Mississippi–Alabama barrier islands
The Mississippi–Alabama barrier islands are a chain of barrier islands in the Gulf of Mexico along the coasts of Mississippi and Alabama enclosing the Mississippi Sound. The major islands are Cat Island, Ship Island, Horn Island, Petit Bois Island, and Dauphin Island; in the early 20th century the chain also included the Isle of Caprice, which has since been submerged. The islands are separated by wide inlets, several of which have been channelized to form the shipping channels for Gulf coast ports. The shapes and sizes of the islands have changed significantly since the 1800s , with the islands generally shrinking and shifting westward, especially after major tropical cyclones. Most of the islands are uninhabited. Much of the Mississippi portion of the chain is included in the Gulf Islands National Seashore. Geography. The Mississippi–Alabama barrier island chain sits offshore from the Mississippi Gulf Coast and runs parallel to the coast for , roughly from the Bay of St. Louis to Mobile Bay, separating the Mississippi Sound from the Gulf of Mexico. The five main barrier islands, listed from west to east, are Cat Island, Ship Island (both in Harrison County, Mississippi), Horn Island, Petit Bois Island  (both in Jackson County, Mississippi), and Dauphin Island (in Mobile County, Alabama). Another smaller island called Dog Key Island or the Isle of Caprice has intermittently formed and vanished in the inlet between Ship Island and Horn Island; it is currently submerged. The only significant settlement on the island chain is the town of Dauphin Island, Alabama, which occupies the eastern half of that island; the rest of the islands are uninhabited. Portions of the four Mississippi islands have been included in the Gulf Islands National Seashore since its establishment in 1971. The islands have sandy beaches on both their  Gulf and Sound shores; the Gulf side beaches are wider and have finer sands due to the greater wave energy they face. The interiors include areas of sand flats, coastal marshes, dune fields, and brackish ponds. The islands are separated by wide inlets, several of which have been channelized through regular dredging to form deep-draft shipping channels. Ship Island Pass (between Cat Island and Ship Island) includes the shipping channel for Gulfport, Mississippi; Dog Keys Pass (between Ship Island and Horn Island) includes the channel for Biloxi, Mississippi; Horn Island Pass (between Horn Island and Petit Bois Island) includes  the channel for Pascagoula, Mississippi; Petit Bois Pass (between Petit Bois Island and Dauphin Island) has not been channelized; finally, the mouth of Mobile Bay, east of Dauphin Island, includes the channel for Mobile, Alabama. Geomorphology. The barrier islands are the above-water portions of a nearly continuous sand bar that runs the length of the Mississippi Sound. The bar is thought to have begun forming after about as the Gulf's mean sea level fell after the Holocene climatic optimum. The sand is primarily composed of white quartz, with a medium grain size. The shapes and sizes of the  islands have changed significantly since the 1800s, with the islands generally shrinking and drifting westward, in the direction of the predominant longshore current. This littoral current brings sand to the islands from sources to the east, but in recent centuries the chain has generally lost sand on balance. This is thought to be a result of a general weakening of the longshore current, together with the effects of man-made shipping channels (especially the Mobile Ship Channel), which function as sediment traps and subtract from the chain's sediment budget. The imbalance between sediment erosion and deposition has resulted in  the progressive retreat of the islands' shorelines, though the change has not been as rapid among the Mississippi–Alabama barrier islands as among the nearby barrier islands of Louisiana. Recurring major tropical cyclones have periodically altered the islands' shapes through wind, waves, and accompanying storm surges. Although severe storms often noticeably disrupt the morphologies and ecosystems of the islands on the timescale of days, vegetation and land area normally recover over a period of years following a major weather event. The gradual sea level rise in the Gulf during the past century has contributed to the decrease in land area  of the island chain, but the effect is not thought to have been large compared with the influence of the removal of sediment from the system through the dredging of shipping channels. Ecology. The interiors of the islands are vegetated, with pine forests on the higher ridges and marsh vegetation in the lower swales. The larger islands are inhabited by terrestrial animals such as raccoons and feral pigs, semiaquatic animals such as nutria, resident birds such as osprey, and migratory birds in season. The chain's sandy beaches serve as nesting grounds for Atlantic ridley sea turtles. Along the island  chain's north shore are extensive seagrass meadows, including such species as turtle grass, manatee grass, shoal grass, star grass, and wigeon grass. These seagrass beds provide food and habitats for a variety of aquatic fauna, including penaeid shrimp, blue crab, spotted seatrout, and other shellfish and finfish. Islands. Cat Island. Cat Island runs for along the western end of the Mississippi Sound, south of Gulfport. This island has maintained a relatively stable morphology since surveys began, partly due to its relatively high interior elevation. It has a T-shape, with northward and southward spits extending out from its eastern  end. Since surveys began, the southward spit has experienced more erosion than the northward one, and all parts of the island have narrowed. Ship Island. Ship Island runs for along the western part of the Mississippi Sound, south of Biloxi. This island has experienced major morphological changes over the past two centuries, with its eastern spit rapidly receding, and its narrow central segment shifting toward the mainland. The island's central portion has been repeatedly breached by major storms, most recently by Hurricane Camille in 1969; the so-called "Camille Cut" between the western and eastern portions of the island  was filled by the United States Army Corps of Engineers in 2019. Dog Key Island/Isle of Caprice. The shoals between Ship Island and Horn Island have intermittently formed small islands known as the Dog Keys (the namesake of Dog Keys Pass), which have been mapped at various dates between 1848 and 1940. Several smaller shoals grew together into one larger island around the beginning of the 20th century, appearing on a 1917 map from the United States Coast and Geodetic Survey, around long. In 1925 a group of property developers in Biloxi purchased this "Dog Key Island" from the  federal government, built a resort and casino on the island, and renamed it the "Isle of Caprice". By 1932, the island had entirely vanished beneath the surface. Horn Island. Horn Island runs for along the central part of the Mississippi Sound. Since surveys began, the island's east end has receded through erosion, while its west end has grown through spit formation at the down-current end. The east end has lost more land than the west has gained, and the island has generally narrowed over the same period. Petit Bois Island. Petit Bois Island runs for along the eastern  part of the Mississippi Sound, south of Pascagoula. This island has undergone the most dramatic morphological changes in the island chain during the past two centuries. The wider triangular segment that now forms the island's eastern end was its extreme western end as recently as the 1840s, but, as with neighboring Horn Island, the eastern spit has receded rapidly, while a new western tail has grown more slowly. Dauphin Island. Dauphin Island, which has over 1200 residents, runs for at the east end of the Mississippi Sound and marks the western edge of the mouth of Mobile Bay. The  eastern quarter of the island is wider and more elevated, while the western end is narrow and more prone to disturbance by storms. The east end includes the town of Dauphin Island. Since surveys began, the long western tail has generally lengthened, due to sand deposition from the longshore drift, and shifted toward the mainland, due to erosion on the Gulf shore and overwash during major storms.