UK's Physical Landscape
- A landscape is defined as:
The character of an area, resulting from the action and interaction of natural and human elements
- A landscape's character will depend on its initial geology, which gives a landscape its relief, which in turn attracts human action/interaction, for example:
- Slate, (a type of resistant rock) found in the mountains of North Wales, attracted people to quarry for roofing material and generated over four-fifths of all British slate during the Industrial Revolution
Map of upland and lowland UK showing glacial limit and major rivers
Past tectonic activity
- Plate movement has moved the UK from the tropics
- It was partially submerged in warm shallow water which formed the limestones of the Peak District, parts of south Wales and south-west England
- The chalks and clays of England are the youngest rocks in the UK
- These formed in the swamps and shallow seas before the tectonic plates moved the UK to its present position
- When the plates collided, it forced the rocks to fold and uplift creating the mountain ranges of the uplands:
- Scottish Highlands, Snowdonia, and the Lake district etc.
- The pressure and heat created the slate, shale and schist of the uplands
- The UK used to be much closer to a plate boundary than it is now, and volcanic activity formed the granite (igneous rock) of the upper landscape:
- The Giant's Causeway in Northern Ireland is made of huge hexagonal columns of basalt
Glaciation
- During the last Ice Age, both upland and lowland UK landscapes were affected
- The Tees-Exe line roughly marks the southern limit of the UK's glaciation
- Ice sheets covered the upland UK with glaciers forming distinctive places such as Snowdonia and the Lake District
- Lowland UK was affected through a glacial wash of clay and debris