Physical Geography
The physical geography of the UK varies greatly. England consists of mostly lowland terrain, with upland or mountainous terrain only found north-west of the Tees-Exe line. The upland areas include the Lake District, the Pennines, Exmoor and Dartmoor. The lowland areas are typically traversed by ranges of low hills, frequently composed of chalk. The physical geography of Scotland is distinguished by the Highland Boundary Fault which traverses the Scottish mainland from Helensburgh to Stonehaven. The faultline separates the two distinctively different regions of the Highlands to the north and west, and the lowlands to the south and east. Wales is mostly mountainous, though south Wales is less mountainous than north and mid Wales. The geography of Ireland includes the Mourne Mountains as well as Lough Neagh, at 388 square kilometres (150 sq mi), the largest body of water in the UK and Ireland.
The overall geomorphology of the UK was shaped by the combined forces of tectonics and climate change, in particular glaciation.
The exact centre of the island of Great Britain is disputed. Depending upon how it is calculated it can be either Haltwhistle in Northumberland, or Dunsop Bridge in Lancashire.
Read more about this topic: Geography Of The United Kingdom
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