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No rx required when buying your drugs. A photograph of Nettlecombe Court. Within Exmoor National Park there is a site of special scientific interest which is km2 large and a 4 km2 national nature reserve. There is a population of 10, people in Somerset and a census taken in showed that it had increased by 2. There are 1, enlisted buildings in Exmoor National Park and With regards to tourism, over 1. Land uses The main land uses in Somerset are, farmland, which is mainly pastoral sheep farming.
Woodland, where Deciduous and Coniferous trees grow which would have been ideal for fuel and as building materials when early settlers arrived. Settlements, such as Holford and Kilve, and moor land where vegetation such as heather and bracken grows. Page 6 of 59 Land Use map 7. Page 7 of 59 Land use along the course of the River Holford is important to look at because it could affect the characteristics if the channel.
As you can see on the land use map there is a high amount deciduous forest near the source meaning that the trees will intercept rain water and prevent it from reaching the river. This tells us that the sites near the forest will have a shallower depth. As you can see on the land use map on page 6 the River Holford flows through urban areas such as Kilve. In Kilve the channel has been altered by man making them more efficient.
This is due to the fact that there will be less friction between the water and the banks and bed of the river. Farming plays a major role in Somerset because it does not only take up most of the land space but, All together it is 7. The upper course of the River Holford is very steep and the lower course has hardly any gradient. The middle course is less steep when compared to the upper course.
This tells us that there is a decline in gradient from source to mouth. This is the mouth of the River Kilve.
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Page 8 of 59 OS map 9. Devonian Quartzite is found in the upper course of the River Holford where the gradient is steep. It is a hard, impermeable red metamorphic rock and means that the depth will be shallow here as water cannot percolate through it. The width will be narrow here seeing as the river requires more energy to erode the rock.
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Quartzite was once sandstone and this conversion took place after heat and pressure. Its appearance is red because of the amount of iron oxide and other chemical impurities inside it. Permo-Triassic Marl is also found in the upper course of the river and is a soft, impermeable sedimentary rock which is composed mainly of calcium carbonate. This means that the width will be larger here seeing as more erosion takes place in this part of the river.
However, the depth here is deep as less water is lost via percolation. Jurassic Limestone is found in the lower course of the River Holford and is a permeable sedimentary rock which is resistant to erosion. Limestone is mainly made from calcium carbonate. Because Jurassic Limestone is a permeable rock more water is lost via percolation meaning that there is less water in the channel.
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This tells us that the depth of the river will decrease at the sites where the geology is Limestone. This is an example of Quartzite. This is a sample of Jurrasic Limestone. This is an example of Permo- Triassic Marl. Page 10 of 59 Geology and site map Page 11 of 59 Hypotheses Aim: An investigation into the changing physical characteristics form source to mouth of the River Holford. Objectives: We will be looking at a number of different factors that change throughout the course of the river.
These will be the width of the river channel, the average depth, velocity, volume and the gradient. When these readings are taken there should be correlations between them. Hypothesis 1- The width of the river will increase as you move from the source to mouth. The width of a river channel increases as it goes downstream because tributaries and confluences join into it, thus making it wider because it holds more water.
In the upper profile of the river you would find mainly vertical erosionwhich cuts downwards. In the lower course of the river more lateral erosiontakes place which means the river cuts sideways into the valley.
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The river gets more powerful as you go down its course which means that it has more erosioncapability. There is also less energy waste on frictionas there is less substrate is on the bed. This is why you would expect a wider channel in the lower profile of the river. Hypothesis 2- The depth of the river will increase as you go from source to mouth. Depth is how deep the river is. As the River Holford flows along its course, tributaries and confluences join it which means there is more water in the river than at its source.
In the higher profile of the river mainly vertical erosiontakes place. This is the rapid down cutting of the bed. In the lower course of the river there is lateral erosionwhich means that the river erodes the valley sideways. However, as the river continues downstream there is less substrate on the bed which means that there less energy waste on friction. This means that there is more energy to erode the bed. Hypothesis 3- Gradient will decrease as you move from source to mouth. Gradient is the elevation of the river along its course.
This hypothesis has been made because the contour lines of an OS map are closer together at the source than any other point along the rivers course. The map tells us that the source is m high and the mouth is not elevated at all. Rivers cannot flow upwards and always flow at a negative gradient due to gravity. Page 12 of 59 Sequence of work Start Firstly we established our aims and hypotheses before embarking on this trip.
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Preparation Suitable equipment was selectedin order to measure the factors along the river accurately Practice We left school on the 16th October. Shortly after reaching our destination, we went to a nearby river and practised measuring using the different equipment. Fieldwork Many measurements such as the width, depth and gradient, were taken at eight different points along the River Holford. Data Collection The data which was collectedduring the fieldwork was analysed using graphs.
Write up The introduction and the methodology were then written about the background of the area and the different sites at which the different measurements were taken. This is a somatic diagram of how I prepared for and undertook my river study. Page 13 of 59 Methodology Page 14 of 59 Methodology In this section I shall be describing the different sites at which we collectedour primary data and methods that were used to collect this data.
I will also be looking at how the risks were minimized. Risk Assessment Risk How it was minimized There could have been rat faeces in the river which could have caused diseases if it got into the skin.