Earth:Tombolo

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Short description: Deposition landform in which an island is connected to the mainland by a sandy isthmus
Tombolo near Karystos, Euboea, Greece
Tombolo contrasted with other coastal landforms.

A tombolo is a sandy or shingle isthmus. A tombolo, from the Italian tombolo, meaning 'pillow' or 'cushion', and sometimes translated incorrectly as ayre (an ayre is a shingle beach of any kind), is a deposition landform by which an island becomes attached to the mainland by a narrow piece of land such as a spit or bar.[1] Once attached, the island is then known as a tied island.

Several islands tied together by bars which rise above the water level are called a tombolo cluster.[2] Two or more tombolos may form an enclosure (called a lagoon) that can eventually fill with sediment.

Formation

The shoreline moves toward the island (or detached breakwater) due to accretion of sand in the lee of the island, where wave energy and longshore drift are reduced and therefore deposition of sand occurs.

Wave diffraction and refraction

True tombolos are formed by wave refraction and diffraction. As waves near an island, they are slowed by the shallow water surrounding it. These waves then bend around the island to the opposite side as they approach. The wave pattern created by this water movement causes a convergence of longshore drift on the opposite side of the island. The beach sediments that are moving by lateral transport on the lee side of the island will accumulate there, conforming to the shape of the wave pattern. In other words, the waves sweep sediment together from both sides. Eventually, when enough sediment has built up, the beach shoreline, known as a spit, will connect with an island and form a tombolo.[3]

Unidirectional longshore drift

In the case of longshore drift due to an oblique wave direction, like at Chesil Beach or Spurn Head, the flow of material is along the coast in a movement which is not determined by wave diffraction around the now tied island, such as the Isle of Portland, which it has reached. In this and similar cases like Cádiz, while the strip of beach material connected to the island may be technically called a tombolo because it links the island to the land, it is better thought of in terms of its formation as a spit, because the sand or shingle ridge is parallel rather than at right angles to the coast.

Morphology and sediment distribution

Tombolos demonstrate the sensitivity of shorelines. A small piece of land, such as an island, or a beached shipwreck can change the way that waves move, leading to different deposition of sediments. Sea level rise may also contribute to accretion, as material is pushed up with rising sea levels. Tombolos are more prone to natural fluctuations of profile and area as a result of tidal and weather events than a normal beach is. Because of this susceptibility to weathering, tombolos are sometimes made more sturdy through the construction of roads or parking lots. The sediments that make up a tombolo are coarser towards the bottom and finer towards the surface. It is easy to see this pattern when the waves are destructive and wash away finer grained material at the top, revealing coarser sands and cobbles as the base.

Examples


Some of these may be simple isthmuses, and not have the deposition creation that defines a true tombolo.[7]

Image gallery

  • The tombolo connecting St Ninian's Isle with the Shetland Mainland

  • Monte Argentario, Tuscany, Italy

  • Chesil Beach, seen from the Isle of Portland looking towards mainland Dorset

  • The Angel Road of Shōdoshima, Japan

  • Looking south from the summit of Mount Maunganui, New Zealand, to the city of Tauranga

  • The eastern end of Bennett Island with its glaciated tombolo in the background

  • Satellite view of Gwadar, Pakistan

  • An aerial photo of the isthmus of Sutton which connects Howth Head and County Dublin

See also

References

  1. ↑ De Mahiques, Michel Michaelovitch (2016). "Tombolo". Encyclopedia of Estuaries. Encyclopedia of Earth Sciences Series. pp. 713–714. doi:10.1007/978-94-017-8801-4_349. ISBN 978-94-017-8800-7. https://link.springer.com/referenceworkentry/10.1007%2F978-94-017-8801-4_349. Retrieved 2021-04-05. 
  2. ↑ Glossary of Geology and Related Sciences. The American Geological Institute, 1957
  3. ↑ Easterbrook, Don T. (1999). Surface Processes and Landforms (Second ed.). Prentice Hall. ISBN 0-13-860958-6. 
  4. ↑ Neal, William; Orrin H. Pilkey; Joseph T. Kelley (2007). Atlantic Coast Beaches: A Guide to Ripples, Dunes, and Other Natural Features of the Seashore. Missoula, MT: Mountain Press Publishing Company. pp. 272. ISBN 978-0-87842-534-1. 
  5. ↑ Venancio, Kelly Kawai; Garcia, Patrícia Dalsoglio; Gireli, Tiago Zenker; Corrêa, Thiago Bezerra (2020). "Hydrodynamic modeling with scenario approach in the evaluation of dredging impacts on coastal erosion in Santos (Brazil)". Ocean & Coastal Management 195: 105227. doi:10.1016/j.ocecoaman.2020.105227. https://www.researchgate.net/publication/341030281. 
  6. ↑ Brazilian Beach Systems. Coastal Research Library. 17. 2016. doi:10.1007/978-3-319-30394-9. ISBN 978-3-319-30392-5. https://link.springer.com/book/10.1007/978-3-319-30394-9. 
  7. ↑ Owens, Edward H. (1982). Beaches and Coastal Geology. Encyclopedia of Earth Sciences Series. pp. 838–839. doi:10.1007/0-387-30843-1_474. ISBN 978-0-87933-213-6. https://link.springer.com/referenceworkentry/10.1007%2F0-387-30843-1_474. Retrieved 2021-04-05. 

External links



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