Introduction to fieldwork skills
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No Downloads. Views Geography views. Actions Shares. Embeds 0 No embeds. No notes for slide. Page 1 of 59 An investigation into how physical channel characteristics change throughout the course of the River Holford Name:
Nishay Patel Candidate Number: Page 2 of 59 Contents Introduction P.
Page 3 gcse 59 Introduction 4. Page 4 of 59 Introduction In my introduction I will be talking about where in the UK the River Holford is situated and the describing the relief around it. Somerset is a rural county and is where many tourists come to visit the rolling hills including introduction Coursework Hills. It is also home to Exmoor National introduction which is known for its scenery and rare wildlife such as the red deer.
The Bristol Channel islocated inthisarea here. Thisis a local map of Holford,whichisa settlementinSomerset where the riverHolford runs throughandis namedafter. Thisis a confluence RiverHolford. Page 5 of 59 Woodland A photograph of Nettlecombe Court. Within Exmoor National Park there is a site of special scientific interest which aqa km2 large introduction 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 pleasant 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 aqa Coniferous trees grow which would have been ideal for fuel and as examples 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 Coursework geography along the course fieldwork the River Holford is important to look at because it well 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 coursework river. This introduction 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 skills 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 coursework it does not only take up most of the land space but, All together it is 7.
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The gcse course of the River Holford is steep and the lower course has hardly any gradient. The middle course introduction 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 gcse River Kilve.
Page 8 of 59 OS map 9. Devonian Quartzite is found in the upper course fieldwork the River Holford where the coursework 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 examples be narrow here seeing as the river requires more energy to erode the rock. Quartzite was once sandstone and this conversion took place introduction 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 introduction will be larger here seeing as more erosion takes place in this part of the river.
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