Tombolo

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Tombolo near Karystos, Euboea, Greece
Tombolo contrasted with other coastal landforms.

A tombolo is a sandy isthmus. A tombolo, from the Italian tombolo, meaning 'pillow' or 'cushion', and sometimes translated as ayre, is a deposition landform in which an island is attached to the mainland by a narrow piece of land such as a spit or bar. 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.[1] Two or more tombolos may form an enclosure (called a lagoon) that can eventually fill with sediment.

Formation[edit]

The tombolo connecting St Ninian's Isle with the Shetland Mainland
The Angel Road of Shōdo Island, 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
A satellite photo of the isthmus of Sutton which connects Howth Head and County Dublin

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[edit]

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.[2]

Unidirectional longshore drift[edit]

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 Portland, which it has reached. In this and similar cases like Cadiz, 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[edit]

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.

List of tombolos[edit]

[4]

See also[edit]

References[edit]

  1. ^ Glossary of Geology and Related Sciences. The American Geological Institute, 1957
  2. ^ Easterbrook, Don T. Surface Processes and Landforms, Second Edition. 1999 Prentice Hall Inc.
  3. ^ 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. p. 272. ISBN 978-0-87842-534-1.
  4. ^ D.D. Williams, CBI TAMUCC //CBI cbi.tamucc.edu/CHRGIS/University-Beach/

External links[edit]