英语国家概况第一章

Chapter1Land and PeopleGreat Britain is the largest island in Europe. It is made up of England, Scotland, and Wales.Together with Northern Ireland, it forms the United Kingdom of Great Britain and Northern lreland. This is the full name of the country which constitutes all these places. The United Kingdom of Great Britain and Northern Ireland, or the United Kingdom, is “the UK" for short. However,most people call the UK ”Britain" or “Great Britain,” and some people simply say “England," which is incorrect and particularly annoys the Scots.According to the 2011 census, the total population of the UK was around 63 million. It is the third-largest in the European Union (behind Germany and France) and the 22nd-largest in the world.The UK is a developed country. According to 2013 statistics it has the sixth-largest national economy in the world (and third-largest in Europe) measured by nominal GDP and eighth-largest in the world (and second-largest in Europe) measured by purchasing power parity (PPP). It was the world's first industrialized country and the world's foremost power during the 19th and early 20th centuries. The UK remains a great power because it still has considerable economic,cultural,military,scientific and political influence internationally.The capital of the UK is London, which is among the world's leading commercial, financial,and cultural centers. Other major cities include Birmingham,Liverpool, and Manchester in England, Belfast and Londonderry in Northern Ireland, Edinburgh and Glasgow in Scotland, and Swansea and Cardiff in Wales.I.Geographical Features1. The UK's Geographical Location and Its SizeThe UK is bordered on the south by the English Channel. It is bordered on the east by the North Sea, and on the west by the Irish Sea and the Atlantic Ocean. The UK's only land border with another nation is between Northern Ireland and Ireland.The UK is separated from the rest of Europe by the English Channel. The English Channel between England and France is quite narrow and the narrowest part is called the Suraits of Dover, which is only 33 km across. In 1985 the British government and the French government decided to build a channel tunnel under the Straits of Dover so that England and France could be joined together by road. After eight years of hard work this channel tunnel, which is called"Chunnel,” was open to traffic in May 1994.The UK covers a total area of 244,110 sq km. lt runs 1,000 km from north to south and extends,at the widest part, about 500 km. So no part of the UK is very far from the coast and it provides a valuable resource. The British coast is long and has good, deep harbors. Sea routes extend far inland, providing cheap transportation.England is the largest, most populous, and wealthiest division of the UK. It makes up 130,400 sq km of the UK's total area.The area of Scotland is 78,800 sq km, the area of Wales is20,800 sq km, and the area of Northern Ireland is 14,100 sq km.This means that England makes up 53.4% of the area of the UK, Scotland 32.3%, Wales 8.5%, and Northern Ireland 5.8%.2.Rivers and LakesSince the UK has a moist climate with much rainfall, it has many rivers and lakes.Rivers in central and eastern Britain tend to flow slowly and steadily all year long because they are fed by the frequent rain. Many have been navigable, and from the earliest times they have served peoples interested in either commerce or invasion. The Highlands act as a divide and determine whether rivers flow west to the Irish Sea or east to the North Sea.Rivers and streams moving westward down from the Highlands tend to be swift and turbulent; rivers flowing eastward tend to be long and gentle, with slowly moving waters.The Thames and the Severn are the longest rivers in Britain and are almost equal in length. The Severn flows south out of the mountains of central Wales to the Bristol Channel at Bristol. It is 354 km long. The Thames,338 km long, flows eastward out of the Cotswold Hills and weaves through the metropolis of London. The Thames provides water to the city of London and is used to carry commercial freight. Other important rivers in England are the Mersey,which enters the Irish Sea at Liverpool; the River Humber on the east coast,into which the Trent River and several other rivers flow; and the Tyne River in northern England,which flows past Newcastle upon Tyne to the North Sea.In Scotland the important rivers are the Clyde and the Forth, which are joined by a canal. The River Clyde flows northwest, past Glasgow, and empties into the Atlantic at the Firth of Clyde. (Firth is the Scottish name for an arm of the sea that serves as the broad estuary of a river.) The River Forth flows eastward into the Firth of Forth, where Edinburgh rises on its south bank.The most important rivers in Northern Ireland are the Lagan, the Bann, and the Foyle.Most of the large lakes in the UK are located in the upland areas of Scotland and northern England,although Lough Neagh in Northern Ireland is the largest lake in the UK. Loch Lomond, on the southwestern edge of the Highlands of Scotland, is the largest on the island of Great Britain, measuring 37 km long and from 1.6 to 8 km ke Windermere is the largest of 15 major lakes in the famous Lake District of northwestern England.It is about 1.6 km wide and more than 16 km long.