River Eden case study
Where is it?
- North west England between the Lake District and Pennines
Landforms
- V-shaped valleys - ^^600 metres^^ above sea level
- Hell Force Waterfall - hard rock (^^limestone^^), soft rock (^^sandstone^^)
- Meanders near ^^Salkeld^^
- Oxbow lake near ^^Briggle Beck^^
- ^^Carlisle^^ is built on the floodplain
Processes
- Regular freezing in the winter near the source, leading to ^^freeze thaw weathering^^
- Intense rainfall can lead to ^^landslides^^, so more material in the river
- ^^High river volumes^^ can increase geomorphic processes
- ^^Limestone^^ is vulnerable to ^^chemical weathering^^
- West of River Eden there is ^^impermeable rock^^, making ^^flooding more likely^^
- ^^Sandstone^^ is prevalent in in middle+lower courses, ^^increasing erosion^^
Human activity
- ^^10km of flood walls + embankments^^ along river
- ^^Castle Carrow Beck^^ (south west of Carlisle)has been ^^dammed to create a reservoir^^
- Near ^^Dalston^^ (south of Carlisle) ^^1,000 trees^^ have been planted
- Restoration of the river from its ^^previously straightened state^^ (e.g ^^artificial meanders created south west of Appleby - slows river flow^^)