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  2. Spit (landform) - Wikipedia

    en.wikipedia.org/wiki/Spit_(landform)

    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 ...

  3. Cuspate foreland - Wikipedia

    en.wikipedia.org/wiki/Cuspate_foreland

    Cuspate Forelands that move are typical of those that are formed on open coastlines. [1] The direction of migration is often indicated by a series of successive beach ridges on the advancing side of the foreland where there is less wave energy. [1] [4] The movement of cuspate forelands is commonly explained by longshore drift acting as the main ...

  4. List of geographical spits - Wikipedia

    en.wikipedia.org/wiki/List_of_geographical_spits

    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

  5. Orford Ness - Wikipedia

    en.wikipedia.org/wiki/Orford_Ness

    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.

  6. The Structure and Distribution of Coral Reefs - Wikipedia

    en.wikipedia.org/wiki/The_Structure_and...

    Canton Island typifies the isolated coral atolls dotting the Pacific Ocean. The Structure and Distribution of Coral Reefs, Being the first part of the geology of the voyage of the Beagle, under the command of Capt. Fitzroy, R.N. during the years 1832 to 1836, was published in 1842 as Charles Darwin's first monograph, and set out his theory of the formation of coral reefs and atolls.

  7. Spits of the Sea of Azov - Wikipedia

    en.wikipedia.org/wiki/Spits_of_the_Sea_of_Azov

    For example, the Arabat Spit (the largest and most stable spit on the Azov Sea) was formed only around 1100–1200 AD, [4] and some spits were partly or entirely washed away by water currents. [5] Many spits are used as resting ground by migrating birds (mostly ducks, geese, swans, sandpipers , great cormorants and seagulls, see e.g. this and ...

  8. Blakeney Point - Wikipedia

    en.wikipedia.org/wiki/Blakeney_Point

    The 400 m (440 yd) in 1817 had become 320 m (350 yd) by 1835, 275 m (301 yd) in 1907, and 195 m (213 yd) by the end of the 20th century. [1] The spit is moving towards the mainland at about 1 m (1.1 yd) per year; [70] and several former raised islands or "eyes" have already disappeared, first covered by the advancing shingle, and then lost to ...

  9. Spit - Wikipedia

    en.wikipedia.org/wiki/Spit

    Spit (archaeology), a term for a unit of archaeological excavation; Spit (landform), a section of land that extends into a body of water; Spit or rotisserie, a rotating device used for cooking by roasting over an open fire; Spit, another word for saliva. Spitting, the act of forcibly expelling saliva from the mouth