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Geography of England
England comprises most of the central and southern two-thirds of the island of Great Britain, in addition to a number of small islands of which the largest is the Isle of Wight. England is bordered to the north by Scotland and to the west by Wales. It is closer to continental Europe than any other part of mainland Britain, divided from France only by a 33 km (21 mi) sea gap, the English Channel. The 50 km (31 mi) Channel Tunnel, near Folkestone, directly links England to mainland Europe. The English/French border is halfway along the tunnel.
Most of England consists of low hills and plains, with upland and mountainous terrain in the north and west. Uplands in the north include the Pennines, an upland chain dividing east and west, the Lake District, containing the highest mountains in the country, the Cheviot Hills across the Anglo-Scottish border, and the North York Moors near the North Sea. Uplands in the west include Dartmoor and Exmoor in the south west and the Shropshire Hills near Wales. The approximate dividing line between terrain types is often indicated by the Tees–Exe line. To the south of that line, there are larger areas of flatter land, including East Anglia and the Fens, although hilly areas include the Cotswolds, the Chilterns, and the North and South Downs.
The largest natural harbour in England is at Poole, on the south-central coast. Some regard it as the second largest harbour in the world, after Sydney, Australia, although this fact is disputed (see harbours for a list of other large natural harbours).
England has a temperate climate, with plentiful rainfall all year round. It has a milder climate than many places at similar latitudes: for example Newfoundland in Canada, and Sakhalin in Russia. The seasons are quite variable in temperature; however temperatures rarely fall below −5 °C (23 °F) or rise above 30 °C (86 °F). The prevailing wind is from the south-west, frequently bringing mild and wet weather to England from the Atlantic Ocean. It is driest in the east and warmest in the south, which is closest to the European mainland. Snowfall can occur in winter and early spring, although it is not very common away from high ground. England has warmer maximum and minimum temperatures throughout the year than the other countries of the UK, though Wales has milder minima from November to February, and Northern Ireland has warmer maxima from December to February. England is also sunnier throughout the year, but unlike Wales, Northern Ireland and Scotland, the sunniest month is July, totalling around 192.8 hours on average.
The highest temperature recorded in England is 40.3 °C (104.5 °F) on 19 July 2022 at Coningsby. The lowest temperature recorded in England is −26.1 °C (−15.0 °F) on 10 January 1982 at Edgmond, Shropshire. The climate of south-west England is rather distinct and somewhat milder than the rest of England. Crops, flowers and plants can be grown earlier there than in the rest of England and the UK.
England mainly lies within hardiness zone 8, but the Pennines and Cumbrian Mountains lie in the colder zone 7, and south west England, the Irish Sea coast, South coast and London lie in the warmer zone 9. A very small area, the Isles of Scilly, lies in the warmest zone in the British Isles, zone 10 which is close to subtropical.
The Geology of England is mainly sedimentary. The youngest rocks are in the south east, progressing in age in a north-westerly direction. The Tees–Exe line marks the division between younger, softer and low-lying rocks in the south east and older, harder, and generally a higher relief in the north-west. The geology of England is recognisable in the landscape of its counties, for instance Cumbria, Kent and Norfolk all have very distinct and very different looks from each other. The geology of Northern England and Western England tends to be somewhat closer to that of its near neighbours, Wales and Scotland, with the geology of Southern England and Eastern England being more aligned with that found across the North Sea and English Channel in Northern France, Belgium, and the Netherlands.
London is, by far, the largest urban area in England and one of the largest and busiest cities in the world. Other cities, mainly in central and northern England, are of substantial size and influence. The list of England's largest cities or urban areas is open to debate because, although the normal meaning of city is "a continuously built-up urban area", this can be hard to define, particularly because administrative areas in England often do not correspond with the limits of urban development, and many towns and cities have, over the centuries, grown to form complex urban agglomerations. For the official definition of a UK (and therefore English) city, see City status in the United Kingdom.
