RIVER TEES CASE STUDY LANDFORMS

Take a look at our new resources in the shop Dismiss. Interlocking spurs close to Cauldron Snout on the River Tees. Auth with social network: Hurricane Katrina Case Study. River discharge is greater as tributaries have fed their water into the main river.

If you wish to download it, please recommend it to your friends in any social system. Share buttons are a little bit lower. To investigate the main features in the lower course of the river. 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 the waterfall. By continuing to browse the site, you are agreeing to our use of cookies.

Watch the video clip carefully which explain the processes involved in the formation of a meander.

river tees case study landforms

To use this website, you must agree to our Privacy Policyincluding cookie policy. Hurricane Katrina Case Study. Explain fully the processes at work creating the meander.

river tees case study landforms

About project SlidePlayer Terms of Service. The shape of the valley Erosion Landforms with named examples where appropriate. Middle Course Lower Course.

The River Tees Case Study – landforms of erosion and deposition – Internet Geography

How are sand dunes formed? Registration Forgot your password? To investigate the main features in the lower course of the river. Higher Hydrosphere The Upper Course Areas with steep gradients will have an increased velocity and so the potential for erosion is higher, especially landforsm. ALL of us will also be able to explain in simple terms why these differences exist.

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Look carefully at how the shape of the valley changes and the course of the actual river itself. SOME of us will ALSO analyse the factors leading to changes in valley shape and explain in detail the changes in the resulting landforms.

The River Tees Case Study – landforms of erosion and deposition

Also think about other aspects of the river such as its gradient and the volume of water lanfforms is carrying. Although some vertical erosion does take place, lateral erosion is the more dominant force. The River Tees Middle Course. Meanders in the lower course are much larger. Download ppt “Case study: Interlocking spurs close to Cauldron Snout on the River Tees. Why is the weather so bad at the moment?.

Make sure you add labels summarising: Auth with social network: C ALL of us will be able to understand the basic differences between the upper and middle courses.

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

The river from source to mouth Teex the period of the next few lessons you will understand how a studh changes from source to mouth and include this information. Take a look at our new resources in the shop Dismiss. Published by Bennett Barton Modified over 3 years ago. The site is self-funded and your support is really appreciated.

Evidence of past flooding can be seen in the natural levees that have formed.

Case study: The River Tees

To make this website work, we log user data and share it with processors. Landforms in the lower course of a river.

Feedback Privacy Policy Feedback. What landforms and features are associated with the lower course of a river? What do you think forms a V-shaped valley? High Force waterfall on the River Tees.