The United Nations Convention on the Law of the Sea defines a bay as a well-marked indentation in the coastline. This legal definition requires that the penetration of the land into the water be proportional to the width of its mouth. If an area is too small, it becomes merely a curvature and not a bay under international law. A specific geometric test determines this status. The area impounded by the bay must exceed that of a semicircle drawn across its mouth. That line connects two points at the entrance of the indentation. If the calculation fails, the body of water is classified as a bight instead. This distinction matters because it dictates whether waters are considered inland or open sea.
Classifying Coastal Shapes
Open bays appear widest at their mouths and flank headlands on either side. Enclosed bays possess mouths narrower than their widest internal parts. These enclosed forms often sit flanked by at least one peninsula jutting from the mainland. Semi-enclosed types exist when islands create narrower channels within the exit of an open bay. Back-barrier bays separate themselves from open water via barrier islands or spits. Each category reflects distinct physical geography rather than arbitrary naming conventions. The Bay of Bengal stands as the world's largest bay with varied marine geology inside its boundaries. James Bay serves as an example where one bay nests entirely within another larger body called Hudson Bay.Tectonic And Glacial Origins
The largest bays developed through plate tectonics during the Paleozoic era. As the super-continent Pangaea broke apart along curved fault lines, continents moved away to leave large indentations. The Gulf of Guinea formed this way alongside the Gulf of Mexico. Glaciers also carved out specific shapes known as fjords. Heavily glaciated areas like Vyborg Bay on the Gulf of Finland show these deep cuts clearly. Rivers create rias which feature more gradual slopes compared to steep fjord walls. Softer rocks erode rapidly while harder rocks resist erosion to form headlands. This differential erosion creates the irregular coastlines seen around the globe today.