, as in national capital, international law. State refers to the set of governing and supportive institutions that have sovereignty over a definite territory, State recognition signifies the decision of a sovereign state to treat another entity as also being a sovereign state. Recognition can be expressed or implied and is usually retroactive in its effects. It does not necessarily signify a desire to establish or maintain diplomatic relations, There is no definition that is binding on all the members of the community of nations on the criteria for statehood. In actual practice, the criteria are mainly political, not legal, in international law, however, there are several theories of when a state should be recognised as sovereign
32.
Crown dependencies
–
The Crown dependencies are the Isle of Man in the Irish Sea and the Bailiwicks of Jersey and Guernsey in the English Channel. Being independently administered jurisdictions, they do not form part of either the United Kingdom or the British Overseas Territories and they are self-governing possessions of the Crown. Internationally, the dependencies are considered territories for which the United Kingdom is responsible rather than as sovereign states, as a result, they are not member states of the Commonwealth of Nations. However, they do have a relationship with the Commonwealth, the European Union and they are not part of the European Union, although they are within the EUs customs area. In each case, the head of government is referred to as a Chief Minister, the Crown is defined differently in each crown dependency. Legislation of the Isle of Man defines the Crown in right of the Isle of Man as being separate from the Crown in right of the United Kingdom and this constitutional concept is also worded as the Crown in right of the Bailiwick of Guernsey. Each Bailiwick is a Crown dependency and each is headed by a Bailiff, each Bailiwick has its own legal and healthcare systems, and their own separate immigration policies, with local status in one Bailiwick having no jurisdiction in the other. The two Bailiwicks exercise bilateral double taxation treaties, since 1961, the Bailiwicks have had separate courts of appeal, but generally the Bailiff of each Bailiwick has been appointed to serve on the panel of appellate judges for the other Bailiwick. The Bailiwick of Guernsey comprises three separate jurisdictions, Guernsey, which also the nearby islands of Herm and Jethou. Sark, which includes the nearby island of Brecqhou. Alderney, including smaller surrounding uninhabited islands, the parliament of Guernsey is the States of Deliberation, the parliament of Sark is called the Chief Pleas, and the parliament of Alderney is called the States of Alderney. The three parliaments together can also approve joint Bailiwick-wide legislation that applies in those parts of the Bailiwick whose parliaments approve it. Guernsey issues its own coins and banknotes, Guernsey banknotes Coins of the Guernsey pound These circulate freely in both Bailiwicks alongside UK coinage and English and Scottish banknotes and they are not legal tender within the UK. There are no parties in any of the parliaments, candidates stand for election as independents. e. 5432 on 2 wheels and on 4 wheels, the Bailiwick of Jersey consists of the island of Jersey and a number of surrounding uninhabited islands. The parliament is the States of Jersey, the first known mention of which is in a document of 1497, Jersey issues its own coins and banknotes, Jersey banknotes Coins of the Jersey pound These circulate freely in both Bailiwicks alongside UK coinage and English and Scottish banknotes. They are not legal tender within the UK but are legal currency backed by deposits at the Bank of England, there are few political parties, as candidates generally stand for election as independents. The Isle of Mans Tynwald claims to be the worlds oldest parliament in continuous existence, candidates often stand for election as independents, rather than being selected by political parties
33.