Ⅱ.Climate1.A Maritime ClimateWhen we say climate we mean the average weather conditions at a certain place over a period of years.We don’t mean the day-to-day weather conditions at a certain place. Though it seems that people are always complaining about the weather in the UK because it is rainy and so changeable and unpredictable,the climate in the UK is in fact a favorable one. The UK has a maritime climate. Winters are mild,not too cold and summers are cool,not too hot.It has a steady reliable rainfall throughout the whole year.It has a small range of temperature.The average temperature in winter in the north is 4—6℃and in summer in the south is 12—17℃.So even in winter one can still see stretches of green grass in the open country,in the parks and round the houses.2.Factors Which Influence the ClimateThe UK is an island country which lies between latitude 50°to 60°north. It lies farther north than even the northernmost par of Heilonjiang Province of China. Compared with other countries of the same latitudes it has a more moderate climate. This is influenced mainly by three factors:(1)The surrounding waters tend to balance the seasonal differences by heating up the land in winter and cooling it off in summer. As the sea heats up and cools off relativelyb slowly it brings warm air in winter and cool air in summer.(2)The prevailing southwest winds or the Westerlies (winds which come from the west) blow over the country all the year round, bringing warm and wet air in winter and keeping the temperatures moderate.(3) The North Atlantic Drift, which is a warm current, passes the western coast of the British Isles and warms them.Since the UK's climate is of the maritime type, it is characterized by cool temperatures, frequent cloudy days and rainstorms. It changes from day to day, and this makes it difficult to forecast. It is so changeable that sometimes one can experience four seasons in the course of a single day. Day may break as a fine spring morning; an hour or so later black clouds may have appeared from nowhere and rain may be pouring down. At midday conditions may really be wintery with the temperatures down to about 8 °C. Then in the Jater atfternoon the sky will be clear, the sun will begin to shine again, and for an hour or two before darkness falls, it will be summer. It has been said that the uncertainty about the weather has had a definite effect upon the Englishman's character. It tends to make him cautious, for example. You may laugh when you see an Englishman going out on a brilliantly sunny morning wearing a raincoat and carrying an umbrella. However, most frequently it comes in drizzles and you don't necessarily need an umbrella.3.RainfallThe UK has a steady reliable rainfall throughout the whole year.The average annual rainfall in the UK is over 1,000 mm. It has 750 mm to 1,250 mm of rainfall along the coast in the east and south except a small area in the southeastern corner of the country which receives less than 750 mm. In the west there is as much as 1,250 mm to 2.000 mm of rainfall and in some areas in the northwest it is over 2,000 mm.The Westerlies blow over the UK all the year round, bringing warm and wet air from the Atlantic Ocean. They rise, climb the highlands and the mountains in the west, become colder and then cause heavy rainfall. There is not so much rainfall in the east because after climbing over the highlands and mountains the air gets warmer and drier when it descends and does not give so much rain.As a result of the rainfall distribution in Britain there is a water surplus in the north and west, and a water deficit in the south and east. Reservoirs have therefore to be built in such highland areas as Central Wales,the Lake District and the Scottish Highlands, so that water can be stored here and then transferred to the more populated and industrial areas of lowland Britain.Generally speaking,the climate in the UK is favorable and equable (neither too hot nor too cold).Extremes of heat or cold, or of drought or prolonged rainfall are rarely experienced. It is estimated that on average about 3-6 cubic meters of rain per person per day fall over the UK. Thisis far more than is needed,but problems still remain. Sometimes there are several months of drought, and at other times too much rain causes flooding. Fog,smog, frost and severe gales are not uncommon and often cause great damage to crops and to people's life. In 1952 the sulphur dioxide in the four-day London smog,an unhealthy atmosphere formed by mixing smoke and dirt with fog, left 4,000 people dead or dying.Since then most cities in the UK have introduced “clean air zones” whereby factories and households are only allowed to burn smokeless fuel.Although the UK does not experience hurricanes, that is,storms with a strong fast wind such as typhoons or cyclones, many areas are subjected to severe gales, especially in winter.III.Plant and Animal Life1.Plant LifeThe mild climate,ample rain, and long growing season in the UK support a great variety of plants,which grow exceptionally well. Most of the UK was once covered with thick,deciduous forests in which oak trees predominated.