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string(209) ‘ by Dawdon as the result of say action and tidal power: where the mountain is more resilient headlands kind, and exactly where it is more readily eroded bays, like Dawdon Blast Beach, retreat inwards \(Holden, 2005\)\. ‘

Introduction and Backdrop:

This kind of report should assess the panorama evolution of the Durham shoreline, and to decide the past, present and future processes working on the coastline. Natural operations have formed the region pertaining to millions of years, and at present the area is definitely characterized by many physical features. These include Permian Magnesian Limestone Cliffs, froid sediments, increased beaches, incised valleys and small seaside headlands.

In the last 10, 1000 years the introduction of the costal zone has been in response to a switch coming from glacial to interglacial circumstances, and the resultant rising global sea level.

However , during the last century raising human activity offers artificially altered the coastline in a number of methods. In the north east of England, coal mining was the dominant sector until the early 1990’s. This kind of activity was often characterized by the dropping of vast quantities of waste rock and low-grade coal upon the beaches by seaside mines (Humphries, 2001). The disturbances due to active spend tipping to both the shoreline and the organic ecosystems in the area were extensive: in certain parts, the accumulations of waste reached 20m in thickness.

That said, the decline with the coal sector throughout the 1980’s and its ultimate closure brought about a review of the management of the coastline. The effect was the kick off of the alleged ‘Turning the Tide’ task, which was executed to restore earlier environmental circumstances, as well as create new socio-economic opportunities (Wilkinson and McCay, 1998). The website explains what sort of small managing team exists “to guard and boost the special characteristics of this one of a kind coastline (durhamheritagecoast. org). The project caused the removal of professional waste, the development of recreational initiatives and the starting of seaside footpaths. Within both activities and anthropogenic attitudes towards the management of the coastline have allowed the area to redevelop.

We stopped at two sites, at Dawdon (a site popular intended for sea angling) and Whitburn, to execute a number of duties in an attempt to understand these techniques more, and to try and forecast future improvements. As such, I possess divided this kind of project in to three individual categories: yesteryear and long term processes acting on the Clarington coastline, the modern activity in the region and the prediction of what may occur in the future. These types of categories will probably be followed by an analysis and summary.

Earlier and long lasting processes acting on the Oshawa coastline: the long-term development of Dawdon Blast Seaside and Whitburn

Chicken (1984) makes the point that the evolution of coastlines could be analyzed in several ways: geological structure, underwater processes, tidal conditions, changing sea levels and changing climatic operations. By citing the number of impacts that can play a role in the development of coastlines, Bird (1984) helps it be clear that if we are to understand the present and long term processes, we should first gain significant knowledge of the past. Therefore , in order to be familiar with Durham coast completely, we have to first look at the region’s historic geomorphology as well as its underlying geology.

Bridgland (1999) explains how a geology of Dawdon and Whitburn is usually primarily consisting of Permian Magnesian Limestone. Over a limestone lies a part of boulder clay, which will supports grasslands, plant life and also other wildlife. Heading further into time, though, reveals the influence of glaciation for the region’s geological development. Despegado deposits in the region reveal that ice was present until fifteen 1, 000 years ago.

Britain’s glacial record is, in some parts, incomplete and poorly understood. However , facts in the form of froid sediments, erratics, clast textiles and striae can give all of us some understanding as to the place that the ice originate from and how and why the sea-level has changed in the last 10, 000 years. Erratics are simply rocks that have been transported and deposited by a previously existing glacier (Holden, 2005). Holden (2005: 528) also explains how “glacial abrasion triggers striations as well as the smoothing of some surfaces. The evidence with this is in contemporary striae, that have been observed for Whitburn. Clastic fabric is composed of grains of rock, that have been weathered and eroded via previously existing bedrock (Holden, 2005). Travel of clastic material can often be by snow.