Scotland
–
Scotland is a country that is part of the United Kingdom and covers the northern third of the island of Great Britain. It shares a border with England to the south, and is surrounded by the Atlantic Ocean, with the North Sea to the east. In addition to the mainland, the country is made up of more than 790 islands, including the Northern Isles, the Kingdom of Scotland emerged as an independent sovereign state in the Early Middle Ages and continued to exist until 1707. By inheritance in 1603, James VI, King of Scots, became King of England and King of Ireland, Scotland subsequently entered into a political union with the Kingdom of England on 1 May 1707 to create the new Kingdom of Great Britain. The union also created a new Parliament of Great Britain, which succeeded both the Parliament of Scotland and the Parliament of England. Within Scotland, the monarchy of the United Kingdom has continued to use a variety of styles, titles, the legal system within Scotland has also remained separate from those of England and Wales and Northern Ireland, Scotland constitutes a distinct jurisdiction in both public and private law. Glasgow, Scotlands largest city, was one of the worlds leading industrial cities. Other major urban areas are Aberdeen and Dundee, Scottish waters consist of a large sector of the North Atlantic and the North Sea, containing the largest oil reserves in the European Union. This has given Aberdeen, the third-largest city in Scotland, the title of Europes oil capital, following a referendum in 1997, a Scottish Parliament was re-established, in the form of a devolved unicameral legislature comprising 129 members, having authority over many areas of domestic policy. Scotland is represented in the UK Parliament by 59 MPs and in the European Parliament by 6 MEPs, Scotland is also a member nation of the British–Irish Council, and the British–Irish Parliamentary Assembly. Scotland comes from Scoti, the Latin name for the Gaels, the Late Latin word Scotia was initially used to refer to Ireland. By the 11th century at the latest, Scotia was being used to refer to Scotland north of the River Forth, alongside Albania or Albany, the use of the words Scots and Scotland to encompass all of what is now Scotland became common in the Late Middle Ages. Repeated glaciations, which covered the land mass of modern Scotland. It is believed the first post-glacial groups of hunter-gatherers arrived in Scotland around 12,800 years ago, the groups of settlers began building the first known permanent houses on Scottish soil around 9,500 years ago, and the first villages around 6,000 years ago. The well-preserved village of Skara Brae on the mainland of Orkney dates from this period and it contains the remains of an early Bronze Age ruler laid out on white quartz pebbles and birch bark. It was also discovered for the first time that early Bronze Age people placed flowers in their graves, in the winter of 1850, a severe storm hit Scotland, causing widespread damage and over 200 deaths. In the Bay of Skaill, the storm stripped the earth from a large irregular knoll, when the storm cleared, local villagers found the outline of a village, consisting of a number of small houses without roofs. William Watt of Skaill, the laird, began an amateur excavation of the site, but after uncovering four houses
34.
Year
–
A year is the orbital period of the Earth moving in its orbit around the Sun. Due to the Earths axial tilt, the course of a year sees the passing of the seasons, marked by changes in weather, the hours of daylight, and, consequently, vegetation and soil fertility. In temperate and subpolar regions around the globe, four seasons are recognized, spring, summer, autumn. In tropical and subtropical regions several geographical sectors do not present defined seasons, but in the seasonal tropics, a calendar year is an approximation of the number of days of the Earths orbital period as counted in a given calendar. The Gregorian, or modern, calendar, presents its calendar year to be either a common year of 365 days or a year of 366 days, as do the Julian calendars. For the Gregorian calendar the average length of the year across the complete leap cycle of 400 years is 365.2425 days. The ISO standard ISO 80000-3, Annex C, supports the symbol a to represent a year of either 365 or 366 days, in English, the abbreviations y and yr are commonly used. In astronomy, the Julian year is a unit of time, it is defined as 365.25 days of exactly 86400 seconds, totalling exactly 31557600 seconds in the Julian astronomical year. The word year is used for periods loosely associated with, but not identical to, the calendar or astronomical year, such as the seasonal year, the fiscal year. Similarly, year can mean the period of any planet, for example. The term can also be used in reference to any long period or cycle, west Saxon ġēar, Anglian ġēr continues Proto-Germanic *jǣran. Cognates are German Jahr, Old High German jār, Old Norse ár and Gothic jer, all the descendants of the Proto-Indo-European noun *yeh₁rom year, season. Cognates also descended from the same Proto-Indo-European noun are Avestan yārǝ year, Greek ὥρα year, season, period of time, Old Church Slavonic jarŭ, Latin annus is from a PIE noun *h₂et-no-, which also yielded Gothic aþn year. Both *yeh₁-ro- and *h₂et-no- are based on verbal roots expressing movement, *h₁ey- and *h₂et- respectively, the Greek word for year, ἔτος, is cognate with Latin vetus old, from the PIE word *wetos- year, also preserved in this meaning in Sanskrit vat-sa- yearling and vat-sa-ras year. Derived from Latin annus are a number of English words, such as annual, annuity, anniversary, etc. per annum means each year, anno Domini means in the year of the Lord. No astronomical year has an number of days or lunar months. Financial and scientific calculations often use a 365-day calendar to simplify daily rates, in the Julian calendar, the average length of a year is 365.25 days. In a non-leap year, there are 365 days, in a year there are 366 days
35.