(Deciduous trees are those that lose their leaves every year.)The impact of centuries of dense human polpulation has massively altered the flora of the UK, and only tiny remnants of these forests remain today.Before they were affected by centuries of clearing and human use, the great oak forests spread over the best soils in Britain. Forests were unable to establish themselves in the poorer soils of the mountains,wetlands,heath,and moorlands.The plants common to these wilder areas are heather,gorse and peat moss.These regions have been altered by heavy grazing of livestock and by controlled burning.Controlled burning creates environments suitable for game birds,which feed on the shoots of the new covered by towns and farmland.The marginal wetlands that remain continue to be threatened by reclamation for farms and homes,and some wetland plant species now grow only in conservation areas.2. Animal LifeBritain has many smaller mammals, and the larger ones tend to be gentle. The only surviving large mammals are red deer, which live in the Scottish Highlands and in Exmoor in southwestern England, and roe deer, foud in the woodlands of Scotland and southern England. At one time boars (wild pigs) and wolves roamed Britain, but they were hunted to extinction.Many smaller mammals inhabit Britain, including foxes,otters, red squirrels, and wildcats. Otters are found mainly in southwestern England and in the Shetland and Orkney islands.The red squirrel, driven out of most of its range by the imported gray squirrel, is now limited mainly to the Isle of Wight and Scotland. Wildcats are found only in parts of Scotland.Bird-watching is a popular national pastime. Britain is home to a large variety of birds, due in lange measure to its position as a focal point of a migratory network.Saltwater fish were once important to Britain's economy. Cod, herring and mackerel are still caught off the coasts of Britain, although quotas are now imposed. Lobster, crab,and other shellfish are caught along inshore waters.IV. People1.Ethnic GroupsFor centuries people have migrated to the British Isles from many parts of the world,some to avoid political or religious persecution, others to find a better way of life or to escape poverty. In historic times migrants from the European mainland joined the indigenous population of Britain during the Roman Empire and during the invasions of the Angles,Saxons,Jutes,Danes,and Normans. The Irish have long made homes in Great Britain.Many Jews arrived in Britain toward the end of the 19th century and in the 1930s. After 1945 large numbers of other European refugees settled in the country. The large immigrant communities from the West Indies and South Asia date from the 1950s and 1960s. There are also substantial groups of Americans, Australians, and Chinese, as well as various other Europeans, such as Greeks, Russians,Poles, Serbs, Estonians, Latvians, Armenians,Turkish Cypriots, Italians, and Spaniards. Beginning in the early 1970s, Ugandan Asians and immigrants from Latin America, Southeast Asia, and Sri Lanka have sought refuge in Britain. People of Indian, Pakistani, and Bangladeshi origin account for more than half of the total ethnic minority population, and people of West Indian origin are the next largest group. The foreign-born element of the population is concentrated in inner-city areas, and more than half live in Greater London.nguagesOf the surviving languages the earliest to arrive in Britain were the two forms of Celtic: the Goidelic (from which Irish, Manx, and Scottish Gaelic derive) and Brythonic (from which the old Cornish language and modern Welsh have developed). Among the contemporary Celtic languages Welsh is the strongest: about one-fifth of the total population of Wales are able to speak it. Scottish Gaelic is strongest among the inhabitants of the islands of the Outer Hebrides and Skye, although it is still heard in the nearby North West Highlands.In Northern Ireland very little Irish is spoken. The last native speakers of Cornish died in the 18th century.The second link with Indo-European is through the ancient Germanic language group, two branches of which, the North Germanic and the West Germanic, were destined to make contributions to the English language. Modern English is derived mainly from the Germanic dialects spoken by the Angles, Saxons, and Jutes (who all arrived in Britain in the 5th century AD) and heavily influenced by the language of the Danes (Vikings), who began raiding the British Isles in about 