Geography of the United Kingdom

Geography of the United Kingdom

Most of England consists of rolling lowland terrain, divided east from west by more mountainous terrain in the Northwest (Cumbrian Mountains of the Lake District) and north (the upland moors of the Pennines) and limestone hills of the Peak District by the Tees-Exe line. The lower limestone hills of the Isle of Purbeck, Cotswolds, Lincolnshire and chalk downs of the Southern England Chalk Formation. The main rivers and estuaries are the Thames, Severn and the Humber Estuary. The largest urban area is Greater London. Near Dover, the Channel Tunnel links the United Kingdom with France. There is no peak in England that is 1000 metres (3,300 ft) or greater.

Wales is mostly mountainous, the highest peak being Snowdon at 1085 metres (3,560 ft) above sea level. North of the mainland is the island of Anglesey. The largest and capital city is Cardiff, located in South Wales.

Scotland's geography is varied, with lowlands in the south and east and highlands in the north and west, including Ben Nevis, the UK's highest mountain at 1343 metres (4,406 ft). There are many long and deep-sea arms, firths, and lochs. A multitude of islands west and north of Scotland are also included, notably the Hebrides, Orkney Islands and Shetland Islands. The largest city is Glasgow.

Northern Ireland, making up the north-eastern part of Ireland, is mostly hilly. The main cities are Belfast ('Beal Feirste' in Irish) and Londonderry / Derry ('Doire' in Irish). The province is home to one of the UK’s World Heritage Sites, the Giant's Causeway, which consists of more than 40,000 six-sided basalt columns up to 40 feet high (12.2 m).

In total it is estimated that the UK includes around 1098 small islands, some being natural and some being crannogs, a type of artificial island which was built in past times using stone and wood, gradually enlarged by natural waste building up over time.

The United Kingdom Parliament