Upland Landscapes
- The physical landscape of the UK is due to geological processes over time
- Processes involved are:
- Weathering: breakdown of rock in their original place
- Mass movement: weathered material moving down slopes under the influence of gravity
- Erosion, transportation and deposition by rivers
- Geologically the UK is split in half, with an imaginary boundary line running from the Tees estuary in the north-east of England to the Exe estuary in Devon
- We can split the UK into two main features, uplands and lowlands
Uplands - north west
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- Glaciated during the last Ice Age, it is mainly igneous and metamorphic rocks
- The uplands are found mostly in the north and west of the country: Northern Ireland, Scotland, Wales and north England (e.g. Lake District, Grampian Mountains and Snowdonia etc.)
- Climate is wetter and less fluctuating
Map of upland and lowland UK showing glacial limit and major rivers