River tees lower course Rating:
The Augustan Age in English literature refers to the period from the early 18th century to the mid-18th century, during which time the literary culture of England was heavily influenced by the classical ideals of the Roman Empire. This period is named after the Roman Emperor Augustus, who reigned during a time of peace and prosperity in the Roman Empire and is often seen as a model for the English monarchy of the time.
During the Augustan Age, English literature saw a shift towards more formal and polished writing styles, as writers sought to emulate the classical ideals of the Roman Empire. The emphasis was on reason, restraint, and decorum, and writers sought to create works that were well-structured and balanced, with a clear and logical progression of ideas.
One of the most notable writers of the Augustan Age was Alexander Pope, who is known for his poetry, including his famous work "The Rape of the Lock," as well as his translation of Homer's "Iliad." Pope's work is characterized by its use of classical allusions and its emphasis on reason and order, and he is often seen as a key figure in the development of the Augustan style.
Another important writer of the Augustan Age was Jonathan Swift, who is best known for his satirical works such as "Gulliver's Travels" and "A Modest Proposal." Swift's writing is marked by its wit and irony, and he is known for using satire to expose the flaws and follies of society.
The Augustan Age also saw the emergence of the novel as a popular form of literature, with writers such as Daniel Defoe and Samuel Richardson publishing works such as "Robinson Crusoe" and "Pamela." These novels were often concerned with practical and moral issues, and they sought to educate and improve readers through their portrayal of virtuous characters and the resolution of conflicts.
Overall, the Augustan Age in English literature was a time of great cultural and artistic achievement, as writers sought to emulate the classical ideals of the Roman Empire and create works that were polished, well-structured, and intellectually stimulating. It was a time of great innovation and creativity, and the works produced during this period continue to be highly influential and widely read to this day.
The River Tees Case Study
At this stage small meandersor bends and small flood plains can be formed. Settlement first developed within the meanders for defensive reasons: but this has restricted growth in recent times in the town of Yarm In the lower course of the river it opens into the Tees Estuary: there is a lot of deposition evidenced by mud flats at low tide. In this area there are also levees which have formed when the river has flooded. In this area there are also levees which have formed when the river has flooded. The river flows over a layer of hard, basaltic Volcanic rock called Whinstone which is difficult to erode. The River Tees is a fantastic river to study as it contains nearly all of the classic river landforms; V shaped valleys and interlocking spurs, waterfalls, floodplains and levees, meanders and ox bow lakes and an estuary at Tees mouth. Plants grow in the bed of the river and at its edges.
Most rivers begin in hills or mountains. The River meanders greatly across its lower course in County Durham and into the Tees Valley. They were very time consuming and costly for ships to navigate around. As the River Tees starts to erode sideways lateral erosion , it forms meanders. Debris from the waterfall helps erode the plunge pool and the undercut.
The Upper Course Much of the land is either open moorland or rough grazing, where the main land use is sheep farming. Its source is on Cross Fell in the North Pennines and runs into the North Sea at the mouth of the Tees between Hartlepool and Redcar. The limestone erodes backwards, undercutting the Whinstone, which eventually collapses. These flat areas closer to the sea have led to the growth of the industries of Teeside and the urbanisation linked to it. It also contains a deposition. By 1829, the area had been bought by Joseph Pease to build a new coal port, named Port Darlington, and a town in which the port workers could live.
Since the northern meander was shorter and the cut longer, the net reduction in distance was less, but the bypassing of islands and sandbars in the Portrack meander still made it worthwhile. 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. The 70m-wide barrage controls the flow of the river, maintains water levels and prevents localised flooding around Stockton-on-Tees. As for the old meanders which had been cut off, some parts of the old river can be seen winding around Teesdale Park and are a part of the Portrack Marsh Nature Reserve. As the River Tees reaches its middle course lateral erosion overtakes vertical erosion and is evidenced by winding meanders. The river flows over a layer of hard, basaltic Volcanic rock called Whinstone which is difficult to erode.
What is the upper course of the River Tees used for? The work was completed in 1831, resulting in the present river channel. This section of a river is cold, clear and fast-flowing. Waterfalls are also, usually formed at this stage. What is the mouth of the River Tees? 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 this impressive waterfall. Meanders: are major features of the middle course of the River Tees.
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. Cow Green reservoir on the R. When was Tees Barrage opened? It is less steep and has a moderate flow of water. Much of the land is either open moorland or rough grazing, where the main land use is sheep farming. If something more leisurely takes your fancy, you can step aboard one of the local boat trips. The mud of the estuary is an important ecosystem, supporting a wide range of birds and other flora and fauna. Underneath the Whinstone is softer limestone.
Vertical erosion has formed classic V-shaped valleys. Oxbow lakes have formed in some areas. In 1801 Middlesbrough was a simple farming estate with a population of only 25. This sediment is very fine and builds up mudflats. Courses of a river and River Wildlife The upper course of a river is often in steep, mountain areas. A river basically, has three parts.
It has a very steep slope. This winding lowland parts of a river contain muddy, slightly warmer water, which flows more slowly. Many plant and animals live in or near rivers. Rivers flow down to the sea and end there. By 1851 its population rose to 7,600. Pollution has always been a problem in the river, both domestic and industrial; butthe river has become a lot cleaner as industry has closed down and industrial waste has been controlled by the Government and the E.
Cow Green reservoir on the R. The Tees Barrage was built in 1995 to control the flow of the river and prevent flooding, but it has also increased the opportunities to take part in water sports on the river. Where is the lower course of the River Tees? This creates vertical erosion forming a V-shaped valley. These are a natural form of flood defence. Sites such as Seal Sands are protected areas. Yarm The Lower Course From Yarm, the river has levees. Large meanders, large flood plains as well as oxbow lakes can be formed at this stage.
Their first task was to dig a channel, known as the Mandale Cut. This lesson on river landscape also called riverscape explains to you about these courses or stages of a river and their wildlife. Examples can be found along the River Tees. There are rivers on every continent except Antarctica. The limestone erodes backwards, undercutting the Whinstone, which eventually collapses. The Cuts increased the depth of Stockton Quay and improved its usage as a business port. Where is the source of the River Tees? The bottom becomes a mixture of silt and gravel.