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The effects of longshore drift
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Coastal Erosion Problems in Walton on the Naze
The reason for doing this piece of coursework is to investigate the
coastal erosion problems in Walton on the Naze. In this project I will
be answering one main question: What should be done about the erosion
of the Naze?
Walton on the Naze is a seaside resort along the coast of Essex just 8
miles south of Harwich, it is the most easterly part of the Essex
coastline and it is surrounded by the North Sea. Walton is situated in
southeast England and in north Essex, near Clacton (11km direct),
Colchester (27km direct), and Brightlingsea (19km direct). It is a
small English seaside town with a pier and a sandy beach. The Naze
itself is about 1.5 miles north of Walton pier.
The Naze is a promontory that stretches northwards from the edge of
Walton. It separates the inlet of Walton channel to the west, from the
North Sea to the east. Part of the Naze is made up of a hill, which
is being eroded by the sea so that cliffs, up to 20 metres high rise
directly from the beach.
It is a small English seaside town with a pier and a sandy beach. The
Naze itself is about 1.5 miles north of Walton pier.
In 1977 large defence work, including a sea wall and breakwaters, were
undertaken on the southern part of the Naze to protect the cliff top
properties. The unprotected length of coastline runs from the Tower
Break water northwards for approximately 1,000 meters to the start of
the old Anglian Water Authority floodwall. The cliffs decrease in
height northwards from 20 meters to 4 meters. The cliffs are made up
of sand and gravel deposits that lay on top of London clay and it is
because of t...
... middle of paper ...
...Possible improvements:
To improve my results I would use more sophisticated equipment such as
an electronic angle measurer for measuring the angles of the cliff. I
would also hire people to do the work for me so I would be able to get
more accurate results, in a shorter length of time. I would also do a
door-to-door survey, so I could get more questionnaire results and
they would be of what the people next to the sea and people a bit
further away from the sea and make a comparison on the two results. I
would also take more measurements at different times of the year that
were accurate and I could make a better comparison between the
results. I would also take more long shore drift measurements. I
could have also done my write up a bit quicker. We could have also
returned to the Naze and taken more measurements.
The only landmarks available to the eye are dozens of miles of ocean waves, occasionally broken up by an ocean going freighter or container ship that might sometime plod past the area, on their way inbo...
Dawlish warren is a major sand spit at the mouth of the River Exe, and
The Kimmeridge Clay Formation is the penultimate formation of the onshore British Jurrasic Succession. William Smith was the first to document this distinct formation on his map of 1815, and to name as the Oaktree Soil. In 1817, he gave the name Oaktree Clay for the layers of clay between the “Portland Rock” and “Coral Rag and Pisolite” but in 1816 Webster was the first to describe in details the formation and changed to the name now known as kimmeridge Clay Formation after the English village of Kimmeridge on Dorset’s “Jurassic Coast” a place frequently visited by fossil hunters. (Cox and Gallois, 1981).
The Don Valley Brickwork consists of many different layers of geological deposits, allowing us to observe and have a better understanding of how the sediments we see today are formed. The most bottom layer in the Brickworks are from the Georgian Bay Formation, and consists of grey- shale bedrocks. Fossils are often found in this layer and it is estimated that this deposit of sediments is around 445 million years old. Above the bedrocks is a thin layer of grey clay sand and gavels left behind by the Illinoian Glacier. This layer is called the York Till and occurred around 135,000 years ago. The next layer consists of a sandy deposit called the Don Formation, which is formed by the Sangamonian Interglacial Stage. Many plant and animal fossils are found in this layer due to warmer climate around 120,000 years ago. Above it lies the Scarborough Formation, which consist of clay and sand. This sediment likely occurred 115 - 106,000 years ago. The next layer above is the Poetry Road Formation, and consist of sand and gravel. This layer is likely formed during the early Wisconsin glacial substage around 106- 75,000 years ago. Higher is the Sunnybrook Drift which was formed 60 – 75,000 years ago. And on the surface, is the Halton Till, which was left behind by the final push of the Wisconsin Glacier.
coast (as shown in pictures 1 & 2). The area of sea is subject to the
dock as a place for the trade their goods, look at the map below to
See Location Map of the coastline being studied from Herne Bay to Reculver.
which can be used as a river, and also attracts people as it can be
Gloucester Massachusetts is known for its fishing industry. Over 1200 people’s jobs in Gloucester lay in the fishing industry. The fishing industry first derived when people from Europe came over looking for a better life. Gloucester is America’s oldest seaport, and now it is fighting to survive. Now with new rules, and diseases in the sea, the fishing industry will never be what it was decades ago.
The Corrymeela Community that is located on the Antrim Coast is a retreat center which hosts groups and conferences from all over Northern Ireland and the world. Most of the year is spent with different types of groups, including youth, and the summer is spent hosting families who have been affected by the Troubles either financially, by violence, or both.
However, Blackpool has begun to regenerate run down parts of the town. Nearly £300 million is planned for investment to help attract different types of tourists into the area. Blackpool has also been remarketed as a more contemporary resort, with a variety of fine dining restaurants and chic boutique style hotels.
The isle of Barbados lush with a wide range of beaches that is quite exquisite and enjoyable as beach holidays on the shores of the Caribbean Sea. Some of the beaches that are really amazing and enjoyable are Bottom Bay, Dover Beach, Bathsheba Beach, Crane Beach, Accra Beach, Paynes Beach and tons of others with mesmerizing coastal view and tremendous beach parties.
The neighborhoods of low-density residential, commercial, and industrial development display fine restaurants and antique shops with a full facility mountain resorts and a clutter of simple wood frame cottages. The variety of good low-cost accommodations and restaurants with lakes offering whitewater rafting and kayaking; including horseback riding, pack tours, fishing expeditions, and mountain riding.
see two piers jutting out into the Pacific. On either side of the piers are