A tidal strait is technically not a river but a strait connecting two oceans or seas. Tidal straits are narrow seaways through which tidal currents flow. Tidal currents are usually unidirectional but sometimes are bidirectional. They are frequently of tectonic origin. In them, currents develop because of elevation differences between the water basins at both ends. [1]
Tides sometimes allow sediments to collect in tidal straits. [2] [3]
See also
References
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^ Longhitano, Sergio G.; Mellere, Donatella; Steel, Ronald J.; Ainsworth, R. Bruce (April 9, 2012).
"Tidal depositional systems in the rock record: A review and new insights" (PDF). basin.earth.ncu.edu.tw. Retrieved 27 May 2019.
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^ Longhitano, Sergio; Steel, Ronald J. (June 2015).
"Deltas sourcing tidal straits: observations from some field case studies". Retrieved 27 May 2019.
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^ Rossia, V.M.; Longhitano, S.G.; Mellere, D.; Dalrymple, R.W.; Steela, R.J.; Chiarellae, D.; Olariua, C. (November 2017).
"Interplay of tidal and fluvial processes in an early Pleistocene, delta-fed, strait margin (Calabria, Southern Italy)". Marine and Petroleum Geology. 87: 14–30.
doi:
10.1016/j.marpetgeo.2017.02.021. Retrieved 27 May 2019.
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External links
- A facies‐based depositional model for ancient and modern, tectonically–confined tidal straits
- Deltas sourcing tidal straits: observations from some field case studies
- Notes on shipwrecks in the Arthur Kill ship graveyard
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