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How did the River Tees change over time?
Overall, there is a very large change of land use throughout the drainage basin of the River Tees. It starts of being very marshy and in an extremely quiet location, becoming more arable and pastoral, then small settlements are introduced.
Where is the source of the River Tees?
The source of the River Tees is located in the Pennines and it flows east to its mouth where the river joins the North Sea. The upper course has hard impermeable rocks. Here, vertical erosion has formed a V-shaped valley. High Force, the UK's largest waterfall at 21 metres high is located in the upper course.
What causes change in the course of a river?
The meanders cause change in the river course. Ox-bow lakes are formed by the large hydraulic action eroding the insides of meanders, cutting of the curve. This will then eventually dry up and leave meander scars on the land.
Where are the meanders of the River Tees?
As the River Tees starts to erode sideways (lateral erosion), it forms meanders. These can be identified in the middle course near Barnard Castle. Near Yarm, the meanders in the lower course are much larger, and oxbow lakes have formed. In this area there are also levees which have formed when the river has flooded.
Last Update: Oct 2021
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The river tees once provided A dividing line betwixt the kingdoms of bernicia and deira, a national borderline between england and scotland in the.
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