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Coastal processes and landforms. 1. Terms 2. Wave actions 3. Landforms 4. Coral reefs 5. Sediment cells 6. Storm & swell profiles. 7. Coastal management.
Terms ,[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object]
Wave action. ,[object Object],[object Object],2. Describe the processes of marine erosion.  Using examples, explain how marine erosion  can affect cliff coastlines. 3. Describe the processes of marine erosion  and explain how these processes can influence  the formation of a wave-cut platform. 4. Explain how waves can transport and deposit Sediment in coastal areas.
[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],Sea waves generated & types of waves.
Constructive & destructive waves. Constructive waves Destructive waves
[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],Marine erosion and wave-cut platform.
[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],Wave-cut platform
Explanation on how waves transport and  deposit sediment in coastal areas
Landforms ,[object Object],[object Object],[object Object],Describe the main features of spit and salt marshes and explain formation. Explain why spits and salt marshes are subject to  change and are considered fragile environments.  Suggest ways in which they can be protected. With the help of diagrams, describe the features of 3  different types of coastal depositional landform and  explain the formation of each.
Spits & salt marshes. ,[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object]
Diagrams of spit and salt marshes.
Features of spits and salt marshes. ,[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object]
Fragile environments (spits and salt marshes) & ways in which they can be protected. ,[object Object],[object Object],[object Object],[object Object]
Coastal depositional landform and formation.  Coastal depositional landforms: Spits, bars, dunes and salt marshes and beaches ,[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object]
Bars: These form in the same way as a spit initially but bars are created where a spit grows across a bay, joining two headlands. Behind the bar, a lagoon is created, where water has been trapped and the lagoon may gradually be infilled as a salt marsh develops due to it being a low energy zone, which encourages deposition. Example of a Bar:  Slapton Sands - Devon.
[object Object]
 
Cliff profile affected by nature of rocks.
Factors that affect cliff profile. ,[object Object],[object Object]
Factors that affect sea cliff profiles. ,[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object]
Coral reef ,[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object]
Fringing, Barrier and Atoll. ,[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object]
Theories of formation
Changes in sea level affect the formation and continued existence of coral reefs and atolls Coral is sensitive to heat and light it is also sensitive to changes in sea level as reefs cannot survive long periods of sub-aerial exposure.  Falls in sea level can lead to the death of coral and to the emergence  of the reef above high water forming low lying land such as keys.  The islands become colonized by vegetation. To a certain extent reefs can contend with sea level rise leading to the growth of thick reefs (Darwins model).  However rapid rise consequent upon global warming may result in  inundation and destruction.
Condition for coral reef formation ,[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object]
 
Sediment cell and landforms. ,[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object]
Describe and explain the features shown below and account for the  Differences between the storm and swell profiles. STORM & SWELL PROFILES.
Storm and swell profile.
Coastal management Explain how human activities have affected the physical environment  in a coastal area or coastal areas you have studied. Explain the problems of the sustainable management of a stretch or  stretches of coastline you have studied.
Problems of coastal management and evaluate the solution ,[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object]
Human activities affecting coastal environment.
Sustainable management of coastlines. ,[object Object],[object Object],[object Object],[object Object]

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Coastal Processes And Landforms

  • 1. Coastal processes and landforms. 1. Terms 2. Wave actions 3. Landforms 4. Coral reefs 5. Sediment cells 6. Storm & swell profiles. 7. Coastal management.
  • 2.
  • 3.
  • 4.
  • 5. Constructive & destructive waves. Constructive waves Destructive waves
  • 6.
  • 7.
  • 8. Explanation on how waves transport and deposit sediment in coastal areas
  • 9.
  • 10.
  • 11. Diagrams of spit and salt marshes.
  • 12.
  • 13.
  • 14.
  • 15. Bars: These form in the same way as a spit initially but bars are created where a spit grows across a bay, joining two headlands. Behind the bar, a lagoon is created, where water has been trapped and the lagoon may gradually be infilled as a salt marsh develops due to it being a low energy zone, which encourages deposition. Example of a Bar: Slapton Sands - Devon.
  • 16.
  • 17.  
  • 18. Cliff profile affected by nature of rocks.
  • 19.
  • 20.
  • 21.
  • 22.
  • 24. Changes in sea level affect the formation and continued existence of coral reefs and atolls Coral is sensitive to heat and light it is also sensitive to changes in sea level as reefs cannot survive long periods of sub-aerial exposure. Falls in sea level can lead to the death of coral and to the emergence of the reef above high water forming low lying land such as keys. The islands become colonized by vegetation. To a certain extent reefs can contend with sea level rise leading to the growth of thick reefs (Darwins model). However rapid rise consequent upon global warming may result in inundation and destruction.
  • 25.
  • 26.  
  • 27.
  • 28. Describe and explain the features shown below and account for the Differences between the storm and swell profiles. STORM & SWELL PROFILES.
  • 29. Storm and swell profile.
  • 30. Coastal management Explain how human activities have affected the physical environment in a coastal area or coastal areas you have studied. Explain the problems of the sustainable management of a stretch or stretches of coastline you have studied.
  • 31.
  • 32. Human activities affecting coastal environment.
  • 33.