It is these types of separate types of evidence that together suggest that the 1st glacial snow to appear in the region came from the northwest (Lunn, 1995). The 2nd glacial ice cubes witnessed is usually attributed to the Cheviot as well as Tweed location. It has been proven that Whitburn is situated where recently different parts of ice may possibly have competed against one another before sooner or later merging. Johnson (1995) also notes that further proof of glacial activity in the region is available in the form of lakes, that happen to be suggested to have formed during periods of deglaciation.

Shennan et. ‘s (2006) include recently undertaken extensive exploration into family member sea level change, and attempted to rebuild British glaciers sheets. Data suggests that the Durham coastline is still addressing the increasing sea level and quick changes with the last 15, 000 years. Crucial to this area of study is the theory of isostasy, defined simply by Holden (2005: 718) as “the principle by which the Earth’s crust floats upon the denser mantle.  Shennan et. al (2006) make it clear just how relative ocean level alter, as a result of isostasy, depends not simply on sea-level change yet also land-level fluctuations. This can be a principle of isostatic modify.

The significance for past and long-term processes acting on the Durham coastline is that areas that were protected in snow, such as the northeast of Britain, are often still experiencing uplift as a result of their newfound buoyancy. The opposite will also apply to regions that had been not covered in ice cubes, such as the southern part of England, which can be currently subsiding. It is clear that the present day processes have already been shaped by the geological great the Bowmanville coastline.

Present day processes:

Dawdon Blast Beach is displayed in the appendix as physique 1 . The pronounced headlands and bays that exist over the Durham coastline are the response to different costs of erosion. Erosion is occurring at Dawdon because the result of trend action and tidal power: where the mountain is more immune headlands kind, and exactly where it is easier eroded bays, like Dawdon Blast Seaside, retreat inwards (Holden, 2005).

You go through ‘A record on the panorama evolution in the Durham coast’ in category ‘Essay examples’ Limestone, which, as previously said, are at the heart of the geology of the northeast coastline, can be described as rock which could produce intensive and described erosional features. On property these are called karst landscapes, but for the coast the erosion of limestone could lead to the introduction of features such as stacks, stumps and rebattu. The impact of the sea is the cause of very much unstableness over the coastline, rendering sediment and other material for the water to handle and first deposit elsewhere.

Certainly, the northeast coastline has little refuge from the impact of waves. But though erosion by wave action is commonly noticed along the Clarington coastline, the transportation and deposition from the eroded sediment along the shoreline relies on different processes, too. This is because the headland and bay features reduce the effects of longshore drift. The direction of transportation is north to south, and much of the material is trapped by the headland at the southern region end from the bay. It seems that the vehicles of sediment owes most of its presence to the power and path of the breeze, whereas design of the shoreline, and in particular the existence of headlands, is a root of very much deposition.

A number of the coastal features, though, happen to be anthropogenic in nature: mining has inspired Dawdon Great time Beach in several ways over the last 100 years. The vast amounts of squander that was simply likely onto outdoor has afflicted habitats and ecosystems, disappointed visitors and left the neighborhood communities with little pride about their exceptional coastline (durhamheritagecoast. org). But the waste as well raised outdoors level and left many cliffs remote from the sea. Evidence suggests that the puits were also accountable for the creation of a volume of artificial lakes as a result of their pumping away excess water below the natural sea level. The mining industry has had an ecological, environmental, sociable, economic and physical impact on Dawdon Blast Beach in the last 100 years.

Assessing erosion rates and predicting upcoming change:

The beach in Dawdon continues to be eroding in its northern end since the reduction of acquire waste showing. From 1994 onwards the beach has been supervised by the Environment Agency to evaluate erosion prices. In an attempt to predict any foreseeable future change within the coastline, we used a leveling strategy to construct our profile in the Dawdon Fun time Beach (figure 4), before comparing it with the organization data from 1994 to 2010 (figure 5). Figure 5 shows clearly that, over a relatively short period of the time (since 1994), the beach has suffered significant economic depression and yeast sediment loss. Learning the reason behind the erosion costs is an important take into account trying to determine any future changes.

