Lulworth Cove Coursework

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Geography Coursework

Lulworth Cove

Geography Coursework

David Hutton 10A

The management of Lulworth Cove benefits and sustains coastal environment

Aims and Introduction

In this coursework I am going to be exploring the advantages and disadvantages of tourism to the Lulworth area and how the management of Lulworth Cove benefits and sustains the coastal environment. The aim will be to show how the council are trying to slow down the erosion rate of the area, and if tourism has helped or has been a disadvantage to the region. While doing this, many methods were performed to get the most accurate results, as I will discuss later.

Lulworth Cove is situated on the south coast of England; in the county of Dorset. It is near the village of west Lulworth which is located around 8 miles west of Weymouth on the Jurassic coast world heritage site. 

Lulworth Cove and its surrounding area is one of the most visited geographical sites in the world. This means that there is a vast amount of tourists visiting the region each year; over 1 million a year. As a result of this there have been some vast changes to Lulworth and its coastal environment.

Lulworth is a band of rock strata running parallel to the shore; a concordant coastline. This concordant coastline has formed several coves across the area, such as Lulworth Cove which we all know so famously today.

Figure 2 – Aerial view of Lulworth Cove

Lulworth Cove would have been formed over hundreds of thousands of years. Initially there would have been several bands of rock running parallel to the shore. Before the limestone cliff face we see today there was clay and different sands, these have been eroded at a fast rate. This leaves Portland and Purbeck limestone to form the shoreline, this rock type is much more robust and resistant to erosion and the constant waves thrashing at it. A weakness in this limestone means that the sea is able to break it down due to hydraulic action, eventually this weakness will erode to an extent that it forms the entrance to the weaker rock types; such as clays and sands. Erosion is now able to carry on at a quicker pace than with the limestone. This therefore forms the cove.

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Stair Hole, less than a mile up the coast is another example of erosion. It is younger than Lulworth cove and this may give us an idea to what Lulworth Cove would have looked like in the past.

Method

During my visit to Lulworth Cove I did many surveys and took several statistics of the various places we were. The different techniques will tell us if the tourism is helping the coastal environment.

One survey I did focus directly on the tourists, by using a tourist questionnaire and tally chart. However, not all the people we asked ...

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