A Geography Coursework A Geography Coursework When working on the persuasive essay, a student has to collect all valuable and time-tested sources to prove his knowledge of the certain issue A geography coursework purchase college papers.
We come together to aid our enjoyment of reading Bernard Cornwell's novels. Here we can find background information on places and characters that are key to the context of the novel. It reaches the sea at a substantial ria, the Exe Estuary, on the south English Channel coast of Devon.
Historically, its lowest bridging point was at Exeter, though there is now a viaduct for the M5 motorway about 3 km south of the city centre. Topography The river's name derives from the Celtic word Isca meaning, simply, water.
The seaside town of Exmouth is at the east side of the estuary mouth, and Dawlish Warren is at the west, with its long sand spit extending across the mouth. The river fuelled Exeter's growth and relative importance in medieval times and the city's first industrial area was developed at Exe Island, created by a series of leats to the west of the city.
The island was home to numerous watermills producing paper and textiles; it also created valuable land through drainage of the marshlands.
Tides on the river are limited at Countess Wear, the site of a weir commissioned by the Countess of Devon in the 13th century. The Exeter Canal bypasses this weir to enable ships to reach Exeter Quay. At high tide, the estuary forms a large body of water that is River holford coursework used for water sports especially sailing, windsurfing and water skiing.
Railways run along both sides of the estuary. The Exmouth to Starcross Ferry carries passengers across the mouth of the estuary during the summer months, linking the harbour at Exmouth with a pier adjacent to Starcross railway station on the South Devon main line.
Powderham Estuary of the River Uisc Wildlife At low tide, extensive mud flats are exposed, and these are an important feeding source for wading birds. Along with other rias in South West England, the Exe estuary is an important site for wintering waders.
Dawlish Warren is a favoured site for birdwatching. The river is acidic and populated with wild brown trout and some grayling, the average size being oz. Unlike many West Country rivers there are no seatrout, but there is a run of atlantic salmon. Just metres below the union of the River Barle is one of the best, and highest salmon pools on the river: There are many weirs on the river.
Several stretches, particularly below Farleigh Hungerford are used for coarse fishing and some trout fishing. In April the Mendip Power Group started electricity generation at Tellisford Mill, and it is ultimately expected to produce 75 kW. The valley of the river consists of three tributary valleys extending down from the surrounding farmland to merge with the River Haddeo in the south.
The tributary valleys include the River Pulham, which passes the village of Brompton Regis and continues to Hartford where it joins the Haddeo. In - South West Water commissioned a detailed assessment of fish population, physical habitat, flow and water quality data within the River Haddeo, since it has been subject to regulated releases from Wimbleball Reservoir, to identify potential bottlenecks restricting the development of juvenile salmon populations Hoar Oak Water is a moorland tributary of the East Lyn River in Exmoor, Somerset.
Area of Outstanding Natural Beauty in Somerset. It is approximately 4. The river is used as an outdoor classroom for students of Fluvial Geomorphology.
The geology of the river consists of three different rock types at the top of the river there is the Devonian Quartzite Metamorphicin the middle of the river there is the Permo-Triassic Marl Sedimentary and the lower part of the river consists of Jurassic Limestone Sedimentary.
The first two rock types are impermeable meaning there is little drainage for the river but the river depth becomes smaller as the water flows over the permeable limstone which will allow water to pass through.
Quartzite is also very resistant to chemical weathering and can form ridges. The river was excavated as a five mile long straight channel using a dragline during the early years of World War II.
It was constructed as a priority war work. Its main function was to provide an all year-round guaranteed supply of 4. It was also intended to help drain parts of the lower Brue Valley. It was connected to the South Drain at Gold Corner. It implemented parts of a drainage plan for the Somerset Levels first drawn up in but not implemented until World War II.
The Huntspill River has retention sluices at both ends, so that it acts as a long reservoir.coursework. (a)* The table shows the annotations for Dunlop Street. Write the letters A.
to. F to match with numbers. in the correct box number on Figure 1. B. has been done for you. In which direction is the River Holford flowing? (ii) Name the woodland to the north west of Kilve. Fieldwork Methodology The two dominant methodologies of fieldwork practice, the traditional and the scientific, have different aims implicit within them.
The traditional approaches, sometimes termed 'fieldwork excursions' have aims rooted in the development of content knowledge. Dear Parent/Guardian 4th June Geography Trip to River Holford on Monday 18th June The purpose of this visit is to provide students with the opportunity to experience a number of field work techniques in preparation for their course work which will make up 20% of their grade.
Course content. Our exam board is AQA. Through each of the varied topics, you will be asked to question the impact of humans on natural systems and to consider the importance of maintaining those natural systems for humans to survive. The river emerged from a spring in the upper hills and we walked along several kilometres of its course, through narrow steep valleys down to the open fields around the hamlet of Holford.
The river crossed over distinct breaks in the local geology resulting is dramatic changes in its behaviour. This is a series of processes by which water is evaporated from the sea and eventually condenses and precipitates over the land.
It is the main input to the drainage basin and you can read detailed notes on this process at the Met Office's website. There are many changes that occur in rivers as a.