Hub AI
Geography of England AI simulator
(@Geography of England_simulator)
Geography of England
England comprises most of the central and southern two-thirds of the island of Great Britain, in addition to a number of small islands of which the largest is the Isle of Wight. England is bordered to the north by Scotland and to the west by Wales. It is closer to continental Europe than any other part of mainland Britain, divided from France only by a 33 km (21 mi) sea gap, the English Channel. The 50 km (31 mi) Channel Tunnel, near Folkestone, directly links England to mainland Europe. The English/French border is halfway along the tunnel.
Most of England consists of low hills and plains, with upland and mountainous terrain in the north and west. Uplands in the north include the Pennines, an upland chain dividing east and west, the Lake District, containing the highest mountains in the country, the Cheviot Hills across the Anglo-Scottish border, and the North York Moors near the North Sea. Uplands in the west include Dartmoor and Exmoor in the south west and the Shropshire Hills near Wales. The approximate dividing line between terrain types is often indicated by the Tees–Exe line. To the south of that line, there are larger areas of flatter land, including East Anglia and the Fens, although hilly areas include the Cotswolds, the Chilterns, and the North and South Downs.
The largest natural harbour in England is at Poole, on the south-central coast. Some regard it as the second largest harbour in the world, after Sydney, Australia, although this fact is disputed (see harbours for a list of other large natural harbours).
England has a temperate climate, with plentiful rainfall all year round. It has a milder climate than many places at similar latitudes: for example Newfoundland in Canada, and Sakhalin in Russia. The seasons are quite variable in temperature; however temperatures rarely fall below −5 °C (23 °F) or rise above 30 °C (86 °F). The prevailing wind is from the south-west, frequently bringing mild and wet weather to England from the Atlantic Ocean. It is driest in the east and warmest in the south, which is closest to the European mainland. Snowfall can occur in winter and early spring, although it is not very common away from high ground. England has warmer maximum and minimum temperatures throughout the year than the other countries of the UK, though Wales has milder minima from November to February, and Northern Ireland has warmer maxima from December to February. England is also sunnier throughout the year, but unlike Wales, Northern Ireland and Scotland, the sunniest month is July, totalling around 192.8 hours on average.
The highest temperature recorded in England is 40.3 °C (104.5 °F) on 19 July 2022 at Coningsby. The lowest temperature recorded in England is −26.1 °C (−15.0 °F) on 10 January 1982 at Edgmond, Shropshire. The climate of south-west England is rather distinct and somewhat milder than the rest of England. Crops, flowers and plants can be grown earlier there than in the rest of England and the UK.
England mainly lies within hardiness zone 8, but the Pennines and Cumbrian Mountains lie in the colder zone 7, and south west England, the Irish Sea coast, South coast and London lie in the warmer zone 9. A very small area, the Isles of Scilly, lies in the warmest zone in the British Isles, zone 10 which is close to subtropical.
The Geology of England is mainly sedimentary. The youngest rocks are in the south east, progressing in age in a north-westerly direction. The Tees–Exe line marks the division between younger, softer and low-lying rocks in the south east and older, harder, and generally a higher relief in the north-west. The geology of England is recognisable in the landscape of its counties, for instance Cumbria, Kent and Norfolk all have very distinct and very different looks from each other. The geology of Northern England and Western England tends to be somewhat closer to that of its near neighbours, Wales and Scotland, with the geology of Southern England and Eastern England being more aligned with that found across the North Sea and English Channel in Northern France, Belgium, and the Netherlands.
London is, by far, the largest urban area in England and one of the largest and busiest cities in the world. Other cities, mainly in central and northern England, are of substantial size and influence. The list of England's largest cities or urban areas is open to debate because, although the normal meaning of city is "a continuously built-up urban area", this can be hard to define, particularly because administrative areas in England often do not correspond with the limits of urban development, and many towns and cities have, over the centuries, grown to form complex urban agglomerations. For the official definition of a UK (and therefore English) city, see City status in the United Kingdom.