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Longshore drift
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Birling Gaps and Eastbourne's Coastline
My project is on Birling Gaps and Eastbourne's coastline. Their grid references are 553,960 (Birling Gap) and 630,003 (Eastbourne). These are both situated in the south east of England on the south east coast. The reason we are doing our work on these particular places is that these places have a recurring problem. Erosion.
!! BIRLING GAP !! & !! EASTBOURNE !!
Birling Gap and Eastbourne are both areas of coastline along the south east of England. We are focusing on these areas because they are areas, which the cliff-face is being eroded away. The erosion is happening at an incredible rate. This is because the cliff is made from chalk, which is a soft and
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Photo of a wave cut platform and the lighthouse.
Task
Having completed my fieldwork, I am being asked to structure a report, which will attempt to challenge the hypotheses that state -
1. The pattern of beach material along the coastline reflects natural beach processes.
2. Destructive beach profiles are steeper in gradient than constructive beach profiles.
3. Some parts of the East Sussex coast are managed better than Birling Gap.
4. Coastal management decisions do not reflect the land use of the surroundings.
Method ======
At each location I needed to collect information such as the name, grid reference, draw a field sketch, write a site description and find out the issues concerning coastal management. I need to level the beach profile and find out the direction of long shore drift. Landscape evaluations, Bi-polar scales, field sketching and photographs were very useful for this bit. All the information collected will help me write an illustrated description of each area. This plus other evidence should enable me to be able to accept or challenge the hypothesis'
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What processes operate like swash and backwash and long shore drift? And then I have to answer the question how are those processes linked to natural processes? And then find out and state whether it is true or false.
These 3 graphs (fig.1, 2, 3, 4, 5,6) are showing average rock size for Birling gap, rock type for both and rock size for both.
I also have some other graphs for beach profiles at birling gap and Eastbourne, long shore drift at Eastbourne and Birling Gap (fig 7,8 fig 9) these processes at Eastbourne do not compare (that much) to natural processes. Because if you look at figures 1 and 2 you will see that Birling Gap has a weak positive correlation and Eastbourne's results are all over that place with no correlation. This shows that the average rock size it completely different at Eastbourne because of the way the council always has to move the shingle around to help manage the beach properly.
Hypothesis 2
I found out that the gradient
Investigating the Geographical Processes that are Affecting the Physical and Built Coastal Environment There are three geographical processes that are affecting the physical and built coastal environment, they are; erosion, deposition, and transportation. Erosion is the group of natural processes, including weathering, dissolution, abrasion, corrosion, and transportation, by which material is worn away from the earth’s surface, this is mainly caused by wind, running water, and waves breaking on the coast. Deposition is the depositing something or the laying down of matter by a natural process. Transportation is when sand is moved along the coast by long shore drift. At North Cronulla beach erosion is evident.
town was just a small hamlet the only protection from the sea was by a
This shows that it is eroded at one end more which is a sign of long
In Roman times St. Mary's Church was built with Twin Towers as part of the building. Originally the church was 3kms away from the sea but as the cliff was eroded it eventually became next to the see. There was a danger the cliff under the Twin Towers and therefore the Twin Towers themselves would be destroyed by erosion. To stop this happening many coastal defences and different types of management have been erected. The initial try at coastal management was in 1809.
There are many different types of coasts that exist throughout the United States. The south shore of Long Island has a unique types of coast known as a barrier beach. Barrier beaches are long narrow land forms that are composed of sand and other lose sediments. These sediments are brought together by the actions of waves, currents and storm surges. Barrier beaches are subject to constant changes by the same forces. Sand is constantly eroded in one area an deposited in another. Barrier coasts are important for a number of reasons; they protect the mainland of Long Island from the open ocean and flooding during storms, for recreational use and the unique ecosystems which exist on barrier beaches.
This could be due to the loss of the Handbridge mills and also be because of the increase of bars in Chester City Centre, a haven for young people (just up the road). The first hydroelectric power station in Europe was built in Chester in the 20th century (1930). It was built on the site of the old flourmills along the River Dee, the most obvious sign of continuity in Handbridge is the River Dee itself we know this because from then to now it has always powered what ever has been put along side it e.g. the mills.
"Dugway Proving Ground." Wikipedia. Wikimedia Foundation, 16 Mar. 2014. Web. 19 Mar. 2014. Retrieved from http://en.wikipedia.org/wiki/Dugway_Proving_Ground
and link up with Burgoyne in Albany. The goal of this plan was to isolate
The Jericho Covered Bridge in Kingsville, Maryland was built in 1865 and restored in 1982. The bridge is 100 feet long and cased in cedar planks and timber beams. Legend has it that after the Civil War many lynchings occurred on the bridge. Passersby were supposedly captured on the bridge and hung from the upper rafters. The bridge is very close to my house and I have driven over it several times. The storyteller, age 19, also lives a couple minutes away from the bridge. He has lived in Kingsville, Maryland his entire life. He recalled a dramatic story he had heard from his older brother involving the haunted bridge.
Hmm, one that is still going strong is about… well I don't remember the name but it's this castle in Port Townsend, overlooking the bay.
The location of the study area is Silver Beach in Kurnell Peninsula, near Cronulla. It is located in the Sutherland Shire, south of Sydney Central Business District (CBD) and just directly south of Kingsford Smith International Airport. The area also has a historical significance as it is near the landing place of Captain James Cook on the 28th of April 1770 in Botany Bay.
OWLCREEK BRIDGE" ." ABP Journal. 1.1 (2005): n. page. Web. 23 Mar. 2014. Bierce, Ambrose “An Occurrence at Owl Creek Bridge”. The Norton Introduction to
...e deposits of the Bonneville flood make it one of the most competent in North America. The
This paper will attempt to do several things in regards to the Great Lakes Heritage Coast. First, the author will provide some background information pertinent to this issue. Secondly, a summary of the current status of the Great Lakes Heritage Coast as presented by the guest speaker. Furthermore, the author of this paper will provide a personal opinion in regards to the importance of a partnership with First Nations along the coast.
Factors Influencing Coastal Processes In this essay I aim to describe and explain factors affecting coastal processes. I will focus and explore how waves, tides, winds and mass movement processes can change the form of the coasts within our lifetime. The three key questions I will focus on are: * What are the energy and sediment inputs into the coastal system?