Silurian
–
The Silurian is a geologic period and system spanning 24.6 million years from the end of the Ordovician Period, at 443.8 million years ago, to the beginning of the Devonian Period,419.2 Mya. As with other periods, the rock beds that define the periods start and end are well identified. The base of the Silurian is set at a major Ordovician-Silurian extinction event when 60% of marine species were wiped out, a significant evolutionary milestone during the Silurian was the diversification of jawed and bony fish. However, terrestrial life would not greatly diversify and affect the landscape until the Devonian, the Silurian system was first identified by British geologist Sir Roderick Impey Murchison, who was examining fossil-bearing sedimentary rock strata in south Wales in the early 1830s. He named the sequences for a Celtic tribe of Wales, the Silures, inspired by his friend Adam Sedgwick and this naming does not indicate any correlation between the occurrence of the Silurian rocks and the land inhabited by the Silures. As it was first identified, the Silurian series when traced farther afield quickly came to overlap Sedgwicks Cambrian sequence, however, charles Lapworth resolved the conflict by defining a new Ordovician system including the contested beds. An early alternative name for the Silurian was Gotlandian after the strata of the Baltic island of Gotland, the French geologist Joachim Barrande, building on Murchisons work, used the term Silurian in a more comprehensive sense than was justified by subsequent knowledge. He divided the Silurian rocks of Bohemia into eight stages and his interpretation was questioned in 1854 by Edward Forbes, and the later stages of Barrande, F, G and H, have since been shown to be Devonian. Despite these modifications in the groupings of the strata, it is recognized that Barrande established Bohemia as a classic ground for the study of the earliest fossils. The epoch is named for the town of Llandovery in Carmarthenshire, the Wenlock, which lasted from 433.4 ±1.5 to 427.4 ±2.8 mya, is subdivided into the Sheinwoodian and Homerian ages. It is named after Wenlock Edge in Shropshire, England, during the Wenlock, the oldest known tracheophytes of the genus Cooksonia, appear. The first terrestrial animals also appear in the Wenlock, represented by air-breathing millipedes from Scotland. The Ludlow, lasting from 427.4 ±1.5 to 423 ±2.8 mya, comprises the Gorstian stage, lasting until 425.6 million years ago, and it is named for the town of Ludlow in Shropshire, England. The Pridoli, lasting from 423 ±1.5 to 419.2 ±2.8 mya, is the final and it is named after one locality at the Homolka a Přídolí nature reserve near the Prague suburb Slivenec in the Czech Republic. Přídolí is the old name of a field area. The high sea levels of the Silurian and the flat land resulted in a number of island chains. The southern continents remained united during this period, the melting of icecaps and glaciers contributed to a rise in sea level, recognizable from the fact that Silurian sediments overlie eroded Ordovician sediments, forming an unconformity. The continents of Avalonia, Baltica, and Laurentia drifted together near the equator and this event is the Caledonian orogeny, a spate of mountain building that stretched from New York State through conjoined Europe and Greenland to Norway
36.
Plate tectonics
–
The theoretical model builds on the concept of continental drift developed during the first few decades of the 20th century. The geoscientific community accepted plate-tectonic theory after seafloor spreading was validated in the late 1950s, the lithosphere, which is the rigid outermost shell of a planet, is broken up into tectonic plates. The Earths lithosphere is composed of seven or eight major plates, where the plates meet, their relative motion determines the type of boundary, convergent, divergent, or transform. Earthquakes, volcanic activity, mountain-building, and oceanic trench formation occur along plate boundaries. The relative movement of the plates typically ranges from zero to 100 mm annually, tectonic plates are composed of oceanic lithosphere and thicker continental lithosphere, each topped by its own kind of crust. Along convergent boundaries, subduction carries plates into the mantle, the material lost is balanced by the formation of new crust along divergent margins by seafloor spreading. In this way, the surface of the lithosphere remains the same. This prediction of plate tectonics is also referred to as the conveyor belt principle, earlier theories, since disproven, proposed gradual shrinking or gradual expansion of the globe. Tectonic plates are able to move because the Earths lithosphere has greater strength than the underlying asthenosphere. Lateral density variations in the result in convection. Plate movement is thought to be driven by a combination of the motion of the seafloor away from the ridge and drag, with downward suction. Another explanation lies in the different forces generated by forces of the Sun. The relative importance of each of these factors and their relationship to other is unclear. The outer layers of the Earth are divided into the lithosphere and asthenosphere and this is based on differences in mechanical properties and in the method for the transfer of heat. Mechanically, the lithosphere is cooler and more rigid, while the asthenosphere is hotter, in terms of heat transfer, the lithosphere loses heat by conduction, whereas the asthenosphere also transfers heat by convection and has a nearly adiabatic temperature gradient. The key principle of plate tectonics is that the lithosphere exists as separate and distinct tectonic plates, Plate motions range up to a typical 10–40 mm/year, to about 160 mm/year. The driving mechanism behind this movement is described below, tectonic lithosphere plates consist of lithospheric mantle overlain by either or both of two types of crustal material, oceanic crust and continental crust. Average oceanic lithosphere is typically 100 km thick, its thickness is a function of its age, as passes, it conductively cools
37.