Inspite of the closure from the mining market some in years past, the heritage of the spend left on Dawdon Fun time Beach goes on today. The waste created from the fun time furnace and mining industry actually inhibits heavy chafing to some elements of the high cliff, acting since an man-made wall to the power of the sea and wind. However , since this squander is eventually removed (it is predicted to have completely gone inside 15 years) the coves at Dawdon will become significantly exposed to the influence of natural procedures, and hefty erosion can be predicted to happen. This will lead to further inland retreat and lengthening in the bay.

Since explained previous, the process of longshore drift and sediment transport travels in the north towards the south along Dawdon Blast Seashore. Like the waste materials, the transferred sediment provides for a temporary blockade and signifies that the southern end with the beach will remain protected for longer. As the sediment transferred by longshore drift minimizes in variety, further chafing is forecasted to occur. Eventually, it will be necessary for anthropogenic intervention to prevent the coastline from being worn away too intensely. Human involvement may come as sea obstacles, or even in the introduction of sediment in which it has been considerably removed.


This task has uncovered how the Bowmanville coast has been shaped throughout geological record, examined the modern day procedures currently surrounding it to make an attempt for predicting future erosion costs and development. It is crystal clear that equally natural and anthropogenic processes have had a tremendous influence around the development of areas. The current coast and its landscape owe much of its living to the historic glaciers as well as the force with the tides, both equally past and present. Yet this task has also unveiled the magnitude to which liveliness and production of waste have inspired natural geological development. The waste made out of the recently booming mines has affected not only the modern processes (ironically, it in fact protected the cliffs via coastal erosion) but also what will happen in the foreseeable future.

The seal of the exploration industry, nevertheless, and the release of the ‘Turning the Tide’ project ensures that there is even more chance of the coastline re-discovering its organic state in the foreseeable future. Now all that can be seen from the colliery will be two set ups adjacent to the car park, and the predicted associated with all the existing waste implies that natural techniques will once again assume all their authority. Consequently, in the future we expect to see greater erosion rates than which at present exist. All the processes and impacts that the project offers investigated experienced influence, great on negative, on the development of the Durham coastal location, which has been and continues to be a cultural advantage, important to the region’s economic system, wellbeing and natural demeure.


Parrot, E. C. F. 1984 ‘Coasts: an introduction to coastal geomorphology. ‘ Blackwell third edition

Bridgland, D. R. 1999 ‘The Pleistocene Of North-East Britain. ‘ In: Bridgland, G. R., Horton, B. L. , Innes, J. B. (Eds). ‘The Quaternary Of North-East England. ‘ Discipline Guide, Square Research Connection, London, 1-9 www.durhamheritagecoast.org (accessed 8/4/2011)

Holden J, 2006, ‘An Introduction to Physical Location and the Environment, ‘ Second Edition, Pearson Education Essex

Humphries, D. 2001. ‘A review of family member sea-level rise caused by mining-induced subsidence in the coastal sector: some implications for elevated coastal downturn. ‘ Weather Research 18, 147-156

Manley, G., 1995: ‘Robson’s Geology of North East Britain. ‘ Transactions of the All-natural History Contemporary society of Northumbria 56, portion 5.

Lunn, A., 1995: ‘Quaternary. ‘ In: Manley, G., 95 (ed): ‘Robson’s Geology of North East England. ‘ Transactions from the Natural Record Society of Northumbria 56, part 5, 297-312.

Shennan, I., Bradley, S., Milne, G., Creeks, A., Bassett, S. , Hamilton, S. 2006 ‘Relative sea-level alterations, glacial isostatic modelling and ice-sheet reconstructions from the British Isles because the Last Despegado Maximum. ‘ Journal of Quaternary Research. 21: 585-599

Wilkinson, D. L. and McCay, In. A. J. (1998). In Fox, H. R., Moore, H. Meters. and McIntosh, A. M. (eds) ‘Land Reclamation: Achieving Sustainable Rewards, ‘ Balkerna: Rotterdam

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