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costal structure

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  • 1. Marine Coastal Structure Submitted to: Dr. s.k.rout Submitted by: Kartik Mondal AEM-124 FS-10/13 F.F.SC
  • 2. Coastal System A beach is part of a coastal system, which includes several zones defined by their proximity to shore and the dominant processes that occur within them.
  • 3. Offshore to Shoreface • Offshore and shoreface portions of the coastal profile are permanently submerged in water, below the low tide mark. • An important feature that separates the offshore from shoreface zones is fairweather wave base – the depth at which water is affected by wave movement under normal weather conditions.
  • 4. Offshore zone • The offshore zone lies below fairweather wave base and is therefore unaffected by normal waves. • The offshore zone normally only receives fine sediment that settles from suspension (but can receive coarser grained sediment during storms, when wave base is lowered).
  • 5. Shoreface zone (lower part) • The shoreface zone lies above fairweather wave base and is constantly affected by normal waves. • The gentle gradient of the lower shoreface results from the smoothing out of sediment associated with the back and forth movement of the waves.
  • 6. Shoreface zone (upper part) • Near the top of the shoreface zone, the base of a wave is slowed down due to friction with the seabed • The wave is oversteepened, and breaks, losing much of its energy. • Due to the loss of energy, some sediment can be deposited in sand bars.
  • 7. Foreshore (The lower part of a beach) • Once a wave breaks, its water moves as a sheet upslope as swash, and falls back toward the sea as backwash. The narrow area in which this occurs is called the swash zone. • The location of swash zone shifts due to the rising and falling of the water level, associated with tides. • The area affected by the swash zone on a daily basis is called the foreshore (between low and high tide marks)
  • 8. Foreshore (the lower part of a beach) • As the flow of swash slows (and eventually stops) in its upper reaches, some of the sediment carried by the water can be deposited. • But much of the sediment is returned back down to the upper shoreface due to backwash.
  • 9. Backshore • Beyond the Foreshore of some beaches is a backshore zone, characterized by dunes. Dunes are constructed by windblown sediment transported from the foreshore and elsewhere. • Sediment can also be transported to the backshore area during storms, when big waves can reach far inland (note that a storm beach face can be seen well away from the normal beach face).
  • 10. So where does beach sediment come from ? • Not all shorelines are alike. Whereas some shorelines are dominated by deposition (as is the case for sandy beaches), others are dominated by erosion. Erosional shoreline area (material removed) Erosional shoreline area (material removed)
  • 11. • Shorelines characterized by exposed bedrock and strong wave activity are important suppliers of beach sediment. • Minerals of beach sediment derived mostly from eroded rocks along the coast match those of the source rocks. Sediment from coastal erosion
  • 12. Sediment from rivers • …But most sediment supplied to beaches along continental coastlines is delivered to the coast by rivers. • When a river enters a large body of water (e.g. ocean), its flow rapidly decreases, resulting in the deposition of sediment at the river mouth. • The resulting sediment deposit is a delta. •
  • 13. Importance Of Coastal Zone The dynamic processes that occur within the coastal zones produce diverse and productive ecosystems which have been of great importance historically for human populations. Coastal margins equate to only 8% of the worlds surface area but provide 25% of global productivity. Stress on this environment comes with approximately 70% of the world’s population being within a day’s walk of the coast. Two-thirds of the world’s cities occur on the coast. Valuable resources such as fish and minerals are considered to be common property and are in high demand for coastal dwellers for subsistence use, recreation and economic development.  Through the perception of common property, these resources have been subjected to intensive and specific exploitation. For example; 90% of the world’s fish harvest comes from within national exclusive economic zones, most of which are within the sight of shore.  As a whole, human activity in the coastal zone generally degrades the systems by taking unsustainable quantities of resources.The effects are further exacerbated with the input of pollutant wastes.This provides the need for management. Due to the complex nature of human activity in this zone a holistic approach is required to obtain a sustainable outcome.
  • 14. Reference: WEBSITES : www.google.com www.wikipedia.com www.worldofteaching.com BOOKS : “Text Book of Ecology and Environmental Science” - M.Prasanthrajan and P.P.Mahendran
  • 15. Thank You