From Wikipedia, the free encyclopedia
Narrow seaway connecting two oceans or seas
A tidal strait, between two landmasses
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
^ 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 . {{
cite web }}
: CS1 maint: multiple names: authors list (
link )
^ Longhitano, Sergio; Steel, Ronald J. (June 2015).
"Deltas sourcing tidal straits: observations from some field case studies" . Retrieved 27 May 2019 . {{
cite web }}
: CS1 maint: multiple names: authors list (
link )
^ 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 . {{
cite journal }}
: CS1 maint: multiple names: authors list (
link )
External links