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Unit 4, Lesson 2
        12/4/2011
Getting Started

Take a look at how wave erosion has made an impact on
                   just one coastline.

         Pay particular attention to the flags!
Waves are energy travelling
 through some sort of material.
They are created from wind blowing over the
                    water.
Parts of a wave
Measuring Waves
What do the pictures mean?
 Wave height: the vertical distance from the
                  highest
       part of a wave to the lowest

Wavelength: the horizontal distance between
      one wave crest and the next crest
What influences the size of a wave?
 Strong winds for an extended (long) period
                   of time

                    -VS-

  Strong winds for a short period of time
BIG     waves!



BIG storm, but don’t worry…it all fizzles
              out by morning
How do waves reach the shore?


 Generally, they arrive at an angle
    One part of the wave reaches shallow water
     sooner than the rest
    The water “feels” the bottom, which slows
     down the wave
Wave Refraction
 Makes the wave
  “bend”
 Can change the
  energy of the wave:
   Concentrate it
   Disperse it
How do waves erode the shoreline?
 As the waves break over time, they steadily
    erode away a little bit of the shoreline
Formations caused by wave erosion
Wave-Cut Cliffs



     Waves that cut into the bottom
     part of a cliff, eroding away the
     soil and rocks there
Arch
                                                Right
                                                there




A cliff eroded from two sides, which produces an open
Sea Stack

   A piece of tall
   rock that remains
   after the material
   above the arch
   eventually erodes
   away
So… a sea stack is the “grown-up”
of the arch.
Beaches= Deposition
Beaches
                    can also
                    be made
                    of…
                                Quartz

        Coral




                     Shells
That beach was
most likely made               Volcanic
from a mixture of                Rock
coral and shells
Difference between Winter and
             Summer
 During the summer, waves of lower energy
  bring sand up on to the beach and leave it
  there—makes soft sand
 Communities sometimes truck in loads of
  sand for the summer, as it is carried away
  by the waves because of its density
 During the winter, waves and storms of
  higher energy bring the sand back offshore—
  makes a steeper and rockier beach
Deposition Formations

Spit:




        Ridges of sand that extend away from the shore
Barrier Islands

             Land
            formed
            by sand

           (Miami Beach)
Issues with Urbanization on Barrier Islands
  A barrier island is the first line of defense
         against hurricanes—if there are
   houses/businesses instead, it will hit them
                       first
Groin

Traps sand on one
      side of
 structure, instead
of allowing sand to
   roll down the
     coastline
Issues with Constructing Groins
 The other side of the groin no longer has
  sand (it is collected by the wall)
 Often, another groin will be built to catch
  sand farther down
Structures built parallel to the
          shoreline

          Breakwater



            Seawall
Differences?
Breakwater: built away from the shore in the
 water
      A breakwater in a bay area can help keep boats
       safe from the energy of breaking waves
Sea Wall
 Built right along the shore
Please refer to the
“Interactive Activity”

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Wave Erosion and Deposition Lesson Power Point

  • 1. Unit 4, Lesson 2 12/4/2011
  • 2. Getting Started Take a look at how wave erosion has made an impact on just one coastline. Pay particular attention to the flags!
  • 3.
  • 4. Waves are energy travelling through some sort of material. They are created from wind blowing over the water.
  • 5. Parts of a wave
  • 7. What do the pictures mean? Wave height: the vertical distance from the highest part of a wave to the lowest Wavelength: the horizontal distance between one wave crest and the next crest
  • 8.
  • 9. What influences the size of a wave? Strong winds for an extended (long) period of time -VS- Strong winds for a short period of time
  • 10. BIG waves! BIG storm, but don’t worry…it all fizzles out by morning
  • 11. How do waves reach the shore?  Generally, they arrive at an angle  One part of the wave reaches shallow water sooner than the rest  The water “feels” the bottom, which slows down the wave
  • 12. Wave Refraction  Makes the wave “bend”  Can change the energy of the wave:  Concentrate it  Disperse it
  • 13.
  • 14. How do waves erode the shoreline? As the waves break over time, they steadily erode away a little bit of the shoreline
  • 15. Formations caused by wave erosion
  • 16. Wave-Cut Cliffs Waves that cut into the bottom part of a cliff, eroding away the soil and rocks there
  • 17. Arch Right there A cliff eroded from two sides, which produces an open
  • 18. Sea Stack A piece of tall rock that remains after the material above the arch eventually erodes away
  • 19. So… a sea stack is the “grown-up” of the arch.
  • 20.
  • 22. Beaches can also be made of… Quartz Coral Shells That beach was most likely made Volcanic from a mixture of Rock coral and shells
  • 23. Difference between Winter and Summer  During the summer, waves of lower energy bring sand up on to the beach and leave it there—makes soft sand  Communities sometimes truck in loads of sand for the summer, as it is carried away by the waves because of its density  During the winter, waves and storms of higher energy bring the sand back offshore— makes a steeper and rockier beach
  • 24.
  • 25. Deposition Formations Spit: Ridges of sand that extend away from the shore
  • 26. Barrier Islands Land formed by sand (Miami Beach)
  • 27. Issues with Urbanization on Barrier Islands A barrier island is the first line of defense against hurricanes—if there are houses/businesses instead, it will hit them first
  • 28. Groin Traps sand on one side of structure, instead of allowing sand to roll down the coastline
  • 29. Issues with Constructing Groins  The other side of the groin no longer has sand (it is collected by the wall)  Often, another groin will be built to catch sand farther down
  • 30.
  • 31. Structures built parallel to the shoreline  Breakwater  Seawall
  • 32. Differences? Breakwater: built away from the shore in the water  A breakwater in a bay area can help keep boats safe from the energy of breaking waves
  • 33. Sea Wall  Built right along the shore
  • 34. Please refer to the “Interactive Activity”