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theory on how groynes stop longshore drift
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To determine how groynes prevent longshore drift.
The issue:
Longshore drift influences the deposition and erosion of sediments. Waves erode the coast and transport the eroded material along the coastline. Over a period of time, the material will be deposited on a beach or form a larger feature such as a spit. Groynes are structures built at equal intervals along the coastline. Their purpose is to restrict longshore drift, preventing coastal erosion.
Figure 1 - Google Maps
About the location:
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.
Figure 2 - Close up of the study area, Silver beach is located just on the border of Captain Cook Drive
Figure 3 - Captain Cook Obelisk, taken by Saksham Yadav on 25/2/14 at Botany Bay
Importance of the issue:
Longshore drift is a process by which sediments are transported from one place to another. When this process occurs, beaches, spits and sandbars are accreted over time. If the process of longshore drift is altered by factors such as stronger winds and stronger currents, beach erosion begins at a faster rate and this may result in many serious problems. The main stakeholders of longshore drift are resort owners. They rely on people to visit their resorts and enjoy the beach. However, if longshore drift erodes too much sand, it can permanently deprive sand from the area, which can also threaten structures close to the shoreline.
How the issu...
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...otection: Groynes." Coastal Protection: Groynes. Slideshare, n.d. Web. .
"Geography Site: Coasts - Longshore Drift." Geography Site: Coasts - Longshore Drift. N.p., 11 Jan. 2008. Web. .
"Groynes as Shore Protection." - Coastal Wiki. N.p., 24 Oct. 2012. Web. .
"Landing Place Reserve." Kurnell. N.p., n.d. Web. .
"Silver Beach, Kurnell." - Sutherland Shire Council. N.p., n.d. Web. .
Figure 9 - Captain Cook Obelisk (Vando in the foreground) - Photo by Saksham Yadav at Botany Bay
coast (as shown in pictures 1 & 2). The area of sea is subject to the
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.
is being eroded by the sea so that cliffs, up to 20 metres high rise
Longshore drift influences the deposition and erosion of sediments. Waves erode the coast and transport the eroded material along the coastline. Over a period of time, the material will be deposited on a beach or form a larger feature such as a spit. Groynes are structures built at equal intervals along the coastline. Their purpose is to restrict longshore drift, preventing coastal erosion.
In 2001, the two proprietors decided to do something to protect their property. On December eleventh, Pismo Beach authorized a Coastal Development Permit that allowed them to begin construction of a seawall to act as a buffer against the erosive impacts of water that crash upon the side of the cliff (W12b). The seawall stands fifteen to twenty feet above the water and is one hundred sixty-five feet in length with a width of one and a half feet (W12b). Looking at this wall, I thought it was a shelf of sedimentary rock of which the face of the cliff was naturally composed. However, after closer examination, I realized that it actually was man-made. According to my cousin, who was a member of the construction crew for the Cavanaugh-Grossman Seawall, the cosmetic appearance of the bulkhead was required to be the same color as the bluff which it protects. This wall towers fifteen to twenty feet above the surface of the ocean water, stretches one hundred sixty-five feet along the cliff, and is one and a half feet thick. As I gazed upon it, I thought to myself that no wave could penetrate this giant edifice.
name. The first beach on the right was code named “Utah”. The second beach from
Semaphore Beach is affected by many factors such as natural processes and human impacts including marine litter and the discharge of stormwater. Therefore, several plans have been employed to ensure that the coast is supported through the method of counteracting erosion. However in the future, many management strategies have been put into consideration as well as the environmental, economic and social impacts as well as the predicted consequences. These impacts include traffic related incidents, noises and air pollution and the disruption of wildlife and the erosion of dunes. A method that should be considered for future management of the beach is the use of a concave sea wall, although efficient, this structure would be quite costly. Without the use of coastal management, Semaphore Beach would be unsupported, therefore negatively being affected by a variety of
One reason for this erosion is the oil and natural gas business. This industry has built many wellheads out in the Gulf, which transport the mined resources back to the coast through extensive underwater pipeline canals and navigational channels. The intrusive nature of this system requires the removal of land from the delta. An oil and gas industry-funded study found that this industry has removed one-third of the delta-land loss. Another human-induced risk factor was the US Army Corps of Engineer...
the coast some of the artifacts may be floating in the Sea. For example, pumice, a brilliant,
...ansportation in the natural direction of the littoral drift. This particular jetty is responsible for the accretion of sediment immediately adjacent to the South Jetty (Kraus).
Erosion is when the elements such as wind, water, and ice remove pieces of land. (“What is Coastal Erosion?”) Coastal Erosion takes place when destructive waves wear parts of the coast away. Four ways in which this takes place are corrasion/abrasion, hydraulic action, attrition, and corrosion/solution. (“Internet Geography”) Corrasion/abrasion is when materials are hurled at the base of cliffs through waves. Hydraulic action is when waves hit the base of a cliff and air is compacted, when the wave leaves air is rushed out and often this causes the material to break. Attrition is when the waves cause rocks and pebbles to smash into each other and eventually break into pieces. Finally, Corrosion/solution is when certain types of cliff erode from the result of acids in the sea. (“Internet Geography”) Coastal Erosion is the natural process of taking land away permanently from one place to put it somewhere else. (“What is Coastal Erosion?”) Eroding coastlines are an abundant and important topic because it can change people’s surroundings in a negative way. I would like to address the questions surrounding Coastal Erosion.
As storms and wave heights, along with a general change in wave and wind direction, surge during the fall and winter months, beach berms and occasionally the dunes erode in reaction, causing the beach to lower as sand is hauled offshore from the upper portions of the beach and deposited in shielding offshore sandbars (Learn More about Beaches & Dunes). The result is typically a flatter, more concave beach shape. The sandbars that form offshore in winter help protect the beach by causing waves to break farther offshore. There tends to be more coarse sediments in beach deposits, and any large storm can...
Just as important as understanding the definition of coastal erosion, is appreciating where the phenomenon it is happening. It is important to recognize that coastal erosion does not affect every beach and coastal area in the world. In fact, there are many areas of the world’s coasts that are actually growing from sediment deposits. Whether a particular costal area is growing or eroding is the result of complex natural (and sometime unnatural) process (Williams). Furthermore, the ability of scientists to find out exactly if a coast is eroding (and if it is, by how much) is critical for science to better understand the issue of coastal erosion. Scientists are able to look at geological data and take specific measurements of coastlines at different times of day and at different tida...
Surfers, swimmers and sunbathers use beaches for recreation. People fish off beaches for food. Since many people take their vacations at the beach, lots of beaches in tropical locations are important to their country’s economy. Entire cities, regions and countries depend on the money tourists spend while visiting the beach. Beaches are naturally very dynamic places, but people try to control them and build permanent structures, such as houses, restaurants, shops and hotels, on or near the shore. The natural erosion and deposition of beaches becomes a problem. Beaches con disappear over time, or even over night during severe storms. Beaches are areas of loose sediment (sand, gravel, cobbles) controlled by ocean processes. Most beaches have several characteristic features. First are offshore bars, which help protect beaches from erosion. Next is the foreshore, which rises from the water toward the crest of the next feature; a berm. On low-lying shores, dunes form behind beaches. Dunes look like rolling hills of sand and are blown into place by the wind. New, smaller dunes are often changing shape as the wind continues to affect them. Waves and currents move the accumulated sediment constantly creating, eroding and changing the coastlines.
This is when the rock fragments from Otakamiro Headland are ripped away by waves, broken down by attrition and transported along the coast where they are deposited as beaches and sand dunes. The movement of the material is called Longshore Drift; the direction of the deposit depends on the direction of the winds.