Pin It on Pinterest. Share buttons are a little bit lower. We think you have liked this presentation. Meanders in the lower course are much larger. Evidence of past flooding can be seen in the natural levees that have formed. Although some vertical erosion does take place, lateral erosion is the more dominant force.
The River Tees Case Study – landforms of erosion and deposition
Although gradients are gentler, velocity is greater as there is now less friction from the river bed and banks.
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Case study: The River Tees
Auth with social network: If you wish to download it, please recommend it to your friends in any social system. Higher Hydrosphere The Upper Course Areas with steep gradients will have an increased velocity and so the potential for erosion is higher, especially vertical.
Related Topics Use the images below to explore related GeoTopics. In its upper course, the River Tees flows over hard, impermeable rocks.
Why is the weather so bad at the moment?. The flow of the river begins to meander rather than flowing straight.
About project SlidePlayer Terms of Service. If you’ve found the resources twes this page useful please consider making a secure donation via PayPal to support the development of the site. How are sand dunes formed? What landforms and features are associated with the lower course of a river? The River Tees”— Presentation transcript: SOME of us will ALSO analyse the factors leading to changes in valley shape and explain in detail the changes in the resulting landforms.
River Tees: Case Study of River and Landforms by Gemma Pollard on Prezi
Case study: The River Tees – ppt video online download
Vertical erosion has formed classic V-shaped valleys. Share buttons are a little bit lower. Oxbow lakes have formed in some areas.