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River landforms - EdexcelCase study - river landforms: River Tees

Erosional landforms include interlocking spurs, waterfalls and gorges. Meanders and oxbow lakes use erosional and depositional processes in their creation. Examples can be found along the River Tees.

Part of GeographyChanging UK landscapes

Case study - river landforms: 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.
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.
OS map of The River Tees
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 supports wildlife in the area. Sites such as Seal Sands are protected areas.
The River Tees estuary and its mudflats
Image caption,
The River Tees estuary and its mudflats