Distinctive Landscapes

Landscapes

  • A landscape comprises of all the visible features of an area of land
  • This includes physical features and human features
    • A landscape with more physical features, such as mountains or forest, is described a as natural landscape
    • A landscape with more human features, such as towns or cities, is described as a built landscape

UK Landscapes

  • The UK has a varied physical landscape as the relief of the land changes in various parts of the country
  • Relief refers to the way landscapes change in height
  • Upland areas are high above sea level
    • These are mostly found in the north and west of the UK
    • They are generally formed of harder rocks such as slate and granite
    • The land is often steep
    • The climate tends to be cooler and wetter
    • The harsh climate and thin soils allow rough vegetation to thrive, and some upland areas are used for forestry
    • Land uses include sheep farming, quarrying and tourism
    • Found in
      • Scotland – The Northwest Highlands, Grampian Mountains, Southern Uplands
      • England – The Pennines, Lake District, Dartmoor
      • Wales – The Brecon Beacons, Snowdonia
  • Lowland areas are not very high above sea level
    • These are mostly found in the south and east of the UK
    • They are generally formed of softer rock such as chalk and clay
    • The land is often flat with rolling hills
    • Vegetation grows easily in the fertile soil and includes grassy meadows and deciduous forests
    • Land uses include dairy and arable farming, quarrying and tourism
    • Most urban areas and industries are in lowland areas
    • Found in Lincolnshire, The Fens in East Anglia, Midlands, London Basin, Vale of York
  • Glaciated landscapes are formed from where ice covered the land in the ice age and left valleys and deposited material
    • They are mostly found in upland areas and in the north-west of the UK
    • In upland Britain, glaciation carved huge, U-shaped valleys and eroded down steep mountain peaks and ridges
    • In non-glaciated lowland areas, periglacial conditions during the ice age formed V-shaped valleys as the water eroded the chalk permafrost