790 and later colonized parts of northern and eastern England.Under the Norman and Angevin kings, England formed part of a continental empire,and the prolonged connection with France retained by its new rulers and landlords made a deep impression on the English language. Many additions to the English language have been made since the 14th century,but the Normans were the last important linguistic group to enter Britain.3.ReligionThe various Christian denominations in the UK have emerged from schisms that divided the church over the centuries.The greatest of these occurred in England in the 16th century, when Henry VIII rejected the supremacy of the Pope. This break with Rome facilitated the adoption of some Protestant tenets (a principle or belief held by a person) and the founding of the Church of England,still the state church in England,although Roman Catholicism has retained adherents (supporters).In Scotland the Reformation gave rise to the Church of Scotland,which was governed by presbyteries—local bodies composed of ministers and elders—rather than by bishops,as was the case in England.Roman Catholicism in Ireland as a whole was almost undisturbed by theseevents,but in what became Northern Ireland the Anglican and Scottish (Presbyterian) churches had many adherents.The British tradition of religious tolerance has been particularly important since the 1950s, when immigrants began to introduce a great variety of religious beliefs.There are large and growing communities that pactice Islam, Hinduism, and Sikhism.The largest number of Muslims came from Pakistan and Bangladesh.,The lange Sikh and Hindu communities originated in India. There are also many Buddhist groups.4.UrbanizationBy any standard the UK is among the most urbanized of countries. The greatest overall change that accompanied Britain's early industrial development was, in fact, the large-scale urbanization. The increasing percentage of employees in offices and service industries ensures continued urban growth, Of every 10 people in the UK, nine live in towns and more than three of them in one of the country's 10 largest metropolitan areas. The Greater London metropolitan area—the greatest port, the largest center of industry, the most important center of office employment, and the capital city—is by far the largest of these. The need for accommodating business premises (offices) has displaced population from Inner London, and this outward movement, in part, has led to the development of new towns outside the 16-km-wide Green Belt that surrounds London's built-up area.Large metropolitan areas also formed in industrial areas during the 19th and early 20th centuries.Although coalfields or textile manufacture started the initial growth of many of these urban areas, coal mining had virtually ceased in all of them by the end of the 20th century, and heavy industry and textile production had given way to a more diverse form of manufacturing and service activities. Birmingham dominates the extensive built-up area of the West Midlands metropolitan area,but the industrial Black Country—named for its formerly polluted skies and grimy buildings—also has several large and flourishing towns.In Greater Manchester, with a similar number of inhabitants, urbanization accompanied the mechanization of the cotton textile industry. Across the Pennines similar mechanization of wool textiles created the West Yorkshire metropolitan area, with Leeds and Bradford as its twin centers. The metropolitan area of Tyne and Wear (centered on Newcastle upon Tyne) and the Greater Glasgow metropolitan area are also located on coalfields. Greater Glasgow has about one-third of Scotland's people. Merseyside (centered on Liverpool) has traditionally served as a seaport and distribution center for Greater Manchester and the rest of Lancashire.Other large metropolitan areas in Great Britain include South Yorkshire(centered on Sheffield),Nottingham,and Bristol.About one-fifth of Northern Ireland’s people live in Belfast.In addition to these large metropolitan areas,there are many other minor urban areas and large towns,several of which line the coast.With so much urban and suburban concentration, the problems of air,water,and noise pollution have caused much concern in the UK. Clean-air legislation has brought considerable progress in controlling air pollution.Smoke-control areas have been established in most cities and towns, and there has been a shift from coal to cieaner fuels.Pollution of the rivers remains a large problem, particularly in the highly industrialized parts of the UK, but vigilance,research, and control by the National River Authorities and general public concern for the environment are encouraging features of contemporary Britain.5. Population GrowthFrom the 18th century until well into the 19th century, Britain's population soared as the death rate dropped and the birth rate remained high. During this period the total population increased from about 6 million in the 1760s to 