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River landforms - EduqasCase study - river landforms - River Tees

Erosional landforms include V-shaped valleys, interlocking spurs, waterfalls and gorges. Meanders and oxbow lakes are formed from erosion and deposition. Depositional landforms include floodplains.

Part of GeographyLandscape and physical processes

Case study - river landforms - River Tees

River Tees

The River Tees is located in the north of England. The of the River Tees is located in the Pennines and it flows east to its where the river joins the North Sea.

The River Tees runs from Cross Fell to the North Sea, in northeast England. The upper course ends with High Force. The middle course runs near Barnard Castle.

Upper course

  • The has hard impermeable rocks. Here, has formed a V-shaped valley.
  • High Force, the UK's largest at 21 metres high is located in the upper course. An area of hard rock, called Whin Sill (or Whinstone), is located above a layer of soft rocks (sandstone and shale) and together they create this impressive waterfall.
A photo of High Force waterfall
Image caption,
High Force waterfall

Middle course

  • As the River Tees starts to erode sideways (), it forms . These can be identified in the near Barnard Castle.
A photo of OS map
Image caption,
漏 Crown copyright and database rights 2015 Ordnance Survey

Lower course

  • Near Yarm, the meanders in the are much larger, and have formed. In this area there are also which have formed when the river has flooded.
  • The River Tees has a very large with mudflats and sandbanks which support wildlife in the area. Sites such as Seal Sands are protected areas.
A photo of the River Tees estuary and its mudflats
Image caption,
The River Tees estuary and its mudflats