The River Tees Case Study – landforms of erosion and deposition – Internet Geography. A river process consists of three 1.erosion (in the upper course) 2.transportation(in the middle course) and 3.deposition (in the lower course). The upper course contains steep v shaped valleys, interlocking spurs, waterfalls such as High Force falls … V-shaped valley 2. Main features along the River Tees upper course. What are the different types of volcano? There are 9 reservoirs in the River Tees drainage basin. 1) In the lower course of the river the gradient is gentler than in the upper course. 2. Learn vocabulary, terms, and more with flashcards, games, and other study tools. The rivers in the Upper Tees have steep channel gradients and valley sides. The river has more energy and the volume amount of water is high. Features of the upper course VERTICAL EROSION is the main process in the upper course of the river, as the river wants to get to sea level. Find out more. 3. ... What are the main features of a volcano? The River Tees in northern England has its source in the Pennine Hills on Cross Fell and flows into the North Sea near Middlesbrough. Walkers on the Pennine Way walk a … This gives the river a lot of potential energy. Task 1 - Turn to page 12 of the OCR B Geography textbook** and define and explain the formation of a meander. 4 of 12. In the upper course of a river gradients are steep and river channels are narrow. At Caldron Snout and High Force there are waterfalls where the river crosses the hard dolerite outcrop of the Whin Sill. The River Tees”— Presentation transcript: We think you have liked this presentation. Registration Forgot your password? Landforms in the upper course of the river. In the mid-catchment, the valley widens out and channel slopes become much gentler. The river is trying to cut down to its base level or downwards so it mainly does this through vertical erosion. The faster water travels around the outside of the bend, eroding the banks through abrasion and hydraulic action. 1. This is the part of the river closest to the source. Underneath the Whinstone is softer limestone. 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. its landforms should be divided into three regions. BBC Bitesize – upper course features. These include waterfalls, v-shaped valleys and interlocking spurs. The source is in the Pennines near Cross Fell, 893m above sea level. Here, vertical erosion has formed a V-shaped valley. These include waterfalls, v-shaped valleys and interlocking spurs. Here, vertical erosion has formed a V-shaped valley. The upper course has hard impermeable rocks. Where is the source located? It is 85 miles long. GCSE Revision - Rivers - The Upper Course: In the upper course, the river is high above seal level. The upper, the middle and lower course of the River Tees The source of the River Tees is Cross Fell in the Pennines. In its upper course, the River Tees flows over hard, impermeable rocks. The gradient is steep. As the result of this typical features include steep valley sides, interlocking spurs, rapids, gorges and waterfalls. The River Tees is located in the north of England. One of Britain’s most famous long distance footpaths traverses Cross Fell. Landforms in the upper course of the river. C ALL of us will be able to understand the basic differences between the upper and middle courses. The river is small and flows quickly. Meander and Oxbow lake, Levées, Estuaries and Floodplains. It is 85 miles long. The Upper Course. The lower catchment is close to sea level and predominantly tidal in nature. Full lesson of activities to guide KS4 students through the features of the upper course of the river. Main features along the River Tees middle and lower course. 3 of 12. We are using the River Tees in the northeast of England as our main … Vertical erosion has led to the formation of this landform. Objective: To learn about the features associated with the middle course of the river Garonne. Here are some facts about the River Tees. It is 85 miles long. The largest is Cow Green Reservoir completed in 1971.

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