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Great Britain (Scottish Gaelic: Breatainn Mhòr, Welsh: Prydain Fawr, Cornish: Breten Veur, Scots: Graet Breetain) is the larger of the two main islands of the British Isles, the largest island in Europe and the ninth largest island in the world. Great Britain is also the third most populated island on earth, with a population of 58 million people and is the world's 5th largest economy. It lies to the northwest of Continental Europe, with Ireland to the west, and makes up the largest part of the territory of the country known as the United Kingdom of Great Britain and Northern Ireland. It is surrounded by over 1,000[2] smaller islands and islets.
Great Britain (Scottish Gaelic: Breatainn Mhòr, Welsh: Prydain Fawr, Cornish: Breten Veur, Scots: Graet Breetain) is the larger of the two main islands of the British Isles, the largest island in Europe and the ninth largest island in the world. Great Britain is also the third most populated island on earth, with a population of 58 million people and is the world's 5th largest economy. It lies to the northwest of Continental Europe, with Ireland to the west, and makes up the largest part of the territory of the country known as the United Kingdom of Great Britain and Northern Ireland. It is surrounded by over 1,000[2] smaller islands and islets.
England, Scotland and Wales are mostly situated on the island, along with their capital cities, London, Edinburgh and Cardiff respectively.
Geographical definition
Great Britain is the largest island of the British Isles. It lies to the northwest of Continental Europe, with Ireland to the west, and makes up the larger part of the territory of the United Kingdom. It is surrounded by 1000 smaller islands and islets. It occupies an area of 209,331 km² (80,823 square miles).
It is the third most populous island after Java and Honshū.
Great Britain stretches over about ten degrees of latitude on its longer, north–south axis. Geographically, the island is marked by low, rolling countryside in the east and south, while hills and mountains predominate in the western and northern regions.
The English Channel is of geologically recent origins, having been dry land for most of the Pleistocene period. It is thought to have been created between 450,000 and 180,000 years ago by two catastrophic glacial lake outburst floods caused by the breaching of the Weald-Artois Anticline, a ridge which held back a large proglacial lake in the Doggerland region, now submerged under the North Sea. The flood would have lasted several months, releasing as much as one million cubic metres of water per second. The cause of the breach is not known but may have been caused by an earthquake or simply the build-up of water pressure in the lake. As well as destroying the isthmus that connected Britain to continental Europe, the flood carved a large bedrock-floored valley down the length of the English Channel, leaving behind streamlined islands and longitudinal erosional grooves characteristic of catastrophic megaflood events.
Population
The population of Great Britain (1995 estimate) is about 58,093,000. The overall population density is 238 persons per sq km (616 per sq mi). A small percentage of Britons live in rural areas; 89 percent are urban dwellers. The largest cities in Great Britain are London (population, 1991 preliminary, 6,803,100), Birmingham (934,900), Leeds (674,400), and Glasgow (654,542). Most Britons (94 percent) are either English, Scottish, Irish, or Welsh. The remainder include Indians, West Indians, Pakistanis, Africans, Bangladeshis, Chinese, and Arabs. The country's official language is English. Numerically, the Church of England (or Anglican Church) has the largest number of adherents of any religion in Great Britain, accounting for 48 percent of the population; most members reside in England. The second largest religion, statistically, is Roman Catholicism (16 percent); Catholics reside throughout the kingdom. Other religions include Protestantism (which includes the state religions of both Wales and Scotland), Islam, Judaism, Hinduism, and Sikhism.
For further information on population distribution, principal cities, racial origins, religion, and culture in England, Scotland, Wales, and Northern Ireland, see the articles dealing with the component parts of the kingdom.
Climate of Great Britain
The climate in Great Britain is generally mild and temperate due to the influence of the Gulf Stream. The south-western winds carry the warmth and moisture into Britain. The climate in Britain is usually described as cool, temperate and humid.
British people say: "Other countries have a climate, in England we have weather."
The weather in Britain changes very quickly. One day may be fine and the next day may be wet. The morning may be warm and the evening may be cool. Therefore it is natural for the people to use the comparison "as changeable as the weather" of a person who often changes his mood or opinion about something. The weather is the favourite topic of conversation in Britain. When two Englishmen are introduced to each other, if they can't think of any thing else to talk about, they talk about weather. When two people meet in the street they will often say something about weather as they pass, just to show their friendliness.
Every daily paper publishes a weather forecast. Both the radio and television give the weather forecast several times each day.
The English also say that they have three variants of weather: when it rains in the morning, when it rains in the afternoon or when in rains all day long. Sometimes it rains so heavily that they say "It's raining cats and dogs".
Rainfall is more or less even throughout the year. In the mountains there is heavier rainfall then in the plains of the south and east. The driest period is from March to June and the wettest months are from October to January. The average range of temperature (from winter to summer) is from 15 to 23 degrees above zero. During a normal summer the temperature sometimes rises above 30 degrees in the south. Winter temperatures below 10 degrees are rare. It seldom snows heavily in winter, the frost is rare. January and February are usually the coldest months, July and August the warmest. Still the wind may bring winter cold in spring or summer days. Sometimes it brings the whirlwinds or hurricanes. Droughts are rare.
So, we may say that the British climate has three main features: it is mild, humid and changeable. That means that it is never too hot or too cold. Winters are extremely mild. Snow may come but it melts quickly. In winter the cold is humid cold, not the dry one.
This humid and mild climate is good for plants. The trees and flowers begin to blossom early in spring.
In the British homes there has been no central heating up till recently. The fireplaces are often used. but the coal is not used as it's very expensive. Britain has no good coal now and imports it itself. Many schools and universities have no central heating either, and the floors there are made of stone. The British bedroom is especially cold, sometimes electric blankets or hotwater bottles are used.