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A spit may be considered a special form of a shoal. As spits grow, the water behind them is sheltered from wind and waves, and a salt marsh is likely to develop. Dungeness Spit in the Strait of Juan de Fuca, on the U.S. Pacific coast. Wave refraction can occur at the end of a spit, carrying sediment around the end to form a hook or recurved ...
The debate involving how cuspate forelands form is ongoing. [2] However, the most widely accepted process of formation involves long shore drift. [1] Where longshore drift occurs in opposite directions, two spits merge into a triangular protrusion along a coastline or lakeshore. [1]
Toronto Islands (former spit, now detached), Toronto, Ontario; Leslie Street Spit, man-made spit created as part of new harbour project; Long Point, Ontario; Point Pelee, Ontario on Lake Erie; Rondeau Provincial Park - a crescentric sand spit on Lake Erie; Blackie Spit (east section of the Crescent Beach), South Surrey, British Columbia
Therefore, many spits stretch to the south into the sea and are continuations of the (right) river banks (see table and map). The Chushka and Tuzla spits are located inside the Strait of Kerch; the former spit is formed by the outflow of water from the Azov Sea to the Black Sea and therefore also faces south, whereas the latter is facing north ...
Orford Ness is a cuspate foreland shingle spit on the Suffolk coast in Great Britain, linked to the mainland at Aldeburgh and stretching along the coast to Orford and down to North Weir Point, opposite Shingle Street. It is divided from the mainland by the River Alde, and was formed by longshore drift along the coast.
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Larvikite rocks shipped from Norway now defend the start of the spit. The spit formed from loose flint pebbles which had been eroded from the cliffs further west. [5] Although originally formed by natural processes, Hurst Spit has been declining in volume, probably since the 1940s when coast protection works in Christchurch Bay first began to interrupt the flow of the shingle towards the spit. [6]
SH 75 skirts the hills of Banks Peninsula close to the spit's eastern end. [1] Although usually referred to as a spit, Kaitorete is technically a barrier beach. A spit is widest at the updrift end and tapers to a narrow tip at the downdrift end, but Kaitorete is narrower at the southernmost (updrift) end and widest at the northernmost ...