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What Is A Tombolo?How Is A Tombolo formed?Tombolos Around The WorldA tombolo is a coastal formation that means when translated from Italian “mound” It appears to be a small island that has not fully separated from the mainland This islandlike landform is actually attached to the coast by a thin sand bar or spit Tombolos are sometimes referred to as “tied islands” because it seems to tethered to the coast These formation can be either solitary or found in clusters When clustered the sand bars may form a lagoonlike enclosure near the coast These types of lagoons are likely to fill with sediment over time Longshore Drift Longshore drift occurs as waves push sediment (which may consist of sand silt and clay) towards the coastline at an angle Instead of landing on the beach this sediment begins to build up between the beach and an island creating the bar mentioned above and effectively “tying” the island to the mainland This drift is often influenced by the wind direction When created by longshore drift these formation are sometimes not considered a true tombolo Wave Diffraction And Refraction A true tombolo is formed by wave diffraction and refraction Waves move toward the coastline and are slowed down as they enter the shallower water They first reach the islands that are close to the shore Because these waves are moving at a slower than normal pace they move around the island instead of over it As the water moves more slowly around the island it picks up sediment along the way When the waves meet on the other side of the island (the side facing the coast) the sediment is Changing Tombolos Because of the unique shape of tombolos they tend to be more likely to change over time due to weathering and tides than the regular coastline Sometimes the island at the end of the bar or spit is large enough that it supports commercial or residential activity In order to prevent changes to the tombolo the bar is reinforced with cement roads or parking lots This prevents wind and waves from washing away the finer sediment on top of the bar One of the most wellknown tombolos around the world is Chesil Beach located on the southern coast of Dorset in England This beach connects to the Isle of Portland a 4mile long limestone island It is an inhabited island with a population of around 12400 The island and the beach belong to the Jurassic Coast a UNESCO World Heritage Site which is protected due to its unique geological formation Some scientists however have suggested that Chesil Beach is not actually a true tombolo Additionally this site is an important bird nesting area between April and August access to several areas here is prohibited during this time Another wellknown tombolo is the Aupouri Peninsula in New Zealand It is located on the northern side of the North Island between the Tasman Sea and the Pacific Ocean This site is interesting because it is a peninsula within a peninsula making up part of the North Auckland Peninsula This tombolo creates the Rangaunu Harbour as well as several othe Author Amber Pariona.
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Coastal Landforms: What Is A Tombolo? WorldAtlas
Tombolo Coastal landscapes Higher Geography Revision
Tombolo A tombolo is formed when a spit connects the mainland coast to an island A spit is a feature that is formed through deposition of material at coastlines The process of longshore drift.