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By:
Syazwani Ismail
   Spit is a long narrow ridges of sand and shingle which
       is projected into the sea from coastline




http://worldlywise.pbworks.com/w/page/15409212/Unit%201%20Section%20A%20-
%20How%20physical%20processes%20have%20created%20coastal%20landforms
   Longshore drift transports material along the coastline

   Spits formed in shallow and sheltered water when
    there is a change in the direction of the coastline

   Deposition occurs resulting in the accumulation of
    sand and shingle

   The material initially deposited is the largest
    material, dropped due to the reduction in energy
   Finer material is then deposited, helping to build up
    the rest of the spit

    As spit grow outwards, a change in wind direction may
    result in a change in the direction of the spit forming a
    curved end (recurved laterals)

   If growing across a river estuary, the length of the spit
    will be restricted

   A salt marsh may form in the sheltered, low energy
    zone behind the spit.
http://geobytesgcse.blogspot.com/2007/08/coastal-deposition-landforms-features.html
   a ridge of sand and shingle joining the mainland to an
          island




http://80.59.24.98/Joomla/index.php/geog-historia/prof-d-marcelino-urresti/88-tema-1o-relieve-
costero
   Tombolo's are created through the process of
    longshore drift

   A tombolo is formed where the spit continues to
    grow until it reaches an island, forming a link with
    the mainland, just like bridges
http://geobytesgcse.blogspot.com/2007/08/coastal-deposition-landforms-features.html
   a ridge of sand and shingle which has joined two
         headlands, cutting off a bay




http://www.3plains.com/uploads/image/wallpapers/ocean-wallpaper-2.jpg
   (a) a spit grows the whole way across a bay
    (b) a sandbank devlops offshore, parallel to the
    shore, and is moved towards the coastline by the
    waves and wind until it joins the mainland
   Behind the bar, a lagoon is created, where water has
    been trapped and the lagoon may gradually be infilled
    as a salt marsh
   Over time the lagoon will become infilled by
    deposition
http://geobytesgcse.blogspot.com/2007/08/coastal-deposition-landforms-features.html
Features           Spits
                              Summary
                                 Tombolos                      Bars

What is it?        a ridge of sand and   a ridge of sand and
                                                          a ridge of sand and
                   shingle projecting    shingle joining the
                                                          shingle which has
                   from the mainland     mainland to an   joined two
                   into the sea          island           headlands, cutting
                                                          off a bay
How does it form? when there is a    formed when spit (a)form when a
                  break in the       continue to grow spit grows the
                  coastline and drop outwards             whole way across a
                  in energy, long-   connecting the       bay
                  shore drift        mainland to the       (b) a sandbank
                  deposited the      offshore island just develops offshore,
                  material and build like bridges         parallel to the
                  up spit                                 shore until it joins
                                                          the mainland
Example            Hurst Castle Spit     Isle of Portland      Slapton Sands

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Formation of spits, tombolos and bars

  • 2.
  • 3. Spit is a long narrow ridges of sand and shingle which is projected into the sea from coastline http://worldlywise.pbworks.com/w/page/15409212/Unit%201%20Section%20A%20- %20How%20physical%20processes%20have%20created%20coastal%20landforms
  • 4. Longshore drift transports material along the coastline  Spits formed in shallow and sheltered water when there is a change in the direction of the coastline  Deposition occurs resulting in the accumulation of sand and shingle  The material initially deposited is the largest material, dropped due to the reduction in energy
  • 5. Finer material is then deposited, helping to build up the rest of the spit  As spit grow outwards, a change in wind direction may result in a change in the direction of the spit forming a curved end (recurved laterals)  If growing across a river estuary, the length of the spit will be restricted  A salt marsh may form in the sheltered, low energy zone behind the spit.
  • 7. a ridge of sand and shingle joining the mainland to an island http://80.59.24.98/Joomla/index.php/geog-historia/prof-d-marcelino-urresti/88-tema-1o-relieve- costero
  • 8. Tombolo's are created through the process of longshore drift  A tombolo is formed where the spit continues to grow until it reaches an island, forming a link with the mainland, just like bridges
  • 10. a ridge of sand and shingle which has joined two headlands, cutting off a bay http://www.3plains.com/uploads/image/wallpapers/ocean-wallpaper-2.jpg
  • 11. (a) a spit grows the whole way across a bay (b) a sandbank devlops offshore, parallel to the shore, and is moved towards the coastline by the waves and wind until it joins the mainland  Behind the bar, a lagoon is created, where water has been trapped and the lagoon may gradually be infilled as a salt marsh  Over time the lagoon will become infilled by deposition
  • 13. Features Spits Summary Tombolos Bars What is it? a ridge of sand and a ridge of sand and a ridge of sand and shingle projecting shingle joining the shingle which has from the mainland mainland to an joined two into the sea island headlands, cutting off a bay How does it form? when there is a formed when spit (a)form when a break in the continue to grow spit grows the coastline and drop outwards whole way across a in energy, long- connecting the bay shore drift mainland to the (b) a sandbank deposited the offshore island just develops offshore, material and build like bridges parallel to the up spit shore until it joins the mainland Example Hurst Castle Spit Isle of Portland Slapton Sands