Summit
–
A summit is a point on a surface that is higher in elevation than all points immediately adjacent to it. Mathematically, a summit is a maximum in elevation. The topographic terms acme, apex, peak, and zenith are synonymous, the UIAA definition is that a summit is independent if it has a prominence of 30 metres or more, it is a mountain if it has a prominence of at least 300 metres. This can be summarised as follows, A pyramidal peak is an exaggerated form produced by ice erosion of a mountain top, Summit may also refer to the highest point along a line, trail, or route. In many parts of the western United States, the term refers to the highest point along a road, highway. For example, the highest point along Interstate 80 in California is referred to as Donner Summit while the highest point on Interstate 5 is Siskiyou Mountain Summit, geoid Hill List of highest mountains Maxima and minima Nadir Summit accordance Peak finder
38.
Lough Neagh
–
Lough Neagh is a large freshwater lake in Northern Ireland. It is the largest lake by area in the British Isles and it supplies 40% of Northern Irelands water. Its main inflows are the Upper River Bann and River Blackwater and its name comes from Irish, Loch nEachach, meaning Eachaidhs lake. The lough is owned by the Earl of Shaftesbury, located 20 miles west of Belfast, it is about 20 miles long and 9 miles wide. It is very shallow around the margins and the depth in the main body of the lake is about 30 feet. As one of its sources is the Upper Bann, the Lough can itself be considered as part of the Bann, five of the six counties of Northern Ireland have shores on the Lough, and its area is split among them. The lough is used by Northern Ireland Water as a source of fresh water, the lough supplies 40% of the regions drinking water. There have long been plans to increase the amount of water drawn from the lough, through a new treatment works at Hog Park Point. In 2012, it was reported that the Earl is considering transferring ownership of the Lough to the Northern Ireland Assembly, traditional working boats on Lough Neagh include wide-beamed 4. 9-to-6. 4-metre clinker-built, sprit-rigged working boats and smaller flat-bottomed cots and flats. Barges, here called lighters, were used until the 1940s to transport coal over the lough, until the 17th century, log boats were the main means of transport. Few traditional boats are now, but a community-based group on the southern shore of the lough is rebuilding a series of working boats. The Lower Bann was also navigable to Coleraine and the Antrim coast, of these waterways, only the Lower Bann remains open today, although a restoration plan for the Ulster Canal is currently in progress. Lough Neagh Rescue provides a search and rescue service 24 hours a day and has 3 stations and these are at Antrim Ardboe and Kinnego Marinas. Kinnego being is headquarters and founding station It is a service funded by the district councils bordering the Lough. Its members are trained and are a declared facility for the Maritime. Lough Neagh attracts bird watchers from many due to the number and variety of birds which winter and summer in the boglands. These European eels make their way from the Sargasso Sea in the Atlantic Ocean, some 4,000 miles along the Gulf Stream to the mouth of the River Bann and they remain there for some 10 to 15 years, maturing, before returning to the Sargasso to spawn. Today Lough Neagh eel fisheries export their eels to restaurants all over the world, nobel laureate Seamus Heaney produced a collection of poems A Lough Neagh Sequence celebrating the eel-fishermens traditional techniques and the natural history of their catch
39.
Temperate climate
–
In geography, temperate or tepid latitudes of Earth lie between the tropics and the polar regions. The temperatures in these regions are relatively moderate, rather than extremely hot or cold. The north temperate zone extends from the Tropic of Cancer to the Arctic Circle, the south temperate zone extends from the Tropic of Capricorn to the Antarctic Circle. In some climate classifications, the zone is often divided into several smaller climate zones. These include Humid subtropical climate, Mediterranean climate, oceanic, subtropical climates are located between 23. 5° and 35. 0° north or south latitude on the eastern or leeward sides of landmasses. This climate has long, generally hot, summers and short, mild winters and these climates may occur in southern Asia, the southeastern United States, parts of eastern Australia, and in eastern coastal South America. Mediterranean climates, occur between 30° and 42° north and south latitude, on the sides of landmasses. This climate has hot summers and short mild winters, however, seasonal rainfall is the opposite of that of the subtropical humid type. These climates occur near the rimlands of the Mediterranean Sea, in western Australia, in California, the oceanic climates occur in the higher middle latitudes, between 45° and 60° north and south latitude. They are created by the flow from the cool high latitude oceans to their west. This causes the climate to have cool summers and cool winters, annual rainfall is spread throughout the entire year. Regions with this climate include Western Europe, northwestern North America, the Continental climates occur in middle latitudes, between 35° or 40° to 55°. These climates are normally inland or on sides of landmasses. They feature warm to hot summers and cold winters, with a large temperature variation. Regions with this climate include northern temperate Asia, the northern United States, southern Canada, the vast majority of the worlds human population resides in temperate zones, especially in the northern hemisphere, due to its greater mass of land. The richest temperate flora in the world is found in southern Africa, geographical zone Habitat Köppen climate classification Middle latitudes Polar circle Subtropics
40.