26 million in the 1870s. Toward the end of the 19th century and into the 20th century the birth rate stabilized and the death rate remained low. The population took on the characteristics of a modern, developed,and prosperous state. Family size decreased and the median age of the population pared to the rest of the world, the UK has a smaller percentage of younger people and a higher percentage of older people, with more than 20% over the age of 60; those under the age of 15 make up only 13% of the population. Britain's population has been growing slowly, slower than the average for countries in the European Union (EU).6. Migration PatternsBeginning in the 1950s, the immigration of nonwhite(“New Commonwealth") people from such developing nations as India, Pakistan, and the countries of the West Indies became significant, and from 1957 until 1962 there was a net migration gain. Since then restriction on the entry of New Commonwealth citizens has decreased the primary inflow,but dependents of immigrants already in the UK are still admitted. The reasons for restricting entry were in part economic but were also associated with the resistance of the existing population to the new arrivals. Nevertheless, thc UK continues to gain people from the New Commonwealth.Migration within the UK has at times been sizable. Until 1700 the relatively small population was sparsely distributed and largely rural and agricultural, much as it had been in medieval times. From the mid-18th century, scientific and technological innovations created the first modern industrial state.At the same time, agriculture underwent technical and tenurial changes that allowed increased production with a smaller workforce, and revolutionary improvements in transport made the movement of materials and people easier. As a result,by the late 19th century a mainly rural population had largely become a nation of industrial workers and town dwellers.Industry, as well as the urban centers that inevitably grew up around it, concentrated near the coalfields,while the railway network, which grew rapidly ather 1830,enhanced the commercial importance of many towns.The migration of people,especially young people, from the country to industrialized towns took place at an uprecedented rate in the early railway age, and such movements were relatively confined geographically.Migration from agricultural Ireland was an exception, for, when the disastrous potato disease of 1845-1849 led to widespread famine, large numbers moved to Great Britain to become urban workers in Lancashire,Clydeside (the Glasgow region), and London.The rural exodus (a lot of people leaving a place at the same time) went on, but on a greatly reduced scale after 1901.Soon after World War I, new interregional migration flows began when the formerly booming 19th-century industrial and mining districts lost much of their economic momentum. Declining heavy industry in Clydeside, northeastern England, South Wales, and parts of Lancashire and Yorkshire caused a lot of people to lose jobs, and many migrated to the relatively more prosperous Midlands and southern England. This movement of people continued until it was checked by the relatively full employment conditions that occurred soon after the start of World War II.In the 1950s job opportunities in the UK improved with government sponsored diversification of industry, reducing the volume of migration to the south. The decline of certain northern industries—coal mining, shipbuilding, and cotton textiles in particular—had nevertheless reached a critical level by the late 1960s, and the emergence of new growth points in the West Midlands and southeastern England made the drift to the south a continuing feature of British economic life. During the 1960s and 1970s the areas of most rapid growth were East Anglia, the South West, and the East Midlands, partly because of limitations on growth in Greater London and the development of new towns in surrounding areas.During the 1980s the government largely abandoned subsidies for industry and adopted a program of rationalization and privatization. This resulted in the collapse of coal mining and heavy industry in the north and the West Midlands of England and in the Lowlands of Scotland and a similar loss of heavy industry in Northern Ireland, thus creating a wave of migration from these regions to the more prosperous south of England, especially East Anglia,the East Midlands,and the South West.As the economy became stable during the 1990s,migration from Scotland, Northern Ireland, and northern England decreased.While the South East (including Greater London) was the chief destination of external immigrants into Britain, this region, along with the West Midlands, produced a growing internal migration to surrounding regions of England during the 1990s. This pattern reflected a larger trend of migration out of older urban centers throughout Britain to surrounding rural areas and small towns at the end of the 20th century.。