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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. Spits of the Sea of Azov - Wikipedia

    en.wikipedia.org/wiki/Spits_of_the_Sea_of_Azov

    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 ...

  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. Longshore drift - Wikipedia

    en.wikipedia.org/wiki/Longshore_drift

    Spits are formed when longshore drift travels past a point (e.g. river mouth or re-entrant) where the dominant drift direction and shoreline do not veer in the same direction. [6] As well as dominant drift direction, spits are affected by the strength of wave-driven current, wave angle and the height of incoming waves. [7]

  6. Hurst Spit - Wikipedia

    en.wikipedia.org/wiki/Hurst_Spit

    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]

  7. Arabat Spit - Wikipedia

    en.wikipedia.org/wiki/Arabat_Spit

    The southern part of the spit viewed from Arabat Fortress Aerial view of the spit between the Syvash lagoons (left) and Sea of Azov (right). The Arabat Spit (Ukrainian: Арабатська коса; Russian: Арабатская коса; Crimean Tatar: Arabat beli) or Arabat Arrow is a barrier spit that separates the large, shallow, salty Syvash lagoons from the Sea of Azov.

  8. Saliva - Wikipedia

    en.wikipedia.org/wiki/Saliva

    Saliva on a baby's lips. Saliva (commonly referred to as spit or drool) is an extracellular fluid produced and secreted by salivary glands in the mouth.In humans, saliva is around 99% water, plus electrolytes, mucus, white blood cells, epithelial cells (from which DNA can be extracted), enzymes (such as lipase and amylase), and antimicrobial agents (such as secretory IgA, and lysozymes).

  9. Kaitorete Spit - Wikipedia

    en.wikipedia.org/wiki/Kaitorete_Spit

    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 (downdrift) end. Unlike a spit, it is attached to land at both ends (although somewhat tenuously at its westernmost extremity).