Oceanic climate
–
Oceanic climates are defined as having a monthly mean temperature below 22 °C in the warmest month, and above 0 °C in the coldest month. It typically lacks a dry season, as precipitation is evenly dispersed throughout the year. Oceanic climates generally have cool summers and mild to cool winters, Oceanic climates are most dominant in Europe, where they spread much farther inland than in other continents. Oceanic climates can have much storm activity as they are located in the belt of the stormy westerlies, many oceanic climates have frequent cloudy or overcast conditions due to the near constant storms and lows tracking over or near them. Precipitation is both adequate and reliable throughout the year in oceanic climates, extended months of rain and cloudy conditions are common in oceanic climates. Seattle is an example of this, between October and May, Seattle experiences high rainfall and is mostly or partly cloudy six out of every seven days. In most areas with a climate, precipitation comes in the form of rain for the majority of the year. However, some areas with this climate see some snowfall annually during winter, outside of Australia and parts of New Zealand, most areas with an oceanic climate experience at least one snowstorm per year. In the poleward locations of the climate zone, snowfall is more frequent. Overall temperature characteristics of the oceanic climates feature cool temperatures and infrequent extremes of temperature, summers are cool, with the warmest month having a mean temperature below 22 °C. Poleward of the latter is a zone of the subpolar oceanic climate, with long and cold winters and cool. Examples of this climate include parts of coastal Iceland in the Northern Hemisphere and extreme southern Chile, Oceanic climates are not necessarily always found in coastal locations on the aforementioned parallels, however, in most cases oceanic climates parallel higher middle latitude oceans. The polar jet stream, which moves in a west to east direction across the middle latitudes, advancing low pressure systems, storms, in coastal areas of the higher middle latitudes, the prevailing onshore flow creates the basic structure of most oceanic climates. Oceanic climates are a product and reflection of the adjacent to them. In summer, high pressure pushes the prevailing westerlies north of many oceanic climates. As a result of the Gulf Stream, west-coast areas located in high latitudes like Ireland, the UK, Oceanic climates in Europe occur mostly in Northwest Europe, from Ireland and Great Britain eastward to central Europe. Most of France, Germany, Norway, the north coast of Spain, examples of oceanic climates are found in London, Bergen, Dublin, Berlin, Bilbao, Donostia-San Sebastian, Biarritz, Bayonne, Zürich, Copenhagen and Paris. With decreasing distance to the Mediterranean Sea, the climate of Northwest Europe gradually changes to the subtropical dry-summer or Mediterranean climate of southern Europe
41.
North Atlantic Current
–
The North Atlantic Current, also known as North Atlantic Drift and North Atlantic Sea Movement, is a powerful warm western boundary current that extends the Gulf Stream north-eastward. The NAC originates from where the Gulf Stream turns north at the Southeast Newfoundland Rise, the NAC flows northward east of the Grand Banks, from 40°N to 51°N, before turning sharply east to cross the Atlantic. It transports more warm water to northern latitudes than any other boundary current. It reaches speeds of 2 knots near the North American coast, directed by topography, the NAC meanders heavily but, in contrast to the meanders of the Gulf Stream, the NAC meanders remain stable without breaking off into eddies. The colder parts of the Gulf Stream turn northward near the tail of the Grand Banks at 50°W where the Azores Current branches off to flow south of the Azores, from there the NAC flow north-eastward east of the Flemish Cap. Approaching the Mid-Atlantic Ridge, it turns eastward and becomes much broader. It then splits into a colder, north-eastern branch and an eastern branch. West of Continental Europe, it splits into two major branches, one branch goes southeast, later to become the Canary Current as it passes northwest Africa and turns southwest. The other major branch continues north along the coast of Northwestern Europe, other branches include the Irminger Current and the Norwegian Current. The North Atlantic Current, together with the Gulf Stream, have a reputation for having a considerable warming influence on European climate. The principal cause for differences in climate between North America and Europe is, however, winds rather than ocean currents. North Atlantic Oscillation Ocean gyre Physical oceanography Notes Sources The North Atlantic Current, elizabeth Rowe, Arthur J. Mariano, Edward H. Ryan, The Cooperative Institute for Marine and Atmospheric Studies
.svg)
