Geography of Scotland

The geography of Scotland is varied, from rural lowlands to unspoilt uplands, and from large cities to sparsely inhabited islands. Located in Northern Europe, Scotland comprises the northern one third of the island of Great Britain as well as 790 surrounding islands encompassing the major archipelagoes of the Shetland Islands, Orkney Islands and the Inner and Outer Hebrides.

Scotland's only land border is with England, which runs for 60 miles (97 km) in a northeasterly direction from the Solway Firth in the west to the North Sea on the east coast. Separated by the North Channel, the island of Ireland lies 13 miles (21 km) from Mull of Kintyre on the Scottish mainland. Norway is located 190 miles (310 km) to the northeast of Scotland across the North Sea. The Atlantic Ocean, which fringes the coastline of western and northern Scotland and its islands, influences the temperate, maritime climate of the country.

Scotland contains the majority of mountainous terrain in the UK. The topography of Scotland is distinguished by the Highland Boundary Fault – a geological rock fracture – which traverses the Scottish mainland from Helensburgh to Stonehaven. The faultline separates two distinctively different physiographic regions; namely the Highlands to the north and west and the Lowlands to the south and east. The more rugged Highland region contains the majority of Scotland's mountainous terrain, including the highest peak, Ben Nevis.

Lowland areas, in the southern part of Scotland, are flatter and home to most of the population, especially the narrow waist of land between the Firth of Clyde and the Firth of Forth known as the Central Belt.Glasgow is the largest city in Scotland, although Edinburgh is the capital and political centre of the country. While the Lowlands are less elevated, upland and mountainous terrain is located across the Southern Uplands.

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