River tees upper course. Landforms in the upper course of a river 2022-10-31

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The River Tees is a major river in northern England that rises in the Pennines and flows eastwards for approximately 185 miles, eventually emptying into the North Sea. The upper course of the River Tees is located in the county of Cumbria, in the north west of England, and flows through a variety of landscapes, including rolling hills, open moorland, and forests.

The upper course of the River Tees begins in the heart of the Pennine Hills, near the village of Cross Fell. From here, the river flows eastwards, passing through a number of small towns and villages, including Dufton and Middleton-in-Teesdale. As it flows through this region, the river is fed by a number of smaller tributaries, including the River Leek and the River Balder.

One of the most significant features of the upper course of the River Tees is the presence of a number of waterfalls, including High Force and Low Force. These waterfalls are formed as the river flows over hard rock formations, causing it to drop dramatically in elevation. The waterfalls are a popular tourist attraction, and are surrounded by beautiful scenery, including rolling hills and forests.

As the River Tees continues on its journey eastwards, it enters the North Pennines Area of Outstanding Natural Beauty. This region is home to a variety of wildlife, including red grouse, golden plover, and curlew. The river also flows through a number of important habitats, including blanket bogs, heathland, and grassland, providing a home for a wide range of plant and animal species.

The upper course of the River Tees is an important region for both tourism and agriculture. The river and its surroundings are popular with hikers and outdoor enthusiasts, who come to enjoy the beautiful scenery and the opportunity to spot a wide range of wildlife. The region is also home to a number of farms, which produce a range of crops and livestock.

In conclusion, the upper course of the River Tees is a beautiful and varied region that is rich in natural beauty and important habitats. It is an important area for both tourism and agriculture, and is home to a wide range of plant and animal species. Whether you are interested in outdoor adventure or simply want to relax and enjoy the scenery, the upper course of the River Tees is an excellent destination.

RIVER TEES Flashcards

river tees upper course

What is the shape of a river in the upper course? The gradient here is steep and the river channel is narrow. Conclusion These changes have affected the extent of settlement as well as the land use along the river. The river erodes the softer rock faster, through hydraulic action and abrasion. Some types of rocks shale, for example wear away more easily than others such as sandstone or limestone. How is the course of a river different on a plain? When the river reaches the middle course the land has been slightly flattened by vertical erosion and larger settlements have resulted.


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Change in land use along the River Tees.

river tees upper course

The river erodes the softer rock faster, through hydraulic action and abrasion. The river is fed by many tributaries and its volume of water increases. The Upper Course A series of reservoirs have been built to provide water for the industrial cities to the east; e. The soft rock is eroded quicker than the hard rock and this creates a step. This happens when a river flows over a band of hard rock that lies over the top of the softer, less resistant rock. The land has few uses other than for sheep faming as it is of a poor quality.

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How did the River Tees shape the land?

river tees upper course

In the upper course of a river, water flows quickly through a narrow channel with a steep gradient; as it does so it cuts downwards. V-shaped Upper course river features include steep-sided V-shaped valleys, interlocking spurs, rapids, waterfalls and gorges. What is the upper course of the river Tees used for? How does a gorge formed in the upper course? Falling water and rock particles erode the soft rock below, forming a plunge pool. Middle As the river continues downstream it begins to meander, the land becomes flatter, as the river valley has been laterally eroded. What is the River Tees basin? What is the purpose of the Tees Barrage? High Force waterfall on the River Tees. It erodes its bed and banks and carries large boulders of rock with it. The site has a diverse mix of habitats, mainly dry heath, with wet heath and blanket mire in areas that are poorly drained.

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What is the main process in the rivers upper course?

river tees upper course

Answer: Large parts of the northern lowland of Asia are marshy because these are drained by three rivers, Yenisei, Ob and Lena. There is some limited employment in forestry but the majority of land in the middle course of the river is used for arable farming. Perhaps some decorative shrubs in tubs or pots. Rapids Rapids are fast flowing, turbulent sections of the river where the bed has a relatively steep gradient. The video below shows an overhang beneath Summerhill Force waterfall, Bowlees, Teesdale. Gorge A gorge can be formed as a waterfall retreats up a valley.

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Landforms in the upper course of a river

river tees upper course

Why does the upper course of rivers in the northern lowland become marshy? As the river moves through the upper course, it cuts downwards. Below is a video featuringSkógafoss which is a waterfall situated on the Skógá River in the south of Iceland at the cliffs of the former coastline. The height and number of waterfalls along a stream or river depend upon the type of rocks that are being eroded by the water. The land here is predominately used for farming as well though in the past it has been used for mining. This erosion, together with the movement of weathered material at the sides of the river, creates the classic V-shaped valley. Eventually, the overhang collapses as it cannot support itself.

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river tees upper course

At 22 metres it is the tallest waterfall in England. Why is the middle course of a river important? Employment opportunities are also restricted to mainly agriculture and forestry related jobs; as a result the population density in this part of the river valley is extremely low. This typically occurs in areas where alternatingbands of rock, made up of soft and hard rock, form the bedrock. Vertical erosion has formed classic V-shaped valleys. Another example of a waterfall is High Force on the River Tees. The main function of a river in its upper course is erosion. Rapids on the River Tees Rapids form when there is vertical bedding which is when alternate bands of hard and soft rock cross the channel.

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river tees upper course

This process repeats causing the waterfall to retreat upstream, leaving behind a steep and narrow gorge. Lower course river features include wide flat-bottomed valleys, floodplains and deltas. This is because the land is flat and there is good fertile soil, so crops can easily grow. . Where is the main erosion in a river? The source of the River Tees is located in the Pennines and the river flows east to its mouth where it joins the North Sea. They are typical of the upper valley but can be found in the rivers lower courses.

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river tees upper course

Over time an overhang of hard rock forms. Rivers begin high up in the mountains so they flow quickly downhill eroding the landscape vertically. The upper course of a river is where the river begins its path toward the sea. How is a V shaped valley formed? This explains why the river is forced to flow around them. This happens when a river flows over a band of hard rock that lies over the top of the softer, less resistant rock.

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river tees upper course

Larger towns have sprung up here e. Hence, the speed of the current is also less, compared to the upper course. Why is the upper course of a river V-shaped? As one can see changes in industry and economy have affected what the land is being used for e. The upper course of a river is where the river begins its path toward the sea. Due to the steep slopes and harsh climate the building of communications links was very challenging and therefore settlements are extremely rare, limited to isolated farmhouses.

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