We are using the River Tees in the northeast of England as our main … To investigate the main features in the lower course of the river. These include waterfalls, v-shaped valleys and interlocking spurs. Full lesson of activities to guide KS4 students through the features of the upper course of the river. What are the different types of volcano? The river has more energy and the volume amount of water is high. Here, vertical erosion has formed a V-shaped valley. The limestone erodes backwards, undercutting the Whinstone, which eventually collapses. There are 9 reservoirs in the River Tees drainage basin. Vertical erosion has led to the formation of this landform. In the mid-catchment, the valley widens out and channel slopes become much gentler. In its upper course the Tees flows in a typical Pennines dale (valley) where high moorlands flank an attenuated strip of farmland. 5 of 12. The rivers in the Upper Tees have steep channel gradients and valley sides. The upper course contains steep v shaped valleys, interlocking spurs, waterfalls such as High Force falls … 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). Start studying River tees case study - river features. As the result of this typical features include steep valley sides, interlocking spurs, rapids, gorges and waterfalls. It is 85 miles long. In the upper course of a river gradients are steep and river channels are narrow. The river tees is a complex river. Main features along the River Tees middle and lower course. Main features along the River Tees upper course. 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. 2. 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. This is the part of the river closest to the source. The River Tees Case Study – landforms of erosion and deposition – Internet Geography. Learn vocabulary, terms, and more with flashcards, games, and other study tools. The River Tees rises on the eastern slopes of the North Pennines and flows east for 85 miles to finally reach the North Sea near Middlesborough. The Canal & River Trust are responsible for the 22 miles from Worsall, (the highest tidal point in the river until the barrage was built) through Yarm and up to and including the iconic Tees Barrage in Stockton-On-Tees. The River Tees is located in the north of England. Walkers on the Pennine Way walk a … 3 of 12. Thus it tends to wind its way along, leaving the more resistant areas of rock as interlocking spurs. The lower catchment is close to sea level and predominantly tidal in nature. Task 1 - Turn to page 12 of the OCR B Geography textbook** and define and explain the formation of a meander. Vertical erosion is greatest in the upper course of a river. Where is the source located? Landforms in the upper course of the river. 3. One of Britain’s most famous long distance footpaths traverses Cross Fell. Where are Rapids located? River Features found in the Upper Course. Here are some facts about the River Tees. 4 of 12. The River Tees is located in the north of England. The River Tees in northern England has its source in the Pennine Hills on Cross Fell and flows into the North Sea near Middlesbrough. its landforms should be divided into three regions. Registration Forgot your password? Here, vertical erosion has formed a V-shaped valley. Some features expected in this section of the river are V- shaped valleys, interlocking spurs, a river bed with large rocks and stones,gorges, fast flowing rapids and waterfalls. The gradient is steep. 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. V-shaped valley 2. The River Tees in northern England has its source in the Pennine Hills on Cross Fell and flows into the North Sea near Middlesbrough. The river flows over a layer of hard, basaltic (Volcanic) rock called Whinstone which is difficult to erode. These include waterfalls, v-shaped valleys and interlocking spurs. 2) In the lower course there is more lateral (sideways) erosion.The channel is wide and deep.The river has less friction to overcome which means that the river can flow faster. The upper, the middle and lower course of the River Tees The source of the River Tees is Cross Fell in the Pennines. 1) In the lower course of the river the gradient is gentler than in the upper course. Waterfalls These occur when there are horizontal The river is small and flows quickly. Underneath the Whinstone is softer limestone. GCSE Revision - Rivers - The Upper Course: In the upper course, the river is high above seal level.