Atchafalaya Basin

The Atchafalaya Basin and the surrounding plain of the Atchafalaya River is filled with bayous, baldcypress swamps, and marshes, which give way to brackish estuarine conditions and end in the Spartina grass marshes where the Atchafalaya River meets the Gulf of Mexico. It includes the Lower Atchafalaya River, the Wax Lake outlet, Atchafalaya Bay, and the Atchafalaya River and bayous Chêne, Boeuf, and Black navigation channel. The basin, which is susceptible to long periods of deep flooding, is sparsely inhabited. The basin is about in width from east to west and in length. The basin is the largest existing wetland in the United States with an area of , including the surrounding swamps outside of the levees that historically were connected to the basin. The basin contains nationally significant expanses of bottomland hardwoods, swamplands, bayous, and back-water lakes. The thousands of acres of forest and farmland are home to the Louisiana black bear (Ursus americanus luteolus), which has been on the United States Fish and Wildlife Service threatened list since 1992. The few roads that cross the basin follow the tops of levees. Interstate 10 crosses on elevated pillars on the continuous Atchafalaya Basin Bridge from Grosse Tête to Henderson. The Atchafalaya National Wildlife Refuge was established in 1984 to improve plant communities for endangered and declining species of wildlife, waterfowl, migratory birds and alligators. ==Hydrogeology==

The basin has a long relationship with the Mississippi River throughout the Holocene epoch, and the geology of the modern basin is a direct manifestation of that relationship. The central basin is further bordered by man-made levees designed to contain and funnel floodwaters released from the Mississippi at the Old River Control Structure and the Morganza Spillway south toward Morgan City and eventually to the Gulf of Mexico. Historically there were small and few channel connections to the Mississippi River. The historic lack of significant channel connection indicates that the Atchafalaya Basin did not receive significant sediment from the Mississippi except during large floods. During the mid-19th century, manmade channel alterations, including the removal of a large log jam and dredging, permanently connected the Atchafalaya River to the Mississippi River. From then until the completion of the Old River Control Structure in 1963, the Mississippi was increasingly diverting flow into the shorter and steeper path of the Atchafalaya channel. By law, a regulated 30 percent of the latitudinal flow water from the Mississippi, Red and Black rivers is diverted into the Atchafalaya at the Old River Control Structure. This flow diverts on average 25 percent of the Mississippi River flow down the Atchafalaya. In times of extreme flooding, the US Army Corps of Engineers (USACE) may open the Morganza Spillway and other spillways to relieve pressure on levees and control structures along the Mississippi. On May 13, 2011, in the face of a rising Mississippi River that threatened to flood New Orleans and other heavily populated parts of Louisiana, USACE ordered the Morganza Spillway opened for the first time since 1973. This water floods the Atchafalaya Basin between the levees along the western and eastern limits of the Morganza and Atchafalaya basin floodways. ==Ecology==

The control of the river's floods, along with those of the Mississippi River, has become a controversial issue in recent decades. The US Geological Survey (USGS) reports that Mississippi River delta salt marshes are wetlands degrading at a rate of . The Atchafalaya River deltas are the only locations of land growth along the Louisiana Gulf Coast. During the early 20th century, the basin was designated as a spillway for floods of the Mississippi River. In order to facilitate this emergency plan without flooding adjacent agriculture and towns, protective levees were built dividing the Atchafalaya Basin Floodway from large portions of the historic swamp boundaries. A central channel was dredged through some existing channels and in some places through swamp forest. At that point the isolated basin was permanently connected to a very large, sediment-rich river. When the flow plan was implemented (1950–1974), 30 percent of the total Atchafalaya River flow was designated to be directed off the main channel, 15 percent to the east and 15 percent to the west side. As a result of the Atchafalaya River channel bed incision, in the early 21st century the flow distribution is 13 percent of the total flow, with a flow distribution of 7 percent to the east side and 6 percent to the west side as reported by the USGS. This decrease in flow across the floodplain, in conjunction with high organic deposition from trees and floating vegetation and high water temperature, has resulted in large areas of low-dissolved oxygen water. Where once the water was black (1850), the water became brown (1927). Where the water was formerly brown (1927), it is now black (2009). During the period of 1960–1980, oil and gas exploration and development in Louisiana increased dramatically. Numerous large access canals and pipeline canals were dredged through deep swamp areas, across bayous, and across the Atchafalaya River. In some areas of the basin, there are or more of access canals to every of natural bayou. These large channels ( wide by deep) have fundamentally changed the hydrology of the swamps. Deep swamp areas that were hydraulically isolated from sediment were connected directly to the river and its sediment and suffered rapid filling. The USGS has measured sediment deposition rates of up to per year where these channels enter open water, and per year on adjacent floodplains. In some places natural bayous have filled in due to flow capture by access canals. Spoil material from the canals was deposited adjacent to the canals, further impeding the natural flow across the floodplain. == Bayou Chene ==

From 1830 to 1953, the community of Bayou Chene thrived as a center for logging, hunting, trapping, and fishing in the heart of the Atchafalaya Basin. Now buried underneath at least 12 feet of silt, Bayou Chene is one of several abandoned communities in the midst of the basin. The earliest settlers of the Bayou Chene region were the native Chitimacha tribe. Several villages important to the Chitimacha were located around Bayou Chene including the Village of Bones or Namu Katsi and the Cottonwood Village, known as Kushuh Namu in the Chitimacha language. One of the earliest written accounts of the Bayou Chene region comes from French explorer C.C. Robin who, while paddling through the basin in 1803, wrote: By 1841, between 15 and 20 families were farming along the banks of "Oak Bayou" or Bayou Chene. The population rose quickly over the next 20 years, as the United States Census of 1860 records 675 residents in the community. Writing about her family's experiences in the region, Gwen Roland describes how the community relied upon the basin's waters for everything, including transportation: The Great Mississippi Flood of 1927 nearly demolished the community. Rising seven feet above natural levees, the floodwaters inundated Bayou Chene for weeks. The Great Depression hit the residents of Bayou Chene hard, but many former residents look fondly on the massive flood control projects promulgated by the U.S. Army Corps of Engineers that provided gainful employment during the period. As a result of the 1927 flood, the entire basin was designated an official floodway, and a series of man-made levees were built that would permanently alter flooding patterns in the region. Further flooding in 1937 encouraged many residents to move their homes to higher ground, but even these measures were not enough to protect the community from annual flooding. After years of rising waters, the community came to an end with the closing of the post office at Bayou Chene in 1952. Most of Bayou Chene's former residents relocated to the fringes of the basin in towns like New Iberia, St. Martinville, and Breaux Bridge. ==Gallery==

File:AtchafalayaBay.jpg|Aerial view of the Big Island Mining Project restoration site on Atchafalaya Bay File:AB Bridge I-10.jpg|View of the south side of the I-10 bridge crossing the basin File:AtchafalayaBasinPanorama.jpg|Panorama of the Atchafalaya Basin ==See also==