Investigate the impact of tourism and of a Park and Ride scheme on the natural limestone environment of Cheddar, in order to decide whether this Park and Ride should be built.

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Paragraph 1: Introduction

Cheddar, in Southwest England, is famous for its gorge and caves, which are features of the limestone area in which the town is located. Every year, these interesting landforms attract increasing amounts of tourists, which endanger the natural limestone environment of Cheddar, in particular the gorge.

A Park and Ride, which would be built at the Eastern entrance to the gorge, has been suggested as a possible way of solving this problem.

The aim of my coursework will be to investigate the impact of tourism and of a Park and Ride scheme on the natural limestone environment of Cheddar, in order to decide whether this Park and Ride should be built.

This decision-making exercise will be a cross-unit task, referring to two parts of the syllabus: “Water, Landforms and People”(physical geography) and “People, Work and Development”(human geography).

In the context of physical geography, I will look at the formation of the limestone scenery in Cheddar. The human aspect of my coursework will cover the impacts of tourism on this scenery, as well as the economical and social effects of a Park and Ride on the local area.

Collection of primary data:

In order to understand how the landforms at Cheddar were made, and how tourism can damage them, I have studied in class the action of water on limestone and the features it creates.

The primary data I needed, in order to analyse physical features and the importance of tourism, was collected during a field trip to Cheddar. It included a land use survey and visits to the caves, gorge and panoramic tower, all of which will help me determine how important tourism is to the local economy, and whether a Park and Ride might disrupt it. I also carried out a traffic survey to get an idea of the number of visitors and of the damage done to the gorge. Finally, I questioned a number of tourists to see if a Park and Ride scheme was really needed, and to understand why so many people come to visit Cheddar.

Location of Cheddar:

 Cheddar is situated in the South-West of England, in North Somerset. Map    shows that it is in the Mendip Hills, quite close to the Bristol Channel, to Bristol city (about 20 miles to the North-East) and to Bath (approximately 30 miles to the East). Cheddar is very accessible: it is quite near to junction 21 (12 miles away) and 22 of the M5 motorway (which links to the North and the Midlands). The M4 (which goes to South-Wales and London) can be reached easily, just above Bristol. The closest airport, Bristol international, is only 12 miles away and so is the closest railway station, in Yatton.

The area around Cheddar (which includes highly visited sites like Bath, Weston-Super-Mare, Wells and Glastonbury) relies a lot on tertiary industry, especially tourism.

Method:

In order to decide whether the Park and Ride should be built, I will first describe the characteristics of limestone scenery in the Cheddar area.

I will also investigate how tourism and traffic affect the natural environment in

Cheddar, and whether a Park and Ride scheme would be an effective way of protecting it.

In a second chapter I will display the results of my surveys, which will be referred to in other parts of the investigation.

My third chapter will look at the impacts of a Park and Ride on different groups of people. I will then weigh all environmental, economical, and social effects of the Park and Ride (or its absence) on the local area, and decide if it should be built.

Finally a conclusion will sum up my investigation, in which I will evaluate how reliable my decision was, depending on the quantity and accuracy of the information collected.

TASK 1: Limestone Landforms in Cheddar:

In order to understand why there is such an exceptional scenery at Cheddar, we need to look in detail at the particularities of limestone, the rock found in the Cheddar area.

Limestone is called a “sedimentary” rock because it was formed from layers of dead sea animals and corals, called sediments. These deposited at the bottom of the sea millions of years ago. These sediments gradually got buried under new layers, and the weight squeezed the water out of them. As the water disappeared, the salts it contained crystallized and cemented the sediment particles together, forming the rock.

There are three types of limestone:

Jurassic limestone, Chalk, and Carboniferous limestone, which is the type found in the Mendip Hills, where Cheddar is located .This kind of limestone was formed during the carboniferous era. It is gray, hard, and contains many fossils.

The special landforms found in Cheddar, which are called “karst” landforms, are due to certain particularities of carboniferous limestone:

Because it is made from the remains of seashells and corals (which contain Calcium and Carbon), carboniferous limestone consists mainly of Calcium carbonate. Rainwater contains dissolved Carbon dioxide, which is a weak acid (carbonic acid). This acid reacts with rocks that contain Calcium carbonate, and dissolves them slowly. This phenomenon called chemical weathering, dissolves limestone and removes it in solution (dissolved).

Limestone is laid out in layers, due to the gradual deposition of sediments at the time when the rock was forming. The layers are separated by bedding planes, which are horizontal. The vertical cracks are called joints. Both bedding planes and joints are areas of weakness, so they are dissolved by chemical weathering.

This explains another characteristic of limestone: it is pervious. This means that the rock is permeable, but the water can only pass through the rock along the bedding planes and down the joints.

As we will soon see, all landforms at Cheddar are due to the action of water (through chemical weathering) on carboniferous limestone, particularly on the bedding planes and joints.

The most important feature of the Cheddar landscape is the gorge. There are three theories as to how gorges are formed:

  1. A large underground cave is eroded and weathered. Its roof collapses, leaving a steep-sided valley, a gorge. Gordall (Yorkshire) is thought to have formed in this way.
  2. After an ice age, an ice sheet melts. This creates a huge volume of water that will erode valleys rapidly, causing steep sides as in a gorge.
  3. Gorges can also be formed by a waterfall, when a river flows on a layer of hard rock that has softer rock underneath. The falling water erodes the layer of soft rock, but not the hard rock, which overhangs. Gradually, the hard rock looses its support (the soft rock) and the overhanging part falls. This means that the waterfall moves back and slowly cuts its way up the valley, leaving a gorge.

I think that the most likely theory for Cheddar would be number 2_if Cheddar had been formed by a cave collapsing (like in theory 1), it is likely that there would be remains of the cave’s roof, so the bottom of the gorge would contain many blocks of rock and rubble. This is not the case in Cheddar, and the gorge is about 4 km long, which seems very big for a cave. I do not think that option 3 is very likely either: gorges created by waterfalls go straight, whilst Cheddar gorge has many turns. And although the river Yeo might have flown on the surface thousands of years ago, there is no evidence to support this theory, as there is no layer of hard rock on top of the limestone in the area of Cheddar. Theory 2 seems more likely_Four distinct layers can be seen on the sides of the gorge, which seem to correspond to the 4 ice ages that began over 2 million years ago. This suggests that Cheddar gorge was carved by floodwater from the melting ice sheet that stopped at Gloucester.

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The river drainage at Cheddar is typical of a limestone area: the gorge is a dry valley, because the river Yeo has gone underground through a swallow hole (at Compton Martin, grid reference 543 576 on the ordinate survey map), where the water disappears down the joints it has widened, mostly by chemical weathering. The river Yeo flows 30 meters below Gough’s cave, and reappears at a resurgence next to the tourist information center (grid reference 467 538). Diagram   page   shows the cause of this resurgence_the water underground has reached a layer of impermeable rock and cannot ...

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