Inlet

An inlet is an indentation of a shoreline, usually long and narrow, such as a small bay or arm,[1] that often leads to an enclosed body of salt water, such as a sound, bay, lagoon, or marsh.

Bay at the Gulf of Salerno

Overview

In sea coasts, the term "inlet" usually refers to the actual connection between a bay and the ocean and is often called an "entrance" or a recession in the shore of a sea, lake, or river. A certain kind of inlet created by glaciation is a fjord, typically but not always in mountainous coastlines and also in montane lakes.

Complexes of large inlets or fjords may be called sounds, e.g., Puget Sound, Howe Sound, Karmsund (sund is Scandinavian for "sound"). Some fjord-type inlets are called canals, e.g., Portland Canal, Lynn Canal, Hood Canal, and some are channels, e.g., Dean Channel and Douglas Channel.

Tidal amplitude, wave intensity, and wave direction are all factors that influence sediment flux in inlets.[2]

On low slope sandy coastlines, inlets often separate barrier islands and can form as the result of storm events.[3] Alongshore sediment transport can cause inlets to close if the action of tidal currents flowing through an inlet do not flush accumulated sediment out of the inlet.[4]

gollark: Three of those are software, not hardware.
gollark: Again, PRISM.
gollark: * copied, not lost
gollark: I mean, see, osmarks.tk employs something like one person and we have two servers! Google has thousands of people who maybe have access, could actually make money off selling data, and has a lot of places it could get lost.
gollark: You SHOULD NOT trust them. You have NO VALID REASON to trust them. You have MANY GOOD REASONS to distrust them.

See also

Notes

  1. "inlet". Dictionary.com. Ask.com. Retrieved July 6, 2014.
  2. Chen, Jia-Lin; Hsu, Tian-Jian; Shi, Fengyan; Raubenheimer, Britt; Elgar, Steve (2015-06-01). "Hydrodynamic and sediment transport modeling of New River Inlet (NC) under the interaction of tides and waves". Journal of Geophysical Research: Oceans. 120 (6): 4028–4047. doi:10.1002/2014JC010425. hdl:1912/7468. ISSN 2169-9291.
  3. Safak, Ilgar; Warner, John C.; List, Jeffrey H. (2016-12-01). "Barrier island breach evolution: Alongshore transport and bay-ocean pressure gradient interactions". Journal of Geophysical Research: Oceans. 121 (12): 8720–8730. doi:10.1002/2016jc012029. hdl:1912/8812. ISSN 2169-9291.
  4. Swart, H. E. de; Zimmerman, J. T. F. (2009). "Morphodynamics of Tidal Inlet Systems". Annual Review of Fluid Mechanics. 41 (1): 203–229. doi:10.1146/annurev.fluid.010908.165159.

References

  • Bruun, Per; A.J. Mehta (1978). Stability of Tidal Inlets: Theory and Engineering. Amsterdam: Elsevier Scientific Pub. Co. p. 510. ISBN 978-0-444-41728-2. be pub co
This article is issued from Wikipedia. The text is licensed under Creative Commons - Attribution - Sharealike. Additional terms may apply for the media files.