Monday, January 28, 2019
Describe and explain the changes that take place in land use of the River Tees drainage basin
In the first  hunt down of the  rendr Tees, the  discharge is  usually not usable. There is snow melt from the mountains, this  characters dead  atomic number 18a and not crops can be  haven and the conditions are too harsh for e precise animals in Britain to live in. This  withal causes in truth snowy,  come downy and cold  abide which  in any case makes it impossible for pastoral    force field. There is also marshy moorlands  some the source, so again the land can not be use for any  dust of faming. There is also the hilly situation. The land is not  plain as it runs down then Pennines, the interlocking spurs cause a  prodigious difference in land angles and a v-shaped valley is form well-nigh the river.This is not ideal for farming, travelling and, because of the poor weather conditions, the rain will run down the lands, possibly causing  drenchs. A  identification number lower down the river, the weather is not so extreme and the land is  utilize for sheep grazing. There is not    much grass so  on that point is not much available. There is also the Cow Green reservoir, on the Tees itself built in 1970. This  operator that the  body of water can be controlled by humans, therefore stopping excess water pouring through the river. This means the flood plain is going to be usable for farming because the river  stream will be controlled, therefore stopping floods which would ruin the land.This also helps the  risk of infection of flooding further down the course by lowering the hydraulic action. High Force waterfall is a  grown feature of the Rive Tees. It affects the land because it is constantly forming a gorge of recession. This happens because the soft rock, limestone underneath the  rugged rock, Whinstone is eroded by the water, this causes the hard rock to fall. This cycle is repeated and the waterfall slowly moves up the river. This is also a tourist attraction, which could cause the land to be quite rough  ascribable to walkers, tourists and their cars.The   re is also pastoral farming around the waterfall, because the land is unaffected by the water, due to the low plunge pool. In the  mettle course, the shape of the river obviously  miscellanys.  high up it was reasonably straight and narrow, with many small tributaries. In the middle course of the Tees, there are many large meanders and the river is very  roomy and with only a few large tributaries. This changes the land quite a lot. The meanders cause change in the river course. Ox-bow lakes are formed by the large hydraulic action eroding the insides of meanders, cutting of the curve.This will then  at last dry up and leave meander scars on the land. This could mean the scars grow different land to the surrounding area and not  fitting in comparison. For example if the land around a meander scar is used for  arable farming, but a newly grown section is suitable for pastoral farming, there is wasted land. The meanders are so large that form Darlington to Teesmouth it is 30km as the    crow flies, but going by river it is 75km long. And in the nineteenth centaury, some of the river was manually cut-off to shorten boat journeys up to Stockton and Yarm, so it was  veritable(a)  semipermanent.In 1810, the Tees Navigation Company cut the neck of the Mandale Loop, a large meander near Stockton. This shortened the route by 4km and more was unnaturally straightened. The water now moves faster but the flood risk is also lower. The meanders also cause a higher risk of flood, because the water travels very fast in large quantities. This means the surrounding land is  deep and used for agriculture. In this course of the river, the meanders home a small  town called Yarm which is a historic market town. Yarm has a few settlements and a local anesthetic church. This means the land is civilised and is used for transport and living on.Yarm was  formerly an Inland Port which was prone to flooding. A Flood Defence  organisation was set up in Yarm and spent i??2. 1  cardinal on red   ucing the flood risk. They reinforced concrete walls, built flood gates, used gabions to protect walls and embankments, built fishing platforms and replanted any land that was  ruined by floods. In the lower part of the middle course, in-between Stockton and Yarm, a barrage was built in 1995. It cost i??54  one million million to build and controls 22km of river. It was built because it was harshly affecting the surrounding land because of the  permanent high tide, resulting in a very high flood risk.Because it has  move the flood risk and there is also no tidal  premix now, it is a catalyst for 500 million of investment in offices, houses, education,  unfilled and shopping. This obviously changes the land use as it is not used for farming but more economic purposes. The key points of how land use has changed in the Middle course to the upper because it is a lot flatter, has larger meanders and has an urban settlement. In the lower course of the river there are large areas of flat m   uddy land. This land is used for migratory birds and seals for example, hence why they are called Seal Sands.However, the majority of the land use in the lower course of the Tees in industrial. It homes oil refineries, aluminium smelters, stockyard, railways and more. This causes pollution in the river and the surrounding land, and is both domestic and industrial, because there are also many settlements. This has been helped recently by the Government, who closed down some industry and waste has been cleaned. The land around the mouth of the river is very marshy with some drained land as well. It is impossible to grow crops on and to use pastorally. It is very industrial  financial backing many boats with imports and boats with exports.It is very urban with large settlements and cities. It is much wider than the rest of the river and the water is very deep for shipping. Bridges have also been made, encouraging the land to be used for transport. Overall, there is a very large change    of land use throughout the drainage basin of the River Tees. It starts of being very marshy and in an extremely quiet location, becoming more arable and pastoral, then small settlements are introduced. Next the farming is not longer appropriate and the settlements are larger, with a very large industrial area at the bottom of the river.  
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