RIVER TEES CASE STUDY LANDFORMS

SOME of us will ALSO analyse the factors leading to changes in valley shape and explain in detail the changes in the resulting landforms. Where are deserts located? Meanders in the lower course are much larger. Registration Forgot your password? About project SlidePlayer Terms of Service.

The upper, the middle and lower course of the River Tees. In its upper course, the River Tees flows over hard, impermeable rocks. Explain fully the processes at work creating the meander. What landforms and features are associated with the lower course of a river? To make this website work, we log user data and share it with processors. We think you have liked this presentation. Although gradients are gentler, velocity is greater as there is now less friction from the river bed and banks.

Where are deserts located? Sorry, your blog cannot share posts by email.

river tees case study landforms

Please Support Internet Geography If you’ve found the resources on this site useful please consider making a secure donation via PayPal to support the development of the site. Evidence of past flooding can be seen in the natural levees that have formed. Look carefully at how the shape of the valley changes and the course of the actual river itself.

Vertical erosion has formed classic V-shaped valleys. Related Topics Use the images below to explore related GeoTopics.

If you’ve found the resources on this page useful lanvforms consider making a secure donation via PayPal to support the development of the site. Higher Hydrosphere The Upper Course Areas with steep gradients will have an increased velocity and so the potential for erosion is higher, especially vertical.

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Case study: The River Tees

To investigate the main features in the lower course of the river. Registration Forgot your password? C ALL of us will be able to understand the basic differences between the upper and middle courses. Make sure you add labels summarising: Typhoon Haiyan Case Study.

river tees case study landforms

In its upper course, the River Tees flows over hard, impermeable rocks. Landforms in the lower course of a river.

Make frequent and accurate reference to key terms such as erosion, deposition, point bar river cliff etc. Meanders in the lower course are much larger.

The River Tees Case Study – landforms of erosion and deposition

The river from source to mouth Over the period of the next few lessons you will understand how a river changes from source to mouth and include this information. How do you think it is formed?

The flow of the river begins to meander rather than flowing straight. The River Tees”— Presentation transcript: Share buttons are a little bit lower. Watch the video clip carefully which explain the processes involved in the formation of a meander.

Case study: The River Tees – ppt video online download

If you’ve found the resources on this site useful please consider making a secure donation via PayPal to support the development of the site. ALL of us will also be able to explain in simple terms why these differences exist. It flows east from its source in the Pennines to its mouth, on the North Sea coast. SOME of us will ALSO analyse the factors leading to changes in valley shape and stidy in detail the changes in the resulting landforms. Oxbow lakes have formed in some areas.

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The River Tees Case Study — landforms of erosion and deposition. Explain fully the processes at work creating the meander.

River landforms – AQA – Revision 4 – GCSE Geography – BBC Bitesize

Although gradients are gentler, velocity is greater as there is now less friction from the river bed and banks. To make this website work, we log user data and share it with processors. Hurricane Katrina Case Study. The River Tees Middle Course. Feedback Privacy Policy Feedback.