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Book created by:Laurentiu Lungu
Anas Haraka
Sotiraq Gega
Andrea Giordano
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 archipelagos of the Shetland Islands, Orkney Islands and the Inner and Outer Hebrides.
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.
Geology and morphology
The land area of Scotland is around 80,240 km², which is equivalent to 32% of the area of the UK. The mainland of Scotland has 9,910 km of coastline.
The morphology of Scotland was formed by the action of tectonic plates, and subsequent erosion arising from glaciation. The major division of Scotland is the Highland Boundary Fault, which separates the land into 'highland' to the north and west, and 'lowland' to the south and east.
The oldest rocks of Scotland are the Lewisian gneisses, which were formed in the Precambrian period, up to 3 billion years ago. They are among the oldest rocks in the world.
The morphology of Scotland was formed by the action of tectonic plates, and subsequent erosion arising from glaciation. The major division of Scotland is the Highland Boundary Fault, which separates the land into 'highland' to the north and west, and 'lowland' to the south and east.
The oldest rocks of Scotland are the Lewisian gneisses, which were formed in the Precambrian period, up to 3 billion years ago. They are among the oldest rocks in the world.
During the Precambrian, the Torridonian sandstones and the Moine were also laid down. Further sedimentary deposits were formed through the Cambrian period, some of which metamorphosed into the Dalradian series. The area which would become Scotland was at this time close to the south pole.
Scotland's wildlife is typical of the north-west of Europe, although several of the larger mammals such as the lynx, brown bear, wolf, elk and walrus were hunted to extinction in historic times. There are important populations of seals and internationally significant nesting grounds for a variety of seabirds such as gannets. The golden eagle is something of a national icon.
Scotland's wildlife is typical of the north-west of Europe, although several of the larger mammals such as the lynx, brown bear, wolf, elk and walrus were hunted to extinction in historic times. There are important populations of seals and internationally significant nesting grounds for a variety of seabirds such as gannets. The golden eagle is something of a national icon.
Topography
Scotland contains the most mountainous terrain in Great Britain. Much of the highest uplands lie to the north and west of the Highland Boundary Fault in the Northwest Highlands and Grampian ranges. The jagged Cuillin, on the Isle of Skye, represents a major mountain range that is not located on the Scottish mainland. Located at the western end of the Grampian Mountains, at an altitude of 1,345 m, Ben Nevis is the highest mountain in Scotland and Great Britain.
Mountains in Scotland are categorised by their height. Peaks over 3,000 ft (914.4 m) are known as Munros. There are 282 Munros in Scotland, all within the Highlands.
The west coast in particular is heavily indented, with long promontories separated by fjordlike sea lochs. The east coast is more regular, with a series of large estuarine inlets, or firths, and long sandy beaches, for example at Aberdeen. Much of the Scottish coastline consists of a machair formation, a dune pasture land formed as sea levels subsided.
Mountains in Scotland are categorised by their height. Peaks over 3,000 ft (914.4 m) are known as Munros. There are 282 Munros in Scotland, all within the Highlands.
The west coast in particular is heavily indented, with long promontories separated by fjordlike sea lochs. The east coast is more regular, with a series of large estuarine inlets, or firths, and long sandy beaches, for example at Aberdeen. Much of the Scottish coastline consists of a machair formation, a dune pasture land formed as sea levels subsided.