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Bay
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A bay is a recessed, body of water that directly connects to a larger main body of water, such as an , a , or another bay. A large bay is usually called a gulf, , sound, or bight. A is a small, circular bay with a narrow entrance. A is an elongated bay formed by glacial action. The term embayment is also used for , such as extinct bays or freshwater environments.

A bay can be the of a river, such as the , an estuary of the Susquehanna River. Bays may also be nested within each other; for example, is an arm of in . Some large bays, such as the Bay of Bengal and Hudson Bay, have varied .

The land surrounding a bay often reduces the strength of and blocks . Bays may have as wide a variety of shoreline characteristics as other shorelines. In some cases, bays have beaches, which "are usually characterized by a steep upper foreshore with a broad, flat fronting terrace".Maurice Schwartz, Encyclopedia of Coastal Science (2006), p. 129. Bays were significant in the history of because they provided easy access to marine resources like . Later they were important in the development of sea as the safe they provide encouraged their selection as .


Definition
The United Nations Convention on the Law of the Sea defines a bay as a well-marked indentation in the coastline, whose penetration is in such proportion to the width of its mouth as to contain land-locked waters and constitute more than a mere curvature of the coast. An indentation, however, shall not be regarded as a bay unless its area is as large as (or larger than) that of the whose is a line drawn across the mouth of that indentation — otherwise it would be referred to as a bight. United Nations Convention on the Law of the Sea


Types
  • Open bay — a bay that is widest at the mouth, flanked by .
  • Enclosed bay — a bay whose mouth is narrower than its widest part, flanked by at least one .
  • Semi-enclosed bay — an open bay whose exit is made into narrower channels by one or more within its mouth.
    • Back-barrier bay — a semi-enclosed bay separated from open water by one or more or spits.


Formation
There are various ways in which bays can form. The largest bays have developed through .
(1982). 9780112022572, The Hamlyn Publishing Group.
As the super-continent broke up along curved and indented fault lines, the continents moved apart and left large bays; these include the Gulf of Guinea, the Gulf of Mexico, and the Bay of Bengal, which is the world's largest bay.

Bays also form through coastal by rivers and . A bay formed by a glacier is a . are created by rivers and are characterised by more gradual slopes. Deposits of softer rocks erode more rapidly, forming bays, while harder rocks erode less quickly, leaving .


See also

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